Hourly station‐based precipitation characteristics over the Tibetan Plateau

Li Jian

摘要

ABSTRACT >Based on precipitation data collected from 100 surface stations on the Tibetan Plateau, the summer climatology of the hourly characteristics of precipitation events, including hourly frequency and intensity, frequency–intensity structure, diurnal circle, and duration, was comprehensively analysed. Both hourly frequency and intensity are high (low) over the southeastern (western and northern) plateau. In the Yurlung Zangbo River valley, which is located on the central southern plateau, the precipitation frequency is low and the intensity is high. The proportion of strong (weak) precipitation, in terms of frequency, is relatively large (small) in this valley, and similar features with respect to the frequency–intensity structure were also found for the northeastern plateau. In contrast, precipitation over the southern edge of the plateau is characterized by high frequency and low intensity, and the percentage of weak precipitation hours is higher than in other regions. Most stations over the plateau exhibit precipitation peaks either in late afternoon or around midnight. The late afternoon (midnight) peak is mainly contributed to by precipitation events that are short (long) in duration. These ‘short‐afternoon’ and long‐nighttime' types constitute the two major modes of precipitation over the plateau. Extreme events tend to begin in late afternoon, reach a maximum around midnight, and stop in the morning. The possible mechanisms are discussed. The quantity of available water vapour determines the geographical distribution of precipitation frequency through modulating the duration of precipitation events. High‐intensity events are related to well‐organized convective systems. The ratio of short‐afternoon and long‐nighttime precipitation is significantly influenced by local topography. </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> >基于从100个表面站收集的降水数据在藏高原上，全面分析了沉淀事件的每小时特征的夏季气候学，包括每小时频率和强度，频率强度结构，昼夜圆圈和持续时间。在东南部（西部和北部）高原上的每小时频率和强度都很高（低）。在位于南高原中央南高原的Yurlung Zangbo河谷，降水频率低，强度高。在该谷的频率方面，强（弱）降水的比例在该谷比较大（小），以及东北高原的频率强度结构相对于频率强度结构的相似特征。相比之下，高原南部边缘的沉淀特征在于高频和低强度，弱沉淀小时率高于其他地区。大多数高原上的车站在下午晚些时候或午夜左右表现出沉淀峰。下午晚期（午夜）峰值主要是通过持续时间短（长）的降水事件。这些“短期”和长夜间的类型构成了高原的两种主要降水模式。极端事件倾向于在下午晚些时候开始，午夜左右达到最大值，并在早上停下来。讨论了可能的机制。可用水蒸气的数量通过调节降水事件的持续时间来确定降水频率的地理分布。高强度事件与良好组织的对流系统有关。短午后和长夜间降水的比例受到当地地形的显着影响。</ 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3期</span><b style="margin: 0 2px;">|</b><span>共11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=Li Jian&option=202" target="_blank" rel="nofollow">Li Jian;</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>LaSW Chinese Academy of Meteorological SciencesChina Meteorological AdministrationBeijing 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=precipitation&option=203" rel="nofollow">precipitation;</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=duration&option=203" rel="nofollow">duration;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Tibetan Plateau&option=203" rel="nofollow">Tibetan Plateau;</a> </p> <div class="translation"> 机译：降水;昼夜周期;持续时间;藏高原; 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communications network, a base station and a network</a> <b>[P]</b> . <span> 外国专利：  US2008039142A1 </span> <span> . 2008-02-14</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：用于确定无线通信网络中的基站中的天线路径的特性的方法，基站和网络 </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('0704023002967','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 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