Towards continuous measurements of snow drift and sublimation in polar environments

In polar regions, and specifically in continental Antarctica, the local surface mass and energy balances can be largely controlled by snow transport in form of drifting and blowing snow particles, and sublimation both from the snow or ice surface and from the airborne snow particles. Adverse conditi...

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Main Authors: Huwald, H., Sigmund, A., Allegri, B., Colety, B., Frischholz, Y., Kolinski, J., Lehning, M.
Format: Conference Object
Language:English
Published: 2023
Subjects:
Online Access:https://gfzpublic.gfz-potsdam.de/pubman/item/item_5020971
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spelling ftgfzpotsdam:oai:gfzpublic.gfz-potsdam.de:item_5020971 2023-07-30T03:57:01+02:00 Towards continuous measurements of snow drift and sublimation in polar environments Huwald, H. Sigmund, A. Allegri, B. Colety, B. Frischholz, Y. Kolinski, J. Lehning, M. 2023-07-11 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5020971 eng eng info:eu-repo/semantics/altIdentifier/doi/10.57757/IUGG23-4561 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5020971 XXVIII General Assembly of the International Union of Geodesy and Geophysics (IUGG) info:eu-repo/semantics/conferenceObject 2023 ftgfzpotsdam https://doi.org/10.57757/IUGG23-4561 2023-07-09T23:40:22Z In polar regions, and specifically in continental Antarctica, the local surface mass and energy balances can be largely controlled by snow transport in form of drifting and blowing snow particles, and sublimation both from the snow or ice surface and from the airborne snow particles. Adverse conditions in such extreme environments make continuous and reliable measurements of snow drift and sublimation a challenge, especially during the period of polar night and in absence of maintenance. Additionally, existing state-of-the-art snow mass and moisture flux measurement systems have relatively large power requirements, often resulting in spurious values or data gaps due to insufficient power supply from the autonomous wind and solar based power systems. In this contribution, we present observations of drifting snow events and latent heat fluxes obtained from collocated installations of classical eddy covariance instrumentation, optical snow particle counters, and acoustic particle flux devices deployed in Queen Maud Land, East Antarctica. We investigate the coherence of the optical and low-power acoustic snow drift measurements and compare them to numerical simulations of mass fluxes at the sensor sites. Furthermore, to mitigate the problems of potential power failure, low-power, fast-response humidity sensors are tested in laboratory and field settings to obtain latent heat flux estimates at largely reduced power consumption in comparison to eddy covariance measurements using infra-red gas analysers. Promising or successful novel systems may be a viable alternative for recording continuous time series of sublimation, in particular in the polar night season, and at significantly lower cost. Conference Object Antarc* Antarctica East Antarctica polar night Queen Maud Land GFZpublic (German Research Centre for Geosciences, Helmholtz-Zentrum Potsdam) East Antarctica Queen Maud Land ENVELOPE(12.000,12.000,-72.500,-72.500)
institution Open Polar
collection GFZpublic (German Research Centre for Geosciences, Helmholtz-Zentrum Potsdam)
op_collection_id ftgfzpotsdam
language English
description In polar regions, and specifically in continental Antarctica, the local surface mass and energy balances can be largely controlled by snow transport in form of drifting and blowing snow particles, and sublimation both from the snow or ice surface and from the airborne snow particles. Adverse conditions in such extreme environments make continuous and reliable measurements of snow drift and sublimation a challenge, especially during the period of polar night and in absence of maintenance. Additionally, existing state-of-the-art snow mass and moisture flux measurement systems have relatively large power requirements, often resulting in spurious values or data gaps due to insufficient power supply from the autonomous wind and solar based power systems. In this contribution, we present observations of drifting snow events and latent heat fluxes obtained from collocated installations of classical eddy covariance instrumentation, optical snow particle counters, and acoustic particle flux devices deployed in Queen Maud Land, East Antarctica. We investigate the coherence of the optical and low-power acoustic snow drift measurements and compare them to numerical simulations of mass fluxes at the sensor sites. Furthermore, to mitigate the problems of potential power failure, low-power, fast-response humidity sensors are tested in laboratory and field settings to obtain latent heat flux estimates at largely reduced power consumption in comparison to eddy covariance measurements using infra-red gas analysers. Promising or successful novel systems may be a viable alternative for recording continuous time series of sublimation, in particular in the polar night season, and at significantly lower cost.
format Conference Object
author Huwald, H.
Sigmund, A.
Allegri, B.
Colety, B.
Frischholz, Y.
Kolinski, J.
Lehning, M.
spellingShingle Huwald, H.
Sigmund, A.
Allegri, B.
Colety, B.
Frischholz, Y.
Kolinski, J.
Lehning, M.
Towards continuous measurements of snow drift and sublimation in polar environments
author_facet Huwald, H.
Sigmund, A.
Allegri, B.
Colety, B.
Frischholz, Y.
Kolinski, J.
Lehning, M.
author_sort Huwald, H.
title Towards continuous measurements of snow drift and sublimation in polar environments
title_short Towards continuous measurements of snow drift and sublimation in polar environments
title_full Towards continuous measurements of snow drift and sublimation in polar environments
title_fullStr Towards continuous measurements of snow drift and sublimation in polar environments
title_full_unstemmed Towards continuous measurements of snow drift and sublimation in polar environments
title_sort towards continuous measurements of snow drift and sublimation in polar environments
publishDate 2023
url https://gfzpublic.gfz-potsdam.de/pubman/item/item_5020971
long_lat ENVELOPE(12.000,12.000,-72.500,-72.500)
geographic East Antarctica
Queen Maud Land
geographic_facet East Antarctica
Queen Maud Land
genre Antarc*
Antarctica
East Antarctica
polar night
Queen Maud Land
genre_facet Antarc*
Antarctica
East Antarctica
polar night
Queen Maud Land
op_source XXVIII General Assembly of the International Union of Geodesy and Geophysics (IUGG)
op_relation info:eu-repo/semantics/altIdentifier/doi/10.57757/IUGG23-4561
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5020971
op_doi https://doi.org/10.57757/IUGG23-4561
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