1 FOEHN WINDS IN THE MCMURDO DRY VALLEYS OF ANTARCTICA

A foehn wind is a warm, dry, downslope wind resulting from synoptic-scale, cross-barrier flow over a mountain range. Foehn winds are a climatological

Bibliographic Details
Main Authors: Daniel F. Steinhoff, David H. Bromwich, Johanna C. Speirs, Hamish A. Mcgowan, Andrew J. Monaghan
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Subjects:
McMurdo Dry Valleys
Antarc*
Antarctica
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.580.3254
http://www.scires.com/divisions/meeting2009/abstracts/day2_08.pdf
Description
Summary:A foehn wind is a warm, dry, downslope wind resulting from synoptic-scale, cross-barrier flow over a mountain range. Foehn winds are a climatological

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