{"id":1073,"date":"2017-01-01T00:00:00","date_gmt":"2017-01-01T00:00:00","guid":{"rendered":"http:\/\/localhost\/meteo\/publications\/kalkavouras-p-bossioli-e-bezantakos-s-bougiatioti-a-kalivitis-n-stavroulas-i-kouvarakis-g-protonotariou-a-p-dandou-a-biskos-g-mihalopoulos-n-nenes-a-and-tombrou-m-new-partic\/"},"modified":"2017-01-01T00:00:00","modified_gmt":"2017-01-01T00:00:00","slug":"kalkavouras-p-bossioli-e-bezantakos-s-bougiatioti-a-kalivitis-n-stavroulas-i-kouvarakis-g-protonotariou-a-p-dandou-a-biskos-g-mihalopoulos-n-nenes-a-and-tombrou-m-new-partic","status":"publish","type":"publications","link":"https:\/\/www.iersd.noa.gr\/en\/publications\/kalkavouras-p-bossioli-e-bezantakos-s-bougiatioti-a-kalivitis-n-stavroulas-i-kouvarakis-g-protonotariou-a-p-dandou-a-biskos-g-mihalopoulos-n-nenes-a-and-tombrou-m-new-partic\/","title":{"rendered":"Kalkavouras P., Bossioli E., Bezantakos S., Bougiatioti A., Kalivitis N., Stavroulas I., Kouvarakis G., Protonotariou A. P., Dandou A., Biskos G., Mihalopoulos N., Nenes A., and Tombrou M.: New Particle Formation in the South Aegean Sea during the Etesians: importance for CCN production and cloud droplet number , Atmospheric Chemistry and Physics Vol 17 p.175\u2013192"},"content":{"rendered":"","protected":false},"template":"","meta":{"_acf_changed":false,"footnotes":""},"class_list":["post-1073","publications","type-publications","status-publish","hentry"],"acf":[],"_links":{"self":[{"href":"https:\/\/www.iersd.noa.gr\/en\/wp-json\/wp\/v2\/publications\/1073","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\/1073\/revisions"}],"wp:attachment":[{"href":"https:\/\/www.iersd.noa.gr\/en\/wp-json\/wp\/v2\/media?parent=1073"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}