A high school geography question about climate is controversial.

This thing has to be analyzed specifically, and I also support the idea that it belongs to the temperate oceanic climate, for the following reasons:

Looking at the air temperature, first of all, it can be judged that it belongs to the climate of the Northern Hemisphere, and it should be temperate, so d can be ruled out

In addition, looking at the rainfall, it is definitely an annual rain type and a large rainfall, and the precipitation is evenly distributed throughout the year, while the Mediterranean climate and the temperate continental climate have obvious seasonal changes, and the precipitation The Mediterranean climate cannot exceed 1500, let alone the temperate continental climate, so ab is excluded

As for what you said about the temperature below 0 degrees in January and February, this is normal, first of all, according to the definition, a temperate oceanic climate is a multi-year average temperature above 0 degrees, not specifically every year Secondly, there are slight differences between regions, for example, there must be a difference in the average temperature in January between the temperate oceanic climate in southern and northern Europe, and this place may belong to the northerly region, so this may be the case.

Finally, the weather is unusual, for example, this year in Europe's temperate oceanic climate zone must have been a few degrees below zero.

Give a reward if it's good! Hehe.

It stands to reason that b,c is excluded if the temperature of the coldest month is less than 0 degrees Celsius, but if it is in the middle of a mountainous area, the temperature is likely to be lower than in other regions, such as the plains. Because the concept of a temperate oceanic climate applies to plains. Just C.

There is more precipitation in the local area, the precipitation is uniform, and the precipitation is large, and AB is excluded. Exclude d from the temperature distribution. Therefore, the climate of a place is not static, affected by a variety of factors, and varies from year to year, so it is not excluded that the temperate oceanic climate has low temperatures.

1. The North American continent is larger than Australia.

2. Mexico plays with the warm current more powerful than the East Australian warm current.

3. The Appalachian Mountains are relatively low and gentle, which has little effect on blocking the warm and humid air flow of the ocean.

First of all, its land area is larger than that of Australia, the monsoon force is relatively strong, and the thermal difference between sea and land is large. Topography also plays a role, with Australia's Great Dividing Range being perpendicular to the wind, preventing water vapour from penetrating deep into the interior of the continent. The topographic characteristics of North America are high on the east and west sides and low in the middle, which is conducive to the deep penetration of moist water vapor into the interior of the continent. Ocean currents affect North America by the Gulf Stream, which flows from south to north, which is conducive to water vapor penetrating the interior of the continent.

Australia is affected by the East Australian Current, which flows from north to south, which is not conducive to the deep penetration of water vapor into the interior of the continent.

1.Because the Gulf Coast of the United States is the Mississippi Plain, which is flat, while the eastern part of Australia is the higher Great Dividing Range, blocking the deep penetration of warm and humid air currents over the ocean.

2.The U.S. Gulf Stream is the strongest in the world, so it warms and humidifies more than the East Australian Current.

1. You should be talking about the climate of India. Because it seems that the tropical monsoon climate in India is caused by the difference in heat on land and sea and the seasonal movement of the pressure belt and wind belt. The summer monsoon in India is a southwesterly wind formed by the geostrophic deflection force of the northern hemisphere after the trade wind belt of the southern hemisphere crosses the equator.

It may be that India is at a lower latitude. The monsoon climate in China, the United States, Brazil, Australia, etc., has nothing to do with the seasonal movement of the pressure belt and wind belt.

2. The trade winds are about 30 degrees north and south latitudes, and you just need to remember the areas with monsoon climates in this region (north and south of China, southeast Brazil, etc., there are in the book), these places are naturally monsoons, and other regions are not.

1. The blowing direction of the wind is mainly affected by high and low pressure, and the rotation direction of air pressure is related to the geostrophic deflection force, the clockwise direction of the south and north (cyclone-low pressure), and the south-north reverse (anticyclone-high pressure), you can look at your air pressure rotation chart according to what I said, and then remember a few high-pressure and low-pressure cyclones, let me give you an example, such as Mongolian high pressure, Pacific low pressure, Mongolian high pressure location find, remember the direction of rotation, the flow of air pressure is high pressure to low pressure flow, so it is blown from land to the ocean, The opposite is true, when the northern hemisphere (Asia) winter, the land is (Mongolian) high pressure, the ocean is (Pacific) low pressure, the direction of rotation, it is the northwest wind blowing by Mongolia or Siberia, this can also be seen from the map, you can take a closer look, you first summarize what I told you, if you can understand, I will explain to you other about air pressure.

