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我省地处华北大平原之西,属山陕黄土高原的一部分。全省大部地区海拔在千米以上,由于受地质构造和河流切割作用的影响,高原面貌已缺乏完整的形态。就自然地理情况来看,山地多,平原少,沟壑縱横,山岭重迭,地形起伏变化很大,再加上緯度和海陆位置的关系,使得本省的气候错綜复杂,土壤类型多种多样。一、自然环境概况及其特点由于本省位居内陆高原,气候变化受地理环境的影响很大,一年中绝大部分时间受蒙古高气压控制,加之又为塞潮入侵我国的要冲,受海洋气候调剂作用很少,各地气候差异很大。大致晋南和晋中属于暖温带干旱森林和森林草原型的气候。晋北和晋西北则
The province is located in the west of the Great Plains of North China, is part of the Shan-Shan Loess Plateau. Most parts of the province at an elevation of more than one kilometer, due to geological structure and the impact of river cutting, the plateau has a lack of complete morphology. In terms of physical and geographical conditions, there are many mountains, few plains, ravines and mountains, overlapping mountains and undulating terrain. Coupled with the relationship between latitude and land-sea position, the climate in this province is intricate with varied types of soil. I. Overview of the natural environment and its characteristics As a result of the province’s inland plateau, climate change is greatly affected by the geographical environment, the vast majority of the year under the control of Mongolia’s high pressure, combined with the implosion of the implosion of China’s impulse, by The role of the marine climate adjustment is very small, very different climate across. Generally, Jinnan and Jinzhong belong to the climate of warm temperate arid forest and forest prairie. North Shanxi and Shanxi Northwest then