Abbot, D. S. and Pierrehumbert, T. T. (2010). Mudball: surface dust and Snowball Earth deglaciation. Geophys. Res. Lett., 115: D03104, doi: 10.1029/2009JD012007.Google Scholar

Abdalati, W. (2007). Greenland Ice Sheet melt characteristics derived from passive micro-wave data. Boulder, CO: National Snow and Ice Data Center. Digital media.Google Scholar

Abdalati, W. and Steffen, K. (1997). Snowmelt on the Greenland Ice Sheet as derived from passive microwave satellite data. J. Climate, 10: 165–75.Google Scholar

Abdalati, W. and Steffen, K. (2001). Greenland Ice Sheet melt extent: 1979–1999. J. Geophys. Res., 106 (D24): 33, 983–8.Google Scholar

Abel, G. (1955). Températures et formation de glace dans les grottes du Salzburg (Autriche), Proc. 1st Int. Cong. Speleol., Paris, 1953. 2: 321–4.Google Scholar

Ablain, M., et al. (2017). TOPEX-A Drift and Impacts on GMSL Time Series, https://meetings.aviso.altimetry.fr/fileadmin/user_upload/tx_ausyclsseminar/files/Poster_OSTST17_GMSL_Drift_TOPEX-A.pdf.Google Scholar

Abram, N. J., Wolff, E. W., and Curran, M. A. J. (2013). A review of sea ice proxy information from polar ice cores. Quat. Sci. Rev., 79: 168–83, doi: 10.1016/j.quascirev.2013.01.01.Google Scholar

Abramov, V. A. (1992). Russian iceberg observations in the Barents Sea, 1933–1990. Polar Res., 11: 93–7.Google Scholar

Abramov, V. A. (1996). Atlas of Arctic icebergs. Fair Lawn, NJ: Backbone Publishing Co. 70 pp.Google Scholar

ACIA (2005). Arctic climate impact assessment. New York: Cambridge University Press, 1042 pp.Google Scholar

Ackerman, S. A., et al. (1998). Discriminating clear sky from clouds with MODIS, J. Geophys. Res., 103 (D24): 32, 141–57.Google Scholar

Ackerman, S. A., et al. (1995). Cirrus cloud properties derived from high spectral resolution infrared spectrometry during FIRE II .2. Aircraft HIS results, J Atmos. Sci., 52: 4246–63.Google Scholar

Ackley, S. F. (1979). Mass-balance aspects of Weddell sea pack ice. J. Glaciol., 24 (90): 391–405.Google Scholar

Ackley, S. F. (1996). Sea ice. In Trigg, George L et al., (eds.), Encyclopedia of applied physics. New York: VCH Publishers. 17: pp. 81–103.Google Scholar

Ackley, S. F., Lange, M., and Wadhams, P. (1990). Snow cover effects on Antarctic sea ice thickness. In Ackley, S. F. and Weeks, W. F. (eds.), Sea ice properties and processes. CRREL Monograph 90–1. Hanover, NH: US Army Cold Regions Research and Engineering Laboratory Engin. Lab. pp. 225–9.Google Scholar

Adam, J. C., Hamlet, A. F., and Lettenmaier, D. P. (2009). Implications of global climate change for snowmelt hydrology in the twenty-first century. Hydrol. Proc., 23: 962–72.Google Scholar

Adams, P. (1992). J. B. Tyrell and D. H. Dunble on lake ice. Arctic 45: 195–8.Google Scholar

Adrian, R. and Hintze, T. (2000). Effects of winter air temperature on the ice phenology of the Müggelsee (Berlin, Germany). Verh. Int. Verein. Limnol., 27: 2808–11.Google Scholar

Adusumilli, S., Fricker, H. A., Siegfried, M. R., Padman, L., Paolo, F. S., and Ligtenberg, S. R. M. (2018). Variable basal melt rates of Antarctic Peninsula ice shelves, 1994–2016, Geophys. Res. Lett., 45: 4086–95, doi: 10.1002/2017GL076652.Google Scholar

Afultis, M. A. (1987). Iceberg populations south of 48° N since 1900. Report of the International Ice Patrol in the North Atlantic. Bull. No. 74, CG 188–42. U.S. Dept. of Transportation, U.S. Coast Guard. pp. 63–7, 358.Google Scholar

Afultis, M. A. and Martin, S. (1987). Satellite passive microwave studies of the Sea of Okhotsk ice cover and its relation to oceanic processes, 1978–1982. J. Geophys. Res., 92: 13,013–28.Google Scholar

Agassiz, L. (1967). Studies on glaciers (trans. of Agassiz, L. 1840 Études sur les glaciers, trans., ed. Carozzi, A. V). New York: Hafner Publ. Co. 213 pp.Google Scholar

Ahlmann, H. W. (1924). Le niveau de glaciation comme fonction de l’accumulation d’humidité sous forme solide. Geogr. Ann, 6: 223–72.Google Scholar

Ahlmann, H. W. (1935). Scientific results of the Norwegian-Swedish Spitsbergen Expedition in 1934. Part V. Geogr. Annal., 17: 167–218.Google Scholar

Ahlmann, H. W. (1948). Glaciological research on the North Atlantic coast. Roy. Geogr. Soc., Res. Ser., no. 1. 83 pp.Google Scholar

Ahlmann, H. W. and Tryselius, O. (1929). Der Kårsa Gletscher in Swedisch Lappland. Geogr. Annal., 11: 1–32.Google Scholar

Aizen, V. B., et al. (2006). Glacier changes in the central and northern Tien Shan during the last 140 years based on surface and remote-sensing data. Annals Glaciol., 43: 202–13.CrossRefGoogle Scholar

Alekseyev, V. R., et al. (eds.). (1973). Siberian naleds. USSR Academy of Sciences (1969). Draft Translation 399. Hanover, NH: US Army Cold Regions Research and Engineering Laboratory. 300 pp.Google Scholar

Alexeev, S. V., Alexeeva, L. P., and Kononov, A. M. (2008). Permafrost and cryopegs of the Anabar shield. In Kane, D. L. and Hinkel, K. M. (eds.), Proceedings of the ninth international conference on permafrost, Fairbanks, AK: University of Alaska, Institute of Northern Engineering. pp. 31–5.Google Scholar

Alford, D. and Armstrong, R. (2010). The role of glaciers in stream flow from the Nepal Himalaya. The Cryosphere Discuss, 4: 469–94.Google Scholar

Allen, C., et al. (1997). Airborne radio echo sounding of outlet glaciers in Greenland, Int. J. Re. Sens. 18(14): 3103–8.Google Scholar

Allen, J. R. and Long, D. G. (2006). Microwave observations of daily Antarctic sea-ice edge expansion and contraction rates. IEEE Geosci. Remote Sensing Lett., 3: 54–8.Google Scholar

Allen, P. A. and Etienne, J. L. (2008). Sedimentary challenge to Snowball Earth. Nat. Geosci., 1: 818–25.Google Scholar

Alley, R. B. (2000). The two-mile time machine: ice cores, abrupt climate change, and our future. Princeton, NJ: Princeton University Press. 229 pp.Google Scholar

Alley, R. B., et al. (2009). Past extent and status of the Greenland Ice Sheet. In Alley, R. B., Brigham-Grette, J., Miller, G. H., and Polyak, L., (eds.), Past climate variability and change in the Arctic and at high latitudes. U.S. Climate Change and Science Program, Synthesis and Assessment 1.2. Reston, VA: US Geological Survey. pp. 303–415.Google Scholar

Alley, R. B., et al. (2010). History of the Greenland Ice Sheet: Paleoclimatic insights. Quat. Sci. Rev., 29 (15–16): 1728–56.Google Scholar

Alley, R. B. and Clark, P. U. (1999). The deglaciation of the Northern Hemisphere: a global perspective. Ann. Rev. Earth Planet. Sci., 27: 149–82.Google Scholar

Allison, I., Barry, R. G., and Goodison, B. E. (2001). Climate and cryosphere (CliC) project science and co-ordination plan (Version 1). Geneva: World Meteorological Organization. WMO/TD 1053, 96 pp.Google Scholar

Allison, I. and Kruss, P. (1977). Estimation of recent climatic change in Irian Jaya by numerical modeling of its tropical glaciers. Arct. Alp. Res., 9: 49–60.Google Scholar

Allison, I. and Peterson, J. A. (1976). Ice areas on Puncak Jaya – their extent and recent history. In Hope, G. S., Peterson, J. A., Radok, U., and Allison, I. (eds.), The equatorial glaciers of New Guinea – results of the 1971–1973 Australian Universities’ expeditions to Irian Jaya: survey, glaciology, meteorology, biology and paleoenvironments. Rotterdam: A. A. Balkema. pp. 27–38.Google Scholar

Allix, A. (1924). Avalanches. Geogr. Rev., 14 (4): 519–60.CrossRefGoogle Scholar

Alvarez-Solas, J., et al. (2010). Links between ocean temperature and iceberg discharge during Heinrich Events. Natur Geeosci., 3: 122–6.Google Scholar

AMAP (2017). Snow, water, ice and permafrost in the Arctic (SWIPA). Oslo, Norway:Arctic Council Secretariat.Google Scholar

Anacona, P. I., Mackintosh, A., and Norton, K. P. (2015). Hazardous processes and events from glacier and permafrost areas: lessons from the Chilean and Argentinean Andes. Earth Surf. Proc. Land., 40 (1): 2–21, 37, doi: 10.1002/esp.3524.Google Scholar

Anandakrishnan, S., et al. (2007). Discovery of till deposition at the grounding line of Whillans Ice Stream. Science, 315: 1835–8.Google Scholar

Anderson, E. A. (1976). A point energy and mass balance model of a snow cover, NOAA Technical Report NWS, 19: 150 pp.Google Scholar

Andersen, S., et al. (2007). Intercomparison of passive microwave sea ice concentration retrievals over the hh-concentration Arctic sea ice. J. Geophys. Res., 112: C08004. doi: 10.1029/2006JC003543.Google Scholar

Anderson, M. R., Crane, R. G., and Barry, R. G. (1985). Characteristics of Arctic Ocean ice determined from SMMR data for 1979: case studies in the seasonal sea ice zone. Adv. Space Res,. 5 (6) G. Ohring and H. J. Bolle (eds.). Space Observations for Climate Studies: 257–61.Google Scholar

Anderson, R. K., et al. (2008). A millennial perspective on Arctic warming from 14 C in quartz and plants emerging from beneath ice caps. Geophys. Res. Lett., 35: L01502. doi: 10.1029/2007GL032057.Google Scholar

Andreadis, K. M. and Lettenmaier, D. P. (2006). Assimilating remotely sensed snow observations into a macroscale hydrology model. Adv. Water Resour., 29: 872–86.Google Scholar

Andreas, E. L., et al. (1990). Lidar-derived particle concentrations in plumes from Arctic leads. Annals Glaciol., 14: 9–12.Google Scholar

Andreas, E. L., Jordan, R. E., and Makshtas, A. P. (2005). Simulations of snow, ice, and near-surface atmospheric processes on Ice Station Weddell. Bound.-Layer Met., 114: 439–60.Google Scholar

Andrews, J. T. (2000). Icebergs and iceberg rafted detritus (IRD) in the North Atlantic: facts and assumptions. Oceanography, 13 (3): 100–8.Google Scholar

Andrews, J. T. and Miller, G. H. (1972): Quaternary history of northern Cumberland Peninsula, Baffin Island, N.W.T., Canada. Part IV: maps of the present glaciation limits and lowest equilibrium line altitude for north and south Baffin Island. Arct. Alp. Res., 4: 45–59.Google Scholar

