Numerical simulation of Eurasian teleconnection pattern in atmospheric circulation during the Northern Hemisphere winter

Author:

Gambo K.,Li Lu,Weijing Li

Publisher

Springer Science and Business Media LLC

Subject

Atmospheric Science

Reference13 articles.

1. Bjerknes, J. (1969), Atmospheric teleconnections from the equatorial Pacific.Mon. Wea. Rev.,97:162–172.

2. Doberitz, R. (1968), Cross spectrum analysis of rainfall and sea temperature at the equatorial Pacific Ocean,Bonn Meteor. Abh.,8, 61.

3. Gambo, K. and K. Kudo. (1983), Three-dimensional teleconnections in the zonally asymmetric height field during the Northern Hemisphere Winter.J. Meteor. Soc. Japan, 61:36–50.

4. Chan, S. J., J. W. Lingaas, M. E. Schlesinger, R. L. Mobley and W. L. Gates (1982), A documentation of the OSU two-level atmospheric general circulation model, Climate Research Institute Oregon State University, Report No. 35.

5. Hoskins, B. J. and D. J. Karoly (1981), The steady linear response of a spherical atmosphere to thermal and orographic forcing.J. Atmos. Sci.,38: 1179–1196.

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