{"id":10639,"date":"2025-07-24T16:50:40","date_gmt":"2025-07-24T08:50:40","guid":{"rendered":"https:\/\/exps.pccu.edu.tw\/exprs\/?post_type=experiment_iop&#038;p=10639"},"modified":"2025-07-24T16:50:40","modified_gmt":"2025-07-24T08:50:40","slug":"iop2-4","status":"publish","type":"experiment_iop","link":"https:\/\/exps.pccu.edu.tw\/exprs\/experiment_iop\/iop2-4\/","title":{"rendered":"IOP2"},"content":{"rendered":"\n<p>A weak squall line developed over the Taiwan straits and moved toward central and southern Taiwan. The P-3 aircraft reached the squall line just before it moved on-shore. The airborne Doppler radar did not operate. The ground-based Doppler radars collected some excellent data on the northern portion of the line as it moved on-shore. The aircraft then flew to a meso-low that had developed on the east side of the island and then flew north and sampled a pre-frontal and frontal squall line that had developed over the ocean, just north of Taiwan.<\/p>\n","protected":false},"template":"","iop_summary_tag":[73,111,74],"class_list":["post-10639","experiment_iop","type-experiment_iop","status-publish","hentry","iop_summary_tag-front","iop_summary_tag-low-level-jet","iop_summary_tag-mcs"],"_links":{"self":[{"href":"https:\/\/exps.pccu.edu.tw\/exprs\/wp-json\/wp\/v2\/experiment_iop\/10639","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=10639"}],"wp:term":[{"taxonomy":"iop_summary_tag","embeddable":true,"href":"https:\/\/exps.pccu.edu.tw\/exprs\/wp-json\/wp\/v2\/iop_summary_tag?post=10639"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}