青藏高原东北部青海省1960 - 2008年气温和降水的时空变化

Ying Yang, G. Dong, Yan Zhao, Guoqiang Li, Lele Ren, Keyan Fang, Xiandu Wu
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引用次数: 2

摘要

采用t检验方法对1960—2008年青海省气温和降水资料的线性斜率进行了分析。研究结果表明,在此期间,青海省的气温和降水均呈上升趋势,但存在波动。此外,气温与降水变化呈高度正相关。以夏季风为主的青海省东南部(SEQP)和以西风带为主的青海省西北部(NWQP)的长期气温和降水趋势基本一致,气温和降水均呈上升趋势。总的来说,西北qp的温度变化幅度大于东南qp。而西北qp的降水变化幅度与东南qp接近。降水增加趋势的核心区位于高海拔地区,如青海高原南部和祁连山,而降水增加趋势不显著的地区位于低洼地区,如青海湖盆地和柴达木盆地。这种对比模式可能是地形引起的抬升和下沉空气动力学的结果。
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SPATIOTEMPORAL VARIABILITY OF TEMPERATURE AND PRECIPITATION DURING 1960—2008INFERRED FROM INSTRUMENTAL RECORDS IN QINGHAI PROVINCE,NORTHEASTERN TIBETAN PLATEAU
Linear slopes of instrumental temperature and precipitation data from 1960to 2008in Qinghai Province,China,were analyzed to observe their temporal trends by a T-test method.Our findings indicate that both temperature and precipitation exhibit an increasing trend with fluctuations during that period across Qinghai Province.In addition,temperature and precipitation variations are highly positively correlated.The long-term temperature and precipitation trends of southeast Qinghai Province(SEQP),which is mainly controlled by the summer monsoon,and those of northwest Qinghai Province(NWQP),which is dominated by the Westerlies,are generally in agreement,with both temperature and precipitation exhibiting a rising trend.In general,the amplitude of temperature changes in the NWQP is larger than that in the SEQP.However,the amplitude of precipitation changes in NWQP is close to that in SEQP.The core regions that exhibit an increasing precipitation trend are located in high-altitude areas,such as southern Qinghai Plateau and Qilian Mountains,while the regions with an insignificant increasing trend are located in low-lying areas,such as Qinghai Lake Basin and Qaidam Basin.The contrasting pattern may be a result of topography-induced uplifting and subsiding air dynamics.
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