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- W2178520608 abstract "Abstract The surface wind pattern over the ice sheets of Antarctica is irregular with marked areas of airflow confluence near the coastal margins. Where cold air from a large interior area of the ice sheet converges (a confluence zone), an anomalously large supply of air is available to feed the coastal katabatic winds, which, as a result, are intensified and more persistent. The confluence zone inland of Siple Coast, West Antarctica, differs from its East Antarctic counterparts in that the terrain slopes become gentler rather than steeper as the coast is approached. In addition, synoptic processes exert substantially more impact on the behavior of the surface winds. A month-long field program to study the dynamics of the springtime katabatic wind confluence zone has been carried out near Siple Coast. Two sites, Upstream B (83.5°S, 136.1°W) and South Camp (84.5°S, 134.3°W), were established roughly perpendicular to the downslope direction. The field program involved the use of the ground-based remote sens..." @default.
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- W2178520608 date "1997-02-01" @default.
- W2178520608 modified "2023-09-29" @default.
- W2178520608 title "Dynamics of the Katabatic Wind Confluence Zone near Siple Coast, West Antarctica" @default.
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- W2178520608 doi "https://doi.org/10.1175/1520-0450(1997)036<0097:dotkwc>2.0.co;2" @default.
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