{"title":"Development and Evaluation of a New Correlated K-Distribution Scheme for BCC_RAD Radiative Transfer Model","authors":"Liting Liu, Hua Zhang","doi":"10.1029/2024JD041257","DOIUrl":null,"url":null,"abstract":"<p>With the significant increase in the abundance of greenhouse gases in the atmosphere over recent decades, more of the weak gaseous absorption bands are required to be incorporated in the gas optics model to improve the computational accuracy of radiation, and thus the warming effect of gases. Based on the latest HITRAN2020 spectroscopic data, a new 36-band correlated <i>k</i>-distribution (CKD) scheme is developed with high spectral band resolution for radiative transfer model. By considering errors of both radiative fluxes and atmospheric heating rates, optimizations are made to select the overlapping method and the number of <i>k</i>-distribution quadrature points in each band. The new CKD model exhibits a remarkable improvement in heating rates and radiative fluxes relative to the previous 17-band model when performing the identical radiative transfer calculations under 50 atmospheric profiles. The heating rate root-mean-square errors (RMSEs) of the 36-band model are 0.101 and 0.075 K d<sup>−1</sup> below 4 hPa for longwave and shortwave, respectively, when validated against the line-by-line benchmarks. The longwave irradiance RMSE is 0.47 W m<sup>−2</sup> at the top of atmosphere, and the shortwave RMSE is 2.15 W m<sup>−2</sup> at the surface. Furthermore, the cases simulating radiative forcing induced by varying gas concentrations demonstrate the ability of the 36-band model to study the warming effect of greenhouse gases.</p>","PeriodicalId":15986,"journal":{"name":"Journal of Geophysical Research: Atmospheres","volume":"130 1","pages":""},"PeriodicalIF":3.4000,"publicationDate":"2025-01-04","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Journal of Geophysical Research: Atmospheres","FirstCategoryId":"89","ListUrlMain":"https://agupubs.onlinelibrary.wiley.com/doi/10.1029/2024JD041257","RegionNum":2,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q2","JCRName":"METEOROLOGY & ATMOSPHERIC SCIENCES","Score":null,"Total":0}
引用次数: 0
Abstract
With the significant increase in the abundance of greenhouse gases in the atmosphere over recent decades, more of the weak gaseous absorption bands are required to be incorporated in the gas optics model to improve the computational accuracy of radiation, and thus the warming effect of gases. Based on the latest HITRAN2020 spectroscopic data, a new 36-band correlated k-distribution (CKD) scheme is developed with high spectral band resolution for radiative transfer model. By considering errors of both radiative fluxes and atmospheric heating rates, optimizations are made to select the overlapping method and the number of k-distribution quadrature points in each band. The new CKD model exhibits a remarkable improvement in heating rates and radiative fluxes relative to the previous 17-band model when performing the identical radiative transfer calculations under 50 atmospheric profiles. The heating rate root-mean-square errors (RMSEs) of the 36-band model are 0.101 and 0.075 K d−1 below 4 hPa for longwave and shortwave, respectively, when validated against the line-by-line benchmarks. The longwave irradiance RMSE is 0.47 W m−2 at the top of atmosphere, and the shortwave RMSE is 2.15 W m−2 at the surface. Furthermore, the cases simulating radiative forcing induced by varying gas concentrations demonstrate the ability of the 36-band model to study the warming effect of greenhouse gases.
近几十年来,随着大气中温室气体丰度的显著增加,需要在气体光学模型中加入更多的弱气体吸收带,以提高辐射的计算精度,从而提高气体的增温效应。基于最新的HITRAN2020光谱数据,提出了一种具有高光谱分辨率的36波段相关k分布(CKD)方案。在考虑辐射通量和大气升温速率误差的基础上,对重叠方式和各波段k分布交点个数进行了优化选择。在50个大气剖面下进行相同的辐射传输计算时,与以前的17波段模式相比,新的CKD模式在加热速率和辐射通量方面有显著改善。通过逐行基准验证,36波段模型在4 hPa以下的长波和短波升温速率均方根误差(rmse)分别为0.101和0.075 K d - 1。大气顶部长波辐照度RMSE为0.47 W m−2,地表短波辐照度RMSE为2.15 W m−2。此外,模拟不同气体浓度引起的辐射强迫的案例也证明了36波段模式研究温室气体增温效应的能力。
期刊介绍:
JGR: Atmospheres publishes articles that advance and improve understanding of atmospheric properties and processes, including the interaction of the atmosphere with other components of the Earth system.