Asymmetric effects of soil moisture on mean daily maximum and minimum temperatures over eastern China

Asymmetric effects of soil moisture on mean daily maximum and minimum temperatures over eastern China
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土壤湿度对中国东部地区日平均最高气温和最低气温的不对称影响

DOI:
10.1007/s00703-013-0284-2
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发表时间:
2012-12
影响因子:
2
通讯作者:
Jingyong Zhang
Jingyong Zhang
中科院分区:
地球科学4区
文献类型:
--
作者:
Lingyun Wu;Jingyong Zhang

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This study statistically investigates the effects of soil moisture on mean daily maximum () and minimum temperatures () over eastern China in spring (from March to May), summer (from June to August) and fall (from September to November), using the Global Land Data Assimilation System (GLDAS) soil moisture and observational temperatures. The results show that soil moisture exerts asymmetric effects onand, thereby has substantial effects on the diurnal temperature range (DTR) in the three seasons. The soil moisture feedbacks on,, and DTR are found to evidently vary with season. In spring and summer, soil moisture exerts stronger negative forcing onthan, and thus has negative effects on the DTR over many areas of northern China. In fall, soil moisture has much stronger positive effects onthan, and thus has significant negative effects on the DTR over Northeast China and some areas of the climatic and ecological transition zone of northern China. The uncertainties in the employed data and method should be noted. Therefore, the results need to be further investigated by other data sets and methods in the future.
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影响因子: 3.8
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