{"id":1274,"date":"2025-06-25T05:15:33","date_gmt":"2025-06-25T05:15:33","guid":{"rendered":"https:\/\/cametocean.com\/?page_id=1274"},"modified":"2025-06-25T05:40:33","modified_gmt":"2025-06-25T05:40:33","slug":"bay-of-bengal-cyclonic-hindcast","status":"publish","type":"page","link":"https:\/\/cametocean.com\/?page_id=1274","title":{"rendered":"Bay of Bengal"},"content":{"rendered":"\n<p><strong>Description<\/strong><\/p>\n\n\n\n<p>A hindcast of cyclonic waves for the Bay of Bengal was developed following the method outlined in <a href=\"https:\/\/cametocean.com\/?page_id=1255\" data-type=\"page\" data-id=\"1255\">Cyclonic Wave Hindcasts<\/a><\/p>\n\n\n\n<p><strong>Key features<\/strong><\/p>\n\n\n\n<ul class=\"wp-block-list\">\n<li>Cyclones for the period 1990 to 2023 are included in the last version of this data set.<\/li>\n\n\n\n<li>The computational rectangular grid has a resolution of 0.1\u00b0 x 0.1\u00b0 and covers the area between 05.00\u00b0and 23.00\u00b0 N and between 078.00\u00b0 and 098.00\u00b0E<\/li>\n\n\n\n<li>Model outputs were verified against available satellite measurements in the area<\/li>\n<\/ul>\n\n\n\n<figure class=\"wp-block-image size-large\"><img loading=\"lazy\" decoding=\"async\" width=\"1024\" height=\"899\" src=\"https:\/\/cametocean.com\/wp-content\/uploads\/2025\/06\/BoB_CycloneHndcast-1024x899.png\" alt=\"\" class=\"wp-image-1275\" srcset=\"https:\/\/cametocean.com\/wp-content\/uploads\/2025\/06\/BoB_CycloneHndcast-1024x899.png 1024w, https:\/\/cametocean.com\/wp-content\/uploads\/2025\/06\/BoB_CycloneHndcast-300x263.png 300w, https:\/\/cametocean.com\/wp-content\/uploads\/2025\/06\/BoB_CycloneHndcast-768x674.png 768w, https:\/\/cametocean.com\/wp-content\/uploads\/2025\/06\/BoB_CycloneHndcast-342x300.png 342w, https:\/\/cametocean.com\/wp-content\/uploads\/2025\/06\/BoB_CycloneHndcast.png 1232w\" sizes=\"auto, (max-width: 1024px) 100vw, 1024px\" \/><\/figure>\n","protected":false},"excerpt":{"rendered":"<p>Description A hindcast of cyclonic waves for the Bay of Bengal was developed following the method outlined in Cyclonic Wave Hindcasts Key features<\/p>\n","protected":false},"author":1,"featured_media":1179,"parent":1255,"menu_order":3,"comment_status":"closed","ping_status":"closed","template":"","meta":{"footnotes":""},"class_list":["post-1274","page","type-page","status-publish","has-post-thumbnail","hentry"],"_links":{"self":[{"href":"https:\/\/cametocean.com\/index.php?rest_route=\/wp\/v2\/pages\/1274","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/cametocean.com\/index.php?rest_route=\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/cametocean.com\/index.php?rest_route=\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/cametocean.com\/index.php?rest_route=\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/cametocean.com\/index.php?rest_route=%2Fwp%2Fv2%2Fcomments&post=1274"}],"version-history":[{"count":3,"href":"https:\/\/cametocean.com\/index.php?rest_route=\/wp\/v2\/pages\/1274\/revisions"}],"predecessor-version":[{"id":1288,"href":"https:\/\/cametocean.com\/index.php?rest_route=\/wp\/v2\/pages\/1274\/revisions\/1288"}],"up":[{"embeddable":true,"href":"https:\/\/cametocean.com\/index.php?rest_route=\/wp\/v2\/pages\/1255"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/cametocean.com\/index.php?rest_route=\/wp\/v2\/media\/1179"}],"wp:attachment":[{"href":"https:\/\/cametocean.com\/index.php?rest_route=%2Fwp%2Fv2%2Fmedia&parent=1274"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}