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Surface wind, subcloud humidity and the stability of the tropical climate Cover

Surface wind, subcloud humidity and the stability of the tropical climate

Open Access
|Jan 2001

Abstract

The dominant balance in the tropical ocean surface energy budget is between radiative heating and evaporative cooling. It has been proposed recently that a positive correlation between surface wind and ocean temperature could enhance the stabilising effect of evaporation. The issue is studied here using a single-column radiative-convective model of the tropical atmosphere. It is found that the proposed coupling of surface wind to temperature will indeed always increase the stability of the system, but the extent to which it does so depends in an essential way on the strength of the upper tropospheric water vapour feedback.

Language: English
Page range: 513 - 525
Submitted on: May 31, 2000
Accepted on: Feb 2, 2001
Published on: Jan 1, 2001
Published by: Stockholm University Press
In partnership with: Paradigm Publishing Services

© 2001 Rodrigo Caballero, published by Stockholm University Press
This work is licensed under the Creative Commons Attribution 4.0 License.