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...

Full description

Bibliographic Details
Main Authors: Teresa Valkonen, Patrick Stoll, Yurii Batrak, Morten Køltzow, Thea Maria Schneider, Emmy E. Stigter, Ola B. Aashamar, Eivind Støylen, Marius O. Jonassen
Format: Article
Language:English
Published: Taylor & Francis Group 2020-01-01
Series:Tellus: Series A, Dynamic Meteorology and Oceanography
Subjects:
Online Access:http://dx.doi.org/10.1080/16000870.2020.1838181
id doaj-c2428b7dae914896a8954706f858bf41
record_format Article
spelling 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 AT teresavalkonen evaluationofasubkilometrenwpsysteminanarcticfjordvalleysysteminwinter
AT patrickstoll evaluationofasubkilometrenwpsysteminanarcticfjordvalleysysteminwinter
AT yuriibatrak evaluationofasubkilometrenwpsysteminanarcticfjordvalleysysteminwinter
AT mortenkøltzow evaluationofasubkilometrenwpsysteminanarcticfjordvalleysysteminwinter
AT theamariaschneider evaluationofasubkilometrenwpsysteminanarcticfjordvalleysysteminwinter
AT emmyestigter evaluationofasubkilometrenwpsysteminanarcticfjordvalleysysteminwinter
AT olabaashamar evaluationofasubkilometrenwpsysteminanarcticfjordvalleysysteminwinter
AT eivindstøylen evaluationofasubkilometrenwpsysteminanarcticfjordvalleysysteminwinter
AT mariusojonassen evaluationofasubkilometrenwpsysteminanarcticfjordvalleysysteminwinter
_version_ 1724263598716354560