Evaluation of a sub-kilometre NWP system in an Arctic fjord-valley system in winter
Terrain challenges the prediction of near-surface atmospheric conditions, even in kilometre-scale numerical weather prediction (NWP) models. In this study, the ALADIN-HIRLAM NWP system with 0.5 km horizontal grid spacing and an increased number of vertical levels is compared to the 2.5-km model syst...
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doaj-c2428b7dae914896a8954706f858bf412021-02-18T10:31:40ZengTaylor & Francis GroupTellus: Series A, Dynamic Meteorology and Oceanography1600-08702020-01-0172112110.1080/16000870.2020.18381811838181Evaluation of a sub-kilometre NWP system in an Arctic fjord-valley system in winterTeresa Valkonen0Patrick Stoll1Yurii Batrak2Morten Køltzow3Thea Maria Schneider4Emmy E. Stigter5Ola B. Aashamar6Eivind Støylen7Marius O. Jonassen8Development Centre for Weather Forecasting, Norwegian Meteorological InstituteDepartment of Physics and Technology, University of TromsøDevelopment Centre for Weather Forecasting, Norwegian Meteorological InstituteDevelopment Centre for Weather Forecasting, Norwegian Meteorological InstituteDepartment of Physics, University of PotsdamDepartment of Physical Geography, Utrecht UniversityForecasting Department, Norwegian Meteorological InstituteDevelopment Centre for Weather Forecasting, Norwegian Meteorological InstituteDepartment of Arctic Geophysics, The University Centre in SvalbardTerrain challenges the prediction of near-surface atmospheric conditions, even in kilometre-scale numerical weather prediction (NWP) models. In this study, the ALADIN-HIRLAM NWP system with 0.5 km horizontal grid spacing and an increased number of vertical levels is compared to the 2.5-km model system similar to the currently operational NWP system at the Norwegian Meteorological Institute. The impact of the increased resolution on the forecasts’ ability to represent boundary-layer processes is investigated for the period from 12 to 16 February 2018 in an Arctic fjord-valley system in the Svalbard archipelago. Model simulations are compared to a wide range of observations conducted during a field campaign. The model configuration with sub-kilometre grid spacing improves both the spatial structure and overall verification scores for the near-surface temperature and wind forecasts compared to the 2.5-km experiment. The sub-kilometre experiment successfully captures the wind channelling through the valley and the temperature field associated with it. In a situation of a cold-air pool development, the sub-kilometre experiment has a particularly high near-surface temperature bias at low elevations. The use of measurement campaign data, however, reveals some encouraging results, e.g. the sub-kilometre system has a more realistic vertical profile of temperature and wind speed, and the surface temperature sensitivity to the net surface energy is closer to the observations. This work demonstrates the potential of sub-kilometre NWP systems for forecasting weather in complex Arctic terrain, and also suggests that the increase in resolution needs to be accompanied with further development of other parts of the model system.http://dx.doi.org/10.1080/16000870.2020.1838181numerical weather predictionatmospheric boundary layercold-air poolvalley channellingsvalbard |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Teresa Valkonen Patrick Stoll Yurii Batrak Morten Køltzow Thea Maria Schneider Emmy E. Stigter Ola B. Aashamar Eivind Støylen Marius O. Jonassen |
spellingShingle |
Teresa Valkonen Patrick Stoll Yurii Batrak Morten Køltzow Thea Maria Schneider Emmy E. Stigter Ola B. Aashamar Eivind Støylen Marius O. Jonassen Evaluation of a sub-kilometre NWP system in an Arctic fjord-valley system in winter Tellus: Series A, Dynamic Meteorology and Oceanography numerical weather prediction atmospheric boundary layer cold-air pool valley channelling svalbard |
author_facet |
Teresa Valkonen Patrick Stoll Yurii Batrak Morten Køltzow Thea Maria Schneider Emmy E. Stigter Ola B. Aashamar Eivind Støylen Marius O. Jonassen |
author_sort |
Teresa Valkonen |
title |
Evaluation of a sub-kilometre NWP system in an Arctic fjord-valley system in winter |
title_short |
Evaluation of a sub-kilometre NWP system in an Arctic fjord-valley system in winter |
title_full |
Evaluation of a sub-kilometre NWP system in an Arctic fjord-valley system in winter |
title_fullStr |
Evaluation of a sub-kilometre NWP system in an Arctic fjord-valley system in winter |
title_full_unstemmed |
Evaluation of a sub-kilometre NWP system in an Arctic fjord-valley system in winter |
title_sort |
evaluation of a sub-kilometre nwp system in an arctic fjord-valley system in winter |
publisher |
Taylor & Francis Group |
series |
Tellus: Series A, Dynamic Meteorology and Oceanography |
issn |
1600-0870 |
publishDate |
2020-01-01 |
description |
Terrain challenges the prediction of near-surface atmospheric conditions, even in kilometre-scale numerical weather prediction (NWP) models. In this study, the ALADIN-HIRLAM NWP system with 0.5 km horizontal grid spacing and an increased number of vertical levels is compared to the 2.5-km model system similar to the currently operational NWP system at the Norwegian Meteorological Institute. The impact of the increased resolution on the forecasts’ ability to represent boundary-layer processes is investigated for the period from 12 to 16 February 2018 in an Arctic fjord-valley system in the Svalbard archipelago. Model simulations are compared to a wide range of observations conducted during a field campaign. The model configuration with sub-kilometre grid spacing improves both the spatial structure and overall verification scores for the near-surface temperature and wind forecasts compared to the 2.5-km experiment. The sub-kilometre experiment successfully captures the wind channelling through the valley and the temperature field associated with it. In a situation of a cold-air pool development, the sub-kilometre experiment has a particularly high near-surface temperature bias at low elevations. The use of measurement campaign data, however, reveals some encouraging results, e.g. the sub-kilometre system has a more realistic vertical profile of temperature and wind speed, and the surface temperature sensitivity to the net surface energy is closer to the observations. This work demonstrates the potential of sub-kilometre NWP systems for forecasting weather in complex Arctic terrain, and also suggests that the increase in resolution needs to be accompanied with further development of other parts of the model system. |
topic |
numerical weather prediction atmospheric boundary layer cold-air pool valley channelling svalbard |
url |
http://dx.doi.org/10.1080/16000870.2020.1838181 |
work_keys_str_mv |
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