{"id":904,"date":"2023-04-10T15:11:14","date_gmt":"2023-04-10T19:11:14","guid":{"rendered":"https:\/\/dev.seagrant.w3.uvm.edu\/2023\/04\/10\/are-you-prepared-if-we-have-spring-flooding\/"},"modified":"2025-10-22T17:49:08","modified_gmt":"2025-10-22T21:49:08","slug":"are-you-prepared-if-we-have-spring-flooding","status":"publish","type":"post","link":"https:\/\/www.uvm.edu\/seagrant\/2023\/04\/10\/are-you-prepared-if-we-have-spring-flooding\/","title":{"rendered":"Are You Prepared If We Have Spring Flooding?"},"content":{"rendered":"<p>\n\tApril showers (and snowmelt) can bring May flowers and spring flooding. Let&#8217;s learn about the factors that can cause spring flooding in the Lake Champlain Basin, and how you can prepare!\u00a0<\/p>\n<p>\n\tIn the winter, much of the precipitation we receive is stored as snow and ice in higher elevations of the basin. This year\u2019s mid-March snowstorms pushed our snow levels above average as recorded by the <a href=\"https:\/\/matthewparrilla.com\/mansfield-stake\/\" target=\"_blank\">National Weather Service at the top of Mount Mansfield<\/a>. As winter turns to spring, much of this snow and ice stored high up in the mountains will melt and drain into Lake Champlain.\u202f\u00a0<\/p>\n<p>\n\tLake Champlain usually reaches its peak water level in May, when it absorbs the last of winter\u2019s snowmelt and \u00a0spring rains. The lake\u2019s average water level is 95.5 feet\u2014any water level higher than 100 feet is considered to be in flood stage. Lake Champlain\u2019s water level is measured by the USGS. <a href=\"https:\/\/waterdata.usgs.gov\/monitoring-location\/04294500\/#parameterCode=62615&#038;period=P7D\" target=\"_blank\">Check out today&#8217;s levels<\/a>. \u00a0<picture  title=\"Fluvial erosion resulting from flooding on Vermont Route 4 in Killington, VT during Tropical Storm Irene Photo Credit: Mansfield Heliflight\" data-picture-mapping=\"half_width\" data-picture-align=\"right\">\n<!--[if IE 9]><video style=\"display: none;\"><![endif]--><source srcset=\"\/\/www.uvm.edu\/seagrant\/sites\/default\/files\/styles\/half-width__wide\/public\/uploads\/fluvial%20erosion%202.jpeg?itok=SkMgPU45 1x\" media=\"(min-width: 1200px)\" \/><source srcset=\"\/\/www.uvm.edu\/seagrant\/sites\/default\/files\/styles\/half-width__desk\/public\/uploads\/fluvial%20erosion%202.jpeg?itok=3GTcvexl 1x\" media=\"(min-width: 960px)\" \/><source srcset=\"\/\/www.uvm.edu\/seagrant\/sites\/default\/files\/styles\/half-width__tablet\/public\/uploads\/fluvial%20erosion%202.jpeg?itok=ADsw5zSG 1x\" media=\"(min-width: 600px)\" \/><source srcset=\"\/\/www.uvm.edu\/seagrant\/sites\/default\/files\/styles\/full-width__mobile\/public\/uploads\/fluvial%20erosion%202.jpeg?itok=-lmweF6q 1x\" media=\"(min-width: 0)\" \/><!--[if IE 9]><\/video><![endif]--><br \/>\n<!--[if lt IE 9]>\n<img decoding=\"async\"  data-picture-mapping=\"half_width\" data-picture-align=\"right\" src=\"\/\/www.uvm.edu\/seagrant\/sites\/default\/files\/styles\/flexslider_full\/public\/uploads\/fluvial%20erosion%202.jpeg?itok=VI9cw3s8\" alt=\"Fluvial erosion resulting from flooding on Vermont Route 4 in Killington, VT during Tropical Storm Irene\" title=\"Fluvial erosion resulting from flooding on Vermont Route 4 in Killington, VT during Tropical Storm Irene Photo Credit: Mansfield Heliflight\" \/>\n<![endif]--><br \/>\n<!--[if !lt IE 9]><!--><br \/>\n<img  data-picture-mapping=\"half_width\" data-picture-align=\"right\" srcset=\"\/\/www.uvm.edu\/seagrant\/sites\/default\/files\/styles\/flexslider_full\/public\/uploads\/fluvial%20erosion%202.jpeg?itok=VI9cw3s8 800w\" alt=\"Fluvial erosion resulting from flooding on Vermont Route 4 in Killington, VT during Tropical Storm Irene\" title=\"Fluvial erosion resulting from flooding on Vermont Route 4 in Killington, VT during Tropical Storm Irene Photo Credit: Mansfield Heliflight\" \/><br \/>\n<!