Andreescu, M.-P. and Frost, D. B. (1998). Weather and traffic accidents in Montreal, Canada. Clim. Res., 9: 225–30.Google Scholar

Anisimov, O. A. (1989) Changing climate and permafrost distribution in the Soviet Arctic. Phys. Geog., 10(3): 285–93.Google Scholar

Anisimov, O. A. and Nelson, F. E. (1990). Application of mathematical models to investigate the interaction between the climate and permafrost. Soviet Met. Hydrol., 1990 (10): 8–13.Google Scholar

Anisimov, O. A. and Nelson, F. E. (1996). Permafrost distribution in the Northern Hemisphere under scenarios of climatic change. Global Planet. Change, 14: 59–72.Google Scholar

Anisimov, O. A. and Nelson, F. E. (1997). Permafrost zonation and climate change in the Northern Hemisphere: results from transient general circulation models. Clim. Change, 35: 241–58.Google Scholar

Anisimov, O. A. and Reneva, S. (2006). Permafrost and changing climate: the Russian perspective. Ambio, 35 (4): 169–75.Google Scholar

Anisimov, O. A., Shiklomanov, N. I., and Nelson, F. E. (1997). Global warming and active layer thickness: results from transient general circulation models. Global Planet. Change, 15: 61–77.Google Scholar

Anisimov, O. A., Shiklomanov, N. I., and Nelson, F. E. (2002). Variability of seasonal thaw depth in permafrost regions: A stochastic modelling approach. Ecol. Modelling, 153: 217–27.Google Scholar

Aniya, M., et al. (1996). Inventory outlet glaciers of the Southern Patagonia Icefield, South America. Photogram, Eng, Rem. Sensing, 62: 1361–9.Google Scholar

Anschutz, H., et al. (2009). Revisiting sites of the South Pole Queen Maud Land Traverses in East Antarctica: Accumulation data from shallow firn cores. J. Geophys. Res., 114: D24106, doi: 10.1029/2009JD012204.Google Scholar

Arctic and Antarctic Research Institute. (2007). Sea ice charts of the Russian Arctic in gridded format, 1933–2006. Edited and compiled by Smolyanitsky, V., et al., Boulder, CO: National Snow and Ice Data Center. Digital media.Google Scholar

Arctic Climatology Project. (2000). Environmental Working Group joint U.S.-Russian sea ice atlas. Tanis, F. and Smolyanitsky, V. (eds.). Ann Arbor, MI: Environmental Research Institute of Michigan in association with the National Snow and Ice Data Center. CD-ROM.Google Scholar

Arctic Report Card (2009). www.arctic.noaa.gov/reportcard/Google Scholar

Arendt, A., et al. (2002). Rapid wastage of Alaska glaciers and their contribution to rising sea level. Science, 297 (5580): 382–6.CrossRefGoogle ScholarPubMed

Arendt, A. A., et al. (2009). Validation of high-resolution GRACE mascon estimates of glacier mass changes in the St. Elias Mountains, Alaska, USA, using aircraft laser altimetry. J. Glaciol., 54 (188): 778–87.Google Scholar

Arendt, A., et al. (2012). Randolph Glacier Inventory [v2.0]: A Dataset of Global Glacier Outlines. Global Land Ice Measurements from Space, Boulder Colorado, USA. Digital Media 32 pp. Available online at: http://www.glims.org/RGI/RGI_Tech_Report_V2.0.pdfGoogle Scholar

Arendt, A., et al. (2015). Randolph Glacier Inventory – A Dataset of Global Glacier Outlines: Version 5.0. Boulder, CO, USA: Global Land Ice Measurements from Space.Google Scholar

Arenstein, J. (1849). Beobachtungen über die Eisverhältnisse der Donau. 1847/48 und 1848/49. Wissenschaft, Vienna: Sitzunsgbericht Akad. 5: 331.Google Scholar

Armitage, T. W. K., Bacon, S., and Kwok, R. (2018). Arctic sea level and surface circulation response to the Arctic Oscillation. Geophy. Res. Lett., 45: 6576–84.Google Scholar

Armour, K. C. et al. (2016). Southern Ocean warming delayed by circumpolar upwelling and equatorward transport. Nat. Geosci., 9 (7): 549, doi: 10.1038/Ngeo2731.Google Scholar

Armstrong, B. R. and Williams, K. (1986). The avalanche book. Golden, CO: Fulcrum. 240 pp.Google Scholar

Armstrong, R. (2001). Historical Soviet daily snow depth version 2 (HSDSD). Boulder, CO: National Snow and Ice Data Center. CD-ROM.Google Scholar

Armstrong, R. L., Brodzik, M. J., Savoie, M., and Knowles, K., (2006). Multi-Sensor snow mapping and global trends, WDC for Glaciology, Boulder, 30th Anniversary Workshop, University of Colorado, Boulder, October 25, 2006.Google Scholar

Armstrong, R., Alford, D., and Racoviteanu, A. (2009). Glaciers as indicators of climate change – the special case of the high elevation glaciers of the Nepal Himalaya. In Water storage. A strategy for climate change adaptation in the Himalaya. Sustainable Mountain Development No. 56. Kathmanudu, Nepal: ICIMOD. pp. 16–18.Google Scholar

Armstrong, R. L. and Armstrong, B. R. (1987). Snow and avalanche climates of the western United States: A comparison of maritime, intermountain and continental conditions. Avalanche Formation, Movement and Effects. IAHS Publ., 162: 282–94.Google Scholar

Armstrong, R. and Brodzik, M. J. (2002). Hemispheric-scale comparison and evaluation of passive microwave snow algorithms. Annals Glaciol., 34: 38–44.Google Scholar

Armstrong, R., Brodzik, M. J., and Savoie, M. H. (2003). Multi-sensor approach to mapping snow cover using data from NASA’s EOS Aqua and Terra spacecraft (AMSR-E and MODIS). Boulder, CO: National Snow and Ice Data Center (NSIDC), University of Colorado.Google Scholar

Armstrong, R. L., Brodzik, M. J., Knowles, K., and Savoie, M. (2005). Global monthly EASE-Grid snow water equivalent climatology. Boulder, CO: National Snow and Ice Data Center. Digital media.Google Scholar

Armstrong, R. L. and Brun, E. (eds.) (2008). Snow and climate: Physical processes, surface energy exchange and modeling. Cambridge: Cambridge University Press. 222 pp.Google Scholar

Armstrong, R. L. (2010). The glaciers of the Hindu Kush–Himalayan region. Technical Paper. Kathmandu, Nepal: CIMOD. 20 pp.Google Scholar

Armstrong, R. L., and Brodzik, M. J. (2001). Recent Northern Hemisphere snow extent: a comparison of data derived from visible and microwave sensors. Geophy. Res. Lett., 28 (19): 3673–6.Google Scholar

Armstrong, T. E. (1952). The northern sea route: Soviet exploitation of the North East Passage. Cambridge: Scott Polar Research Institute. Special publ. no. 1, 20 pp.Google Scholar

Arzel, O., Fichefet, T., and Goosse, H. (2006). Sea ice evolution over the 20th and 21st centuries as simulated by current AOGCMs. Ocean Modelling, 12: 401–15.Google Scholar

Ashton, G. D. (1980). Freshwater ice growth, motion, and decay. In Colbeck, S. C. (ed.), Dynamics of snow and ice masses. New York: Academic Press. pp. 261–304.Google Scholar

Aspen Environmental Group and Cubed, M. (2005). Potential changes in hydropower production from global climate change in California and the western United States. CEC-700–2005–010. California Energy Commission. 65 pp.Google Scholar

Asplin, M. G., Lukovich, J. V., and Barber, D. G. (2009). Atmospheric forcing of the Beaufort Sea ice gyre: Surface pressure climatology and sea ice motion. J. Geophys. Res., 114 (D00D05): 9.Google Scholar

Assel, R. and Herche, L. (2000). Coherence of long-term lake ice records. Verh. Int. Verein. Limnol., 27: 2789–92.Google Scholar

Assel, R., Cronk, K., and Norton, D. (2003). Recent trends in Laurentian Great Lakes ice cover. Clim. Change 57: 185–204.Google Scholar

Ashton, G. D. (ed.) (1986). River and lake ice engineering. Highlands Ranch, CO: Water Resources Publication. 486 pp.Google Scholar

Astakov, V. I. (1986). Geological conditions for the burial of Pleistocene glacier ice on the Yensisey. Polar Geog. Geol., 10: 286–95.Google Scholar

Atkinson, D. E., et al. (2006). Canadian cryospheric responses to an anomalous warm summer: synthesis of the climate change action fund project the state of the arctic cryosphere during the extreme warm summer of 1998. Atmos.-Ocean, 44: 347–76.Google Scholar

Aubekerov, B. and Gorbunov, A. P. (1999). Quaternary permafrost and mountian glaciation in Kazakhstan. Permafrost Periglac. Proc., 10: 65–80.Google Scholar

Ávila, E. E., et al. (2009). Initial stages of the riming process on ice crystals, Geophys. Res. Lett., 36: L09808. doi:10.1029/2009GL037723.Google Scholar

Bader, H. (1961). The Greenland ice sheet, CRREL Mongr, I B2; Hannover, NH, US Army Cold Regions Research and Engineering Laboratory, 18 pp. https://erdc-library.erdc.dren.mil/jspui/bitstream/11681/2674/1/CRREL-Mono-1-B2.pdfGoogle Scholar

Bader, H., et al. (1939). Der Schnee und seine Metamorphose. Beitr. Geologie der Schweiz, Geotechnische Serie-Hydrologie, Issue 3. Bern: Kümmerly and Frey, (In English as Snow and its metamorphosis. Snow, Ice and Permafrost research Establishment, SIPRE Translation No. 14, 1954, 313 pp.)Google Scholar

von Baer, K. E. (1838a). On the ground ice or frozen soil of Siberia. J. Roy. Geog. Soc., 8: 210–13.Google Scholar

von Baer, K. E. (1838b). Intelligence upon the frozen ground in Siberia. J. Roy. Geog. Soc., 8: 401–6.Google Scholar

Bahr, D. B. (1997a). Global distribution of glacier properties: A stochastic scaling paradigm. Water Resour. Res., 33: 1669–79.Google Scholar

Bahr, D. B. (1997b). Width and length scaling of glaciers. J. Glaciol., 43 (145): 557–62.Google Scholar

Bahr, D. and Dyurgerov, M. B. (1999). Characteristic mass-balance scaling with valley glacier size. J. Glaciol., 45 (149): 17–21.Google Scholar

Bahr, D. B., Dyurgerov, M., and Meier, M. F. (2009). Sea-level rise from glaciers and ice caps: A lower bound. Geophys. Res. Lett., 36: L03501. doi: 10.1029/2008GL036309.Google Scholar

Bahr, D. B., Meier, M. F., and Peckham, S. D. (1997). The physical basis of glacier volume – area scaling. J. Geophys. Res., 102 (B9): 20, 355–62.Google Scholar

Bakkehøi, S. Domaas, U., and Lied, K. (1983). Calculation of snow avalanche run-out distance. Annal. Glaciol., 4: 24–9.Google Scholar

Ballantyne, J. and Long, D. G. (2002). A mulitdecadal study of the number of Antarctic icebergs using scatterometer data. Geoscience and Remote Sensing Symposium 2002, IGARSS ’02, IEEE International, vol. 5: 3029–31. https://ieeexplore.ieee.org/stamp/stamp.jsp?arnumber=1237370Google Scholar

Bales, R. C., et al. (2009). Annual accumulation for Greenland updated using ice core data developed during 2000–2006 and analysis of daily coastal meteorological data. J. Geophys. Res., 114 (D06115): 14.Google Scholar

