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Observational evidence that soil moisture variations affect precipitation - art. no. 1241

机译:土壤水分变化影响降水的观测证据-艺术。没有。 1241

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摘要

1] Land-atmosphere feedback, by which precipitation-induced soil moisture anomalies affect subsequent precipitation, may be an important element of Earth's climate system, but its very existence has never been demonstrated conclusively at regional to continental scales. Evidence for the feedback is sought in a 50-year observational precipitation dataset covering the United States. The precipitation variance and autocorrelation fields are characterized by features that agree (in structure, though not in magnitude) with those produced by an atmospheric general circulation model (AGCM). Because the model-generated features are known to result from land-atmosphere feedback alone, the observed features are suggestive of the existence of feedback in nature. [References: 14
机译:1]陆地大气反馈可能是地球气候系统的重要组成部分,而降水引起的土壤水分异常会影响随后的降水,但它的存在从未在区域到大陆尺度上得到最终证实。在涵盖美国的50年观测降水数据集中寻求反馈的证据。降水方差和自相关场的特征是与大气总循环模型(AGCM)产生的特征(结构上,尽管大小不同)一致。由于已知模型生成的特征仅来自陆地-大气反馈,因此观察到的特征暗示了自然界中存在反馈。 [参考:14

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