Yukimarimo at Dome C, Antarctica
ABSTRACT Balls of frost (yukimarimo) up to 12 cm in diameter and weighing up to 14 g were observed forming in light winds in the temperature range, −70 to −60 °C at Dome Charlie, Antarctica, during the 2014 winter. Their density ranged from 15 to 60 kg m −3 . Meteorological conditions during four fo...
| Published in: | Journal of Glaciology |
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| Main Author: | |
| Format: | Article in Journal/Newspaper |
| Language: | English |
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Cambridge University Press (CUP)
2016
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| Subjects: | |
| Online Access: | http://dx.doi.org/10.1017/jog.2016.30 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143016000307 |
| Summary: | ABSTRACT Balls of frost (yukimarimo) up to 12 cm in diameter and weighing up to 14 g were observed forming in light winds in the temperature range, −70 to −60 °C at Dome Charlie, Antarctica, during the 2014 winter. Their density ranged from 15 to 60 kg m −3 . Meteorological conditions during four formation periods are tabulated. Their formation seems to be due to a clumping of crystals caused by electrostatic attraction, followed by the collection of hoarfrost crystals while rolling along the snow surface. |
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