At resolutions greater than T639, which has a grid box dimension of about, the Arakawa-Schubert convective scheme produces minimal convective precipitation, making most precipitation unrealistically stratiform in nature.
32.
In the 1850s, mining began on stratiform native copper deposits in felsite-pebble conglomerates and in the upper zones of basalt lava flows ( locally called " amygdaloids " ).
33.
:Altostratus is a mid-level opaque or translucent stratiform or non-convective veil of grey / blue-grey cloud that often forms along warm fronts and around low-pressure areas.
34.
Later, in the 20th Century, an IMC commission for the study of clouds put forward a refined and more restricted definition of the genus nimbus, effectively reclassifying it as a stratiform cloud type.
35.
If the warm air mass is unstable, mixing of the warm moist air will produce thunderstorms that are embedded among the stratiform clouds ahead of the front, and after frontal passage, thundershowers may continue.
36.
Low �tage clouds have no height-related prefixes, so stratiform and stratocumuliform clouds based around 2 kilometres or lower are known simply as cumulus clouds with little vertical development are also commonly classified as low-�tage.
37.
Convective processes involve strong vertical motions that can cause the overturning of the atmosphere in that location within an hour and cause heavy precipitation, while stratiform processes involve weaker upward motions and less intense precipitation over a longer duration.
38.
When a low stratiform cloud contacts the ground, it is called fog if the prevailing surface visibility is less than 1 kilometer, although radiation and advection types of fog tend to form in clear air rather than from stratus layers.
39.
Moderate to large cumuliform and cumulonimbiform heaps and deep stratiform layers that occupy more than one altitude range are usually classified as vertical or multi-�tage . cumulonimbus may form anywhere from near the surface to intermediate heights of around 3 kilometres.
40.
However, the diabatic effects are responsible for the jet subsiding behind the leading edge of the MCS . The sinking of the jet first starts when the mid level inflow goes under the trailing stratiform cloud before descending to the melting layer.
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