Draw up statistical models that can be used on a nationwide basis in order to study various management strategies and their effects on possible extreme events\u2019 vulnerabilities.<\/li>\n<\/ol>\n<\/ol>\n<\/ol>\nAll this will be done is several ways. As stated above, the history of various lake water quality change and watershed land use will be analyzed through satellite imagery. Using Landsat, images as far back as 1972, and MODIS, along with USGS gaging stations, we can find the history of water quality and the amount of algal biomass in various lakes over a period of time. This project will hone in on four different hydrologic regions: the Lower Peninsula, the High Plains Aquifer, the Kentucky-Oklahoma corridor, and the California mountains and Central Valley. These areas were chosen due to our prediction that there will be large discrepancies among the algal biomasses\u2019 responses to various extreme events. By this, we are trying to better understand how to predict algal blooms, how to better manage algal blooms, and how to better understand the impact of extreme events in various regions.<\/p>\n
The PI \u00a0for this project is Jane Stevenson. The co PIs are David Hyndman, Nathan Moore, and Jiaguo Qi. This project is funded by the EPA and received a grant on December 22, 2011 for $750,000.<\/p>\n","protected":false},"excerpt":{"rendered":"
Six Word Summary: Extreme Events Change Nutrient Delivery, Blooms Furthering steps taken by a past EPA Grant, this project is looking at predicting harmful algal blooms using remote sensing, hydrologic models, and landscape features. With current extreme events, such as droughts and storms, caused by climate change, we want to assess how they will impact … <\/p>\n
Continue reading “Forecasting and Evaluating Vulnerability of Watersheds to Climate Change, Extreme Events, and Algal Blooms”<\/span><\/a><\/p>\n","protected":false},"author":669,"featured_media":0,"comment_status":"closed","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[15],"tags":[],"class_list":["post-1127","post","type-post","status-publish","format-standard","hentry","category-completed"],"_links":{"self":[{"href":"https:\/\/hydrogeology.msu.edu\/wp-json\/wp\/v2\/posts\/1127","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/hydrogeology.msu.edu\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/hydrogeology.msu.edu\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/hydrogeology.msu.edu\/wp-json\/wp\/v2\/users\/669"}],"replies":[{"embeddable":true,"href":"https:\/\/hydrogeology.msu.edu\/wp-json\/wp\/v2\/comments?post=1127"}],"version-history":[{"count":12,"href":"https:\/\/hydrogeology.msu.edu\/wp-json\/wp\/v2\/posts\/1127\/revisions"}],"predecessor-version":[{"id":1912,"href":"https:\/\/hydrogeology.msu.edu\/wp-json\/wp\/v2\/posts\/1127\/revisions\/1912"}],"wp:attachment":[{"href":"https:\/\/hydrogeology.msu.edu\/wp-json\/wp\/v2\/media?parent=1127"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/hydrogeology.msu.edu\/wp-json\/wp\/v2\/categories?post=1127"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/hydrogeology.msu.edu\/wp-json\/wp\/v2\/tags?post=1127"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}