{"id":10647,"date":"2025-07-25T11:37:32","date_gmt":"2025-07-25T03:37:32","guid":{"rendered":"https:\/\/exps.pccu.edu.tw\/exprs\/?post_type=experiment_iop&#038;p=10647"},"modified":"2025-07-25T11:37:32","modified_gmt":"2025-07-25T03:37:32","slug":"iop10-3","status":"publish","type":"experiment_iop","link":"https:\/\/exps.pccu.edu.tw\/exprs\/experiment_iop\/iop10-3\/","title":{"rendered":"IOP10"},"content":{"rendered":"\n<p>An ocean MCS developed near the southeast coast of Taiwan and slowly moved up the coast over the next 24 hours. The first flight was rapidly developing. The ground-based Doppler radars observed the upper levels of the storm over much of the development stage and its movement northward. The next afternoon, a second flight of the P-3 investigated the structure of a meso-low along the northeast coast of Taiwan that had apparently developed in response to the convective system.<\/p>\n","protected":false},"template":"","iop_summary_tag":[74,110],"class_list":["post-10647","experiment_iop","type-experiment_iop","status-publish","hentry","iop_summary_tag-mcs","iop_summary_tag-mesolow"],"_links":{"self":[{"href":"https:\/\/exps.pccu.edu.tw\/exprs\/wp-json\/wp\/v2\/experiment_iop\/10647","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=10647"}],"wp:term":[{"taxonomy":"iop_summary_tag","embeddable":true,"href":"https:\/\/exps.pccu.edu.tw\/exprs\/wp-json\/wp\/v2\/iop_summary_tag?post=10647"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}