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Abstract:
The mass stream function of zonal mean meridional circulation is calculated in terms of NCEP/NCAR monthly meridional wind speed and vertical velocity, and the climatic and anomalous features of zonal mean SST and meridional circulation are investigated. Results show that (1) a joint ascending branch of Northern and Southern Hadley circulation is on the side of the summer hemisphere near the equator ,being well consistent with the extremum of [SST ],and a strong descending by the winter-hemispheric side.(2)El Nino-related [SST] in low latitudes is an important outer-forcing source for anomaly meridional circulation, which is affected by seasonal variation of basic airflow and [SST ], and interannual and interdecadal changes of [SST] .
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References
[1]
|
LORENZ E N. The nature and theory of general circulation [M]. Beijing: Science Press, 1976. 26-27. |
[2]
|
YE Du-zheng, ZHU Bao-zhen. Some basic issues about general circulation [M]. Beijing: Science Press, 1958.44-56. |
[3]
|
WU Guo-xong, TIBALDI S. The effects of mechanical forcing on the mean meridional circulation andtransfer properties of the atmosphere [J]. Advances in Atmospheric Sciences, 1987, 4: 24-42. |
[4]
|
GREEN J S A. Transfer properties of the large-scale eddies and the general circulation of the atmosphere [J].Quarterly Journal of Royal Meteorological Society, 1970, 94: 157-185. |
[5]
|
BJERKNES J. A possible response of the atmospheric Hadley circulation to equatorial anomalies of oceantemperature [J]. Tellus, 1966, 18: 820-829. |
[6]
|
WU Guo-xiong, CUBASCH U. The effects of SSTA on zonally mean meridional circulation andcharacteristics of atmospheric transportation [J]. Scientia Sinica, 1986, 10: 1110-1120. |
[7]
|
WANG Pan-xing. Diagnosis of mean meridional circulation of the model atmosphere in the GCM with lowresolution vertically [J]. Journal of Nanjing Institute of Meteorology, 1994, 17: 200-204. |
[8]
|
KALNAY E, KANAMITSU M, KISTLER R. The NCEP/NCAR 40-year reanalysis project [J]. Bulletin of theAmerican Meteorological Society, 1996, 77: 437-471. |
[9]
|
Service Center for Atmospheric information, Nanjing Institute of Meteorology, Earth Science Department,Council of Natural Science Foundation of China. Bulletin of Data [J]. Journal of Nanjing Institute ofMeteorology, 1998, 21: 455-458. |
[10]
|
PALMEN E, VUORELA L. On the mean meridional circulations in the northern hemisphere during thewinter season [J]. Quarterly Journal of Royal Meteorological Society, 1963, 89: 131-138. |
[11]
|
VUOROLA L A, TUOMINEN L. On the mean zonal and meridional circulations and the flux of moisturein the northern hemisphere during the summer season [J]. Pure Applied Geophysics, 1964, 57: 167-180. |
[12]
|
WU Guo-xiong, TIBALDI S. A calculation scheme for atmospheric mean meridional circulation [J].Scientia Sinica (Series B), 1988, 4: 1-8. |
[13]
|
ZHAO Zhen-guo, JIANG Bo-ren, CHEN Guo-zhen. Relationship of ENSO event with the snow cover inAinghai-Xizang Plateau and atmosphere circulation in the East Asia [J]. Shandong Meteorology, 1999, 4: 1-8. |
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