Modelling stable atmospheric boundary layers over snow
Thesis entitled: Modelling Stable Atmospheric Boundary Layers over Snow H.A.M. Sterk Wageningen, 29th of April, 2015 Summary The emphasis of this thesis is on the understanding and forecasting of the Stable Boundary Layer (SBL) over snow-covered surfaces. SBLs typically form at night and in polar re...
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Wageningen University
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ftunivwagenin:oai:library.wur.nl:wurpubs/486869 2024-02-11T09:54:57+01:00 Modelling stable atmospheric boundary layers over snow Sterk, H.A.M. Holtslag, Bert Steeneveld, Gert-Jan 2015 application/pdf https://research.wur.nl/en/publications/modelling-stable-atmospheric-boundary-layers-over-snow en eng Wageningen University https://edepot.wur.nl/339836 https://research.wur.nl/en/publications/modelling-stable-atmospheric-boundary-layers-over-snow Wageningen University & Research atmospheric boundary-layer modeling models snow turbulence weather forecasting atmosferische grenslaag modellen modelleren sneeuw turbulentie weersvoorspelling Doctoral thesis 2015 ftunivwagenin 2024-01-24T23:18:35Z Thesis entitled: Modelling Stable Atmospheric Boundary Layers over Snow H.A.M. Sterk Wageningen, 29th of April, 2015 Summary The emphasis of this thesis is on the understanding and forecasting of the Stable Boundary Layer (SBL) over snow-covered surfaces. SBLs typically form at night and in polar regions (especially in winter), when radiative cooling at the surface causes a cooler surface than the overlying atmosphere and a stable stratification develops. This means that potential temperature increases with height and buoyancy effects suppress turbulence. Turbulence is then dominated by mechanical origin. If sufficient wind shear can be maintained, turbulence remains active, otherwise it will cease. A proper representation of SBLs in numerical weather prediction models is critical, since many parties rely on these forecasts. For example, weather prediction is needed for wind energy resources, agricultural purposes, air-quality studies, and aviation and road traffic. Knowledge on SBLs is also essential for climate modelling. In the Arctic regions, climate change is most pronounced due to stronger changes in near-surface temperature compared to other latitudes. Though this `Arctic amplification' is not yet fully understood, possible responsible processes are the ice-albedo feedback, alterations in cloud cover and water vapour, different atmospheric and oceanic circulations, and the weak vertical mixing in the lower atmosphere. However, many interactions exist between these processes. With positive feedbacks, changes are even further enhanced. This could have worldwide consequences, i.e. due to affected atmospheric circulations and sea level rise with Greenland's melting ice-sheets. Scientists try to explain the observed climate changes, as well as provide outlooks for future changes in climate and weather. However, the understanding is hampered by the fact that many model output variables (e.g. regarding the 2 m temperature) vary substantially between models on the one hand, and from observations on the other ... Doctoral or Postdoctoral Thesis albedo Arctic Climate change Wageningen UR (University & Research Centre): Digital Library Arctic |
institution |
Open Polar |
collection |
Wageningen UR (University & Research Centre): Digital Library |
op_collection_id |
ftunivwagenin |
language |
English |
topic |
atmospheric boundary-layer modeling models snow turbulence weather forecasting atmosferische grenslaag modellen modelleren sneeuw turbulentie weersvoorspelling |
spellingShingle |
atmospheric boundary-layer modeling models snow turbulence weather forecasting atmosferische grenslaag modellen modelleren sneeuw turbulentie weersvoorspelling Sterk, H.A.M. Modelling stable atmospheric boundary layers over snow |
topic_facet |
atmospheric boundary-layer modeling models snow turbulence weather forecasting atmosferische grenslaag modellen modelleren sneeuw turbulentie weersvoorspelling |
description |
Thesis entitled: Modelling Stable Atmospheric Boundary Layers over Snow H.A.M. Sterk Wageningen, 29th of April, 2015 Summary The emphasis of this thesis is on the understanding and forecasting of the Stable Boundary Layer (SBL) over snow-covered surfaces. SBLs typically form at night and in polar regions (especially in winter), when radiative cooling at the surface causes a cooler surface than the overlying atmosphere and a stable stratification develops. This means that potential temperature increases with height and buoyancy effects suppress turbulence. Turbulence is then dominated by mechanical origin. If sufficient wind shear can be maintained, turbulence remains active, otherwise it will cease. A proper representation of SBLs in numerical weather prediction models is critical, since many parties rely on these forecasts. For example, weather prediction is needed for wind energy resources, agricultural purposes, air-quality studies, and aviation and road traffic. Knowledge on SBLs is also essential for climate modelling. In the Arctic regions, climate change is most pronounced due to stronger changes in near-surface temperature compared to other latitudes. Though this `Arctic amplification' is not yet fully understood, possible responsible processes are the ice-albedo feedback, alterations in cloud cover and water vapour, different atmospheric and oceanic circulations, and the weak vertical mixing in the lower atmosphere. However, many interactions exist between these processes. With positive feedbacks, changes are even further enhanced. This could have worldwide consequences, i.e. due to affected atmospheric circulations and sea level rise with Greenland's melting ice-sheets. Scientists try to explain the observed climate changes, as well as provide outlooks for future changes in climate and weather. However, the understanding is hampered by the fact that many model output variables (e.g. regarding the 2 m temperature) vary substantially between models on the one hand, and from observations on the other ... |
author2 |
Holtslag, Bert Steeneveld, Gert-Jan |
format |
Doctoral or Postdoctoral Thesis |
author |
Sterk, H.A.M. |
author_facet |
Sterk, H.A.M. |
author_sort |
Sterk, H.A.M. |
title |
Modelling stable atmospheric boundary layers over snow |
title_short |
Modelling stable atmospheric boundary layers over snow |
title_full |
Modelling stable atmospheric boundary layers over snow |
title_fullStr |
Modelling stable atmospheric boundary layers over snow |
title_full_unstemmed |
Modelling stable atmospheric boundary layers over snow |
title_sort |
modelling stable atmospheric boundary layers over snow |
publisher |
Wageningen University |
publishDate |
2015 |
url |
https://research.wur.nl/en/publications/modelling-stable-atmospheric-boundary-layers-over-snow |
geographic |
Arctic |
geographic_facet |
Arctic |
genre |
albedo Arctic Climate change |
genre_facet |
albedo Arctic Climate change |
op_relation |
https://edepot.wur.nl/339836 https://research.wur.nl/en/publications/modelling-stable-atmospheric-boundary-layers-over-snow |
op_rights |
Wageningen University & Research |
_version_ |
1790609754094043136 |