Baldocchi, D. D., Matt, D. R., Hutchison, B. A., and McMillen, R. T. (1984). Solar radiation within an oak-hickory forest: an evaluation of the extinction coefficients for several radiation components for fully-leafed and leafless periods. Agric. For. Meteorol., 32: 307–22.Google Scholar

Bamber, J. L. (1994). Ice sheet altimeter processing scheme. Int. J. Remote Sens., 15: 925–38.Google Scholar

Bamber, J. L., Alley, R. B., and Joughin, I. (2007). Rapid response of modern day ice sheets to external forcing. Earth Planet. Sci. Lett., 257: 1–13.Google Scholar

Bamber, J. L. and Bentley, C. R. (1994). Comparison of satellite-altimetry and ice-thickness measurements of the Ross Ice Shelf, Antarctica. Ann. Glaciol., 20: 357–64.Google Scholar

Bamber, J. L. and Kwok, R. (2004). Remote sensing techniques. In Bamber, J. L. and Payne, A. J. (eds.), Mass balance of the cryosphere: Observations and modelling of contemporary and future changes. Cambridge: Cambridge University Press. pp. 59–113.Google Scholar

Bamber, J. L. and Payne, A. J. (eds.). (2004). Mass balance of the cryosphere: Observations and modelling of contemporary and future changes. Cambridge: Cambridge University Press. 666 pp.Google Scholar

Bamber, J. L. and Rivera, A. (2007). A review of remote sensing methods for glacier mass balance determination. Glob. Planet. Change, 59: 133–48.Google Scholar

Bamber, J. L., Vaughan, D. G., and Joughin, I. (2000). Widespread complex flow in the interior of the Antarctic Ice Sheet. Science 287 (5456): 1248–50.Google Scholar

Bamber, J. L., et al. (2009). Reassessment of the potential sea-level rise from a collapse of the West Antarctic Ice Sheet. Science 324: 901–3.Google Scholar

Bamber, J. L., Westaway, R. M., Marzeion, B., and Wouters, B. (2018). The land ice contribution to sea level during the satellite era, Environ. Res. Lett., 13 (6): 063008, doi:10.1088/1748-9326/aac2f0.Google Scholar

Barber, D. G., et al. (2001a). Physical processes within the North Water (NOW) polynya, Atmosphere – Ocean, 39 (3): 163–6.Google Scholar

Barber, D. G., et al. (2001b). Sea-ice and meteorological conditions in Northern Baffin Bay and the North Water Polynya between 1979 and 1996. Atmosphere – Ocean 39 (3): 343–59.Google Scholar

Barber, D. G. and Massom, R. A. (2007). The role of sea ice in bipolar polynya processes. In Smith, W. O. and Barber, D. G. (eds.), Polynyas: Windows into polar oceans. New York: Elsevier. 474 pp.Google Scholar

Barclay, D. J., Wiles, G. C., and Calkin, P. E. (2009). Holocene glacier fluctuations in Alaska, Quat. Sci. Rev. 28: 2034–48.Google Scholar

Bareiss, J. and Görgen, K. (2005). Spatial and temporal variability of sea ice in the Laptev Sea: and review of satellite passive-microwave data and model results, 1979 to 2002. Glob. Planet. Change 48: 28–54.Google Scholar

Barendregt, R. W. and Dud-Rodkin, A. (2004). Chronology and extent of Late Cenozpic ice sheets in North America: A magnetostratigraphic assessment. In Ehlers, J. and Gibbard, P. L. (eds.), Quaternary glaciations extent and chronology. Part 2. North America. Amsterdam: Elsevier. pp. 1–8;Google Scholar

Barendregt, R. and Irving, E. (1998). Changes in the extent of North American ice sheets during the late Cenozoic. Can. J. Earth Sci. 35 (5): 504–9.Google Scholar

Barichivich, J., Briffa, K. R., and Myneni, R. B., et al. (2013). Large-scale variations in the vegetation growing season and annual cycle of atmospheric CO₂ at high northern latitudes from 1950 to 2011. Glob. Chang. Biol., 19: 3167–83, doi: 10.1111/gcb.12283.Google Scholar

Barker, P. F., Dickmann, B., and Escutia, C. (2007b). Onset of Cenozoic Antarctic glaciation. Deep-Sea Res. II, 54: 2293–307.Google Scholar

Barker, P. F., et al. (2007a). Onset and role of the Antarctic Circumpolar Current, Deep-sea Res. Part 2. Topical Studies in Oceanography, 54 (21–22): 2388–98.Google Scholar

Barker, S., et al. (2009). Interhemispheric Atlantic seesaw response during the last deglaciation. Nature, 457: 1097–103.Google Scholar

Barletta, , V. R., et al. (2013). Scatter of mass changes estimates at basin scale for Greenland and Antarctica. The Cryosphere, 7: 1411–32, https://doi.org/10.5194/tc-7–1411-2013, 2013Google Scholar

Barnes, H. T. (1906). Ice formation: with special reference to anchor-ice and frazil. New York: J. Wiley and Sons. 260 pp.Google Scholar

Barnett, T. P., Adam, J. C., and Lettenmaier, D. P. (2005). Potential impacts of a warming climate on water availability in snow-dominated regions, Nature, 438: 303–9.Google Scholar

Barnett, T. P., Pierce, D. W., Hidalgo, H. G., Bonfils, C., Santer, B. D., Das, T., Bala, G., Wood, A. W., Nozawa, T., Mirin, A. A., Cayan, D. R., and Dettinger, M. D. (2008). Human-induced changes in the hydrology of the western United States. Science, 319: 1080–3.Google Scholar

Barrans, N. E. and Sharp, M. J. (2010). Sustained rapid shrinkage of Yukon glaciers since the 1957–1958 International Geophysical Year, Geophys. Res. Lett., 37: L07501. doi: 10.1029/2009GL042030.Google Scholar

Barry, R. G. (1966). Meteorological aspects of the glacial history of Labrador-Ungava with special reference to vapor transport, Geogr. Bull. (Ottawa) 8 (4): 319–40.Google Scholar

Barry, R. G. (1985). Snow and ice data. In Hecht, A. D. (ed.), Paleoclimate analysis and modeling. New York: J. Wiley and Sons, 259–90.Google Scholar

Barry, R. G. (1987). The cryosphere – neglected component of the climate system. In Radok, U. (ed.), Towards understanding climate change. Boulder, CO: Westview Press, 35–67.Google Scholar

Barry, R. G. (1989). The present climate of the Arctic Ocean and possible past and future states. In Herman, Y. (ed.), The arctic seas: climatology, oceanography, biology and geology. Van Nostrand: Reinhold Co. pp. 1–46.Google Scholar

Barry, R. G. (1991). Observational evidence of changes in global snow and ice cover. In Schlesinger, M. E. (ed.), Greenhouse gas-induced climatic change: a critical appraisal of simulations and observations. Amsterdam: Elsevier. pp. 329–45.Google Scholar

Barry, R. G. (1993). Canada’s cold seas. In French, H. M. and Slaymaker, O. (eds.), Canada’s cold environments. Montreal: McGill-Queen’s University Press. pp. 29–61.Google Scholar

Barry, R. G. (1995a). Observing systems and data sets related to the cryosphere in Canada: A contribution to planning for the Global Climate Observing System. Atmosphere-Ocean, 33 (4): 771–807.Google Scholar

Barry, R. G. (1996). The parameterization of surface albedo for sea ice and its snow cover. Progr. Phys. Geog., 20 (1): 61–77.Google Scholar

Barry, R. G. (1997). Cryospheric data for model validations: requirements and status. Annals Glaciol., 26: 371–5.Google Scholar

Barry, R. G. (2000). Data on the geographical distribution of sea ice. In Tanis, F. and Smolianitsky, V. (eds.), Atlas climatology project environmental working group. Joint U.S.-Russian Atlas of Arctic Sea Ice. NSIDC, Boulder, CO. CD-ROM.Google Scholar

Barry, R. G. (2002a). History of the World Data Center for Glaciology, Boulder, and the National Snow and Ice Data Center at the University of Colorado. Glaciol. Data Report GD-30. Twenty-fifth Anniversary. Monitoring an Evolving Cryosphere. NSIDC, Univ. of Colorado, Boulder, CO. pp. 1–7.Google Scholar

Barry, R. G. (2002b). The role of snow and ice in the global climate system: A review. Polar Geog., 24 (3): 235–46.Google Scholar

Barry, R. G. (2003). Mountain cryospheric studies and the WCRP Climate and Cryosphere (CliC) Project. J. Hydrology Special Issue: Mountain Hydrology and Water Resources (eds., H. Lang and G. Kaser) 282 (1–4): 177–81.Google Scholar

Barry, R. G. (2006). The status of research on glaciers and global glacier recession: A review, Progr. Phys. Geogr., 30 (3): 285–306.Google Scholar

Barry, R. G. (2008). Mountain weather and climate. 3rd edn. Cambridge: Cambridge University Press. 506 pp.Google Scholar

Barry, R. G., (2009). Snow cover. In Cuff, D. and Goudie, A. (eds.), The Oxford companion to global change. Oxford Reference Online. Oxford University Press. University of Glasgow. May 26, 2009. www.oxfordreference.com/view/10.1093/acref/9780195324884.001.0001/acref-9780195324884Google Scholar

Barry, R. G. and Carleton, A. M. (2001). Synoptic and dynamic climatology. London: Routledge. 620 pp.Google Scholar

Barry, R. G., Fallot, J.-M., and Armstrong, R. L. (1995). Twentieth-century variability in snow cover conditions and approaches to detecting and monitoring changes: Status and prospects. Progr. Phys. Geog., 19 (4): 520–32.Google Scholar

Barry, R. G. and Maslanik, J. A. (1989). Arctic sea ice characteristics and associated atmosphere-ice interactions in summer inferred from SMMR data and drifting buoys: 1979 to 1985. R.G. GeoJournal, 18: 35–44.Google Scholar

Barry, R. G., Moritz, R. E., and Rogers, J. C. (1979). The fast ice regimes of the Beaufort and Chukchi Sea coasts, Alaska. Cold Regions Sci. Technol., 1: 129–52.Google Scholar

Barry, R. G., et al. (1989). Characteristics of Arctic sea ice from remote sensing data and their relationship to atmospheric processes. Annals Glaciol., 12: 9–15.Google Scholar

Barry, R. G., et al. (1993). The Arctic sea-ice-climate system: Observations and modeling. Rev. Geophys., 31: 397–422.Google Scholar

Barry, R. G. and Serreze, M. C. (2000). Atmospheric components of the Arctic ocean freshwater balance and their interannual variability. In Lewis, E. L., et al. (eds.) The freshwater budget of the arctic ocean. Springer, Netherlands: Kluwer Academic Publ.: pp. 45–56Google Scholar

Barry, R. G., Jania, J., and Birkenmajer, K. (2011). A. B. Dobrowolski – the first cryospheric scientist – and the subsequent development of cryospheric science. Hist. Geo-Space Sci., 2: 75–79Google Scholar

Barry, R. and Gan, T. Y. (2011). Global Cryosphere, Past, Present and Future, 472 pages, UK: Cambridge University Press, ISBN: 9780521769815 (Hardcover) & 9780521156851 (Paperback).Google Scholar

Barsch, D. (1988). Rock glaciers. In Clark, M. J. (ed.), Advances in periglacial geomorphology. Chichester: John Wiley and Sons. pp. 69–90.Google Scholar

Bartelt, P., Salm, B., and Gruber, U. (1999). Calculating dense-snow avalanche runout using a Voellmy-fluid model with active/passive longitudinal straining. J. Glaciol., 45 (150): 242–54.Google Scholar

Bartelt, P. and Lehning, M. (2002). A physical SNOWPACK model for the Swiss avalanche warning services, Part I: Numerical model. Cold Reg. Sci. Technol., 35 (3): 123–45.Google Scholar

