全球变暖背景下温室效应的光谱能量分布分析

Analysis on Spectral Energy Distribution of Greenhouse Effect Under Global Warming Background

利用一维辐射传递方程及LBLRTM逐线积分模式建立计算模型，对工业革命前与目前大气构成情况下温室效应的能量分布及其光谱吸收机理进行分析，在保持温室气体浓度为当前水平的基础上，研究温室效应能量分布与地表温度之间的相互耦合机理。结果表明：工业革命前地球的温暖环境主要来自于大气温室气体的（100～370） cm－1、（640～710） cm－1以及（1370～2000） cm－1三个强吸收带对于地球长波辐射的吸收，而地球当前的变暖则源自于大气的（370～640） cm－1和（710～1370） cm－1两个弱吸收带的作用，其对工业革命以来所额外增加的温室效应贡献分别达到了25％和55％；地表温度升高，温室效应在全波段范围内也会随之增强，但不同谱带处的温室效应贡献以地球平均温度所对应的辐射峰值波数为界线，峰值波数右侧的温室效应贡献将会增加，在其左侧的贡献比例则会减小。

In a one-dimensional radiation transfer model, energy distribution and spectral absorption mechanism of greenhouse effect under Pre-Industrial and current atmospheric compositions were analyzed. Coupling mechanism between greenhouse effect and surface temperature was investigated on the basis of greenhouse gas concentrations at current level. It shows that warm environment before Industrial Revolution is mainly due to three strong absorption bands of greenhouse gases, which are （100-370） cm-1 , （640-710） cm-1 and （1 370-2 000） cm-1 respectively. However, current global warming is originated from weak absorption bands of greenhouse gases, that is, radiation absorptions by （370-640） cm-1and （710-1 370） cm-1. Contributions to greenhouse effect increment of these weak bands after Industrial Revolution are 25% and 55% respectively. With rising temperature, contribution of right side of the earth’ s radiation peak wavenumber to total greenhouse effect shows positive change, while contribution of left side shows negative change.