Summertime boundary layer winds over the Darwin–Hatherton glacial system, Antarctica: observed features and numerical analysis

Abstract Three temporary Automatic Weather Stations measured summertime surface layer climate over the Darwin–Hatherton Glacial system. These data were used to test a Polar optimized Weather Research and Forecasting model (Polar-WRF) simulation for December as a case study. Observations show differe...

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Published in:Antarctic Science
Main Authors: Zawar-Reza, Peyman, George, Steve, Storey, Bryan, Lawson, Wendy
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 2010
Subjects:
Bia
Online Access:http://dx.doi.org/10.1017/s0954102010000817
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0954102010000817
id crcambridgeupr:10.1017/s0954102010000817
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spelling crcambridgeupr:10.1017/s0954102010000817 2024-03-03T08:38:42+00:00 Summertime boundary layer winds over the Darwin–Hatherton glacial system, Antarctica: observed features and numerical analysis Zawar-Reza, Peyman George, Steve Storey, Bryan Lawson, Wendy 2010 http://dx.doi.org/10.1017/s0954102010000817 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0954102010000817 en eng Cambridge University Press (CUP) https://www.cambridge.org/core/terms Antarctic Science volume 22, issue 6, page 619-632 ISSN 0954-1020 1365-2079 Geology Ecology, Evolution, Behavior and Systematics Oceanography journal-article 2010 crcambridgeupr https://doi.org/10.1017/s0954102010000817 2024-02-08T08:45:45Z Abstract Three temporary Automatic Weather Stations measured summertime surface layer climate over the Darwin–Hatherton Glacial system. These data were used to test a Polar optimized Weather Research and Forecasting model (Polar-WRF) simulation for December as a case study. Observations show differences in hourly averaged solar and net all-wave radiation between white ice and blue ice areas (BIAs). Although the down-welling solar radiation is higher over the white ice region, the net all-wave energy is higher over the BIA. Derived albedo for each surface type confirms that the blue ice areas have lower albedo. Also, the hourly averaged temperatures are higher at lower elevation stations, creating a gradient towards the Ross Ice Shelf. Analysis shows that there is a diurnal oscillation in strength and intensity of the katabatic wind. The two lower stations register a distinct reversal of wind direction in the early afternoon due to intrusion of an anabatic circulation. Anabatic winds are not prevalent further up the Darwin Glacier. A high-resolution Polar-WRF simulation as a case study shows good agreement with observations. The December 2008 case study is characterized by a strong south-westerly katabatic wind over Hatherton, whereas the flow over Lower Darwin was diurnally reversing. Polar-WRF shows that the katabatic front advanced and retreated periodically between Hatherton and Lower Darwin. Article in Journal/Newspaper Antarc* Antarctic Science Antarctica Darwin Glacier Ice Shelf Ross Ice Shelf Cambridge University Press Ross Ice Shelf Bia ENVELOPE(22.891,22.891,70.317,70.317) Darwin Glacier ENVELOPE(159.000,159.000,-79.883,-79.883) Antarctic Science 22 6 619 632
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
topic Geology
Ecology, Evolution, Behavior and Systematics
Oceanography
spellingShingle Geology
Ecology, Evolution, Behavior and Systematics
Oceanography
Zawar-Reza, Peyman
George, Steve
Storey, Bryan
Lawson, Wendy
Summertime boundary layer winds over the Darwin–Hatherton glacial system, Antarctica: observed features and numerical analysis
topic_facet Geology
Ecology, Evolution, Behavior and Systematics
Oceanography
description Abstract Three temporary Automatic Weather Stations measured summertime surface layer climate over the Darwin–Hatherton Glacial system. These data were used to test a Polar optimized Weather Research and Forecasting model (Polar-WRF) simulation for December as a case study. Observations show differences in hourly averaged solar and net all-wave radiation between white ice and blue ice areas (BIAs). Although the down-welling solar radiation is higher over the white ice region, the net all-wave energy is higher over the BIA. Derived albedo for each surface type confirms that the blue ice areas have lower albedo. Also, the hourly averaged temperatures are higher at lower elevation stations, creating a gradient towards the Ross Ice Shelf. Analysis shows that there is a diurnal oscillation in strength and intensity of the katabatic wind. The two lower stations register a distinct reversal of wind direction in the early afternoon due to intrusion of an anabatic circulation. Anabatic winds are not prevalent further up the Darwin Glacier. A high-resolution Polar-WRF simulation as a case study shows good agreement with observations. The December 2008 case study is characterized by a strong south-westerly katabatic wind over Hatherton, whereas the flow over Lower Darwin was diurnally reversing. Polar-WRF shows that the katabatic front advanced and retreated periodically between Hatherton and Lower Darwin.
format Article in Journal/Newspaper
author Zawar-Reza, Peyman
George, Steve
Storey, Bryan
Lawson, Wendy
author_facet Zawar-Reza, Peyman
George, Steve
Storey, Bryan
Lawson, Wendy
author_sort Zawar-Reza, Peyman
title Summertime boundary layer winds over the Darwin–Hatherton glacial system, Antarctica: observed features and numerical analysis
title_short Summertime boundary layer winds over the Darwin–Hatherton glacial system, Antarctica: observed features and numerical analysis
title_full Summertime boundary layer winds over the Darwin–Hatherton glacial system, Antarctica: observed features and numerical analysis
title_fullStr Summertime boundary layer winds over the Darwin–Hatherton glacial system, Antarctica: observed features and numerical analysis
title_full_unstemmed Summertime boundary layer winds over the Darwin–Hatherton glacial system, Antarctica: observed features and numerical analysis
title_sort summertime boundary layer winds over the darwin–hatherton glacial system, antarctica: observed features and numerical analysis
publisher Cambridge University Press (CUP)
publishDate 2010
url http://dx.doi.org/10.1017/s0954102010000817
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0954102010000817
long_lat ENVELOPE(22.891,22.891,70.317,70.317)
ENVELOPE(159.000,159.000,-79.883,-79.883)
geographic Ross Ice Shelf
Bia
Darwin Glacier
geographic_facet Ross Ice Shelf
Bia
Darwin Glacier
genre Antarc*
Antarctic Science
Antarctica
Darwin Glacier
Ice Shelf
Ross Ice Shelf
genre_facet Antarc*
Antarctic Science
Antarctica
Darwin Glacier
Ice Shelf
Ross Ice Shelf
op_source Antarctic Science
volume 22, issue 6, page 619-632
ISSN 0954-1020 1365-2079
op_rights https://www.cambridge.org/core/terms
op_doi https://doi.org/10.1017/s0954102010000817
container_title Antarctic Science
container_volume 22
container_issue 6
container_start_page 619
op_container_end_page 632
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