{"id":10648,"date":"2025-07-25T11:40:22","date_gmt":"2025-07-25T03:40:22","guid":{"rendered":"https:\/\/exps.pccu.edu.tw\/exprs\/?post_type=experiment_iop&#038;p=10648"},"modified":"2025-07-25T11:40:22","modified_gmt":"2025-07-25T03:40:22","slug":"iop11-3","status":"publish","type":"experiment_iop","link":"https:\/\/exps.pccu.edu.tw\/exprs\/experiment_iop\/iop11-3\/","title":{"rendered":"IOP11"},"content":{"rendered":"\n<p>During the P-3 topographic mission the ground-based Doppler radars observed two periods of organized convection over northwest Taiwan. During the second event, while the P-3 was flying the topographic pattern, the aircraft collected Doppler radar data in the vicinity of the ground-based Dopplers. Thus, there is about a one-hour period in which triple Doppler radar data is available. After the system dissipated, the aircraft completed its circumnavigation mission.<\/p>\n","protected":false},"template":"","iop_summary_tag":[],"class_list":["post-10648","experiment_iop","type-experiment_iop","status-publish","hentry"],"_links":{"self":[{"href":"https:\/\/exps.pccu.edu.tw\/exprs\/wp-json\/wp\/v2\/experiment_iop\/10648","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=10648"}],"wp:term":[{"taxonomy":"iop_summary_tag","embeddable":true,"href":"https:\/\/exps.pccu.edu.tw\/exprs\/wp-json\/wp\/v2\/iop_summary_tag?post=10648"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}