Millennial timescale carbon cycle and climate change in an efficient Earth system model

A new Earth system model, GENIE-1, is presented which comprises a 3-D frictional geostrophic ocean, phosphate-restoring marine biogeochemistry, dynamic and thermodynamic sea-ice, land surface physics and carbon cycling, and a seasonal 2-D energy-moisture balance atmosphere. Three sets of model clima...

Full description

Bibliographic Details
Published in:Climate Dynamics
Main Authors: Lenton, T.M., Williamson, M.S., Edwards, N.R., Marsh, R., Price, A.R., Ridgwell, A.J., Shepherd, J.G., Cox, S.J.
Format: Article in Journal/Newspaper
Language:English
Published: 2006
Subjects:
Online Access:https://eprints.soton.ac.uk/26700/
https://eprints.soton.ac.uk/26700/1/lent_06.pdf
id ftsouthampton:oai:eprints.soton.ac.uk:26700
record_format openpolar
spelling ftsouthampton:oai:eprints.soton.ac.uk:26700 2023-07-30T04:03:50+02:00 Millennial timescale carbon cycle and climate change in an efficient Earth system model Lenton, T.M. Williamson, M.S. Edwards, N.R. Marsh, R. Price, A.R. Ridgwell, A.J. Shepherd, J.G. Cox, S.J. 2006 text https://eprints.soton.ac.uk/26700/ https://eprints.soton.ac.uk/26700/1/lent_06.pdf en eng https://eprints.soton.ac.uk/26700/1/lent_06.pdf Lenton, T.M., Williamson, M.S., Edwards, N.R., Marsh, R., Price, A.R., Ridgwell, A.J., Shepherd, J.G. and Cox, S.J. (2006) Millennial timescale carbon cycle and climate change in an efficient Earth system model. Climate Dynamics, 26 (7-8), 687-711. (doi:10.1007/s00382-006-0109-9 <http://dx.doi.org/10.1007/s00382-006-0109-9>). Article PeerReviewed 2006 ftsouthampton https://doi.org/10.1007/s00382-006-0109-9 2023-07-09T20:41:02Z A new Earth system model, GENIE-1, is presented which comprises a 3-D frictional geostrophic ocean, phosphate-restoring marine biogeochemistry, dynamic and thermodynamic sea-ice, land surface physics and carbon cycling, and a seasonal 2-D energy-moisture balance atmosphere. Three sets of model climate parameters are used to explore the robustness of the results and for traceability to earlier work. The model versions have climate sensitivity of 2.8–3.3°C and predict atmospheric CO2 close to present observations. Six idealized total fossil fuel CO2 emissions scenarios are used to explore a range of 1,100–15,000 GtC total emissions and the effect of rate of emissions. Atmospheric CO2 approaches equilibrium in year 3000 at 420–5,660 ppmv, giving 1.5–12.5°C global warming. The ocean is a robust carbon sink of up to 6.5 GtC year?1. Under ‘business as usual’, the land becomes a carbon source around year 2100 which peaks at up to 2.5 GtC year?1. Soil carbon is lost globally, boreal vegetation generally increases, whilst under extreme forcing, dieback of some tropical and sub-tropical vegetation occurs. Average ocean surface pH drops by up to 1.15 units. A Greenland ice sheet melt threshold of 2.6°C local warming is only briefly exceeded if total emissions are limited to 1,100 GtC, whilst 15,000 GtC emissions cause complete Greenland melt by year 3000, contributing 7 m to sea level rise. Total sea-level rise, including thermal expansion, is 0.4–10 m in year 3000 and ongoing. The Atlantic meridional overturning circulation shuts down in two out of three model versions, but only under extreme emissions including exotic fossil fuel resources. Article in Journal/Newspaper Greenland Ice Sheet Sea ice University of Southampton: e-Prints Soton Greenland Climate Dynamics 26 7-8 687 711
institution Open Polar
collection University of Southampton: e-Prints Soton
op_collection_id ftsouthampton
