Local and Remote Responses to Excessive Snow Mass over Eurasia Appearing in the Northern Spring and Summer Climate
Author:
Affiliation:
1. Institute of Geoscience, University of Tsukuba
2. Meteorological Research Institute
Publisher
Meteorological Society of Japan
Subject
Atmospheric Science
Link
https://www.jstage.jst.go.jp/article/jmsj1965/69/4/69_4_473/_pdf
Reference42 articles.
1. Arakawa A. and W.H. Schubert, 1974: Interaction of a cumulus cloud ensemble with the large-scale environment. Part I. J. Atmos. Sci., 31, 674-701.
2. Asakura, T., 1968: Dynamic climatology of atmospheric circulation over east Asia centered in Japan. Papers Meteor. Geophys., 19, 1-68.
3. Barnett, T.P., 1985: Variations in near-global sea level pres sure. J. Atmos. Sci., 42, 478-501.
4. Barnett, T.P., L. Dumenil, U. Schlese, E. Roeckner and M. Latif, 1989: The effect of Eurasian snow cover on regional and global climate variations. J. Atmos. Sci., 46, 661-685.
5. Blanford, H.F., 1884: On the connexion of Himalayan snowfall and seasons of drought in India. Proc. Royal Soc. London, 37, 3-22.
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