{"id":77860,"date":"2026-08-25T11:47:51","date_gmt":"2026-08-25T11:47:51","guid":{"rendered":"https:\/\/lisbonsightsailing.com\/?post_type=glossario&#038;p=77860"},"modified":"2026-08-26T16:36:22","modified_gmt":"2026-08-26T16:36:22","slug":"warm-front","status":"publish","type":"glossario","link":"https:\/\/lisbonsightsailing.com\/en\/glossario\/warm-front\/","title":{"rendered":"Warm Front"},"content":{"rendered":"\n<p class=\"wp-block-paragraph\">This occurs when a mass of warm, less dense air advances, overriding a retreating mass of cold air. Because warm air is lighter, it rises smoothly and gradually over the slope of cold air, causing a slower and more continuous weather transition. It begins with high clouds (<em>Cirrus<\/em>) and evolves into low, dense clouds (<em>Nimbostratus<\/em>), resulting in moderate, continuous, and prolonged rainfall (reduced visibility or fog), followed by a rise in temperature.  <\/p>\n","protected":false},"featured_media":0,"template":"","meta":{"_acf_changed":false},"tema-glossario":[2493],"tema-da-pergunta":[],"class_list":["post-77860","glossario","type-glossario","status-publish","hentry","tema-glossario-navigation"],"acf":[],"_links":{"self":[{"href":"https:\/\/lisbonsightsailing.com\/en\/wp-json\/wp\/v2\/glossario\/77860","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/lisbonsightsailing.com\/en\/wp-json\/wp\/v2\/glossario"}],"about":[{"href":"https:\/\/lisbonsightsailing.com\/en\/wp-json\/wp\/v2\/types\/glossario"}],"wp:attachment":[{"href":"https:\/\/lisbonsightsailing.com\/en\/wp-json\/wp\/v2\/media?parent=77860"}],"wp:term":[{"taxonomy":"tema-glossario","embeddable":true,"href":"https:\/\/lisbonsightsailing.com\/en\/wp-json\/wp\/v2\/tema-glossario?post=77860"},{"taxonomy":"tema-da-pergunta","embeddable":true,"href":"https:\/\/lisbonsightsailing.com\/en\/wp-json\/wp\/v2\/tema-da-pergunta?post=77860"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}