Identifying and correcting oblique striping in the topodata digital elevation model.
Autor(a) principal: | |
---|---|
Data de Publicação: | 2013 |
Outros Autores: | , , , |
Idioma: | eng |
Título da fonte: | Repositório Institucional da EMBRAPA (Repository Open Access to Scientific Information from EMBRAPA - Alice) |
Texto Completo: | http://www.alice.cnptia.embrapa.br/alice/handle/doc/974950 |
Resumo: | The Topodata digital elevation model (DEM) is the best DEM available for digital soil mapping (DSM) in Brazil. However, it is not ready to use. We show that the kriging interpolator used to downscale the SRTM DEM from 3 arc-seconds to 1 arc-second spatial resolution increased the double oblique striping (15º and 60º) so common to SRTM DEMs. This is because kriging is quite sensitive to outliers. Besides, the Gaussian model of spatial covariance used in the downscaling enhanced the sensitivity of kriging to outliers, thus enhancing the striping. 2D Fast Fourier Transform can be used to identify whether a destriping procedure need to be employed. The bilinear or cubic resampling methods should be used to warp Topodata DEMs because they are insensitive to the double oblique striping. |
id |
EMBR_e523522347b56fc68f4ade38aa13380e |
---|---|
oai_identifier_str |
oai:www.alice.cnptia.embrapa.br:doc/974950 |
network_acronym_str |
EMBR |
network_name_str |
Repositório Institucional da EMBRAPA (Repository Open Access to Scientific Information from EMBRAPA - Alice) |
repository_id_str |
2154 |
spelling |
Identifying and correcting oblique striping in the topodata digital elevation model.SRTM downscalingDEM warping2D Fast Fourier TransformThe Topodata digital elevation model (DEM) is the best DEM available for digital soil mapping (DSM) in Brazil. However, it is not ready to use. We show that the kriging interpolator used to downscale the SRTM DEM from 3 arc-seconds to 1 arc-second spatial resolution increased the double oblique striping (15º and 60º) so common to SRTM DEMs. This is because kriging is quite sensitive to outliers. Besides, the Gaussian model of spatial covariance used in the downscaling enhanced the sensitivity of kriging to outliers, thus enhancing the striping. 2D Fast Fourier Transform can be used to identify whether a destriping procedure need to be employed. The bilinear or cubic resampling methods should be used to warp Topodata DEMs because they are insensitive to the double oblique striping.Alessandro Samuel-Rosa, UFRRJ; Lúcia H. C. dos Anjos, UFRRJ; GUSTAVO DE MATTOS VASQUES, CNPS; Mauro A. H. Antunes, UFRRJ; Ricardo S. D. Dalmolin, UNIVERSIDADE FEDERAL DE SANTA MARIA.SAMUEL-ROSA, A.ANJOS, L. H. C. dosVASQUES, G. de M.ANTUNES, M. A. H.DALMOLIN, R. S. D.2014-01-06T11:11:11Z2014-01-06T11:11:11Z2014-01-0620132016-12-12T11:11:11ZArtigo em anais e proceedingsinfo:eu-repo/semantics/publishedVersionIn: CONGRESSO BRASILEIRO DE CIÊNCIA DO SOLO, 34., 2013, Florianópolis. Anais... Florianópolis: Sociedade Brasileira de Ciência do Solo, 2013.http://www.alice.cnptia.embrapa.br/alice/handle/doc/974950enginfo:eu-repo/semantics/openAccessreponame:Repositório Institucional da EMBRAPA (Repository Open Access to Scientific Information from EMBRAPA - Alice)instname:Empresa Brasileira de Pesquisa Agropecuária (Embrapa)instacron:EMBRAPA2017-08-16T03:54:22Zoai:www.alice.cnptia.embrapa.br:doc/974950Repositório InstitucionalPUBhttps://www.alice.cnptia.embrapa.br/oai/requestcg-riaa@embrapa.bropendoar:21542017-08-16T03:54:22Repositório Institucional da EMBRAPA (Repository Open Access to Scientific Information from EMBRAPA - Alice) - Empresa Brasileira de Pesquisa Agropecuária (Embrapa)false |
dc.title.none.fl_str_mv |
Identifying and correcting oblique striping in the topodata digital elevation model. |
title |
Identifying and correcting oblique striping in the topodata digital elevation model. |
spellingShingle |
Identifying and correcting oblique striping in the topodata digital elevation model. SAMUEL-ROSA, A. SRTM downscaling DEM warping 2D Fast Fourier Transform |
