Primarily, the extent to which the air is forced to rise. When more air rises, more of it reaches its dewpoint, condensing and eventually forming precipitation (rain or snow). There are different ways to get this, but the most common is for there to be some vorticity (energy) in the form of what we call a shortwave that gets injected into the mid levels of the atmosphere. Additionally, anywhere where warm air is forced to rise over cold air, as it is ahead of a warm front, provides some weak lift. Finally, instability provided by relatively warm water (as can happen near the Atlantic Ocean or Great Lakes) provides lift, as does physically forcing it over a barrier such as a mountain range.
The next most important factor is to have a source of moisture in the low-mid levels of the atmosphere. The Atlantic Ocean and Gulf of Mexico are great sources of moisture.
Precipitation tends to occur as rain or snow on mountaintops because as air rises up a mountain, it cools down. When the air cools, it can no longer hold as much moisture, causing the water vapor to condense and form clouds. This can lead to rain or snow depending on the temperature at higher elevations.
This can happen when the temperature of the air is close to freezing. If colder air is closer to the ground, snow will form. If warmer air is present, the snow will melt into rain before reaching the ground. This can result in a mix of rain and snow falling from the same storm system.
air rain and snow
Rain falls faster than snow from the sky because raindrops are larger and heavier than snowflakes, allowing them to fall at a quicker rate. Snowflakes are lighter and can be easily slowed down or carried by wind currents.
The amount of water vapor in the air has the greatest effect on the formation of rain or snow. When the air is saturated with water vapor and condensation occurs, precipitation can form as rain or snow depending on temperature conditions.
The Maritime Polar air mass brings rain and snow to the Pacific Northwest.
Often, the rain or snow falls on only one side of the mountain, the windward side. The other side of the mountain, the leeward side, which receives much less rain or snow. is said to be ' rain shadow'
The Maritime Polar air mass brings rain and snow to the Pacific Northwest.
Rain, snow, and ice are three forms of precipitation, liquid or ice formed by the condensation of water vapor from the air.
Wind, Rain, Snow, and sea
snow or rain
unbearingly cold frosty freezing icey air cold wind ect think of the weather :snow?rain?is the rain cold? is the snow icy? housestones? sorry if this didnt help :) x