{"id":40546,"date":"2015-12-11T12:50:27","date_gmt":"2015-12-11T11:50:27","guid":{"rendered":"https:\/\/www.sonnenseite.com\/science\/cold-hot-or-dry-persistent-weather-extremes-associated-with-decreased-storm-activity.html"},"modified":"2015-12-11T12:50:27","modified_gmt":"2015-12-11T11:50:27","slug":"cold-hot-or-dry-persistent-weather-extremes-associated-with-decreased-storm-activity","status":"publish","type":"post","link":"https:\/\/www.sonnenseite.com\/en\/science\/cold-hot-or-dry-persistent-weather-extremes-associated-with-decreased-storm-activity\/","title":{"rendered":"Cold, hot or dry: Persistent weather extremes associated with decreased storm activity"},"content":{"rendered":"<p>A decrease in storm activity over large parts of the US, Europe, Russia, and China is found to influence weather extremes &ndash; cold ones in winter, hot or dry ones in summer.<\/p>\n<p> <!--more--> <\/p>\n<p>This is now shown in a study by scientists from the Potsdam Institute  for Climate Impact Research. The observed changes in storm activity are  likely related to changes in other atmospheric dynamics like the jet  stream &ndash; strong westerly winds circling the Northern hemisphere high up  in the sky.<\/p>\n<p>&ldquo;Less or less severe storms in the mid-latitudes, this at first sight  seems to be good news &ndash; but unfortunately it isn&rsquo;t,&rdquo; says lead-author  Jascha Lehmann. &ldquo;These storms have a moderating effect on land  temperatures as they bring maritime air from the oceans to the  continents and a lack of them can thus favor extreme temperatures.&rdquo; <\/p>\n<p>  In the Northern Hemisphere mid-latitudes, much of the day-to-day  weather variability is determined by the storm track regions located  over the Atlantic and Pacific oceans. Here, weather systems, including  storms, are generated and travel eastwards to the continents. In winter,  storms bring air from the relatively warm oceans to the continents and  thus have a warming effect. In summer, the effect reverses with winds  bringing relatively cool and moist air from the sea. The authors show  that a lack of such weather systems can thus favor more persistent heat  and drought events in summer, and cold spells in winter. <\/p>\n<p> &ldquo;This  summer a severe drought in China&rsquo;s northern bread basket region  Liaoning threatened crop yields, while California has been experiencing a  prolonged drought for no less than three consecutive years,&rdquo; says  Lehmann. Comprehensive analysis of satellite weather data shows that  these are indeed regions where significant reductions in storm activity  are detected during the rainy season. In summer, storm activity calmed  down over as much as 80 percent of the land area in the mid-latitudes.  In winter the changes are more patchy, yet pronounced reductions are  found over eastern US and large parts of Europe and Asia. This includes  regions like New York and Chicago which suffered from record-breaking  cold temperatures in recent winters.<\/p>\n<p> These detected changes in  mid-latitude storm tracks are likely linked to changes in the jet stream  and planetary waves in the atmosphere. Such dynamical changes favor  certain types of weather situations in some regions and others  elsewhere. &ldquo;Regional changes are mostly due to natural variability but  on top of that we see this pronounced overall weakening in summer storm  activity,&rdquo; says co-author Dim Coumou, &rdquo;This is also something projected  by climate models under future emission scenarios. However, the data so  far is not sufficient to say whether the storm activity changes are  caused by climate change &ndash; this has to be investigated further.&rdquo;<\/p>\n<p>  Although average summer storm activity decreases, the most intense  winter storms are projected to increase in frequency under continued  global warming. This could have severe implications for heavy rainfall  events. Also, the most intense hurricanes and typhoons in the tropics  are likely to increase under future warming because they&rsquo;re driven by  rising ocean surface temperatures. In the Northern mid-latitudes, the  main driver is the temperature difference between the warm equator and  the cold Arctic; a difference that is shrinking because man-made warming  is over-proportionate in the Arctic. <\/p>\n<p> &ldquo;Altogether our study  highlights how sensitive regional weather conditions are to any changes  in large-scale atmosphere dynamics,&rdquo; says Coumou. &ldquo;This can have serious  impacts for people on the ground.&rdquo;<\/p>\n<p> <strong>Article:<\/strong> Lehmann, J., Coumou, D. (2015): The influence of mid-latitude storm tracks on hot, cold, dry and wet extremes. <a href=\"http:\/\/www.nature.com\/articles\/srep17491\" target=\"_blank\" rel=\"noopener noreferrer\"><em>Nature Scientific Reports<\/em>. [DOI 10.1038\/srep17491]<\/a><\/p>\n<h5 class=\"green\">Source<\/h5>\n<p><a href=\"https:\/\/www.pik-potsdam.de\/news\/press-releases\/cold-hot-or-dry-persistent-weather-extremes-associated-with-decreased-storm-activity?set_language=en\" target=\"_blank\" rel=\"noopener noreferrer\">Potsdam Institute for Climate Impact Research 2015<\/a><\/p>\n<div class=\"shariff shariff-align-flex-start shariff-widget-align-flex-start\"><div class=\"ShariffHeadline\">Diese Meldung teilen<\/div><ul class=\"shariff-buttons theme-round orientation-horizontal buttonsize-medium\"><li class=\"shariff-button facebook shariff-nocustomcolor\" style=\"background-color:#4273c8;border-radius:1%\"><a href=\"https:\/\/www.facebook.com\/sharer\/sharer.php?u=https%3A%2F%2Fwww.sonnenseite.com%2Fen%2Fscience%2Fcold-hot-or-dry-persistent-weather-extremes-associated-with-decreased-storm-activity%2F\" title=\"Bei Facebook teilen\" aria-label=\"Bei Facebook teilen\" role=\"button\" rel=\"nofollow\" class=\"shariff-link\" style=\";border-radius:1%; 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