Cloud and precipitation properties from ground-based remote-sensing instruments in East Antarctica
http://www.the-cryosphere.net/9/285/2015/tc-9-285-2015.pdf A new comprehensive cloud–precipitation–meteorological observatory has been established at Princess Elisabeth base, located in the escarpment zone of Dronning Maud Land (DML), East Antarctica. The observatory consists of a set of ground-base...
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Language: | English |
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ftunivleuven:oai:lirias.kuleuven.be:123456789/487430 2023-05-15T13:49:09+02:00 Cloud and precipitation properties from ground-based remote-sensing instruments in East Antarctica Gorodetskaya, Irina Kneifel, Stefan Maahn, Maximilian Van Tricht, Kristof Thiery, Wim Schween, Jan Mangold, Alexander Crewell, Susanne Van Lipzig, Nicole 2015-01 3540956 bytes application/pdf https://lirias.kuleuven.be/handle/123456789/487430 https://doi.org/10.5194/tc-9-285-2015 https://lirias.kuleuven.be/bitstream/123456789/487430/1//Gorodetskaya_2015_TheCryosphere.pdf en eng Cryosphere vol:9 pages:285-304 https://lirias.kuleuven.be/handle/123456789/487430 1994-0416 doi:10.5194/tc-9-285-2015 1994-0424 https://lirias.kuleuven.be/bitstream/123456789/487430/1//Gorodetskaya_2015_TheCryosphere.pdf 307370;public Antarctica clouds precipitation surface mass balance ground-based remote sensing meteorology Article IT 307370;Article 2015 ftunivleuven https://doi.org/10.5194/tc-9-285-2015 2017-06-02T19:29:42Z http://www.the-cryosphere.net/9/285/2015/tc-9-285-2015.pdf A new comprehensive cloud–precipitation–meteorological observatory has been established at Princess Elisabeth base, located in the escarpment zone of Dronning Maud Land (DML), East Antarctica. The observatory consists of a set of ground-based remote-sensing instruments (ceilometer, infrared pyrometer and vertically profiling precipitation radar) combined with automatic weather station measurements of near-surface meteorology, radiative fluxes, and snow height. In this paper, the observatory is presented and the potential for studying the evolution of clouds and precipitating systems is illustrated by case studies. It is shown that the synergetic use of the set of instruments allows for distinguishing ice, liquid-containing clouds and precipitating clouds, including some information on their vertical extent. In addition, wind-driven blowing snow events can be distinguished from deeper precipitating systems. Cloud properties largely affect the surface radiative fluxes, with liquid-containing clouds dominating the radiative impact. A statistical analysis of all measurements (in total 14 months mainly during summer–beginning of winter) indicates that these liquid-containing clouds occur during as much as 20% of the cloudy periods. The cloud occurrence shows a strong bimodal distribution with clear-sky conditions 51% of the time and complete overcast conditions 35% of the time. Snowfall occurred during 17% of the cloudy periods with a predominance of light precipitation and only rare events with snowfall >1 mm h−1 water equivalent (w.e.). Three of such intense snowfall events occurred during 2011 contributing to anomalously large annual surface mass balance (SMB). Large accumulation events (>10 mm w.e. day−1) during the radar-measurement period of 26 months were always associated with snowfall, but at the same time other snowfall events did not always lead to accumulation. The multiyear deployment of a precipitation radar in Antarctica allows for assessing the contribution of the snowfall to the local SMB and comparing it to the other SMB components. During 2012, snowfall rate was 110 ± 20 mm w.e. yr−1, from which surface and drifting snow sublimation removed together 23%. Given the measured yearly SMB of 52 ± 3 mm w.e., the residual term of 33 ± 21 mm w.e. yr−1 was attributed to the wind-driven snow erosion. In general, this promising set of robust instrumentation allows for improved insight into cloud and precipitation processes in Antarctica and can be easily deployed at other Antarctic stations. status: published Article in Journal/Newspaper Antarc* Antarctic Antarctica DML Dronning Maud Land East Antarctica KU Leuven: Lirias Antarctic Dronning Maud Land East Antarctica Princess Elisabeth Base ENVELOPE(23.200,23.200,-71.570,-71.570) The Cryosphere 9 1 285 304 |
institution |
Open Polar |
collection |
KU Leuven: Lirias |
op_collection_id |
ftunivleuven |
language |
English |
topic |
Antarctica clouds precipitation surface mass balance ground-based remote sensing meteorology |
spellingShingle |
Antarctica clouds precipitation surface mass balance ground-based remote sensing meteorology Gorodetskaya, Irina Kneifel, Stefan Maahn, Maximilian Van Tricht, Kristof Thiery, Wim Schween, Jan Mangold, Alexander Crewell, Susanne Van Lipzig, Nicole Cloud and precipitation properties from ground-based remote-sensing instruments in East Antarctica |
