Heterogeneous water storage and thermal regime of supraglacial ponds on debris‐covered glaciers

Watson Cameron Scott; Quincey Duncan J.; Carrivick Jonathan L.; Smith Mark W.; Rowan Ann V.; Richardson Robert

摘要

Abstract > The water storage and energy transfer roles of supraglacial ponds are poorly constrained, yet they are thought to be important components of debris‐covered glacier ablation budgets. We used an unmanned surface vessel (USV) to collect sonar depth measurements for 24 ponds to derive the first empirical relationship between their area and volume applicable to the size distribution of ponds commonly encountered on debris‐covered glaciers. Additionally, we instrumented nine ponds with thermistors and three with pressure transducers, characterizing their thermal regime and capturing three pond drainage events. The deepest and most irregularly‐shaped ponds were those associated with ice cliffs, which were connected to the surface or englacial hydrology network (maximum depth?=?45.6?m), whereas hydrologically‐isolated ponds without ice cliffs were both more circular and shallower (maximum depth?=?9.9?m). The englacial drainage of three ponds had the potential to melt ~100?±?20?×?10 3 ?kg to ~470?±?90?×?10 3 ?kg of glacier ice owing to the large volumes of stored water. Our observations of seasonal pond growth and drainage with their associated calculations of stored thermal energy have implications for glacier ice flow, the progressive enlargement and sudden collapse of englacial conduits, and the location of glacier ablation hot‐spots where ponds and ice cliffs interact. Additionally, the evolutionary trajectory of these ponds controls large proglacial lake formation in deglaciating environments. Copyright ? 2017 John Wiley & Sons, Ltd. </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”> <标题类型=“main”>抽象</ title> >水超透池塘的储存和能量转移角色受到严重限制，但他们被认为是杂物覆盖的冰川消融预算的重要组成部分。我们使用无人面的表面船（USV）来收集24个池塘的声纳深度测量，以获得适用于杂草覆盖冰川常见的池塘尺寸分布的地区和体积之间的第一个实证关系。此外，我们用热敏电阻和三个带有压力传感器的九个池塘，表征了它们的热调节和捕获三个池塘排水事件。最深层和最不规则的池塘是与冰峭壁相关的池塘，它们连接到表面或enjlacial水文网络（最大深度？=Δ=45.6μm），而没有冰峭壁的水文隔离的池塘既有圆形和浅薄（最大深度？=？9.9？m）。三个池塘的闭口排水有熔化〜100？±20？×10 3 </ sup> kg至〜470？±90？×10 3 </ sup>由于储水量大量的储存而冰川冰。我们对季节性池塘生长和排水的观察，其相关的储存热能计算对冰川冰流量有影响，展会扩大和脑卒中的突然塌陷以及冰川消融热点的位置，其中池塘和冰峭壁相互作用。另外，这些池塘的进化轨迹控制了拆分环境中的大型Proglacial湖泊形成。版权？ 2017年John Wiley＆amp; SONS，LTD。</ p> </ abstract> </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-22319/'>《Earth Surface Processes and Landforms: The journal of the British Geomorphological Research Group》</a> <b style="margin: 0 2px;">|</b><span>2018年第1期</span><b style="margin: 0 2px;">|</b><span>共13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=Watson Cameron Scott&option=202" target="_blank" rel="nofollow">Watson Cameron Scott;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Quincey Duncan J.&option=202" target="_blank" rel="nofollow">Quincey Duncan J.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Carrivick Jonathan L.&option=202" target="_blank" rel="nofollow">Carrivick Jonathan L.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Smith Mark W.&option=202" target="_blank" rel="nofollow">Smith Mark W.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Rowan Ann V.&option=202" target="_blank" rel="nofollow">Rowan Ann V.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Richardson Robert&option=202" target="_blank" rel="nofollow">Richardson Robert;</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>School of Geography and Water @ leedsUniversity of LeedsLeeds UK;</p> <p>School of Geography and Water @ leedsUniversity of LeedsLeeds UK;</p> <p>School of Geography and Water @ leedsUniversity of LeedsLeeds UK;</p> <p>School of Geography and Water @ leedsUniversity of LeedsLeeds UK;</p> <p>Department of GeographyUniversity of SheffieldSheffield UK;</p> <p>School of Mechanical EngineeringUniversity of LeedsLeeds UK;</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=bathymetry&option=203" rel="nofollow">bathymetry;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=debris‐covered glaciers&option=203" rel="nofollow">debris‐covered glaciers;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=ice cliffs&option=203" rel="nofollow">ice cliffs;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=glacial lake&option=203" rel="nofollow">glacial lake;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=supraglacial ponds&option=203" rel="nofollow">supraglacial ponds;</a> </p> <div class="translation"> 机译：沐浴覆盖冰川;冰峭壁;冰川湖;超限池塘; 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