{"id":4481,"date":"2021-12-06T11:27:54","date_gmt":"2021-12-06T11:27:54","guid":{"rendered":"http:\/\/www.iersd.noa.gr\/?post_type=publications&#038;p=4481"},"modified":"2021-12-06T11:27:54","modified_gmt":"2021-12-06T11:27:54","slug":"kambezidis-h-d-psiloglou-b-e-gavriil-a-petrinoli-k-detection-of-upper-and-lower-planetary-boundary-layer-curves-and-estimation-of-their-heights-from-ceilometer-observations-under-all-weather","status":"publish","type":"publications","link":"https:\/\/www.iersd.noa.gr\/en\/publications\/kambezidis-h-d-psiloglou-b-e-gavriil-a-petrinoli-k-detection-of-upper-and-lower-planetary-boundary-layer-curves-and-estimation-of-their-heights-from-ceilometer-observations-under-all-weather\/","title":{"rendered":"Kambezidis H.D., Psiloglou B. E., Gavriil  A., Petrinoli K., 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, 13,  2175-2204, 2021. DOI: 10.3390\/rs13112175"},"content":{"rendered":"","protected":false},"template":"","meta":{"_acf_changed":false,"footnotes":""},"class_list":["post-4481","publications","type-publications","status-publish","hentry"],"acf":[],"_links":{"self":[{"href":"https:\/\/www.iersd.noa.gr\/en\/wp-json\/wp\/v2\/publications\/4481","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\/4481\/revisions"}],"wp:attachment":[{"href":"https:\/\/www.iersd.noa.gr\/en\/wp-json\/wp\/v2\/media?parent=4481"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}