Accuracy assessment of SRTM v4 and ASTER GDEM v2 over the Altiplano watershed using ICESat/GLAS data
Descripción del Articulo
The new Global Digital Elevation Model (GDEM v2) has been available since 17 October 2011. With a resolution of approximately 30 m, this model should provide more accurate information than the latest version of Shuttle Radar Topographic Mission (SRTM v4) with a resolution of 90 m outside of the USA....
| Autores: | , , , , , , , , , |
|---|---|
| Formato: | artículo |
| Fecha de Publicación: | 2015 |
| Institución: | Servicio Nacional de Meteorología e Hidrología del Perú |
| Repositorio: | SENAMHI-Institucional |
| Lenguaje: | inglés |
| OAI Identifier: | oai:repositorio.senamhi.gob.pe:20.500.12542/56 |
| Enlace del recurso: | https://hdl.handle.net/20.500.12542/56 https://doi.org/10.1080/01431161.2014.999166 |
| Nivel de acceso: | acceso cerrado |
| Materia: | Aneroid altimeters Digital Instruments Forestry Geomorphology Radio Altimeters Tracking Radar Radar |
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| dc.title.en_US.fl_str_mv |
Accuracy assessment of SRTM v4 and ASTER GDEM v2 over the Altiplano watershed using ICESat/GLAS data |
| title |
Accuracy assessment of SRTM v4 and ASTER GDEM v2 over the Altiplano watershed using ICESat/GLAS data |
| spellingShingle |
Accuracy assessment of SRTM v4 and ASTER GDEM v2 over the Altiplano watershed using ICESat/GLAS data Satgé, F. Aneroid altimeters Digital Instruments Forestry Geomorphology Radio Altimeters Tracking Radar Radar |
| title_short |
Accuracy assessment of SRTM v4 and ASTER GDEM v2 over the Altiplano watershed using ICESat/GLAS data |
| title_full |
Accuracy assessment of SRTM v4 and ASTER GDEM v2 over the Altiplano watershed using ICESat/GLAS data |
| title_fullStr |
Accuracy assessment of SRTM v4 and ASTER GDEM v2 over the Altiplano watershed using ICESat/GLAS data |
| title_full_unstemmed |
Accuracy assessment of SRTM v4 and ASTER GDEM v2 over the Altiplano watershed using ICESat/GLAS data |
| title_sort |
Accuracy assessment of SRTM v4 and ASTER GDEM v2 over the Altiplano watershed using ICESat/GLAS data |
| author |
Satgé, F. |
| author_facet |
Satgé, F. Bonnet, M.P Timouk, F. Calmant, S. Pillco, R. Molina, J. Lavado-Casimiro, W. Arsen, A. Crétaux, J.F. Garnier, J. |
| author_role |
author |
| author2 |
Bonnet, M.P Timouk, F. Calmant, S. Pillco, R. Molina, J. Lavado-Casimiro, W. Arsen, A. Crétaux, J.F. Garnier, J. |
| author2_role |
author author author author author author author author author |
| dc.contributor.author.fl_str_mv |
Satgé, F. Bonnet, M.P Timouk, F. Calmant, S. Pillco, R. Molina, J. Lavado-Casimiro, W. Arsen, A. Crétaux, J.F. Garnier, J. |
| dc.subject.en_US.fl_str_mv |
Aneroid altimeters Digital Instruments Forestry Geomorphology Radio Altimeters Tracking Radar |
| topic |
Aneroid altimeters Digital Instruments Forestry Geomorphology Radio Altimeters Tracking Radar Radar |
| dc.subject.es_PE.fl_str_mv |
Radar |
| description |
The new Global Digital Elevation Model (GDEM v2) has been available since 17 October 2011. With a resolution of approximately 30 m, this model should provide more accurate information than the latest version of Shuttle Radar Topographic Mission (SRTM v4) with a resolution of 90 m outside of the USA. The accuracies of these two recently released digital elevation models (DEMs) were assessed over the Altiplano watershed in South America using ICESat/GLAS data (Ice, Cloud and Land Elevation Satellite/Geoscience Laser Altimeter System). On the global scale, GDEM v2 is more accurate than SRTM v4, which presents a negative bias of approximately 8.8 m. Strong correlations between the DEMs’ accuracies and mean slope values occurred. Regarding land cover, SRTM v4 could be more accurate or easier to correct on a smaller scale than GDEM v2. Finally, a merged and corrected DEM that considers all of these observations was built to provide more accurate information for this region. The new model featured lower absolute mean errors, standard deviations, and root mean square errors relative to SRTM v4 or GDEM v2. |
| publishDate |
2015 |
| dc.date.accessioned.none.fl_str_mv |
2019-07-22T14:24:00Z |
| dc.date.available.none.fl_str_mv |
2019-07-22T14:24:00Z |
| dc.date.issued.fl_str_mv |
2015-01 |
| dc.type.en_US.fl_str_mv |
info:eu-repo/semantics/article |
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article |
| dc.identifier.uri.none.fl_str_mv |
https://hdl.handle.net/20.500.12542/56 |
| dc.identifier.isni.none.fl_str_mv |
0000 0001 0746 0446 |
| dc.identifier.doi.none.fl_str_mv |
https://doi.org/10.1080/01431161.2014.999166 |
| url |
https://hdl.handle.net/20.500.12542/56 https://doi.org/10.1080/01431161.2014.999166 |
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0000 0001 0746 0446 |
