Exploring alternative possibilities for sublimation measurements over snow and ice surfaces

Sublimation of snow is a major depletion mechanism, particularly in dry and windy environments such as high mountains or polar regions. Yet the quantification of the latent heat flux is a difficult task, and both measurements and estimates from models still have large uncertainties. In particular, r...

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Main Authors: Huwald, Hendrik, Sigmund, Armin, Gerber, Franziska, Lehning, Michael
Format: Text
Language:unknown
Published: 2023
Subjects:
Online Access:http://infoscience.epfl.ch/record/300848
https://infoscience.epfl.ch/record/300848/files/Poster_white.pdf
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spelling ftinfoscience:oai:infoscience.epfl.ch:300848 2023-10-09T21:47:04+02:00 Exploring alternative possibilities for sublimation measurements over snow and ice surfaces Huwald, Hendrik Sigmund, Armin Gerber, Franziska Lehning, Michael 2023-03-09T09:51:06Z http://infoscience.epfl.ch/record/300848 https://infoscience.epfl.ch/record/300848/files/Poster_white.pdf unknown http://infoscience.epfl.ch/record/300848 https://infoscience.epfl.ch/record/300848/files/Poster_white.pdf http://infoscience.epfl.ch/record/300848 Text 2023 ftinfoscience 2023-09-17T23:48:45Z Sublimation of snow is a major depletion mechanism, particularly in dry and windy environments such as high mountains or polar regions. Yet the quantification of the latent heat flux is a difficult task, and both measurements and estimates from models still have large uncertainties. In particular, remote areas in high mountain terrain and on the large polar ice sheets are known to have insufficient spatial coverage through measurements and insufficient capabilities of models to accurately estimate snow sublimation. Additionally, power requirements for eddy covariance (EC) systems are often beyond supply in extreme environments. We present latent heat flux measurements obtained using standard EC instrumentation from several high-alpine and Antarctic field sites and compute corresponding sublimation rates. Where possible, these quantities are compared to sublimation rates derived from measurements of meteorological variables along a vertical profile (bulk approach). This study further explores the suitability of (low-cost) alternative sensors and instrumentation to determine latent heat fluxes over snow and ice-covered surfaces. Specifically, inexpensive fast-response humidity sensors are in the focus of the approach. If successful, this may lead to denser networks of surface stations in the Alps and potentially in polar regions, capable to measure sublimation from snow. A similar approach is tested for fast-frequency air temperature measurements, investigating whether such a methodology is viable in typically stably stratified boundary layers over cold surfaces. At its early stage, this project is largely explorative but may pave the road for interesting and affordable sensing solutions for measuring turbulent heat fluxes in cold, snow and ice-covered environments as standard components on existing traditional automatic weather stations. Text Antarc* Antarctic EPFL Infoscience (Ecole Polytechnique Fédérale Lausanne) Antarctic
institution Open Polar
collection EPFL Infoscience (Ecole Polytechnique Fédérale Lausanne)
op_collection_id ftinfoscience
language unknown
description Sublimation of snow is a major depletion mechanism, particularly in dry and windy environments such as high mountains or polar regions. Yet the quantification of the latent heat flux is a difficult task, and both measurements and estimates from models still have large uncertainties. In particular, remote areas in high mountain terrain and on the large polar ice sheets are known to have insufficient spatial coverage through measurements and insufficient capabilities of models to accurately estimate snow sublimation. Additionally, power requirements for eddy covariance (EC) systems are often beyond supply in extreme environments. We present latent heat flux measurements obtained using standard EC instrumentation from several high-alpine and Antarctic field sites and compute corresponding sublimation rates. Where possible, these quantities are compared to sublimation rates derived from measurements of meteorological variables along a vertical profile (bulk approach). This study further explores the suitability of (low-cost) alternative sensors and instrumentation to determine latent heat fluxes over snow and ice-covered surfaces. Specifically, inexpensive fast-response humidity sensors are in the focus of the approach. If successful, this may lead to denser networks of surface stations in the Alps and potentially in polar regions, capable to measure sublimation from snow. A similar approach is tested for fast-frequency air temperature measurements, investigating whether such a methodology is viable in typically stably stratified boundary layers over cold surfaces. At its early stage, this project is largely explorative but may pave the road for interesting and affordable sensing solutions for measuring turbulent heat fluxes in cold, snow and ice-covered environments as standard components on existing traditional automatic weather stations.
format Text
author Huwald, Hendrik
Sigmund, Armin
Gerber, Franziska
Lehning, Michael
spellingShingle Huwald, Hendrik
Sigmund, Armin
Gerber, Franziska
Lehning, Michael
Exploring alternative possibilities for sublimation measurements over snow and ice surfaces
author_facet Huwald, Hendrik
Sigmund, Armin
Gerber, Franziska
Lehning, Michael
author_sort Huwald, Hendrik
title Exploring alternative possibilities for sublimation measurements over snow and ice surfaces
title_short Exploring alternative possibilities for sublimation measurements over snow and ice surfaces
title_full Exploring alternative possibilities for sublimation measurements over snow and ice surfaces
title_fullStr Exploring alternative possibilities for sublimation measurements over snow and ice surfaces
title_full_unstemmed Exploring alternative possibilities for sublimation measurements over snow and ice surfaces
title_sort exploring alternative possibilities for sublimation measurements over snow and ice surfaces
publishDate 2023
url http://infoscience.epfl.ch/record/300848
https://infoscience.epfl.ch/record/300848/files/Poster_white.pdf
geographic Antarctic
geographic_facet Antarctic
genre Antarc*
Antarctic
genre_facet Antarc*
Antarctic
op_source http://infoscience.epfl.ch/record/300848
op_relation http://infoscience.epfl.ch/record/300848
https://infoscience.epfl.ch/record/300848/files/Poster_white.pdf
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