Resolving mass flux at high spatial and temporal resolution using GRACE intersatellite measurements
The GRACE mission is designed to monitor mass flux on the Earth's surface at one month and high spatial resolution through the estimation of monthly gravity fields. Although this approach has been largely successful, information at submonthly time scales can be lost or even aliased through the...
Gespeichert in:
Veröffentlicht in: | Geophysical research letters 2005-02, Vol.32 (4), p.L04310.1-n/a |
---|---|
Hauptverfasser: | , , , , , , , |
Format: | Artikel |
Sprache: | eng |
Schlagworte: | |
Online-Zugang: | Volltext |
Tags: |
Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
|
container_end_page | n/a |
---|---|
container_issue | 4 |
container_start_page | L04310.1 |
container_title | Geophysical research letters |
container_volume | 32 |
creator | Rowlands, D. D. Luthcke, S. B. Klosko, S. M. Lemoine, F. G. R. Chinn, D. S. McCarthy, J. J. Cox, C. M. Anderson, O. B. |
description | The GRACE mission is designed to monitor mass flux on the Earth's surface at one month and high spatial resolution through the estimation of monthly gravity fields. Although this approach has been largely successful, information at submonthly time scales can be lost or even aliased through the estimation of static monthly parameters. Through an analysis of the GRACE data residuals, we show that the fundamental temporal and spatial resolution of the GRACE data is 10 days and 400 km. We present an approach similar in concept to altimetric methods that recovers submonthly mass flux at a high spatial resolution. Using 4° × 4° blocks at 10‐day intervals, we estimate the mass of surplus or deficit water over a 52° × 60° grid centered on the Amazon basin for July 2003. We demonstrate that the recovered signals are coherent and correlate well with the expected hydrological signal. |
doi_str_mv | 10.1029/2004GL021908 |
format | Article |
fullrecord | <record><control><sourceid>proquest_cross</sourceid><recordid>TN_cdi_proquest_miscellaneous_1530994788</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><sourcerecordid>1530994788</sourcerecordid><originalsourceid>FETCH-LOGICAL-a5111-41ba0e0b967987757c82957aeca66d55d316771f2e0ba3cc2a20de5b3b9d0db73</originalsourceid><addsrcrecordid>eNp9kE1v1DAQhiNEJZaWGz_AFyQOBMZ2HMfHalWyoIhKqwJHa-I4rSEfi8eB9t-T1VbAidPMSM_zavRm2UsObzkI804AFHUDghuonmQbbooirwD002wDYNZd6PJZ9pzoGwBIkHyTub2nefgZpls2IhHrh-WeYWJ34faO0QFTwIHh1LHkx8Mc1yMehSWFeWILHb16f7m9YmFKPhImPwwheTZ6pCX60U-JLrKzHgfyLx7nefb5_dXNdpc31_WH7WWTo-Kc5wVvETy0ptSm0lppVwmjNHqHZdkp1Uleas17sTIonRMooPOqla3poGu1PM9en3IPcf6xeEp2DOTWh3Dy80KWKwnGFLqqVvTNCXVxJoq-t4cYRowPloM9dmn_7XLFXz0mIzkc-oiTC_TXKUulNKiVEyfuVxj8w38zbb1vuJGcr1J-kgIlf_9HwvjdllpqZb9-qu2u2X6UX2ppd_I3vG2R_Q</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>1530994788</pqid></control><display><type>article</type><title>Resolving mass flux at high spatial and temporal resolution using GRACE intersatellite measurements</title><source>Wiley Online Library Free Content</source><source>Access via Wiley Online Library</source><source>Wiley-Blackwell AGU Digital Library</source><source>EZB-FREE-00999 freely available EZB journals</source><creator>Rowlands, D. D. ; Luthcke, S. B. ; Klosko, S. M. ; Lemoine, F. G. R. ; Chinn, D. S. ; McCarthy, J. J. ; Cox, C. M. ; Anderson, O. B.</creator><creatorcontrib>Rowlands, D. D. ; Luthcke, S. B. ; Klosko, S. M. ; Lemoine, F. G. R. ; Chinn, D. S. ; McCarthy, J. J. ; Cox, C. M. ; Anderson, O. B.</creatorcontrib><description>The GRACE mission is designed to monitor mass flux on the Earth's surface at one month and high spatial resolution through the estimation of monthly gravity fields. Although this approach has been largely successful, information at submonthly time scales can be lost or even aliased through the estimation of static monthly parameters. Through an analysis of the GRACE data residuals, we show that the fundamental temporal and spatial resolution of the GRACE data is 10 days and 400 km. We present an approach similar in concept to altimetric methods that recovers submonthly mass flux at a high spatial resolution. Using 4° × 4° blocks at 10‐day intervals, we estimate the mass of surplus or deficit water over a 52° × 60° grid centered on the Amazon basin for July 2003. We demonstrate that the recovered signals are coherent and correlate well with the expected hydrological signal.