Bartholomew, I., et al. (2010). Seasonal evolution of subglacial drainage and acceleration in a Greenland outlet glacier. Nature Geosci., 3 (6): 408–11.CrossRefGoogle Scholar

Bartlett, P. A., MacKay, M. D., and Verseghy, D. L. (2006). Modified snow algorithms in the Canadian Land Surface Scheme: Model runs and sensitivity analysis at three boreal forest stands. Atmos. Ocean, 44 (3): 207–22, doi: 10.3137/ao.440301.Google Scholar

Bassford, R. P., et al. (2006). Quantifying the mass balance of ice caps on Severnaya Zemlya, Russian High Arctic. I: Climate and mass balance of the Vavilov Ice Cap. Arct. Antarct. Alpine Res., 38: 1–12.Google Scholar

Batirov, R. S., et al. (2003). Avalanches of Uzbekistan. Tashkent: SANIGMI. 119 pp.Google Scholar

Battle, W. R. B. and Lewis, W. V. (1951). Temperature observations in Bergschrunds and their relationship to cirque erosion. J. Geol., 59 (6): 537–45.Google Scholar

Bauer, A. (1955). The balance of the Greenland ice sheet, J. Glaciol., 2 (17): L456–62.Google Scholar

Bayr, K. J., Hall, D. K., and Kovalick, W. M. (1994). Observations on glaciers in the eastern Austrian Alps using satellite data. Internat. J. Remote Sens., 15: 1733–42.Google Scholar

Bazant, Z. P., Zi, G., and McClung, D. (2003). Size effect law and fracture mechanics of the triggering of dry snow slab avalanches, J. Geophys. Res., 108 (B2): 2119. doi: 10.1029/2002JB001884.Google Scholar

Bazhev, A. (1997). Methods determining the internal infiltration accumulation of glaciers. In Kotltakov, V. M. (ed.), 34 Selected papers on main ideas of the Soviet glaciology, 1940s to 1980s, Moscow: Glaciological Association, Institute of Geography, RAN. pp. 371–81.Google Scholar

Beaty, C. B. (1975). Sublimation or melting: Observations from the White Mountains, California and Nevada, USA, J. Glaciol., 14: 275–86.Google Scholar

Becker, A., et al. (2013). A description of the global land-surface precipitation data products of the Global Precipitation Climatology Centre with sample applications including centennial (trend) analysis from 1901–present, Earth Syst. Sci. Data, 5: 71–99.CrossRefGoogle Scholar

Beckley, B. D., et al. (2017). On the ‘Cal-Mode’ Correction to TOPEX Satellite Altimetry and Its Effect on the Global Mean Sea Level Time Series, J Geophy Res-Oceans, 122: 8371–84, https://doi.org/10.1002/2017jc013090Google Scholar

Bedford, D. P. and Barry, R. G. (1994). Glacier trends in the Caucasus, 1960s to 1980s, Phys. Geog., 15: 414–24.Google Scholar

Bedford, D. and Douglass, A. (2008). Changing properties of snowpack in the Great Salt Lake Basin, western United States, from a 26-year SNOTEL record. Prof. Geog. 60: 374–86.Google Scholar

Beedle, M. J. (2005). Climatic drivers of glacier mass balance in southeast Alaska in the second half of the twentieth century. M.A. thesis, Boulder, CO: University of Colorado, 172 pp.Google Scholar

Beedle, M. J., et al. (2008). Improving estimation of glacier volume change: a GLIMS case study of Bering Glacier System, Alaska. The Cryosphere, 2: 33–51.Google Scholar

Belchansky, G. I., Douglas, D. C., and Platonov, N. G. (2004). Duration of the Arctic melt season: regional and interannual variability, 1979–2001. J. Climate, 17: 67–80.Google Scholar

Bell, R., et al. (2007). Large subglacial lakes in East Antarctica at the onset of fast-flowing ice streams. Nature, 445: 904–7.Google Scholar

Bell, R., et al. (2011). Widespread persistent thickening of the East Antarctic Ice Sheet by freezing from the base. Science, 331 (6024): 1592–5, doi: 10.1126/science.1200109.Google Scholar

Beltos, S. (2017). Frequency of ice-jam flooding of Peace-Athabasca Delta. Can. J. Civ. Eng., NRC Res. Press, 45: 71–5 dx.doi.org/10.1139/cjce-2017–0434Google Scholar

Beltaos, S., Tang, P., and Rowsell, R. Ice jam modelling and field data collection for flood forecasting in the Saint John River, Canada, Hydrological Processes, 26: 2535–45, doi: 10.1002/hyp.9293.Google Scholar

Beltaos, S. (ed.). (1995). River ice jams. Highlands Ranch, CO: Water Resources Publ., 390 pp.Google Scholar

Beltaos, S. (2001). Hydraulic roughness of breakup ice jams. ASCE J. Hydraul. Eng., 127 (8): 650–6.Google Scholar

Beltaos, S. (2007). The role of waves in ice-jam flooding of the Peace–Athabasca delta, Hydrol. Process., 21 (19): 2548–59.Google Scholar

Beltaos, S. (2008a). Progress in the study and management of river ice jams. Cold Reg. Sci. Technol., 51: 2–19.Google Scholar

Beltaos, S. (ed.). (2008b). River ice breakup. Highlands Ranch, CO: Water Resources Publ., 462 pp.Google Scholar

Beltaos, S. (2010). Internal strength properties of river ice jams. Cold Reg. Sci. Technol., 62: 83–91.Google Scholar

Beltaos, S. and Carter, T. (2009). Field studies of ice breakup and jamming in the Mackenzie delta. 15th Workshop on river ice. St. John’s, Newfoundland. Committee on River Ice Processes and the Environment. pp. 266–83.Google Scholar

Beltaos, S. and Prowse, T. (2009). River-ice hydrology in a shrinking cryosphere. Hydrol. Process., 23: 122–44.Google Scholar

Beltaos, S., et al. (2006). Climatic effects on ice-jam flooding of the Peace-Athabaska delta. Hydrol. Proc., 20 (19): 4031–50.Google Scholar

Bengtsson, L. (1986). Spatial variability of lake ice covers. Geogr. Ann., 68A (1–2): 113–21.Google Scholar

Beniston, M., Farinotti, D., Stoffel, M., Andreassen, L. M., Coppola, E., Eckert, N., et al. (2018). The European mountain cryosphere: a review of its current state, trends, and future challenges. Cryosphere 12: 759–94, doi: 10.5194/tc-12-759-2018.Google Scholar

Benn, D. I. and Lehmkuhl, F. (2000). Mass balance and equilibrium-line altitudes of glaciers in high mountain environments. Quart. Int., 65–66: 15–29.Google Scholar

Benn, D. I., Warren, C. R., and Mottram, R. H. (2007). Calving processes and the dynamics of calving glaciers. Earth Sci. Rec., 82: 143–79.Google Scholar

Benn, D., et al. (2009). Englacial drainage systems formed by hydrologically driven crevasse propagation. J. Glaciol., 55 (191): 513–23.Google Scholar

Benson, B. and Magnuson, J. (2000), updated 2007. Global lake and river ice phenology database. Boulder, CO: National Snow and Ice Data Center/World Data Center for Glaciology. Digital media.Google Scholar

Benson, C. S. (1962). Stratigraphic studies in the snow and firn of Greenland ice sheet. US Army, Hanover, NH. CRREL Research Report 70, 93 pp.Google Scholar

Bentley, M. J., et al. (2006). Geomorphological evidence and cosmogenic 10Be/26Al exposure ages for the Last Glacial Maximum and deglaciation of the Antarctic Peninsula Ice Sheet. Bull. Geol. Soc. Amer., 118: 1149–59.Google Scholar

Bentley, M. J., et al. (2009). Mechanisms of Holocene palaeoenvironmental change in the Antarctic Peninsula region. Holocene, 19: 51–69.Google Scholar

Bentley, W. A. and Humphries, W. J. (1931). Snow crystals. New York: McGraw-Hill (reprinted by Dover Publications, New York, 1964, 1973).Google Scholar

Benn, D. L. and Evans, D. J. A. (1998). Glaciers and glaciation. London: Arnold. 734 pp.Google Scholar

Bereiter, B., et al. (2015). Revision of the EPICA Dome C CO2 record from 800 to 600 kyr before present. Geophys. Res. Lett., 42: 542–9, doi: 10.1002/2014GL061957.Google Scholar

Berg, N. H. (1986). Blowing snow at a Colorado alpine site: Measurements and implications. Arctic Alp. Res., 18: 147–61.Google Scholar

Berger, A. and Loutre, M. F. (2010). Modeling the 100-kyr glacial–interglacial cycles. Glob. Planet. Change, 72 (4): 275–81.Google Scholar

Berger, C. L., et al. (2002). A climatology of northwest Missouri snowfall events: Long- term trends and interannual variability. Phys. Geogr., 23: 427–48.Google Scholar

Bergeron, V., Berger, C., and Betterton, M. D. (2006). Controlled irradiative growth of penitentes. Phys. Rev. Lett., 96 (098502): 4.Google Scholar

Berghuijs, W. R., Woods, R. A., and Hrachowitz, M. (2014). A precipitation shift from snow towards rain leads to a decrease in streamflow. Nat. Clim. Chang. 4: 583–6, doi: 10.1038/nclimate2246.Google Scholar

Bergström, S. (1995), The HBV model. In Singh, V. P. (ed.), Computer models of watershed hydrology. Highlands Ranch, CO: Water Resources Publications, pp. 443–76.Google Scholar

Berro, D. C., Mercalli, L., and Mortara, G. (2007). Evoluzions dei ghiacciai italiani nel periodo 2000–2007. Nimbus, 15 (3–4): 6–29.Google Scholar

Berthier, E., et al. (2007). Remote sensing estimates of glacier mass balances in the Himachal Pradesh (Western Himalaya, India). Rem. Sensing Environ., 108: 327–38.Google Scholar

Berthier, E., et al. (2010). Contribution of Alaska glaciers to sea-level rise derived from satellite imagery. Nature Geosci., 3: 92–5.Google Scholar

Betin, V. V. and Preobazhensky, Y. V. (1959). Variations in the state of the ice on the Baltic Sea and in the Danish Sound. Trudy Gos. Okean. Inst. (Moscow), 37: 3–13.Translation 102, U.S. Navy Hydrographic Office, 1961.Google Scholar

Betterton, M. D. (2001). Theory of structure formation in snowfields motivated by penitentes, suncups, and dirt cone. Phys. Rev. E., 63 (056129): 12.Google Scholar

Bhampri, R. and Bolch, T. (2009). Glacier mapping: A review with special reference to the Indian Himalayas. Progr. Phys. Geog., 33: 672–705.Google Scholar

Bhattacharya, I., et al. (2009). Surface melt area variability of the Greenland ice sheet: 1979–2008. Geophys. Res. Lett., 36: L20502, doi: 10.1029/2009GL039798.Google Scholar

Bhatt, U. S., et al. (2007). Examining glacier mass balances with a hierarchical modeling approach. J. Computing Sci. Eng., 9: 61–7.Google Scholar

Bianchi Janetti, E., et al. (2008). Regional snow-depth estimates for avalanche calculations using a two-dimensional model with snow entrainment. Annla Glaciol., 49: 63–70.Google Scholar

Bieniek, P. A., Bhatt, U. S., Rundquist, L. A., Lindsey, S. D., Zhang, X., and Thoman, R. L. (2011). Large-scale climate controls of interior Alaska river ice breakup. J. Clim. 24: 286–97. https://doi.org/10.1175/2010JCLI3809.1Google Scholar

