Climates of Warm Earth-like Planets I: 3-D Model Simulations
M.J. Way, A.D. Del Genio, I. Aleinov, T.L. Clune, M. Kelley, N.Y., Kiang

TL;DR
This study uses 3-D climate models to simulate Earth-like planets with varying insolation and rotation, focusing on climate feedbacks, ocean heat transport effects, and implications for habitability.
Contribution
First comprehensive 3-D simulations of Earth-like planets with modern topography, exploring climate responses to rotation and insolation variations, including ocean heat transport effects.
Findings
Slower rotation leads to cooler temperatures due to water vapor reduction.
Ocean heat transport influences climate sensitivity and heat distribution.
Cloud parameterization uncertainties affect habitability assessments.
Abstract
We present a large ensemble of simulations of an Earth-like world with increasing insolation and rotation rate. Unlike previous work utilizing idealized aquaplanet configurations we focus our simulations on modern Earth-like topography. The orbital period is the same as modern Earth, but with zero obliquity and eccentricity. The atmosphere is 1 bar N-dominated with CO=400 ppmv and CH=1 ppmv. The simulations include two types of oceans; one without ocean heat transport (OHT) between grid cells as has been commonly used in the exoplanet literature, while the other is a fully coupled dynamic bathtub type ocean. The dynamical regime transitions that occur as day length increases induce climate feedbacks producing cooler temperatures, first via the reduction of water vapor with increasing rotation period despite decreasing shortwave cooling by clouds, and then via…
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