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Article

A Statistical–Dynamical Downscaling Technique for Wind Resource Mapping: A Regional Atmospheric-Circulation-Type Approach with Numerical Weather Prediction Modeling

by
Xsitaaz T. Chadee
1,*,
Naresh R. Seegobin
2,† and
Ricardo M. Clarke
1
1
Environmental Physics Lab, Department of Physics, Faculty of Science and Technology, The University of the West Indies, St. Augustine Campus, Circular Road, St. Augustine 330912, Trinidad and Tobago
2
Department of Computing and Information Technology, Faculty of Science and Technology, The University of the West Indies, St. Augustine Campus, Circular Road, St. Augustine 330912, Trinidad and Tobago
*
Author to whom correspondence should be addressed.
Current address: Campus Information Technology Services, The University of the West Indies, St. Augustine Campus, Circular Road, St. Augustine 330912, Trinidad and Tobago.
Wind 2025, 5(1), 7; https://doi.org/10.3390/wind5010007 (registering DOI)
Submission received: 26 November 2024 / Revised: 19 February 2025 / Accepted: 20 February 2025 / Published: 1 March 2025

Abstract

Many Caribbean low-latitude small island states lack wind maps tailored to capture their wind features at high resolutions. However, high-resolution mesoscale modeling is computationally expensive. This study proposes a statistical–dynamical downscaling (SDD) method that integrates an atmospheric-circulation-type (CT) approach with a high-resolution numerical weather prediction (NWP) model to map the wind resources of a case study, Trinidad and Tobago. The SDD method uses a novel wind class generation technique derived directly from reanalysis wind field patterns. For the Caribbean, 82 wind classes were defined from an atmospheric circulation catalog of seven types derived from 850 hPa daily wind fields from the NCEP-DOE reanalysis over 32 years. Each wind class was downscaled using the Weather Research and Forecasting (WRF) model and weighted by frequency to produce 1 km × 1 km climatological wind maps. The 10 m wind maps, validated using measured wind data at Piarco and Crown Point, exhibit a small positive average bias (+0.5 m/s in wind speed and +11 W m−2 in wind power density (WPD)) and capture the shape of the wind speed distributions and a significant proportion of the interannual variability. The 80 m wind map indicates from good to moderate wind resources, suitable for determining priority areas for a detailed wind measurement program in Trinidad and Tobago. The proposed SDD methodology is applicable to other regions worldwide beyond low-latitude tropical islands.
Keywords: wind map; numerical weather prediction model; statistical–dynamical downscaling; atmospheric circulation type; small island; tropical; Trinidad and Tobago; Caribbean; wind energy wind map; numerical weather prediction model; statistical–dynamical downscaling; atmospheric circulation type; small island; tropical; Trinidad and Tobago; Caribbean; wind energy

Share and Cite

MDPI and ACS Style

Chadee, X.T.; Seegobin, N.R.; Clarke, R.M. A Statistical–Dynamical Downscaling Technique for Wind Resource Mapping: A Regional Atmospheric-Circulation-Type Approach with Numerical Weather Prediction Modeling. Wind 2025, 5, 7. https://doi.org/10.3390/wind5010007

AMA Style

Chadee XT, Seegobin NR, Clarke RM. A Statistical–Dynamical Downscaling Technique for Wind Resource Mapping: A Regional Atmospheric-Circulation-Type Approach with Numerical Weather Prediction Modeling. Wind. 2025; 5(1):7. https://doi.org/10.3390/wind5010007

Chicago/Turabian Style

Chadee, Xsitaaz T., Naresh R. Seegobin, and Ricardo M. Clarke. 2025. "A Statistical–Dynamical Downscaling Technique for Wind Resource Mapping: A Regional Atmospheric-Circulation-Type Approach with Numerical Weather Prediction Modeling" Wind 5, no. 1: 7. https://doi.org/10.3390/wind5010007

APA Style

Chadee, X. T., Seegobin, N. R., & Clarke, R. M. (2025). A Statistical–Dynamical Downscaling Technique for Wind Resource Mapping: A Regional Atmospheric-Circulation-Type Approach with Numerical Weather Prediction Modeling. Wind, 5(1), 7. https://doi.org/10.3390/wind5010007

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