A study of precipitating clouds close to fronts using microwave radiometry and radar in Svalbard, Arctic
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説明
Developed cyclones and deeply occluded fronts are often found in polar regions. Observations of precipitating clouds associated with fronts and a cyclone were carried out in Ny-Alesund, Svalbard, using a microwave radiometer and other meteorological instruments. Precipitating clouds to the north of a warm front were stratiform and held no liquid water. Precipitating clouds in and behind two occluded fronts and a cold front were convective clouds. Precipitating clouds in the centre of a cyclone were also convective, while precipitating clouds behind the cyclone were stratiform. Some clouds contained no liquid water, but others contained a substantial amount.
収録刊行物
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- Atmospheric Research
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Atmospheric Research 49 253-265, 1998-09-01
Elsevier BV
