I summarize the characteristics of high school geography July, and the range is willing.

In July, ah...The continent is hotter than the ocean, the continent has low pressure, and the ocean is high pressure.

The direct point of the sun is in the northern hemisphere, where the days are longer and the nights are shorter, and the southern hemisphere is the opposite.

The wind belt pressure zone moves northward with the direct point, at this time the southwest wind blows in South Asia, and the east Asia is from the sea to the land, and the southeast wind is [China.

Because of the drought, there will be fewer rivers in the south than in the previous month.

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July is too much, such as the northern hemisphere enters summer, the southeast coast of China blows southeast winds, the direct sun is in the northern hemisphere, the middle and lower reaches of the Yangtze River have droughts, the subtropical high moves northward, the Mediterranean climate zone, such as Western Europe, dry and rainy.

For example, in the Northern Hemisphere, July is summer, the sun shines directly on the Northern Hemisphere, the days are long and the nights are short, and low pressure forms on the land.

In July, the frontal rain belt moved to North China, and the middle and lower reaches of the Yangtze River were drought.

The eastern part of China was affected by the southeast monsoon in July, and the southwest was affected by the southeast and southwest monsoons.

In fact, in July, China's land is in a state of low pressure, and the rainy season is continuous, because the direct sun is in the northern hemisphere around June 22, resulting in the so-called thermal problem; The drought is that the Yangtze River area in China is affected by the high-pressure air flow of the Pacific Ocean, resulting in the inability to form precipitation.

July in the Northern Hemisphere is summer. July is winter in the Southern Hemisphere. In July, the Earth is located at aphelion and rotates slowly.

In the middle and lower reaches of the Yangtze River in China, the rainy weather (quasi-stationary front) is from June to July, and the drought (subtropical high control) is from July to August. The southeast monsoon blows in July, and the wind blows from the ocean to the land, and there is a lot of precipitation. I can't remember.

There is no such thing as non-zonal climate. It can only be said that the climatic causes of a certain place are non-zonal.

Typical have specialization:

1. The temperate continental climate of the Patagonian plateau was supposed to be a temperate oceanic climate.

2. The tropical desert climate off the coast of Somalia was supposed to be a tropical rainforest climate.

3. The savannah climate of the East African Plateau and the Guyana Plateau should have been a tropical rainforest climate.

4. The tropical rainforest climate on the eastern coast of Madagascar, the southeastern coast of Mexico, the southeastern coast of Brazil, and the northeastern coast of Australia should have been a savannah climate.

5. The tropical desert climate of the Thar Desert was supposed to be a tropical monsoon climate.

That's all there is to it, and nothing else is typical.

For example, the effects of ocean currents – such as the tropical deserts off the coast of Peru, the rainforests of northeastern Australia.

Topography – such as the formation of a temperate continental climate on the Patagonian plateau in southern South America.

Water sources – such as Xinjiang oases, etc.

1. East African plateau-savannah climate on the east side of the African equator (high terrain);

2. The coast of the Gulf of Guinea in Africa - the tropical rainforest climate extends to the north (under the influence of the warm current of the Gulf of Guinea, the coastline is perpendicular to the southwest monsoon);

3. The eastern part of Madagascar - tropical rainforest climate (windward slope of the southeast trade wind mountains, the influence of the Madagascar warm current);

4. West coast of North America - temperate oceanic climate confined to the coast (Andean influence);

5. East coast of Central America - tropical rainforest climate (the windward slope of the Northeast Trade Wind Mountains and the warm current of the Gulf of Mexico);

6. West coast of South America - tropical desert climate is long and narrow from north to south (Andean Mountains, Peruvian cold current);

7. Both sides of the equator in western South America - alpine climate (influence of the Andes);

8. East Brazil, South America - tropical rainforest climate (southeast trade windward slope, Brazil warm current influence);

9. The northern part of the east coast of Australia - tropical rainforest climate (the windward slope of the southeast trade wind mountains, the influence of the warm current of East Australia);

10. Thar Desert, India (tropical desert climate: difficult to reach by southwest monsoon).

Mediterranean climate zone? It depends on what you mean by "special climate characteristics".