{"id":3050,"date":"2018-03-16T12:25:03","date_gmt":"2018-03-16T11:25:03","guid":{"rendered":"https:\/\/www.essl.org\/cms\/?p=3050"},"modified":"2018-03-20T15:19:33","modified_gmt":"2018-03-20T14:19:33","slug":"more-european-hail-and-lightning-according-to-new-statistical-method","status":"publish","type":"post","link":"https:\/\/www.essl.org\/cms\/more-european-hail-and-lightning-according-to-new-statistical-method\/","title":{"rendered":"New statistical method shows increases in European hail and lightning"},"content":{"rendered":"<p>Researchers at ESSL, Munich Re, the Ludwig-Maximilians University Munich (LMU) and the German Aerospace Centre DLR have developed a new statistical method to investigate trends in thunderstorm and severe weather activity. Anja R\u00e4dler, the main developer of this method, called AR-CHaMo, will defend her Ph.D. thesis on this topic at LMU.<\/p>\n<p>Anja R\u00e4dler says: &#8220;the strength of our approach is that we are now able to assess changes in severe weather frequency using climate models that are themselves too coarse to simulate each and every thunderstorm&#8221;. To do this, the probability of lightning and severe weather is determined as a function of parameters such as instability, moisture and wind shear, using severe weather observations from ESSL&#8217;s <a href=\"https:\/\/www.eswd.eu\">European Severe Weather Database<\/a>.<\/p>\n<div id=\"attachment_3051\" style=\"width: 762px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/www.essl.org\/cms\/wp-content\/uploads\/hail_now_map.png\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-3051\" class=\"wp-image-3051 size-full\" src=\"https:\/\/www.essl.org\/cms\/wp-content\/uploads\/hail_now_map.png\" alt=\"Annual number of 6-hourly periods with hail of 2 cm or larger in Europe (1979 - 2016), modelled using AR-CHaMo. From: R\u00e4dler et al, 2018.\" width=\"752\" height=\"501\" srcset=\"https:\/\/www.essl.org\/cms\/wp-content\/uploads\/hail_now_map.png 752w, https:\/\/www.essl.org\/cms\/wp-content\/uploads\/hail_now_map-300x200.png 300w, https:\/\/www.essl.org\/cms\/wp-content\/uploads\/hail_now_map-450x300.png 450w\" sizes=\"auto, (max-width: 752px) 100vw, 752px\" \/><\/a><p id=\"caption-attachment-3051\" class=\"wp-caption-text\">Annual number of 6-hourly periods with hail of 2 cm or larger in Europe (1979 &#8211; 2016), modelled using AR-CHaMo. <a href=\"https:\/\/journals.ametsoc.org\/doi\/10.1175\/JAMC-D-17-0132.1\">From: R\u00e4dler et al, 2018<\/a>.<\/p><\/div>\n<p>In a new <a href=\"https:\/\/journals.ametsoc.org\/doi\/10.1175\/JAMC-D-17-0132.1\">article in the Journal of Applied Meteorology and Climatology<\/a>, the development of AR-CHaMo is explained in detail, and trends of lightning and severe weather frequency since 1979 are presented. The basis of these projections are a numerical model (ERA-Interim), that simulates the past weather since 1979. The annual average predicted number of large hail events (see map below) conforms quite well to what we know: the Alpine forelands are the Europe&#8217;s hailfall hotbed.<\/p>\n<p>The number of simulated hail events was not constant during the last three decades. When considering hail activity over Central Europe, significant increases are detected.<\/p>\n<div id=\"attachment_3053\" style=\"width: 778px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/www.essl.org\/cms\/wp-content\/uploads\/hail_trend_timeseries.png\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-3053\" class=\"wp-image-3053 size-full\" src=\"https:\/\/www.essl.org\/cms\/wp-content\/uploads\/hail_trend_timeseries.png\" alt=\"Simulated number of 6-hourly periods with hail &gt; 2 cm across Germany and the Alps (blue) and Western and Central Europe (green), 1979-2016.\" width=\"768\" height=\"502\" srcset=\"https:\/\/www.essl.org\/cms\/wp-content\/uploads\/hail_trend_timeseries.png 768w, https:\/\/www.essl.org\/cms\/wp-content\/uploads\/hail_trend_timeseries-300x196.png 300w, https:\/\/www.essl.org\/cms\/wp-content\/uploads\/hail_trend_timeseries-459x300.png 459w\" sizes=\"auto, (max-width: 768px) 100vw, 768px\" \/><\/a><p id=\"caption-attachment-3053\" class=\"wp-caption-text\">Simulated number of 6-hourly periods with hail &gt; 2 cm across Germany and the Alps (blue) and Western and Central Europe (green), 1979-2016. From: <a href=\"https:\/\/journals.ametsoc.org\/doi\/10.1175\/JAMC-D-17-0132.1\">R\u00e4dler et al, 2018<\/a>.