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广州健仑生物科技有限公司

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【Seracare产品介绍】

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【公司名称】 广州健仑生物科技有限公司
【】    杨永汉 
【】 
【腾讯 】 2042552662
【公司地址】 广州清华科技园创新基地番禺石楼镇创启路63号二期2幢101-3室
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就范围来说，自然带的划分，早期主要是根据不同纬度所获得
太阳辐射能的差异，把地球表面划分为5个带：热带、北温带、南温带：北寒带、南寒带。后来又根据各地气候、生物等差异进行了细分。
在大洋主要是根据海洋的气候、水文、生物等自然地理要素的差异，把大洋表层划分为7个带：赤道带，南热带、北热带，南温带、北温带，南极带、北极带。
由于大陆的情况复杂，地带性分异也较大洋明显，因此对大陆上自然带的划分比大洋细，不同学者的分带也不同。
以气候特点为标志划分大陆自然带，南半球和北半球从赤道向两极可分为：赤道带、热带、亚热带、暖温带、中温带、寒温带、亚寒带、寒带，共15个自然带。由于大陆自然带受到非地带性因素的影响而复杂化，每一自然带的典型特征在植被类型上具有较鲜明的表现，因此陆地自然带又可分为：热带雨林带、热带稀树草原带、热带荒漠带、亚热带荒漠草原带、亚热带森林带、温带荒漠带、温带草原带、温带阔叶林带、亚寒带针叶林带、寒带苔原带、极地冰原带。
气候、生物和土壤等相互形成的自然带，随海拔高度增高形成垂直自然带。山地自然环境比低平地区
复杂，所以山地垂直自然带比水平自然带复杂得多。
例如，北半球北回归线以北地区的山地，南坡（阳坡）比北坡（阴坡）要获得更多的热量，因此，尽管 南北坡海拔高度大致相同，但南坡气温高于北坡；潮湿气流如果与山地延伸方向相垂直或斜交，那么，迎风坡多雨，背风坡少雨。
例如中国东部山地，夏季因气流来自东南方向，所以南坡降水量多于北坡，以致南北坡相同 海拔水热状况不一，所以南北坡垂直自然带有明显差异。同是一个山地，南北坡坡麓可以分属不同的气候 带和自然带。
例如，中国秦岭南坡坡麓属于亚热带常绿阔叶林带，北坡坡麓则属于暖温带落叶阔叶林带。 任何一个山地垂直自然带，总是在相应的水平自然带基础上形 成和发展起来的。与水平自然带相*的山麓自然带，称为垂直自然带基带。
一般说来，山地所处地理 纬度愈低、气候愈湿润、相对高度愈大，垂直自然带表现愈完整。南极大陆气候严寒，呈现茫茫一片冰原 景观，就谈不上真正的垂直自然带。
On a global scale, the division of the natural belt was mainly based on different latitudes.
The difference in solar radiation energy divides the earth's surface into five zones: the tropical zone, the north temperate zone, and the southern temperate zone: the north frigid zone and the south frigid zone. Later, they were subdivided based on differences in climate and biology.
In the ocean, the ocean surface is mainly divided into seven zones according to the differences of the ocean's climate, hydrology, biology and other natural geographical factors: the equatorial belt, the southern tropics, the northern tropics, the South Temperate Zone, the North Temperate Zone, the Antarctic Zone, and the Arctic Zone.
Due to the complex conditions in the mainland and the obvious differences in zonality between the oceans, the division of the natural belts on the mainland is smaller than that of the oceans, and the zoning of different scholars is also different.
Climatic features are used to mark the mainland's natural belts. The southern and northern hemispheres can be divided from the equator to the poles: the equatorial belt, the tropics, the subtropical zone, the warm temperate zone, the middle temperate zone, the cold temperate zone, the sub-frigid zone, and the cold zone. There are 15 natural zones in the world. Since the mainland natural belts are complicated by the influence of non-zonal factors, the typical characteristics of each natural belt have a distinct expression in vegetation types, so the natural belts in the land can be further divided into: tropical rain forest belts, tropical savannah belts. , tropical desert belt, subtropical desert grassland belt, subtropical forest belt, temperate desert belt, temperate grassland belt, temperate broad-leaved forest belt, sub-arctic coniferous forest belt, cold belt tundra belt, polar ice sheet belt.
The natural belt formed by the interaction of climate, biology and soil forms a vertical natural belt with increasing altitude. Natural environment in the mountainous area than in the low flat area
Complex, so the vertical natural belt is much more complex than the horizontal natural belt.
For example, in the mountains north of the Northern Hemisphere Tropic of Cancer, the south slope (sunny slope) needs more heat than the northern slope (yin slope). Therefore, although the altitudes of the north and south slopes are roughly the same, the temperature on the south slope is higher than that on the north slope; If the moist air flow is perpendicular or oblique to the direction of the mountain extension, then the windward slope is rainy and the leeward slope is less rainy.
For example, in the eastern mountainous regions of China, the summer rainfall is from the southeastern direction, so the southern slope has more precipitation than the northern slope, resulting in different water and heat conditions at the same elevation on the north and south slopes. Therefore, the vertical nature of the north and south slopes is obviously different. The same is a mountainous area. The slopes on the north and south slopes can be divided into different climatic zones and natural zones.
For example, the slopes of the southern slope of the Qinling Mountains in China belong to the subtropical evergreen broad-leaved forest belt, while the slopes of the northern slope belong to the warm-temperate deciduous broad-leaved forest belt. Any vertical natural belt in the mountains is always formed and developed on the basis of the corresponding horizontal natural belt. Hawthorn's natural belt, which is consistent with the horizontal natural belt, is called vertical natural belt.
In general, the lower the geographical latitude, the wetter the climate, the higher the relative height, the more complete the vertical natural belt. The climate of the Antarctic continent is very cold and it presents a vast landscape of ice fields. There is no real vertical natural belt.