{"id":3105,"date":"2022-02-07T10:08:07","date_gmt":"2022-02-07T15:08:07","guid":{"rendered":"http:\/\/oceanweatherservices.com\/blog\/?p=3105"},"modified":"2022-02-07T10:09:04","modified_gmt":"2022-02-07T15:09:04","slug":"north-pacific-marine-weather-outlook-2","status":"publish","type":"post","link":"https:\/\/oceanweatherservices.com\/blog\/2022\/02\/07\/north-pacific-marine-weather-outlook-2\/","title":{"rendered":"North Pacific Marine Weather Outlook"},"content":{"rendered":"<p><span style=\"font-weight: 400;\">The primary jet stream continues to be displaced south of 40 N latitude over the western and central North Pacific then turns northeastward towards the Gulf of Alaska due to a persistent blocking ridge over the easternmost North Pacific.\u00a0<\/span><\/p>\n<div id=\"attachment_3106\" style=\"width: 615px\" class=\"wp-caption alignleft\"><a href=\"http:\/\/oceanweatherservices.com\/blog\/wp-content\/uploads\/2022\/02\/Temp-500-fcst.jpg\"><img aria-describedby=\"caption-attachment-3106\" decoding=\"async\" loading=\"lazy\" class=\" wp-image-3106\" src=\"http:\/\/oceanweatherservices.com\/blog\/wp-content\/uploads\/2022\/02\/Temp-500-fcst.jpg\" alt=\"\" width=\"605\" height=\"383\" srcset=\"https:\/\/oceanweatherservices.com\/blog\/wp-content\/uploads\/2022\/02\/Temp-500-fcst.jpg 962w, https:\/\/oceanweatherservices.com\/blog\/wp-content\/uploads\/2022\/02\/Temp-500-fcst-300x190.jpg 300w, https:\/\/oceanweatherservices.com\/blog\/wp-content\/uploads\/2022\/02\/Temp-500-fcst-768x486.jpg 768w\" sizes=\"(max-width: 605px) 100vw, 605px\" \/><\/a><p id=\"caption-attachment-3106\" class=\"wp-caption-text\">NOAA OPC 500mb Forecast Track<\/p><\/div>\n<p>&nbsp;<\/p>\n<p><span style=\"font-weight: 400;\">As a result the primary storm tracks will be from south of Japan to near 42N\/180 then northeast over the Gulf of Alaska. Frequent gale to storm westerlies likely south of low pressure centers with brief intervals of hurricane-force conditions possible, especially in the central North Pacific.<\/span><\/p>\n<div id=\"attachment_3107\" style=\"width: 611px\" class=\"wp-caption alignnone\"><a href=\"http:\/\/oceanweatherservices.com\/blog\/wp-content\/uploads\/2022\/02\/temp-48hr-sfc-1.jpg\"><img aria-describedby=\"caption-attachment-3107\" decoding=\"async\" loading=\"lazy\" class=\" wp-image-3107\" src=\"http:\/\/oceanweatherservices.com\/blog\/wp-content\/uploads\/2022\/02\/temp-48hr-sfc-1.jpg\" alt=\"\" width=\"601\" height=\"382\" srcset=\"https:\/\/oceanweatherservices.com\/blog\/wp-content\/uploads\/2022\/02\/temp-48hr-sfc-1.jpg 957w, https:\/\/oceanweatherservices.com\/blog\/wp-content\/uploads\/2022\/02\/temp-48hr-sfc-1-300x191.jpg 300w, https:\/\/oceanweatherservices.com\/blog\/wp-content\/uploads\/2022\/02\/temp-48hr-sfc-1-768x489.jpg 768w\" sizes=\"(max-width: 601px) 100vw, 601px\" \/><\/a><p id=\"caption-attachment-3107\" class=\"wp-caption-text\">NOAA OPC Surface Forecast<\/p><\/div>\n","protected":false},"excerpt":{"rendered":"<p>The primary jet stream continues to be displaced south of 40 N latitude over the western and central North Pacific then turns northeastward towards the Gulf of Alaska due to a persistent blocking ridge over the easternmost North Pacific.\u00a0 <a href=\"https:\/\/oceanweatherservices.com\/blog\/2022\/02\/07\/north-pacific-marine-weather-outlook-2\/\">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":[169,3,167,57],"tags":[28,19,5,6,11],"_links":{"self":[{"href":"https:\/\/oceanweatherservices.com\/blog\/wp-json\/wp\/v2\/posts\/3105"}],"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=3105"}],"version-history":[{"count":2,"href":"https:\/\/oceanweatherservices.com\/blog\/wp-json\/wp\/v2\/posts\/3105\/revisions"}],"predecessor-version":[{"id":3109,"href":"https:\/\/oceanweatherservices.com\/blog\/wp-json\/wp\/v2\/posts\/3105\/revisions\/3109"}],"wp:attachment":[{"href":"https:\/\/oceanweatherservices.com\/blog\/wp-json\/wp\/v2\/media?parent=3105"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/oceanweatherservices.com\/blog\/wp-json\/wp\/v2\/categories?post=3105"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/oceanweatherservices.com\/blog\/wp-json\/wp\/v2\/tags?post=3105"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}