title_short |
Identifying and correcting oblique striping in the topodata digital elevation model. |
title_full |
Identifying and correcting oblique striping in the topodata digital elevation model. |
title_fullStr |
Identifying and correcting oblique striping in the topodata digital elevation model. |
title_full_unstemmed |
Identifying and correcting oblique striping in the topodata digital elevation model. |
title_sort |
Identifying and correcting oblique striping in the topodata digital elevation model. |
author |
SAMUEL-ROSA, A. |
author_facet |
SAMUEL-ROSA, A. ANJOS, L. H. C. dos VASQUES, G. de M. ANTUNES, M. A. H. DALMOLIN, R. S. D. |
author_role |
author |
author2 |
ANJOS, L. H. C. dos VASQUES, G. de M. ANTUNES, M. A. H. DALMOLIN, R. S. D. |
author2_role |
author author author author |
dc.contributor.none.fl_str_mv |
Alessandro Samuel-Rosa, UFRRJ; Lúcia H. C. dos Anjos, UFRRJ; GUSTAVO DE MATTOS VASQUES, CNPS; Mauro A. H. Antunes, UFRRJ; Ricardo S. D. Dalmolin, UNIVERSIDADE FEDERAL DE SANTA MARIA. |
dc.contributor.author.fl_str_mv |
SAMUEL-ROSA, A. ANJOS, L. H. C. dos VASQUES, G. de M. ANTUNES, M. A. H. DALMOLIN, R. S. D. |
dc.subject.por.fl_str_mv |
SRTM downscaling DEM warping 2D Fast Fourier Transform |
topic |
SRTM downscaling DEM warping 2D Fast Fourier Transform |
description |
The Topodata digital elevation model (DEM) is the best DEM available for digital soil mapping (DSM) in Brazil. However, it is not ready to use. We show that the kriging interpolator used to downscale the SRTM DEM from 3 arc-seconds to 1 arc-second spatial resolution increased the double oblique striping (15º and 60º) so common to SRTM DEMs. This is because kriging is quite sensitive to outliers. Besides, the Gaussian model of spatial covariance used in the downscaling enhanced the sensitivity of kriging to outliers, thus enhancing the striping. 2D Fast Fourier Transform can be used to identify whether a destriping procedure need to be employed. The bilinear or cubic resampling methods should be used to warp Topodata DEMs because they are insensitive to the double oblique striping. |
publishDate |
2013 |
dc.date.none.fl_str_mv |
2013 2014-01-06T11:11:11Z 2014-01-06T11:11:11Z 2014-01-06 2016-12-12T11:11:11Z |
dc.type.driver.fl_str_mv |
Artigo em anais e proceedings |
dc.type.status.fl_str_mv |
info:eu-repo/semantics/publishedVersion |
status_str |
publishedVersion |
dc.identifier.uri.fl_str_mv |
In: CONGRESSO BRASILEIRO DE CIÊNCIA DO SOLO, 34., 2013, Florianópolis. Anais... Florianópolis: Sociedade Brasileira de Ciência do Solo, 2013. http://www.alice.cnptia.embrapa.br/alice/handle/doc/974950 |
identifier_str_mv |
In: CONGRESSO BRASILEIRO DE CIÊNCIA DO SOLO, 34., 2013, Florianópolis. Anais... Florianópolis: Sociedade Brasileira de Ciência do Solo, 2013. |
url |
http://www.alice.cnptia.embrapa.br/alice/handle/doc/974950 |
dc.language.iso.fl_str_mv |
eng |
language |
eng |
dc.rights.driver.fl_str_mv |
info:eu-repo/semantics/openAccess |
eu_rights_str_mv |
openAccess |
dc.source.none.fl_str_mv |
reponame:Repositório Institucional da EMBRAPA (Repository Open Access to Scientific Information from EMBRAPA - Alice) instname:Empresa Brasileira de Pesquisa Agropecuária (Embrapa) instacron:EMBRAPA |
instname_str |
Empresa Brasileira de Pesquisa Agropecuária (Embrapa) |
instacron_str |
EMBRAPA |
institution |
EMBRAPA |
reponame_str |
Repositório Institucional da EMBRAPA (Repository Open Access to Scientific Information from EMBRAPA - Alice) |
collection |
Repositório Institucional da EMBRAPA (Repository Open Access to Scientific Information from EMBRAPA - Alice) |
repository.name.fl_str_mv |
Repositório Institucional da EMBRAPA (Repository Open Access to Scientific Information from EMBRAPA - Alice) - Empresa Brasileira de Pesquisa Agropecuária (Embrapa) |
repository.mail.fl_str_mv |
cg-riaa@embrapa.br |
_version_ |
1817695314299060224 |