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Climatic Geography

Introduction to climatic geography:

The study of climatic geography is a branch of physical geography, concerned with the study of the atmosphere and through the study of climate and climate (solar radiation, heat, atmospheric pressure, wind, evaporation, weather and manifestations of condensation), the study of climate on a large scale.

The difference between climate and weather:

A short period of time In a short period of time.

Climate (climate): It expresses the averages of the climatic elements in that external geographical area. The export of the climate of the State of Palestine is moderate, hot and dry in summer and moderately rainy in winter, Malaysia's climate is hot and rainy throughout the year.

Climate elements:

First, solar radiation

Browse exposure A large part of which exhibits contact and dispersion, this simple part that reaches the ground floor and the surface of the ground provides it with about 99.97% of the total thermal energy.

Second; the atmospheric temperature

Atmosphere differs from one atmosphere to another, the atmosphere from one atmosphere to another aircraft, and this one from the atmosphere through several ways:

1. direct solar radiation.
2. Geothermal radiation.

Third: atmospheric pressure

Its height equals 76 cm height 76 cm height equals 76 cm, alto measured on iron poles, or metal barometer.

Fourth: Wind and its types

Winds move from areas of high atmospheric pressure to the northern hemisphere and to the left of the southern hemisphere (Corolios) due to the rotation of the earth around itself, determining the direction of the winds blowing from them, for example if the winds blow from the so-called westerly and so on, types of winds:

1. Permanent wind: blowing constantly and regularly.
2. Seasonal: It blows in specific seasons according to the variation in temperature and atmospheric pressure between the land.
3. Local area: local wind.
4. Daily: It occurs throughout the day in an orderly fashion through variations in temperature and atmospheric pressure.

Fifthly: Doubt varies according to its standards to:

1. Absolute circumference: A certain amount of water vapor weight in the Pacific Ocean's surface and vegetation temperature
2. In engineering drawing, pictures taken in engineering drawing The temperature rises. 65% cause overheating.

Sixth: evaporation

1. The process of turning water into a gaseous state, always occurs in nature, when the water on the surface of the earth and the wet bodies on it are exposed to any temperature, evaporation can occur from frozen water to the gaseous state directly without going through the liquid state. This is what is known as (sublimation ).
2. Depends on the home page in the heat, which helps in speed of the previous graph, which helps in increasing the speed of the home page in the previous graph.

Seven: condensation

• Water turns into liquid, liquid, liquid, liquid if exposed to this liquid in case of exposure to liquid, liquid, liquid, liquid liquid, liquid liquid, liquid liquid, liquid liquid, liquid liquid, liquid liquid, liquid liquid in the normal direction. It condenses in many forms.

Eighth: Precipitation

• The vapor condenses, falling in the form of rain, snow or hail.
• Precipitation is classified according to its composition into:

1. terrain rain.
2. Academy study rains.
3. Precipitation escalation (gestational age).

• The amount of precipitation according to the amount of its fall to:

1. Heavy rain: more than 1500 mm/week.
2. Average rain: between 500 and 1500 mm / week.
3. Rain is rare: less than 500 mm/week.