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The Effect of Atmospheric Pressure on Snowball Earth Deglaciation

机译:大气压力对雪球地球扩大的影响

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The most common explanation for the escape from a Snowball Earth state involves, among other factors, a strong greenhouse effect caused by a large partial pressure of CO2. This leads to an increase in surface pressure, which most models do not account for. With a higher surface pressure, pressure broadening increases, and convection reaches a deeper layer, both of which result in higher surface temperatures. The latter mechanism, which has not previously been reported, is found to be a greater source of warming than pressure broadening in the normal range of CO2 partial pressures at the point of deglaciation.
机译:逃离雪球地球国家的最常见解释涉及由其他因素引起的强大的温室效应,这是由CO 2的大部分压力引起的强烈温室效应。这导致表面压力的增加,大多数模型不占用。具有较高的表面压力,压力扩大增加,对流达到深层层,这两层都导致表面温度更高。尚未报道的后一种机构被认为是比在脱光点的CO 2部分压力的正常范围内的压力扩大的更大来源。

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