<\/p><\/div>\n<p>Of course, it is of interest to know what the reason for the increase is. Anja R\u00e4dler: &#8220;we found that the driving factor is the increasing humidity close to the earth&#8217;s surface. This is something we expect to happen when temperatures increase, because warmer air can contain more moisture.&#8221; Indeed, temperature has increased since 1979, at least partly, because of the rising CO2 content of the atmosphere.<\/p>\n<p>The map below shows which areas have seen the strongest increase, according to ERA-Interim and the AR-CHaMo model.<\/p>\n<div id=\"attachment_3052\" style=\"width: 896px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/www.essl.org\/cms\/wp-content\/uploads\/hail_trend.png\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-3052\" class=\"size-full wp-image-3052\" src=\"https:\/\/www.essl.org\/cms\/wp-content\/uploads\/hail_trend.png\" alt=\"Trend of number of 6-hourly periods with severe hail (1979-2016). Dots denote where a ignificant trend was found.\" width=\"886\" height=\"538\" srcset=\"https:\/\/www.essl.org\/cms\/wp-content\/uploads\/hail_trend.png 886w, https:\/\/www.essl.org\/cms\/wp-content\/uploads\/hail_trend-300x182.png 300w, https:\/\/www.essl.org\/cms\/wp-content\/uploads\/hail_trend-768x466.png 768w, https:\/\/www.essl.org\/cms\/wp-content\/uploads\/hail_trend-494x300.png 494w\" sizes=\"auto, (max-width: 886px) 100vw, 886px\" \/><\/a><p id=\"caption-attachment-3052\" class=\"wp-caption-text\">Trend of number of 6-hourly periods with severe hail of 2cm or larger (1979-2016). Dots denote where a ignificant trend was found. From: <a href=\"https:\/\/journals.ametsoc.org\/doi\/10.1175\/JAMC-D-17-0132.1\">R\u00e4dler et al, 2018<\/a>.<\/p><\/div>\n<p>The next question Anja and her team will address is what will happen in the future. First results that were <a href=\"https:\/\/journals.ametsoc.org\/doi\/10.1175\/MWR-D-15-0104.1\">published by the ESSL team in 2017<\/a> suggest that the moisture increase will continue and create more situations favorable for severe thunderstorms during the 21st century. Using the new AR-CHaMo method, the team will soon be able to give an estimate of how much more hail, tornadoes, severe winds and lightning we should count on in different climate change scenarios.<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Researchers at ESSL, Munich Re, the Ludwig-Maximilians University Munich (LMU) and the German Aerospace Centre DLR have developed a new statistical method to investigate trends in thunderstorm and severe weather activity. Anja R\u00e4dler, the main developer of this method, called &hellip; <a href=\"https:\/\/www.essl.org\/cms\/more-european-hail-and-lightning-according-to-new-statistical-method\/\">Continue reading <span class=\"meta-nav\">&rarr;<\/span><\/a><\/p>\n","protected":false},"author":5,"featured_media":0,"comment_status":"closed","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[7],"tags":[],"class_list":["post-3050","post","type-post","status-publish","format-standard","hentry","category-news"],"_links":{"self":[{"href":"https:\/\/www.essl.org\/cms\/wp-json\/wp\/v2\/posts\/3050","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/www.essl.org\/cms\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/www.essl.org\/cms\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/www.essl.org\/cms\/wp-json\/wp\/v2\/users\/5"}],"replies":[{"embeddable":true,"href":"https:\/\/www.essl.org\/cms\/wp-json\/wp\/v2\/comments?post=3050"}],"version-history":[{"count":6,"href":"https:\/\/www.essl.org\/cms\/wp-json\/wp\/v2\/posts\/3050\/revisions"}],"predecessor-version":[{"id":3061,"href":"https:\/\/www.essl.org\/cms\/wp-json\/wp\/v2\/posts\/3050\/revisions\/3061"}],"wp:attachment":[{"href":"https:\/\/www.essl.org\/cms\/wp-json\/wp\/v2\/media?parent=3050"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.essl.org\/cms\/wp-json\/wp\/v2\/categories?post=3050"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.essl.org\/cms\/wp-json\/wp\/v2\/tags?post=3050"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}