2. The trade winds are perennial winds, and there are several trade winds on the earth. The monsoon is a wind that blows according to the influence of air pressure, season, temperature, latitude, etc., and changes with the seasons, and it is not a wind that blows in the same direction throughout the year.

The specific heat capacity of water is larger than that of land, so the temperature of land rises faster than that of the ocean in summer, the temperature of the ocean is lower than that of land, and the air pressure is higher than that of land, and the wind blows from the ocean to the land, forming the summer monsoon. Because the land has a smaller specific heat capacity, heat is lost faster than the ocean. In autumn and winter, the temperature on land is lower than that of the ocean, the air pressure is higher than that of the ocean, and the wind blows from the land to the ocean, forming the winter wind.

Heat capacity is the ability of an object to absorb and store heat. The difference in heat between land and sea is the main cause of the monsoon climate. For example:

China faces the world's largest ocean, the Pacific Ocean, and is backed by the world's largest continent, the Eurasian continent, which causes a strong difference in sea and land heat, so China's climate has obvious monsoon characteristics. Effect of land and sea distribution on atmospheric circulation Effect of land and sea distribution on atmospheric circulation: Differences in thermal properties between land and sea lead to the fracture of the pressure zone in the Northern Hemisphere and the distribution of blocks. The subpolar pressure zone is cut off by the Mongolian-Siberian high, leaving the subpolar depression only over the ocean, forming the Icelandic low in the North Atlantic and the Aleutian low in the North Pacific.

Therefore, the difference between land and sea heat and the pressure and wind bands are interrelated.

The second question trade wind (trade wind) in the low atmosphere on both sides of the equator, the northern hemisphere blows northeast wind, the southern hemisphere blows southeast wind, the direction of this wind rarely changes, they are like this year after year, stable appearance, very credit, this is the reason why trade wind is translated as "trade wind" in Chinese.

The monsoon is a wind system that prevails over a large area due to the temperature difference between the continent and the adjacent oceans, and the wind direction changes significantly with the seasons.

The monsoon is a large-scale convection phenomenon caused by factors such as land and sea distribution, atmospheric circulation, and continental topography, with a one-year cycle. Asia is the most famous monsoon region in the world, and its monsoon is characterized by the existence of two main monsoon circulations, namely the northeast monsoon in winter and the southwest monsoon in summer. Generally speaking, November to March of the following year is the winter monsoon period, June and September are the summer monsoon period, and April May and October are the transition period between summer and winter monsoon.

However, the seasons vary from region to region, so the division of the monsoon is not exactly the same.

The monsoon is a large-scale wind system with significant seasonal changes in wind direction, and is a planetary-scale circulation system like the wind belt, which is caused by the difference between ocean and land temperatures in winter and summer. The monsoon blows from the ocean to the continent in the summer and from the continent to the ocean in the winter. Agree.

It is recommended that you understand and memorize the 13 types of climate with air pressure and wind zones.

1. Southern South African Plateau (20°S to 30°S).

In January, the southern hemisphere is summer, and a wide range of thermal depressions form in the interior of the continent, and the warm and humid southeast trade winds over the warm current blow to the mainland, bringing more precipitation to the South African plateau, forming a wet season.

In July, the southern hemisphere is winter, and the average altitude of the South African highlands is more than 1,000 meters, due to the high terrain and lower temperatures, a high pressure forms in the southern part of the continent and connects with the maritime high in the east of Nafeng. Due to the control of the subtropical high pressure zone, downdrafts prevail. Coupled with the presence of high pressure on land, the influence of trade winds from the ocean is reduced, resulting in a dry season.

This results in a savannah climate on the eastern coast of the continent near the Tropic of Capricorn in Africa.

2, East African Plateau.

In summer, the two places are controlled by the warm and humid southwest monsoon that passes over the warm current and is uplifted by the terrain, respectively. And due to the convergence of the southwest monsoon and the northeast trade winds, there is more convective rain and abundant precipitation, forming a wet season. In winter, the order is accepted.

1. The northeast trade winds of the dry eggplant source are controlled to form a dry season.

In the northern hemisphere summer (July), the southeast trade winds in the southern hemisphere deflect northward across the equator to the right, forming the southwest monsoon. During the Southern Hemisphere summer (January), the northeast trade winds in the Northern Hemisphere deflect south across the equator to the left, forming the northwest monsoon. )

Can you give points?