{"id":46357,"date":"2019-06-17T13:58:24","date_gmt":"2019-06-17T12:58:24","guid":{"rendered":"https:\/\/www.lse.ac.uk\/granthaminstitute\/?post_type=publication&#038;p=46357"},"modified":"2024-08-19T14:18:36","modified_gmt":"2024-08-19T13:18:36","slug":"the-need-for-bottom-up-assessments-of-climate-risks-and-adaptation-in-climate-sensitive-regions","status":"publish","type":"publication","link":"https:\/\/www.lse.ac.uk\/granthaminstitute\/publication\/the-need-for-bottom-up-assessments-of-climate-risks-and-adaptation-in-climate-sensitive-regions\/","title":{"rendered":"The need for bottom-up assessments of climate risks and adaptation in climate-sensitive regions"},"content":{"rendered":"<!DOCTYPE html PUBLIC \"-\/\/W3C\/\/DTD HTML 4.0 Transitional\/\/EN\" \"http:\/\/www.w3.org\/TR\/REC-html40\/loose.dtd\">\n<?xml encoding=\"UTF-8\"><p><strong>Abstract<\/strong><\/p>\n<p>Studies of climate change at specific intervals of future warming have primarily been addressed through top-down approaches using climate projections and modelled impacts. In contrast, bottom-up approaches focus on the recent past and present vulnerability. Here, we examine climate signals at different increments of warming and consider the need to reconcile top-down and bottom-up approaches. We synthesise insights from recent studies in three climate-sensitive systems where change is a defining feature of the human-environment system. Whilst top-down and bottom-up approaches generate complementary insights into who and what is at risk, integrating their results is a much-needed step towards developing relevant information to address the needs of immediate adaptation decisions.<\/p>\n<p>Conway, D., Nicholls, R.J., Brown, S., Tebboth, M.G.L., Adger, W.N., Ahmad, B., Biemans, H., Crick, F., Lutz, A.F., Safra De Campos, R., Said, M., Singh, C., Zaroug, M.A.H., Ludi, E., New, M. and Wester, P. (2019). In:&nbsp;Nature Climate Change 9,&nbsp;503&ndash;511.<a class=\"link link--external\" title=\"https:\/\/doi.org\/10.1038\/s41558-019-0502-0\" href=\"https:\/\/doi.org\/10.1038\/s41558-019-0502-0\" aria-describedby=\"link-description-new-window\" target=\"_blank\" rel=\"noopener\">https:\/\/doi.org\/10.1038\/s41558-019-0502-0&#65279;<svg xmlns=\"http:\/\/www.w3.org\/2000\/svg\" viewbox=\"0 0 16 16\" role=\"img\" aria-hidden=\"true\"><path d=\"M14.42 1.04L3.2.7a.8.8 0 00-.8.76v.1a.8.8 0 00.76.7l9.39.3L.93 14.16c-.3.3-.3.8 0 1.1l.09.08c.3.23.73.2 1.01-.07L13.65 3.65l.29 9.4a.8.8 0 00.8.76.79.79 0 00.77-.8L15.17 1.8a.82.82 0 00-.75-.76z\" fill=\"#2e3152\"><\/path><\/svg><\/a><\/p>\n\n","protected":false},"excerpt":{"rendered":"<!DOCTYPE html PUBLIC \"-\/\/W3C\/\/DTD HTML 4.0 Transitional\/\/EN\" \"http:\/\/www.w3.org\/TR\/REC-html40\/loose.dtd\">\n<?xml encoding=\"UTF-8\"><p>Abstract Studies of climate change at specific intervals of future warming have primarily been addressed through top-down approaches using climate&hellip;<\/p>\n\n","protected":false},"author":12,"featured_media":0,"template":"","tags":[],"publication-type":[436],"topic_area":[4692],"class_list":["post-46357","publication","type-publication","status-publish","hentry","publication-type-research-articles","topic_area-adaptation-and-resilience"],"acf":{"exclude_from_sync":{"ref_value":"field_560538b0e7350","value":"0","type":false,"post_type":""},"downloads":{"ref_value":"field_52f16cc1a80f2","value":false,"type":"repeater","post_type":""},"rss_newsletter":{"ref_value":"field_54f5c2c1544d8","value":"","type":false,"post_type":""},"profile_link":{"ref_value":"field_52f164b5189e9","value":["declan-conway","florence-crick"],"type":"relationship","post_type":"profile"},"article_link":{"ref_value":"field_52eee3c7f0586","value":"https:\/\/www.nature.com\/articles\/s41558-019-0502-0","type":false,"post_type":""},"article_link_title":{"ref_value":"field_5322399d89d42","value":"external link to paper","type":false,"post_type":""},"spotlight":{"ref_value":"field_52f80896506d3","value":"","type":false,"post_type":""}},"yoast_head":"<!-- This site is optimized with the Yoast SEO plugin v27.3 - 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