500hPa全球动能年际变率及1983和1987年两个厄尼诺年动能距平的差异
ON THE INTERANNUAL VARIABILITY IN GLOBAL KINETIC ENERGY AT 500hPa AND THE DIFFERENCE IN ENERGY ANOMALIES BETWEEN THE TWO EI NIÑO YEARS OF 1983 AND 1987
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摘要: 利用1980-1988年9年期间ECMWF500hPa全球风场资料,计算7个“纬度带”上三种基本动能模态,研究这些动能模态的各年异常情况。结果表明,1983年是这9年内动能唯一的正值异常年,而1987年和1985年动能基本上属于正常年,只有个别动能模态有异常。这说明,1980年代两个厄尼诺年的异常情况有很大的差异。动能模态与赤道东太平洋海温距平(SSTA)的后延相关表明,1983年事件的影响可以波及范围相当广泛甚至波及全球大气,而1987年事件所能影响的范围远比1983年事件要小。此外,还表明北半球副热带急流轴附近是对SSTA响应的敏感地区。Abstract: Using the materials of 21 kinetic energy items (abbreviated to KED which are incorporated seven latitudinal belts with three primary energy modes, at 500hPa in the whole range of the globe during the 9 years of 1980-1988, the anomaly in kinetic energy for each year is investigaed. The annual anomaly was classified into four grades, i.e. anomalous, subanomalous, fair average anomalous and approximately normal. It is shown that 1983 was the only anomalous year during the nine years studied, but the 1987 El Ninño year and the 1985 La Nina year both belonged to the approximately normal one. So, there are great differences in the grade of the energy anomaly between the two El Ninño years during eighties. The main KEIs by which the anomalies were characterized during the three event years, all are very high lag-cross correlation coefficients with SSTA in the equatorial eastern Pacific. It is shown that the anomalies of these KEIs responded to the three events. Besides, it is also shown that the northern subtropical jet is a sensitive region to respond to the SSTA. In responses to the three events there were three different typical character in the subtropical jet.
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Keywords:
- El Ninñ /
- o /
- Global kinetic energy
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Quiroz R S. The climate of the El Ninño-winter of 1982-83: a season of extraordinary climate anomalies. Mon Wea Rev. 1983. 111 (8):1685-1706.
Zhao Hanguang. Zhang Xiangong. Ding Yihui. El Ninño and the anomalies climate in China. Acta Meteorologica Sinica, 1989, 3 (4):471-481.
Zang Hengfan.Wang Shaowu. El Ninño and Anti-El Ninño events in 1854-1987. Acta Oceanologica Sinica 1990.9 (2):353-362.
Ardanuy P E. Krishnamurti T N. Divergent circulations inferred from Nimbus-7 ERB: Application to the 1982-1983 ENSO-event. J Meteor Soc Japan 1987. 65 (3):353-370.
吴国雄,Cubasch U. El Ninño海温异常对纬向平均经圈环流及大气箱送特征的影响.中国科学.B辑,1986. 10:1109-1120. 于惠岑.蒲书蔑.1986/1987厄尔尼诺期间的西风强化和海气相互作用过程的分析.大气科学,1992. 4: 427-435. 陈月娟.丁明.太平洋海温对其上空环流影响的分析及数值试验.大气科学.1992, 16 (5):592-600. Qiu Yongyan. On the seasonal transition and the interannual variation in global kinetic energy at 500hPa. accompanied with anomalies of energy during the 1982/83 ENSO. Adv Atmos Sci, 1993. 10 (2):248-256.
中国人民解放军总参谋部气象局译,南半球气象学,1975. 330. Bjerknes J.A possible response of the atmospheric Hadley circulation to equatorial anomalies of ocean temperalure. Tellus. 1966. 18: 820-829.
Kousky V E, Leetman A. The 1986-87 Pacific warm episode: Evolution of oceanic and atmospheric anomaly field.J Climate. 1989. 2 (3):254-267.
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