topic_facet |
Antarctica clouds precipitation surface mass balance ground-based remote sensing meteorology |
description |
http://www.the-cryosphere.net/9/285/2015/tc-9-285-2015.pdf A new comprehensive cloud–precipitation–meteorological observatory has been established at Princess Elisabeth base, located in the escarpment zone of Dronning Maud Land (DML), East Antarctica. The observatory consists of a set of ground-based remote-sensing instruments (ceilometer, infrared pyrometer and vertically profiling precipitation radar) combined with automatic weather station measurements of near-surface meteorology, radiative fluxes, and snow height. In this paper, the observatory is presented and the potential for studying the evolution of clouds and precipitating systems is illustrated by case studies. It is shown that the synergetic use of the set of instruments allows for distinguishing ice, liquid-containing clouds and precipitating clouds, including some information on their vertical extent. In addition, wind-driven blowing snow events can be distinguished from deeper precipitating systems. Cloud properties largely affect the surface radiative fluxes, with liquid-containing clouds dominating the radiative impact. A statistical analysis of all measurements (in total 14 months mainly during summer–beginning of winter) indicates that these liquid-containing clouds occur during as much as 20% of the cloudy periods. The cloud occurrence shows a strong bimodal distribution with clear-sky conditions 51% of the time and complete overcast conditions 35% of the time. Snowfall occurred during 17% of the cloudy periods with a predominance of light precipitation and only rare events with snowfall >1 mm h−1 water equivalent (w.e.). Three of such intense snowfall events occurred during 2011 contributing to anomalously large annual surface mass balance (SMB). Large accumulation events (>10 mm w.e. day−1) during the radar-measurement period of 26 months were always associated with snowfall, but at the same time other snowfall events did not always lead to accumulation. The multiyear deployment of a precipitation radar in Antarctica allows for assessing the contribution of the snowfall to the local SMB and comparing it to the other SMB components. During 2012, snowfall rate was 110 ± 20 mm w.e. yr−1, from which surface and drifting snow sublimation removed together 23%. Given the measured yearly SMB of 52 ± 3 mm w.e., the residual term of 33 ± 21 mm w.e. yr−1 was attributed to the wind-driven snow erosion. In general, this promising set of robust instrumentation allows for improved insight into cloud and precipitation processes in Antarctica and can be easily deployed at other Antarctic stations. status: published |
format |
Article in Journal/Newspaper |
author |
Gorodetskaya, Irina Kneifel, Stefan Maahn, Maximilian Van Tricht, Kristof Thiery, Wim Schween, Jan Mangold, Alexander Crewell, Susanne Van Lipzig, Nicole |
author_facet |
Gorodetskaya, Irina Kneifel, Stefan Maahn, Maximilian Van Tricht, Kristof Thiery, Wim Schween, Jan Mangold, Alexander Crewell, Susanne Van Lipzig, Nicole |
author_sort |
Gorodetskaya, Irina |
title |
Cloud and precipitation properties from ground-based remote-sensing instruments in East Antarctica |
title_short |
Cloud and precipitation properties from ground-based remote-sensing instruments in East Antarctica |
title_full |
Cloud and precipitation properties from ground-based remote-sensing instruments in East Antarctica |
title_fullStr |
Cloud and precipitation properties from ground-based remote-sensing instruments in East Antarctica |
title_full_unstemmed |
Cloud and precipitation properties from ground-based remote-sensing instruments in East Antarctica |
title_sort |
cloud and precipitation properties from ground-based remote-sensing instruments in east antarctica |
publishDate |
2015 |
url |
https://lirias.kuleuven.be/handle/123456789/487430 https://doi.org/10.5194/tc-9-285-2015 https://lirias.kuleuven.be/bitstream/123456789/487430/1//Gorodetskaya_2015_TheCryosphere.pdf |
long_lat |
ENVELOPE(23.200,23.200,-71.570,-71.570) |
geographic |
Antarctic Dronning Maud Land East Antarctica Princess Elisabeth Base |
geographic_facet |
Antarctic Dronning Maud Land East Antarctica Princess Elisabeth Base |
genre |
Antarc* Antarctic Antarctica DML Dronning Maud Land East Antarctica |
genre_facet |
Antarc* Antarctic Antarctica DML Dronning Maud Land East Antarctica |
op_relation |
Cryosphere vol:9 pages:285-304 https://lirias.kuleuven.be/handle/123456789/487430 1994-0416 doi:10.5194/tc-9-285-2015 1994-0424 https://lirias.kuleuven.be/bitstream/123456789/487430/1//Gorodetskaya_2015_TheCryosphere.pdf |
op_rights |
307370;public |
op_doi |
https://doi.org/10.5194/tc-9-285-2015 |
container_title |
The Cryosphere |
container_volume |
9 |
container_issue |
1 |
container_start_page |
285 |
op_container_end_page |
304 |
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1766250953683501056 |