hi help me now peeps?

Question

please name 3 forms of precipitation

Answer 1

sorry I can't help u

Answer 2

A headlong fall or rush.
Abrupt or impulsive haste.
A hastening or acceleration, especially one that is sudden or unexpected: He is responsible for the precipitation of his own demise.
Meteorology.
Any form of water, such as rain, snow, sleet, or hail, that falls to the earth's surface.
The quantity of such water falling in a specific area within a specific period.
Chemistry. The process of separating a substance from a solution as a solid.

(Is that enough)............

Answer 3

3 forms of Precipitations are:

Convective precipitation:

Convective precipitationConvective, or showery, precipitation occurs from convective clouds, e.g., cumulonimbus or cumulus congestus. It falls as showers, with rapidly changing intensity and at one moment only over patches, as convective clouds have limited horizontal extent. Convective precipitation is most important in the tropics. Graupel and hail always indicate convection. In midlatitudes, convective precipitation is associated with cold fronts (often behind the front), squall lines, and warm fronts with significant available moisture.

Stratiform precipitation:

Stratiform, or large-scale, precipitation occurs as a consequence of slow (cm/s) ascent of air in synoptic systems, such as along cold fronts, and in advance of warm fronts. Similar is the ascent is seen around Tropical cyclones outside of the eyewall, and in comma head precipitation patterns around mid-latitude cyclones.


Orographic precipitation:

Orographic precipitationOrographic precipitation occurs on the windward side of mountains and is caused by the rising air motion of a large-scale flow of moist air across the mountain ridge, resulting in adiabatic cooling and condensation. In parts of the world subjected to relatively consistent winds (for example the trade winds), a wetter climate prevails on the windward side of a mountain than on the leeward (downwind) side as moisture is removed by orographic precipitation, leaving drier air (see katabatic wind) on the descending (generally warming), leeward side where a rain shadow is observed. Similarly, the interior of larger mountain zones is often quite dry, such as the Great Basin in North America.

Orographic precipitation is well known on oceanic islands, such as the Hawaiian Islands, where much of the rainfall received on an island is on the windward side, and the leeward side tends to be quite dry, almost desert-like, by comparison. This phenomenon results in substantial local gradients of average rainfall, with coastal areas receiving on the order of 500 to 750 mm per year (20 to 30 inches), and interior uplands receiving over 2.5 m per year (100 inches). Leeward coastal areas are especially dry 500 mm per year (20 inches)at Waikiki), and the tops of moderately high uplands are especially wet ~12 m per year (~475 inches) at Wai'ale'ale on Kaua'i).

Answer 4

I have no idea why brainless people use the word "Lil" in their name

Answer 5

umm... rain, snow, and hail?