</description><identifier>ISSN: 0094-8276</identifier><identifier>EISSN: 1944-8007</identifier><identifier>DOI: 10.1029/2004GL021908</identifier><identifier>CODEN: GPRLAJ</identifier><language>eng</language><publisher>Washington, DC: Blackwell Publishing Ltd</publisher><subject>Amazon Basin ; Earth sciences ; Earth, ocean, space ; Exact sciences and technology ; Flux ; Geophysics ; GRACE (experiment) ; Hydrology ; Monitors ; River basins ; Spatial resolution</subject><ispartof>Geophysical research letters, 2005-02, Vol.32 (4), p.L04310.1-n/a</ispartof><rights>Copyright 2005 by the American Geophysical Union.</rights><rights>2005 INIST-CNRS</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a5111-41ba0e0b967987757c82957aeca66d55d316771f2e0ba3cc2a20de5b3b9d0db73</citedby><cites>FETCH-LOGICAL-a5111-41ba0e0b967987757c82957aeca66d55d316771f2e0ba3cc2a20de5b3b9d0db73</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://onlinelibrary.wiley.com/doi/pdf/10.1029%2F2004GL021908$$EPDF$$P50$$Gwiley$$H</linktopdf><linktohtml>$$Uhttps://onlinelibrary.wiley.com/doi/full/10.1029%2F2004GL021908$$EHTML$$P50$$Gwiley$$H</linktohtml><link.rule.ids>314,780,784,1417,1433,11514,27924,27925,45574,45575,46409,46468,46833,46892</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=16655705$$DView record in Pascal Francis$$Hfree_for_read</backlink></links><search><creatorcontrib>Rowlands, D. D.</creatorcontrib><creatorcontrib>Luthcke, S. B.</creatorcontrib><creatorcontrib>Klosko, S. M.</creatorcontrib><creatorcontrib>Lemoine, F. G. R.</creatorcontrib><creatorcontrib>Chinn, D. S.</creatorcontrib><creatorcontrib>McCarthy, J. J.</creatorcontrib><creatorcontrib>Cox, C. M.</creatorcontrib><creatorcontrib>Anderson, O. B.</creatorcontrib><title>Resolving mass flux at high spatial and temporal resolution using GRACE intersatellite measurements</title><title>Geophysical research letters</title><addtitle>Geophys. Res. Lett</addtitle><description>The GRACE mission is designed to monitor mass flux on the Earth's surface at one month and high spatial resolution through the estimation of monthly gravity fields. Although this approach has been largely successful, information at submonthly time scales can be lost or even aliased through the estimation of static monthly parameters. Through an analysis of the GRACE data residuals, we show that the fundamental temporal and spatial resolution of the GRACE data is 10 days and 400 km. We present an approach similar in concept to altimetric methods that recovers submonthly mass flux at a high spatial resolution. Using 4° × 4° blocks at 10‐day intervals, we estimate the mass of surplus or deficit water over a 52° × 60° grid centered on the Amazon basin for July 2003. We demonstrate that the recovered signals are coherent and correlate well with the expected hydrological signal.</description><subject>Amazon Basin</subject><subject>Earth sciences</subject><subject>Earth, ocean, space</subject><subject>Exact sciences and technology</subject><subject>Flux</subject><subject>Geophysics</subject><subject>GRACE (experiment)</subject><subject>Hydrology</subject><subject>Monitors</subject><subject>River basins</subject><subject>Spatial resolution</subject><issn>0094-8276</issn><issn>1944-8007</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2005</creationdate><recordtype>article</recordtype><recordid>eNp9kE1v1DAQhiNEJZaWGz_AFyQOBMZ2HMfHalWyoIhKqwJHa-I4rSEfi8eB9t-T1VbAidPMSM_zavRm2UsObzkI804AFHUDghuonmQbbooirwD002wDYNZd6PJZ9pzoGwBIkHyTub2nefgZpls2IhHrh-WeYWJ34faO0QFTwIHh1LHkx8Mc1yMehSWFeWILHb16f7m9YmFKPhImPwwheTZ6pCX60U-JLrKzHgfyLx7nefb5_dXNdpc31_WH7WWTo-Kc5wVvETy0ptSm0lppVwmjNHqHZdkp1Uleas17sTIonRMooPOqla3poGu1PM9en3IPcf6xeEp2DOTWh3Dy80KWKwnGFLqqVvTNCXVxJoq-t4cYRowPloM9dmn_7XLFXz0mIzkc-oiTC_TXKUulNKiVEyfuVxj8w38zbb1vuJGcr1J-kgIlf_9HwvjdllpqZb9-qu2u2X6UX2ppd_I3vG2R_Q</recordid><startdate>200502</startdate><enddate>200502</enddate><creator>Rowlands, D. D.</creator><creator>Luthcke, S. B.</creator><creator>Klosko, S. M.</creator><creator>Lemoine, F. G. R.</creator><creator>Chinn, D. S.</creator><creator>McCarthy, J. J.</creator><creator>Cox, C. M.</creator><creator>Anderson, O. B.</creator><general>Blackwell Publishing Ltd</general><general>American Geophysical Union</general><scope>BSCLL</scope><scope>IQODW</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>8FD</scope><scope>FR3</scope><scope>H8D</scope><scope>KR7</scope><scope>L7M</scope></search><sort><creationdate>200502</creationdate><title>Resolving mass flux at high spatial and temporal resolution using GRACE intersatellite measurements</title><author>Rowlands, D. D. ; Luthcke, S. B. ; Klosko, S. M. ; Lemoine, F. G. R. ; Chinn, D. S. ; McCarthy, J. J. ; Cox, C. M. ; Anderson, O. B.