{"id":17,"date":"2014-11-17T16:17:49","date_gmt":"2014-11-17T23:17:49","guid":{"rendered":"https:\/\/blogs.ubc.ca\/slopestabilitygis\/?page_id=17"},"modified":"2014-12-08T00:12:08","modified_gmt":"2014-12-08T03:12:08","slug":"results","status":"publish","type":"page","link":"https:\/\/blogs.ubc.ca\/slopestabilitygis\/results\/","title":{"rendered":"Results"},"content":{"rendered":"<p><strong>General MCE<\/strong><br \/>\nThe general MCE shows that an intermediate level of landslide\u00a0potential dominates (0.2-0.6) across most of Vancouver Island (Figure 1). There is very few areas where there is a high\u00a0potential (0.6 &#8211; 0.85) of landslides on Vancouver Island. The areas of low landslide\u00a0potential (0.0 &#8211; 0.2) also seem relatively small.<\/p>\n<p><a href=\"https:\/\/blogs.ubc.ca\/slopestabilitygis\/files\/2014\/11\/CaptureGen.jpg\"><img loading=\"lazy\" decoding=\"async\" class=\"alignnone wp-image-223 size-full\" src=\"https:\/\/blogs.ubc.ca\/slopestabilitygis\/files\/2014\/11\/CaptureGen.jpg\" alt=\"CaptureGen\" width=\"733\" height=\"733\" srcset=\"https:\/\/blogs.ubc.ca\/slopestabilitygis\/files\/2014\/11\/CaptureGen.jpg 733w, https:\/\/blogs.ubc.ca\/slopestabilitygis\/files\/2014\/11\/CaptureGen-150x150.jpg 150w, https:\/\/blogs.ubc.ca\/slopestabilitygis\/files\/2014\/11\/CaptureGen-300x300.jpg 300w\" sizes=\"auto, (max-width: 733px) 100vw, 733px\" \/><\/a><br \/>\nFigure 1: General MCE<\/p>\n<p><strong>Deterministic MCE<\/strong><br \/>\nThe deterministic MCE map of landslide\u00a0potential is dominated by extremes (Figure 2). Either areas seem to be at high\u00a0potential of landslides (0.6-0.85) or low\u00a0potential (0.0 &#8211; 0.2). There seems to be fewer areas of intermediate\u00a0potential compared to the general MCE.<\/p>\n<p><a href=\"https:\/\/blogs.ubc.ca\/slopestabilitygis\/files\/2014\/11\/Captured.jpg\"><img loading=\"lazy\" decoding=\"async\" class=\"alignnone wp-image-218 size-full\" src=\"https:\/\/blogs.ubc.ca\/slopestabilitygis\/files\/2014\/11\/Captured.jpg\" alt=\"Captured\" width=\"738\" height=\"737\" srcset=\"https:\/\/blogs.ubc.ca\/slopestabilitygis\/files\/2014\/11\/Captured.jpg 738w, https:\/\/blogs.ubc.ca\/slopestabilitygis\/files\/2014\/11\/Captured-150x150.jpg 150w, https:\/\/blogs.ubc.ca\/slopestabilitygis\/files\/2014\/11\/Captured-300x300.jpg 300w\" sizes=\"auto, (max-width: 738px) 100vw, 738px\" \/><\/a><br \/>\nFigure 2: Deterministic MCE<\/p>\n<p><strong>Sensitivity Analysis<\/strong><br \/>\nThe map of the equal weighting MCE sensitivity analysis for the deterministic MCE shows a far lower landslide\u00a0potential across Vancouver Island (Figure 3). Previous areas that were high or intermediate\u00a0potential are now designated as intermediate and low\u00a0potential respectively.<\/p>\n<p><a href=\"https:\/\/blogs.ubc.ca\/slopestabilitygis\/files\/2014\/11\/CaptureSens.jpg\"><img loading=\"lazy\" decoding=\"async\" class=\"alignnone wp-image-221 size-full\" src=\"https:\/\/blogs.ubc.ca\/slopestabilitygis\/files\/2014\/11\/CaptureSens.jpg\" alt=\"CaptureSens\" width=\"732\" height=\"731\" srcset=\"https:\/\/blogs.ubc.ca\/slopestabilitygis\/files\/2014\/11\/CaptureSens.jpg 732w, https:\/\/blogs.ubc.ca\/slopestabilitygis\/files\/2014\/11\/CaptureSens-150x150.jpg 150w, https:\/\/blogs.ubc.ca\/slopestabilitygis\/files\/2014\/11\/CaptureSens-300x300.jpg 300w\" sizes=\"auto, (max-width: 732px) 100vw, 732px\" \/><\/a><br \/>\nFigure 3: Equal weighting sensitivity analysis<\/p>\n","protected":false},"excerpt":{"rendered":"<p>General MCE The general MCE shows that an intermediate level of landslide\u00a0potential dominates (0.2-0.6) across most of Vancouver Island (Figure 1). There is very few areas where there is a high\u00a0potential (0.6 &#8211; 0.85) of landslides on Vancouver Island. The &hellip; <a href=\"https:\/\/blogs.ubc.ca\/slopestabilitygis\/results\/\">Continue reading <span class=\"meta-nav\">&rarr;<\/span><\/a><\/p>\n","protected":false},"author":23318,"featured_media":0,"parent":0,"menu_order":4,"comment_status":"open","ping_status":"open","template":"","meta":{"footnotes":""},"class_list":["post-17","page","type-page","status-publish","hentry"],"_links":{"self":[{"href":"https:\/\/blogs.ubc.ca\/slopestabilitygis\/wp-json\/wp\/v2\/pages\/17","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/blogs.ubc.ca\/slopestabilitygis\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/blogs.ubc.ca\/slopestabilitygis\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/blogs.ubc.ca\/slopestabilitygis\/wp-json\/wp\/v2\/users\/23318"}],"replies":[{"embeddable":true,"href":"https:\/\/blogs.ubc.ca\/slopestabilitygis\/wp-json\/wp\/v2\/comments?post=17"}],"version-history":[{"count":18,"href":"https:\/\/blogs.ubc.ca\/slopestabilitygis\/wp-json\/wp\/v2\/pages\/17\/revisions"}],"predecessor-version":[{"id":224,"href":"https:\/\/blogs.ubc.ca\/slopestabilitygis\/wp-json\/wp\/v2\/pages\/17\/revisions\/224"}],"wp:attachment":[{"href":"https:\/\/blogs.ubc.ca\/slopestabilitygis\/wp-json\/wp\/v2\/media?parent=17"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}