Biftu, G. F. and Gan, T. Y. (2001). Semi-distributed, physically based, hydrological modeling of the Paddle River Basin, Alberta using remotely sensed data. J. Hydrol., 244: 137–56, doi: 10.1016/S0022–1694(01)00333-X.Google Scholar

Bigg, G. R. (1999). An estimate of the flux of iceberg calving from Greenland. Arct. Antarct. Alp. Res., 31: 174–8.Google Scholar

Bigg, G. R., et al. (1997). Modelling the dynamics and thermodynamics of icebergs. Cold Regions Sci. Technol. 26: 113–35.CrossRefGoogle Scholar

Bigg, G. R. and Wilton, D. J. (2014). Iceberg risk in the Titanic year of 1912: was it exceptional? Weather, 69 (4): 100–4., RMS, https://doi.org/10.1002/wea.2238CCrossRefGoogle Scholar

Bilello, M. A. (1980). Maximum thickness and subsequent decay of lake, river, and fast sea ice in Canada and Alaska. Hanover, NH: U.S. Army Cold Regions Research and Engineering Laboratory, CRREL Report 80–6.Google Scholar

Bindschadler, R., et al. (1996). Surface velocity and mass balance of ice streams D and E, West Antarctica. J. Glaciol., 42 (142): 461–75.Google Scholar

Bindschadler, R., et al. (2008). The Landsat image mosaic of Antarctica. Rem. Sensing Environ., 112 (12): 4214–26.Google Scholar

Bindschadler, R., et al. (2011). Getting around Antarctica: new high-resolution mappings of the grounded and freely-floating boundaries of the Antarctic ice sheet created for the International Polar Year. Cryosphere, 5: 569–88.Google Scholar

Bintanja, R. and van de Wal, R. S. W. (2008). North American ice-sheet dynamics and the onset of 100,000-year glacial cycles. Nature, 454: 869–72.Google Scholar

Bintanja, R., van der Linden, E. C., and Hazeleger, W. (2011). Boundary layer stability and Arctic climate change: a feedback study using EC-Earth. Climate Dynamics, 39: 2659–73.Google Scholar

Birkenmajer, K., et al. (2005). First Cenozoic glaciers in West Antarctica. Polish Polar Res., 26: 3–12.Google Scholar

Birkeland, K. W. (1998). Terminology and predominant processes associated with the formation of weak layers of near-surface crystals in the mountain snowpack. Arct. Alp. Res., 30 (2): 193–9.Google Scholar

Birkeland, K. W. (2001). Spatial patterns of snow stability throughout a small mountain range, J. Glaciol., 47 (157): 176–86.Google Scholar

Bishop, M. and Barry, R. G., et al. (2004). Global land ice measurements from space (GLIMS): Remote sensing and GIS investigations of the Earth’s cryosphere. Geocarto Internat., 19: 57–84.Google Scholar

Biskaborn, B. K., Smith, S. L., Noetzli, J., Matthes, H., Vieira, G., Streletskiy, D. A., Schoeneich, P., Romanovsky, V. E., Lewkowicz, A. G., Abramov, A., et al. (2019). Permafrost is warming at a global scale, Nat. Commun., 10: 264.Google Scholar

Bjørk, A. A., et al. (2012). An aerial view of 80 years of climate-related glacier fluctuations in southeast Greenland, Nat. Geosci., 5: 427–32.Google Scholar

Björnsson, H. (2002). Subglacial lakes and jökulhlaups in Iceland. Global Planet. Change, 35: 255–71.Google Scholar

Björnsson, H. (2009). Jöklar á Íslandi (Glaciers in Iceland). Reyjavik: Opna, 478 pp.Google Scholar

Björnsson, H., et al. (2003). Surges of glaciers in Iceland. Ann. Glaciol., 36: 82–90.Google Scholar

Björnsson, H., et al. (2006). Climate change response of Vatnajökull, Hofsjökull and Langjökull ice caps, Iceland. European Conference on Impacts of Climate Change on Renewable Energy Sources Reykjavik, Iceland, June 5–9, 2006, 4 pp.Google Scholar

Bleil, U. and Thiede, J. (1990). The geological history of Cenozoic polar oceans: Arctic versus Antarctic – an Introduction. In Bleil, U. and Thiede, J. (eds.), The geological history of Cenozoic polar oceans: Arctic versus Antarctic. Dordrecht, Netherlands: Kluwer. pp. 1–8.Google Scholar

Bliss, A., Hock, R., and Cogley, J. G. (2013). A new inventory of mountain glaciers and ice caps for the Antarctic periphery. Ann. Glaciol., 54: 191–9.CrossRefGoogle Scholar

Blunier, T., et al. (1997). Timing of the Antarctic Cold Reversal and the atmospheric CO2 increase with respect to the Younger Dryas event. Geophys. Res. Lett., 24 (21): 2683–6.Google Scholar

Bockheim, J. G., et al. (2008). Distribution of permafrost types and buried ice in ice-free areas of Antarctica. In Kane, D. L. and Hinkel, K. M. (eds.), Proceedings of the Ninth International Conference on Permafrost, Fairbanks, AK: University of Alaska, Institute of Northern Engineering. pp. 125–30.Google Scholar

Boé, J., Hall, A., and Qu, X. (2009). September sea-ice cover in the Arctic Ocean projected to vanish by 2100. Nature Geoscience 2: 341–3.Google Scholar

Bolch, T., Menounos, B., and Wheate, R. (2010). Landsat-based inventory of glaciers in western Canada, 1985–2005. Remote Sens. Environ. 114: 127–37. doi: 10.1016/j.rse.2009.08.015.Google Scholar

Bolch, T. (2007). Climate change and glacier retreat in northern Tien Shan (Kazakhstan/ Kyrgyzstan) using remote sensing data. Global Planet. Change 56: 1–12.Google Scholar

Bolsenga, S. J. (1968). River ice jams. A literature review. U.S. Lake Survey, Rep. 5–5. Detroit, MI: Dept. of the Army, Corps of Engineers, Lake Survey District. 568 pp.Google Scholar

Bond, G., et al. (1993). Correlations between climate records from North Atlantic sediments and Greenland ice. Nature, 365: 143–7.Google Scholar

Bony, S., et al. (2015). Clouds, circulation and climate sensitivity, Nat. Geosci., 8: 261–8, https://doi.org/10.1038/ngeo2398.Google Scholar

Boon, S., et al. (2010). Forty-seven years of research on the Devon Island Ice Cap, Arctic Canada. Arctic, 63: 13–29.Google Scholar

Borodachev, B. E. and Shilnikov, V. I. (2003). Istoriya L’dovoi Aviatsionnoi Razedki v Arktikei na Zamerzayushchikh Moryakh Rossii (1924–1993) (The History of Aerial Ice Reconnaissance in the Arctic and Ice-covered Seas of Russia, 1924–1993). Gidrometeoizdat: St. Petersburg, 441 pp.Google Scholar

Borstad, C. P. and McClung, D. M. (2009). Sensitivity analyses in snow avalanche dynamics modeling and implications when modeling extreme events. Canad. Geotech. J. 46 (9): 1024–33.Google Scholar

Boulton, G. S., Peacock, J. D., and Sutherland, D. G. (2002). Quaternary. In Trewin, N. H. (ed.), The geology of Scotland. 4th edn., London: The Geological Society. pp. 409–30.Google Scholar

Bourke, R. H. and Garrett, R. P. (1987). Sea ice thickness distribution in the Arctic Ocean. Cold. Regions Sci. Technol. 13: 259–80.Google Scholar

Bourke, R. H. and Mclaren, A. S. (1992). Contour mapping of Arctic Basin ice draft and roughness parameters. J. Geophys. Res., 97: 17, 715–28.Google Scholar

Bovis, M. J. (1977). Statistical forecasting of snow avalanches, San Juan Mountains, southern Colorado. USA J. Glaciol., 18 (78): 87–99.CrossRefGoogle Scholar

Bovis, M. J. and Mears, A. I. (1976). Statistical prediction of snow avalanche runout from terrain variables in Colorado. Arct. Alp. Res., 8: 115–20.Google Scholar

Box, J. E., et al. (2009). Greenland. Arctic Report Card 2009. www.arctic.noaa.gov/reportcard/Google Scholar

Bradley, R. S. and England, J. H. (2008). The Younger Dryas and the sea of ancient ice. Quat. Res., 70 (1): 1–10.Google Scholar

Bradley, R. S., et al. (2009). Recent changes in freezing level heights in the Tropics with implications for the deglacierization of high mountain regions. Geophys. Res. Lett. 36: L17701. doi: 10.1029/2009GL037712.Google Scholar

Braithwaite, R. J., Zhang, Y., and Raper, S. C. B. (2002). Temperature sensitivity of the mass balance of mountain glaciers and ice caps as a climatological characteristic. Zeit. Gletscherk. Glazial., 38: 35–61.Google Scholar

Brandt, R. E., et al. (2005). Surface albedo of the Antarctic sea ice zone. J. Clim., 18: 3606–22.Google Scholar

Bras, R. L. (1990). Hydrology, An introduction to hydrologic science. Reading, MA: Addison Wesley. 643 pp.Google Scholar

Braun, L. N., Weber, M., and Schulz, M. (2000). Consequences of climate change for runoff from Alpine regions. Annals Glaciol., 31: 19–25.Google Scholar

Braun, M., Humbert, A., and Moll, A. (2009). Changes of Wilkins Ice Shelf over the past 15 years and inferences on its stability. The Cryosphere, 3: 41–56.Google Scholar

Brenner, A. C., DiMarzio, J. P., and Zwally, H. J. (2007). Precision and accuracy of satellite radar and laser altimeter data over the continental ice sheets. IEEE Trans. Geosci. Remote Sens., 45: 321–31.Google Scholar

Brigham, L. W., Grishchenk, V. D., and Kamesaki, K. (1999). The natural environment, ice navigation and ship Technology. In Østreng, W. (ed.), The natural and societal challenges of the Northern Sea Route. A reference work. Dordrecht: Kluwer Academic Publishers. pp. 48–120.Google Scholar

British Glaciological Society. (1949). Joint Meeting of the British Glaciological Society, the British Rheologists’ Club and the Institute of Metals. J. Glaciol., 1: 231–40.Google Scholar

Brockamp, B. and Mothes, H. (1930). Seismische Untersuchungen aufdem Pasterzegletscher. Zeit. Geophys., 6: 482–500.Google Scholar

Broecker, W. S. (1997).Thermohaline circulation, the Achilles Heel of our climate system: Will man-made CO2 upset the current balance? Science, 278 (5343): 1582–8.Google Scholar

Broecker, W. S., et al. (2010). Putting the Younger Dryas cold event into context. Quat. Sci. Rev., 29 (9–10): 1078–81.Google Scholar

Brohan, P., et al. (2006). Uncertainty estimates in regional and global observed temperature changes: A new data set from 1850. J. Geophys. Res., 111: D12106, doi: 10.1029/2005JD006548.Google Scholar

Bromirski, P. D. , Sergienko, O. V. , and MacAyeal, D. R. (2009). Transoceanic infra-gravity waves impacting Antarctic ice shelves. Geophys. Res. Lett., 37: L02502, doi: 10.1029/2009GL041488.Google Scholar

Bromwich, D. H. and Kurtz, D. D. (1984). Katabatic wind forcing of the Terra Nova Bay polynya. J.Geophys. Res., 89: 3561–72.Google Scholar

Bromwich, D. H. and Parish, T. R. (1998). Chapter 4 of Meteorology of the Antarctic, Meteorology of the Southern Hemisphere. In Karoly, D. J. and Vincent, D. G. (eds.), American Meteorological Society, ISBN: 978-1-935704-10-2Google Scholar

