{"id":1126,"date":"2016-01-01T00:00:00","date_gmt":"2016-01-01T00:00:00","guid":{"rendered":"http:\/\/localhost\/meteo\/publications\/proestakis-e-kazadzis-s-lagouvardos-k-kotroni-v-amiridis-v-marinou-e-price-c-and-kazantzidis-a-aerosols-and-lightning-activity-the-effect-of-vertical-profile-and-aerosol-type-atmosphe\/"},"modified":"2016-01-01T00:00:00","modified_gmt":"2016-01-01T00:00:00","slug":"proestakis-e-kazadzis-s-lagouvardos-k-kotroni-v-amiridis-v-marinou-e-price-c-and-kazantzidis-a-aerosols-and-lightning-activity-the-effect-of-vertical-profile-and-aerosol-type-atmosphe","status":"publish","type":"publications","link":"https:\/\/www.iersd.noa.gr\/en\/publications\/proestakis-e-kazadzis-s-lagouvardos-k-kotroni-v-amiridis-v-marinou-e-price-c-and-kazantzidis-a-aerosols-and-lightning-activity-the-effect-of-vertical-profile-and-aerosol-type-atmosphe\/","title":{"rendered":"Proestakis E., Kazadzis S., Lagouvardos K., Kotroni V.,Amiridis V., Marinou E., Price C. and Kazantzidis A. : Aerosols and lightning activity: The effect of vertical profile and aerosol type, Atmospheric Research Vol 182 p.243-255 Doi: 10.1016\/j.atmosres.2016.07.031, 2016"},"content":{"rendered":"","protected":false},"template":"","meta":{"_acf_changed":false,"footnotes":""},"class_list":["post-1126","publications","type-publications","status-publish","hentry"],"acf":[],"_links":{"self":[{"href":"https:\/\/www.iersd.noa.gr\/en\/wp-json\/wp\/v2\/publications\/1126","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\/1126\/revisions"}],"wp:attachment":[{"href":"https:\/\/www.iersd.noa.gr\/en\/wp-json\/wp\/v2\/media?parent=1126"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}