-- <![endif]-->\n<\/picture><\/p>\n<p>\n\tBut the risk of spring flooding exists beyond the lake. Flooding events actually occur more often in rivers and streams as water moves through narrow river valleys towards the lake.\u202f\u00a0<\/p>\n<p>\n\tFlooding events in rivers and streams are intensified by springtime temperatures that fluctuate well above and below freezing. This can speed up or stop flow as ice, snow, and water interact. Snow-covered ground acts like a speedy runway for rainwater entering rivers and streams, giving them added power. Chunks of ice can pile up in rivers, forming ice jams that divert, slow, or stop water flow.\u202f\u00a0<\/p>\n<p>\n\tTwo main types of hazards occur as a result of snowmelt, heavy spring rain, and fluctuating temperatures. The first is the flooding or inundation itself caused by rising levels of lake or river water. Picture water covering areas of land that are normally dry. This can damage homes and buildings and be dangerous to drive or walk through. The second hazard is fluvial erosion, which occurs when fast moving water carries away material from stream beds and banks.\u00a0This can make roads, buildings, and utility lines unsafe by undercutting them or even carrying them away.\u00a0<\/p>\n<p>\n\tFlooding is a natural function of water moving throughout different elevations in our mountainous watershed, but it can cause serious destruction to homes and infrastructure in flood-prone areas. This destruction is predicted to increase as climate change brings more intense storms to the Lake Champlain basin at a higher frequency. The restoration of our waterway&#8217;s natural buffers\u2014shorelines and wetlands\u2014will help to minimize flood damage and give our lakes, rivers, and streams the room they need to move into their natural floodplains.\u00a0\u00a0<\/p>\n<p>\n\t<picture  title=\"Inundation flooding at Burlington, Vermont's waterfront Photo Credit: Aude Lochet\" data-picture-mapping=\"half_width\" data-picture-align=\"left\">\n<!--[if IE 9]><video style=\"display: none;\"><![endif]--><source srcset=\"\/\/www.uvm.edu\/seagrant\/sites\/default\/files\/styles\/half-width__wide\/public\/uploads\/Inundation%20Flooding.jpg?itok=wu_32egl 1x\" media=\"(min-width: 1200px)\" \/><source srcset=\"\/\/www.uvm.edu\/seagrant\/sites\/default\/files\/styles\/half-width__desk\/public\/uploads\/Inundation%20Flooding.jpg?itok=nRsDELqv 1x\" media=\"(min-width: 960px)\" \/><source srcset=\"\/\/www.uvm.edu\/seagrant\/sites\/default\/files\/styles\/half-width__tablet\/public\/uploads\/Inundation%20Flooding.jpg?itok=gJ6pUWMU 1x\" media=\"(min-width: 600px)\" \/><source srcset=\"\/\/www.uvm.edu\/seagrant\/sites\/default\/files\/styles\/full-width__mobile\/public\/uploads\/Inundation%20Flooding.jpg?itok=vGmhDz4e 1x\" media=\"(min-width: 0)\" \/><!--[if IE 9]><\/video><![endif]--><br \/>\n<!--[if lt IE 9]>\n<img decoding=\"async\"  data-picture-mapping=\"half_width\" data-picture-align=\"left\" src=\"\/\/www.uvm.edu\/seagrant\/sites\/default\/files\/styles\/flexslider_full\/public\/uploads\/Inundation%20Flooding.jpg?itok=-yUq8HRP\" alt=\"Inundation flooding at Burlington, Vermont's waterfront\" title=\"Inundation flooding at Burlington, Vermont's waterfront Photo Credit: Aude Lochet\" \/>\n<![endif]--><br \/>\n<!--[if !lt IE 9]><!--><br \/>\n<img  data-picture-mapping=\"half_width\" data-picture-align=\"left\" srcset=\"\/\/www.uvm.edu\/seagrant\/sites\/default\/files\/styles\/flexslider_full\/public\/uploads\/Inundation%20Flooding.jpg?itok=-yUq8HRP 800w\" alt=\"Inundation flooding at Burlington, Vermont's waterfront\" title=\"Inundation flooding at Burlington, Vermont's waterfront Photo Credit: Aude Lochet\" \/><br \/>\n<!