Brönnimann, S., et al. (2008). Can we reconstruct Arctic sea ice back to 1900 with a hybrid approach? Clim. Past Discuss., 4: 955–79.Google Scholar

Bronselaer, B., Winton, M., Griffies, S., Hurlin, W., Rodgers, K., Serigenko, O., Stouffer, R., and Russell, J., J. (2018). Change in future climate due to Antarctic meltwater, Nature, 564: 53–58, doi: 10.1038/s41586-018-0712-z.Google Scholar

Brown, C. S., Meier, M. F., and Post, A. (1982). Calving speed of Alaska tidewater glaciers, with application to Columbia Glacier. U.S. Geol. Surv. Profess. Paper 1258-C, 13 pp.Google Scholar

Brown, J., Ferrians, Jr., O. J., Heginbottom, J. A., and Melnikov, E. S. (1997). Circum-arctic map of permafrost and ground-ice conditions, circum-pacific mMap series, US Geological Survey, ISBN 0-607-88745-1Google Scholar

Brown, J., et al. (1998). revised (2001). Circum-Arctic map of permafrost and ground ice conditions. Boulder, CO: National Snow and Ice Data Center/World Data Center for Glaciology. Digital Media.Google Scholar

Brown, J., Hinkel, K. M., and Nelson, F. E. (2000). The circumpolar active layer monitoring (CALM) program: research designs and initial results. Polar Geogr., 24: 165–258.Google Scholar

Brown, L. and Duguay, C. (2011). The fate of lake ice in the North American Arctic. The Cryosphere, 5 (4): 869–92, doi: 10.5194/tc-5-869-2011.Google Scholar

Brown, R. D. (1998). El Nino and North American snow cover. Proc. 55th Eastern Snow Conference, Jackson, N. H., June 4–6, pp. 165–72.Google Scholar

Brown, R. (Coordinating editor). (1999). Canadian contributions to GCOS. Freshwater ice.Google Scholar

Brown, R., Vikhamar-Schuler, D., Bulygina, O., Derksen, C., Loujus, K., Mudryk, L., et al. (2017). Arctic terrestrial snow cover. In Snow, Water, Ice and Permafrost in the Arctic (SWIPA) 2017, Oslo, Norway: Arctic Monitoring and Assessment Programme (AMAP). pp. 25–64.Google Scholar

Brown, R. D., Brasnett, B., and Robinson, D. (2003). Gridded North American monthly snow depth and snow water equivalent for GCM evaluation. Atmosphere-Ocean, 41 (1): 1–14, doi: 10.3137/ao.410101.Google Scholar

Brown, R. D. (2000). Northern Hemisphere snow cover variability and change, 1915–1997. J. Climate, 13: 2339–55.Google Scholar

Brown, R. and Armstrong, R. L. (2008). Snow-cover data: measurement, products and sources. In Armstrong, R. L. and Brun, E. (eds.), Snow and climate: physical processes, surface energy exchange and modeling. Cambridge, UK: Cambridge University Press. pp. 181–216.Google Scholar

Brown, R. D. and Cote, P. (1992). Interannual variability of landfast ice thickness in the Canadian High Arctic, 1950–89. Arctic, 45: 273–84.Google Scholar

Brown, R. D. and Mote, P.W. (2009). The response of Northern Hemisphere snow cover to a changing climate. J. Climate, 22: 2124–45.CrossRefGoogle Scholar

Brown, R. D., Walker, A., and Goodison, B. E. (2000). Seasonal snow cover monitoring in Canada – an assessment of Canadian contributions for global climate monitoring. Proc. 57th Eastern Snow Conference, Syracuse, NY, May 17–19, 2000: pp. 131–41.Google Scholar

Brown, R. D., et al. (2004). Climate variability and change – cryosphere. In Threats to water availability in Canada, NWRI scientific assessment, Report Series No. 3, Environment Canada, 128 pp.Google Scholar

Brown, R. D. and Robinson, D. A. (2011). Northern Hemisphere spring snow cover variability and change over 1922–2010 including an assessment of uncertainty. Cryosphere, 5: 219–29, doi: 10.5194/tc-5-219-2011.CrossRefGoogle Scholar

Bruce, I. (2009). On thin ice: winter sports and climate change, 54 pages, David Suzuki Foundation, ISBN 978–1-897375–24-2.Google Scholar

Brun, E., et al. (1992). A numerical model to simulate snow cover stratigraphy for operational avalanche forecasting. J. Glaciol., 38: 13–22.Google Scholar

Brun, E. et al. (2012). Simulation of northern Eurasian local snow depth, mass, and density using a detailed snowpack model and meteorological reanalyses. Journal of Hydrometeorology, 14 (1): 203–19, doi: 10.1175/jhm-d-12-012.1.Google Scholar

Brun, F., Berthier, E., Wagnon, P., Kääb, A., and Treichler, D. (2017). A spatially resolved estimate of High Mountain Asia glacier mass balances from 2000 to 2016. Nat. Geosci., 10: 668. Available at: https://doi.org/10.1038/ngeo2999Google Scholar

Brutsaert, W. (1982). Evaporation into the atmosphere, 299 pp., D. Reidel, Dordecht, Netherlands.Google Scholar

Budd, W. F., Dingle, R., and Radok, U. (1964). Byrd snow drift project. meteorology dept., Australia: University of Melbourne, Publ. No. 6.Google Scholar

Budd, W. F., Jenssen, D., and Radok, U. (1971). Derived physical characteristics of the Antarctic ice sheet. ANARE interim report series, A(IV) Glaciology, 120, 178 pp.Google Scholar

Budd, W. F. and Jenssen, D. (1975). Numerical modeling of glacier systems. Proc. Moscow Sympos. on Snow and Ice in Mountainous Regions Internat. Assoc. Hydrol. Sci. Publ. No. 104: 257–91.Google Scholar

Budd, W. F., and McInnes, B. J. (1979). Periodic surging of the Antarctic ice sheet – an assessment by modelling. Hydrol Sci. Bull., 24: 95–104.Google Scholar

Budd, W. F., Smith, I. L., and Wishart, E. (1967). The Amery ice shelf. In Oura, H. (ed.), Physics of snow and ice. Proceedings of the international conference on low temperature science. I (1). Sapporo: Hokkaido University. pp. 447–67.Google Scholar

Budyko, M. I. (1969). The effect of solar radiation variations on the climate of the earth. Tellus, 21: 611–19.Google Scholar

Bulygina, O. N., Razuvaev, V. N., and Korshunova, N. N., (2009), Changes in snow cover over Northern Eurasia in the last few decades, Environ. Res. Lett., 4 (045026): 6, doi: 10.1088/1748–9326/4/4/045026.Google Scholar

Bulygina, O., Groisman, P. Y., Razuvaev, V. N., and Korshunova, N. N. (2011). Changes in snow cover characteristics over Northern Eurasia since 1966. Environ Res Lett., 6 (4): doi: 10.1088/1748-9326/6/4/045204.Google Scholar

Burgess, D. O., et al. (2005). Flow dynamics and iceberg calving rates of the Devon ice cap, Nunavut, Canada. J. Glaciol., 51: 219–30.Google Scholar

Burgess, D. and Sharp, M. J. (2008). Recent changes in thickness of the Devon Island ice cap, Canada. J. Geophys. Res., 113 (B7): B07204, doi: 10.1029/2007JB005238.Google Scholar

Burgess, E. W., et al. (2010). A spatially calibrated model of annual accumulation rate on the Greenland Ice Sheet (1958–2007). J. Geophys. Res., 115: F02004, doi: 10.1029/2009JF001293.Google Scholar

Bürki, R. , Elsasser, H. , and Abegg, B. (2003). Climate change and winter sports: Environmental and economic threats. 5th World Conference on Sport and Environment, Turin, December 2–3, 2003. IOC/UNEP.Google Scholar

Burn, C. R. and Nelson, F. E. (2006). Comment on “A projection of severe near-surface permafrost degradation during the 21st century” by David M. Lawrence and Andrew G. Slater. Geophys. Res. Lett., 33: L21503, doi: 10.1029/2006GL027077.Google Scholar

Burn, C. R. and Kokelj, S. V. (2009). The environment and permafrost of the Mackenzie Delta area. Permafrost Periglac. Proc., 10: 83–105.Google Scholar

Burnett, A. W., et al. (2003). Increasing Great Lake-effect snowfall during the Twentieth Century: A regional response to global warming? J. Clim., 16: 3535–41.Google Scholar

Burrows, C. J. (1976). Icebergs in the Southern Ocean. New Zealand Geographer, 32: 127–38.Google Scholar

Buser, O. (1983). Avalanche forecast with the method of nearest neighbours: an interactive approach.Cold Reg. Sci. Technol., 8: 155–63.Google Scholar

Butkovich, T. R. (1954). Ultimate strength of ice. SIPRE Res. Rep., 11 (US Army): 12.Google Scholar

Butsic, V., Hanak, E., and Valletta, R. (2009). Climate Change and Housing Prices: Hedonic Estimates for Ski Resorts in Western North America, Working Paper 2008–12, Federal Reserve Bank San Francisco.Google Scholar

Butt, M. (2009). Application of global snow model for the estimation of snow depth in the UK. Meteorol. Atmos. Phy., 105: 181–90.Google Scholar

Caian, M., Koenigk, T., Döscher, R., and Devasthale, A. (2018). An interannual link between Arctic sea-ice cover and the North Atlantic Oscillation. Climate Dynamics, 50: 423–41.Google Scholar

CAA, 2016, Technical aspects of snow avalanche risk management—Resources and Guidelines for Avalanche Practitioners in Canada. In Campbell, C., Conger, S.,Google Scholar

Caine, N. (2002). Declining ice thickness on an alpine lake is generated by increased winter precipitation. Clim. Change, 54 (4): 463–70.Google Scholar

Callaghan, T. V., et al. (2010). A new climate era in the sub-Arctic: Accelerating climate changes and multiple impacts, Geophysical Research Letters, 37: L14705, doi: 10.1029/2009GL042064.Google Scholar

Callaghan, T. V., et al. (2011a). Chapter 4. Changing snow cover and its impacts. In Snow, water, ice and permafrost in the Arctic (SWIPA), 4:1-58 Oslo: Arctic Monitoring and Assessment Programme (AMAP), 538 pp.Google Scholar

Callaghan, T. V., et al. (2011b). The changing face of Arctic snow cover: A synthesis of observed and projected changes. Ambio., 40 (Suppl 1): 17–31, doi: 10.1007/s13280-011-0212-y.Google Scholar

Campbell, E. C., et al. (2019). Antarctic offshore polynyas linked to Southern Hemisphere climate anomalies. Nature, 570: 319–25, https://doi.org/10.1038/s41586-019–1294-0Google Scholar

Campbell, I. B. and Claridge, G. C. C. (2009). Antarctic permafrost soils. In Margesin, R. (ed.), Permafrost soils. Berlin: Springer Verlag. pp. 17–31.Google Scholar

Campbell, W. J. (1965). The wind-driven circulation of ice and water in a polar ocean. J Geophys Res., 70: 3279–01.Google Scholar

Caputo, M. V. and Crowell, J. C. (1985). Migration of glacial centers across Gondwana during Paleozoic Era Geol. Soc. Amer. Bull., 96 (8): 1020–36.Google Scholar

Callendar, G. S. (1938). The artificial production of carbon dioxide and its influence on temperature. Quart. J. Roy. Met. Soc., 64: 223–40.Google Scholar

Callendar, G. S. (1961). Temperature fluctuations and trends over the earth. Quart. J. Roy. Met. Soc., 87: 1–12.Google Scholar

