Arizona Heating and Cooling Climatic Factors

Arizona has three principal topographic areas, whichand juniper trees. Most of Arizona lies in the drainage
control the Arizona heating and air climate. Thebasin of the Colorado River, which empties eventually
northeastern section of the state has a high plateauinto the Gulf of California. The world-famous Grand
which averages 6,000 feet in elevation. There is aCanyon extends towards the southwest 217 miles
mountainous area which runs from southeast tofrom the confluence of the Little Colorado with the
northwest with between 9,000 and 12,000 feetmain river. The width of the Grand Canyon varies
elevations. The southwestern part of the statefrom 4 to almost 18 miles, and its depth varies from
features desert valleys and low mountain ranges. An2700 to 5700 feet.
unbroken forest of Ponderosa Pine lies between theArizona heating and cooling in winter can result from
White Mountain region and the San Franciscomasses of cold air which travel from Canada, bringing
Mountains, and this strip of forest continues north ofwith them below-zero temperatures in the
the Grand Canyon along the Kaibab Plateau and onmountainous and high plateau areas in the central and
into the southern part of Utah. The highest point innorthern parts of the state. Low temperatures can
Arizona, with elevation 12,611 feet, is Humphreysreach 35° below zero Fahrenheit in the winter. In
Peak which is northwest of Flagstaff. The secondthe summer months at lower elevations
highest point is Baldy Peak, elevation 11,490 feet,temperatures exceeding 125° Fahrenheit have
located in eastern Arizona's White Mountains. On thebeen recorded. Moreover, there can be vast
other hand, the elevations of the desert Valleys inextremes between daytime and nighttime
the Lower Colorado River Valley in the southwesterntemperatures exceeding 50° Fahrenheit in many
portion of the state are as low as 100 feet.parts of the state in the drier months of the year. In
Arizona heating and precipitation vary considerably asthe winter the daytime temperature in the desert
a result of this topographic variation. In the highervalleys can average 70° Fahrenheit, with the
elevations, which run diagonally from the southeastnighttime temperature falling to below freezing. In the
of the state to the northwest, the rainfall averagessummer in the pine clad forests in the central region
between 25" and 30" per year. On the other hand,of Arizona the daytime temperature may average
the desert regions in the southwest portions of the80° Fahrenheit and then fall to 35°
state average as low as 3" to 4" per year. TheFahrenheit at night. As one might suppose, the length
northeastern plateau region receives about 10" ofof the possible growing season can vary a great deal
precipitation per year. Because most of thein different parts of the state, averaging under three
vegetation in this region consists of native grassesmonths in the higher regions in the north and east
and sagebrush, the area is utilized mostly for grazing.whereas the lower desert valleys can go for years
The high ridges in this area are covered with pinionwithout a freeze.