Temperature, wind and atmospheric circulation in East Queen Maud Land, Antarctica

Proxy observations of wind and temperature are carried out in East Queen Maud Land. The atmospheric circulation patterns are further studied by in situ observation of the diurnal wind vector variation and the upper air soundings. It was revealed that the high wind directional constancy at Mizuho Sta...

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Bibliographic Details
Main Author: Tokio Kikuchi
Format: Article in Journal/Newspaper
Language:English
Japanese
Published: National Institute of Polar Research 1997
Subjects:
Online Access:https://doi.org/10.15094/00008958
https://doaj.org/article/cbfcd5436f65422784f090588d150b08
Description
Summary:Proxy observations of wind and temperature are carried out in East Queen Maud Land. The atmospheric circulation patterns are further studied by in situ observation of the diurnal wind vector variation and the upper air soundings. It was revealed that the high wind directional constancy at Mizuho Station is derived not only from the katabatic wind but also from the general synoptic pressure patterns. The katabatic wind is weakened when the westerly wind intensifies as part of the 30 to 50 day cycle synoptic pattern changes (T. YASUNARI and S. KODAMA, J. Geophys. Res., 98,13063,1992) of which the cause is still to be solved.