Data for "Nonlinear coupling between longwave radiative climate feedbacks"

Published: 25 February 2021| Version 1 | DOI: 10.17632/pb35hm5ksd.1
Contributor:
han huang

Description

enso_dx.nc: contains the response of feedback variables in ENSO case (figure 1) 4xco2_dx.nc: the same as enso_dx.nc but in 4xco2 case enso_dR.nc: contains the truth of each feedback simulated by RRTM in ENSO case, such as dR_total, dRq, dRt, dRc, dRcq, dRct, dRqt (figure 2-3, table 1), for both TOA upward and SFC downward enso_dRc_estimate.nc contains 1. dRc and dRcq truth value simulated by RRTM. 2. dRc estimated in the kernel (ACRF) method (figure 4) 3. dRcq estimated by the one-layer model and RRTM-simulated univariate cloud feedback with instantaneous/monthly mean profiles (figure 5, table 2) 4. dRc and dRcq estimated by the combination of kernel method and one-layer model (equation 21, figure 8, table 3) 4xco2_dR.nc: contains the truth of each feedback simulated by RRTM in 4xCO2 case, such as dR_total, dRq, dRt, dRc, dRcq, dRct, dRqt (table 3), for both TOA upward and SFC downward 4xco2_dRc_estimate.nc contains 1. dRc and dRcq truth value simulated by RRTM. 2. dRcq estimated by the one-layer model and RRTM-simulated univariate cloud feedback with instantaneous/monthly mean profiles (figure 6-7)

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Institutions

McGill University

Categories

Climate Feedback

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