Major role of water bodies on diurnal precipitation regimes in Eastern Africa

Camberlin Pierre; Gitau Wilson; Planchon Olivier; Dubreuil Vincent; Funatsu Beatriz M.; Philippon Nathalie

摘要

ABSTRACT >Mean diurnal rainfall regimes over Eastern Africa (also referred to as the Greater Horn of Africa) are studied based on 3‐hourly data from the TRMM 3B42 data set, averaged over a 17‐year period (1998–2014). The consistency with long‐term mean raingauge data, available for partly independent periods, varies from good (Sudan, Ethiopia, Eritrea and Somalia) to very good (Kenya, Tanzania and Uganda). Over sea (Indian Ocean and Red Sea), the diurnal rainfall distribution is quite uniform; however, a morning peak dominates and there is evidence of offshore phase propagation south of the equator. Over land, both rainfall frequency and rainfall amounts show a dominant afternoon maximum (1500–1800 East African Time, i.e. GMT + 3). However, many inland regions show a delayed rainfall maximum (evening, night‐time or morning). The evening to night‐time maximum found over some land areas is associated with a phase propagation from areas showing an afternoon peak. This occurs west of high ground areas (Sudan and parts of the Great Lakes region) and in belts parallel to the seashores (Eritrea, northeastern Ethiopia, Somalia and eastern Kenya). The latter provide indirect evidence that sea breeze effects can be detected at unexpectedly great distances from the coast (up to 300–400 km) in parts of Eastern Africa. A remarkable ring of early afternoon (1500) maxima is found around most lakes, although some east–west asymmetries occur. Over the lakes, a morning or late night maximum is mostly found. It is generally inversely related to the distance to the shorelines for the larger lakes, but over the mid‐size lakes it is replaced by or competes with a late afternoon to evening maximum. </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”> <title type =“main”>抽象</ title> >东非的平均降雨制度（也根据TRMM 3B42数据集的3小时数据进行了基于3小时的数据，在17年（1998-2014）上平均进行了基于3小时的数据进行了研究。与长期平均raInauge数据的一致性可用于部分独立的时间，从好（苏丹，埃塞俄比亚，厄立特里亚和索马里）不同（肯尼亚，坦桑尼亚和乌干达）不同。海上（印度洋和红海），昼夜降雨分布相当均匀;然而，早晨的巅峰占主导地位，有证据表明赤道南部的海洋相传。在土地上，降雨频率和降雨量均显示出优势下午最多（1500-1800东非时间，即GMT + 3）。然而，许多内陆地区展示了延迟的降雨量（晚上，夜间或早晨）。在某些陆地区域发现的夜间最大值与显示下午峰值的区域的相传相关。这发生在高地区（苏丹和大湖区的一部分）和与海岸（厄立特里亚，东北埃塞俄比亚，索马里和东肯尼亚）平行的皮带中。后者提供间接证据，即海风效应在东非的部分地区的海岸（高达300-400公里）的意外距离出乎意料的距离。虽然发生了一些东西的不对称，但在大多数湖泊周围都发现了一个卓越的下午（1500）最大值的戒指。在湖泊上，大多数最大的早晨或深夜。它通常与较大湖泊的海岸线的距离相反，但在中尺寸的湖泊上，它被替换或与晚上最大的次数竞争。</ 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2期</span><b style="margin: 0 2px;">|</b><span>共17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=Camberlin Pierre&option=202" target="_blank" rel="nofollow">Camberlin Pierre;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Gitau Wilson&option=202" target="_blank" rel="nofollow">Gitau Wilson;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Planchon Olivier&option=202" target="_blank" rel="nofollow">Planchon Olivier;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Dubreuil Vincent&option=202" target="_blank" rel="nofollow">Dubreuil Vincent;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Funatsu Beatriz M.&option=202" target="_blank" rel="nofollow">Funatsu Beatriz M.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Philippon Nathalie&option=202" target="_blank" rel="nofollow">Philippon Nathalie;</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 de Recherches de Climatologie/BiogéosciencesUMR 6282 CNRS/University of Bourgogne Franche‐ComtéDijon France;</p> <p>Department of MeteorologyUniversity of NairobiKenya;</p> <p>Department of GeographyLETG Rennes COSTEL/UMR 6554 CNRS/Université Rennes 2France;</p> <p>Department of GeographyLETG Rennes COSTEL/UMR 6554 CNRS/Université Rennes 2France;</p> <p>Department of GeographyLETG Rennes COSTEL/UMR 6554 CNRS/Université Rennes 2France;</p> <p>CNRS IRD IGEUniv. Grenoble AlpesFrance;</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=Horn of Africa&option=203" rel="nofollow">Horn of Africa;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=East Africa&option=203" rel="nofollow">East Africa;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Lake Victoria&option=203" rel="nofollow">Lake Victoria;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Indian Ocean&option=203" rel="nofollow">Indian Ocean;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=rainfall&option=203" rel="nofollow">rainfall;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=diurnal cycle&option=203" rel="nofollow">diurnal cycle;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=sea breeze&option=203" rel="nofollow">sea breeze;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=lakes&option=203" rel="nofollow">lakes;</a> </p> <div class="translation"> 机译：非洲的号角;东非;维多利亚湖;印度洋;降雨;昼夜循环;海风;湖泊; </div> </li> </ul> </div> </div> <div class="literature cardcommon"> <div class="similarity "> <h3 class="all_title" id="enpatent66">相似文献</h3> <div class="similaritytab clearfix"> <ul> <li class="active" >外文文献</li> <li >中文文献</li> <li >专利</li> </ul> </div> <div class="similarity_details"> <ul > <li> <div> <b>1. </b><a class="enjiyixqcontent" href="/journal-foreign-detail/0704023003049.html">Major role of water bodies on diurnal precipitation regimes in Eastern Africa</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Camberlin Pierre&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Camberlin Pierre,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Gitau Wilson&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Gitau Wilson,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Planchon Olivier&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Planchon Olivier,</a> <a href="/journal-foreign-21026/" target="_blank" rel="nofollow" class="tuijian_authcolor">International Journal of Climatology: A Journal of the Royal Meteorological Society .</a> <span>2018</span><span>,第2期</span> </span> </div> <p class="zwjiyix translation" style="max-width: initial;height: auto;word-break: break-all;white-space: initial;text-overflow: initial;overflow: initial;"> <span>机译：水体对东非昼夜降水制度的主要作用</span> </p> </li> <li> <div> <b>2. </b><a class="enjiyixqcontent" href="/journal-foreign-detail/0704020649510.html">Intraseasonal to Interannual Modulation of Diurnal Precipitation Distribution Over Eastern Africa</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Pierre Camberlin&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Pierre Camberlin,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Wilson Gitau&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Wilson Gitau,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=George Kiladis&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">George Kiladis,</a> <a href="/journal-foreign-34649/" target="_blank" rel="nofollow" class="tuijian_authcolor">Journal of Geophysical Research, D. 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