DOI: 10.5281/zenodo.6762449
title: What Controls the Mean East–West Sea Surface Temperature Gradient in the Equatorial Pacific: The Role of Cloud Albedo

description: Climatologies for the climate model simulations performed by Burls and Fedorov 2014, Journal of Climate, https://doi.org/10.1175/JCLI-D-13-00255.1. This table shows how the names of the simulation files provided in this dataset relate to the experiment names provided in Table 1 of Burls and Fedorov (2014, JOC). Experiment # in Article (Table 1) Name of Files 1 PreInd_T31_gx3v7*.nc 2 80p_op_LWP_1590deg_T31_gx3v7*.nc 3 60p_op_LWP_1590deg_T31_gx3v7*.nc 4 40p_op_LWP_1590deg_T31_gx3v7*.nc 5 20p_op_LWP_1590deg_T31_gx3v7*.nc 6 20p_LWP_1590deg_T31_gx3v7*.nc 7 40p_LWP_1590deg_T31_gx3v7*.nc 8 60p_LWP_1590deg_T31_gx3v7*.nc 9 80p_LWP_1590deg_T31_gx3v7*.nc 10 20p_ILWP_1590deg_tropx2_T31_gx3v7*.nc 11 40p_ILWP_1590deg_tropx2_T31_gx3v7*.nc 12 60p_ILWP_1590deg_tropx2_T31_gx3v7*.nc 13 80p_ILWP_1590deg_tropx2_T31_gx3v7*.nc 14 20p_ILWP_1590deg_tropx4_T31_gx3v7*.nc 15 40p_ILWP_1590deg_tropx4_T31_gx3v7*.nc 16 60p_ILWP_1590deg_tropx4_T31_gx3v7*.nc 17 80p_ILWP_1590deg_tropx4_T31_gx3v7*.nc 18 20p_ILWP_3060deg_tropx8_T31_gx3v7*.nc 19 40p_ILWP_3060deg_tropx8_T31_gx3v7*.nc 20 60p_ILWP_3060deg_tropx8_T31_gx3v7*.nc 21 80p_ILWP_3060deg_tropx8_T31_gx3v7*.nc 22 PreInd_0.9x1.25_gx1v6*.nc 23 40p_LWP_1590deg_0.9x1.25_gx1v6*.nc 24 60p_LWP_1590deg_0.9x1.25_gx1v6*.nc 25 40p_ILWP_1590deg_tropx2_0.9x1.25_gx1v6*.nc 26 60p_ILWP_1590deg_tropx2_0.9x1.25_gx1v6*.nc Article abstract: The mean east–west sea surface temperature gradient along the equator is a key feature of tropical climate. Tightly coupled to the atmospheric Walker circulation and the oceanic east–west thermocline tilt, it effectively defines tropical climate conditions. In the Pacific, its presence permits the El Niño–Southern Oscillation phenomenon. What determines this temperature gradient within the fully coupled ocean–atmosphere system is therefore a central question in climate dynamics, critical for understanding past and future climates. Using a comprehensive coupled model [Community Earth System Model (CESM)], the authors demonstrate how the meridional gradient in cloud albedo between the tropics and midlatitudes (Δα) sets the mean east–west sea surface temperature gradient in the equatorial Pacific. To change Δα in the numerical experiments, the authors change the optical properties of clouds by modifying the atmospheric water path, but only in the shortwave radiation scheme of the model. When Δα is varied from approximately −0.15 to 0.1, the east–west SST contrast in the equatorial Pacific reduces from 7.5°C to less than 1°C and the Walker circulation nearly collapses. These experiments reveal a near-linear dependence between Δα and the zonal temperature gradient, which generally agrees with results from the Coupled Model Intercomparison Project phase 5 (CMIP5) preindustrial control simulations. The authors explain the close relation between the two variables using an energy balance model incorporating the essential dynamics of the warm pool, cold tongue, and Walker circulation complex.
description: {"references": ["Burls, N. J., & Fedorov, A. V. (2014). What controls the mean east\u2013west sea surface temperature gradient in the equatorial Pacific: The role of cloud albedo. Journal of Climate, 27(7), 2757-2778."]}