Carenzo, M., et al. (2009). Assessing the transferability and robustness of an enhanced temperature-index glacier-melt model. J. Glaciol., 55 (190): 258–74.Google Scholar

Carey, K. L. (1973). Icings developed from surface water and ground water. Cold Regions Sci, Eng. Monogr. III D3. Hannover, NH: US Army Cold Regions Research and Engineering Laboratory. 65 pp.Google Scholar

Carey, M. (2005). Living and dying with glaciers: people’s historical vulnerability to avalanches and outburst floods in Peru. Global and Planetary Change, 47: 122–34.Google Scholar

Carmack, E. and Melling, H. (2011). Warmth from the deep. Nature Geosci, 4: 7–8, https://doi.org/10.1038/ngeo1044.CrossRefGoogle Scholar

Carlson, A. E., et al. (2007). Geochemical proxies of North American freshwater routing during the Younger Dryas cold event. Proc. Nat. Acad. Sci., 104: 6556–61.Google Scholar

Carlson, A. E., et al. (2008). Rapid early Holocene deglaciation of the Laurentide ice sheet. Nature Geoscience, 1: 62–4.Google Scholar

Carozzi, A. V. (ed.). (1967). Studies on glaciers. Transl. of Agassiz, L. 1840 Etudes sur les glaciers, Neuchatel. New York: Hafner Publishing Co. 213 pp.Google Scholar

Carr, M. L., Gaughan, S. P., George, C. R., and Mason, J. G., (2015). CRREL’s Ice Jam Database: Improvements and Updates, 18th Workshop on Hydraulics of Ice Covered Rivers Quebec City, Canada, August 18–20, 2015.Google Scholar

Carrivick, , J. L., et al. (2012). Late-Holocene changes in character and behaviour of land-terminating glaciers on James Ross Island, Antarctica. J. Glaciol., 58: 1176–90.Google Scholar

Carrivick, J. L., et al. (2017). Ice-dammed lake drainage evolution at Russell Glacier, West Greenland. Frontiers in Earth Science, 5: 100.Google Scholar

Carsey, F. D. (ed.). (1992). Microwave remote sensing of sea ice. Washington, DC: American Geophysical Union. 462 pp.Google Scholar

Carsey, F. D., et al. (1993). Status and future directions of remote sensing of sea. In: F.D. Carsey (ed.) Microwave Remote Sensing of Sea Ice. Amer. Geophys. Union, 26: 443–6.Google Scholar

Casassa, G., et al. (2002). Current knowledge of the Southern Patagonia Icefield. In Casassa, G., Sepu´lveda, F. V., and Sinclair, R. (eds.), The Patagonian ice fields: a unique natural laboratory for environmental and climate change studies. New York: Kluwer Academic/Plenum Publishers. pp. 67–83.Google Scholar

Castebrunet, H., et al. (2014). Projected changes of snow conditions and avalanche activity in a warming climate: the French Alps over the 2020–2050 and 2070–2100 periods. The Cryosphere, 8 (5): 1673–97, doi: 10.5194/tc-8-1673-2014.Google Scholar

Cavalieri, D. J., Gloersen, P., and Campbell, W. J. (1984). Determination of sea ice parameters with Nimbus 7 SMMR. J. Geophys. Res., 89 (D4): 5355–69.Google Scholar

Cayan, D. R., et al. (2001). Changes in the onset of spring in the western United States. Bull. Am. Met. Soc., 82: 399–415.Google Scholar

Cazenave, , A., et al. (2018). Global sea level budget 1993-present. Earth System Science Data, 10 (3), http://doi.org/10.5194/essd-10–1551-2018Google Scholar

Cazenave, A., Lombard, A., and Llovel, W. (2008). Present-day sea level rise: A synthesis, Comptes Rendus Geosciences, 340 (11): 761–70.Google Scholar

Chamberlin, T. C. (1894). Glacial studies in Greenland. J. Geol., 2 (7): 649–66.Google Scholar

Chamberlin, T. C. (1897). Glacial studies in Greenland. X. The Bowdoin Glacier. J. Geol., 5 (3): 229–40.Google Scholar

Chang, A. T. C., Foster, J. L., and Hall, D. K. (1987). Nimbus-7 derived global snow cover parameters. Annals Glaciol., 9: 39–44.Google Scholar

Chang, A. T. C., Foster, J. L., and Rango, A. (1991). Utilization of surface cover composition to improve the microwave determination of snow water equivalent in a mountain basin. Int. J. Remote Sensing, 12 (11): 2311–9.Google Scholar

Chang, A. T. C., et al. (1982). Snow water equivalent accumulation by microwave radiometry. Cold Reg. Sci. Technol., 5 (3): 259–67.Google Scholar

Chang, A. J. , et al. (1997). Snow parameters derived from microwave measurements during the BOREAS winter field campaign. J. Geophys. Res., 102: 29663–71.Google Scholar

Chapin, F. S., et al. (2005). Role of land-surface changes in Arctic summer warming. Science, 310 (5748): 657–60.Google Scholar

Chapman, W. L. and Walsh, J. E. (2007). Simulations of Arctic temperature and pressure by global coupled models. J. Clim., 20: 609–32, doi: 10.1175/JCLI4026.1.Google Scholar

Charrassin, J.-B., et al. (2008). Southern Ocean frontal structure and sea-ice formation rates revealed by elephant seals. Proc. Nat. Acad. Sci., 105 (33): 11,634–9.Google Scholar

Chekotillo, A., Tsvid, A. A., and Makarov, V. N. (1960). Naledy na territorii SSSR i bor’ba s nim (Icings in the USSR snf their control). Blaoveshchensk: Amur. Knizhn. Izdat. 207 pp. (transl. 1965 for CRREL, US Army, Hanover, NH).Google Scholar

Chen, F., et al. (2014). Modeling seasonal snowpack evolution in the complex terrain and forested Colorado Headwaters region: A model intercomparison study. J. Geophys. Res. Atmos., 119 (13): 795–13,819, doi: 10.1002/2014JD022167.Google Scholar

Chen, J. L., Wilson, C. R., and Tapley, B. D., (2013). Contribution of ice sheet and mountain glacier melt to recent sea level rise. Nat. Geosci., 9: 549–52, https://doi.org/10.1038/NGEO1829Google Scholar

Chen, J.-Y. and Funk, M. (1990). Mass balance of Rhonegletscher during 1982/83–1986/87. J. Glaciol., 36 (123): 199–209.Google Scholar

Chen, J.-Y. and Ohmura, A. (1990). Estimation of Alpine glacier water resources and their change since the 1870s. Hydrology in Mountainous Regions. I – Uydrological Measurements; the Water Cycle (Proceedings of two Lausanne Symposia, August 1990). IAHS Publ. no. 193, pp. 127–35.Google Scholar

Chen, J. L., et al. (2009). Accelerated Antarctic ice loss from gravity measurements. Nature Geosci., 2: 859–62.Google Scholar

Chen, J. L., Wilson, C. R., and Tapley, B. D. (2006). Satellite gravity measurements confirm accelerated melting of Greenland ice sheet. Science, 313: 1958–60.Google Scholar

Chen, Y. and She, Y. (2019). Temporal and Spatial Variations of River Ice Breakup Timing across Canada, CGU HS Committee on River Ice Processes and the Environment, 20th Workshop on the Hydraulics of Ice Covered Rivers Ottawa, Ontario, Canada, May 14–16, 2019.Google Scholar

Chen, J. M., Rich, P. M., Gower, S. T., Norman, J. M., and Plummer, S. (1997). Leaf area index of boreal forests: Theory, techniques and measurements. J. Geophys. Res., 102: 29,429–44.Google Scholar

Cheng, G. and Dramis, F. (1992). Distribution of mountain permafrost and climate. Permafrost & Periglac. Proc., 3: 83–91.Google Scholar

Cherry, J. E., et al. (2007). Development of the pan-Arctic snowfall reconstruction: new land-based solid precipitation estimates for 1940–99. J. Hydromet., 8 (6): 1243–63.Google Scholar

Chinn, T. J. (1999). New Zealand glacier response to climate change of the past two decades. Global Planet. Change, 22 (1–4): 155–68.Google Scholar

Christoffersen, P., et al. (2018). Cascading lake drainage on the Greenland Ice Sheet triggered by tensile shock and fracture, Nat. Commun., Vol. 9, Article number:1064.Google Scholar

Choudhury, B. J., (1993), Reflectivities of selected land surfaces types at 19 and 37 GHz from SSM/I observations. Remote Sens. Environ., 46: 1–17.CrossRefGoogle Scholar

Chudinova, S. M., Frauenfeld, O. W., Barry, R. G., Zhang, T.-J., and Sorokovikov, V. A. (2006). Relationship between air and soil temperature trends and periodicities in the permafrost regions of Russia. J. Geophys. Res., 111 (F02008): 15.Google Scholar

Church, et al. (2013). Sea level change, in climate change 2013, the physical science basis. In Stocker, T. F., et al. (eds.), Contribution of WG I to AR5 of the intergovernmental panel on climate change, Cambridge, UK: Cambridge University Press.Google Scholar

Ciracì, E., Velicogna, I., and Swenson, S. (2020). Continuity of the mass loss of the world’s glaciers and ice caps from the GRACE and GRACE follow‐on missions. Geophy. Res. Lett., 47 (9): e2019GL086926. https://doi.org/10.1029/2019GL086926Google Scholar

Clair, T. A. and Ehrman, J. M. (1998). Using neural networks to assess the influence of changing seasonal climates in modifying discharge, dissolved organic carbon, and nitrogen export in eastern Canadian rivers. Water Res. Res., 34 (3): 447–55.Google Scholar

Clark, M. P., Serreze, M. C., and Barry, R. G. (1996). Characteristics of Arctic Ocean climate based on COADS data, 1980–1993. Geophys. Res. Lett., 23 (15): 1953–6.Google Scholar

Clark, P. U. and Huybers, P. (2009). Global change: Interglacial and future sea level. Nature, 462: 856–7.Google Scholar

Clark, P. U. and Pollard, D. (1998). Origin of the middle Pleistocene transition by ice sheet erosion of regolith. Paleoceanog., 13: 1–9.Google Scholar

Clark, P. U., et al. (2009). The last glacial maximum. Science, 325 (5941): 710–14.Google Scholar

Clarke, G. K. C. (1991). Length, width and slope influences on glacier surging. J. Glaciol., 36: 236–46.Google Scholar

Clarke, G. K. C. (2003). Hydraulics of subglacial outburst floods: new insights from the Spring-Hutter formulation. J. Glaciol., 49 (165): 299–313.Google Scholar

Clarke, G. K. C. (2005). Subglacial processes. Annu. Rev. Earth Planet. Sci., 33: 247–76.Google Scholar

Clarke, G. K. C. et al. (2015). Projected deglaciation of western Canada in the twenty-first century. Nat. Geosci., 8 (5): 372–7, doi: 10.1038/ngeo2407.Google Scholar

Clifford, D. (2010). Global estimates of snow water equivalent from passive microwave instruments: history, challenges and future developments. Int. J.Rem. Sensing, 31 (14): 3707–26.Google Scholar

Cline, D. K. , et al. (2007). Overview of the Second Cold Land Processes Experiment (CLPX-II). IEEE Proc. International Geoscience and Remote Sensing Symposium, Barcelona.Google Scholar

Cogley, J. G. (2009). Geodetic and direct mass-balance measurements: comparison and joint analysis. Ann. Glaciol., 50: 96–100.Google Scholar

Colbeck, S. C. (1983). Theory of metamorphism of dry snow. J. Geophys. Res., 88: 5475–82.Google Scholar

Colbeck, S. C. (1997). A review of sintering in seasonal snow. CRREL Report 97–10. Hanover, NH: US Army Cold Regions Research & Engineering Laboratory. 17 pp.Google Scholar

