Correction of Hydrological and Oceanic Effects from GRACE Data by Combination of the Steric Sea Level, Altimetry Data and GLDAS Model
In this study, a scheme to estimate oceanic and hydrological effects in the GRACE (Gravity Recovery and Climate Experiment) data is presented. The aim is to reveal tectonic signals for the case of the Sumatra earthquake on 26 December 2004. The variations of hydrological and oceanic effects are esti...
Gespeichert in:
| Veröffentlicht in: | Acta geophysica 2016-08, Vol.64 (4), p.1193-1210 |
|---|---|
| Hauptverfasser: | , , |
| Format: | Artikel |
| Sprache: | eng |
| Schlagworte: | |
| Online-Zugang: | Volltext |
| Tags: |
Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
|
| container_end_page | 1210 |
|---|---|
| container_issue | 4 |
| container_start_page | 1193 |
| container_title | Acta geophysica |
| container_volume | 64 |
| creator | Fatolazadeh, Farzam Voosoghi, Behzad Raoofian Naeeni, Mehdi |
| description | In this study, a scheme to estimate oceanic and hydrological effects in the GRACE (Gravity Recovery and Climate Experiment) data is presented. The aim is to reveal tectonic signals for the case of the Sumatra earthquake on 26 December 2004. The variations of hydrological and oceanic effects are estimated with the aid of data set of GRACE, altimetry, World Ocean Atlas, and the GLDAS model for a period of January 2003 to December 2006. The time series of computed gravity changes over Sumatra region show some correlations to the deformation resulting from the earthquake occurred in December 2004. The maximum and minimum impacts of hydrological and oceanic effects on gravity changes are about 3 μGal in radial direction and–5 μGal in northward direction. The maximum and minimum amounts of gravitational gradient changes after the correction are 0.2 and–0.25 mE, which indicates the significant influences of hydrological and oceanic sources on the desired signal. |
| doi_str_mv | 10.1515/acgeo-2016-0034 |
| format | Article |
| fullrecord | <record><control><sourceid>proquest_cross</sourceid><recordid>TN_cdi_proquest_journals_1865246506</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><sourcerecordid>4312310061</sourcerecordid><originalsourceid>FETCH-LOGICAL-a429t-99a1b30de878b048451b392ec492aa061424e9d21cea66126a996aae2ef577dd3</originalsourceid><addsrcrecordid>eNqNkEFLwzAYhosoOKdnrwGv1iVpkjYXYdS5CZOB03P51n6dHV0z007pD_B_m9oJHjx4yhd4n-dLXs-7ZPSGSSZHkK7R-Jwy5VMaiCNvwCIt_VBIeXyYlQz5qXdW1xtKlaCMD7zP2FiLaVOYipiczNrMmtKsixRKAlVGFilCVaRkkucuVZPcmi2ZPo3jCbmDBsiqJbHZrooKfhTNK5Jlg9ZBSwQyx3csr8m4bIotNrbtsU49nd-Nl-TRZFieeyc5lDVeHM6h93I_eY5n_nwxfYjHcx8E142vNbBVQDOMwmhFRSSku2qOqdAcgComuECdceYerRTjCrRWAMgxl2GYZcHQu-q9O2ve9lg3ycbsbeVWJixSkgslqXKpUZ9Kralri3mys8UWbJswmnRdJ99dJ13XSde1I2574gNK9_UM13bfuuGX_m9SCcGYDpyA9oLararW_yCDL3M8law</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>1865246506</pqid></control><display><type>article</type><title>Correction of Hydrological and Oceanic Effects from GRACE Data by Combination of the Steric Sea Level, Altimetry Data and GLDAS Model</title><source>Springer Nature - Complete Springer Journals</source><creator>Fatolazadeh, Farzam ; Voosoghi, Behzad ; Raoofian Naeeni, Mehdi</creator><creatorcontrib>Fatolazadeh, Farzam ; Voosoghi, Behzad ; Raoofian Naeeni, Mehdi</creatorcontrib><description>In this study, a scheme to estimate oceanic and hydrological effects in the GRACE (Gravity Recovery and Climate Experiment) data is presented. The aim is to reveal tectonic signals for the case of the Sumatra earthquake on 26 December 2004. The variations of hydrological and oceanic effects are estimated with the aid of data set of GRACE, altimetry, World Ocean Atlas, and the GLDAS model for a period of January 2003 to December 2006. The time series of computed gravity changes over Sumatra region show some correlations to the deformation resulting from the earthquake occurred in December 2004. The maximum and minimum impacts of hydrological and oceanic effects on gravity changes are about 3 μGal in radial direction and–5 μGal in northward direction. The maximum and minimum amounts of gravitational gradient changes after the correction are 0.2 and–0.25 mE, which indicates the significant influences of hydrological and oceanic sources on the desired signal.