The 10–30‐day oscillation of winter rainfall in southern China and its relationship with circulation patterns in different latitudes

Yao Suxiang; Tong Qiaoyu; Li Tim; Gong Kejian

摘要

Abstract >Intraseasonal oscillation (ISO) of winter rainfall in southern China and its relationship with the circulation patterns in different latitudes are investigated using ERA‐Interim reanalysis data and observations. The results show that the rainfall in southern China has obvious ISO characteristics, with a dominant period of 10–30?days. The convergence of the whole layer integral water vapour flux can satisfactorily represent the rainfall rate, and the intraseasonal (10–30‐day filtered) rainfall is converted into a function of different time scale wind and water vapour. At the intraseasonal time scale, rainfall (10–30‐day filtered) is determined by both the 10–30‐day wind and the background (greater than 30?days) moisture. Nine days before the peak day of the intraseasonal rainfall in southern China, there is an abnormal low‐pressure system (10–30‐day filtered) in the polar region (east to Novaya Zemlya), and the low‐pressure system gradually strengthens because of the intraseasonal relative vorticity advection at high levels. The intraseasonal relative vorticity advection guides the intraseasonal geopotential anomaly to move from the high latitude to the low latitude, and the low‐pressure system at the surface also moves southward. There is no intraseasonal precipitation until the low‐pressure system at the surface moves to the region near southern China, because there is little water vapour in northern China and ample water vapour in the south. After the occurrence of precipitation, the vorticity advection from the high latitude no longer affects the strength of the low‐pressure system, but the intraseasonal diabatic heating accompanied by precipitation causes a second drop in pressure from ?3?days to ?1 day and makes the low‐pressure system strongest here. In addition, the geopotential anomaly (10–30‐day filtered) in low latitudes moves eastward along the southern foothills of the Tibetan plateau, which can guide the low‐pressure system to move southward until it reaches southern China. </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> <P>中国南部冬季降雨的季节性振荡（ISO）及其与不同纬度的循环模式的关系进行了使用时代再分析数据和观察。结果表明，中国南方的降雨具有明显的ISO特征，主导地位为10-30日。整层整体水蒸气通量的收敛可以令人满意地代表降雨率，并且陷入困境（10-30天过滤）降雨转化为不同时间尺度风和水蒸气的功能。在季节性时间尺度下，降雨（10-30天过滤）由10-30天的风和背景（大于30？天）的水分决定。九天在中国南部陷入困境的季节性峰值前，在极地区域（东到Novaya Zemlya）中存在异常的低压系统（10-30天过滤），低压系统逐渐加强，因为高水平的季节性相对涡流平流。陷入困境的相对涡度平流导向从高纬度到低纬度的渗透性地形异常异常，并且表面的低压系统也向南移动。直到表面的低压系统移动到中国南部的区域，直到南方附近的地区，南部的水蒸气很少，南方水蒸气就没有水蒸气。在沉淀发生后，从高纬度的涡流平流不再影响低压系统的强度，但伴有沉淀的渗透性蛋白糖尿病加热会导致来自β3？天的第二次下降？1天，并制作这里最强的低压系统。此外，低纬度地理位置异常（10-30天过滤）沿着藏高原南麓向东移动，这可以引导低压系统向南移动，直到它到达中国南方。</ 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>2020年第6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=Yao Suxiang&option=202" target="_blank" rel="nofollow">Yao Suxiang;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Tong Qiaoyu&option=202" target="_blank" rel="nofollow">Tong Qiaoyu;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Li Tim&option=202" target="_blank" rel="nofollow">Li Tim;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Gong Kejian&option=202" target="_blank" rel="nofollow">Gong Kejian;</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>Key Laboratory of Meteorological Disaster of Ministry of Education/Joint International Research Laboratory of Climate and Environment Change/Collaborative Innovation Center on Forecast and Evaluation of Meteorological DisastersNanjing University of Inform;</p> <p>Key Laboratory of Meteorological Disaster of Ministry of Education/Joint International Research Laboratory of Climate and Environment Change/Collaborative Innovation Center on Forecast and Evaluation of Meteorological DisastersNanjing University of Inform;</p> <p>International Pacific Research Center and Department of Atmospheric SciencesUniversity of Hawaii at ManoaHonolulu Hawaii;</p> <p>Observation office of Meteorology Observatory of Ningxia Civil Aviation ATCNingxia China;</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=10–30‐day oscillation&option=203" rel="nofollow">10–30‐day oscillation;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=circulation in different latitudes&option=203" rel="nofollow">circulation in different latitudes;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=diabatic heating&option=203" rel="nofollow">diabatic heating;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=relative vorticity advection&option=203" rel="nofollow">relative vorticity advection;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=winter rainfall&option=203" rel="nofollow">winter rainfall;</a> </p> <div class="translation"> 机译：10-30天振荡;不同纬度的循环;糖尿病加热;相对涡度平流;冬季降雨; </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/0704023002577.html">The 10–30‐day oscillation of winter rainfall in southern China and its relationship with circulation patterns in different latitudes</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Yao Suxiang&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Yao Suxiang,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Tong 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tuijian_authcolor">,巩远发</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=邓锐捷&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,邓锐捷</a> <span> <a href="/journal-cn-4784/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 大气科学 </a> </span> <span> . 