Abstract
Wind and temperature profiles measured near the Antarctic Georg von Neumayer Station in January and February 1983 are analysed with respect to situations of low cloud cover. In these situations, shallow inversions develop in the period of low sun elevation. The structure of these inversions in comparison with those in midlatitudes is explained by considering the heat fluxes near the ground, the influence of surface friction over different terrain roughness and for different Coriolis parameters.
Full Text 
Sign-in/Register to access full text options
Sign-in/Register to access full text options 
Published version (
Free)
Free) 
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 call
