{"id":872,"date":"2020-02-11T16:09:33","date_gmt":"2020-02-11T20:09:33","guid":{"rendered":"https:\/\/www2.whoi.edu\/site\/aomip\/?page_id=872"},"modified":"2021-06-18T09:33:45","modified_gmt":"2021-06-18T13:33:45","slug":"turbulent-heat-fluxes","status":"publish","type":"page","link":"https:\/\/www2.whoi.edu\/site\/aomip\/data\/atmospheric-forcing-data\/turbulent-heat-fluxes\/","title":{"rendered":"Turbulent Heat Fluxes"},"content":{"rendered":"\n\n\t<h1>Turbulent Heat Fluxes<\/h1>\n<p>Turbulent fluxes (<a href=\"https:\/\/www2.whoi.edu\/site\/aomip\/references#Parkinson_1979\">Parkinson and Washington<\/a>, 1979) are defined with the sign convention that an upward directed flux is a positive quantity.<\/p>\n<h2>Sensible<\/h2>\n<p>The sensible heat flux associated with the temperature difference between the air and underlying ocean surface is <img loading=\"lazy\" src=\"https:\/\/www2.whoi.edu\/site\/aomip\/wp-content\/uploads\/sites\/100\/2020\/02\/sensible_ocean_test.jpg\" alt=\"sensible heat flux\" width=\"213\" height=\"33\" \/>.<\/p>\n<p>The sensible heat flux associated with the temperature difference between the air and underlying ice\/snow surface is <img loading=\"lazy\" src=\"https:\/\/www2.whoi.edu\/site\/aomip\/wp-content\/uploads\/sites\/100\/2020\/02\/sensible_ice_84914.jpg\" alt=\"ice\/snow surface \" width=\"215\" height=\"33\" \/>.<\/p>\n<h2>Latent<\/h2>\n<p>The latent heat flux associated with\u00a0<a href=\"https:\/\/www2.whoi.edu\/site\/aomip\/data\/atmospheric-forcing-data\/evaporation-and-precipitation\/\">evaporation<\/a> over the ocean surface is <img loading=\"lazy\" src=\"https:\/\/www2.whoi.edu\/site\/aomip\/wp-content\/uploads\/sites\/100\/2020\/02\/latent_ocean_84913-1.jpg\" alt=\"\" width=\"110\" height=\"30\" \/>.<\/p>\n<p>The latent heat flux associated with\u00a0<a href=\"https:\/\/www2.whoi.edu\/site\/aomip\/data\/atmospheric-forcing-data\/evaporation-and-precipitation\/\">sublimation<\/a>\u00a0over the ice\/snow surface is <img loading=\"lazy\" src=\"https:\/\/www2.whoi.edu\/site\/aomip\/wp-content\/uploads\/sites\/100\/2020\/02\/latent_ice_84912.jpg\" alt=\"Latent Ice\" width=\"108\" height=\"30\" \/>.<\/p>\n\n","protected":false},"excerpt":{"rendered":"<p>Turbulent Heat Fluxes Turbulent fluxes (Parkinson and Washington, 1979) are defined with the sign convention that an upward directed flux is a positive quantity. Sensible The sensible heat flux associated with the temperature difference between the air and underlying ocean surface is . The sensible heat flux associated with the temperature difference between the air&hellip;<\/p>\n","protected":false},"author":83,"featured_media":0,"parent":805,"menu_order":9,"comment_status":"closed","ping_status":"closed","template":"tpl-sidebar.php","meta":{"advanced-sidebar-menu\/link-title":"","advanced-sidebar-menu\/exclude-page":false},"_links":{"self":[{"href":"https:\/\/www2.whoi.edu\/site\/aomip\/wp-json\/wp\/v2\/pages\/872"}],"collection":[{"href":"https:\/\/www2.whoi.edu\/site\/aomip\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/www2.whoi.edu\/site\/aomip\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/www2.whoi.edu\/site\/aomip\/wp-json\/wp\/v2\/users\/83"}],"replies":[{"embeddable":true,"href":"https:\/\/www2.whoi.edu\/site\/aomip\/wp-json\/wp\/v2\/comments?post=872"}],"version-history":[{"count":3,"href":"https:\/\/www2.whoi.edu\/site\/aomip\/wp-json\/wp\/v2\/pages\/872\/revisions"}],"predecessor-version":[{"id":1700,"href":"https:\/\/www2.whoi.edu\/site\/aomip\/wp-json\/wp\/v2\/pages\/872\/revisions\/1700"}],"up":[{"embeddable":true,"href":"https:\/\/www2.whoi.edu\/site\/aomip\/wp-json\/wp\/v2\/pages\/805"}],"wp:attachment":[{"href":"https:\/\/www2.whoi.edu\/site\/aomip\/wp-json\/wp\/v2\/media?parent=872"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}