


{"id":82369,"date":"2019-01-30T12:13:22","date_gmt":"2019-01-30T17:13:22","guid":{"rendered":"https:\/\/mrnf.gouv.qc.ca\/?post_type=cpt_publication&#038;p=82369"},"modified":"2026-08-04T13:21:19","modified_gmt":"2026-08-04T17:21:19","slug":"ice-bridges-st-lawrence-river","status":"publish","type":"cpt_publication","link":"https:\/\/mrnf.gouv.qc.ca\/en\/our-publications\/ice-bridges-st-lawrence-river\/","title":{"rendered":"Ice bridges on the St. Lawrence River as an index of winter severity from 1620 to 1910"},"content":{"rendered":"\n<p>Published in <b>Journal of Climate 20(F\u00e9vrier): 757-764<\/b><\/p>\n<p>Temperature reconstruction of the last thousand years suggests that an unprecedented warming (+0.6\u00b0C) occurred over the globe in the last century. However, regional variations in climate are not resolved by Northern Hemisphere reconstructions. In northeastern North America, past climate and, particularly, past winter variations are poorly known. Here, the authors report on the variation of a winter temperature index during the 1620\u20131910 period, based on the ice bridge formation (IBF) rate on the Saint Lawrence River at Qu\u00e9bec City (Canada), combined with instrumental data (1876\u20132000). During this 300-yr period, the IBF rate shows that winters in the seventeenth and eighteenth centuries were warmer than those in the nineteenth century. In particular, the IBF rate suggests that winter severity culminated in the 1850\u20131900 period, while very few ice bridges were reported between 1620 and 1740, presumably because of warmer temperatures and the relative scarcity of historical documents for the 1680\u20131740 period. These data suggest that winter temperature, particularly between ~1800 and 1910, was 2.4\u00b0 to 4.0\u00b0C colder than the last 30-yr average. Major volcanic eruptions had a significant positive impact on IBF rates, which is consistent with their role as important climate-forcing events.<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Published in Journal of Climate 20(F\u00e9vrier): 757-764 Temperature reconstruction of the last thousand years suggests that an unprecedented warming (+0.6\u00b0C) occurred over the globe in the last century. However, regional variations in climate are not resolved by Northern Hemisphere reconstructions. In northeastern North America, past climate and, particularly, past winter variations are poorly known. Here, [&hellip;]<\/p>\n","protected":false},"template":"","format":"standard","cptt_secteur":[1179],"cptt_theme":[1183,1185,1180],"cptt_categ_publi":[1149],"cptt_auteurs_ministeriels":[1091,1099],"class_list":["post-82369","cpt_publication","type-cpt_publication","status-publish","format-standard","hentry","cptt_secteur-forests","cptt_theme-ecosystems-and-environment","cptt_theme-forest-ecology","cptt_theme-forestry-research","cptt_categ_publi-scientific-article","cptt_auteurs_ministeriels-d-houle","cptt_auteurs_ministeriels-j-d-moore"],"acf":[],"yoast_head":"<!-- This site is optimized with the Yoast SEO plugin v24.9 - https:\/\/yoast.com\/wordpress\/plugins\/seo\/ -->\n<title>Ice bridges on the St. Lawrence River as an index of winter severity from 1620 to 1910 - Minist\u00e8re des Ressources naturelles et des For\u00eats<\/title>\n<meta name=\"description\" content=\"Report on the variation of a winter temperature index during the 1620\u20131910 period, based on the ice bridge formation rate on the Saint Lawrence River\" \/>\n<meta name=\"robots\" content=\"index, follow, max-snippet:-1, max-image-preview:large, max-video-preview:-1\" \/>\n<link rel=\"canonical\" href=\"https:\/\/mrnf.gouv.qc.ca\/en\/our-publications\/ice-bridges-st-lawrence-river\/\" \/>\n<meta property=\"og:locale\" content=\"en_US\" \/>\n<meta property=\"og:type\" content=\"article\" \/>\n<meta property=\"og:title\" content=\"Ice bridges on the St. Lawrence River as an index of winter severity from 1620 to 1910 - Minist\u00e8re des Ressources naturelles et des For\u00eats\" \/>\n<meta property=\"og:description\" content=\"Report on the variation of a winter temperature index during the 1620\u20131910 period, based on the ice bridge formation rate on the Saint Lawrence River\" \/>\n<meta property=\"og:url\" content=\"https:\/\/mrnf.gouv.qc.ca\/en\/our-publications\/ice-bridges-st-lawrence-river\/\" \/>\n<meta property=\"og:site_name\" content=\"Minist\u00e8re des Ressources naturelles et des For\u00eats\" \/>\n<meta property=\"article:publisher\" content=\"https:\/\/www.facebook.com\/RessourcesNaturellesForets\/\" \/>\n<meta property=\"article:modified_time\" content=\"2026-08-04T17:21:19+00:00\" \/>\n<meta property=\"og:image\" content=\"\/wp-content\/uploads\/Image-g%c3%a9n%c3%a9rale-hiver_FB.jpg\" \/>\n\t<meta property=\"og:image:width\" content=\"1200\" \/>\n\t<meta property=\"og:image:height\" content=\"630\" \/>\n\t<meta property=\"og:image:type\" content=\"image\/jpeg\" \/>\n<meta name=\"twitter:card\" content=\"summary_large_image\" \/>\n<meta name=\"twitter:site\" content=\"@mrnfqc\" \/>\n<meta name=\"twitter:label1\" content=\"Est. reading time\" \/>\n\t<meta name=\"twitter:data1\" content=\"2 minutes\" \/>\n<script type=\"application\/ld+json\" class=\"yoast-schema-graph\">{\"@context\":\"https:\/\/schema.org\",\"@graph\":[{\"@type\":\"WebPage\",\"@id\":\"https:\/\/mrnf.gouv.qc.ca\/en\/our-publications\/ice-bridges-st-lawrence-river\/\",\"url\":\"https:\/\/mrnf.gouv.qc.ca\/en\/our-publications\/ice-bridges-st-lawrence-river\/\",\"name\":\"Ice bridges on the St. Lawrence River as an index of winter severity from 1620 to 1910 - 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