language English
description A new Earth system model, GENIE-1, is presented which comprises a 3-D frictional geostrophic ocean, phosphate-restoring marine biogeochemistry, dynamic and thermodynamic sea-ice, land surface physics and carbon cycling, and a seasonal 2-D energy-moisture balance atmosphere. Three sets of model climate parameters are used to explore the robustness of the results and for traceability to earlier work. The model versions have climate sensitivity of 2.8–3.3°C and predict atmospheric CO2 close to present observations. Six idealized total fossil fuel CO2 emissions scenarios are used to explore a range of 1,100–15,000 GtC total emissions and the effect of rate of emissions. Atmospheric CO2 approaches equilibrium in year 3000 at 420–5,660 ppmv, giving 1.5–12.5°C global warming. The ocean is a robust carbon sink of up to 6.5 GtC year?1. Under ‘business as usual’, the land becomes a carbon source around year 2100 which peaks at up to 2.5 GtC year?1. Soil carbon is lost globally, boreal vegetation generally increases, whilst under extreme forcing, dieback of some tropical and sub-tropical vegetation occurs. Average ocean surface pH drops by up to 1.15 units. A Greenland ice sheet melt threshold of 2.6°C local warming is only briefly exceeded if total emissions are limited to 1,100 GtC, whilst 15,000 GtC emissions cause complete Greenland melt by year 3000, contributing 7 m to sea level rise. Total sea-level rise, including thermal expansion, is 0.4–10 m in year 3000 and ongoing. The Atlantic meridional overturning circulation shuts down in two out of three model versions, but only under extreme emissions including exotic fossil fuel resources.
format Article in Journal/Newspaper
author Lenton, T.M.
Williamson, M.S.
Edwards, N.R.
Marsh, R.
Price, A.R.
Ridgwell, A.J.
Shepherd, J.G.
Cox, S.J.
spellingShingle Lenton, T.M.
Williamson, M.S.
Edwards, N.R.
Marsh, R.
Price, A.R.
Ridgwell, A.J.
Shepherd, J.G.
Cox, S.J.
Millennial timescale carbon cycle and climate change in an efficient Earth system model
author_facet Lenton, T.M.
Williamson, M.S.
Edwards, N.R.
Marsh, R.
Price, A.R.
Ridgwell, A.J.
Shepherd, J.G.
Cox, S.J.
author_sort Lenton, T.M.
title Millennial timescale carbon cycle and climate change in an efficient Earth system model
title_short Millennial timescale carbon cycle and climate change in an efficient Earth system model
title_full Millennial timescale carbon cycle and climate change in an efficient Earth system model
title_fullStr Millennial timescale carbon cycle and climate change in an efficient Earth system model
title_full_unstemmed Millennial timescale carbon cycle and climate change in an efficient Earth system model
title_sort millennial timescale carbon cycle and climate change in an efficient earth system model
publishDate 2006
url https://eprints.soton.ac.uk/26700/
https://eprints.soton.ac.uk/26700/1/lent_06.pdf
geographic Greenland
geographic_facet Greenland
genre Greenland
Ice Sheet
Sea ice
genre_facet Greenland
Ice Sheet
Sea ice
op_relation https://eprints.soton.ac.uk/26700/1/lent_06.pdf
Lenton, T.M., Williamson, M.S., Edwards, N.R., Marsh, R., Price, A.R., Ridgwell, A.J., Shepherd, J.G. and Cox, S.J. (2006) Millennial timescale carbon cycle and climate change in an efficient Earth system model. Climate Dynamics, 26 (7-8), 687-711. (doi:10.1007/s00382-006-0109-9 <http://dx.doi.org/10.1007/s00382-006-0109-9>).
op_doi https://doi.org/10.1007/s00382-006-0109-9
container_title Climate Dynamics
container_volume 26
container_issue 7-8
container_start_page 687
op_container_end_page 711
_version_ 1772814959057567744