{"id":4257,"date":"2020-12-01T08:04:58","date_gmt":"2020-12-01T08:04:58","guid":{"rendered":"http:\/\/www.iersd.noa.gr\/?post_type=publications&p=4257"},"modified":"2021-12-06T09:58:47","modified_gmt":"2021-12-06T09:58:47","slug":"Kokkalis-P-Alexiou-D-Papayannis-A-Rocadenbosch-F-Soupiona-O-Raptis-PI-Mylonaki-M-Tzanis-CG-Christodoulakis-J-Application-and-Testing-of-the-Extended-K","status":"publish","type":"publications","link":"https:\/\/www.iersd.noa.gr\/en\/publications\/Kokkalis-P-Alexiou-D-Papayannis-A-Rocadenbosch-F-Soupiona-O-Raptis-PI-Mylonaki-M-Tzanis-CG-Christodoulakis-J-Application-and-Testing-of-the-Extended-K\/","title":{"rendered":"Kokkalis P., Alexiou D., Papayannis A., Rocadenbosch F., Soupiona O., Raptis P.I., Mylonaki M., Tzanis C.G., Christodoulakis J., Application and Testing of the Extended-Kalman-Filtering Technique for Determining the Planetary Boundary-Layer Height over Athens, Greece, Boundary-Layer Meteorology, 176(1), 2020, 125-147, 2020. DOI: 10.1007\/s10546-020-00514-z"},"content":{"rendered":"","protected":false},"template":"","meta":{"_acf_changed":false,"footnotes":""},"class_list":["post-4257","publications","type-publications","status-publish","hentry"],"acf":[],"_links":{"self":[{"href":"https:\/\/www.iersd.noa.gr\/en\/wp-json\/wp\/v2\/publications\/4257","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\/4257\/revisions"}],"wp:attachment":[{"href":"https:\/\/www.iersd.noa.gr\/en\/wp-json\/wp\/v2\/media?parent=4257"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}