(1) Latitude
(2) Elevation
(3) Nearby Water
(4) Ocean Currents
(5) Topography
(6) Vegetation
(7) Prevailing Winds
(8) Precipitation
Cannon Beach
is geographically located along a narrow strip of Oregon coastline. It is considered to be part of the marine west
coast climate. This climate is very
humid throughout most of the year. Its
geographic location puts Cannon Beach in the direct path of westerly winds from
the Pacific Ocean, which helps to produce cloudy skies, abundant precipitation,
and mild temperatures. The Coastal Range
mountains to the east of Cannon Beach helps to influence the climate also.
The most
important climate control of this area is the west coast location in the
mid-latitudes. The Maritime Polar air
masses are constantly moving ashore bringing high humidity from the water and
mild temperatures. Since the ocean does
not heat or cool as quickly as land, the ocean currents help moderate the
temperature of Cannon Beach. In addition
to affecting temperature, warm ocean currents help promote instability in the
atmosphere, enhancing uplift and precipitation.
As stated
above, the orientation of the mountains to the east of Cannon Beach has an
important role in the climate of this area. The north-south orientation acts as a barrier
to oceanic air masses in the Westerlies forcing them to rise and cool
resulting in the production of cloudy, rainy conditions along the coast. The north-south aligned mountains cause this
uplift and precipitation on their windward western slopes and dry conditions on
the leeward eastern slopes. The ocean
currents essentially parallel the direction of the global wind system. Mid-latitude weather systems tend to move in
a west-to-east direction in North America.
Since this
blog is limited in space, I have attached several other slides containing more information
on Cannon Beach climate.
Sources:
http://highered.mcgraw-hill.com/sites/dl/free/0072873647/574123/ch08.pdf
http://www4.uwsp.edu/geo/faculty/ritter/geog101/textbook/climate_systems/marine_west_coast.html
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