Get PDF (2323K) - Wiley Online Library
Get PDF (2323K) - Wiley Online Library
Get PDF (2323K) - Wiley Online Library
You also want an ePaper? Increase the reach of your titles
YUMPU automatically turns print PDFs into web optimized ePapers that Google loves.
EURASIAN SNOW COVER AND ATMOSPHERIC CIRCULATION 621<br />
200<br />
300<br />
400<br />
500<br />
600<br />
700<br />
800<br />
900<br />
1000<br />
40N 45N 50N 55N 60N 65N 70N<br />
200<br />
300<br />
400<br />
500<br />
600<br />
700<br />
800<br />
900<br />
1000<br />
40N 45N 50N 55N 60N 65N 70N<br />
200<br />
300<br />
400<br />
500<br />
600<br />
700<br />
800<br />
900<br />
1000<br />
40N 45N 50N 55N 60N 65N 70N<br />
Figure 4. The 11-year mean (1980–90) pressure–latitude sections of meridional and vertical wind fields along a longitudinal sector<br />
averaged over 30–60 °E for (a) March, (b) April and (c) May. The shaded regions are southerly wind components greater than 1 m s −1<br />
Copyright © 2003 Royal Meteorological Society Int. J. Climatol. 23: 615–629 (2003)
Change language