Observation and Simulation of Wind Speed and Wind Power Density over Bac Lieu Region

In this study, the WRF (Weather Research and Forecasting) model was used to simulate and investigate diurnal and annual variations of wind speed and wind power density over Southern Vietnam at 2‐km horizontal resolution for two years (2016 and 2017). The model initial and boundary conditions are fro...

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Main Authors: Hiep Van Nguyen, Pham Xuan Thanh, Nguyen Duc Nam, Nguyen Xuan Anh, Pham Le Khuong, Hoang Hai Son, Nguyen Tien Manh, Pham Chi Cong
Format: Article
Language:English
Published: Wiley 2021-01-01
Series:Advances in Meteorology
Online Access:http://dx.doi.org/10.1155/2021/8823940
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author Hiep Van Nguyen
Pham Xuan Thanh
Nguyen Duc Nam
Nguyen Xuan Anh
Pham Le Khuong
Hoang Hai Son
Nguyen Tien Manh
Pham Chi Cong
author_facet Hiep Van Nguyen
Pham Xuan Thanh
Nguyen Duc Nam
Nguyen Xuan Anh
Pham Le Khuong
Hoang Hai Son
Nguyen Tien Manh
Pham Chi Cong
author_sort Hiep Van Nguyen
collection DOAJ
description In this study, the WRF (Weather Research and Forecasting) model was used to simulate and investigate diurnal and annual variations of wind speed and wind power density over Southern Vietnam at 2‐km horizontal resolution for two years (2016 and 2017). The model initial and boundary conditions are from the National Centers for Environmental Prediction (NCEP) Final Analyses (FNL). Observation data for two years at 20 m height at Bac Lieu station were used for model bias correction and investigating diurnal and annual variation of wind speeds. The results show that the WRF model overestimates wind speeds. After bias correction, the model reasonably well simulates wind speeds over the research area. Wind speed and wind power density show much higher values at levels of 50–200 m above ground levels than near ground (20 m) level and significantly higher near the coastal regions than inland. Wind speed has significant annual and diurnal cycles. Both annual and diurnal cycles of wind speeds were well simulated by the model. Wind speed is much stronger during daytime than at nighttime. Low-level wind speed reaches the maximum at about 14 LT to 15 LT when the vertical momentum mixing is highly active. Wind speeds over the eastern coastal region of Southern Vietnam are much stronger in winter than in summer due to two main reasons, including (1) stronger large-scale wind speed in winter than in summer and (2) funnel effect creating a local maximum wind speed over the nearshore ocean which then transports high-momentum air inland in winter.
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spelling doaj-art-bb85e7f9098048049cc1ed5752fcbd4c2025-02-03T05:58:21ZengWileyAdvances in Meteorology1687-93091687-93172021-01-01202110.1155/2021/88239408823940Observation and Simulation of Wind Speed and Wind Power Density over Bac Lieu RegionHiep Van Nguyen0Pham Xuan Thanh1Nguyen Duc Nam2Nguyen Xuan Anh3Pham Le Khuong4Hoang Hai Son5Nguyen Tien Manh6Pham Chi Cong7Institute of Geophysics (IGP), Vietnam Academy of Science and Technology (VAST), Hanoi, VietnamInstitute of Geophysics (IGP), Vietnam Academy of Science and Technology (VAST), Hanoi, VietnamInstitute of Geophysics (IGP), Vietnam Academy of Science and Technology (VAST), Hanoi, VietnamInstitute of Geophysics (IGP), Vietnam Academy of Science and Technology (VAST), Hanoi, VietnamInstitute of Geophysics (IGP), Vietnam Academy of Science and Technology (VAST), Hanoi, VietnamInstitute of Geophysics (IGP), Vietnam Academy of Science and Technology (VAST), Hanoi, VietnamInstitute of Geophysics (IGP), Vietnam Academy of Science and Technology (VAST), Hanoi, VietnamVietnam Research Institute of Electronics, Informatics and Automation (VIELINA), Hanoi, VietnamIn this study, the WRF (Weather Research and Forecasting) model was used to simulate and investigate diurnal and annual variations of wind speed and wind power density over Southern Vietnam at 2‐km horizontal resolution for two years (2016 and 2017). The model initial and boundary conditions are from the National Centers for Environmental Prediction (NCEP) Final Analyses (FNL). Observation data for two years at 20 m height at Bac Lieu station were used for model bias correction and investigating diurnal and annual variation of wind speeds. The results show that the WRF model overestimates wind speeds. After bias correction, the model reasonably well simulates wind speeds over the research area. Wind speed and wind power density show much higher values at levels of 50–200 m above ground levels than near ground (20 m) level and significantly higher near the coastal regions than inland. Wind speed has significant annual and diurnal cycles. Both annual and diurnal cycles of wind speeds were well simulated by the model. Wind speed is much stronger during daytime than at nighttime. Low-level wind speed reaches the maximum at about 14 LT to 15 LT when the vertical momentum mixing is highly active. Wind speeds over the eastern coastal region of Southern Vietnam are much stronger in winter than in summer due to two main reasons, including (1) stronger large-scale wind speed in winter than in summer and (2) funnel effect creating a local maximum wind speed over the nearshore ocean which then transports high-momentum air inland in winter.http://dx.doi.org/10.1155/2021/8823940
spellingShingle Hiep Van Nguyen
Pham Xuan Thanh
Nguyen Duc Nam
Nguyen Xuan Anh
Pham Le Khuong
Hoang Hai Son
Nguyen Tien Manh
Pham Chi Cong
Observation and Simulation of Wind Speed and Wind Power Density over Bac Lieu Region
Advances in Meteorology
title Observation and Simulation of Wind Speed and Wind Power Density over Bac Lieu Region
title_full Observation and Simulation of Wind Speed and Wind Power Density over Bac Lieu Region
title_fullStr Observation and Simulation of Wind Speed and Wind Power Density over Bac Lieu Region
title_full_unstemmed Observation and Simulation of Wind Speed and Wind Power Density over Bac Lieu Region
title_short Observation and Simulation of Wind Speed and Wind Power Density over Bac Lieu Region
title_sort observation and simulation of wind speed and wind power density over bac lieu region
url http://dx.doi.org/10.1155/2021/8823940
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