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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Bibliographic Details
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:
Geology
Ecology, Evolution, Behavior and Systematics
Oceanography
Ross Ice Shelf
Bia
Darwin Glacier
Antarc*
Antarctic Science
Antarctica
Ice Shelf
Online Access:http://dx.doi.org/10.1017/s0954102010000817
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0954102010000817
Description
Summary: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.

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