</description><identifier>ISSN: 1895-6572</identifier><identifier>EISSN: 1895-7455</identifier><identifier>DOI: 10.1515/acgeo-2016-0034</identifier><language>eng</language><publisher>Cham: Springer International Publishing</publisher><subject>Altimetry ; Earth and Environmental Science ; Earth Sciences ; Earthquakes ; Geophysics/Geodesy ; Geotechnical Engineering & Applied Earth Sciences ; GLDAS model ; GRACE data ; gravitational gradient changes ; Gravity ; hydrological and oceanic effects ; Plate tectonics ; Seismic activity ; Seismology ; Structural Geology ; World Ocean Atlas</subject><ispartof>Acta geophysica, 2016-08, Vol.64 (4), p.1193-1210</ispartof><rights>Fatolazadeh et al. 2016</rights><rights>Acta Geophysica is a copyright of Springer, 2016.</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a429t-99a1b30de878b048451b392ec492aa061424e9d21cea66126a996aae2ef577dd3</citedby><cites>FETCH-LOGICAL-a429t-99a1b30de878b048451b392ec492aa061424e9d21cea66126a996aae2ef577dd3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1515/acgeo-2016-0034$$EPDF$$P50$$Gspringer$$Hfree_for_read</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1515/acgeo-2016-0034$$EHTML$$P50$$Gspringer$$Hfree_for_read</linktohtml><link.rule.ids>314,778,782,27911,27912,41475,42544,51306</link.rule.ids></links><search><creatorcontrib>Fatolazadeh, Farzam</creatorcontrib><creatorcontrib>Voosoghi, Behzad</creatorcontrib><creatorcontrib>Raoofian Naeeni, Mehdi</creatorcontrib><title>Correction of Hydrological and Oceanic Effects from GRACE Data by Combination of the Steric Sea Level, Altimetry Data and GLDAS Model</title><title>Acta geophysica</title><addtitle>Acta Geophys</addtitle><description>In this study, a scheme to estimate oceanic and hydrological effects in the GRACE (Gravity Recovery and Climate Experiment) data is presented. The aim is to reveal tectonic signals for the case of the Sumatra earthquake on 26 December 2004. The variations of hydrological and oceanic effects are estimated with the aid of data set of GRACE, altimetry, World Ocean Atlas, and the GLDAS model for a period of January 2003 to December 2006. The time series of computed gravity changes over Sumatra region show some correlations to the deformation resulting from the earthquake occurred in December 2004. The maximum and minimum impacts of hydrological and oceanic effects on gravity changes are about 3 μGal in radial direction and–5 μGal in northward direction. The maximum and minimum amounts of gravitational gradient changes after the correction are 0.2 and–0.25 mE, which indicates the significant influences of hydrological and oceanic sources on the desired signal.</description><subject>Altimetry</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Earthquakes</subject><subject>Geophysics/Geodesy</subject><subject>Geotechnical Engineering & Applied Earth Sciences</subject><subject>GLDAS model</subject><subject>GRACE data</subject><subject>gravitational gradient changes</subject><subject>Gravity</subject><subject>hydrological and oceanic effects</subject><subject>Plate tectonics</subject><subject>Seismic activity</subject><subject>Seismology</subject><subject>Structural Geology</subject><subject>World Ocean