Local‐Scale Advection of Sensible and Latent Heat During Snowmelt

Harder Phillip; Pomeroy John W.; Helgason Warren

摘要

Abstract >The breakup of snow cover into patches during snowmelt leads to a dynamic, heterogeneous land surface composed of melting snow, and wet and dry soil and plant surfaces. Energy exchange with the atmosphere is therefore complicated by horizontal gradients in surface temperature and humidity as snow surface temperature and humidity are regulated by the phase change of melting snow unlike snow‐free areas. Airflow across these surface transitions results in local‐scale advection of energy that has been documented as sensible heat during snowmelt, while latent heat advection has received scant attention. Herein, results are presented from an experiment measuring near‐surface profiles of air temperature and humidity across snow‐free to snow‐covered transitions that demonstrates that latent heat advection can be the same order of magnitude as sensible heat advection and is therefore an important source of snowmelt energy. Latent heat advection is conditional on an upwind source of water vapor from a wetted snow‐free surface. </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 Type =“Main”XML：Lang =“en”> <标题类型=“main”>抽象</ title> >在雪花期间将雪覆盖的分解导致动态，异构的土地表面组成熔化雪，湿土和植物表面。因此，随着暖雪的相变与无雪区，散热和湿度的水平梯度，表面温度和湿度的水平梯度是通过水平梯度的能量交换。这些表面过渡的气流导致局部规模的能量平流，这些能量被记录在雪花期间被记录为明智的热量，而潜在的热情平流受到了很少的关注。在此，从测量空气温度和湿度的近表面谱的实验中提出了对雪覆盖的过渡的实验中提出的，这表明潜在的热线平流可以与明智的热平流相同，因此是一个重要的来源雪花能量。潜热平流是在湿润的无雪表面上升压水蒸气源的条件。</ 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-23539/'>《Geophysical Research Letters》</a> <b style="margin: 0 2px;">|</b><span>2017年第19期</span><b style="margin: 0 2px;">|</b><span>共9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=Harder Phillip&option=202" target="_blank" rel="nofollow">Harder Phillip;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Pomeroy John W.&option=202" target="_blank" rel="nofollow">Pomeroy John W.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Helgason Warren&option=202" target="_blank" rel="nofollow">Helgason Warren;</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>Centre for HydrologyUniversity of SaskatchewanSaskatoon Saskatchewan Canada;</p> <p>Centre for HydrologyUniversity of SaskatchewanSaskatoon Saskatchewan Canada;</p> <p>Centre for HydrologyUniversity of SaskatchewanSaskatoon Saskatchewan Canada;</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/163.html" title="地球物理学">地球物理学;</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=latent heat&option=203" rel="nofollow">latent heat;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=sensible heat&option=203" rel="nofollow">sensible heat;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=local‐scale advection&option=203" rel="nofollow">local‐scale advection;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=snowmelt&option=203" rel="nofollow">snowmelt;</a> </p> <div class="translation"> 机译：潜热;明智的热量;局部规模平流;融雪; 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