Describing the climate generally pays attention only to temperature and precipitation???

Climate is the general state of the atmosphere in a certain area of the earth for many years, and it is the comprehensive expression of various weather processes in that period. Various statistics (mean, extreme, probability, etc.) of meteorological elements (temperature, precipitation, wind, etc.) are the basic basis for expressing climate.

When judging and describing the climate, it is generally based on the annual distribution of temperature and precipitation (e.g., whether the precipitation is summer rain, winter rain, year-round rain, etc.).

That's enough, unless something is more difficult, such as a highland climate, where you need to know the altitude.

Three climatic elements: temperature, precipitation, and prevailing wind direction.

Temperature, precipitation, air pressure, prevailing wind direction, the description of the college entrance examination requires only the first two, unless it has requirements, generally do not give too much consideration.

Describing the climate generally focuses on temperature and precipitation, in addition to vegetation (species of flora and fauna, characteristics, etc.).

As for others, such as air pressure, wind direction, etc., they vary greatly and are uncertain, especially with little correlation with the seasons, especially wind.

Therefore, the description of climate is generally dominated by temperature and precipitation, followed by vegetation.

Describing the climate generally pays attention only to temperature and precipitation???

- Because temperature and precipitation are the two dominant factors of climate! ~

Yes, other factors such as topography, underlying surface, etc. affect temperature and precipitation, so the climate of a place is determined by temperature and precipitation.

Yes, and barometric pressure and so on.

1. The factors that affect the temperature include latitude factors, topographic factors, and ocean currents.

factors, vegetation coverage, etc.

1) The higher the latitude, the lower the temperature, and the lower the latitude, the higher the temperature;

2) The higher the altitude, the lower the temperature, and the lower the altitude, the higher the temperature;

3) The warm current will increase the temperature of the area through which the orange is passed, and the cold current will reduce the temperature of the area through which it passes.

4) The higher the vegetation coverage, the smaller the diurnal and annual temperature ranges, and the lower the vegetation coverage, the greater the diurnal and annual temperature ranges.

2. The factors affecting precipitation include latitude factors, land and sea factors, ocean current factors, topographic factors, and atmospheric circulation.

factors, etc. 1) The lower the latitude, the more precipitation, and vice versa. For example, there is more precipitation at the equator and less precipitation at the poles;

2) the precipitation in the plains and lowlands near the sea is more than that in the plateaus and mountains in the inland (more precipitation in the coastal areas and less precipitation in the inland);

3) There was more precipitation in the Diwumu area through which the warm current passed, and less precipitation in the area where the cold current passed.

4) There is more precipitation on the windward slope and less precipitation on the leeward slope;

5) There is more precipitation in areas where the front passes, and less or even no precipitation in areas controlled by a single air mass.

Temperature characteristics: cold or hot.

Precipitation characteristics: humid and rainy or dry and rainy.

From high and low temperatures to fluctuating temperatures (when it is the hottest, coldest, or even warmer), the amount of precipitation and which month has the most precipitation and the least precipitation. And which climate is in line with. For example, the Mediterranean climate is then described.

Taking Shanghai as an example, the four seasons are distinct, the minimum temperature of the year is above freezing, and the precipitation is abundant, mostly concentrated in summer.

The specific heat of water is very large, and in the three-state cycle of water, a large amount of heat will be released or absorbed. The most direct precipitation is to drop the condensed water droplets of cold water at high altitude on the ground, so that the surface temperature will be lowered, and indirectly, it will also drop with the cold air flow required for precipitation and the evaporation of rainwater on the ground.

The factors of precipitation, sufficient water vapor, as well as the temperature difference and pressure difference caused by the convergence of cold and warm air currents, will accelerate the process of water vapor condensation. Then, it's the complex underlying surface that influences. It is best not to have too much updraft in the lower airflow, which hinders the convergence of warm and humid airflow and cold airflow at high altitude.

Without condensation after cold air, water vapor from high altitude does not fall to the ground. The lower layer is also not enough to cool down, and the water vapor cannot be dissipated, which will increase the surface humidity, and the water vapor may appear in the form of fog.

1.Tropical rainforest climate: hot and rainy all year round; 2.Savannah climate: dry and rainy seasons are distinct, and high temperatures are high throughout the year.

3.Tropical desert climate: hot and dry all year round; 4.

High temperature and rain in summer, low temperature and little rain in winter; 6.Mediterranean climate: high temperature and little rain in summer, low temperature and rainy winter 7

Temperate monsoon climate: hot and rainy in summer, cold and dry in winter; 7.Temperate oceanic climate:

Mild and humid all year round; 8.Temperate continental climate: (including temperate steppe climate and temperate desert climate) with high temperature and rain in summer, cold and dry in winter; 9.

Subarctic coniferous forest climate: mild and humid in summer, cold and dry in winter; 10.Tundra climate:

Summers are mild and humid, while winters are cold and dry; 11.Icy climate: cold and dry all year round; 12.

Alpine and plateau climate: depending on the latitude and longitude location, the position of the sea and land, etc.