Idealized single-forcing GCM simulations with GFDL CM2.1

This repository contains a set of single-forcing general circulation model (GCM) simulations run with the Geophysical Fluid Dynamics Laboratory (GFDL) Climate Model 2.1 (CM2.1). In each of these equilibrium simulations, one climate forcing was altered while all others were held constant at preindust...

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Main Authors: Erb, Michael, Broccoli, Anthony, Raney, Bryan
Format: Other/Unknown Material
Language:English
Published: Zenodo 2018
Subjects:
Online Access:https://doi.org/10.5281/zenodo.1194480
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author Erb, Michael
Broccoli, Anthony
Raney, Bryan
author_facet Erb, Michael
Broccoli, Anthony
Raney, Bryan
author_sort Erb, Michael
collection Zenodo
description This repository contains a set of single-forcing general circulation model (GCM) simulations run with the Geophysical Fluid Dynamics Laboratory (GFDL) Climate Model 2.1 (CM2.1). In each of these equilibrium simulations, one climate forcing was altered while all others were held constant at preindustrial levels, modeling the climate response to individual climate forcings. Simulations were run for obliquity (low and high obliquity), precession (four phases of the precession cycle with high eccentricity, and one simulation with eccentricity set to zero), half CO 2 , and LGM-sized ice sheets. The values chosen for the orbital simulations represent the extreme values of the past 900 thousand years. Simulations were run for at least 500 years, and forcings do not change from year to year. The uploaded files are 100 year annual-means and monthly climatologies. Variables are presented for the atmosphere, ocean, sea ice, and land. Monthly ocean files are not currently available; please contact Michael Erb at michael.p.erb@gmail.com if you are interested in those results. === FORCINGS === Preindustrial climate forcings were set to the following values: - Obliquity: 23.439° - Longitude of perihelion: 102.93° - Eccentricity: 0.0167 - CO 2 : 286 ppm - Ice sheets: 0 ka BP The remaining simulations explore the climate response to a change in one of these forcings, with all other forcings set to preindustrial levels. Forcings are specified as follows: - lo_obliq and hi_obliq: Obliquity is set to 22.079° or 24.480°, respectively. - 0_AEQ, 90_WSOL, 180_VEQ, and 270_SSOL: Perihelion occurs at the NH autumnal equinox, winter solstice, vernal equinox, or summer solstice, respectively, with eccentricity set to 0.0493. This corresponds to a longitude of perihelion of 0°, 90°, 180°, or 270°, respectively. - ECC_0: Eccentricity is set to 0. - half_CO2: CO 2 is set to 143 ppm. - ice_sheets: Ice sheets and sea level are set to Last Glacial Maximum (LGM) levels. Ice sheets come from the ICE-5G reconstruction. A note about preindustrial ...
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spelling ftzenodo:oai:zenodo.org:1194480 2025-01-17T00:46:15+00:00 Idealized single-forcing GCM simulations with GFDL CM2.1 Erb, Michael Broccoli, Anthony Raney, Bryan 2018-04-09 https://doi.org/10.5281/zenodo.1194480 eng eng Zenodo https://doi.org/10.5281/zenodo.1194479 https://doi.org/10.5281/zenodo.1194480 oai:zenodo.org:1194480 info:eu-repo/semantics/openAccess Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode Climate Modeling GCM GFDL CM2.1 Paleoclimate Milankovitch Obliquity Precession Eccentricity CO2 Ice sheets Single-forcing Fingerprint info:eu-repo/semantics/other 2018 ftzenodo https://doi.org/10.5281/zenodo.119448010.5281/zenodo.1194479 2024-12-06T16:25:14Z This repository contains a set of single-forcing general circulation model (GCM) simulations run with the Geophysical Fluid Dynamics Laboratory (GFDL) Climate Model 2.1 (CM2.1). In each of these equilibrium simulations, one climate forcing was altered while all others were held constant at preindustrial levels, modeling the climate response to individual climate forcings. Simulations were run for obliquity (low and high obliquity), precession (four phases of the precession cycle with high eccentricity, and one simulation with eccentricity set to zero), half CO 2 , and LGM-sized ice sheets. The values chosen for the orbital simulations represent the extreme values of the past 900 thousand years. Simulations were run for at least 500 years, and forcings do not change from year to year. The uploaded files are 100 year annual-means and monthly climatologies. Variables are presented for the atmosphere, ocean, sea ice, and land. Monthly ocean files are not currently available; please contact Michael Erb at michael.p.erb@gmail.com if you are interested in those results. === FORCINGS === Preindustrial climate forcings were set to the following values: - Obliquity: 23.439° - Longitude of perihelion: 102.93° - Eccentricity: 0.0167 - CO 2 : 286 ppm - Ice sheets: 0 ka BP The remaining simulations explore the climate response to a change in one of these forcings, with all other forcings set to preindustrial levels. Forcings are specified as follows: - lo_obliq and hi_obliq: Obliquity is set to 22.079° or 24.480°, respectively. - 0_AEQ, 90_WSOL, 180_VEQ, and 270_SSOL: Perihelion occurs at the NH autumnal equinox, winter solstice, vernal equinox, or summer solstice, respectively, with eccentricity set to 0.0493. This corresponds to a longitude of perihelion of 0°, 90°, 180°, or 270°, respectively. - ECC_0: Eccentricity is set to 0. - half_CO2: CO 2 is set to 143 ppm. - ice_sheets: Ice sheets and sea level are set to Last Glacial Maximum (LGM) levels. Ice sheets come from the ICE-5G reconstruction. A note about preindustrial ... Other/Unknown Material Sea ice Zenodo
spellingShingle Climate
Modeling
GCM
GFDL
CM2.1
Paleoclimate
Milankovitch
Obliquity
Precession
Eccentricity
CO2
Ice sheets
Single-forcing
Fingerprint
Erb, Michael
Broccoli, Anthony
Raney, Bryan
Idealized single-forcing GCM simulations with GFDL CM2.1
title Idealized single-forcing GCM simulations with GFDL CM2.1
title_full Idealized single-forcing GCM simulations with GFDL CM2.1
title_fullStr Idealized single-forcing GCM simulations with GFDL CM2.1
title_full_unstemmed Idealized single-forcing GCM simulations with GFDL CM2.1
title_short Idealized single-forcing GCM simulations with GFDL CM2.1
title_sort idealized single-forcing gcm simulations with gfdl cm2.1
topic Climate
Modeling
GCM
GFDL
CM2.1
Paleoclimate
Milankovitch
Obliquity
Precession
Eccentricity
CO2
Ice sheets
Single-forcing
Fingerprint
topic_facet Climate
Modeling
GCM
GFDL
CM2.1
Paleoclimate
Milankovitch
Obliquity
Precession
Eccentricity
CO2
Ice sheets
Single-forcing
Fingerprint
url https://doi.org/10.5281/zenodo.1194480