Development of a Global Scatterometer Validation and Monitoring

37 pages Stoffelen (1998b) developed an advanced validation model for winds over the ocean based on triple collocation of scatterometer, buoy, and Numerical Weather Prediction (NWP )model winds. This method has been further tested in the tropical region for wind (Djepa, 2001) and been extended to wi...

Full description

Bibliographic Details
Main Authors: Portabella, Marcos, Stoffelen, Ad
Format: Report
Language:English
Published: 2007
Subjects:
Online Access:http://hdl.handle.net/10261/257167
id ftcsic:oai:digital.csic.es:10261/257167
record_format openpolar
spelling ftcsic:oai:digital.csic.es:10261/257167 2024-02-11T09:56:26+01:00 Development of a Global Scatterometer Validation and Monitoring Portabella, Marcos Stoffelen, Ad 2007-07 http://hdl.handle.net/10261/257167 en eng No Scientific Report SAF/OSI/CDOP/KNMI/SCI/RP/141: 1-37 (2007) http://hdl.handle.net/10261/257167 open informe técnico http://purl.org/coar/resource_type/c_18gh 2007 ftcsic 2024-01-16T11:17:05Z 37 pages Stoffelen (1998b) developed an advanced validation model for winds over the ocean based on triple collocation of scatterometer, buoy, and Numerical Weather Prediction (NWP )model winds. This method has been further tested in the tropical region for wind (Djepa, 2001) and been extended to wind stress modelling in the context of the Climate Monitoring (CM) Satellite Application Facility (SAF) (Stoffelen et al, 2006). In line with user and reviewer recommendations for further validation, we here report on the extension of this activity to the extra-tropics in an Ocean & Sea Ice (OSI )SAF Visiting Scientist (VS) study. Wind forces motion in the ocean and in turn the motion in the ocean determines the weather and climate in large portions of the world. Wind forcing is essential in the El Niño Southern Oscillation (ENSO) and other ocean-atmosphere interaction phenomena, occurring in the Tropics. As such, a homogeneous wind data set of high quality would much advance research on the prediction and mechanisms of seasonal forecasting. Vialard (2000) emphasizes that wind stress is certainly the most important forcing in the tropics. Moreover, ocean circulation and ENSO play a key role in the Earth’ climate. Besides tropical needs, obvious applications of such wind stress product would be among others in the modelling of the Antarctic circumpolar current, forcing of the southern oceans, research on the variability and occurrence of storms, and forcing in complex basins, e.g., the Mediterranean. Complementary to buoy observations, it would be useful to have continuous wind stress time series of high temporal and spatial resolution, extending beyond the buoy area. This would aid in the understanding of the unexplained variability of these wind events from year to year. [.] Peer reviewed Report Antarc* Antarctic Sea ice Digital.CSIC (Spanish National Research Council) Antarctic The Antarctic
institution Open Polar
collection Digital.CSIC (Spanish National Research Council)
op_collection_id ftcsic
language English
description 37 pages Stoffelen (1998b) developed an advanced validation model for winds over the ocean based on triple collocation of scatterometer, buoy, and Numerical Weather Prediction (NWP )model winds. This method has been further tested in the tropical region for wind (Djepa, 2001) and been extended to wind stress modelling in the context of the Climate Monitoring (CM) Satellite Application Facility (SAF) (Stoffelen et al, 2006). In line with user and reviewer recommendations for further validation, we here report on the extension of this activity to the extra-tropics in an Ocean & Sea Ice (OSI )SAF Visiting Scientist (VS) study. Wind forces motion in the ocean and in turn the motion in the ocean determines the weather and climate in large portions of the world. Wind forcing is essential in the El Niño Southern Oscillation (ENSO) and other ocean-atmosphere interaction phenomena, occurring in the Tropics. As such, a homogeneous wind data set of high quality would much advance research on the prediction and mechanisms of seasonal forecasting. Vialard (2000) emphasizes that wind stress is certainly the most important forcing in the tropics. Moreover, ocean circulation and ENSO play a key role in the Earth’ climate. Besides tropical needs, obvious applications of such wind stress product would be among others in the modelling of the Antarctic circumpolar current, forcing of the southern oceans, research on the variability and occurrence of storms, and forcing in complex basins, e.g., the Mediterranean. Complementary to buoy observations, it would be useful to have continuous wind stress time series of high temporal and spatial resolution, extending beyond the buoy area. This would aid in the understanding of the unexplained variability of these wind events from year to year. [.] Peer reviewed
format Report
author Portabella, Marcos
Stoffelen, Ad
spellingShingle Portabella, Marcos
Stoffelen, Ad
Development of a Global Scatterometer Validation and Monitoring
author_facet Portabella, Marcos
Stoffelen, Ad
author_sort Portabella, Marcos
title Development of a Global Scatterometer Validation and Monitoring
title_short Development of a Global Scatterometer Validation and Monitoring
title_full Development of a Global Scatterometer Validation and Monitoring
title_fullStr Development of a Global Scatterometer Validation and Monitoring
title_full_unstemmed Development of a Global Scatterometer Validation and Monitoring
title_sort development of a global scatterometer validation and monitoring
publishDate 2007
url http://hdl.handle.net/10261/257167
geographic Antarctic
The Antarctic
geographic_facet Antarctic
The Antarctic
genre Antarc*
Antarctic
Sea ice
genre_facet Antarc*
Antarctic
Sea ice
op_relation No
Scientific Report SAF/OSI/CDOP/KNMI/SCI/RP/141: 1-37 (2007)
http://hdl.handle.net/10261/257167
op_rights open
_version_ 1790603066172506112