Cloud
High clouds form at altitudes of in the polar regions, in the temperate regions and in the tropics. All cirriform clouds are classified as high and thus constitute a single genus "cirrus" (Ci). Stratocumuliform and stratiform clouds in the high altitude range carry the prefix "cirro-", yielding the respective genus names "cirrocumulus" (Cc) and "cirrostratus" (Cs). When limited-resolution satellite images of high clouds are analysed without supporting data from direct human observations, it becomes impossible to distinguish between individual forms or genus types, which are then collectively identified as "high-type" (or informally as "cirrus-type" even though not all high clouds are of the cirrus form or genus).Non-vertical clouds in the middle level are prefixed by "alto-", yielding the genus names "altocumulus" (Ac) for stratocumuliform types and "altostratus" (As) for stratiform types. These clouds can form as low as above surface at any latitude, but may be based as high as near the poles, at mid latitudes, and in the tropics. As with high clouds, the main genus types are easily identified by the human eye, but it is not possible to distinguish between them using satellite photography. Without the support of human observations, these clouds are usually collectively identified as "middle-type" on satellite images.
Low clouds are found from near surface up to . Genus types in this level either have no prefix or carry one that refers to a characteristic other than altitude. Clouds that form in the low level of the troposphere are generally of larger structure than those that form in the middle and high levels, so they can usually be identified by their forms and genus types using satellite photography alone.
Global Energy and Water Cycle Experiment
GEWEX Cloud System Study (GCSS) task is to individualize modeling for different types of cloud systems. GCSS identifies 5 types of cloud systems:boundary layer, cirrus, extra tropical layer, precipitating convective, and polar. These cloud systems are generally too small to be rationalized in large scale climate modeling, this results in inadequate development of equations resulting in greater statistical uncertainty in results. In order to rationalize these process the study observes cloud systems at single fixed positions on earth in order to better estimate their parameters. These four areas are: Azores and Madeira Islands, Barbados, Equatorial Western Pacific, and Atlantic Tropics. The initial data collection is complete, methods developed for land and aircraft based observations can be compared with satellite observations to that better models of cloud system identification can be made at smaller scales.