Articles | Volume 11, issue 8
https://doi.org/10.5194/gmd-11-3347-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/gmd-11-3347-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Implementation of a simple thermodynamic sea ice scheme, SICE version 1.0-38h1, within the ALADIN–HIRLAM numerical weather prediction system version 38h1
Development Centre for Weather Forecasting, Norwegian Meteorological Institute, Oslo, Norway
Ekaterina Kourzeneva
Finnish Meteorological Institute, Helsinki, Finland
Mariken Homleid
Development Centre for Weather Forecasting, Norwegian Meteorological Institute, Oslo, Norway
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Cited
17 citations as recorded by crossref.
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- Implementation of an Adaptive Bias‐Aware Extended Kalman Filter for Sea‐Ice Data Assimilation in the HARMONIE‐AROME Numerical Weather Prediction System Y. Batrak 10.1029/2021MS002533
- The Cycle 46 Configuration of the HARMONIE-AROME Forecast Model E. Gleeson et al. 10.3390/meteorology3040018
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- On the warm bias in atmospheric reanalyses induced by the missing snow over Arctic sea-ice Y. Batrak & M. Müller 10.1038/s41467-019-11975-3
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17 citations as recorded by crossref.
- Polar low variability and future projections for the Nordic and Barents Seas O. Landgren et al. 10.1002/qj.3608
- HCLIM38: a flexible regional climate model applicable for different climate zones from coarse to convection-permitting scales D. Belušić et al. 10.5194/gmd-13-1311-2020
- Implementation of an Adaptive Bias‐Aware Extended Kalman Filter for Sea‐Ice Data Assimilation in the HARMONIE‐AROME Numerical Weather Prediction System Y. Batrak 10.1029/2021MS002533
- The Cycle 46 Configuration of the HARMONIE-AROME Forecast Model E. Gleeson et al. 10.3390/meteorology3040018
- Validation of lake surface state in the HIRLAM v.7.4 numerical weather prediction model against in situ measurements in Finland L. Rontu et al. 10.5194/gmd-12-3707-2019
- Impact of high‐resolution ocean–atmosphere coupling on fog formation over the North Sea J. Fallmann et al. 10.1002/qj.3488
- Evolving relationship of Nares Strait ice arches on sea ice along the Strait and the North Water, the Arctic’s most productive polynya G. Moore et al. 10.1038/s41598-023-36179-0
- The winter central Arctic surface energy budget: A model evaluation using observations from the MOSAiC campaign A. Solomon et al. 10.1525/elementa.2022.00104
- A Comparison of Sea Surface Temperature Perturbation Methods for a Convection Permitting Ensemble Prediction System Over the European Arctic R. Grote & A. Singleton 10.16993/tellusa.27
- On the warm bias in atmospheric reanalyses induced by the missing snow over Arctic sea-ice Y. Batrak & M. Müller 10.1038/s41467-019-11975-3
- Sea ice cover in the Copernicus Arctic Regional Reanalysis Y. Batrak et al. 10.5194/tc-18-1157-2024
- Relative impact of observations on a regional Arctic numerical weather prediction system R. Randriamampianina et al. 10.1002/qj.4018
- A Kilometer-Scale Coupled Atmosphere-Wave Forecasting System for the European Arctic E. Thomas et al. 10.1175/WAF-D-21-0065.1
- A simple model for daily basin-wide thermodynamic sea ice thickness growth retrieval J. Anheuser et al. 10.5194/tc-16-4403-2022
- Evaluation of a sub-kilometre NWP system in an Arctic fjord-valley system in winter T. Valkonen et al. 10.1080/16000870.2020.1838181
- An NWP Model Intercomparison of Surface Weather Parameters in the European Arctic during the Year of Polar Prediction Special Observing Period Northern Hemisphere 1 M. Køltzow et al. 10.1175/WAF-D-19-0003.1
- On the Importance of Representing Snow Over Sea‐Ice for Simulating the Arctic Boundary Layer G. Arduini et al. 10.1029/2021MS002777
Latest update: 23 Nov 2024
Short summary
The authors discuss the implementation and performance of a simple one-dimensional sea ice scheme within the ALADIN–HIRLAM numerical weather prediction system. This scheme is developed to replace the prescribed sea ice surface temperature that was used before. Numerical experiments over the large ice-covered areas of the European Arctic show that new scheme helps to improve the modelled 2 m temperature in regions that are influenced by sea ice, especially when the forecast is longer than 12 h.
The authors discuss the implementation and performance of a simple one-dimensional sea ice...