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大气温度因素复杂,现撇开太阳运动、地壳运动、大气环流、大气层下垫面等因素,来看其他因素的作用。1.气温上升,导致海水温度上升,浮游生物活动加剧,加快了碳的同化作用以及CO_2以碳酸盐形式沉积的速度,以致海水CO_2浓度剧降,使大气中CO_2渗于水,几方面作用结果是减低了大气CO_2浓度。2.大气CO_2浓度上升,绿色植物的光合作用加强,抑制了大气中浓度上升的趋势。3.石化燃料的使用,产生大量CO_2和尘埃。大气中尘埃含量的增加,加强了对太阳辐射的散射和反射,使达到地表的太阳辐射减弱,导致整个地表降温。4.水体温度上升,促使海水蒸发,使一部分水由水体进入大气层,导致海平面下
The temperature of the atmosphere is complex, and other factors such as solar motion, crustal movement, atmospheric circulation, and underlying surface of the atmosphere are all considered. 1. The rising temperatures lead to an increase in seawater temperature and aggravation of plankton activity, accelerating the assimilation of carbon and the rate of deposition of CO 2 in the form of carbonates, resulting in a drastic drop in CO 2 concentration in the seawater and CO 2 permeation into the atmosphere The result is a reduction of the atmospheric CO 2 concentration. Atmospheric CO 2 concentration increased, photosynthesis of green plants to strengthen, inhibit the concentration of the atmosphere increased. 3. The use of fossil fuels, producing large amounts of CO 2 and dust. The increase of the dust content in the atmosphere strengthens the scattering and reflection of the solar radiation so that the solar radiation reaching the ground surface will be weakened and the entire surface will be cooled down. 4. Water temperature rise, prompting the evaporation of sea water, so that part of the water from the water into the atmosphere, leading to sea level