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中国农学通报 ›› 2013, Vol. 29 ›› Issue (17): 198-201.doi: 10.11924/j.issn.1000-6850.2012-3030

所属专题: 农业气象

• 资源 环境 生态 土壤 气象 • 上一篇    下一篇

气候变暖对辽宁西部地区冻土的影响

杨学强 张国林   

  • 收稿日期:2012-09-05 修回日期:2012-10-10 出版日期:2013-06-15 发布日期:2013-06-15

Impact of Climate Warming on Permafrost in Western Liaoning

  • Received:2012-09-05 Revised:2012-10-10 Online:2013-06-15 Published:2013-06-15

摘要: 为了给工农业生产及冻土研究提供依据,利用辽宁西部1960/1961—2009/2010年冬季的气候资料,分析辽西半干旱区冻土持续期、冻土最大深度变化特征以及对气候变暖的响应。结果表明:辽宁西部地区冻土持续期变暖明显,气温倾向率为0.787℃/10 a,近10年比20世纪60年代升高3.2℃。在气候变暖环境下,冻土封冻始期变化平缓;冻土层化通日期存在提前趋势,近10年比20世纪60年代提前7天;冻土持续期存在缩短趋势,但不明显;冻土最大深度明显变浅,倾向率为-4.120 cm/10 a,近10年比20世纪60年代变浅12 cm。气温、地面温度及降水量对冻土最大深度影响显著,与气温存在线性关系,当气温每升高1℃,冻土最大深度将变浅5.74 cm。冻土层变浅有利于工农业生产,同时也有利于病虫越冬和界限北移,对防虫防疫不利。

关键词: 园林应用, 园林应用

Abstract: In order to provide the basis for industrial & agricultural production and permafrost research, analyze the permafrost duration, variation characteristics at maximum depth of permafrost and response to climate warming in semi-arid region of western Liaoning based on winter climate data from 1960/1961 to 2009/2010. The results showed that: permafrost duration in the western Liaoning was obviously impacted by climate warming, the temperature tendency was 0.787℃/10 a, nearly 10 a, 3.2℃ higher than the 1960s. Under the warming environment, permafrost frozen period changed smoothly; the permafrost melting date was being ahead of time, nearly 10 a, 7 d earlier than in the 1960s; the permafrost duration was decreasing, but not obvious; permafrost maximum depth was significantly decreasing, the temperature tendency was -4.120 cm/10 a, nearly 10 a, 12 cm less than the 1960s. Air temperature, ground temperature and precipitation made the significant impact on permafrost maximum depth, there was a linear relationship between air temperature and permafrost maximum depth, when the temperature increased by 1°C, the maximum depth of permafrost would decrease by 5.74 cm. The shallowing permafrost was conducive to industrial & agricultural production, and however, it caused pest overwintering and northward movement of plague boundaries, resulting in unfavorable impact on pest control and epidemic prevention.