2016</span><span>,第004期</span> </span> </div> </li> <li> <div> <b>5. </b><a class="enjiyixqcontent" href="/academic-journal-cn_journal-meteorological-sciences_thesis/0201254096927.html">北半球冬季中纬度位势高度场的季节内振荡</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=姚素香&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 姚素香</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=龚克坚&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,龚克坚</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=赵琛&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,赵琛</a> <span> <a href="/journal-cn-5002/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 气象科学 </a> </span> <span> . 2016</span><span>,第005期</span> </span> </div> </li> <li> <div> <b>6. </b><a class="enjiyixqcontent" href="/academic-conference-cn_meeting-40539_thesis/020222449730.html">2016年夏季河北降水与10-30天低频振荡的关系</a> <b>[C]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=韩世茹&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 韩世茹</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=史印山&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,史印山</a> <span> <a href="/conference-cn-40539/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 第34届中国气象学会年会 </a> <span> <span> . 2017</span> </span> </div> </li> <li> <div> <b>7. </b><a class="enjiyixqcontent" href="/academic-degree-domestic_mphd_thesis/020313101975.html">中国冬季地面气温10-30天低频变化及其与乌拉尔山环流和低纬度地区对流的关系</a> <b>[A] </b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=张文正&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 张文正</a> <span> . 2017</span> </span> </div> </li> </ul> <ul style="display: none;"> <li> <div> <b>1. </b><a class="enjiyixqcontent" href="/patent-detail/06130436086785.html">Composition priority for mucosal and oral administration containing HCG fragments This application was filed with EP03076028.4 filed with the European Patent Office (EPO) on April 8, 2003 and with EPO on April 8, 2003 EP03076029.2, EP03076027.6 filed with EPO on April 8, 2003, EP03076026.8 filed with EPO on April 8, 2003, EP03076022.7 filed with EPO on April 8, 2003, US10 / 409,671, EP03076021.9 filed with EPO on April 8, 2003, EP0307625.0 filed with EPO on April 8, 2003, EP03076024.3 filed with EPO on April 8, 2003, EP 03076030.0, 200, filed with EPO on April 8, 2003 April 8 days EP03076023.5 filed to the EPO, the claims CN03131227.6 priority of which was filed on China Patent Office on April 30, 2003.</a> <b>[P]</b> . <span> 外国专利：  JP2007525426A </span> <span> . 2007-09-06</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：含有HCG片段的粘膜和口服给药的组合物优先权本申请与2003年4月8日向欧洲专利局（EPO）提交的EP03076028.4以及2003年4月8日向EPO提交的EP03076029.2，EP03076027.6一起提交在2003年4月8日向EPO提交了EP03076026.8，在2003年4月8日向EPO提交了EP03076022.7，在2003年4月8日向EPO提交了US10 / 409,671，EP03076021.9，向EPPO提交了于2003年4月8日向欧洲专利局提交，EP03076024.3与2003年4月8日向欧洲专利局提交，EP 03076030.0，200，于2003年4月8日向欧洲专利局提交，EP03076023.5向欧洲专利局提交，要求CN03131227.6优先权其中已于2003年4月30日提交中国专利局。 </span> </p> </li> <li> <div> <b>2. </b><a class="enjiyixqcontent" href="/patent-detail/06130444439996.html">Method for packing powder-form or granular material particularly in a bag with capacity of 50 kg to 4000 kg involves bag having permeability to water vapor from 0.1 to 10 g/m2/day and a permeability to oxygen of 0.05 to 30 cc/m2/day</a> <b>[P]</b> . <span> 外国专利：  ES2186486A1 </span> <span> . 2003-05-01</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：特别是将粉末状或粒状材料包装在容量为50kg至4000kg的袋中的方法涉及具有0.1至10g / m 2 /天的水蒸气渗透性和0.05至30cc / m 2的氧渗透性的袋。天 </span> </p> </li> <li> <div> <b>3. </b><a class="enjiyixqcontent" href="/patent-detail/06130446760826.html">Method for packing powder-form or granular material particularly in a bag with capacity of 50 kg to 4000 kg involves bag having permeability to water vapor from 0.1 to 10 g/m2/day and a permeability to oxygen of 0.05 to 30 cc/m2/day</a> <b>[P]</b> . <span> 外国专利：  NL1016180C2 </span> <span> . 2002-03-15</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：特别是将粉末状或粒状材料包装在容量为50kg至4000kg的袋中的方法涉及具有0.1至10g / m 2 /天的水蒸气渗透性和0.05至30cc / m 2的氧渗透性的袋。天 </span> </p> </li> </ul> </div> </div> </div> <div class="theme cardcommon" style="overflow: auto;display:none"> <h3 class="all_title" id="enpatent55">相关主题</h3> <ul id="subject"> </ul> </div> </div> </div> </div> <div class="right rightcon"> <div class="details_img cardcommon clearfix" style="margin-bottom: 10px;display:none;" > </div> </div> </div> <div id="thesis_get_original1" class="downloadBth" style="bottom: 19px;z-index: 999;" onclick="ywcd('0704023002577','4',7,2,1,'',this,24)" class="delivery" prompt="010401" title="通过人工服务将文献原文发送至邮箱" >获取原文</div> <div class="journalsub-pop-up" style="display: none"> <div class="journal-sub"> <h2>期刊订阅</h2> <img src="https://cdn.zhangqiaokeyan.com/img/loginclose.png" alt="关闭" onclick="$('.journalsub-pop-up').hide()"> <p class="pardon">抱歉，该期刊暂不可订阅，敬请期待！</p> <p 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