Collins, D. N. (2006). Climatic variation and runoff in mountain basins with differing proportions of glacier cover. Nordic Hydrol., 37: 315–26.Google Scholar

Cogley, J. G. (2005). Mass and energy balances of glaciers and ice sheets. In Anderson, M. G. (ed.), Encyclopedia of hydrological sciences, vol. 4. New York: J. Wiley and Sons. pp. 2555–74.Google Scholar

Cogley, J. G., (2008). Measured rates of glacier shrinkage. Geophys. Res. Abstracts, 10: EGU2008-A-11595.Google Scholar

Cogley, J. G. (2009a). Geodetic and direct mass-balance measurements: comparison and joint analysis. Annals Glaciol., 50: 96–100.Google Scholar

Cogley, J. G. (2009b). A more complete version of the World Glacier Inventory. Annals Glaciol., 50 (53): 32–8.Google Scholar

Collins, D. N. (2008). Climatic warming, glacier recession and runoff from Alpine basins after the Little Ice Age maximum. Ann. Glaciol., 48: 119–24.Google Scholar

Colony, R., Radionov, V., and Tanis, F. I. (1998). Measurements of precipitation and snow pack at the Russian North Pole drifting stations. Polar Record, 34: 3–14.Google Scholar

Comiso, J. C. (1986). Characteristics of Arctic winter sea ice from satellite multispectral microwave observation. J. Geophys, Res., 91 (Cl): 975–94.Google Scholar

Comiso, J. C. (2010). Variability and trends of the global sea ice cover. In Thomas, D. N. and Dieckmann, G. S. (eds.), Sea ice. 2nd edn. Chichester: Wiley-Blackwell. pp. 205–46.Google Scholar

Comiso, J. C. (2012). Large decadal decline in the Arctic multiyear ice cover. J. Clim., 25: 1176–93.Google Scholar

Comiso, J. C., Kwok, R., Martin, S., and Gordon, A. L. (2011). Variability and trends in sea ice extent and ice production in the Ross Sea. J Geophys Res., 116 (C04):021. https://doi.org/10.1029/2010JC006391Google Scholar

Comiso, J. C., et al. (2017). Positive trend in the Antarctic sea ice cover and associated changes in surface temperature. J. of Climate, 30 (6): 2251–67, doi: 10.1175/Jcli-D-16-0408.1.Google Scholar

Comiso, J. C., Parkinson, C. L., Gersten, R., and Stock, L. (2008). Accelerated decline in the Arctic Sea ice cover. Geophys. Res. Letters, 35: L01703. https://doi.org/10.1029/2007GL031972Google Scholar

Comiso, J. C., Cavalieri, D. J., and Markus, T. (2003). Sea ice concentration, ice temperature, and snow depth using AMSR-E data. IEEE Trans. Geosci. Remote Sensing, 42: 243–52.Google Scholar

Comiso, J. C., Cavalieri, D., Parkinson, C., and Gloersen, P. (1997). Passive microwave algorithms for sea ice concentrations: A comparison of two techniques. Remote Sensing Environ., 60 (3): 357–84.Google Scholar

Committee on Climate, Energy, and National Security. (2009). Scientific value of Arctic sea ice imagery derived products. Washington, DC: National Research Council. 48 pp.Google Scholar

Connolly, R., et al. (2019). Northern hemisphere snow-cover trends (1967–2018): a comparison between climate models and observations. Geoscience, 9: 135, doi: 10.3390/geosciences9030135.Google Scholar

Conway, H. and Abrahamson, J. (1984). Snow-slope stability – a probabilistic approach. J. Glaciol., 34 (117): 170–7.Google Scholar

Conway, H., et al. (1999). Past and future grounding-line retreat of the West Antarctic ice sheet. Science, 286: 280–3.Google Scholar

Cook, A. J., et al. (2005). Retreating glacier fronts on the Antarctic Peninsula over the past half-century. Science, 308: 541–4.Google Scholar

Cook, A. J. and Vaughan, D. G. (2010). Overview of areal changes of the ice shelves on the Antarctic Peninsula over the past 50 years. Cryosphere, 4: 77–98.Google Scholar

Cooley, S. and Pavelsky, T. (2016). Spatial and temporal patterns in Arctic river ice breakup revealed by automated ice detection from MODIS imagery. Remote Sensing of Environment, 175: 310–22, http://dx.doi.org/10.1016/j.rse.2016.01.004Google Scholar

Coon, M. D., et al. (1998). The architecture of anisotropic elastic-plastic sea ice mechanics constitutive law. J. Geophys. Res., 103 (C10): 21, 915–25.Google Scholar

Copland, L. and Mueller, D. (2017). Arctic ice shelves and ice islands. Dordrecht: Springer. DOI: 10.1007/978-94-024-1101-0_11.Google Scholar

Copland, L., Sharp, M. J., and Dowdeswell, J. A. (2003). The distribution and flow characteristics of surge-type glaciers in the Canadian High Arctic. Ann. Glaciol., 36L: 73–81.Google Scholar

Costard, F., et al. (2007). Impact of the global warming on the fluvial thermal erosion over the Lena River in central Siberia. Geophys. Res. Lett., 34: L14501, doi: 10.1029é2007GL030212.Google Scholar

Cotté, C. and Guinet, C. (2007). Historical whaling records reveal major regional retreat of Antarctic sea ice. Deep Sea Res., 54: 243–52.Google Scholar

Cox, J. (2005). The snow/snow water equivalent ratio and its predictability across Canada. MSc thesis, Montreal: McGill University. 102 pp.Google Scholar

Crary, A. P. (1958). Arctic ice island and ice shelf studies. Part I. Arctic, 11: 2–42.Google Scholar

Crary, A. P. (1960). Arctic ice islands and ice shelf studies. Part. II. Arctic., 13: 32–50.Google Scholar

Crary, A. P., et al. (1962). Glaciological regions of the Ross Ice Shelf. J. Geophys. Res., 67: 2791–807.Google Scholar

Crocker, G. B. and Cammaert, A. B. (1994). Measurements of bergy bit and growler populations off Canada’s East Coast. In: Proc. of IAHR Ice Symposium, Trondheim, Norway, August 23–26, 1994, Vol 1: 167–76.Google Scholar

Crites, H., Kokelj, S. V., and Lacelle, D. (2020). Icings and groundwater conditions in permafrost catchments of northwestern Canada. Sci Rep, 10: 3283, https://doi.org/10.1038/s41598-020–60322-wGoogle Scholar

Cullen, , et al. (2013). A century of ice retreat on Kilimanjaro: The mapping reloaded. Cryosphere, 7: 419–31.Google Scholar

Curran, M. A. J., et al. (2003). Ice core evidence for sea ice decline since the 1950s. Science 302, 295: 1890–2.Google Scholar

Curry, J. A., Schramm, J. L., and Ebert, E. E. (1995). Sea ice-albedo climate feedback mechanism. Journal of Climate, 8: 240–7.Google Scholar

Cuffey, K. M. and Paterson, W. S. B. (2010). The physics of glaciers. 4th edn. Burlington, MA: Butterworth-Heinemann/Elsevier. 704 pp.Google Scholar

Czudek, T. and Demek, J. (1970). Thermokarst in Siberia and its influence on the development of lowland relief. Quat. Res., 1: 103–20.Google Scholar

Dadic, R., et al. (2010). Wind influence on snow depth distribution and accumulation over glaciers. J. Geophys. Res., 115: F01012. doi: 10.1029/2009JF001261.Google Scholar

Dahl, S. O., et al. (2005). Weichselian glaciation history in the Rondane ‘dry valleys’ of central Scandinavia. Geological Society of America. 2005 Salt Lake City Annual Meeting, paper 178–9.Google Scholar

Dahl-Jensen, D., et al. (2009). The greenland ice sheet in a changing climate: snow, water, ice and permafrost in the arctic (SWIPA). Oslo: Arctic Monitoring and Assessment Programme (AMAP). 115 pp.Google Scholar

Dai, J. C., et al. (2009). Cold decade (AD 1810–1819) caused by Tambora (1815) and another (1809) stratospheric volcanic eruption. Geophy. Res. Lett., 36: L22703, doi: 10.1029/2009GL040882.Google Scholar

Daly, S. F. (2008). Evolution of frazil ice. Proceedings of 19th IAHR International Symposium on Ice “Using New Technology to Understand Water-Ice Interaction.” Jasek. M. (ed). Vol. 1: 29–47.Google Scholar

Dansgaard, W., et al. (1969). One thousand centuries of climatic record from camp century on the greenland ice sheet. Science, 166 (3903): 377–80.Google Scholar

Darby, D. A. (2003). Sources of sediment found in sea ice from the western Arctic Ocean, new insights into processes of entrainment and drift patterns. J. Geophys. Res., 108 (C8): 3257.Google Scholar

Darby, D. A. (2008). Arctic perennial ice cover over the last 14 million years. Paleoceanog., 23: PA1S07.Google Scholar

Darwin, C. (1839). Journal of researches into the natural history and geology of the countries visited during the voyage of H.M.S. Beagle round the world, under the Command of Capt. Fitz Roy, R.N. 2nd edn. London, UK: H. Colburn. p. 325. (http://darwin-online.org.uk/content/frameset?itemID=F20&viewtype=text&pageseq=1).Google Scholar

Das, S. B., et al. (2008). Fracture propagation to the base of the Greenland Ice Sheet during supraglacial lake drainage. Science, 320: 778–81.Google Scholar

Davies, B. J. and Glasser, N. F. (2012). Accelerating shrinkage of Patagonian glaciers from the “Little Ice Age” (c. AD 1870) to 2011. J. Glaciol., 58: 1063–84.Google Scholar

Davis, P. T., Menounos, B., and Osborn, G. (2009). Introduction, Holocene and latest Pleistocene alpine glacier fluctuations: a global perspective. Quat. Sci. Rev., 28 (21–22): 2021–33.Google Scholar

De Angelis, H. and Skvarca, P. (2003). Glacier surge after ice shelf collapse. Science, 299 (5612): 1560–2.Google Scholar

DeBeer, C. M., Wheater, H. S., Carey, S. K., and Chun, K. P. (2016). Recent, climatic, cryospheric, and hydrological changes over the interior of western Canada: A review and synthesis. Hydrology and Earth System Sciences, 20: 1573–98.Google Scholar

DeConto, R. M., et al. (2008). Thresholds for Cenozoic bipolar glaciation. Nature, 455: 652–6.Google Scholar

DeConto, R. M. and Pollard, D. (2016). Contribution of Antarctica to past and future sea-level rise. Nature, 531: 591–7.Google Scholar

de Freitas, C. R. (1975). Estimation of the disruptive impacts of snowfalls in urban areas. J. Appl. Met., 14: 1166–73.Google Scholar

de la Mare, W. K. (1997). Abrupt mid-twentieth-century decline in Antarctic sea-ice extent from whaling records. Nature, 389: 57–60.Google Scholar

de la Mare, W. K. (2009). Changes in Antarctic sea-ice extent from direct historical observations and whaling records. Climatic Change, 92: 461–93.Google Scholar

de Quervain, M. R. (1950). Die Festigkeitseigenschaften der Schneedecke und ihre Messung. Geofis. pura appl., 18: 3–15.Google Scholar

de Quervain, M. and Meister, R. (1987). Fifty years of snow profiles on the Weissflujoch and relations to the surrounding avalanche activity (1936/37–1985–86). In Salm, B. and Guler, H. (eds.), Avalanche formation, movement and effects. Proceedings of the Davos Symposium), IAHS Publ. no. 162, Wallingford, UK: IAHS. pp. 161–81.Google Scholar