1 latitude. The lower the latitude, the higher the heat.
② Terrain. The higher the altitude, the lower the temperature.
(3) mountain block. In winter, the temperature is very high where there are mountains in the north of this area.
④ Ocean current. Warm current warms up and cold current cools down.
⑤ Air mass in front. The cold air mass cools down and the warm air mass cools down.
⑥ Underlying surface. Daytime temperature: desert > wasteland > grassland > forest > lake (low water content type, high daytime temperature)? City > Suburb (Heat Island Effect)
⑦ Land and sea position. Summer land > sea? Winter sea > land
⑧ Weather conditions. Daytime? Sunny > cloudy? Cloudy day > sunny day at night (heat preservation function of atmosphere)
Pet-name ruby land and sea breeze. Sea breeze enhances oceanity and warms up.
Attending the downward flow. The downward flow of the valley can raise the temperature (burn the wind) or lower the temperature (the cold air at high places is heavy and sinks down the slope), depending on what you need.
The yin and yang slopes of mountains.
These 1 1 factors can be summarized as follows:
Latitude, Earth, Mountain, Ocean, Forward, Down, Sea, Sky, Wind, Downstream, Yin and Yang Slope.
It can be imagined that the mountain ocean in the latitude faces the sea, and then a gust of wind blows it into the sky, meets the downward airflow and rolls down the sunny slope.
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