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Observational evidence of the combined influence of atmospheric circulations and local factors on near‐surface meteorology in Dagze Co basin, inner Tibetan Plateau

机译:大气环盆地近地表气象综合影响的观察证据综合影响,内藏高原

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ABSTRACT >Based on meteorological observations of three automatic weather stations (AWSs), spanning an altitudinal range of 1400 m from 4480 to 5880 m above sea level (m a.s.l.) during August 2015 to August 2016, this study presents a description of the spatio‐temporal characteristics of the near‐surface meteorology of the Dagze Co (lake) basin in the interior of the Tibetan Plateau. We also investigated the influence of synoptic atmospheric systems and local factors on the meteorological characteristics. We found that the onset and withdrawal of the South Asian summer monsoon triggered seasonal shift in meteorological variables including wind direction, precipitation, and relative humidity. In addition, the magnitude of various meteorological factors during the monsoonal period is clearly associated with the intensity of the South Asian summer monsoon, which subsequently controls the lake water budget of Dagze Co. Moreover, both the local topography and the existence of the lake contribute significantly to the altitudinal variation of several meteorological factors. For example, the orographic precipitation near the glaciated area at 5880 m a.s.l. was about three times greater than in the area adjacent to the lake. The dominating katabatic wind over these glaciated areas weakens the up‐valley wind and consequently wind speed tends to decrease with increasing elevation during the monsoonal season. In addition, different levels of cloudiness between the low‐altitude lake and the glaciated mountain area contribute to a 40–50% reduction in incoming short‐wave radiation receipt. Our observations will hopefully contribute to future glacio‐hydrological studies and will help to evaluate statistically/dynamically downscaled climate fields in the interior of Tibetan Plateau which contains numerous lakes and glaciers. </abstract> </span> <span class="z_kbtn z_kbtnclass hoverxs" style="display: none;">展开▼</span> </div> <div class="translation abstracttxt"> <span class="zhankaihshouqi fivelineshidden" id="abstract"> <span>机译:</span><abstract xmlns =“http://www.wiley.com/namespaces/wiley”type =“main”xml:lang =“en”> <title type =“main”>基于的</ title> >本研究期间,三次自动气象站(AWSS)的气象观测,跨越海拔4400米至5880米(M ASL)的海拔1400米至5880米,介绍了对时空特征的描述藏高原内部Dagze Co(Lake)盆地近表面气象。我们还研究了天气大气系统和地方因素对气象特征的影响。我们发现南亚夏季季风的发病和撤回触发了气象变量的季节性转变,包括风向,降水和相对湿度。此外,在季风期间的各种气象因素的大小明显与南亚夏季季风的强度有关,随后控制了Dagze公司的湖泊水预算,这两个地形和湖泊的存在贡献显着达到几种气象因素的高度变化。例如,在5880 m A.L的冰川区域附近的地形沉淀。比湖泊相邻的地区大约三倍。这些冰川区域的主导的Katabatic风削弱了上谷风,因此风速随着季风季节期间的增加而趋于降低。此外,低空湖泊和冰川山区之间的不同水平的浑浊有助于40-50%的传入短波辐射收据减少。我们的观察结果希望有助于未来的巨大水文研究,并有助于评估藏高高原内部的统计/动态较低的气候田,其中包含许多湖泊和冰川。</ p> </摘要> </span> <span class="z_kbtn z_kbtnclass hoverxs" style="display: none;">展开▼</span> </div> </div> <div class="record"> <h2 class="all_title" id="enpatent33" >著录项</h2> <ul> <li> <span class="lefttit">来源</span> <div style="width: 86%;vertical-align: text-top;display: inline-block;"> <a href='/journal-foreign-21026/'>《International Journal of Climatology: A Journal of the Royal Meteorological Society》</a> <b style="margin: 0 2px;">|</b><span>2018年第4期</span><b style="margin: 0 2px;">|</b><span>共11页</span> </div> </li> <li> <div class="author"> <span class="lefttit">作者</span> <p id="fAuthorthree" class="threelineshidden zhankaihshouqi"> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Yang Wei&option=202" target="_blank" rel="nofollow">Yang Wei;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Guo Xiaofeng&option=202" target="_blank" rel="nofollow">Guo Xiaofeng;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Wang Yongjie&option=202" target="_blank" rel="nofollow">Wang Yongjie;</a> </p> <span class="z_kbtnclass z_kbtnclassall hoverxs" id="zkzz" style="display: none;">展开▼</span> </div> </li> <li> <div style="display: flex;"> <span class="lefttit">作者单位</span> <div style="position: relative;margin-left: 3px;max-width: 639px;"> <div class="threelineshidden zhankaihshouqi" id="fOrgthree"> <p>Key Laboratory of Tibetan Environment Changes and Land Surface ProcessesInstitute of Tibetan Plateau Research Chinese Academy of SciencesBeijing China;</p> <p>State Key Laboratory of Atmospheric Boundary Layer Physics and Atmospheric ChemistryInstitute of Atmospheric Physics Chinese Academy of SciencesBeijing China;</p> <p>Key Laboratory of Tibetan Environment Changes and Land Surface ProcessesInstitute of Tibetan Plateau Research Chinese Academy of SciencesBeijing China;</p> </div> <span class="z_kbtnclass z_kbtnclassall hoverxs" id="zhdw" style="display: none;">展开▼</span> </div> </div> </li> <li > <span class="lefttit">收录信息</span> <span style="width: 86%;vertical-align: text-top;display: inline-block;"></span> </li> <li> <span class="lefttit">原文格式</span> <span>PDF</span> </li> <li> <span class="lefttit">正文语种</span> <span>eng</span> </li> <li> <span class="lefttit">中图分类</span> <span><a href="https://www.zhangqiaokeyan.com/clc/1232.html" title="气候学">气候学;</a></span> </li> <li class="antistop"> <span class="lefttit">关键词</span> <p style="width: 86%;vertical-align: text-top;"> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=lake&option=203" rel="nofollow">lake;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=meteorology&option=203" rel="nofollow">meteorology;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=monsoon&option=203" rel="nofollow">monsoon;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Dagze Co&option=203" rel="nofollow">Dagze Co;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Tibetan Plateau&option=203" rel="nofollow">Tibetan Plateau;</a> </p> <div class="translation"> 机译:湖;气象学;季风;达格尔有限公司;藏高原; 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