The Physical Environment
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Atmospheric Moisture

Forms of precipitation

There are a variety of different types of precipitation but we’ll only treat four of the more common ones here. The kind of precipitation received  depends on the variation of temperature above the surface. Rain is precipitation in liquid form. Snow is precipitation in solid form as (typically) a hexagonal crystal shape. Size and shape of the crystal is dependent on moisture content and temperature of the air. Recall that in the middle and high latitudes rain begins as snow. If the air temperature near the surface is above freezing, the snow will melt into rain and fall in liquid form. If the air temperatures are below freezing on its journey toward the surface, precipitation will be in the form of snow. Sleet occurs when snow falls through a warm layer of air and melts. Before reaching the ground, the precipitation passes through a cold layer of air causing the water to refreeze and fall as sleet. Freezing rain occurs when snow melts upon passing through a warm layer of air and then freezes on the surface whose temperature is at or below freezing. Significant amounts of freezing rain coats the surface with a glaze of ice making roadways treacherous and toppling trees and downing power lines. Hail falls as rounded pellets or balls of ice from severe thunderstorms.  Vertical motions up-and-down through the storm create concentric rings of ice around the hail stone.

 

Heavy ice downs power lines (historical photograph)

Figure 7.32 A heavy cover of ice and snow bring down these power lines
(Source: NOAA)

 

Assess your basic understanding of the preceeding material by "Looking Back: Stability, Clouds and Precipitation" or skip and continue reading.

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For Citation: Ritter, Michael E. The Physical Environment: an Introduction to Physical Geography.
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Michael Ritter (tpeauthor@mac.com)

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