Spring
provides a smooth transition between winter and summer seasons, and
plenty yağmurlarıyla noticeable, especially in areas close to the coast
during these months has seen intense team-planting activities (Table-2).
Spring season starts from March to show up, get into the months of
April and May. This season, the average monthly temperatures of 15 ° C
is on. Covers a period of approximately three months of the fall season
is summer, but part of September, November, also features the relatively
winter.
Actual pressure in the?
Values for the annual running of Trabzon is looking to be the total
value of 1011.1 MB. Pressure is lower than the other months during the
summer months, whereas the annual average during the winter months is
very little on.
frequencies of
wind direction in our province, area of contact centers, movement of
the pressure, in the shape of features and is under the influence of the
Black Sea. Winds blowing from the north and south by land and sea
breeze winds dominance feels way. Close to the sea areas south and
southwest winds are more effective. Winds blow-dry February, March and
April, are seen and may find an annual average of twelve days.
The
amount of annual rainfall in the province of Trabzon in the course of
the year, rainfall conditions in the area due to the formation of the
Black Sea side, rising immediately from the shore of the Black Sea with a
slope rising from the land surface temperature-dependent relationship
between the main effective factor. To varying conditions of rainfall
over short distances (microclimate areas) is an important feature of our
region. Therefore, the need in our province and throughout the coastal
and inland differences between the shows.
Rates
are high relative humidity in summer, especially in the area and
observed limit to expanding inland. This season the Black Sea north of
the evaporation, when the air is calm and keep close to the shore
segments under the influence of the low pressure center over time,
moving towards the southern areas of high winds, thanks to Mary, moved
here because of the moisture directly from the highland areas, which
often continues until noon on a clear open- valleys throughout the state
of the weather, then rising water vapor, completely covering the pitch,
and sometimes for days çekilmemektedir.
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