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According
to the combination of meteorological elements it is possible to
allocate three basic types of climate in Crimea such as:
- dry-temperate continental plain steppe climate,
with hot dry summer and cool damp winter,
- temperate -wet -hill-forest mild-continental
climate with warm, rather damp summer and cool damp winter,
- submediterranean mild-continental south-coast
climate with hot dry summer and relatively warm, damp winter.
There are a lot of intermediate variants between
these types of climate. For example, in foothill areas (Simferopol,
Zuya, Belogorsk) the climate is transitive from plain steppe to
hill-forest - it is possible to call it foothill forest-steppe climate.
In the flat-plain Crimea the climate is steppe,
temperately continental, dry: cool winter (average temperature in
January is from-3 up to 0°C) and hot summer (average temperature
in July is from +21 up to +23°C) Amount of precipitation is
- 350-450 mm/a year, and their big part drops out in the summer
as downpours.
Distinctions between climates of seaside territories
(Chernomorskoye, Yevpatoria, Kerch) and the central part of peninsula
(Krasnogvardeyskoye, Dzankoy, Pervomayskoye) are observed. In the
seaside part relative humidity and intensity of solar radiation
are higher, but cloudiness and amount of precipitation is lower.
Such climate can be called marine steppe.
Climatic characteristics of geographical
areas of the Crimea
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Geographical areas
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Average temperatures, °ó
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Number of the days without frost
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Number of precipitation, mm/per annum
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In June
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In January
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Flat plain Crimea
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Prysivashye
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+22.5 +23.5
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-1.0 -2.3
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190-205
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340-450
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Tarkhankut plain
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+22.5 +23.0
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-0.3 -2.0
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190-225
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340-400
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Central Crimean Plain
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+22.0 +23.0
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-1.5 -2.2
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170-185
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425-480
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Kerch Peninsula
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+23.0 +23.5
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0 -1.3
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200-225
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350-420
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Mountainous Crimea
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Foothill
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+22.0 +22.3
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-1.5 +2.0
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150-240
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350-600
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Main mountain range
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+15.0 +21.0
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-4.0 0
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150-180
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600-1200
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Southern Coast
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+23.0 +24.5
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+2.0 +4.0
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230-260
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350-650
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In the foothill area (Simferopol, Belogorsk)
the amount of precipitation increases up to 500-600 mm / a year,
summer temperatures decrease.
In mountains we can observe the decrease of summer
and winter temperatures, the amount of precipitation is increased.
Every 100 m high the temperature goes down on average by 0.5-0.6°ó,
the amount of precipitation grows by 50-70 mm /a year. Therefore,
on yailas (Crimean mountain pastures) average monthly winter temperatures
comprise up to -4 ... -5 °ó, and amount of precipitation - 1000-1500
mm /a year.
As far as the climate concerns, the Southern
Coast of the Crimea is the most interesting. This is the only place
in Ukraine with a sub-Mediterranean, in other words - almost Mediterranean
climate. Winter is soft, with positive temperatures there.
Comparison of climatic characteristics
of Yalta and resorts on the Mediterranean coast
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The name of the resort
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Temperature in
January º ó
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Temperature in July º ó
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Temperature of water in July º ó
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The relative humidity in July, %
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Quantity of days with precipitation in
July
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Yalta
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4.0
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23.7
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23.1
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61
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5.2
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Nice (France)
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7.0
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23.0
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21.3
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54
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3.0
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Marseilles (France)
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6.1
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22.2
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21.3
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54
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3.0
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Athenes (Greece))
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8.3
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26.7
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24.4
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48
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3.0
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Limassol (Cyprus)
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11.7
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25.6
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25.9
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60
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0
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Haifa (Israel)
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13.9
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27.8
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26.9
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71
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0
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Valencia (Spain)
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10.0
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24.0
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24.0
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62
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2.0
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Antalya (Turkey))
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9.9
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28.1
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25.8
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62
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0
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The
climate of Yalta is cooler in comparison with the resorts located
on the Mediterranean Sea. Especially it is true for winter. There
are sometimes frosts up to-15 °ó in Yalta. Such low temperatures
prevent subtropical cultures from growing.
In Crimea there are some hundreds versions of
local climates.
The climate in valley of the Salgir River differs
from the climate of cuesta ridges by higher daytime temperature
and lower temperature at night. The valley winds frequently blow
there bringing cool air from mountains.
The specific climate is formed in the Baydarskaya
Valley. This part of the valley of the Chernaya River (the Black
River) is hollow; therefore, in a windless weather cold air flowing
down from the slopes of nearby mountains is accumulated in it. As
a result, the absolute minimum of temperature is lower in the valley
in comparison with adjoining areas.
Local climates are formed also due to foens,
breezes, and hill-valley winds. The influence of breezes is especially
bright in the Crimea. They appear in summer and are caused by uneven
heating of the land and the sea: in the afternoon the wind blows
from the sea to the land, and at night - on the contrary. Breezes
can be considered as analogues of Asian monsoons, except the continent
(Asia) and the ocean (the Pacific) interact there, and the change
of a wind direction occurs in summer and in winter. Due to breezes,
summer midday and afternoon heat is softened at the coast.
Location of the Crimea within the limits of the
sea variant of East Mediterranean climate makes its climatic conditions
really comfortable. Even in Simferopol located not at the coast,
but in the central part of the peninsula, the climate is much more
comfortable for the person in comparison with the same latitudes
(45º) of the Eastern hemisphere (with colder winter and
contrast climate in seasons) and Western hemisphere (where summer
is rather cool).
Some "climate records"
of the Crimean peninsula for the last 150-200 years:
- The highest temperature in summer - the absolute
maximum (+40.7°ó) - was registered in August 1930 in the settlement
of Klepinino.
- The lowest temperature in winter - an absolute
minimum (-36,8°ó) - was registered in January 1940 in the
settlement of Nizhnegorsky.
- Winter of 1953-1954 was the coldest and the
snowiest when almost for 50 days the temperature was below-10°ó.
- Winter of 1965-1966 was the warmest, when
there was no snow on the Crimean yailas, and the thawing weather
proceeded in Simferopol almost for three months.
- The maximum of precipitation - 1718 mm - was
registered in 1981 on the mount of Ai Petri.
- The longest drought was in 1947 when even
in mountains there were no rains almost for 100 days.
- The maximum quantity of foggy days (not only
in the Crimea, but also in Ukraine) was observed on Ai Petri (in
1970 - 215 days).
- The windiest point not only in the Crimea,
but also in Ukraine is Ai Petri (in 1949 the wind velocity was
more than 15 m/sec for 125 days). The highest speed of the wind
- 50 m/sec - was also registered on Ai Petri.
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