Assessment and Calibration of ERA5 Severe Winds in the Atlantic Ocean Using Satellite Data

In this paper, we analyze the surface winds of ECMWF ERA5 reanalysis in the Atlantic Ocean. The first part addresses a reanalysis validation, studying the spatial distribution of the errors and the performance as a function of the percentiles, with a further investigation under cyclonic conditions....

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Main Authors: Ricardo M. Campos, Carolina B. Gramcianinov, Ricardo de Camargo, Pedro L. da Silva Dias
Format: Article
Language:English
Published: MDPI AG 2022-10-01
Series:Remote Sensing
Subjects:
Online Access:https://www.mdpi.com/2072-4292/14/19/4918
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author Ricardo M. Campos
Carolina B. Gramcianinov
Ricardo de Camargo
Pedro L. da Silva Dias
author_facet Ricardo M. Campos
Carolina B. Gramcianinov
Ricardo de Camargo
Pedro L. da Silva Dias
author_sort Ricardo M. Campos
collection DOAJ
description In this paper, we analyze the surface winds of ECMWF ERA5 reanalysis in the Atlantic Ocean. The first part addresses a reanalysis validation, studying the spatial distribution of the errors and the performance as a function of the percentiles, with a further investigation under cyclonic conditions. The second part proposes and compares two calibration models, a simple least-squares linear regression (LR) and the quantile mapping method (QM). Our results indicate that ERA5 provides high-quality winds for non-extreme conditions, especially at the eastern boundaries, with bias between −0.5 and 0.3 m/s and RMSE below 1.5 m/s. The reanalysis errors are site-dependent, where large RMSE and severe underestimation are found in tropical latitudes and locations following the warm currents. The most extreme winds in tropical cyclones show the worst results, with RMSE above 5 m/s. Apart from these areas, the strong winds at extratropical locations are well represented. The bias-correction models have proven to be very efficient in removing systematic bias. The LR works well for low-to-mild wind intensities while the QM is better for the upper percentiles and winds above 15 m/s—an improvement of 10% in RMSE and 50% for the bias compared to the original reanalysis is reported.
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spelling doaj.art-894b20e67df2438bafe7d87dc21807d32023-11-23T21:40:53ZengMDPI AGRemote Sensing2072-42922022-10-011419491810.3390/rs14194918Assessment and Calibration of ERA5 Severe Winds in the Atlantic Ocean Using Satellite DataRicardo M. Campos0Carolina B. Gramcianinov1Ricardo de Camargo2Pedro L. da Silva Dias3Cooperative Institute for Marine and Atmospheric Studies (CIMAS), University of Miami, 4600 Rickenbacker Causeway, Miami, FL 33149, USAInstitute for Coastal Systems Analysis and Modeling, Helmholtz-Zentrum Hereon, Max-Planck-Straße 1, 21502 Geesthacht, GermanyDepartamento de Ciências Atmosféricas, Instituto de Astronomia, Geofísica e Ciências Atmosféricas, Universidade de São Paulo, Rua do Matão 1226, Cidade Universitária, São Paulo 05508-000, BrazilDepartamento de Ciências Atmosféricas, Instituto de Astronomia, Geofísica e Ciências Atmosféricas, Universidade de São Paulo, Rua do Matão 1226, Cidade Universitária, São Paulo 05508-000, BrazilIn this paper, we analyze the surface winds of ECMWF ERA5 reanalysis in the Atlantic Ocean. The first part addresses a reanalysis validation, studying the spatial distribution of the errors and the performance as a function of the percentiles, with a further investigation under cyclonic conditions. The second part proposes and compares two calibration models, a simple least-squares linear regression (LR) and the quantile mapping method (QM). Our results indicate that ERA5 provides high-quality winds for non-extreme conditions, especially at the eastern boundaries, with bias between −0.5 and 0.3 m/s and RMSE below 1.5 m/s. The reanalysis errors are site-dependent, where large RMSE and severe underestimation are found in tropical latitudes and locations following the warm currents. The most extreme winds in tropical cyclones show the worst results, with RMSE above 5 m/s. Apart from these areas, the strong winds at extratropical locations are well represented. The bias-correction models have proven to be very efficient in removing systematic bias. The LR works well for low-to-mild wind intensities while the QM is better for the upper percentiles and winds above 15 m/s—an improvement of 10% in RMSE and 50% for the bias compared to the original reanalysis is reported.https://www.mdpi.com/2072-4292/14/19/4918marine surface windssatellite datareanalysis calibrationcyclonic windsbias correction
spellingShingle Ricardo M. Campos
Carolina B. Gramcianinov
Ricardo de Camargo
Pedro L. da Silva Dias
Assessment and Calibration of ERA5 Severe Winds in the Atlantic Ocean Using Satellite Data
Remote Sensing
marine surface winds
satellite data
reanalysis calibration
cyclonic winds
bias correction
title Assessment and Calibration of ERA5 Severe Winds in the Atlantic Ocean Using Satellite Data
title_full Assessment and Calibration of ERA5 Severe Winds in the Atlantic Ocean Using Satellite Data
title_fullStr Assessment and Calibration of ERA5 Severe Winds in the Atlantic Ocean Using Satellite Data
title_full_unstemmed Assessment and Calibration of ERA5 Severe Winds in the Atlantic Ocean Using Satellite Data
title_short Assessment and Calibration of ERA5 Severe Winds in the Atlantic Ocean Using Satellite Data
title_sort assessment and calibration of era5 severe winds in the atlantic ocean using satellite data
topic marine surface winds
satellite data
reanalysis calibration
cyclonic winds
bias correction
url https://www.mdpi.com/2072-4292/14/19/4918
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