# Resolving Orbital and Climate Keys of Earth and Extraterrestrial   Environments with Dynamics 1.0: A General Circulation Model for Simulating   the Climates of Rocky Planets

**Authors:** M. J. Way, Igor Aleinov, David. S. Amundsen, Mark Chandler, Thomas, Clune, Anthony D. Del Genio, Yuka Fujii, Maxwell Kelley, Nancy Y. Kiang,, Linda Sohl, Kostas Tsigaridis

arXiv: 1701.02360 · 2017-07-26

## TL;DR

ROCKE-3D is a versatile 3D general circulation model developed for simulating atmospheres of terrestrial planets within the Solar System and beyond, accommodating diverse planetary conditions and compositions.

## Contribution

It extends the capabilities of the existing ModelE2 to model a wide range of planetary atmospheres, including exoplanets, with various atmospheric and surface conditions.

## Key findings

- Successfully simulates diverse planetary atmospheres
- Validates model across different pressures and compositions
- Expands modeling to exoplanetary environments

## Abstract

Resolving Orbital and Climate Keys of Earth and Extraterrestrial Environments with Dynamics (ROCKE-3D) is a 3-Dimensional General Circulation Model (GCM) developed at the NASA Goddard Institute for Space Studies for the modeling of atmospheres of Solar System and exoplanetary terrestrial planets. Its parent model, known as ModelE2 (Schmidt et al. 2014), is used to simulate modern and 21st Century Earth and near-term paleo-Earth climates. ROCKE-3D is an ongoing effort to expand the capabilities of ModelE2 to handle a broader range of atmospheric conditions including higher and lower atmospheric pressures, more diverse chemistries and compositions, larger and smaller planet radii and gravity, different rotation rates (slowly rotating to more rapidly rotating than modern Earth, including synchronous rotation), diverse ocean and land distributions and topographies, and potential basic biosphere functions. The first aim of ROCKE-3D is to model planetary atmospheres on terrestrial worlds within the Solar System such as paleo-Earth, modern and paleo-Mars, paleo-Venus, and Saturn's moon Titan. By validating the model for a broad range of temperatures, pressures, and atmospheric constituents we can then expand its capabilities further to those exoplanetary rocky worlds that have been discovered in the past and those to be discovered in the future. We discuss the current and near-future capabilities of ROCKE-3D as a community model for studying planetary and exoplanetary atmospheres.

## Full text

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## Figures

15 figures with captions in the complete paper: https://tomesphere.com/paper/1701.02360/full.md

## References

131 references — full list in the complete paper: https://tomesphere.com/paper/1701.02360/full.md

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Source: https://tomesphere.com/paper/1701.02360