{"id":3214,"date":"2022-03-06T15:22:03","date_gmt":"2022-03-06T20:22:03","guid":{"rendered":"http:\/\/oceanweatherservices.com\/blog\/?p=3214"},"modified":"2022-03-06T15:23:22","modified_gmt":"2022-03-06T20:23:22","slug":"north-pacific-marine-weather-outlook-6","status":"publish","type":"post","link":"https:\/\/oceanweatherservices.com\/blog\/2022\/03\/06\/north-pacific-marine-weather-outlook-6\/","title":{"rendered":"North Pacific Marine Weather Outlook"},"content":{"rendered":"<div id=\"attachment_3215\" style=\"width: 465px\" class=\"wp-caption alignleft\"><a href=\"http:\/\/oceanweatherservices.com\/blog\/wp-content\/uploads\/2022\/03\/temp-0-.jpg\"><img aria-describedby=\"caption-attachment-3215\" decoding=\"async\" loading=\"lazy\" class=\" wp-image-3215\" src=\"http:\/\/oceanweatherservices.com\/blog\/wp-content\/uploads\/2022\/03\/temp-0--300x192.jpg\" alt=\"\" width=\"455\" height=\"291\" srcset=\"https:\/\/oceanweatherservices.com\/blog\/wp-content\/uploads\/2022\/03\/temp-0--300x192.jpg 300w, https:\/\/oceanweatherservices.com\/blog\/wp-content\/uploads\/2022\/03\/temp-0--768x491.jpg 768w, https:\/\/oceanweatherservices.com\/blog\/wp-content\/uploads\/2022\/03\/temp-0-.jpg 959w\" sizes=\"(max-width: 455px) 100vw, 455px\" \/><\/a><p id=\"caption-attachment-3215\" class=\"wp-caption-text\">NOAA OPC 500 mb Forecast Chart<\/p><\/div>\n<p><span style=\"font-weight: 400;\">A blocking ridge has re-established itself over the eastern North Pacific, effectively shunting storm tracks from the western North Pacific northward towards the eastern Bering Sea. At the same time, a large semi stationary upper-level and surface level low prevail over the northwestern North Pacific which continues to depress the prevailing jet and storm tracks south of 40 N over the western North Pacific.\u00a0<\/span><\/p>\n<div id=\"attachment_3216\" style=\"width: 632px\" class=\"wp-caption alignleft\"><a href=\"http:\/\/oceanweatherservices.com\/blog\/wp-content\/uploads\/2022\/03\/temp-1-.jpg\"><img aria-describedby=\"caption-attachment-3216\" decoding=\"async\" loading=\"lazy\" class=\" wp-image-3216\" src=\"http:\/\/oceanweatherservices.com\/blog\/wp-content\/uploads\/2022\/03\/temp-1-.jpg\" alt=\"\" width=\"622\" height=\"390\" srcset=\"https:\/\/oceanweatherservices.com\/blog\/wp-content\/uploads\/2022\/03\/temp-1-.jpg 967w, https:\/\/oceanweatherservices.com\/blog\/wp-content\/uploads\/2022\/03\/temp-1--300x188.jpg 300w, https:\/\/oceanweatherservices.com\/blog\/wp-content\/uploads\/2022\/03\/temp-1--768x482.jpg 768w\" sizes=\"(max-width: 622px) 100vw, 622px\" \/><\/a><p id=\"caption-attachment-3216\" class=\"wp-caption-text\">NOAA OPC 48 hour Surface Forecast<\/p><\/div>\n<p>&nbsp;<\/p>\n<p><span style=\"font-weight: 400;\">The eastern ridge is expected to gradually weaken and drift southeastward later this week.<\/span><\/p>\n","protected":false},"excerpt":{"rendered":"<p>A blocking ridge has re-established itself over the eastern North Pacific, effectively shunting storm tracks from the western North Pacific northward towards the eastern Bering Sea.  <a href=\"https:\/\/oceanweatherservices.com\/blog\/2022\/03\/06\/north-pacific-marine-weather-outlook-6\/\">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":[169,57],"tags":[19,5,11],"_links":{"self":[{"href":"https:\/\/oceanweatherservices.com\/blog\/wp-json\/wp\/v2\/posts\/3214"}],"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=3214"}],"version-history":[{"count":3,"href":"https:\/\/oceanweatherservices.com\/blog\/wp-json\/wp\/v2\/posts\/3214\/revisions"}],"predecessor-version":[{"id":3219,"href":"https:\/\/oceanweatherservices.com\/blog\/wp-json\/wp\/v2\/posts\/3214\/revisions\/3219"}],"wp:attachment":[{"href":"https:\/\/oceanweatherservices.com\/blog\/wp-json\/wp\/v2\/media?parent=3214"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/oceanweatherservices.com\/blog\/wp-json\/wp\/v2\/categories?post=3214"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/oceanweatherservices.com\/blog\/wp-json\/wp\/v2\/tags?post=3214"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}