-- <![endif]-->\n<\/picture>People and buildings in flood zones are at risk. It is important to be informed about your home\u2019s flood risk in spring and throughout the year. The Federal Emergency Management Agency (FEMA) maps flood-prone areas throughout the country. Plug your address into their <a href=\"https:\/\/msc.fema.gov\/portal\/home\" target=\"_blank\">Flood Map<\/a> or contact a local government official to gain a better understanding of your risk.\u202f Sign up for <a href=\"https:\/\/vem.vermont.gov\/vtalert\">VT-Alert<\/a> to stay in the know about weather advisories and road closures. The <a href=\"https:\/\/www.fema.gov\/emergency-managers\/practitioners\/integrated-public-alert-warning-system\/public\/emergency-alert-system\">Emergency Alert System (EAS)<\/a> also provides flood related emergency alerts. \u00a0<\/p>\n<p>\n\tTo prepare your home for flooding, contact your insurance agent to discuss your flood insurance coverage. Elevate basement utilities and materials to minimize potential damage. Develop a Family Emergency Kit and a Family Communication Plan. Visit <a href=\"https:\/\/vem.vermont.gov\/preparedness\/floods\" target=\"_blank\">VT Emergency Management\u2019s Community Preparedness<\/a> website for more detailed information on how to prepare and respond to a flood.\u00a0\u00a0<\/p>\n<p>\n\tWant to take a deep dive into flood resilience on the community and individual levels? Take a look at Lake Champlain Sea Grant\u2019s webinar, <a href=\"https:\/\/www.uvm.edu\/seagrant\/how-avoid-damage-flooding\" target=\"_blank\">\u201cHow to Avoid Damage from Flooding\u201d<\/a> and the State of Vermont\u2019s <a href=\"https:\/\/floodready.vermont.gov\/\" target=\"_blank\">Flood Ready website<\/a>.\u00a0<\/p>\n","protected":false},"excerpt":{"rendered":"<p>April showers (and snowmelt) can bring May flowers and spring&#8230;<\/p>\n","protected":false},"author":1,"featured_media":1548,"comment_status":"closed","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"_eb_attr":"","_price":"","_stock":"","_tribe_ticket_header":"","_tribe_default_ticket_provider":"","_tribe_ticket_capacity":"0","_ticket_start_date":"","_ticket_end_date":"","_tribe_ticket_show_description":"","_tribe_ticket_show_not_going":false,"_tribe_ticket_use_global_stock":"","_tribe_ticket_global_stock_level":"","_global_stock_mode":"","_global_stock_cap":"","_tribe_rsvp_for_event":"","_tribe_ticket_going_count":"","_tribe_ticket_not_going_count":"","_tribe_tickets_list":"[]","_tribe_ticket_has_attendee_info_fields":false,"footnotes":""},"categories":[1],"tags":[],"post_folder":[],"class_list":["post-904","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-uncategorized"],"acf":[],"_links":{"self":[{"href":"https:\/\/www.uvm.edu\/seagrant\/wp-json\/wp\/v2\/posts\/904","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/www.uvm.edu\/seagrant\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/www.uvm.edu\/seagrant\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/www.uvm.edu\/seagrant\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/www.uvm.edu\/seagrant\/wp-json\/wp\/v2\/comments?post=904"}],"version-history":[{"count":1,"href":"https:\/\/www.uvm.edu\/seagrant\/wp-json\/wp\/v2\/posts\/904\/revisions"}],"predecessor-version":[{"id":1225,"href":"https:\/\/www.uvm.edu\/seagrant\/wp-json\/wp\/v2\/posts\/904\/revisions\/1225"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/www.uvm.edu\/seagrant\/wp-json\/wp\/v2\/media\/1548"}],"wp:attachment":[{"href":"https:\/\/www.uvm.edu\/seagrant\/wp-json\/wp\/v2\/media?parent=904"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.uvm.edu\/seagrant\/wp-json\/wp\/v2\/categories?post=904"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.uvm.edu\/seagrant\/wp-json\/wp\/v2\/tags?post=904"},{"taxonomy":"post_folder","embeddable":true,"href":"https:\/\/www.uvm.edu\/seagrant\/wp-json\/wp\/v2\/post_folder?post=904"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}