Reconstructed Wind Fields from Multi-Satellite Observations

We present and validate a method of reconstructing high-resolution sea surface wind fields from multi-sensor satellite data over the Grand Banks of Newfoundland off Atlantic Canada. Six-hourly ocean wind fields from blended products (including multi-satellite measurements) with 0.25° spatial resolut...

Full description

Bibliographic Details
Published in:Remote Sensing
Main Authors: Ruohan Tang, Deyou Liu, Guoqi Han, Zhimin Ma, Brad de Young
Format: Article in Journal/Newspaper
Language:English
Published: MDPI AG 2014
Subjects:
SAR
Q
Online Access:https://doi.org/10.3390/rs6042898
https://doaj.org/article/86d0642707f34da48322ebdf379a684b
id ftdoajarticles:oai:doaj.org/article:86d0642707f34da48322ebdf379a684b
record_format openpolar
spelling ftdoajarticles:oai:doaj.org/article:86d0642707f34da48322ebdf379a684b 2023-05-15T17:22:20+02:00 Reconstructed Wind Fields from Multi-Satellite Observations Ruohan Tang Deyou Liu Guoqi Han Zhimin Ma Brad de Young 2014-03-01T00:00:00Z https://doi.org/10.3390/rs6042898 https://doaj.org/article/86d0642707f34da48322ebdf379a684b EN eng MDPI AG http://www.mdpi.com/2072-4292/6/4/2898 https://doaj.org/toc/2072-4292 2072-4292 doi:10.3390/rs6042898 https://doaj.org/article/86d0642707f34da48322ebdf379a684b Remote Sensing, Vol 6, Iss 4, Pp 2898-2911 (2014) sea surface winds SAR scatterometer reconstruction heapsort bucket method topdown search modified Gauss–Markov theorem Science Q article 2014 ftdoajarticles https://doi.org/10.3390/rs6042898 2022-12-31T10:54:09Z We present and validate a method of reconstructing high-resolution sea surface wind fields from multi-sensor satellite data over the Grand Banks of Newfoundland off Atlantic Canada. Six-hourly ocean wind fields from blended products (including multi-satellite measurements) with 0.25° spatial resolution and 226 RADARSAT-2 synthetic aperture radar (SAR) wind fields with 1-km spatial resolution have been used to reconstruct new six-hourly wind fields with a resolution of 10 km for the period from August 2008 to December 2010, except July 2009 to November 2009. The reconstruction process is based on the heapsort bucket method with topdown search and the modified Gauss–Markov theorem. The result shows that the mean difference between the reconstructed wind speed and buoy-estimated wind speed is smaller than 0.6 m/s, and the standard deviation is smaller than 2.5 m/s. The mean difference in wind direction between reconstructed and buoy estimates is 3.7°; the standard deviation is 40.2°. There is fair agreement between the reconstructed wind vectors and buoy-estimated ones. Article in Journal/Newspaper Newfoundland Directory of Open Access Journals: DOAJ Articles Canada Remote Sensing 6 4 2898 2911
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic sea surface winds
SAR
scatterometer
reconstruction
heapsort bucket method
topdown search
modified Gauss–Markov theorem
Science
Q
spellingShingle sea surface winds
SAR
scatterometer
reconstruction
heapsort bucket method
topdown search
modified Gauss–Markov theorem
Science
Q
Ruohan Tang
Deyou Liu
Guoqi Han
Zhimin Ma
Brad de Young
Reconstructed Wind Fields from Multi-Satellite Observations
topic_facet sea surface winds
SAR
scatterometer
reconstruction
heapsort bucket method
topdown search
modified Gauss–Markov theorem
Science
Q
description We present and validate a method of reconstructing high-resolution sea surface wind fields from multi-sensor satellite data over the Grand Banks of Newfoundland off Atlantic Canada. Six-hourly ocean wind fields from blended products (including multi-satellite measurements) with 0.25° spatial resolution and 226 RADARSAT-2 synthetic aperture radar (SAR) wind fields with 1-km spatial resolution have been used to reconstruct new six-hourly wind fields with a resolution of 10 km for the period from August 2008 to December 2010, except July 2009 to November 2009. The reconstruction process is based on the heapsort bucket method with topdown search and the modified Gauss–Markov theorem. The result shows that the mean difference between the reconstructed wind speed and buoy-estimated wind speed is smaller than 0.6 m/s, and the standard deviation is smaller than 2.5 m/s. The mean difference in wind direction between reconstructed and buoy estimates is 3.7°; the standard deviation is 40.2°. There is fair agreement between the reconstructed wind vectors and buoy-estimated ones.
format Article in Journal/Newspaper
author Ruohan Tang
Deyou Liu
Guoqi Han
Zhimin Ma
Brad de Young
author_facet Ruohan Tang
Deyou Liu
Guoqi Han
Zhimin Ma
Brad de Young
author_sort Ruohan Tang
title Reconstructed Wind Fields from Multi-Satellite Observations
title_short Reconstructed Wind Fields from Multi-Satellite Observations
title_full Reconstructed Wind Fields from Multi-Satellite Observations
title_fullStr Reconstructed Wind Fields from Multi-Satellite Observations
title_full_unstemmed Reconstructed Wind Fields from Multi-Satellite Observations
title_sort reconstructed wind fields from multi-satellite observations
publisher MDPI AG
publishDate 2014
url https://doi.org/10.3390/rs6042898
https://doaj.org/article/86d0642707f34da48322ebdf379a684b
geographic Canada
geographic_facet Canada
genre Newfoundland
genre_facet Newfoundland
op_source Remote Sensing, Vol 6, Iss 4, Pp 2898-2911 (2014)
op_relation http://www.mdpi.com/2072-4292/6/4/2898
https://doaj.org/toc/2072-4292
2072-4292
doi:10.3390/rs6042898
https://doaj.org/article/86d0642707f34da48322ebdf379a684b
op_doi https://doi.org/10.3390/rs6042898
container_title Remote Sensing
container_volume 6
container_issue 4
container_start_page 2898
op_container_end_page 2911
_version_ 1766108915153502208