
Cirrus spissatus
© Wetterkurs.ch
The name "spissatus" (Latin: thickened, dense) describes a cirrus that is so compact and optically dense that it can partially or completely obscure the sun. In contrast to the delicate, translucent forms of other cirrus types, Cirrus spissatus appears as a grey-white to whitish field in the sky that looks noticeably thicker. These clouds frequently form from the upper parts of powerful cumulonimbus clouds (known as anvil remnants) or through strong lifting processes in the upper troposphere. They consist entirely of ice crystals and can reach a considerable horizontal extent. Cirrus spissatus is the densest of all cirrus types and sometimes forms the transition to cirrostratus.
Highlighted: all genera with which spissatus occurs.
Cirrus spissatus can carry different meteorological significance depending on its origin. If it derives from the remnants of a cumulonimbus anvil, it indicates past thunderstorm activity and has no immediate forecasting relevance. However, if it appears ahead of an approaching warm front, it can be regarded as a harbinger of increasing cloud cover and subsequent precipitation. In conjunction with a build-up and spread of high clouds, Cirrus spissatus can indicate a deterioration in weather within the next 12 to 24 hours. When occurring in isolation, it is generally of little meteorological significance.