Impact of the selected boundary layer schemes and enhanced horizontal resolution on the Weather Research and Forecasting model performance on James Ross Island, Antarctic Peninsula
The output of the various Weather Research and Forecasting (WRF) model configurations was compared with ground-based observations in the northern part of James Ross Island, Antarctic Peninsula. In this region, a network of automatic weather stations deployed at ice-free sites (as well as small glaci...
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ftmasarykunivojs:oai:ojs.journals.muni.cz:article/25396 2023-05-15T13:46:41+02:00 Impact of the selected boundary layer schemes and enhanced horizontal resolution on the Weather Research and Forecasting model performance on James Ross Island, Antarctic Peninsula Matějka, Michael Láska, Kamil 2022-09-05 application/pdf https://journals.muni.cz/CPR/article/view/25396 eng eng Masaryk Univerzity https://journals.muni.cz/CPR/article/view/25396/25168 https://journals.muni.cz/CPR/article/view/25396 Copyright (c) 2022 Czech Polar Reports https://creativecommons.org/licenses/by-nc-nd/4.0/ CC-BY-NC-ND Czech Polar Reports; Vol 12 No 1 (2022); 15-30 Czech Polar Reports; Vol. 12 No. 1 (2022); 15-30 1805-0697 1805-0689 polar meteorology numerical simulation WRF model air temperature snow cover wind speed Antarctic Peninsula info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2022 ftmasarykunivojs 2022-09-12T23:20:07Z The output of the various Weather Research and Forecasting (WRF) model configurations was compared with ground-based observations in the northern part of James Ross Island, Antarctic Peninsula. In this region, a network of automatic weather stations deployed at ice-free sites (as well as small glaciers) is operated by the Czech Antarctic Research Programme. Data from these stations provide a unique opportunity to evaluate the WRF model in a complex terrain of James Ross Island. The model was forced by the ERA5 reanalysis data and the University of Bremen sea ice data. The model configurations include a novel Three-Dimensional Scale-Adaptive Turbulent Kinetic Energy (3D TKE) planetary boundary layer scheme and a more traditional Quasi-Normal Scale Elimination (QNSE) scheme. Impact of model horizontal resolution was evaluated by running simulations in both 700 m and 300 m. The validation period, 25 May 2019 to 12 June 2019, was selected to cover different stratification regimes of air temperature and a significant snowfall event. Air temperature was simulated well except for strong low-level inversions. These inversions occurred in 44% of all cases and contributed to a higher mean bias (2.0–2.9°C) at low-elevation sites than at high altitude sites (0.2–0.6°C). The selection of the 3D TKE scheme led to improvement at low-elevation sites; at high altitude sites, the differences between model configurations were rather small. The best performance in wind speed simulation was achieved with the combination of the 3D TKE scheme and 300 m model resolution. The most important improvement was decrease of bias at a coastal Mendel Station from 3.5 m·s‑1 with the QNSE scheme on the 700 m grid to 1.2 m·s‑1 with the 3D TKE scheme on the 300 m grid. The WRF model was also proven to simulate a large snowfall event with a good correspondence with the observed snow height. Article in Journal/Newspaper Antarc* Antarctic Antarctic Peninsula James Ross Island Ross Island Sea ice Masaryk University Journals Antarctic Antarctic Peninsula Ross Island |
institution |
Open Polar |
collection |
Masaryk University Journals |
op_collection_id |
ftmasarykunivojs |
language |
English |
topic |
polar meteorology numerical simulation WRF model air temperature snow cover wind speed Antarctic Peninsula |
spellingShingle |
polar meteorology numerical simulation WRF model air temperature snow cover wind speed Antarctic Peninsula Matějka, Michael Láska, Kamil Impact of the selected boundary layer schemes and enhanced horizontal resolution on the Weather Research and Forecasting model performance on James Ross Island, Antarctic Peninsula |
topic_facet |
