Skip to main content Accessibility help
×
Hostname: page-component-77c89778f8-gvh9x Total loading time: 0 Render date: 2024-07-16T16:07:13.685Z Has data issue: false hasContentIssue false

34 - The energy budget at selected stations over the north Indian Ocean during MONSOON-77

Published online by Cambridge University Press:  05 November 2011

R. R. Rao
Affiliation:
National Institute of Oceanography, India
K. V. Sunderaramam
Affiliation:
Naval Physical and Oceanographic Laboratory, India
M. R. Santa Devi
Affiliation:
Naval Physical and Oceanographic Laboratory, India
Get access

Summary

The heat budget of the oceanic surface at selected stations over the north Indian Ocean is evaluated for the three phases of MONSOON-77 by computing the insolation, effective back radiation, latent heat flux and sensible heat flux using empirical expressions. The diurnal variations of wet bulb depression, sea-surface temperature, T, and wind speed are examined for each of three phases of the monsoon over the eastern Arabian Sea and the central Bay of Bengal. The so-called ‘heat potential’ values (T≥27°C) of the upper-oceanic layer at the stations located over the offshore trough along the west coast of India are computed and related to the net heat gain at the surface. Mean temperature and thickness values of the mixed layer are also analysed. The results are discussed in relation to the behaviour of the summer monsoon over India.

Introduction

The net energy accumulated over the tropics is transported to higher latitudes by the atmospheric and oceanic circulations in maintaining the thermal equilibrium of the earth–atmosphere system. Earlier studies have indicated that the atmosphere transports more energy than the oceans. However, the studies of Von der Haar and Oort (1973) based on satellite radiation data clearly indicate that the oceans play the larger role in transporting the surplus energy from the tropics. The relative contributions of the Indian, Atlantic and Pacific oceans must clearly differ.

Type
Chapter
Information
Monsoon Dynamics , pp. 509 - 522
Publisher: Cambridge University Press
Print publication year: 1981

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

Save book to Kindle

To save this book to your Kindle, first ensure coreplatform@cambridge.org is added to your Approved Personal Document E-mail List under your Personal Document Settings on the Manage Your Content and Devices page of your Amazon account. Then enter the ‘name’ part of your Kindle email address below. Find out more about saving to your Kindle.

Note you can select to save to either the @free.kindle.com or @kindle.com variations. ‘@free.kindle.com’ emails are free but can only be saved to your device when it is connected to wi-fi. ‘@kindle.com’ emails can be delivered even when you are not connected to wi-fi, but note that service fees apply.

Find out more about the Kindle Personal Document Service.

Available formats
×

Save book to Dropbox

To save content items to your account, please confirm that you agree to abide by our usage policies. If this is the first time you use this feature, you will be asked to authorise Cambridge Core to connect with your account. Find out more about saving content to Dropbox.

Available formats
×

Save book to Google Drive

To save content items to your account, please confirm that you agree to abide by our usage policies. If this is the first time you use this feature, you will be asked to authorise Cambridge Core to connect with your account. Find out more about saving content to Google Drive.

Available formats
×