Stochastic spatio-temporal model for wind speed variation in the Arctic

A spatio-temporal transformed Gaussian field has been proposed to model wind variability in the northern North Atlantic, but it does not accurately describe the extreme wind speeds attributed to tropical storms and hurricanes. In Rychlik and Mao (2018), this model was generalized by adding certain n...

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Bibliographic Details
Published in:Ocean Engineering
Main Authors: Mao, Wengang, Rychlik, Igor
Language:unknown
Published: 2018
Subjects:
Online Access:https://doi.org/10.1016/j.oceaneng.2018.07.043
https://research.chalmers.se/en/publication/33cd6e8b-cb37-4920-8244-9943e2ead3fd
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author Mao, Wengang
Rychlik, Igor
author_facet Mao, Wengang
Rychlik, Igor
author_sort Mao, Wengang
collection Unknown
container_start_page 237
container_title Ocean Engineering
container_volume 165
description A spatio-temporal transformed Gaussian field has been proposed to model wind variability in the northern North Atlantic, but it does not accurately describe the extreme wind speeds attributed to tropical storms and hurricanes. In Rychlik and Mao (2018), this model was generalized by adding certain number of random components to model rare events with extreme wind speeds or severe storms, and was named the hybrid model.In this study, these models are further developed and validated to properly describe the variation of wind speeds in the Arctic area. In most locations, the transformed Gaussian field is a sufficiently accurate model. However, in some regions, e.g., the Laptev and Beaufort Seas, this model severely underestimates the frequencies of extreme wind speeds. Therefore, the hybrid model is further improved to add Poisson distributed random storm events to describe the wind variation in these regions, and is named as the Poisson hybrid model. There are also locations, e.g., along the east coast of Greenland, where the frequencies of high wind speeds are severely overestimated by the transformed Gaussian model. It is shown that this model can be used to estimate the long-term distribution of wind speeds, predict extreme wind speeds and simulate the spatio-temporal wind fields for practical applications.
genre Arctic
Greenland
laptev
North Atlantic
genre_facet Arctic
Greenland
laptev
North Atlantic
geographic Arctic
Greenland
geographic_facet Arctic
Greenland
id ftchalmersuniv:oai:research.chalmers.se:506436
institution Open Polar
language unknown
op_collection_id ftchalmersuniv
op_container_end_page 251
op_doi https://doi.org/10.1016/j.oceaneng.2018.07.043
op_relation http://dx.doi.org/10.1016/j.oceaneng.2018.07.043
publishDate 2018
record_format openpolar
spelling ftchalmersuniv:oai:research.chalmers.se:506436 2025-06-15T14:20:22+00:00 Stochastic spatio-temporal model for wind speed variation in the Arctic Mao, Wengang Rychlik, Igor 2018 text https://doi.org/10.1016/j.oceaneng.2018.07.043 https://research.chalmers.se/en/publication/33cd6e8b-cb37-4920-8244-9943e2ead3fd unknown http://dx.doi.org/10.1016/j.oceaneng.2018.07.043 Vehicle Engineering Oceanography Hydrology Water Resources Probability Theory and Statistics Wind speed Spatio-temporal wind statistics Hermite transformation Exponential transformation The Arctic Extreme wind Poisson hybrid model Gaussian field 2018 ftchalmersuniv https://doi.org/10.1016/j.oceaneng.2018.07.043 2025-05-19T04:26:16Z A spatio-temporal transformed Gaussian field has been proposed to model wind variability in the northern North Atlantic, but it does not accurately describe the extreme wind speeds attributed to tropical storms and hurricanes. In Rychlik and Mao (2018), this model was generalized by adding certain number of random components to model rare events with extreme wind speeds or severe storms, and was named the hybrid model.In this study, these models are further developed and validated to properly describe the variation of wind speeds in the Arctic area. In most locations, the transformed Gaussian field is a sufficiently accurate model. However, in some regions, e.g., the Laptev and Beaufort Seas, this model severely underestimates the frequencies of extreme wind speeds. Therefore, the hybrid model is further improved to add Poisson distributed random storm events to describe the wind variation in these regions, and is named as the Poisson hybrid model. There are also locations, e.g., along the east coast of Greenland, where the frequencies of high wind speeds are severely overestimated by the transformed Gaussian model. It is shown that this model can be used to estimate the long-term distribution of wind speeds, predict extreme wind speeds and simulate the spatio-temporal wind fields for practical applications. Other/Unknown Material Arctic Greenland laptev North Atlantic Unknown Arctic Greenland Ocean Engineering 165 237 251
spellingShingle Vehicle Engineering
Oceanography
Hydrology
Water Resources
Probability Theory and Statistics
Wind speed
Spatio-temporal wind statistics
Hermite transformation
Exponential transformation
The Arctic
Extreme wind
Poisson hybrid model
Gaussian field
Mao, Wengang
Rychlik, Igor
Stochastic spatio-temporal model for wind speed variation in the Arctic
title Stochastic spatio-temporal model for wind speed variation in the Arctic
title_full Stochastic spatio-temporal model for wind speed variation in the Arctic
title_fullStr Stochastic spatio-temporal model for wind speed variation in the Arctic
title_full_unstemmed Stochastic spatio-temporal model for wind speed variation in the Arctic
title_short Stochastic spatio-temporal model for wind speed variation in the Arctic
title_sort stochastic spatio-temporal model for wind speed variation in the arctic
topic Vehicle Engineering
Oceanography
Hydrology
Water Resources
Probability Theory and Statistics
Wind speed
Spatio-temporal wind statistics
Hermite transformation
Exponential transformation
The Arctic
Extreme wind
Poisson hybrid model
Gaussian field
topic_facet Vehicle Engineering
Oceanography
Hydrology
Water Resources
Probability Theory and Statistics
Wind speed
Spatio-temporal wind statistics
Hermite transformation
Exponential transformation
The Arctic
Extreme wind
Poisson hybrid model
Gaussian field
url https://doi.org/10.1016/j.oceaneng.2018.07.043
https://research.chalmers.se/en/publication/33cd6e8b-cb37-4920-8244-9943e2ead3fd