{"id":10645,"date":"2025-07-25T11:31:11","date_gmt":"2025-07-25T03:31:11","guid":{"rendered":"https:\/\/exps.pccu.edu.tw\/exprs\/?post_type=experiment_iop&#038;p=10645"},"modified":"2025-07-25T11:31:28","modified_gmt":"2025-07-25T03:31:28","slug":"iop8-3","status":"publish","type":"experiment_iop","link":"https:\/\/exps.pccu.edu.tw\/exprs\/experiment_iop\/iop8-3\/","title":{"rendered":"IOP8"},"content":{"rendered":"\n<p>The ground-based Doppler radars first observed intense convection developing over the Central Mountain range of Taiwan and monitored the convection as it moved eastward. During the night, the radars observed and collected data on a prefrontal band of convection that developed over the straits and moved over northern Taiwan. Finally, during the second day, the Doppler radars collected data in a second band of convection associated with the surface front, as it passed over the island.<\/p>\n","protected":false},"template":"","iop_summary_tag":[73,112],"class_list":["post-10645","experiment_iop","type-experiment_iop","status-publish","hentry","iop_summary_tag-front","iop_summary_tag-mountain-convection"],"_links":{"self":[{"href":"https:\/\/exps.pccu.edu.tw\/exprs\/wp-json\/wp\/v2\/experiment_iop\/10645","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/exps.pccu.edu.tw\/exprs\/wp-json\/wp\/v2\/experiment_iop"}],"about":[{"href":"https:\/\/exps.pccu.edu.tw\/exprs\/wp-json\/wp\/v2\/types\/experiment_iop"}],"wp:attachment":[{"href":"https:\/\/exps.pccu.edu.tw\/exprs\/wp-json\/wp\/v2\/media?parent=10645"}],"wp:term":[{"taxonomy":"iop_summary_tag","embeddable":true,"href":"https:\/\/exps.pccu.edu.tw\/exprs\/wp-json\/wp\/v2\/iop_summary_tag?post=10645"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}