 |
||||||
| หน้าแรก | โรงเรียนสายน้ำผึ้ง
ในพระอุปถัมภ์ |
|||||
กลุ่มสาระสังคมศึกษา ศาสนาและวัฒนธรรม |
||||||
| สารบัญ | ||||||
climate |
||||||
| Köppen Climate Classification
System The Köppen Climate Classification System is the most widely used for classifying the world's climates. Most classification systems used today are based on the one introduced in 1900 by the Russian-German climatologist Wladimir Köppen divided the Earth's surface into climatic regions that generally coincided with world patterns of vegetation and soils. The Köppen system recognizes five major climate types based on the annual and monthly averages of temperature and precipitation. Each type is designated by a capital letter. |
|
A |
- Moist Tropical Climates are known for their high temperatures year round and for their large amount of year round rain. |
B |
- Dry Climates are characterized by little rain and a huge daily temperature range. Two subgroups, S - semiarid or steppe, and W - arid or desert, are used with the B climates. |
C |
- In Humid Middle Latitude Climates land/water differences play a large part. These climates have warm,dry summers and cool, wet winters. |
D |
- Continental Climates can be found in the interior regions of large land masses. Total precipitation is not very high and seasonal temperatures vary widely. |
E |
- Cold Climates describe this climate type perfectly.
These climates are part of areas where permanent ice and tundra are always
present. Only about four months of the year have above freezing temperatures. Further subgroups are designated by a second, lower case letter which distinguish specific seasonal characteristics of temperature and precipitation |
f |
- Moist with adequate precipitation in all months and no dry season. This letter usually accompanies the A, C, and D climates. |
m |
- Rainforest climate in spite of short, dry season in monsoon type cycle. This letter only applies to A climates. |
s
|
- There is a dry season in the
summer of the respective hemisphere (high-sun season). |
w |
- There is a dry season in the winter of the respective hemisphere (low-sun season). |
| To further denote variations in climate, a third letter was added to the code. | |
a |
- Hot summers where the warmest month is over 22°C (72°F). These can be found in C and D climates. |
b |
- Warm summer with the warmest month below 22°C (72°F). These can also be found in C and D climates. |
c |
- Cool, short summers with less than four months over 10°C (50°F) in the C and D climates. |
d
|
- Very cold winters with the coldest month below -38°C (-36°F) in the D climate only. |
h |
- Dry-hot with a mean annual temperature over 18°C (64°F) in B climates only. |
k |
- Dry-cold with a mean annual temperature under 18°C (64°F) in B climates only. |
Köppen Climate Classification
System |
Tropical Moist Climates : A |
A : tropical climate |
| Dry Climates : B ภูมิอากาศแห้งแล้ง |
B : dry climate |
| Moist subtropical mid-lattitude climate : C ภูมิอากาศอบอุ่นชื้นแถบละติจูดกลาง |
C : warm climate |
| Humid continental climates : D ภูมิอากาศชื้นภาคพื้นทวีป |
D : snow climate |
| Polar Climates : E ภูมิอากาศขั้วโลก |
E : ice climate |
| Highland Climates : H ภูมิอากาศแถบภูเขาสูง |
H : mountain climate |
Copyright By : Chalengsak Chuaorrawan Sainampeung School 186 Sukhumwit 22 Sukhumwit RD Klongtoeay Klongtoeay Thailand e-mail address : chalengsak.ch@gmail.com Tel; 089-200-7752 mobile |
|