| dc.language.iso.en_US.fl_str_mv |
eng |
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eng |
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urn:issn:0143-1161 |
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info:eu-repo/semantics/closedAccess Atribución-NoComercial-SinDerivadas 3.0 Estados Unidos de América |
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http://creativecommons.org/licenses/by-nc-nd/3.0/us/ |
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closedAccess |
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Atribución-NoComercial-SinDerivadas 3.0 Estados Unidos de América http://creativecommons.org/licenses/by-nc-nd/3.0/us/ |
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application/pdf |
| dc.publisher.en_US.fl_str_mv |
Taylor and Francis Ltd. |
| dc.source.es_PE.fl_str_mv |
Servicio Nacional de Meteorología e Hidrología del Perú Repositorio Institucional - SENAMHI |
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reponame:SENAMHI-Institucional instname:Servicio Nacional de Meteorología e Hidrología del Perú instacron:SENAMHI |
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SENAMHI |
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36 |
| dc.source.issue.es_PE.fl_str_mv |
2 |
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465 |
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| dc.source.journal.es_PE.fl_str_mv |
International Journal of Remote Sensing |
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Satgé, F.Bonnet, M.PTimouk, F.Calmant, S.Pillco, R.Molina, J.Lavado-Casimiro, W.Arsen, A.Crétaux, J.F.Garnier, J.2019-07-22T14:24:00Z2019-07-22T14:24:00Z2015-01https://hdl.handle.net/20.500.12542/560000 0001 0746 0446https://doi.org/10.1080/01431161.2014.999166The new Global Digital Elevation Model (GDEM v2) has been available since 17 October 2011. With a resolution of approximately 30 m, this model should provide more accurate information than the latest version of Shuttle Radar Topographic Mission (SRTM v4) with a resolution of 90 m outside of the USA. The accuracies of these two recently released digital elevation models (DEMs) were assessed over the Altiplano watershed in South America using ICESat/GLAS data (Ice, Cloud and Land Elevation Satellite/Geoscience Laser Altimeter System). On the global scale, GDEM v2 is more accurate than SRTM v4, which presents a negative bias of approximately 8.8 m. Strong correlations between the DEMs’ accuracies and mean slope values occurred. Regarding land cover, SRTM v4 could be more accurate or easier to correct on a smaller scale than GDEM v2. Finally, a merged and corrected DEM that considers all of these observations was built to provide more accurate information for this region. The new model featured lower absolute mean errors, standard deviations, and root mean square errors relative to SRTM v4 or GDEM v2.Por paresapplication/pdfengTaylor and Francis Ltd.urn:issn:0143-1161info:eu-repo/semantics/closedAccessAtribución-NoComercial-SinDerivadas 3.0 Estados Unidos de Américahttp://creativecommons.org/licenses/by-nc-nd/3.0/us/Servicio Nacional de Meteorología e Hidrología del PerúRepositorio Institucional - SENAMHI362465488International Journal of Remote Sensingreponame:SENAMHI-Institucionalinstname:Servicio Nacional de Meteorología e Hidrología del Perúinstacron:SENAMHIAneroid altimetersDigital InstrumentsForestryGeomorphologyRadio AltimetersTracking RadarRadarAccuracy assessment of SRTM v4 and ASTER GDEM v2 over the Altiplano watershed using ICESat/GLAS datainfo:eu-repo/semantics/articleLICENSElicense.txtlicense.txttext/plain; charset=utf-81748http://repositorio.senamhi.gob.pe/bitstream/20.500.12542/56/2/license.txt8a4605be74aa9ea9d79846c1fba20a33MD5220.500.12542/56oai:repositorio.senamhi.gob.pe:20.500.12542/562021-03-16 18:33:10.184Repositorio Institucional SENAMHIrepositorio@senamhi.gob.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 |
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Nota importante:
La información contenida en este registro es de entera responsabilidad de la institución que gestiona el repositorio institucional donde esta contenido este documento o set de datos. El CONCYTEC no se hace responsable por los contenidos (publicaciones y/o datos) accesibles a través del Repositorio Nacional Digital de Ciencia, Tecnología e Innovación de Acceso Abierto (ALICIA).
La información contenida en este registro es de entera responsabilidad de la institución que gestiona el repositorio institucional donde esta contenido este documento o set de datos. El CONCYTEC no se hace responsable por los contenidos (publicaciones y/o datos) accesibles a través del Repositorio Nacional Digital de Ciencia, Tecnología e Innovación de Acceso Abierto (ALICIA).