Atlas</subject><issn>1895-6572</issn><issn>1895-7455</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2016</creationdate><recordtype>article</recordtype><sourceid>C6C</sourceid><sourceid>ABUWG</sourceid><sourceid>AFKRA</sourceid><sourceid>AZQEC</sourceid><sourceid>BENPR</sourceid><sourceid>CCPQU</sourceid><sourceid>DWQXO</sourceid><sourceid>GNUQQ</sourceid><recordid>eNqNkEFLwzAYhosoOKdnrwGv1iVpkjYXYdS5CZOB03P51n6dHV0z007pD_B_m9oJHjx4yhd4n-dLXs-7ZPSGSSZHkK7R-Jwy5VMaiCNvwCIt_VBIeXyYlQz5qXdW1xtKlaCMD7zP2FiLaVOYipiczNrMmtKsixRKAlVGFilCVaRkkucuVZPcmi2ZPo3jCbmDBsiqJbHZrooKfhTNK5Jlg9ZBSwQyx3csr8m4bIotNrbtsU49nd-Nl-TRZFieeyc5lDVeHM6h93I_eY5n_nwxfYjHcx8E142vNbBVQDOMwmhFRSSku2qOqdAcgComuECdceYerRTjCrRWAMgxl2GYZcHQu-q9O2ve9lg3ycbsbeVWJixSkgslqXKpUZ9Kralri3mys8UWbJswmnRdJ99dJ13XSde1I2574gNK9_UM13bfuuGX_m9SCcGYDpyA9oLararW_yCDL3M8law</recordid><startdate>20160801</startdate><enddate>20160801</enddate><creator>Fatolazadeh, Farzam</creator><creator>Voosoghi, Behzad</creator><creator>Raoofian Naeeni, Mehdi</creator><general>Springer International Publishing</general><general>De Gruyter</general><general>Springer Nature B.V</general><scope>C6C</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7TG</scope><scope>7XB</scope><scope>88I</scope><scope>8FD</scope><scope>8FE</scope><scope>8FG</scope><scope>8FK</scope><scope>ABJCF</scope><scope>ABUWG</scope><scope>AEUYN</scope><scope>AFKRA</scope><scope>ARAPS</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BGLVJ</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>FR3</scope><scope>GNUQQ</scope><scope>H8D</scope><scope>HCIFZ</scope><scope>KL.</scope><scope>KR7</scope><scope>L6V</scope><scope>L7M</scope><scope>M2P</scope><scope>M7S</scope><scope>P5Z</scope><scope>P62</scope><scope>PCBAR</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PTHSS</scope><scope>Q9U</scope></search><sort><creationdate>20160801</creationdate><title>Correction of Hydrological and Oceanic Effects from GRACE Data by Combination of the Steric Sea Level, Altimetry Data and GLDAS Model</title><author>Fatolazadeh, Farzam ; Voosoghi, Behzad ; Raoofian Naeeni, Mehdi</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a429t-99a1b30de878b048451b392ec492aa061424e9d21cea66126a996aae2ef577dd3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2016</creationdate><topic>Altimetry</topic><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Earthquakes</topic><topic>Geophysics/Geodesy</topic><topic>Geotechnical Engineering & Applied Earth Sciences</topic><topic>GLDAS model</topic><topic>GRACE data</topic><topic>gravitational gradient changes</topic><topic>Gravity</topic><topic>hydrological and oceanic effects</topic><topic>Plate tectonics</topic><topic>Seismic activity</topic><topic>Seismology</topic><topic>Structural Geology</topic><topic>World Ocean Atlas</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Fatolazadeh, Farzam</creatorcontrib><creatorcontrib>Voosoghi, Behzad</creatorcontrib><creatorcontrib>Raoofian Naeeni, Mehdi</creatorcontrib><collection>Springer Nature OA Free Journals</collection><collection>CrossRef</collection><collection>ProQuest Central (Corporate)</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>ProQuest Central (purchase pre-March 2016)</collection><collection>Science Database (Alumni Edition)</collection><collection>Technology Research Database</collection><collection>ProQuest SciTech Collection</collection><collection>ProQuest Technology Collection</collection><collection>ProQuest Central (Alumni) (purchase pre-March 2016)</collection><collection>Materials Science & Engineering Collection</collection><collection>ProQuest Central (Alumni Edition)</collection><collection>ProQuest One Sustainability</collection><collection>ProQuest Central UK/Ireland</collection><collection>Advanced Technologies & Aerospace Collection</collection><collection>ProQuest Central Essentials</collection><collection>ProQuest Central</collection><collection>Technology Collection (ProQuest)</collection><collection>Natural Science Collection (ProQuest)</collection><collection>Earth, Atmospheric & Aquatic Science Collection</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central Korea</collection><collection>Engineering Research Database</collection><collection>ProQuest Central Student</collection><collection>Aerospace Database</collection><collection>SciTech