What's the last sentence of different days in ten miles?

A geographical phenomenon, "There are four seasons in one mountain, and different days in ten miles."

there are four seasons in one mountain, and different days in ten miles. It's about the vertical zonality of mountains. It is in Yunnan-Guizhou area of China. Due to the rugged landform of Yunnan-Guizhou Plateau, there are various weather types in mountainous areas.

The reason why the sky within ten miles is different is that it is the last sentence "There are four seasons in one mountain." We all know that the four seasons are "spring", "summer", "autumn" and "winter", and the four seasons have four temperatures. The climate is large-scale in time and is a synthesis of a large number of weather processes. Weather refers to the synthesis of atmospheric conditions and atmospheric phenomena in a certain area or a short period of time.

Therefore, with the change of solar terms, the "sky" also changes. Therefore, the last sentence of "ten miles is different from the sky" is: "One mountain has four seasons". At the same time, it is also a kind of literary decoration, which is often used to compare the gap, difference and difference between people in the scope of philosophy. From "there are four seasons in one mountain, and different days in ten miles." Evolved into "different days in ten miles, different people in a hundred miles." The metaphorical method of.

Extended data

Atmospheric circulation generally refers to a large-scale atmospheric operation phenomenon with world scale, including both average state and instantaneous phenomenon, with a horizontal scale of more than several thousand kilometers, a vertical scale of more than 1km and a time scale of more than several days. The state of large-scale motion of the atmosphere.

in a large area (such as Europe and Asia, hemisphere and the whole world), the average state of atmospheric movement in a long period (such as months, seasons, years and years) or the change process of atmospheric movement in a certain period (such as one week and rainy season) can be called atmospheric circulation.

the atmospheric circulation is mainly manifested in the east-west wind belt, the three-circle circulation (Hadley circulation, Ferrer circulation and polar circulation), the average ridge of steady distribution, the high-altitude jet and the large disturbance in the westerlies.

the atmospheric circulation is not only an important mechanism for the exchange of physical quantities such as heat, moisture and angular momentum, but also an important result of the transportation, balance and transformation of these physical quantities. The uneven distribution of solar radiation on the earth's surface is the driving force of atmospheric circulation.