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地形对气候的影响(The influence of topography on climate)
地形对气候的影响(The influence of topography on climate)
Nature is an organic whole. There are interdependent relations, mutual influence and mutual restriction among the elements of the geographical environment. As long as one factor changes, will cause the corresponding changes in other factors, a link closely with another link, a process to another process, finally will inevitably lead to the geographical environment from quantitative change to qualitative change, and directly or indirectly affect the survival and development of human beings. The study of the relationship and interaction between these factors is the charm of geographical science, and also the essence of geography. In every element of the geographical environment, except for the geographical latitude, topography is an important factor. The terrain can influence the climate change caused by climate complexity and diversity; terrain can destroy or cover the latitude of geographical environment, which affects the imbalance of the layout of agricultural and sideline production; and beautiful environment, is associated with the topographic conditions of interest income. Therefore, for the study of China terrain not only has theoretical significance, but also for how to according to the specific terrain conditions around the development of rational allocation of agriculture, forestry, animal husbandry, sideline and fishery and tourism industry of local conditions, as well as in the continuous transformation of natural conditions, has important practical significance for developing socialist production. The important geographical significance of Chinese topography can be summarized at least in the following aspects. 1., because of the complexity and diversity of Chinas climate, Chinas topography is complex and diverse, so it is bound to lead to the complexity and diversity of Chinas climate. The terrain influences the climate Chinese the most significant are as follows: (L) the mountains often warm air North bar
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