Please use this identifier to cite or link to this item: https://hdl.handle.net/20.500.14279/4465
DC FieldValueLanguage
dc.contributor.authorHadjimitsis, Diofantos G.-
dc.contributor.authorAgapiou, Athos-
dc.date.accessioned2012-10-22T06:16:17Zen
dc.date.accessioned2013-05-17T10:30:51Z-
dc.date.accessioned2015-12-09T13:51:46Z-
dc.date.available2012-10-22T06:16:17Zen
dc.date.available2013-05-17T10:30:51Z-
dc.date.available2015-12-09T13:51:46Z-
dc.date.issued2011-
dc.identifier.citationJournal of applied remote sensing, 2011, vol. 5, νο. 1en_US
dc.identifier.issn19313195-
dc.identifier.urihttps://hdl.handle.net/20.500.14279/4465-
dc.description.abstractThis study presents an alternative approach for detecting possible archaeological crop marks using medium multitemporal resolution satellite data and field spectroscopy measurements during a whole phenological cycle of the crops and normalized difference vegetation index (NDVI) values. Geophysical surveys have been carried out on areas where archaeological remains with crops existed for validation and verification. The study presents the results obtained by applying the NDVI for a series of multitemporal Landsat TM/ETM+ images acquired from June 2009 to June 2010, intended for detecting archaeological crop marks in the Paphos District area in Cyprus. The results were validated using in situ spectroradiometric measurements using the GER 1500 field spectroradiometer. The authors compared the NDVI values between three sites in which barley crop is cultivated during a complete phenological cycle. The first site was a known archaeological area (Site 1), while the other two sites were healthy cultivated areas (Sites 2 and 3). The sites had similar soil and climatic characteristics. It has been found that during the phenological cycle, the NDVI plot for Site 1 was significantly different from the healthy areas. The detection of possible archaeological areas was based on anomalies observed and measured on vegetation indices, during the phenological cycle, of the “stressed” barley compared to healthy “nonstressed” barley in all three sites. At the end of the life cycle (after June 2010), the local authorities commenced excavation work at Site 1. Buried archaeological remains, 20 to 30 cm below ground surface were found. Anomalies found in the NDVI phenological cycle, as in Site 1, could be used for detecting areas with buried archeological remainsen_US
dc.formatpdfen_US
dc.language.isoenen_US
dc.relation.ispartofJournal of Applied Remote Sensingen_US
dc.rights© SPIEen_US
dc.subjectΑrchaeological crop marksen_US
dc.subjectΒuried archaeological remainsen_US
dc.subjectPhenological cycleen_US
dc.subjectSpectral signature anomaliesen_US
dc.subjectSpectroradiometric measurementsen_US
dc.titleVegetation indices and field spectroradiometric measurements for validation of buried architectural remains: verification under area surveyed with geophysical campaignsen_US
dc.typeArticleen_US
dc.collaborationCyprus University of Technologyen_US
dc.subject.categoryCivil Engineeringen_US
dc.journalsSubscriptionen_US
dc.reviewpeer reviewed-
dc.countryCyprusen_US
dc.subject.fieldEngineering and Technologyen_US
dc.publicationPeer Revieweden_US
dc.identifier.doi10.1117/1.3645590en_US
dc.dept.handle123456789/148en
dc.relation.issue1en_US
dc.relation.volume5en_US
cut.common.academicyear2010-2011en_US
item.openairetypearticle-
item.cerifentitytypePublications-
item.fulltextNo Fulltext-
item.grantfulltextnone-
item.openairecristypehttp://purl.org/coar/resource_type/c_6501-
item.languageiso639-1en-
crisitem.author.deptDepartment of Civil Engineering and Geomatics-
crisitem.author.deptDepartment of Civil Engineering and Geomatics-
crisitem.author.facultyFaculty of Engineering and Technology-
crisitem.author.facultyFaculty of Engineering and Technology-
crisitem.author.orcid0000-0002-2684-547X-
crisitem.author.orcid0000-0001-9106-6766-
crisitem.author.parentorgFaculty of Engineering and Technology-
crisitem.author.parentorgFaculty of Engineering and Technology-
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