Factors of Climate

Climate is defined by several factors, which are called climate controllers. Such as:

*Latitude: According to latitude, the declination of the declination of the ascendant varies, falls somewhat constrictedly, or isolated somewhere. Therefore, heat and humidity vary from place to place. As the sunlight rises in places along the equator, the warmth is higher in those regions. In the northern and southern latitudes, the temperature decreased gradually from the illumination line. In the extreme north and south pole regions of the equator, there is ice in the equatorial distance because the temperature of 1 ° latitude decreases to 1 °.

*Height: Height increases the temperature in the height. The temperature decreases by 6 ° C to 1000 m. Even the height of the height of the two areas of the two latitudes at the same latitudes are very different.

*Distance from the Sea: The degree of humidity of the air depends on how far away from the ocean, and climate warming depends largely on the humidity. Mild warmth prevents moisture in the summer and the warm warmth of the winter in the ocean near the sea. These climate is called equally complex climate.

*Wind Direction: Rainfall in the region where the water flows through the ocean flowing through the ocean, is more than the rainfall. But the dry air flowing from the ground again increases the warmth.

*Rainfall: If there is rainfall in some places then there is less heat in the rain-fed regions. So the climate is warm in the desert area. Moreover, the humidity levels depend on rainfall levels, which control the climate.

*Lawn / Forests: Water vapor condenses through precipitation of plants and evaporates. Due to the deepening of the forest, sunlight does not fall on the ground in some places, so these areas are cold. Moreover, the environment affects the atmospheric conditions by obstructing the winds, cyclones and tornadoes.

*Land Slope: If the sun rays fall along the top of the shield, then the temperature increases with heat becoming hot and the temperature does not rise much when the opposite of the slope starts to rise. Moreover, the collapse of the Surlok, along the slope, makes comparatively warm weather comparable to the fall of the sunlight.

*Soil Specialty: The specialty of the Belima is that it gets as cold as the hot, the faster it cools. Slightly sedimentary sediments are not too hot, and the heating is too late to cool. Therefore, there may be differences in climate and climate on the specificity of soil in any place.