The Top‐of‐Atmosphere, Surface and Atmospheric Cloud Radiative Kernels Based on ISCCP‐H Datasets: Method and Evaluation. Issue 24 (14th December 2021)

• Record Type: Journal Article
• Authors: Zhang, Yuanchong; Jin, Zhonghai; Sikand, Monika
• Is Part Of: Journal of geophysical research. Volume 126:Issue 24(2021)
• Page Start: n/a
• Page End: n/a
• Publication Date: 2021-12-14
• Subjects: cloud radiative kernel -- ISCCP‐FH -- cloud feedback -- cloud radiative effects -- cloud‐type based decomposition -- CERES; Atmospheric physics -- Periodicals; Geophysics -- Periodicals; 551.5
• DOI: 10.1029/2021JD035053
• Languages: English
• ISSNs: 2169-897X

Abstract

Abstract: This study aims to create observation‐based cloud radiative kernel (CRK) datasets and evaluate them by direct comparison of CRK and the CRK‐derived cloud feedback datasets. Based on the International Satellite Cloud Climatology Project (ISCCP) H datasets, we calculate CRKs (called ISCCP‐FH or FH CRKs) as 2D joint function/histogram of cloud optical depth and cloud top pressure for shortwave (SW), longwave (LW), and their sum, Net, at the top of atmosphere (TOA), as well as, for the first time, at the surface (SFC) and in the atmosphere (ATM). With cloud fraction change (CFC) datasets from doubled‐CO2 simulation and short‐term observational anomalies, we derive all the TOA, SFC and ATM cloud feedback for SW, LW and Net using our CRKs.The direct comparison with modeled and observed CRKs (or cloud radiative effects), cloud feedback from previous model results and the Clouds and the Earth's Radiant Energy System products show that our CRKs and CRK‐derived cloud feedback are reasonably well validated. We estimate the uncertainty for the CRK‐derived cloud feedback and show that the CFC‐associated uncertainty contributes >98.5% of the total cloud feedback uncertainty while CRK's is very small. Our preliminary evaluation also shows that some near‐zero/small cloud feedback in the TOA‐alone feedback indeed results from the compensation of sizable cloud feedback of the SFC and ATM feedback and reveals some significant surface and atmospheric cloud feedback whose sum appears insignificant in TOA‐alone feedback. In addition, the atmospheric longwave cloud feedback seems to play a role in enhancing meridional atmospheric energy transport. Key Points: The cloud radiative kernel datasets are created for longwave, shortwave and their sum, net, respectively, at the top of atmosphere, the surface and in the atmosphere. They are evaluated by direct comparison with the counterparts of the other three representative datasets and with the cloud radiative effects from the Clouds and the Earth's Radiant Energy System products. In addition, the kernel‐derived cloud feedback is also directly compared with the previous ensemble results from 10 climate models and the observation‐based results from the Clouds and the Earth's Radiant Energy System products. Both comparisons well‐validated our cloud kernels and their derived cloud feedback The uncertainty budget for cloud kernel‐derived cloud feedback at the top of atmosphere is estimated based on uncertainties of cloud kernels and cloud fraction change from the direct comparisons. It shows that the cloud fraction change associated uncertainty contributes >98.5% of the total cloud feedback uncertainty while cloud kernels' is very small. We have also tested the effect of dry bias of water vapor on the cloud radiative kernel calculation when the clear‐sky water vapor is used for the cloud‐free layers under cloud layers and estimated error/uncertainty may be caused in the calculation by such a dry bias. The results show such‐caused errors/uncertainties are in high order and need not to be taken into account at present Our preliminary evaluation also shows that some near‐zero or small cloud feedback in the top‐of‐atmosphere‐alone feedback results from the compensation of sizable cloud feedback of the surface and atmospheric feedback. It demonstrates how the surface and atmospheric cloud kernel‐derived cloud feedback can be used to reveal some significant surface and atmospheric cloud feedback whose sum appears insignificant in the top‐of‐atmosphere‐alone feedback. In addition, the atmospheric longwave cloud feedback may play a role in enhancing meridional atmospheric energy transport