{"id":6200,"date":"2025-02-21T13:12:12","date_gmt":"2025-02-21T13:12:12","guid":{"rendered":"https:\/\/www.iersd.noa.gr\/publications\/harry-d-kambezidis-basil-e-psiloglou-ariadne-gavriil-kalliopi-petrinoli-detection-of-upper-and-lower-planetary-boundary-layer-curves-and-estimation-of-their-heights-from-ceilometer-observations\/"},"modified":"2025-04-02T08:41:21","modified_gmt":"2025-04-02T08:41:21","slug":"harry-d-kambezidis-basil-e-psiloglou-ariadne-gavriil-kalliopi-petrinoli-detection-of-upper-and-lower-planetary-boundary-layer-curves-and-estimation-of-their-heights-from-ceilometer-observations","status":"publish","type":"publications","link":"https:\/\/www.iersd.noa.gr\/en\/publications\/harry-d-kambezidis-basil-e-psiloglou-ariadne-gavriil-kalliopi-petrinoli-detection-of-upper-and-lower-planetary-boundary-layer-curves-and-estimation-of-their-heights-from-ceilometer-observations\/","title":{"rendered":"Harry D. Kambezidis, Basil E. Psiloglou, Ariadne Gavriil, Kalliopi Petrinoli, Detection of Upper and Lower Planetary-Boundary Layer Curves and Estimation of Their Heights from Ceilometer Observations under All-Weather Conditions: Case of Athens, Greece, Remote Sensing,2023. DOI: 10.3390\/rs13112175"},"content":{"rendered":"","protected":false},"template":"","meta":{"_acf_changed":false,"footnotes":""},"class_list":["post-6200","publications","type-publications","status-publish","hentry"],"acf":[],"_links":{"self":[{"href":"https:\/\/www.iersd.noa.gr\/en\/wp-json\/wp\/v2\/publications\/6200","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/www.iersd.noa.gr\/en\/wp-json\/wp\/v2\/publications"}],"about":[{"href":"https:\/\/www.iersd.noa.gr\/en\/wp-json\/wp\/v2\/types\/publications"}],"version-history":[{"count":0,"href":"https:\/\/www.iersd.noa.gr\/en\/wp-json\/wp\/v2\/publications\/6200\/revisions"}],"wp:attachment":[{"href":"https:\/\/www.iersd.noa.gr\/en\/wp-json\/wp\/v2\/media?parent=6200"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}