Tropical climate

A lot of annual rainfall, which places more than 10,000 mm, depending on season, location and the year is small, but large variations depending.

Meanwhile, the annual range of temperature is within the 6 ℃, and the daily range of temperatures is Large as 5 ~ 15 ℃.

Just below the equator, the Amazon basin of South America, Ecuador, Colombia, Jersey giniman coast of Africa, Southeast Asia, islands in the trade winds of the island and the ocean can have this climate, and range of the climate is from around the world and occupies a large area of ​​1400 ㎢ .
There are many natural benefits which are the sun light, heat, water, many valuable species of plants maneuna, but social economic status is not good for the development, yet.

Temperate zone

Temperature zone is between the tropics and Frigid Zones, and its latitude is between  23.5 ° and 66.5 °. It is mid-latitude zone.The climate is warm and the distinction is evident in both summer and winter.

In eastern Asia, The southern has evergreen oak forests, and the northern has deciduous forests.

1. Temperate arid climate

Belonging to the arid regions of temperate climate.
Because there is less rainfall, it is in the desert or grassland. Inland China and Central Asia belong to such a climate.

2. Temperate monsoon climate

3. Temperate climate

4. Warm with dry winter climate

5. Temperate humid climate

Dry climate

Trees can not grow due to lack of moisture of climate. Wet or dry of climate is  determined by difference between the amount of rainfall and the possibility of evaporation.

Prolonged lack of moisture in the forest land to grow well because it makes plain or a desert, dry, desert climate and grasslands, depending on the severity of the climate can be divided into:

In the arid region occupies about 30% of the total area, mainly under the control of mid-latitude high-pressure units in the distribution of the regression line close to the inside of a Central Asia and the North American continent north latitude 50. To have spread.

Typically, the summer temperature variability and the annual range of large and high daytime temperatures. Many irregular shape of the convective rainfall horyuga, and changes in precipitation are much larger than the wet climate.

The amount of rainfall is high in The low latitudes in the summer, and it is high in high latitudes in winter.