{"id":6793,"date":"2026-01-27T15:21:51","date_gmt":"2026-01-27T14:21:51","guid":{"rendered":"https:\/\/ist.blogs.inrae.fr\/afs\/?p=6793"},"modified":"2026-01-27T15:22:16","modified_gmt":"2026-01-27T14:22:16","slug":"impact-of-extreme-precipitation-events-on-summer-deep-seepage-below-temperate-forests-in-the-northeastern-germany-lowlands","status":"publish","type":"post","link":"https:\/\/ist.blogs.inrae.fr\/afs\/2026\/01\/27\/impact-of-extreme-precipitation-events-on-summer-deep-seepage-below-temperate-forests-in-the-northeastern-germany-lowlands\/","title":{"rendered":"Impact of extreme precipitation events on summer deep seepage below temperate forests in the Northeastern Germany lowlands"},"content":{"rendered":"<script type='text\/javascript' src='https:\/\/d1bxh8uas1mnw7.cloudfront.net\/assets\/embed.js'><\/script><p style=\"text-align: left\"><span style=\"color: #0d5c06;font-size: 10pt\"><strong>Research paper<\/strong><\/span><\/p>\n<p><strong><a href=\"https:\/\/ist.blogs.inrae.fr\/afs\/wp-content\/uploads\/sites\/5\/2026\/01\/26-01-27_Natkhin-M.png\"><img loading=\"lazy\" decoding=\"async\" class=\"wp-image-6795 alignleft\" src=\"https:\/\/ist.blogs.inrae.fr\/afs\/wp-content\/uploads\/sites\/5\/2026\/01\/26-01-27_Natkhin-M-291x300.png\" alt=\"\" width=\"208\" height=\"215\" srcset=\"https:\/\/ist.blogs.inrae.fr\/afs\/wp-content\/uploads\/sites\/5\/2026\/01\/26-01-27_Natkhin-M-291x300.png 291w, https:\/\/ist.blogs.inrae.fr\/afs\/wp-content\/uploads\/sites\/5\/2026\/01\/26-01-27_Natkhin-M-640x660.png 640w, https:\/\/ist.blogs.inrae.fr\/afs\/wp-content\/uploads\/sites\/5\/2026\/01\/26-01-27_Natkhin-M.png 685w\" sizes=\"auto, (max-width: 208px) 100vw, 208px\" \/><\/a>Key message<\/strong><\/p>\n<p align=\"justify\">Stands stocked with European beech (<i>Fagus sylvatica<\/i>\u00a0L.), sessile oak (<i>Quercus petraea<\/i>\u00a0(Matt.) Liebl.), and Scots pine (<i>Pinus sylvestris<\/i>\u00a0L.) show distinct deep seepage patterns. An increasing importance of extreme summer precipitation contributing to deep seepage in the northeastern German lowlands was detected. Extreme summer precipitation events contributed 71% (pine), 22% (young oak), and 15% (beech) of the annual deep seepage. Adapted forest management may promote deep seepage caused by extreme summer precipitation and by precipitation during the winter half-year.<\/p>\n<p><strong>Keywords<\/strong><br \/>\nDeep seepage; Forest hydrology; Large-scale lysimeter; Northeastern Germany lowlands; Intensive forest monitoring station Britz<\/p>\n<div class='altmetric-embed' data-badge-type='donut' data-doi='10.1186\/s13595-025-01318-2'  style='float: right; ' ><\/div>\n<p><strong>Publication<\/strong><br \/>\nNatkhin, M., Strer, M., Sanders, T.\u00a0<i>et al.<\/i>\u00a0Impact of extreme precipitation events on summer deep seepage below temperate forests in the Northeastern Germany lowlands.\u00a0<i>Annals of Forest Science<\/i>\u00a083, 5 (2026). <a href=\"https:\/\/doi.org\/10.1186\/s13595-025-01318-2\">https:\/\/doi.org\/10.1186\/s13595-025-01318-2<\/a><\/p>\n<p><strong>Data availability<\/strong><br \/>\nThe data used in this manuscript is accessible at Natkhin M, Bahr A, Christen B, Strer M (2025) Data used for analysis of extreme precipitation events and their Impact on summer deep seepage on the Intensive Forest Monitoring Station Britz 2025. <a href=\"https:\/\/doi.org\/10.3220\/253-2025-175\">https:\/\/doi.org\/10.3220\/253-2025-175<\/a><\/p>\n<p><strong>Handling editor<\/strong><br \/>\nErwin Dreyer<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Research paper Key message Stands stocked with European beech (Fagus sylvatica\u00a0L.), sessile oak (Quercus petraea\u00a0(Matt.) Liebl.), and Scots pine (Pinus sylvestris\u00a0L.) show distinct deep seepage patterns. An increasing importance of extreme summer precipitation contributing to deep seepage in the northeastern German lowlands was detected. Extreme summer precipitation events contributed 71% (pine), 22% (young oak), and [&hellip;]<\/p>\n","protected":false},"author":240,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[14,1,109,15],"tags":[],"class_list":["post-6793","post","type-post","status-publish","format-standard","hentry","category-article-type","category-non-classe","category-open-access","category-research-paper","cat-14-id","cat-1-id","cat-109-id","cat-15-id"],"_links":{"self":[{"href":"https:\/\/ist.blogs.inrae.fr\/afs\/wp-json\/wp\/v2\/posts\/6793","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/ist.blogs.inrae.fr\/afs\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/ist.blogs.inrae.fr\/afs\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/ist.blogs.inrae.fr\/afs\/wp-json\/wp\/v2\/users\/240"}],"replies":[{"embeddable":true,"href":"https:\/\/ist.blogs.inrae.fr\/afs\/wp-json\/wp\/v2\/comments?post=6793"}],"version-history":[{"count":5,"href":"https:\/\/ist.blogs.inrae.fr\/afs\/wp-json\/wp\/v2\/posts\/6793\/revisions"}],"predecessor-version":[{"id":6813,"href":"https:\/\/ist.blogs.inrae.fr\/afs\/wp-json\/wp\/v2\/posts\/6793\/revisions\/6813"}],"wp:attachment":[{"href":"https:\/\/ist.blogs.inrae.fr\/afs\/wp-json\/wp\/v2\/media?parent=6793"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/ist.blogs.inrae.fr\/afs\/wp-json\/wp\/v2\/categories?post=6793"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/ist.blogs.inrae.fr\/afs\/wp-json\/wp\/v2\/tags?post=6793"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}