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.

subtropical climate

Subtropical climate is not in Koepenui Mediterranean climate category, but generally after genital and dry climate (Step climate and desert climate), the fall. Mediterranean penis is then in the summer, subtropical high-pressure units, and under the influence of the high-temperature drying in the winter is the rainy season is attached to the case pyeonseopung. In addition to the Mediterranean region of North America, California (latitude 34 ~ 43 °) and the coast of South America, Chile (latitude 31 ~ 37 °), southern Africa and is distributed in Australia.

polar climate

Trees at high latitudes in the cold can not saengyukhal a local climate.

Of the year covered in ice or snow and ice climate, moss tundra plants and lichens that can be growed divided into climate.

Also based on a fat dong of permanent to permanent climate of the region is also known as freezing weather.

Average temperature of 10 ℃ of coldist month in the northern hemisphere, isothermal, so the tree limit and almost identical to this one kwaepeneun WP climate (E climate) and the cold climate was the boundary.

In the Antarctic in the southern hemisphere called the extreme weather that can be viewed as the low-temperature climates on earth, and in Antarctica, -88.3 ℃ was observed on the world's lowest.

Characterized by a long winter, and plant growth in the three months period yinaeda tundra.

Most of the eyes, a very small amount of precipitation. Euroseoneun erosive force of the ice is excellent work and the mechanical weathering.

subpolar zone

Boreal climate, as classified by temperature or cold case is referred to as. Between a temperate and relatively high temperatures, and short summers and long winters are characterized by a severe cold. To the north of latitude 40 ° south of the Arctic tundra appears the northern region of Eurasia, North America is that. Except Antarctica and in the cooler areas of the rivers freeze and snow cover period, amounting to a few months time. However, a very short summer growing period is short crop cultivation. Due to the annual range of temperature, seasonal changes are distinct landscapes.
 May-June if the snow melts and the different kinds of flowers start to bloom, September and October, awning nakyeopsuna vegetation. In most areas of coniferous trees in a primeval forest called taiga in Siberia. Trees, crop growing period (average temperature 10 ℃ or higher) are distributed in less than four months. Some of the forest, such as foxes, martens, squirrels are many number of fur. Jujong constitute two of the hunting industry, forestry and agriculture is practiced.

1. cold with dry winter climate

2. humid continental climate

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.

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.