Impact of summer monsoon on the elevation‐dependence of meteorological variables in the south of central Himalaya

Yang Kun; Guyennon Nicolas; Ouyang Lin; Tian Lide; Tartari Gianni; Salerno Franco

摘要

ABSTRACT >The South Asian summer monsoon brings abundant precipitation and associated latent heat release to the south of central Himalaya, and alters hydrothermal conditions of this region. This study explored the impact of South Asian summer monsoon on the elevation‐dependence of meteorological variables along the south slope of Mt. Everest in the central Himalaya, which is crucial to modelling the glacio‐hydrological processes in this elevated region. The data were collected at five stations deployed at 2660–5600 m above sea level (asl) along the slope during 2007–2011. Major findings are the following: (1) The amount of precipitation during the monsoon season usually decreases with elevation but it is relatively uniform between 3600 and 5000 m asl. This uniform profile may be attributed to the monsoon–terrain–land interactions, particularly to the retard effect of glacier cooling on daytime upvalley wind; (2) Cloud shielding effects cause lower solar radiation and higher downward longwave radiation in the monsoon than in the other seasons. In particular, higher elevations have more clouds in the afternoon, resulting in an abnormal elevation‐dependence of solar radiation (i.e. higher elevations receive less solar radiation); (3) Strong daytime upvalley wind and moist convection homogenizes the vertical distributions of air mass along the slope, causing a constant lapse rate of both surface air temperature and dew‐point temperature (representing humidity) during typical monsoon months, but this phenomenon is not found in the other seasons. These findings provide critical guidance for extrapolating the meteorological variables from lower to higher elevations in this region. </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”>抽象</ title> >南方亚洲夏季季风在喜马拉雅中部南部带来丰富的降水和相关的潜热释放，并改变了该地区的水热条件。本研究探讨了南亚夏季季风对MT南坡南坡沿海气象变量的升高的影响。珠穆朗玛峰在中央喜马拉雅山脉，这对建模该升高区域的甘草水文过程至关重要。在2007 - 2011年期间，在沿着坡度在海拔2660-5600米处的五个站点收集数据。主要发现如下：（1）季风季节的降水量通常用升高减少，但在3600和5000米ASL之间相对均匀。这种均匀的型材可以归因于季风 - 地形陆战的相互作用，特别是冰川冷却在白天Upvalley风中的延迟效果; （2）云屏蔽效果导致季风辐射较低，季风较高的龙波辐射而不是在其他季节。特别地，较高的海拔在午后具有更多的云，导致太阳辐射的异常依赖性（即，较高的高度接收太阳辐射）; （3）强大的白天Upvalley风和潮湿对流均匀化沿斜坡的空气质量垂直分布，在典型的季风月内导致表面空气温度和露点温度（代表湿度）的恒定流逝速率，但这种现象不是发现在其他季节。这些调查结果提供了将气象变量从该区域的降低到更高的高度推断出来的关键指导。</ 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12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 Kun&option=202" target="_blank" rel="nofollow">Yang Kun;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Guyennon Nicolas&option=202" target="_blank" rel="nofollow">Guyennon Nicolas;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Ouyang Lin&option=202" target="_blank" rel="nofollow">Ouyang Lin;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Tian Lide&option=202" target="_blank" rel="nofollow">Tian Lide;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Tartari Gianni&option=202" target="_blank" rel="nofollow">Tartari Gianni;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Salerno Franco&option=202" target="_blank" rel="nofollow">Salerno Franco;</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>Ministry of Education Key Laboratory for Earth System Modeling Department of Earth System ScienceTsinghua UniversityBeijing China;</p> <p>National Research CouncilWater Research Institute (IRSA‐CNR)Rome Italy;</p> <p>University of Chinese Academy of SciencesBeijing China;</p> <p>CAS Center for Excellence in Tibetan Plateau Earth SciencesBeijing China;</p> <p>National Research CouncilWater Research Institute (IRSA‐CNR)Brugherio Italy;</p> <p>National Research CouncilWater Research Institute (IRSA‐CNR)Brugherio Italy;</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=elevation dependence&option=203" rel="nofollow">elevation dependence;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=seasonal variation&option=203" rel="nofollow">seasonal variation;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=temperature and humidity lapse rate&option=203" rel="nofollow">temperature and humidity lapse rate;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=cloud–radiation interaction&option=203" rel="nofollow">cloud–radiation interaction;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=summer monsoon&option=203" rel="nofollow">summer monsoon;</a> </p> <div class="translation"> 机译：提升依赖;季节性变化;温度和湿度流逝速率;云辐射相互作用;夏季季风; 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