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Adjusting sea level measurements at the port of Alexandroupolis

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dc.contributor.author Maratos, A en
dc.contributor.author Agatza-Balodimou, AM en
dc.contributor.author Antonopoulos, A en
dc.date.accessioned 2014-03-01T01:16:05Z
dc.date.available 2014-03-01T01:16:05Z
dc.date.issued 2001 en
dc.identifier.issn 00396265 en
dc.identifier.uri https://dspace.lib.ntua.gr/xmlui/handle/123456789/13918
dc.relation.uri http://www.scopus.com/inward/record.url?eid=2-s2.0-0035146643&partnerID=40&md5=5c30e81f747c1e20d18ce0767f68759b en
dc.relation.uri http://www.scopus.com/inward/record.url?eid=2-s2.0-0035146643&partnerID=40&md5=5c30e81f747c1e20d18ce0767f68759b en
dc.subject.other height determination en
dc.subject.other sea level change en
dc.subject.other tide gauge en
dc.subject.other Greece en
dc.title Adjusting sea level measurements at the port of Alexandroupolis en
heal.type journalArticle en
heal.publicationDate 2001 en
heal.abstract The reference surface of heights for the continental Heilenic area is currently defined by the mean sea level of the period 1933-1978, as estimated at the port of Pireaus. However, due to various problems having occurred there since 1981 [3], alternative tide gauge locations in Greece have been sought in order to redefine a height reference surface according to the latest mean sea level variations. The tide gauge at the port of Alexandroupolis belongs to a permanent tidal net [5] consisting of 20 tide gauges (major mareographs) and monitoring sea level variations in Greece (Fig. 1) Our task is primarily to determine mean sea level height in association with a very recent time period and also a suitable measure of the precision of observations thereat. Two main models are considered according to whether variations of astronomical and meteorological nature are modelled or not modelled. Effects of time span of records and of data quality are discussed. en
heal.journalName Survey Review en
dc.identifier.volume 36 en
dc.identifier.issue 1 en
dc.identifier.spage 35 en
dc.identifier.epage 43 en


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