山西东南部气候变暖与冻土的气候特征分析  

Analysis of Climate Warming and Frozen Soil Characteristics in Southeast Shanxi Province

作　　者：王正旺 李晶晶 王媚 王景秀 武志跃 孙英杰 

机构地区：[1]山西省长治市气象局,山西长治046000

出　　处：《中国农学通报》2014年第35期195-200,共6页Chinese Agricultural Science Bulletin

基　　金：山西省气象局重点项目"山西省云量精细化预报方法研究"(sxkzdtq20090504);山西省科技攻关项目"基于Gi S的极端气象灾害预警与评估集成系统"(20090311083)

摘　　要：为了进一步研究在气候变暖情况下土壤封解冻的变化规律,本研究应用山西东南部11个气象观测站近40年气温、平均冻土深度、最大冻土深度、浅层（5-20 cm）冻土封解冻资料,采用统计对比聚类法,分析了气候变暖与冻土的气候变化特征。结果显示：山西东南部气候变暖较为明显,年际线性趋势增温率为0.3℃/10 a,增温贡献最大为冬季。随着冬季气候的变暖,平均冻土深度与最大冻土深度均趋向变浅。在冬春、秋冬2个转换期气候变暖的前提下,浅层冻土的平均冻结终日与始日分别显现出提前和推后,意味着浅层土壤封冻期的缩短。In order to further study the climate warming, soil sealing of thawing, according to the data of temperature, average frozen depths, maximum frozen depths and shallow （5-20 cm） permafrost thaw of 11 meteorological stations in recent 40 years in southeastern Shanxi, the authors used the statistical comparison clustering method to analyze the characteristics of climate warming and climate change of frozen soil. The result showed： the climate warming was evident in southeast Shanxi Province, linear trend of annual increasing rate was 0.3 ℃/10 a, the maximum contribution of warming was winter. As winter climate warming, average frozen depth and maximum frozen depth tended to be decreased. Under the premise of climate warming in winter-spring and autumn-winter, the average freeze ending date and the beginning date of shallow soils were advanced and pushed back respectively, indicated that the shallow soil freezing period was shortening.

关 键 词：气候变化 冻土 封解冻日期 山西东南部 

分 类 号：P467[天文地球—大气科学及气象学]