  {"id":1636,"date":"2024-08-07T11:25:04","date_gmt":"2024-08-07T15:25:04","guid":{"rendered":"https:\/\/umaine.edu\/watershedresearch\/?p=1636"},"modified":"2024-12-27T14:46:56","modified_gmt":"2024-12-27T19:46:56","slug":"flow-regimes-in-the-east-branch-of-the-penobscot-river-are-a-focus-of-wpes-summer-research-activities","status":"publish","type":"post","link":"https:\/\/umaine.edu\/watershedresearch\/2024\/08\/07\/flow-regimes-in-the-east-branch-of-the-penobscot-river-are-a-focus-of-wpes-summer-research-activities\/","title":{"rendered":"Flow regimes in the East Branch of the Penobscot River are a focus of WPES summer research activities"},"content":{"rendered":"\n<p>Undergraduate research assistant, Izaak Krause, from the Dept. of Civil and Environmental Engineering is working with Bea Van Dam and Sean Smith to assemble historic information, compile hydrologic and spatial data, and parameterize a watershed hydrologic model to evaluate flow regimes affecting Atlantic salmon habitat in the East Branch of the Penobscot River. Sponsored by Maine Sea Grant and led by the Penobscot Nation, the project is focused on the examination of scenarios related to watershed conditions, climate, civil infrastructure, and human generated disturbances to help guide river management decision-making. Progress this summer has included field observations, data development, and watershed model construction to advance our understanding of the many factors affecting watershed and river conditions.<\/p>\n\n\n\n<p><\/p>\n\n\n\n<p><\/p>\n\n\n\n<p><\/p>\n\n\n\n<figure class=\"wp-block-image size-full is-resized\"><img loading=\"lazy\" decoding=\"async\" width=\"807\" height=\"711\" src=\"https:\/\/umaine.edu\/watershedresearch\/wp-content\/uploads\/sites\/554\/2024\/08\/EB-Watershed-Graphic_WPES_2024.png\" alt=\"\" class=\"wp-image-1640\" style=\"width:814px;height:auto\" srcset=\"https:\/\/umaine.edu\/watershedresearch\/wp-content\/uploads\/sites\/554\/2024\/08\/EB-Watershed-Graphic_WPES_2024.png 807w, https:\/\/umaine.edu\/watershedresearch\/wp-content\/uploads\/sites\/554\/2024\/08\/EB-Watershed-Graphic_WPES_2024-300x264.png 300w, https:\/\/umaine.edu\/watershedresearch\/wp-content\/uploads\/sites\/554\/2024\/08\/EB-Watershed-Graphic_WPES_2024-768x677.png 768w, 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srcset=\"https:\/\/umaine.edu\/watershedresearch\/wp-content\/uploads\/sites\/554\/2024\/08\/20240824_134636b-1024x768.jpg 1024w, https:\/\/umaine.edu\/watershedresearch\/wp-content\/uploads\/sites\/554\/2024\/08\/20240824_134636b-300x225.jpg 300w, https:\/\/umaine.edu\/watershedresearch\/wp-content\/uploads\/sites\/554\/2024\/08\/20240824_134636b-768x576.jpg 768w, https:\/\/umaine.edu\/watershedresearch\/wp-content\/uploads\/sites\/554\/2024\/08\/20240824_134636b-1536x1152.jpg 1536w, https:\/\/umaine.edu\/watershedresearch\/wp-content\/uploads\/sites\/554\/2024\/08\/20240824_134636b-2048x1536.jpg 2048w, https:\/\/umaine.edu\/watershedresearch\/wp-content\/uploads\/sites\/554\/2024\/08\/20240824_134636b-105x79.jpg 105w, https:\/\/umaine.edu\/watershedresearch\/wp-content\/uploads\/sites\/554\/2024\/08\/20240824_134636b-317x238.jpg 317w, https:\/\/umaine.edu\/watershedresearch\/wp-content\/uploads\/sites\/554\/2024\/08\/20240824_134636b-423x317.jpg 423w, 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srcset=\"https:\/\/umaine.edu\/watershedresearch\/wp-content\/uploads\/sites\/554\/2024\/08\/Matagamon-Tailrace-1024x768.jpg 1024w, https:\/\/umaine.edu\/watershedresearch\/wp-content\/uploads\/sites\/554\/2024\/08\/Matagamon-Tailrace-300x225.jpg 300w, https:\/\/umaine.edu\/watershedresearch\/wp-content\/uploads\/sites\/554\/2024\/08\/Matagamon-Tailrace-768x576.jpg 768w, https:\/\/umaine.edu\/watershedresearch\/wp-content\/uploads\/sites\/554\/2024\/08\/Matagamon-Tailrace-1536x1152.jpg 1536w, https:\/\/umaine.edu\/watershedresearch\/wp-content\/uploads\/sites\/554\/2024\/08\/Matagamon-Tailrace-2048x1536.jpg 2048w, https:\/\/umaine.edu\/watershedresearch\/wp-content\/uploads\/sites\/554\/2024\/08\/Matagamon-Tailrace-105x79.jpg 105w, https:\/\/umaine.edu\/watershedresearch\/wp-content\/uploads\/sites\/554\/2024\/08\/Matagamon-Tailrace-317x238.jpg 317w, https:\/\/umaine.edu\/watershedresearch\/wp-content\/uploads\/sites\/554\/2024\/08\/Matagamon-Tailrace-423x317.jpg 423w, 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a watershed hydrologic model to evaluate flow regimes affecting Atlantic salmon habitat in the East Branch of the Penobscot River. Sponsored by [&hellip;]<\/p>\n","protected":false},"author":644,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"_kad_blocks_custom_css":"","_kad_blocks_head_custom_js":"","_kad_blocks_body_custom_js":"","_kad_blocks_footer_custom_js":"","_monsterinsights_skip_tracking":false,"_monsterinsights_sitenote_active":false,"_monsterinsights_sitenote_note":"","_monsterinsights_sitenote_category":0,"footnotes":""},"categories":[19],"tags":[33,32,31],"class_list":["post-1636","post","type-post","status-publish","format-standard","hentry","category-news","tag-atlantic-salmon","tag-flow-regime","tag-penobscot-river"],"yoast_head":"<!-- This site is optimized with the Yoast SEO plugin v27.2 - https:\/\/yoast.com\/product\/yoast-seo-wordpress\/ -->\n<title>Flow regimes in the East Branch of the Penobscot River are a focus of WPES summer research activities - Watershed Process and Estuary Sustainability Research Group<\/title>\n<meta name=\"robots\" content=\"index, follow, max-snippet:-1, max-image-preview:large, max-video-preview:-1\" \/>\n<link rel=\"canonical\" href=\"https:\/\/umaine.edu\/watershedresearch\/2024\/08\/07\/flow-regimes-in-the-east-branch-of-the-penobscot-river-are-a-focus-of-wpes-summer-research-activities\/\" \/>\n<meta property=\"og:locale\" content=\"en_US\" \/>\n<meta property=\"og:type\" content=\"article\" \/>\n<meta property=\"og:title\" content=\"Flow regimes in the East Branch of the Penobscot River are a focus of WPES summer research activities - Watershed Process and Estuary Sustainability Research Group\" \/>\n<meta property=\"og:description\" content=\"Undergraduate research assistant, Izaak Krause, from the Dept. of Civil and Environmental Engineering is working with Bea Van Dam and Sean Smith to assemble historic information, compile hydrologic and spatial data, and parameterize a watershed hydrologic model to evaluate flow regimes affecting Atlantic salmon habitat in the East Branch of the Penobscot River. 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