data for Antarctic warming with f09_gx1v6

Numerical experiments are carried out with a fully coupled global climate model (Community Earth System Model version 1.2; CESM1.2). The model grid is f09_gx1v6. We reproduced two experiments with higher resolutions to study thewarming mechanisms in Antarctica. They are control run (CTRL; CO2 concen...

Full description

Bibliographic Details
Main Author: Haijin Dai
Format: Other/Unknown Material
Language:unknown
Published: Zenodo 2023
Subjects:
Antarc*
Antarctic
Antarctica
Sea ice
Online Access:https://doi.org/10.5281/zenodo.8283053
id ftzenodo:oai:zenodo.org:8283053
record_format openpolar
spelling ftzenodo:oai:zenodo.org:8283053 2024-09-15T17:47:02+00:00 data for Antarctic warming with f09_gx1v6 Haijin Dai 2023-08-25 https://doi.org/10.5281/zenodo.8283053 unknown Zenodo https://doi.org/10.5281/zenodo.8283052 https://doi.org/10.5281/zenodo.8283053 oai:zenodo.org:8283053 info:eu-repo/semantics/openAccess Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode info:eu-repo/semantics/other 2023 ftzenodo https://doi.org/10.5281/zenodo.828305310.5281/zenodo.8283052 2024-07-25T12:21:00Z Numerical experiments are carried out with a fully coupled global climate model (Community Earth System Model version 1.2; CESM1.2). The model grid is f09_gx1v6. We reproduced two experiments with higher resolutions to study thewarming mechanisms in Antarctica. They are control run (CTRL; CO2 concentration remains 285 ppm), and albedo perturbation run (0.1A; sea-ice albedo is set to 0.1 of its original value and no change in CO2). They all start from a climate equilibrium state (B1850) and integrate over 400 model years. We focus on the equilibrium responsesusing the monthly averaged fields over the last 100 years of integration, unless otherwise stated. Other/Unknown Material Antarc* Antarctic Antarctica Sea ice Zenodo
institution Open Polar
collection Zenodo
op_collection_id ftzenodo
language unknown
description Numerical experiments are carried out with a fully coupled global climate model (Community Earth System Model version 1.2; CESM1.2). The model grid is f09_gx1v6. We reproduced two experiments with higher resolutions to study thewarming mechanisms in Antarctica. They are control run (CTRL; CO2 concentration remains 285 ppm), and albedo perturbation run (0.1A; sea-ice albedo is set to 0.1 of its original value and no change in CO2). They all start from a climate equilibrium state (B1850) and integrate over 400 model years. We focus on the equilibrium responsesusing the monthly averaged fields over the last 100 years of integration, unless otherwise stated.
format Other/Unknown Material
author Haijin Dai
spellingShingle Haijin Dai
data for Antarctic warming with f09_gx1v6
author_facet Haijin Dai
author_sort Haijin Dai
title data for Antarctic warming with f09_gx1v6
title_short data for Antarctic warming with f09_gx1v6
title_full data for Antarctic warming with f09_gx1v6
title_fullStr data for Antarctic warming with f09_gx1v6
title_full_unstemmed data for Antarctic warming with f09_gx1v6
title_sort data for antarctic warming with f09_gx1v6
publisher Zenodo
publishDate 2023
url https://doi.org/10.5281/zenodo.8283053
genre Antarc*
Antarctic
Antarctica
Sea ice
genre_facet Antarc*
Antarctic
Antarctica
Sea ice
op_relation https://doi.org/10.5281/zenodo.8283052
https://doi.org/10.5281/zenodo.8283053
oai:zenodo.org:8283053
op_rights info:eu-repo/semantics/openAccess
Creative Commons Attribution 4.0 International
https://creativecommons.org/licenses/by/4.0/legalcode
op_doi https://doi.org/10.5281/zenodo.828305310.5281/zenodo.8283052
_version_ 1810495544598986752

Similar Items