polar meteorology numerical simulation WRF model air temperature snow cover wind speed Antarctic Peninsula |
description |
The output of the various Weather Research and Forecasting (WRF) model configurations was compared with ground-based observations in the northern part of James Ross Island, Antarctic Peninsula. In this region, a network of automatic weather stations deployed at ice-free sites (as well as small glaciers) is operated by the Czech Antarctic Research Programme. Data from these stations provide a unique opportunity to evaluate the WRF model in a complex terrain of James Ross Island. The model was forced by the ERA5 reanalysis data and the University of Bremen sea ice data. The model configurations include a novel Three-Dimensional Scale-Adaptive Turbulent Kinetic Energy (3D TKE) planetary boundary layer scheme and a more traditional Quasi-Normal Scale Elimination (QNSE) scheme. Impact of model horizontal resolution was evaluated by running simulations in both 700 m and 300 m. The validation period, 25 May 2019 to 12 June 2019, was selected to cover different stratification regimes of air temperature and a significant snowfall event. Air temperature was simulated well except for strong low-level inversions. These inversions occurred in 44% of all cases and contributed to a higher mean bias (2.0–2.9°C) at low-elevation sites than at high altitude sites (0.2–0.6°C). The selection of the 3D TKE scheme led to improvement at low-elevation sites; at high altitude sites, the differences between model configurations were rather small. The best performance in wind speed simulation was achieved with the combination of the 3D TKE scheme and 300 m model resolution. The most important improvement was decrease of bias at a coastal Mendel Station from 3.5 m·s‑1 with the QNSE scheme on the 700 m grid to 1.2 m·s‑1 with the 3D TKE scheme on the 300 m grid. The WRF model was also proven to simulate a large snowfall event with a good correspondence with the observed snow height. |
format |
Article in Journal/Newspaper |
author |
Matějka, Michael Láska, Kamil |
author_facet |
Matějka, Michael Láska, Kamil |
author_sort |
Matějka, Michael |
title |
Impact of the selected boundary layer schemes and enhanced horizontal resolution on the Weather Research and Forecasting model performance on James Ross Island, Antarctic Peninsula |
title_short |
Impact of the selected boundary layer schemes and enhanced horizontal resolution on the Weather Research and Forecasting model performance on James Ross Island, Antarctic Peninsula |
title_full |
Impact of the selected boundary layer schemes and enhanced horizontal resolution on the Weather Research and Forecasting model performance on James Ross Island, Antarctic Peninsula |
title_fullStr |
Impact of the selected boundary layer schemes and enhanced horizontal resolution on the Weather Research and Forecasting model performance on James Ross Island, Antarctic Peninsula |
title_full_unstemmed |
Impact of the selected boundary layer schemes and enhanced horizontal resolution on the Weather Research and Forecasting model performance on James Ross Island, Antarctic Peninsula |
title_sort |
impact of the selected boundary layer schemes and enhanced horizontal resolution on the weather research and forecasting model performance on james ross island, antarctic peninsula |
publisher |
Masaryk Univerzity |
publishDate |
2022 |
url |
https://journals.muni.cz/CPR/article/view/25396 |
geographic |
Antarctic Antarctic Peninsula Ross Island |
geographic_facet |
Antarctic Antarctic Peninsula Ross Island |
genre |
Antarc* Antarctic Antarctic Peninsula James Ross Island Ross Island Sea ice |
genre_facet |
Antarc* Antarctic Antarctic Peninsula James Ross Island Ross Island Sea ice |
op_source |
Czech Polar Reports; Vol 12 No 1 (2022); 15-30 Czech Polar Reports; Vol. 12 No. 1 (2022); 15-30 1805-0697 1805-0689 |
op_relation |
https://journals.muni.cz/CPR/article/view/25396/25168 https://journals.muni.cz/CPR/article/view/25396 |
op_rights |
Copyright (c) 2022 Czech Polar Reports https://creativecommons.org/licenses/by-nc-nd/4.0/ |
op_rightsnorm |
CC-BY-NC-ND |
_version_ |
1766245092245372928 |