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Recovery of sensible heating and its elevation amplification over and around the Tibetan Plateau since 2000s

机译:自2000年代以来藏高高原及其周围地区的康技加热及其高度放大

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摘要

Based on historical observations daily data for 1981-2016 from 130 meteorological stations over and around the Tibetan Plateau (TP), the trends of sensible heat flux (SH) and their elevation dependence were investigated. Results indicate that the SH over and around the TP experienced apparent trends' shift in approximately 2000, demonstrating noticeable reductions during 1981-2000 and pronounced recovery during 2001-2016 for the four seasons. The relation between elevations and trends in SH over and around TP has shown a feature known as "elevation amplification." Pronounced elevation-dependent reductions in SH can be discovered for the four seasons except winter during 1981-2000, and a substantially more significant enhance in SH was found in the higher elevation plateau compared to the lower elevation plateau during 2001-2016. The elevation-dependent trends of surface wind speed (V-0) influenced by the atmospheric circulation anomalies were the dominant factor driving the elevation-dependent trends of SH whenever during 1981-2000 and 2001-2016. During 1981-2000 (2001-2016), the areas to the north of TP warmed more strengthened (weaker) than the areas to the south of TP. It led to the anomalous temperature gradient and geopotential height gradient from the south (north) of TP to the north (south) of TP and resulted in decreasing (increasing) trends of the 500hPa subtropical westerlies over and around the TP. Furthermore, it caused the rate of reduction (increases) in V-0 amplified with elevation, because the higher altitude areas responded more strongly to the changes of atmosphere wind speed. As a result of the elevation-dependent reductions (increases) of V-0, the positive correlation between the subdued (enhanced) SH and elevation occurred in TP during 1981-2000 (2001-2016). The difference in ground-air temperature (Ts-Ta) was another factor influencing elevation dependence of SH trends during 2001-2016, which needs further investigations.
机译:基于历史观察,1981 - 2016年的每日数据来自藏高高原(TP)的130个气象站,研究了明智的热通量(SH)的趋势及其高程依赖性。结果表明,TP超过2000年的SH经历了明显的趋势转变,在1981 - 2000年期间展示了明显的减少,并在2001-2016期间为四季发出恢复。 TP的SH左右升高和趋势之间的关系显示了称为“高度放大”的特征。在1981 - 2000年的冬季除了除冬季除外的四个季节,可以发现SH中的明显高程依赖性,并且在2001 - 2016年期间较低的高度高原相比,在较高的高度高原上发现了SH的大幅增强。受大气循环异常影响的表面风速(V-0)的高程依赖性趋势是在1981-2000和2001-2016期间驾驶SH的高程依赖趋势的主导因素。在1981-2000(2001-2016)期间,TP北部的地区更加加强(弱),而不是TP南部的地区。它导致了从TP北(南部)到TP的南(北)的异常温度梯度和地孔势高度梯度,导致TP等500HPA亚热带韦斯特尔的趋势降低(越来越多)。此外,它导致V-0中的减少(增加)升高,因为较高的海拔区域对大气速度的变化更强烈地响应。由于V-0的升高依赖性减少(增加),在1981-2000(2001-2016)期间,TP在TP中发生了抑制(增强型)SH和高程之间的正相关。地面气温(TS-TA)的差异是影响2001 - 2016年SH趋势的升高依赖性的另一个因素,需要进一步调查。

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  • 来源
    《Theoretical and applied climatology》 |2021年第2期|617-630|共14页
  • 作者单位

    Chinese Acad Sci Northwest Inst Ecoenvironm & Resources Key Lab Land Surface Proc & Climate Change Cold & Lanzhou 730000 Peoples R China|Univ Chinese Acad Sci Beijing 100049 Peoples R China;

    Chinese Acad Sci Inst Tibetan Plateau Res Key Lab Tibetan Plateau Earth Syst Resources & En Land Atmosphere Interact & Its Climat Effects Grp Beijing 100101 Peoples R China|CAS Ctr Excellence Tibetan Plateau Earth Sci Beijing 100101 Peoples R China;

    Chinese Acad Sci Northwest Inst Ecoenvironm & Resources Key Lab Land Surface Proc & Climate Change Cold & Lanzhou 730000 Peoples R China|CAS Ctr Excellence Tibetan Plateau Earth Sci Beijing 100101 Peoples R China;

    Chinese Acad Sci Inst Tibetan Plateau Res Key Lab Tibetan Plateau Earth Syst Resources & En Land Atmosphere Interact & Its Climat Effects Grp Beijing 100101 Peoples R China|CAS Ctr Excellence Tibetan Plateau Earth Sci Beijing 100101 Peoples R China;

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