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我国季平均的0.8m地温距平场与后一季降水场的相关分析
引用本文:汤懋苍,张建,王敬香,杨良. 我国季平均的0.8m地温距平场与后一季降水场的相关分析[J]. 气象学报, 1988, 46(4): 481-485
作者姓名:汤懋苍  张建  王敬香  杨良
作者单位:中国科学院兰州高原大气物理研究所(汤懋苍,张建,王敬香),中国科学院兰州高原大气物理研究所(杨良)
摘    要:从1975年到现在,我们用1.6m地温做汛期(4~9月)降水预报的工作已有13年。根据汤懋苍在美国的工作,用1.02m季平均地温距平做美国下一季的降水预报,其历史检验的效果似乎比中国略好,但美国地温的资料情况比中国要差得多,到1982年为止有1.02m深度地温的测站仅38个,由于资料太少以至于分析图时颇感困难。而中国现有0.8m地温的测站已达200多个,这样所分析出的图任意性很小,所以实际预报的效果应该是中国的比美国的好。

收稿时间:1986-09-24
修稿时间:1987-05-19

THE SIMILARITY BETWEEN THE SEASONAL ANOMALOUS MAPS OF SOIL TEMPERATURE AND THE PRECIPITATION OF THE SUBSEQUENT SEASON
Tang Maocang,Zhang Jian,Wang Jingxiang and Yang Liang. THE SIMILARITY BETWEEN THE SEASONAL ANOMALOUS MAPS OF SOIL TEMPERATURE AND THE PRECIPITATION OF THE SUBSEQUENT SEASON[J]. Acta Meteorologica Sinica, 1988, 46(4): 481-485
Authors:Tang Maocang  Zhang Jian  Wang Jingxiang  Yang Liang
Affiliation:Lanzhou Institute of Plateau Atmospheric Physics, Academia Sinica;Lanzhou Institute of Plateau Atmospheric Physics, Academia Sinica;Lanzhou Institute of Plateau Atmospheric Physics, Academia Sinica;Lanzhou Institute of Plateau Atmospheric Physics, Academia Sinica
Abstract:Based on observations in China during last 30 year s(1954-1983) it was found that seasonal anomalous patterns of soil temperature at a depth of 80cm look similar to the pattens of precipitation of the subsequent season. The mean distance of the maximum axes between the above two elements were less than 2 Lat. with a percent of 76 00.To predict the subsequent season will be a wet(dry) season at east half China, a clear signal is that a cold trough(warm ridge) of 80cm soil temperature have been located in the east edge of Tibet Plateau (100°-105°E) during this season.
Keywords:
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