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作 者:游性恬[1] 熊廷南[1] T.Yasunari H.L.Tanaka
机构地区:[1]北京气象学院,北京100081 [2]筑波大学地球科学系
出 处:《大气科学》2000年第5期660-668,共9页Chinese Journal of Atmospheric Sciences
摘 要:通过大气环流模式试验,研究了春季亚洲中纬带地面湿度异常对其后4个月月平 均气候参数的影响。结果发现:正的地面湿度异常对其后气候参数的影响在第1个月最弱, 第3个月最强;它导致欧亚中高纬带在第2~4个月对流层内的高度和温度都降低,低值系 统发展,副热带高压亦发展,中纬度西风急流相应增强;同时北美东岸有明显的遥相关响 应。The impact of anomalous ground wetness (GW) in spring over Asian mid-latitudes on the monthly climatic parameters in the following four months is investigated with a GCM experiment. The main results are summarized as follows: the effect of positive GW anomalies on the monthly climatic parameters is the weakest for the first following month and the strongest for the third following months; the positive anomalous GW leads to decreases of both height and temperature in the whole troposphere over most mid-high latitudes of Asia for all following four months, to developments of both the depressions in mid-high latitudes and the subtropical high, and thus to intensification of the westerly jet; and some evidences of teleconnection remarkably appear in the atmospheric circulation over the east coast of North America.
分 类 号:P461.6[天文地球—大气科学及气象学]
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