By David H. Bromwich, Charles R. Stearns
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Published via the yank Geophysical Union as a part of the Antarctic study Series.
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Extra resources for Antarctic Meteorology and Climatology: Studies Based on Automatic Weather Stations
Savage, M. , C. R. Stearns, and D. , Dep. , Univ. , Madison, 19856. Savage, M. , C. R. Stearns, and D. , Dep. , Univ. , Madison, 1985c. Savage, M. , C. R. Stearns, G. A. Weidner, and D. , Dep. , Univ. , Madison, 1985d. Savage, M. , C. R. Stearns, G. A. Weidner, and D. , Dep. , Univ. , Madison, 1985e. , The TIROS-N/NOAA A-G satellite series, NOAA Tech. Memo. S. Dep. , Washington, D. C , 1978. , G. A. Weidner, and C. R. , Dep. , Univ. , Madison, 1986. , G. A. Weidner, and C. R. , Dep. , Univ. , Madison, 1987.
Their results are in good agreement 1 36 ANTARCTIC METEOROLOGY AND CLIMATOLOGY TABLE 6. 0 with modeling studies which were carried out more than a decade later [Parish, 1982; Parish and Bromwich, 1987]. Such sastrugi are very pronounced in Adelie Coast and can reach heights exceeding 1 m. Blowing s n o w can t r a n s p o r t large a m o u n t s of snow, and this distribution c a n h a v e great importance for glaciological studies [Radok, 1970]. It h a s b e e n de scribed as a low-level a v a l a n c h e moving slowly to the edge of the Antarctic continent and t h e n out to the o c e a n .
F o r D o m e C, n o relationship is o b s e r v e d , but a well-established d e p e n d e n c y is found for all slope stations; D80 is s h o w n as an e x a m p l e in Figure 11. Colder m o n t h s h a v e stronger w i n d s , a result t o b e e x p e c t e d . Cold t e m p e r a t u r e s normally are associated with strong inversions and h e n c e strong gravitational flow. 2. Radiative Fluxes and Surface Energy Balance During Austral s u m m e r 1985/1986 a large field p r o gram w a s carried out in Adelie C o a s t .
Antarctic Meteorology and Climatology: Studies Based on Automatic Weather Stations by David H. Bromwich, Charles R. Stearns