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The pressure gradient at the edge of an Ice Sheet

✍ Scribed by R. A. Hamilton

Publisher
John Wiley and Sons
Year
1959
Tongue
English
Weight
124 KB
Volume
85
Category
Article
ISSN
0035-9009

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✦ Synopsis

Abstract

Mean sea‐level pressures on the NE coast of Greenland are compared with those of a low‐level station within the edge of the inland ice. The comparison indicates that there is no evidence of an unusually high pressure gradient near the ice edge.

πŸ“œ SIMILAR VOLUMES

The diurnal variation of pressure on the
The diurnal variation of pressure on the Greenland ice sheet
✍ R. A. Hamilton πŸ“‚ Article πŸ“… 1959 πŸ› John Wiley and Sons 🌐 English βš– 281 KB

## Abstract The curve of the diurnal pressure variation at β€˜Northice’ shows a marked minimum in summer and autumn at about 0430 GMT. Maxima occur at 1300 and 2100 separated by a subsidiary minimum at 1730 GMT. The range is 0Β·3 mb.