A comparison of the annual cycle of sea level in coastal areas from gridded satellite altimetry and tide gauges
In this work we compare the annual component of sea level variations derived from 478 worldwide-distributed tide gauges with the annual component computed from a weekly gridded multi-mission altimeter product. Gridded altimetry data products allow for spatio-temporal analyses that are not possible b...
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| Otros Autores: | , , , |
| Formato: | Capítulo de libro |
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Elsevier Ltd
2015
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| LEADER | 16100caa a22011777a 4500 | ||
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| 001 | PAPER-24874 | ||
| 003 | AR-BaUEN | ||
| 005 | 20250217112411.0 | ||
| 008 | 190411s2015 xx ||||fo|||| 00| 0 eng|d | ||
| 024 | 7 | |2 scopus |a 2-s2.0-84918826512 | |
| 030 | |a CSHRD | ||
| 040 | |a Scopus |b spa |c AR-BaUEN |d AR-BaUEN | ||
| 100 | 1 | |a Ruiz Etcheverry, L.A. | |
| 245 | 1 | 2 | |a A comparison of the annual cycle of sea level in coastal areas from gridded satellite altimetry and tide gauges |
| 260 | |b Elsevier Ltd |c 2015 | ||
| 270 | 1 | 0 | |m Saraceno, M.; Centro de Investigación del Mar y la AtmósferaArgentina |
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| 506 | |2 openaire |e Política editorial | ||
| 520 | 3 | |a In this work we compare the annual component of sea level variations derived from 478 worldwide-distributed tide gauges with the annual component computed from a weekly gridded multi-mission altimeter product. Gridded altimetry data products allow for spatio-temporal analyses that are not possible based on along-track altimetry data. However, a precise validation is necessary in the coastal region before the gridded data can be used. Results of the comparisons show that root-mean-square differences (RMSD) between the two datasets are ≤2. cm for 76.4% of the sites. RMSD higher than 4. cm are caused by narrow coastal currents, nearby river outflows or other local phenomena. A methodology is proposed to assess the accuracy of the seasonal component of the gridded altimeter product in regions with a low density net of tide gauges. As a case study it is shown that the Southwestern Atlantic coast is a suitable region to study the spatio-temporal variability of the annual cycle of sea level since RMSD between annual altimetry data and in-situ data are lower than 2.1. cm. © 2014 Elsevier Ltd. |l eng | |
| 536 | |a Detalles de la financiación: National Science Foundation, GEO-1128040 | ||
| 536 | |a Detalles de la financiación: Agenzia Regionale per i Parchi, 3070 | ||
| 536 | |a Detalles de la financiación: Inter-American Institute for Global Change Research | ||
| 536 | |a Detalles de la financiación: This study is a contribution to EUMETSAT/CNES DSP/OT/12-2118 , ANPCyT PICT 2012-0467 , CONICET PIP 112-20110100176 , PIO 133-20130100242 , CONAE-001 and UBACyT 20020100100840 Projects. ARP and OOM acknowledge the support of Grant 3070 from the Inter-American Institute for Global Change Research ( National Science Foundation Grant GEO-1128040 ). The altimeter products were produced by SSALTO/DUACS and distributed by Aviso with support from CNES. Dynamic atmospheric Corrections are produced by CLS Space Oceanography Division using the Mog2D model from Legos and distributed by Aviso, with support from CNES (http://www.aviso.oceanobs.com/). Comments by two anonymous reviewers help improve the paper. | ||
| 593 | |a Departamento de Ciencias de la Atmósfera y los Océanos, Universidad de Buenos Aires, Buenos Aires, Argentina | ||
| 593 | |a Centro de Investigación del Mar y la Atmósfera, Buenos Aires, Argentina | ||
| 593 | |a Instituto Franco Argentino para el estudio del clima y sus impactos (UMI-IFAECI), Argentina | ||
| 593 | |a Departamento Oceanografía, Servicio de Hidrografía Naval, Argentina | ||
| 593 | |a Collecte Localisation Satellites (CLS), Toulouse, France | ||
| 593 | |a Instituto de Oceanografia, Universidade de Federal do Rio Grande, Rio Grande, Brazil | ||
| 690 | 1 | 0 | |a ALTIMETRY |
| 690 | 1 | 0 | |a ANNUAL CYCLE |
| 690 | 1 | 0 | |a COASTAL AREA |
| 690 | 1 | 0 | |a SEA LEVEL ANOMALY |
| 690 | 1 | 0 | |a TIDE GAUGES |
| 690 | 1 | 0 | |a ASSESSMENT METHOD |
| 690 | 1 | 0 | |a COASTAL CURRENT |
| 690 | 1 | 0 | |a COASTAL ZONE |
| 690 | 1 | 0 | |a COMPARATIVE STUDY |
| 690 | 1 | 0 | |a SATELLITE ALTIMETRY |
| 690 | 1 | 0 | |a SATELLITE DATA |
| 690 | 1 | 0 | |a SEA LEVEL CHANGE |
| 690 | 1 | 0 | |a TIDE GAUGE |
| 690 | 1 | 0 | |a ATLANTIC OCEAN |
| 690 | 1 | 0 | |a ATLANTIC OCEAN (SOUTHWEST) |
| 700 | 1 | |a Saraceno, Martín | |
| 700 | 1 | |a Piola, A.R. | |
| 700 | 1 | |a Valladeau, G. | |
| 700 | 1 | |a Möller, O.O. | |
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