{"id":10640,"date":"2025-07-24T17:11:13","date_gmt":"2025-07-24T09:11:13","guid":{"rendered":"https:\/\/exps.pccu.edu.tw\/exprs\/?post_type=experiment_iop&#038;p=10640"},"modified":"2025-07-24T17:11:13","modified_gmt":"2025-07-24T09:11:13","slug":"iop3-3","status":"publish","type":"experiment_iop","link":"https:\/\/exps.pccu.edu.tw\/exprs\/experiment_iop\/iop3-3\/","title":{"rendered":"IOP3"},"content":{"rendered":"\n<p>During the first day of this two day IOP, the aircraft flew a low-level jet pattern, and then a circumnavigation pattern around Taiwan, after no convection had developed in response to the passage of the Mei-Yu front over Taiwan. A few small convective cells developed over the straits and were observed by the ground-based Doppler radars. On the second day of the IOP, a second aircraft mission was flown to investigate the structure of a weak squall line that had developed over the straits and was moving towards the southernmost part of Taiwan. The aircraft was able to make several &#8220;L&#8221; patterns and some in-cloud measurements before the system completely fell apart and moved onshore.<\/p>\n","protected":false},"template":"","iop_summary_tag":[73,111],"class_list":["post-10640","experiment_iop","type-experiment_iop","status-publish","hentry","iop_summary_tag-front","iop_summary_tag-low-level-jet"],"_links":{"self":[{"href":"https:\/\/exps.pccu.edu.tw\/exprs\/wp-json\/wp\/v2\/experiment_iop\/10640","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=10640"}],"wp:term":[{"taxonomy":"iop_summary_tag","embeddable":true,"href":"https:\/\/exps.pccu.edu.tw\/exprs\/wp-json\/wp\/v2\/iop_summary_tag?post=10640"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}