Precipitation Patterns: Midlatitudes to the PolesBeginning along the northwest coast of the United States (coastal Oregon and Washington) and the west coast of Canada (British Columbia) we see a narrow strip of high annual precipitation. The large amount of precipitation is due to the orographic uplift of west - to - east flowing air masses from the ocean. These moist maritime polar air masses are forced to rise up the windward side of north-south oriented mountain chains inducing them to drop copious amounts of precipitation. In many places the amount of precipitation can exceed 100 inches rivaling the amounts found in the tropical rain forests. A short distance inland on the leeward side shows much less precipitation. The lee side of a mountain sits in the "rain shadow".
Traveling down the coast we experience a decrease in precipitation once we get to the southwestern coast of North
America around southern California. The annual rainfall map doesn’t gives us a
very good picture of what the actual precipitation regime is like in this part
of the world though. Examine the climograph for San Francisco, California (Figure 7.38). San Francisco is located in what’s called the dry summer subtropical
climate. The dry summer is due to the presence of the subtropical high that
migrates into this region during the summer. The subsidence of the subtropical high keeps
air from rising off the surface and dries the air through adiabatic warming.
Additionally, as maritime air streams toward land it passes over the cold
California Current. The cold ocean current chills the air near the surface and steepens the environmental lapse rate of temperature in the air mass making it stable (mTs). The combined effect of these factors
inhibits precipitation formation and thus creates the dry summer typical of this
region. Winter is the wet season as subtropical high pressure slides south and
the polar front with its accompanying cyclonic activity migrates into this
region. Figure 7. 39 Annual precipitation coterminous United States (Courtesy National Atlas USGS) Proceeding into the desert of the southwestern portion of the United States a noticeable decrease in precipitation occurs. The meager amount of precipitation found in this region is in part due to the lack of available water for evaporation. The desert is located on the leeward side of mountains which also accounts for part of the dryness. Additionally, a high–level high pressure pattern over the western United States is responsible for the summer-time dry conditions. At the surface, heating creates a shallow region of low pressure. Though air can be uplifted by convection and the convergence of air into the low at the surface, an upper – level high helps to suppress cloud development and precipitation.
Figure 7.40 Clouds rising along the windward slopes of the Colorado Front Range.(Image courtesy Michael Ritter) Moving eastward across the western states one experiences an alternating pattern of lower and higher amounts of precipitation. This pattern is due to the orographic uplift on the wet windward slopes and then drier leeward slopes. The fact that one is a great distance from the source region for moist air also decreases the likelihood for precipitation in the intermountain west. High annual precipitation and humid conditions prevail in the southeastern part of the United States. The source region for maritime tropical air is located over the Gulf of Mexico and the Caribbean. When this air mass streams over land, convective uplift can create significant precipitation. Along the southeast coast the air mass travels over the warm Gulf Stream which increases the instability of the air. The effect of location with respect to the source region can be seen in the pattern of precipitation. Precipitation decreases as one moves inland toward the northwest. Figure 7.41 illustrates the effect of location on the seasonal variation of precipitation as one moves away from the ocean. As one moves poleward the precipitation decreases and becomes more seasonal.
Figure 7. 41 Latitudinal variation of precipitation through the U.S. A moderate amount of precipitation occurs in the central US increasing toward the east and northeast coast of the United States and Canada. This region is dominated by the polar front and cyclonic activity. The clash of cold air masses from the north and warmer ones to the south creates frontal uplift and precipitation. Precipitation decreases northward through Canada as air temperature and its associated saturation point decreases. |
Figure 7. 38 Climograph for San Francisco, CA.
