UNIVERSITY OF TORONTO
ii The carbon cycle model of Rothman et al. [2003] is modified by allowing temperature dependent photosynthetic and remineralization fluxes and through the introduction of a temperature dependent photosynthetic isotopic fractionation. The carbon model is then coupled to the energy balance/ice-sheet...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.547.1777 2023-05-15T16:40:53+02:00 UNIVERSITY OF TORONTO John Wilfrid Crowley J. W. Crowley The Pennsylvania State University CiteSeerX Archives 2006 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.547.1777 http://www.snowballearth.org/JWCrowley_Thesis.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.547.1777 http://www.snowballearth.org/JWCrowley_Thesis.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.snowballearth.org/JWCrowley_Thesis.pdf text 2006 ftciteseerx 2016-01-08T11:20:22Z ii The carbon cycle model of Rothman et al. [2003] is modified by allowing temperature dependent photosynthetic and remineralization fluxes and through the introduction of a temperature dependent photosynthetic isotopic fractionation. The carbon model is then coupled to the energy balance/ice-sheet model (EBM)/(ISM) of Peltier and Tarasov [1999]. Two major solutions are found. For a magnitude of the remineralization flux parameter of 0.0003 or less, a hysteresis loop forms in the temperature-dRad phase space with oscillations having a period controlled by the flux parameter and which can have glacial-interglacial timescales greater than 3Myr. When the magnitude of the remineralization flux parameter is greater than or equal to 0.0006, the system approaches an equilibrium state. There is a suggestion in the results of the simulation with the remineralization flux parameter set to 0.0006 that a Hard Snowball Earth state could exist for values of the flux parameter greater than 0.0006. Isotopic data for inorganic carbon is produced which matches data from the Neoproterozoic era Text Ice Sheet Unknown Peltier ENVELOPE(-63.495,-63.495,-64.854,-64.854) |
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ftciteseerx |
language |
English |
description |
ii The carbon cycle model of Rothman et al. [2003] is modified by allowing temperature dependent photosynthetic and remineralization fluxes and through the introduction of a temperature dependent photosynthetic isotopic fractionation. The carbon model is then coupled to the energy balance/ice-sheet model (EBM)/(ISM) of Peltier and Tarasov [1999]. Two major solutions are found. For a magnitude of the remineralization flux parameter of 0.0003 or less, a hysteresis loop forms in the temperature-dRad phase space with oscillations having a period controlled by the flux parameter and which can have glacial-interglacial timescales greater than 3Myr. When the magnitude of the remineralization flux parameter is greater than or equal to 0.0006, the system approaches an equilibrium state. There is a suggestion in the results of the simulation with the remineralization flux parameter set to 0.0006 that a Hard Snowball Earth state could exist for values of the flux parameter greater than 0.0006. Isotopic data for inorganic carbon is produced which matches data from the Neoproterozoic era |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
John Wilfrid Crowley J. W. Crowley |
spellingShingle |
John Wilfrid Crowley J. W. Crowley UNIVERSITY OF TORONTO |
author_facet |
John Wilfrid Crowley J. W. Crowley |
author_sort |
John Wilfrid Crowley |
title |
UNIVERSITY OF TORONTO |
title_short |
UNIVERSITY OF TORONTO |
title_full |
UNIVERSITY OF TORONTO |
title_fullStr |
UNIVERSITY OF TORONTO |
title_full_unstemmed |
UNIVERSITY OF TORONTO |
title_sort |
university of toronto |
publishDate |
2006 |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.547.1777 http://www.snowballearth.org/JWCrowley_Thesis.pdf |
long_lat |
ENVELOPE(-63.495,-63.495,-64.854,-64.854) |
geographic |
Peltier |
geographic_facet |
Peltier |
genre |
Ice Sheet |
genre_facet |
Ice Sheet |
op_source |
http://www.snowballearth.org/JWCrowley_Thesis.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.547.1777 http://www.snowballearth.org/JWCrowley_Thesis.pdf |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
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1766031304367800320 |