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During
the month of June of each year fall sunlight perpendicular to the
Tropic of Cancer (23.5 degrees to the equator) marked the beginning
of summer climate in the northern hemisphere where this line that
exists on the amount of mid Kingdom solar radiation Fallen lead to
higher temperatures for most areas Which leads to lower air pressure
and a low heat on the Arabian peninsula related sprawl Low seasonal
India, which Limited north and west until it reaches to the eastern
Mediterranean, is among the characteristics that this
low-temperature air mass of very hot and dry and reflected the
temperature in this Chapter reach Britain, where between 44 to 47
degrees Celsius up to 50 degrees Celsius especially at the east of
the Kingdom can rank the first part of this period is, until July
half the dry summer period where there is this period northern winds
and dry warm and active periods leading The polluting peaking amid
the day interaction with the air along the high-centered in the
north west of Saudi Arabia, which arise with differences in the
values of temperature, pressure, and the eastern and central regions
of the Kingdom. The areas west of Saudi Arabia affected by the winds
East (poisons) that blow from time to time and be very hot and dry
and loaded with dust.
The
remainder of the period in question until the end of the summer
period could be classified on the coasts wet summer (July and last
until the end of September) and is characterized by a rise in
temperature and humidity, which runs frequently.
When
the East wind prevails and light to moderate at times eastern region
and are loaded with water vapour and because of the high
temperatures they are demanding significantly (Toz).
Yet
this does not (Iklohma) chapter in Gulf of nice to make the heights
of Asir, Baha and Taif resort destination nationals of the Kingdom
and Gulf countries, so if we gazed rate temperatures about 16
degrees smaller percentage may fall to 10 degrees as previously
recorded Abha in 1994.
If we
add to this mountain terrain and the presence of subtropical Front
(ITCZ), which is characterized by large amounts of water vapor in
the South and moved north to reach the fullest extent of the
district of Medina, cause these things together in rainfall may be
heavy in some years as previously And registered the highest amount
of precipitation in this chapter of Khamis Mushait (146 mm), Abha
(112 mm), Taif (143 mm) and in 1992 had been accompanied by activity
in surface winds depressed by wind where it arrived in Jizan (110
knots in 1991).
It should be
noted that at a time when the rain stopped on the eastern
Mediterranean influence extends well Front subtropical zone until
Medina since the torrential rains of 6 mm and 9 mm Riyadh, both in
July 1978 either Mecca reports had registered the highest amount of
precipitation presidency with the 1992 and 1998 Approximately (40
mm) and during the month of July.
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