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Registros recuperados: 7
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Impact des fines échelles spatio-temporelles de l'atmosphère sur le couplage entre océan hauturier et plateau continental dans un système d'upwelling de bord est ArchiMer
Desbiolles, Fabien.
This study focuses on the oceanic response to fine atmospheric spatial and temporal scales, and especially fine wind patterns in the Benguela and Canary upwelling systems. These regions are under the influence of local or regional wind, blowing parallel to the coast. The wind is the main driver of the cold-water upwelling and is modulated by several physical processes at various scales. The nature of the interactions with the atmosphere, the ocean and the adjacent continent differs according to these processes. For the past 20 years, outstanding efforts have been made in the description and understanding of the atmospheric conditions at the sea surface. An increasing number of space missions and major technical improvements have allowed refinement of the...
Tipo: Text Palavras-chave: Système d'upwelling de bord Est; Fines échelles atmosphériques; Interactions air-mer; Profil du vent à la côte; Diffusiométrie; Modélisation numérique; Eastern boundary upwelling system; Atmospheric fine scales; Air-sea interactions; Coastal wind profile; Scatterometry; Numerical model..
Ano: 2014 URL: http://archimer.ifremer.fr/doc/00405/51693/52257.pdf
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Homogenization of scatterometer wind retrievals ArchiMer
Bentamy, Abderrahim; Grodsky, Semyon A.; Elyouncha, Anis; Chapron, Bertrand; Desbiolles, Fabien.
Surface winds (10 m equivalent neutral wind velocity) from scatterometer missions since 1992 to present require homogenization to meet the requirements for oceanic and atmospheric climate data records. Sources of differences between winds retrieved from different scatterometer measurements mainly arise from calibration/validation procedures used for each scatterometer and differences in measurement physics. In this study, we focus on the calibration/validation component of the European Remote Sensing Satellite (ERS)-1 and ERS-2 wind speed biases. ERS-1 and ERS-2 data, named as WNF products, are from the Institut Français de Recherche pour l'Exploitation de la MER (IFREMER). In addition to WNF data, the newly calibrated ERS-2 products provided by the...
Tipo: Text Palavras-chave: Scatterometer; Surface wind; Homogenization.
Ano: 2017 URL: http://archimer.ifremer.fr/doc/00334/44536/44468.pdf
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Two Decades [1992-2012] of Surface Wind Analyses based on Satellite Scatterometer Observations ArchiMer
Desbiolles, Fabien; Bentamy, Abderrahim; Blanke, Bruno; Roy, Claude; Mestas-nunez, Alberto M.; Grodsky, Semyon A.; Herbette, Steven; Cambon, Gildas; Maes, Christophe.
Surface winds (equivalent neutral wind velocities at 10 m) from scatterometer missions since 1992 have been used to build up a 20-year climate series. Optimal interpolation and kriging methods have been applied to continuously provide surface wind speed and direction estimates over the global ocean on a regular grid in space and time. The use of other data sources such as radiometer data (SSM/I) and atmospheric wind reanalyses (ERA-Interim) has allowed building a blended product available at 1/4° spatial resolution and every 6 hours from 1992 to 2012. Sampling issues throughout the different missions (ERS-1, ERS-2, QuikSCAT, and ASCAT) and their possible impact on the homogeneity of the gridded product are discussed. In addition, we assess carefully the...
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Ano: 2017 URL: http://archimer.ifremer.fr/doc/00366/47686/47725.pdf
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Improvement in airsea flux estimates derived from satellite observations ArchiMer
Bentamy, Abderrahim; Grodsky, Semyon A.; Katsaros, Kristina; Mestas-nunez, Alberto M.; Blanke, Bruno; Desbiolles, Fabien.
