Knowledge of geography in senior one: climate in major regions of the world

1, east coast: monsoon climate is remarkable; (* Same monsoon climate, temperate monsoon climate);

2. Western inland: temperate continental arid and semi-arid climate;

Second, Southeast Asia:

1, tropical monsoon climate; (Distributed in Indo-China Peninsula and most parts of Philippine Islands, with high temperature and rainy summer in the north);

2. Tropical rain forest climate; (distributed in Malay Peninsula and Malay Archipelago, with high temperature and rainy all year round);

Third, South Asia:

1, dominated by tropical monsoon climate; (most parts of the Indian Peninsula);

2. Tropical desert climate; (Middle and lower reaches of India; Pakistan is dominated by tropical deserts);

Fourth, Central Asia:

1, temperate continental arid and semi-arid climate;

Verb (abbreviation for verb) West Asia and North Africa:

1, tropical desert climate is dominant; (more than 7.7 million square kilometers);

2. A small part is Mediterranean climate;

The intransitive verb sub-Saharan Africa:

1, savanna climate (the first in the world);

2. Tropical rain forest climate;

3. Tropical desert climate;

4. Mediterranean climate;

Seven, Europe:

1, temperate maritime climate is dominant (west) → the most typical in the world;

Note: Reasons: ① West wind all the year round; (2) Humidification and warming of the North Atlantic warm current; ③ Topographic factors; (4) Continent contour fracture is beneficial to the depth of west wind;

2. North and South: Mountain climate;

3. Spain, Portugal and so on. : Mediterranean climate;

4. Mid-temperate continental climate;

VIII. Eastern Europe and North Asia:

1, temperate continental climate (Russia);

Nine, North America:

1, dominated by temperate continental climate;

2. Narrow temperate maritime climate (40 N-60 N);

3. Narrow Mediterranean climate; (30n-40n)；

X. Latin America:

1, tropical climate, rainforest grassland climate;

XI。 Oceania:

1, tropical, semicircular: great watershed (tropical rain forest, monsoon humid climate);

Note: The causes of tropical rain forest climate:

① The warm current in eastern Australia raises the temperature and pressure;

② Southeast wind comes from warm current;

(3) Topographic factors: located on the windward slope of the great watershed;

2. Tropical grassland climate (controlled by equatorial depression);

3. Tropical desert climate (crossing the Tropic of Capricorn; Western Australia cold wave);

4. Mediterranean climate on the west coast of the mainland (30-40);

Twelve. Antarctica:

1, cold:

① High latitude and low heat;

(2) The altitude is high, and the cooling range is large;

③ Glaciers reflect the sun very strongly;

2, drying:

① High latitude, low temperature and small evaporation;

② Controlled by polar high all the year round, it flows downwards;

③ Large land area;

3. Gale: average 18m/s, reaching 100m/s, with gale days of magnitude 8 or above lasting more than 300 days in a year;

Thirteen. Arctic:

1, no Antarctic cold (large ocean area, most of which are frozen all year round);

2. The precipitation is richer than that in Antarctica (the temperature is higher and the ocean area is larger), and the annual precipitation is100 mm-150 mm;

3. The wind speed is not as big as that of South Pole.