Climatological factors
Heights
This province totally is a mountainous area along the Zagros that is starting from northwest to southwest. The highest part of the province is in Zardkoohe Bakhtiary to the height of 4300 meters and the lowest zone is situated in East of the province. The heights of province are always snow covered. The role of these heights is to evacuate the humid flows. Because these heights are perpendicular to west humid flows, autumn and winter rains are mostly icy and snow form. These flows are usually Mediterranean which evacuate its moisture in central zone.
Latitude
Chaharmahal va Bakhtiary is not so spreading. So this is not so effective in variation of climate. But it will effects on atmosphere factors like the Sunshine hours and the sun radiation along the north to South direction.
Vegetation
This is related to the climate of the zone, which effects on the zone vegetation. Because of raining in the province with different amount, various kinds of plants in the west,and jungle plants have been appeared which is referred to climate diversity of the region.
Water sources
The existence of water sources helps the weather being temperate. The flow of water in the area is divided into two parts. One of them goes to Karoon and the other goes to Zayandehrood. There more than 200 rivers in the province. They effect on other water sources. Also the region climate and condition is affected. Various plants covering naturally and man made, also effect on the climate.
The summary of appointing the climate of Shahrekord by different methods
Estimated
coefficients
Appointed climates The type of
classification
32.3 Semi Equatorial Hanson
83.189 Extra temperate The coefficient
of temperance
315 Semi dry Blair
14.7 Semi dry Domarton
0.09 Extra dry Selyaninov
0.73 Woody Steppe Ivanov
0.76 Semi humid Barat
27.5 Cold dry Emberger
65 Semi humid Khosh akhlagh
20.8 Semi humid cold winter Gorsczynski
1.77 Semi humid with temperate summer and
very cold winter
Karimi
Temperate cold with dry and hot summer Koppen
Cold steppe Goussen
The summary of appointing the climate of Borujen by different methods
Estimated
coefficients
Appointed climates The type of
classification
32 Semi equatorial Hanson
75.06 Extra temperate The coefficient
of temperance
199 Dry Blair
9.7 Dry De martonne
0.07 Extra dry Selyaninov
0.53 Steppe Ivanov
0.22 Semi dry Barat
37.29 Cold dry Emberger
18.3 Semi dry Khosh akhlagh
20.12 Marine cold dry winter Gorsczynski
2.6 Semi humid – temperate summer very cold
winter
Karimi
Cold temperate with dry warm summer Koppen
Cold steppe Goussen
The summary of appointing the climate of Koohrang by different methods
Estimated
coefficients
Appointed climates The type of
classification
32.4 Equatorial Hanson
66.09 Extra temperate The coefficient
of temperance
1407 Humid Blair
7407 Very humid De martonne
0.42 Extra semi dry Selyaninov
3.78 Extra jungle humid Ivanov
10.05 Woody humid Barat
323.7 Very humid Emberger
121.4 Very humid - very cold Khosh akhlagh
27.9 Marine cold humid winter Gorsczynski
0.37 Very humid - temperate summer
and cold winter
Karimi
Dcbs Cold temperate, cold dry summer Koppen
Cold steppe Goussen
The summary of appointing the climate of Lordegan by different methods
Estimated
coefficients
Appointed climates The type of
classification
31.5 Half equatorial Hanson
98.9 Extra temperate The coefficient
of temperance
540 Semi humid Blair
21.3 Mediterranean De martonne
0.29 Dry Selyaninov
0.83 Jungle plants Ivanov
2.6 Semi humid Barat
86.9 Humid Emberger
47.6 Semi cold humid Khosh akhlagh
20.8 Marine mild winter and semi humid Gorsczynski
Semi humid – warm summer cold winter Karimi
Cas Semi hot – dry warm summer Koppen
Medite rranean dry and warm Goussen
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