A new method is developed to estimate daily turbulent airsea fluxes over the global ocean on a 0.25 degrees grid. The required surface wind speed (w(10)) and specific air humidity (q(10)) at 10m height are both estimated from remotely sensed measurements. w(10) is obtained from the SeaWinds scatterometer on board the QuikSCAT satellite. A new empirical model relating brightness temperatures (T-b) from the Special Sensor Microwave Imager (SSM/I) and q(10) is developed. It is an extension of the author's previous q(10) model. In addition to T-b, the empirical model includes sea surface temperature (SST) and airsea temperature difference data. The calibration of the new empirical q(10) model utilizes q(10) from the latest version of the National Oceanography...
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Ano: 2013 URL: http://archimer.ifremer.fr/doc/00137/24825/23575.pdf
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Short-term upwelling events at the western African coast related to synoptic atmospheric structures as derived from satellite observations ArchiMer
Desbiolles, Fabien; Blanke, Bruno; Bentamy, Abderrahim.
Satellite scatterometers provide continuously valuable surface wind speed and direction estimates over the global ocean on a regular grid both in space and time. The Level 3 data derived from the Advanced Scatterometer (ASCAT), available at 1/4° spatial resolution (hereafter AS25), and Quick Scatterometer (QuikSCAT), available on 1/2° and 1/4° horizontal grids (QS50 and QS25, respectively), are studied at regional scales in both the Benguela and Canary upwelling systems. They are compared to the European Center for Medium-Range Weather Forecast surface wind analysis, with insight into their intrinsic and actual spatial resolutions. In the coastal band, the finest spatial patterns are found in the QS25 winds and are O(75 km). This demonstrates the...
Tipo: Text Palavras-chave: Satellite scatterometer wind fields; Actual wind resolution at regional scales; Short-lived SST anomalies; Eastern-boundary upwelling systems; Modeling.
Ano: 2014 URL: http://archimer.ifremer.fr/doc/00172/28333/26619.pdf
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Origin of fine-scale wind stress curl structures in the Benguela and Canary upwelling systems ArchiMer
Desbiolles, Fabien; Blanke, Bruno; Bentamy, Abderrahim; Grima, Nicolas.
Numerous studies have shown the primary importance of wind stress curl in coastal upwelling dynamics. The main goal of this new analysis is to describe the QuikSCAT surface wind stress curl at various scales in the Benguela and Canary upwelling systems. The dominant spatial pattern is characterized by cyclonic curl near continental boundaries and anticyclonic curl offshore, in association with equatorward alongshore (upwelling favorable) wind stress. At a smaller scale, we demonstrate the sensitivity of the QuikSCAT wind stress curl to coastal processes related to sea surface temperature (SST) mesoscale fluctuations by presenting a linear relationship between the curl and crosswind SST gradients. Despite the spatial and temporal sensitivity of the...
Tipo: Text Palavras-chave: Wind stress; Upwelling; SST-wind interactions.
Ano: 2014 URL: http://archimer.ifremer.fr/doc/00233/34412/32820.pdf
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Response of the Southern Benguela upwelling system to fine-scale modifications of the coastal wind ArchiMer
Desbiolles, Fabien; Blanke, Bruno; Bentamy, Abderrahim; Roy, C..
We analyze the results of a regional model of the Southern Benguela upwelling system forced by wind stress fields derived from QuikSCAT observations. Two different horizontal resolutions are considered for the wind stress: QS25 and QS50, corresponding to native 25 and 50 km grids, respectively. The differences between both products highlight the primary importance of fine-scale momentum fluxes for both the structure and intensity of the wind- and wind curl-driven upwelling. Using QS25, we show that the coastal Ekman transport is reduced, leading to a warmer SST and a reduced oceanic coastal jet. QS25 finer wind stress curl patterns also favor the development of a stronger and shallower poleward undercurrent. The addition of a coastal wind correction to...
Tipo: Text Palavras-chave: Eastern boundary upwelling system; Momentum flux forcing; Wind profile; Numerical modeling; Scatterometry.
Ano: 2016 URL: https://archimer.ifremer.fr/doc/00302/41339/40525.pdf
Registros recuperados: 7
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