Abstract
Recently it has been proposed (in a simple model study of the surface fluxes) that there is a robust mechanism linking the surface temperature and the surface wind via atmospheric angular momentum transport. The analysis of the simple model suggested that the proposed mechanism can enhance the stabilizing effect of evaporation on the surface temperature. This issue is studied here using a simple two zone hemispheric model of the atmosphere-ocean system. We relax the two critical assumptions from the above-mentioned study, namely the assumption of a constant air-sea temperature difference and constant near-surface relative humidity, respectively.
Sign-in/Register to access full text options 
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callMore From: Russian Journal of Numerical Analysis and Mathematical Modelling
Disclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