Premium Collection</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Civil Engineering Abstracts</collection><collection>ProQuest Engineering Collection</collection><collection>Advanced Technologies Database with Aerospace</collection><collection>Science Database (ProQuest)</collection><collection>Engineering Database</collection><collection>Advanced Technologies & Aerospace Database</collection><collection>ProQuest Advanced Technologies & Aerospace Collection</collection><collection>Earth, Atmospheric & Aquatic Science Database</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>Engineering Collection</collection><collection>ProQuest Central Basic</collection><jtitle>Acta geophysica</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Fatolazadeh, Farzam</au><au>Voosoghi, Behzad</au><au>Raoofian Naeeni, Mehdi</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Correction of Hydrological and Oceanic Effects from GRACE Data by Combination of the Steric Sea Level, Altimetry Data and GLDAS Model</atitle><jtitle>Acta geophysica</jtitle><stitle>Acta Geophys</stitle><date>2016-08-01</date><risdate>2016</risdate><volume>64</volume><issue>4</issue><spage>1193</spage><epage>1210</epage><pages>1193-1210</pages><issn>1895-6572</issn><eissn>1895-7455</eissn><abstract>In this study, a scheme to estimate oceanic and hydrological effects in the GRACE (Gravity Recovery and Climate Experiment) data is presented. The aim is to reveal tectonic signals for the case of the Sumatra earthquake on 26 December 2004. The variations of hydrological and oceanic effects are estimated with the aid of data set of GRACE, altimetry, World Ocean Atlas, and the GLDAS model for a period of January 2003 to December 2006. The time series of computed gravity changes over Sumatra region show some correlations to the deformation resulting from the earthquake occurred in December 2004. The maximum and minimum impacts of hydrological and oceanic effects on gravity changes are about 3 μGal in radial direction and–5 μGal in northward direction. The maximum and minimum amounts of gravitational gradient changes after the correction are 0.2 and–0.25 mE, which indicates the significant influences of hydrological and oceanic sources on the desired signal.</abstract><cop>Cham</cop><pub>Springer International Publishing</pub><doi>10.1515/acgeo-2016-0034</doi><tpages>18</tpages><oa>free_for_read</oa></addata></record> |
| fulltext | fulltext |
| identifier | ISSN: 1895-6572 |
| ispartof | Acta geophysica, 2016-08, Vol.64 (4), p.1193-1210 |
| issn | 1895-6572 1895-7455 |
| language | eng |
| recordid | cdi_proquest_journals_1865246506 |
| source | Springer Nature - Complete Springer Journals |
| subjects | Altimetry Earth and Environmental Science Earth Sciences Earthquakes Geophysics/Geodesy Geotechnical Engineering & Applied Earth Sciences GLDAS model GRACE data gravitational gradient changes Gravity hydrological and oceanic effects Plate tectonics Seismic activity Seismology Structural Geology World Ocean Atlas |
| title | Correction of Hydrological and Oceanic Effects from GRACE Data by Combination of the Steric Sea Level, Altimetry Data and GLDAS Model |
| url | https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-01-16T05%3A31%3A34IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-proquest_cross&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Correction%20of%20Hydrological%20and%20Oceanic%20Effects%20from%20GRACE%20Data%20by%20Combination%20of%20the%20Steric%20Sea%20Level,%20Altimetry%20Data%20and%20GLDAS%20Model&rft.jtitle=Acta%20geophysica&rft.au=Fatolazadeh,%20Farzam&rft.date=2016-08-01&rft.volume=64&rft.issue=4&rft.spage=1193&rft.epage=1210&rft.pages=1193-1210&rft.issn=1895-6572&rft.eissn=1895-7455&rft_id=info:doi/10.1515/acgeo-2016-0034&rft_dat=%3Cproquest_cross%3E4312310061%3C/proquest_cross%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_pqid=1865246506&rft_id=info:pmid/&rfr_iscdi=true |