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Evaluation of the ECHAM family radiation codes performance in the representation of the solar signal

机译:评估ECHAM系列辐射代码在太阳信号表示中的性能

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Solar radiation is the main source of energy for the Earth's atmosphere andin many respects defines its composition, photochemistry, temperature profileand dynamics. The magnitude of the solar irradiance variability stronglydepends on the wavelength, making difficult its representation in climatemodels. Due to some deficiencies in the applied radiation codes, severalmodels fail to show a clear response in middle stratospheric heating rates tosolar spectral irradiance variability; therefore, it is important to evaluatemodel performance in this respect before doing multiple runs. In this work weevaluate the performance of three generations of ECHAM (4, 5 and 6) solar radiation schemes by a comparison with the reference high-resolution libRadtran code. We found that all original ECHAM radiation codes miss almost all solar signals in the heating rates inthe mesosphere. In the stratosphere the two-band ECHAM4 code (E4) has analmost negligible radiative response to solar irradiance changes and thesix-band ECHAM5 code (E5c) reproduces only about half of the referencesignal, while representation in the ECHAM6 code (E6) is better – it misses amaximum of about 15% in the upper stratosphere. On the basis of thecomparison results we suggest necessary improvements to the ECHAM familycodes by the inclusion of available parameterizations of the heating rate dueto absorption by oxygen (O2) and ozone (O3). Improvement ispresented for E5c and E6, and both codes, with the introducedparameterizations, represent the heating rate response to the spectral solarirradiance variability simulated with libRadtran much better without asubstantial increase in computer time. The suggested parameterizations arerecommended to be applied in the middle-atmosphere version of the ECHAM-5 and6 models for the study of the solar irradiance influence on climate.
机译:太阳辐射是地球大气层的主要能源,并且在许多方面定义了地球的成分,光化学,温度分布和动力学。太阳辐照度变异性的大小很大程度上取决于波长,因此很难在气候模型中表示出来。由于所应用的辐射规范中的某些缺陷,几种模型未能显示出平流层中层升温速率对太阳光谱辐照度可变性的明确响应。因此,在进行多次运行之前,评估这方面的模型性能非常重要。在这项工作中,我们通过与参考高分辨率libRadtran代码进行比较,评估了三代ECHAM(4、5和6)太阳辐射方案的性能。我们发现,所有原始ECHAM辐射代码都错过了中层加热速率中几乎所有的太阳信号。在平流层中,两频段ECHAM4代码(E4)对太阳辐照度变化的辐射响应几乎可以忽略不计,六频段ECHAM5代码(E5c)仅再现参考信号的一半,而ECHAM6代码(E6)的表示更好–在高层平流层中,它错过了大约15%的最大值。在比较结果的基础上,我们建议对ECHAM族代码进行必要的改进,其中包括可用的因氧(O 2 )和臭氧(O 3 )。对E5c和E6进行了改进,并且两个代码都带有引入的参数化,表示用libRadtran模拟的对光谱太阳辐照度可变性的加热速率响应要好得多,而不会显着增加计算机时间。建议将建议的参数化方法用于ECHAM-5和6模型的大气层版本,以研究太阳辐照度对气候的影响。

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