Verification of the regional atmospheric model CCLM v5.0 with conventional data and lidar measurements in Antarctica

The nonhydrostatic regional climate model CCLM was used for a long-term hindcast run (2002–2016) for the Weddell Sea region with resolutions of 15 and 5 km and two different turbulence parametrizations. CCLM was nested in ERA-Interim data and used in forecast mode (suite of consecutive 30 h long sim...

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Published in:Geoscientific Model Development
Main Authors: Zentek, Rolf, Heinemann, Günther
Format: Text
Language:English
Published: 2020
Subjects:
Online Access:https://doi.org/10.5194/gmd-13-1809-2020
https://gmd.copernicus.org/articles/13/1809/2020/
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spelling ftcopernicus:oai:publications.copernicus.org:gmd76565 2023-05-15T13:55:28+02:00 Verification of the regional atmospheric model CCLM v5.0 with conventional data and lidar measurements in Antarctica Zentek, Rolf Heinemann, Günther 2020-04-06 application/pdf https://doi.org/10.5194/gmd-13-1809-2020 https://gmd.copernicus.org/articles/13/1809/2020/ eng eng doi:10.5194/gmd-13-1809-2020 https://gmd.copernicus.org/articles/13/1809/2020/ eISSN: 1991-9603 Text 2020 ftcopernicus https://doi.org/10.5194/gmd-13-1809-2020 2020-07-20T16:22:18Z The nonhydrostatic regional climate model CCLM was used for a long-term hindcast run (2002–2016) for the Weddell Sea region with resolutions of 15 and 5 km and two different turbulence parametrizations. CCLM was nested in ERA-Interim data and used in forecast mode (suite of consecutive 30 h long simulations with 6 h spin-up). We prescribed the sea ice concentration from satellite data and used a thermodynamic sea ice model. The performance of the model was evaluated in terms of temperature and wind using data from Antarctic stations, automatic weather stations (AWSs), an operational forecast model and reanalyses data, and lidar wind profiles. For the reference run we found a warm bias for the near-surface temperature over the Antarctic Plateau. This bias was removed in the second run by adjusting the turbulence parametrization, which results in a more realistic representation of the surface inversion over the plateau but resulted in a negative bias for some coastal regions. A comparison with measurements over the sea ice of the Weddell Sea by three AWS buoys for 1 year showed small biases for temperature around ±1 K and for wind speed of 1 m s −1 . Comparisons of radio soundings showed a model bias around 0 and a RMSE of 1–2 K for temperature and 3–4 m s −1 for wind speed. The comparison of CCLM simulations at resolutions down to 1 km with wind data from Doppler lidar measurements during December 2015 and January 2016 yielded almost no bias in wind speed and a RMSE of ca. 2 m s −1 . Overall CCLM shows a good representation of temperature and wind for the Weddell Sea region. Based on these encouraging results, CCLM at high resolution will be used for the investigation of the regional climate in the Antarctic and atmosphere–ice–ocean interactions processes in a forthcoming study. Text Antarc* Antarctic Antarctica Sea ice Weddell Sea Copernicus Publications: E-Journals Antarctic The Antarctic Weddell Weddell Sea Geoscientific Model Development 13 4 1809 1825
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description The nonhydrostatic regional climate model CCLM was used for a long-term hindcast run (2002–2016) for the Weddell Sea region with resolutions of 15 and 5 km and two different turbulence parametrizations. CCLM was nested in ERA-Interim data and used in forecast mode (suite of consecutive 30 h long simulations with 6 h spin-up). We prescribed the sea ice concentration from satellite data and used a thermodynamic sea ice model. The performance of the model was evaluated in terms of temperature and wind using data from Antarctic stations, automatic weather stations (AWSs), an operational forecast model and reanalyses data, and lidar wind profiles. For the reference run we found a warm bias for the near-surface temperature over the Antarctic Plateau. This bias was removed in the second run by adjusting the turbulence parametrization, which results in a more realistic representation of the surface inversion over the plateau but resulted in a negative bias for some coastal regions. A comparison with measurements over the sea ice of the Weddell Sea by three AWS buoys for 1 year showed small biases for temperature around ±1 K and for wind speed of 1 m s −1 . Comparisons of radio soundings showed a model bias around 0 and a RMSE of 1–2 K for temperature and 3–4 m s −1 for wind speed. The comparison of CCLM simulations at resolutions down to 1 km with wind data from Doppler lidar measurements during December 2015 and January 2016 yielded almost no bias in wind speed and a RMSE of ca. 2 m s −1 . Overall CCLM shows a good representation of temperature and wind for the Weddell Sea region. Based on these encouraging results, CCLM at high resolution will be used for the investigation of the regional climate in the Antarctic and atmosphere–ice–ocean interactions processes in a forthcoming study.
format Text
author Zentek, Rolf
Heinemann, Günther
spellingShingle Zentek, Rolf
Heinemann, Günther
Verification of the regional atmospheric model CCLM v5.0 with conventional data and lidar measurements in Antarctica
author_facet Zentek, Rolf
Heinemann, Günther
author_sort Zentek, Rolf
title Verification of the regional atmospheric model CCLM v5.0 with conventional data and lidar measurements in Antarctica
title_short Verification of the regional atmospheric model CCLM v5.0 with conventional data and lidar measurements in Antarctica
title_full Verification of the regional atmospheric model CCLM v5.0 with conventional data and lidar measurements in Antarctica
title_fullStr Verification of the regional atmospheric model CCLM v5.0 with conventional data and lidar measurements in Antarctica
title_full_unstemmed Verification of the regional atmospheric model CCLM v5.0 with conventional data and lidar measurements in Antarctica
title_sort verification of the regional atmospheric model cclm v5.0 with conventional data and lidar measurements in antarctica
publishDate 2020
url https://doi.org/10.5194/gmd-13-1809-2020
https://gmd.copernicus.org/articles/13/1809/2020/
geographic Antarctic
The Antarctic
Weddell
Weddell Sea
geographic_facet Antarctic
The Antarctic
Weddell
Weddell Sea
genre Antarc*
Antarctic
Antarctica
Sea ice
Weddell Sea
genre_facet Antarc*
Antarctic
Antarctica
Sea ice
Weddell Sea
op_source eISSN: 1991-9603
op_relation doi:10.5194/gmd-13-1809-2020
https://gmd.copernicus.org/articles/13/1809/2020/
op_doi https://doi.org/10.5194/gmd-13-1809-2020
container_title Geoscientific Model Development
container_volume 13
container_issue 4
container_start_page 1809
op_container_end_page 1825
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