{"id":1979,"date":"2018-06-01T10:59:52","date_gmt":"2018-06-01T15:59:52","guid":{"rendered":"http:\/\/oceanweatherservices.com\/blog\/?p=1979"},"modified":"2018-06-01T16:49:00","modified_gmt":"2018-06-01T21:49:00","slug":"north-atlantic-cooling-will-affect-hurricane-season","status":"publish","type":"post","link":"https:\/\/oceanweatherservices.com\/blog\/2018\/06\/01\/north-atlantic-cooling-will-affect-hurricane-season\/","title":{"rendered":"North Atlantic Cooling will affect the Hurricane Season"},"content":{"rendered":"<div id=\"attachment_1981\" style=\"width: 410px\" class=\"wp-caption alignleft\"><img aria-describedby=\"caption-attachment-1981\" decoding=\"async\" loading=\"lazy\" class=\"wp-image-1981\" src=\"http:\/\/oceanweatherservices.com\/blog\/wp-content\/uploads\/2018\/06\/bermuda-high-300x121.png\" alt=\"Bermuda High\" width=\"400\" height=\"161\" srcset=\"https:\/\/oceanweatherservices.com\/blog\/wp-content\/uploads\/2018\/06\/bermuda-high-300x121.png 300w, https:\/\/oceanweatherservices.com\/blog\/wp-content\/uploads\/2018\/06\/bermuda-high.png 736w\" sizes=\"(max-width: 400px) 100vw, 400px\" \/><p id=\"caption-attachment-1981\" class=\"wp-caption-text\">Bermuda High and Tropical Cyclone tracks<\/p><\/div>\n<p>The main tropical development area for the North Atlantic continues to cool relative to recent averages suggesting a stronger than normal Bermuda-Azores ridge.\u00a0When this high pressure ridge is stronger or displaced west, as it appears to be now, tropical storm formation is less likely due to<\/p>\n<div id=\"attachment_1983\" style=\"width: 485px\" class=\"wp-caption alignright\"><img aria-describedby=\"caption-attachment-1983\" decoding=\"async\" loading=\"lazy\" class=\"wp-image-1983\" src=\"http:\/\/oceanweatherservices.com\/blog\/wp-content\/uploads\/2018\/06\/surpres-april-2018-300x166.png\" alt=\"\" width=\"475\" height=\"262\" srcset=\"https:\/\/oceanweatherservices.com\/blog\/wp-content\/uploads\/2018\/06\/surpres-april-2018-300x166.png 300w, https:\/\/oceanweatherservices.com\/blog\/wp-content\/uploads\/2018\/06\/surpres-april-2018-768x424.png 768w, https:\/\/oceanweatherservices.com\/blog\/wp-content\/uploads\/2018\/06\/surpres-april-2018-1024x565.png 1024w, https:\/\/oceanweatherservices.com\/blog\/wp-content\/uploads\/2018\/06\/surpres-april-2018.png 1042w\" sizes=\"(max-width: 475px) 100vw, 475px\" \/><p id=\"caption-attachment-1983\" class=\"wp-caption-text\">NCEP Reanalysis mean surface pressure April 2018. Image credit <a href=\"https:\/\/www.tropicaltidbits.com\">https:\/\/www.tropicaltidbits.com<\/a><\/p><\/div>\n<p>stronger wind shear and cooler SST temperatures caused by stronger trade winds, however, when tropical cyclones do form, a strong Bermuda-Azores high will tend to cause storms to track farther to the west increasing landfall risks.<\/p>\n<p>&nbsp;<\/p>\n<div id=\"attachment_1980\" style=\"width: 940px\" class=\"wp-caption alignleft\"><img aria-describedby=\"caption-attachment-1980\" decoding=\"async\" loading=\"lazy\" class=\"size-full wp-image-1980\" src=\"http:\/\/oceanweatherservices.com\/blog\/wp-content\/uploads\/2018\/06\/sst-may.jpg\" alt=\"\" width=\"930\" height=\"580\" srcset=\"https:\/\/oceanweatherservices.com\/blog\/wp-content\/uploads\/2018\/06\/sst-may.jpg 930w, https:\/\/oceanweatherservices.com\/blog\/wp-content\/uploads\/2018\/06\/sst-may-300x187.jpg 300w, https:\/\/oceanweatherservices.com\/blog\/wp-content\/uploads\/2018\/06\/sst-may-768x479.jpg 768w\" sizes=\"(max-width: 930px) 100vw, 930px\" \/><p id=\"caption-attachment-1980\" class=\"wp-caption-text\">Sea Surface Temperature Anomaly May 2018<\/p><\/div>\n","protected":false},"excerpt":{"rendered":"<p>The main tropical development area for the North Atlantic continues to cool relative to recent averages suggesting a stronger than normal Bermuda-Azores ridge.\u00a0When this high pressure ridge is stronger or displaced west, as it appears to be now, tropical storm &hellip; <a href=\"https:\/\/oceanweatherservices.com\/blog\/2018\/06\/01\/north-atlantic-cooling-will-affect-hurricane-season\/\">Continue reading <span class=\"meta-nav\">&rarr;<\/span><\/a><\/p>\n","protected":false},"author":1,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":[],"categories":[73,10,102],"tags":[27,9,14],"_links":{"self":[{"href":"https:\/\/oceanweatherservices.com\/blog\/wp-json\/wp\/v2\/posts\/1979"}],"collection":[{"href":"https:\/\/oceanweatherservices.com\/blog\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/oceanweatherservices.com\/blog\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/oceanweatherservices.com\/blog\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/oceanweatherservices.com\/blog\/wp-json\/wp\/v2\/comments?post=1979"}],"version-history":[{"count":6,"href":"https:\/\/oceanweatherservices.com\/blog\/wp-json\/wp\/v2\/posts\/1979\/revisions"}],"predecessor-version":[{"id":1988,"href":"https:\/\/oceanweatherservices.com\/blog\/wp-json\/wp\/v2\/posts\/1979\/revisions\/1988"}],"wp:attachment":[{"href":"https:\/\/oceanweatherservices.com\/blog\/wp-json\/wp\/v2\/media?parent=1979"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/oceanweatherservices.com\/blog\/wp-json\/wp\/v2\/categories?post=1979"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/oceanweatherservices.com\/blog\/wp-json\/wp\/v2\/tags?post=1979"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}