Radar‐based summer precipitation climatology of the Czech Republic

Bli?ňák Vojtěch; Ka?par Marek; Müller Miloslav

摘要

ABSTRACT >To assess the climatology of the Czech Republic (CR) with a high spatial (1?km) resolution, this study uses radar‐based precipitation data collected over the summer seasons of a 10‐year period (2002–2011). Radar reflectivity data were obtained from two C‐band Doppler weather radars, integrated in time and merged with daily precipitation totals from rain gauge measurements. Using radar measurements, daily adjusted precipitation totals were later divided into 10‐min precipitation totals that were continuously accumulated in a series of time windows ranging from 30?min to 24?h. This climatological analysis confirms that altitude substantially influences not only the spatial distribution of mean precipitation but also the spatial distribution of precipitation maxima as well as the diurnal cycle of precipitation in the CR. While the 24‐h totals are generally maximal in mountains, mean and absolute seasonal maxima of short‐term totals (up to 1 and 6?h, respectively) are detected in altitudes between 300 and 600?m a.s.l. Regarding the diurnal cycle, maximum frequency of precipitation occurs 2?h earlier in the mountains, whereas mean totals remain at the same level until 2100 UTC. The mean time during which precipitation maxima occur generally does not change with altitude. Nevertheless, a detailed regional study demonstrates that short‐term precipitation maxima usually start earlier in the afternoon in and around mountainous regions. Long‐term (mainly 6‐h) precipitation maxima occur later than short ones but are substantially less concentrated in time, especially in the mountains. These differences between mountains and lowlands can be explained by smaller relative proportions and earlier onset of convective precipitation in mountains. </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> >评估捷克共和国的气候学（ CR）具有高空间（1 km）的分辨率，本研究采用了在10年期间（2002-2011）的夏季收集的基于雷达的降水数据。雷达反射率数据是从两个C波段多普勒天气雷达获得的，纳入时间，并与雨量计测量的日降水总量合并。使用雷达测量，每日调整后的降水量稍后分为10分钟的降水总量，该总计连续累积在30？min到24？h的一系列窗口中。这种气候学分析证实，高度不仅影响了平均沉淀的空间分布，而且对沉淀最大值的空间分布以及Cr中的沉淀的昼夜循环的空间分布。虽然24-H总量通常在山中最大，但短期总计的平均值和绝对季节性最大值（分别为1和6Ωh）在300到600℃的高度之间被检测到。关于昼夜循环，山上早些时候的沉淀的最大频率发生了2？H，而平均总数仍然在同一水平，直到2100 UTC。降水最大值的平均时间通常不会随高度而改变。然而，详细的区域研究表明，短期降水最大值通常在山区和周围地区的下午早些时候开始。长期（主要是6-h）降水最大值比短，但在时间上显着较小，特别是在山上。山脉和低地之间的这些差异可以通过较小的相对比例和早期的山脉对流沉淀发作来解释。</ 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=Bli?ňák Vojtěch&option=202" target="_blank" rel="nofollow">Bli?ňák Vojtěch;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Ka?par Marek&option=202" target="_blank" rel="nofollow">Ka?par Marek;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Müller Miloslav&option=202" target="_blank" rel="nofollow">Müller Miloslav;</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>Department of MeterorologyInstitute of Atmospheric Physics CASPrague Czech Republic;</p> <p>Department of MeterorologyInstitute of Atmospheric Physics CASPrague Czech Republic;</p> <p>Department of MeterorologyInstitute of Atmospheric Physics CASPrague Czech Republic;</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=weather radar&option=203" rel="nofollow">weather radar;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=rain gauges&option=203" rel="nofollow">rain gauges;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=adjustment&option=203" rel="nofollow">adjustment;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=precipitation climatology&option=203" rel="nofollow">precipitation climatology;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Czech Republic&option=203" rel="nofollow">Czech Republic;</a> </p> <div class="translation"> 机译：天气雷达;雨量仪;调整;降水气候;捷克共和国; </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/0704023003079.html">Radar‐based summer precipitation climatology of the Czech Republic</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Bli?ňák Vojtěch&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Bli?ňák Vojtěch,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Ka?par Marek&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Ka?par Marek,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Müller Miloslav&option=202" target="_blank" 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