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a5111-41ba0e0b967987757c82957aeca66d55d316771f2e0ba3cc2a20de5b3b9d0db73</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2005</creationdate><topic>Amazon Basin</topic><topic>Earth sciences</topic><topic>Earth, ocean, space</topic><topic>Exact sciences and technology</topic><topic>Flux</topic><topic>Geophysics</topic><topic>GRACE (experiment)</topic><topic>Hydrology</topic><topic>Monitors</topic><topic>River basins</topic><topic>Spatial resolution</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Rowlands, D. D.</creatorcontrib><creatorcontrib>Luthcke, S. B.</creatorcontrib><creatorcontrib>Klosko, S. M.</creatorcontrib><creatorcontrib>Lemoine, F. G. R.</creatorcontrib><creatorcontrib>Chinn, D. S.</creatorcontrib><creatorcontrib>McCarthy, J. J.</creatorcontrib><creatorcontrib>Cox, C. M.</creatorcontrib><creatorcontrib>Anderson, O. B.</creatorcontrib><collection>Istex</collection><collection>Pascal-Francis</collection><collection>CrossRef</collection><collection>Technology Research Database</collection><collection>Engineering Research Database</collection><collection>Aerospace Database</collection><collection>Civil Engineering Abstracts</collection><collection>Advanced Technologies Database with Aerospace</collection><jtitle>Geophysical research letters</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Rowlands, D. D.</au><au>Luthcke, S. B.</au><au>Klosko, S. M.</au><au>Lemoine, F. G. R.</au><au>Chinn, D. S.</au><au>McCarthy, J. J.</au><au>Cox, C. M.</au><au>Anderson, O. B.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Resolving mass flux at high spatial and temporal resolution using GRACE intersatellite measurements</atitle><jtitle>Geophysical research letters</jtitle><addtitle>Geophys. Res. Lett</addtitle><date>2005-02</date><risdate>2005</risdate><volume>32</volume><issue>4</issue><spage>L04310.1</spage><epage>n/a</epage><pages>L04310.1-n/a</pages><issn>0094-8276</issn><eissn>1944-8007</eissn><coden>GPRLAJ</coden><abstract>The GRACE mission is designed to monitor mass flux on the Earth's surface at one month and high spatial resolution through the estimation of monthly gravity fields. Although this approach has been largely successful, information at submonthly time scales can be lost or even aliased through the estimation of static monthly parameters. Through an analysis of the GRACE data residuals, we show that the fundamental temporal and spatial resolution of the GRACE data is 10 days and 400 km. We present an approach similar in concept to altimetric methods that recovers submonthly mass flux at a high spatial resolution. Using 4° × 4° blocks at 10‐day intervals, we estimate the mass of surplus or deficit water over a 52° × 60° grid centered on the Amazon basin for July 2003. We demonstrate that the recovered signals are coherent and correlate well with the expected hydrological signal.</abstract><cop>Washington, DC</cop><pub>Blackwell Publishing Ltd</pub><doi>10.1029/2004GL021908</doi><tpages>4</tpages></addata></record> |
fulltext | fulltext |
identifier | ISSN: 0094-8276 |
ispartof | Geophysical research letters, 2005-02, Vol.32 (4), p.L04310.1-n/a |
issn | 0094-8276 1944-8007 |
language | eng |
recordid | cdi_proquest_miscellaneous_1530994788 |
source | Wiley Online Library Free Content; Access via Wiley Online Library; Wiley-Blackwell AGU Digital Library; EZB-FREE-00999 freely available EZB journals |
subjects | Amazon Basin Earth sciences Earth, ocean, space Exact sciences and technology Flux Geophysics GRACE (experiment) Hydrology Monitors River basins Spatial resolution |
title | Resolving mass flux at high spatial and temporal resolution using GRACE intersatellite measurements |
url | https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2024-12-23T04%3A13%3A16IST&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=Resolving%20mass%20flux%20at%20high%20spatial%20and%20temporal%20resolution%20using%20GRACE%20intersatellite%20measurements&rft.jtitle=Geophysical%20research%20letters&rft.au=Rowlands,%20D.%20D.&rft.date=2005-02&rft.volume=32&rft.issue=4&rft.spage=L04310.1&rft.epage=n/a&rft.pages=L04310.1-n/a&rft.issn=0094-8276&rft.eissn=1944-8007&rft.coden=GPRLAJ&rft_id=info:doi/10.1029/2004GL021908&rft_dat=%3Cproquest_cross%3E1530994788%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=1530994788&rft_id=info:pmid/&rfr_iscdi=true |