{"id":1299,"date":"2014-01-01T00:00:00","date_gmt":"2014-01-01T00:00:00","guid":{"rendered":"http:\/\/localhost\/meteo\/publications\/papoutsa-c-retalis-a-toulios-l-and-hadjimitsis-d-defining-the-landsat-tm-etm-and-chris-proba-spectral-regions-in-which-turbidity-can-be-retrieved-in-inland-water-body-using-field-spectroscopy\/"},"modified":"2014-01-01T00:00:00","modified_gmt":"2014-01-01T00:00:00","slug":"papoutsa-c-retalis-a-toulios-l-and-hadjimitsis-d-defining-the-landsat-tm-etm-and-chris-proba-spectral-regions-in-which-turbidity-can-be-retrieved-in-inland-water-body-using-field-spectroscopy","status":"publish","type":"publications","link":"https:\/\/www.iersd.noa.gr\/en\/publications\/papoutsa-c-retalis-a-toulios-l-and-hadjimitsis-d-defining-the-landsat-tm-etm-and-chris-proba-spectral-regions-in-which-turbidity-can-be-retrieved-in-inland-water-body-using-field-spectroscopy\/","title":{"rendered":"Papoutsa C., Retalis A., Toulios L. and Hadjimitsis D.: Defining the Landsat TM\/ETM+ and CHRIS\/PROBA spectral regions in which turbidity can be retrieved in inland water body using field spectroscopy, International Journal of Remote Sensing Vol 35 (5) p.1674-1692 Doi: 10.1080\/01431161.2014.882029, 2014"},"content":{"rendered":"","protected":false},"template":"","meta":{"_acf_changed":false,"footnotes":""},"class_list":["post-1299","publications","type-publications","status-publish","hentry"],"acf":[],"_links":{"self":[{"href":"https:\/\/www.iersd.noa.gr\/en\/wp-json\/wp\/v2\/publications\/1299","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\/1299\/revisions"}],"wp:attachment":[{"href":"https:\/\/www.iersd.noa.gr\/en\/wp-json\/wp\/v2\/media?parent=1299"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}