Evaluation of wind forecasts over Svalbard using the high-resolution Polar WRF with 3DVAR

In this study, the performance of wind forecasts over Svalbard, located between the Arctic Ocean and the Norwegian Sea, was evaluated using the Polar Weather Research and Forecasting (PWRF) model and three-dimensional variational data assimilation (DA) system. The forecasts of the analysis–forecast...

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Published in:Arctic, Antarctic, and Alpine Research
Main Authors: Dae-Hui Kim, Hyun Mee Kim, Jinkyu Hong
Format: Article in Journal/Newspaper
Language:English
Published: Taylor & Francis Group 2019
Subjects:
geo
Online Access:https://doi.org/10.1080/15230430.2019.1676939
https://doaj.org/article/46344fe3bd3642db84e5dece55750fac
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spelling fttriple:oai:gotriple.eu:oai:doaj.org/article:46344fe3bd3642db84e5dece55750fac 2023-05-15T14:14:23+02:00 Evaluation of wind forecasts over Svalbard using the high-resolution Polar WRF with 3DVAR Dae-Hui Kim Hyun Mee Kim Jinkyu Hong 2019-01-01 https://doi.org/10.1080/15230430.2019.1676939 https://doaj.org/article/46344fe3bd3642db84e5dece55750fac en eng Taylor & Francis Group 1523-0430 1938-4246 doi:10.1080/15230430.2019.1676939 https://doaj.org/article/46344fe3bd3642db84e5dece55750fac undefined Arctic, Antarctic, and Alpine Research, Vol 51, Iss 1, Pp 471-489 (2019) polar wrf with 3dvar data assimilation wind forecast polar low svalbard geo demo Journal Article https://vocabularies.coar-repositories.org/resource_types/c_6501/ 2019 fttriple https://doi.org/10.1080/15230430.2019.1676939 2023-01-22T19:12:25Z In this study, the performance of wind forecasts over Svalbard, located between the Arctic Ocean and the Norwegian Sea, was evaluated using the Polar Weather Research and Forecasting (PWRF) model and three-dimensional variational data assimilation (DA) system. The forecasts of the analysis–forecast cycling experiment using the PWRF 3DVAR were compared with those of the cold start experiment using reanalysis as the initial condition. Three strong wind cases that occurred during January and February 2011–2012 were selected, where polar lows were generated on the east coast of Greenland and generated a wind speed above 20 m s−1 in Svalbard. The wind speed forecasts for both cycling and cold start experiments were similar to the highest 10-minute average wind speed for the last 1 hour (HAW). The average root mean square error (RMSE) of the forecasts in the cold start experiment from HAW was 3.78 m s−1 for three cases and was greater than that in the cycling experiment. The forecast performance in the cycling experiment was comparable to, or even better than, that in the cold start experiment, which implies that the cycling system with DA is more useful than the cold start system in forecasting polar weather to support research activities. Article in Journal/Newspaper Antarctic and Alpine Research Arctic Arctic Arctic Ocean Greenland Norwegian Sea Svalbard Unknown Arctic Arctic Ocean Greenland Norwegian Sea Svalbard Arctic, Antarctic, and Alpine Research 51 1 471 489
institution Open Polar
collection Unknown
op_collection_id fttriple
language English
topic polar wrf with 3dvar
data assimilation
wind forecast
polar low
svalbard
geo
demo
spellingShingle polar wrf with 3dvar
data assimilation
wind forecast
polar low
svalbard
geo
demo
Dae-Hui Kim
Hyun Mee Kim
Jinkyu Hong
Evaluation of wind forecasts over Svalbard using the high-resolution Polar WRF with 3DVAR
topic_facet polar wrf with 3dvar
data assimilation
wind forecast
polar low
svalbard
geo
demo
description In this study, the performance of wind forecasts over Svalbard, located between the Arctic Ocean and the Norwegian Sea, was evaluated using the Polar Weather Research and Forecasting (PWRF) model and three-dimensional variational data assimilation (DA) system. The forecasts of the analysis–forecast cycling experiment using the PWRF 3DVAR were compared with those of the cold start experiment using reanalysis as the initial condition. Three strong wind cases that occurred during January and February 2011–2012 were selected, where polar lows were generated on the east coast of Greenland and generated a wind speed above 20 m s−1 in Svalbard. The wind speed forecasts for both cycling and cold start experiments were similar to the highest 10-minute average wind speed for the last 1 hour (HAW). The average root mean square error (RMSE) of the forecasts in the cold start experiment from HAW was 3.78 m s−1 for three cases and was greater than that in the cycling experiment. The forecast performance in the cycling experiment was comparable to, or even better than, that in the cold start experiment, which implies that the cycling system with DA is more useful than the cold start system in forecasting polar weather to support research activities.
format Article in Journal/Newspaper
author Dae-Hui Kim
Hyun Mee Kim
Jinkyu Hong
author_facet Dae-Hui Kim
Hyun Mee Kim
Jinkyu Hong
author_sort Dae-Hui Kim
title Evaluation of wind forecasts over Svalbard using the high-resolution Polar WRF with 3DVAR
title_short Evaluation of wind forecasts over Svalbard using the high-resolution Polar WRF with 3DVAR
title_full Evaluation of wind forecasts over Svalbard using the high-resolution Polar WRF with 3DVAR
title_fullStr Evaluation of wind forecasts over Svalbard using the high-resolution Polar WRF with 3DVAR
title_full_unstemmed Evaluation of wind forecasts over Svalbard using the high-resolution Polar WRF with 3DVAR
title_sort evaluation of wind forecasts over svalbard using the high-resolution polar wrf with 3dvar
publisher Taylor & Francis Group
publishDate 2019
url https://doi.org/10.1080/15230430.2019.1676939
https://doaj.org/article/46344fe3bd3642db84e5dece55750fac
geographic Arctic
Arctic Ocean
Greenland
Norwegian Sea
Svalbard
geographic_facet Arctic
Arctic Ocean
Greenland
Norwegian Sea
Svalbard
genre Antarctic and Alpine Research
Arctic
Arctic
Arctic Ocean
Greenland
Norwegian Sea
Svalbard
genre_facet Antarctic and Alpine Research
Arctic
Arctic
Arctic Ocean
Greenland
Norwegian Sea
Svalbard
op_source Arctic, Antarctic, and Alpine Research, Vol 51, Iss 1, Pp 471-489 (2019)
op_relation 1523-0430
1938-4246
doi:10.1080/15230430.2019.1676939
https://doaj.org/article/46344fe3bd3642db84e5dece55750fac
op_rights undefined
op_doi https://doi.org/10.1080/15230430.2019.1676939
container_title Arctic, Antarctic, and Alpine Research
container_volume 51
container_issue 1
container_start_page 471
op_container_end_page 489
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