Idealized single-forcing GCM simulations with NCAR CESM

This repository contains a set of single-forcing general circulation model (GCM) simulations run with the National Center for Atmospheric Research (NCAR) Community Earth System Model version 1.2 (CESM1.2). In each of these equilibrium simulations, one climate forcing was altered while all others wer...

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Main Authors: Erb, Michael, Jackson, Charles, DiNezio, Pedro
Format: Other/Unknown Material
Language:English
Published: Zenodo 2018
Subjects:
Online Access:https://doi.org/10.5281/zenodo.1194490
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author Erb, Michael
Jackson, Charles
DiNezio, Pedro
author_facet Erb, Michael
Jackson, Charles
DiNezio, Pedro
author_sort Erb, Michael
collection Zenodo
description This repository contains a set of single-forcing general circulation model (GCM) simulations run with the National Center for Atmospheric Research (NCAR) Community Earth System Model version 1.2 (CESM1.2). 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 (or longer) monthly climatologies. For most simulations, variables are presented for the atmosphere (atm), sea ice (cice), land (clm2), and river runoff (rtm). For the ice sheets simulation and its corresponding preindustrial simulation (0ka), only atmospheric output is presented; to inquire about other fields for those simulations, please contact Pedro DiNezio at pdn@ig.utexas.edu. 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 for the 0ka_0urb simulation were set to the following values: - Obliquity: 23.44107° - Longitude of perihelion: 102.7242° - Eccentricity: 0.01670772 - CO 2 : 284.7 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 ...
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spelling ftzenodo:oai:zenodo.org:1194490 2025-01-17T00:46:15+00:00 Idealized single-forcing GCM simulations with NCAR CESM Erb, Michael Jackson, Charles DiNezio, Pedro 2018-04-09 https://doi.org/10.5281/zenodo.1194490 eng eng Zenodo https://doi.org/10.5281/zenodo.1194489 https://doi.org/10.5281/zenodo.1194490 oai:zenodo.org:1194490 info:eu-repo/semantics/openAccess Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode Climate Modeling GCM NCAR CESM Paleoclimate Milankovitch Obliquity Precession Eccentricity CO2 Ice sheets Single-forcing Fingerprint info:eu-repo/semantics/other 2018 ftzenodo https://doi.org/10.5281/zenodo.119449010.5281/zenodo.1194489 2024-12-06T16:05:28Z This repository contains a set of single-forcing general circulation model (GCM) simulations run with the National Center for Atmospheric Research (NCAR) Community Earth System Model version 1.2 (CESM1.2). 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 (or longer) monthly climatologies. For most simulations, variables are presented for the atmosphere (atm), sea ice (cice), land (clm2), and river runoff (rtm). For the ice sheets simulation and its corresponding preindustrial simulation (0ka), only atmospheric output is presented; to inquire about other fields for those simulations, please contact Pedro DiNezio at pdn@ig.utexas.edu. 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 for the 0ka_0urb simulation were set to the following values: - Obliquity: 23.44107° - Longitude of perihelion: 102.7242° - Eccentricity: 0.01670772 - CO 2 : 284.7 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 ... Other/Unknown Material Sea ice Zenodo
spellingShingle Climate
Modeling
GCM
NCAR
CESM
Paleoclimate
Milankovitch
Obliquity
Precession
Eccentricity
CO2
Ice sheets
Single-forcing
Fingerprint
Erb, Michael
Jackson, Charles
DiNezio, Pedro
Idealized single-forcing GCM simulations with NCAR CESM
title Idealized single-forcing GCM simulations with NCAR CESM
title_full Idealized single-forcing GCM simulations with NCAR CESM
title_fullStr Idealized single-forcing GCM simulations with NCAR CESM
title_full_unstemmed Idealized single-forcing GCM simulations with NCAR CESM
title_short Idealized single-forcing GCM simulations with NCAR CESM
title_sort idealized single-forcing gcm simulations with ncar cesm
topic Climate
Modeling
GCM
NCAR
CESM
Paleoclimate
Milankovitch
Obliquity
Precession
Eccentricity
CO2
Ice sheets
Single-forcing
Fingerprint
topic_facet Climate
Modeling
GCM
NCAR
CESM
Paleoclimate
Milankovitch
Obliquity
Precession
Eccentricity
CO2
Ice sheets
Single-forcing
Fingerprint
url https://doi.org/10.5281/zenodo.1194490