dc.contributor.author |
Elias, P |
en |
dc.contributor.author |
Kontoes, C |
en |
dc.contributor.author |
Sykioti, O |
en |
dc.contributor.author |
Avallone, A |
en |
dc.contributor.author |
Van Gorp, S |
en |
dc.contributor.author |
Briole, P |
en |
dc.contributor.author |
Paradissis, D |
en |
dc.date.accessioned |
2014-03-01T01:23:25Z |
|
dc.date.available |
2014-03-01T01:23:25Z |
|
dc.date.issued |
2006 |
en |
dc.identifier.issn |
0143-1161 |
en |
dc.identifier.uri |
https://dspace.lib.ntua.gr/xmlui/handle/123456789/16959 |
|
dc.subject |
Low Frequency |
en |
dc.subject.classification |
Remote Sensing |
en |
dc.subject.classification |
Imaging Science & Photographic Technology |
en |
dc.subject.other |
Atmospheric movements |
en |
dc.subject.other |
Computational methods |
en |
dc.subject.other |
Interferometry |
en |
dc.subject.other |
Pattern recognition |
en |
dc.subject.other |
Deformation pattern |
en |
dc.subject.other |
Radar interferometry |
en |
dc.subject.other |
Remote sensing |
en |
dc.subject.other |
artifact |
en |
dc.subject.other |
earthquake |
en |
dc.subject.other |
ERS-1 |
en |
dc.subject.other |
ERS-2 |
en |
dc.subject.other |
frequency analysis |
en |
dc.subject.other |
numerical method |
en |
dc.subject.other |
radar imagery |
en |
dc.subject.other |
radar interferometry |
en |
dc.subject.other |
synthetic aperture radar |
en |
dc.subject.other |
Athens [Attica] |
en |
dc.subject.other |
Attica |
en |
dc.subject.other |
Eurasia |
en |
dc.subject.other |
Europe |
en |
dc.subject.other |
Greece |
en |
dc.subject.other |
Southern Europe |
en |
dc.title |
A method for minimising of low frequency and unwrapping artefacts from interferometric calculations |
en |
heal.type |
journalArticle |
en |
heal.identifier.primary |
10.1080/01431160600578388 |
en |
heal.identifier.secondary |
http://dx.doi.org/10.1080/01431160600578388 |
en |
heal.language |
English |
en |
heal.publicationDate |
2006 |
en |
heal.abstract |
On 7 September 1999 a magnitude MW=5.9 earthquake occurred in the Athens area of Greece producing a subsidence of 6-7 cm detected by radar interferometry. This study introduces a processing technique, which produces a clear deformation pattern of the earthquake, mostly released from artefacts due to orbital effects, unwrapping cycle slipping errors and atmospherics disturbances. A set of 17 ERS-1 and ERS-2 SAR images acquired between December 1997 and January 2001 has been used. The contribution of each artefact to the interferograms was calculated, both in the frequency and spatial domains. |
en |
heal.publisher |
TAYLOR & FRANCIS LTD |
en |
heal.journalName |
International Journal of Remote Sensing |
en |
dc.identifier.doi |
10.1080/01431160600578388 |
en |
dc.identifier.isi |
ISI:000239239100021 |
en |
dc.identifier.volume |
27 |
en |
dc.identifier.issue |
14 |
en |
dc.identifier.spage |
3079 |
en |
dc.identifier.epage |
3086 |
en |