{"id":18940,"date":"2021-06-10T16:47:43","date_gmt":"2021-06-10T21:47:43","guid":{"rendered":"https:\/\/inside.nssl.noaa.gov\/ewp\/?p=18940"},"modified":"2021-06-22T13:48:47","modified_gmt":"2021-06-22T18:48:47","slug":"using-optical-wind-flow","status":"publish","type":"post","link":"https:\/\/inside.nssl.noaa.gov\/ewp\/2021\/06\/10\/using-optical-wind-flow\/","title":{"rendered":"Using Optical Wind Flow"},"content":{"rendered":"<p><em>Illustrating how this product can be used during the convective season for different wind fields from the boundary layer, up to the jet stream level.<\/em><\/p>\n<figure style=\"width: 904px\" class=\"wp-caption alignnone\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/lh5.googleusercontent.com\/W4cB-PdHEz1aKge6-JK_zz73h48Sei2N_x_xI-DAXk7RS3N5TqfegnXJEZG7sy8osl8ZOQNM2GPj4FXPHuv195DheL2el-GdMaapKNcsjc1yIBAr8pXaajh6OHtvpUtCFsema8Tr\" alt=\"\" width=\"904\" height=\"936\" \/><figcaption class=\"wp-caption-text\">Mid To Upper Level Winds &#8211; Using it for speed, direction and divergence aloft<\/figcaption><\/figure>\n<figure style=\"width: 902px\" class=\"wp-caption alignnone\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/lh5.googleusercontent.com\/etX1OFnzXkksmv2OyYotdky_rkJ31KGgxRhAp1mX8WZb0N7Pq5elIYi8IEC-6pLyo21Ww-y1U_on91eOLroxEIgitDPD-hdDepiGhLdTLDTknHVpCWCm7wVie64fXADC6z8dZti5\" alt=\"\" width=\"902\" height=\"939\" \/><figcaption class=\"wp-caption-text\">All Winds &#8211; Can be used for Low Level Jet and boundaries.<\/figcaption><\/figure>\n<p><img decoding=\"async\" title=\"\" src=\"https:\/\/lh3.googleusercontent.com\/TOoCq7CjXFEmE0fni7HfSXxaPV3SReKU4jG_vLZFDGncRhKwCwjXp-DfjU89eED1C7dpwWgE_-B2kdMk9cypClm1k_EyUX66wf2TsVvQz0LEO_dOTVjzqBCjKgKfzCO_xT_HMdA9\" alt=\"\" \/><\/p>\n<p><img decoding=\"async\" title=\"\" src=\"https:\/\/lh5.googleusercontent.com\/vYrh3L_R-IiRiVG8QbbJDtE-Uc2t99DiuIpH7upkzFsYLoS7NFM5-kvhgn8sigrv7XAekyF4PUbtkE1WQjwmcjw3RbbcSWKnD1kQ8bFfaflRZBqc2edNCRDFGgV5uuoNC9xbrOu7\" alt=\"\" \/><\/p>\n<p><span style=\"font-weight: 400\">&#8211; wxboy65<\/span><\/p>\n","protected":false},"excerpt":{"rendered":"<p>Illustrating how this product can be used during the convective season for different wind fields from the boundary layer, up to the jet stream level. &#8211; wxboy65<\/p>\n","protected":false},"author":181,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[82],"tags":[],"class_list":["post-18940","post","type-post","status-publish","format-standard","hentry","category-optical-flow-winds"],"_links":{"self":[{"href":"https:\/\/inside.nssl.noaa.gov\/ewp\/wp-json\/wp\/v2\/posts\/18940","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/inside.nssl.noaa.gov\/ewp\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/inside.nssl.noaa.gov\/ewp\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/inside.nssl.noaa.gov\/ewp\/wp-json\/wp\/v2\/users\/181"}],"replies":[{"embeddable":true,"href":"https:\/\/inside.nssl.noaa.gov\/ewp\/wp-json\/wp\/v2\/comments?post=18940"}],"version-history":[{"count":2,"href":"https:\/\/inside.nssl.noaa.gov\/ewp\/wp-json\/wp\/v2\/posts\/18940\/revisions"}],"predecessor-version":[{"id":18945,"href":"https:\/\/inside.nssl.noaa.gov\/ewp\/wp-json\/wp\/v2\/posts\/18940\/revisions\/18945"}],"wp:attachment":[{"href":"https:\/\/inside.nssl.noaa.gov\/ewp\/wp-json\/wp\/v2\/media?parent=18940"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/inside.nssl.noaa.gov\/ewp\/wp-json\/wp\/v2\/categories?post=18940"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/inside.nssl.noaa.gov\/ewp\/wp-json\/wp\/v2\/tags?post=18940"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}