ENSO influence on the interannual variability of the Red Sea convergence zone and associated rainfall

Dasari Hari Prasad; Langodan Sabique; Viswanadhapalli Yesubabu; Vadlamudi Brahmananda R.; Papadopoulos Vassilis P.; Hoteit Ibrahim

摘要

ABSTRACT >The Red Sea convergence zone (RSCZ) is formed by opposite surface winds blowing from northwest to southeast directions at around 18°–19°N between October and January. A reverse‐oriented, low‐level monsoon trough at 850?hPa, known as the Red Sea trough (RST), transfers moisture from the southern Red Sea to RSCZ. The positions of the RSCZ and RST and the intensity of the RST have been identified as important factors in modulating weather and climatic conditions across the Middle East. Here, we investigate the influence of the El Ni?o southern oscillation (ENSO) on the interannual variability of RSCZ, RST, and regional rainfall during winter months. Our results indicate that El Ni?o (warm ENSO phase) favours a shift of the RSCZ to the north and a strengthening of the RST in the same direction. Conversely, during November and December of La Ni?a periods (cold ENSO phase), the RSCZ shift to the south and the RST strengthens in the same direction. During El Ni?o periods, southeasterly wind speeds increase (20–30%) over the southern Red Sea and northwesterly wind speeds decrease (10–15%) over the northern Red Sea. Noticeable increases in the number of rainy days and the intensity of rain events are observed during El Ni?o phases. These increases are associated with colder than normal air intrusion at lower levels from the north combined with warm air intrusion from the south over the RSCZ. Our analysis suggests that during El Ni?o winters, warmer sea surface temperatures and higher convective instability over the Red Sea favour local storms conditions and increase rainfall over the Red Sea and adjoining regions. </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> >红海汇聚区（RSCZ）是由十月和一月之间从西北到东南方向吹到东南方向的相反表面风形成。逆向低水平的季风槽，在850？HPA，称为红海槽（RST），将南红海的水分转移到RSCZ。 RSCZ和RST的位置和RST的强度被确定为调节中东天气和气候条件的重要因素。在这里，我们调查EL NI？O Southern振荡（ENSO）对冬季RSCZ，RST和区域降雨的年性变异性的影响。我们的结果表明EL NI？O（温暖的ENSO阶段）有利于RSCZ向北方的偏移，并在同一方向上加强RST。相反，在11月和12月的La Ni？一个时期（冷恩索阶段），RSCZ向南转移，RST在同一方向上加强。在El Ni？O期间，东南风速增加（20-30％）在南方红海和北方红海上的西北风速减少（10-15％）。在EL Ni阶段期间观察到雨天数量和雨季事件的强度显着增加。这些增加与北方较低水平的正常空气侵入与北方的较低水平相结合，与南部的南部的温暖空气侵入。我们的分析表明，在EL NI？O冬季，较温暖的海面温度和红海上更高的对流不稳定性，有利于当地风暴条件，并增加红海和毗邻的地区。</ 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15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=Dasari Hari Prasad&option=202" target="_blank" rel="nofollow">Dasari Hari Prasad;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Langodan Sabique&option=202" target="_blank" rel="nofollow">Langodan Sabique;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Viswanadhapalli Yesubabu&option=202" target="_blank" rel="nofollow">Viswanadhapalli Yesubabu;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Vadlamudi Brahmananda R.&option=202" target="_blank" rel="nofollow">Vadlamudi Brahmananda R.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Papadopoulos Vassilis P.&option=202" target="_blank" rel="nofollow">Papadopoulos Vassilis P.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Hoteit Ibrahim&option=202" target="_blank" rel="nofollow">Hoteit Ibrahim;</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>Physical Sciences and Engineering DivisionKing Abdullah University of Science and Technology (KAUST)Thuwal Saudi Arabia;</p> <p>Physical Sciences and Engineering DivisionKing Abdullah University of Science and Technology (KAUST)Thuwal Saudi Arabia;</p> <p>Weather and Climate Research GroupNational Atmospheric Research LaboratoryTirupati Andhra Pradesh India;</p> <p>Centro de Previs?o de Tempo e Estudos Climáticos (CPTECH)Instituto Nacional de Pesquisas EspaciaisSao Jose dos Campos Brazil;</p> <p>Marine Research CenterHellenic Centre for Marine ResearchAnavyssos Greece;</p> <p>Physical Sciences and Engineering DivisionKing Abdullah University of Science and Technology (KAUST)Thuwal Saudi Arabia;</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=Red Sea convergence zone&option=203" rel="nofollow">Red Sea convergence zone;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Red Sea trough&option=203" rel="nofollow">Red Sea trough;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=ENSO&option=203" rel="nofollow">ENSO;</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=moisture convergence&option=203" rel="nofollow">moisture convergence;</a> </p> <div class="translation"> 机译：红海收敛区;红海槽;enso;降雨;水分收敛; </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/0704023003077.html">ENSO influence on the interannual variability of the Red Sea convergence zone and associated rainfall</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Dasari Hari Prasad&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Dasari Hari Prasad,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Langodan Sabique&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Langodan Sabique,</a> <a 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