The stable atmospheric boundary layer over snow-covered sea ice: Model valuation with fine-scale ISOBAR18 observations

A realistic representation of the stable atmospheric boundary layer in numerical weather prediction (NWP) and climate models is still a challenge. We study the evolution of a stable boundary layer over snow-covered sea ice in Bothnian Bay during wintertime in 2018. We perform high-resolution model e...

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Published in:Quarterly Journal of the Royal Meteorological Society
Main Authors: Lorenz, Torge, Mayer, Stephanie, Kral, Stephan T., Suomi, Irene, Steeneveld, G.J., Holtslag, Bert
Format: Article in Journal/Newspaper
Language:English
Published: 2022
Subjects:
Online Access:https://research.wur.nl/en/publications/the-stable-atmospheric-boundary-layer-over-snow-covered-sea-ice-m
https://doi.org/10.1002/qj.4293
id ftunivwagenin:oai:library.wur.nl:wurpubs/598109
record_format openpolar
spelling ftunivwagenin:oai:library.wur.nl:wurpubs/598109 2024-02-11T10:08:30+01:00 The stable atmospheric boundary layer over snow-covered sea ice: Model valuation with fine-scale ISOBAR18 observations Lorenz, Torge Mayer, Stephanie Kral, Stephan T. Suomi, Irene Steeneveld, G.J. Holtslag, Bert 2022 application/pdf https://research.wur.nl/en/publications/the-stable-atmospheric-boundary-layer-over-snow-covered-sea-ice-m https://doi.org/10.1002/qj.4293 en eng https://edepot.wur.nl/571131 https://research.wur.nl/en/publications/the-stable-atmospheric-boundary-layer-over-snow-covered-sea-ice-m doi:10.1002/qj.4293 https://creativecommons.org/licenses/by-nc-nd/4.0/ Wageningen University & Research Quarterly Journal of the Royal Meteorological Society 148 (2022) 745 ISSN: 0035-9009 Life Science Article/Letter to editor 2022 ftunivwagenin https://doi.org/10.1002/qj.4293 2024-01-24T23:14:00Z A realistic representation of the stable atmospheric boundary layer in numerical weather prediction (NWP) and climate models is still a challenge. We study the evolution of a stable boundary layer over snow-covered sea ice in Bothnian Bay during wintertime in 2018. We perform high-resolution model experiments with the Weather Research and Forecasting model in its single-column model configuration and its default mesoscale configuration to assess which physical processes are essential to predict near-surface variables correctly. We evaluate our model runs against the unique observational dataset collected during ISOBAR18, which combines novel, upper-air measurements by an uncrewed aircraft system with wind lidar, sodar, and conventional meteorological mast data. By analysing surface fluxes in the single-column model, we demonstrate how the atmospheric cooling at the ground can be modelled more realistically than in the mesoscale set-up. We show that surface albedo and sea-ice thickness are essential for the surface energy balance in the model, and we demonstrate how the surface fluxes in the mesoscale downscaling with default settings are subject to strong biases. We also show that the ERA5 reanalysis is not capable of representing the observed surface meteorology in the stable atmospheric boundary layer. Our study illustrates the importance of surface albedo and sea-ice thickness for NWP models. Though a seasonal snow albedo is already in use in many NWP settings, the routine inclusion of sea-ice thickness, in particular, would be a great step forward for weather forecasts and regional climate simulations. Article in Journal/Newspaper Sea ice Wageningen UR (University & Research Centre): Digital Library Quarterly Journal of the Royal Meteorological Society 148 745 2031 2046
institution Open Polar
collection Wageningen UR (University & Research Centre): Digital Library
op_collection_id ftunivwagenin
language English
topic Life Science
spellingShingle Life Science
Lorenz, Torge
Mayer, Stephanie
Kral, Stephan T.
Suomi, Irene
Steeneveld, G.J.
Holtslag, Bert
The stable atmospheric boundary layer over snow-covered sea ice: Model valuation with fine-scale ISOBAR18 observations
topic_facet Life Science
description A realistic representation of the stable atmospheric boundary layer in numerical weather prediction (NWP) and climate models is still a challenge. We study the evolution of a stable boundary layer over snow-covered sea ice in Bothnian Bay during wintertime in 2018. We perform high-resolution model experiments with the Weather Research and Forecasting model in its single-column model configuration and its default mesoscale configuration to assess which physical processes are essential to predict near-surface variables correctly. We evaluate our model runs against the unique observational dataset collected during ISOBAR18, which combines novel, upper-air measurements by an uncrewed aircraft system with wind lidar, sodar, and conventional meteorological mast data. By analysing surface fluxes in the single-column model, we demonstrate how the atmospheric cooling at the ground can be modelled more realistically than in the mesoscale set-up. We show that surface albedo and sea-ice thickness are essential for the surface energy balance in the model, and we demonstrate how the surface fluxes in the mesoscale downscaling with default settings are subject to strong biases. We also show that the ERA5 reanalysis is not capable of representing the observed surface meteorology in the stable atmospheric boundary layer. Our study illustrates the importance of surface albedo and sea-ice thickness for NWP models. Though a seasonal snow albedo is already in use in many NWP settings, the routine inclusion of sea-ice thickness, in particular, would be a great step forward for weather forecasts and regional climate simulations.
format Article in Journal/Newspaper
author Lorenz, Torge
Mayer, Stephanie
Kral, Stephan T.
Suomi, Irene
Steeneveld, G.J.
Holtslag, Bert
author_facet Lorenz, Torge
Mayer, Stephanie
Kral, Stephan T.
Suomi, Irene
Steeneveld, G.J.
Holtslag, Bert
author_sort Lorenz, Torge
title The stable atmospheric boundary layer over snow-covered sea ice: Model valuation with fine-scale ISOBAR18 observations
title_short The stable atmospheric boundary layer over snow-covered sea ice: Model valuation with fine-scale ISOBAR18 observations
title_full The stable atmospheric boundary layer over snow-covered sea ice: Model valuation with fine-scale ISOBAR18 observations
title_fullStr The stable atmospheric boundary layer over snow-covered sea ice: Model valuation with fine-scale ISOBAR18 observations
title_full_unstemmed The stable atmospheric boundary layer over snow-covered sea ice: Model valuation with fine-scale ISOBAR18 observations
title_sort stable atmospheric boundary layer over snow-covered sea ice: model valuation with fine-scale isobar18 observations
publishDate 2022
url https://research.wur.nl/en/publications/the-stable-atmospheric-boundary-layer-over-snow-covered-sea-ice-m
https://doi.org/10.1002/qj.4293
genre Sea ice
genre_facet Sea ice
op_source Quarterly Journal of the Royal Meteorological Society 148 (2022) 745
ISSN: 0035-9009
op_relation https://edepot.wur.nl/571131
https://research.wur.nl/en/publications/the-stable-atmospheric-boundary-layer-over-snow-covered-sea-ice-m
doi:10.1002/qj.4293
op_rights https://creativecommons.org/licenses/by-nc-nd/4.0/
Wageningen University & Research
op_doi https://doi.org/10.1002/qj.4293
container_title Quarterly Journal of the Royal Meteorological Society
container_volume 148
container_issue 745
container_start_page 2031
op_container_end_page 2046
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