Constraining ocean diffusivity from the 8.2 ka event

Greenland ice-core data containing the 8.2 ka event are utilized by a model-data intercomparison within the Earth system model of intermediate complexity, CLIMBER-2.3 to investigate their potential for constraining the range of uncertain ocean diffusivity properties. Within a stochastic version of t...

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Main Authors: Lorenz, A., Held, H., Bauer, E., von Deimling, T.S.
Format: Article in Journal/Newspaper
Language:English
Published: Berlin : Springer Verlag 2010
Subjects:
Online Access:https://oa.tib.eu/renate/handle/123456789/5451
https://doi.org/10.34657/4080
id fttibhannoverren:oai:oa.tib.eu:123456789/5451
record_format openpolar
spelling fttibhannoverren:oai:oa.tib.eu:123456789/5451 2023-05-15T15:11:06+02:00 Constraining ocean diffusivity from the 8.2 ka event Lorenz, A. Held, H. Bauer, E. von Deimling, T.S. 2010 application/pdf text/plain; charset=utf-8 https://oa.tib.eu/renate/handle/123456789/5451 https://doi.org/10.34657/4080 eng eng Berlin : Springer Verlag ISSN:0930-7575 DOI:https://doi.org/10.1007/s00382-009-0590-z https://doi.org/10.34657/4080 https://oa.tib.eu/renate/handle/123456789/5451 CC BY-NC 2.0 Unported https://creativecommons.org/licenses/by-nc/2.0/ frei zugänglich CC-BY-NC Climate Dynamics 34 (2010), Nr. 5 8.2 ka event Bayesian analysis Ocean diffusivity Paleo data Uncertainty diffusivity hydrogeochemistry ice core numerical model stochasticity uncertainty analysis Arctic Greenland ddc:550 status-type:publishedVersion doc-type:article doc-type:Text 2010 fttibhannoverren https://doi.org/10.34657/4080 https://doi.org/10.1007/s00382-009-0590-z 2022-05-07T06:45:23Z Greenland ice-core data containing the 8.2 ka event are utilized by a model-data intercomparison within the Earth system model of intermediate complexity, CLIMBER-2.3 to investigate their potential for constraining the range of uncertain ocean diffusivity properties. Within a stochastic version of the model (Bauer et al. in Paleoceanography 19:PA3014, 2004) it has been possible to mimic the pronounced cooling of the 8.2 ka event with relatively good accuracy considering the timing of the event in comparison to other modelling exercises. When statistically inferring from the 8.2 ka event on diffusivity the technical difficulty arises to establish the related likelihood numerically per realisation of the uncertain model parameters: while mainstream uncertainty analyses can assume a quasi-Gaussian shape of likelihood, with weather fluctuating around a long term mean, the 8.2 ka event as a highly nonlinear effect precludes such an a priori assumption. As a result of this study the Bayesian Analysis leads to a sharp single-mode likelihood for ocean diffusivity parameters within CLIMBER-2.3. Depending on the prior distribution this likelihood leads to a reduction of uncertainty in ocean diffusivity parameters (e. g. for flat prior uncertainty in the vertical ocean diffusivity parameter is reduced by factor 2). These results highlight the potential of paleo data to constrain uncertain system properties and strongly suggest to make further steps with more complex models and richer data sets to harvest this potential. © The Author(s) 2009. Article in Journal/Newspaper Arctic Greenland Greenland ice core ice core Renate - Repositorium für Naturwissenschaften und Technik (TIB Hannover) Arctic Greenland
institution Open Polar
collection Renate - Repositorium für Naturwissenschaften und Technik (TIB Hannover)
op_collection_id fttibhannoverren
language English
topic 8.2 ka event
Bayesian analysis
Ocean diffusivity
Paleo data
Uncertainty
diffusivity
hydrogeochemistry
ice core
numerical model
stochasticity
uncertainty analysis
Arctic
Greenland
ddc:550
spellingShingle 8.2 ka event
Bayesian analysis
Ocean diffusivity
Paleo data
Uncertainty
diffusivity
hydrogeochemistry
ice core
numerical model
stochasticity
uncertainty analysis
Arctic
Greenland
ddc:550
Lorenz, A.
Held, H.
Bauer, E.
von Deimling, T.S.
Constraining ocean diffusivity from the 8.2 ka event
topic_facet 8.2 ka event
Bayesian analysis
Ocean diffusivity
Paleo data
Uncertainty
diffusivity
hydrogeochemistry
ice core
numerical model
stochasticity
uncertainty analysis
Arctic
Greenland
ddc:550
description Greenland ice-core data containing the 8.2 ka event are utilized by a model-data intercomparison within the Earth system model of intermediate complexity, CLIMBER-2.3 to investigate their potential for constraining the range of uncertain ocean diffusivity properties. Within a stochastic version of the model (Bauer et al. in Paleoceanography 19:PA3014, 2004) it has been possible to mimic the pronounced cooling of the 8.2 ka event with relatively good accuracy considering the timing of the event in comparison to other modelling exercises. When statistically inferring from the 8.2 ka event on diffusivity the technical difficulty arises to establish the related likelihood numerically per realisation of the uncertain model parameters: while mainstream uncertainty analyses can assume a quasi-Gaussian shape of likelihood, with weather fluctuating around a long term mean, the 8.2 ka event as a highly nonlinear effect precludes such an a priori assumption. As a result of this study the Bayesian Analysis leads to a sharp single-mode likelihood for ocean diffusivity parameters within CLIMBER-2.3. Depending on the prior distribution this likelihood leads to a reduction of uncertainty in ocean diffusivity parameters (e. g. for flat prior uncertainty in the vertical ocean diffusivity parameter is reduced by factor 2). These results highlight the potential of paleo data to constrain uncertain system properties and strongly suggest to make further steps with more complex models and richer data sets to harvest this potential. © The Author(s) 2009.
format Article in Journal/Newspaper
author Lorenz, A.
Held, H.
Bauer, E.
von Deimling, T.S.
author_facet Lorenz, A.
Held, H.
Bauer, E.
von Deimling, T.S.
author_sort Lorenz, A.
title Constraining ocean diffusivity from the 8.2 ka event
title_short Constraining ocean diffusivity from the 8.2 ka event
title_full Constraining ocean diffusivity from the 8.2 ka event
title_fullStr Constraining ocean diffusivity from the 8.2 ka event
title_full_unstemmed Constraining ocean diffusivity from the 8.2 ka event
title_sort constraining ocean diffusivity from the 8.2 ka event
publisher Berlin : Springer Verlag
publishDate 2010
url https://oa.tib.eu/renate/handle/123456789/5451
https://doi.org/10.34657/4080
geographic Arctic
Greenland
geographic_facet Arctic
Greenland
genre Arctic
Greenland
Greenland ice core
ice core
genre_facet Arctic
Greenland
Greenland ice core
ice core
op_source Climate Dynamics 34 (2010), Nr. 5
op_relation ISSN:0930-7575
DOI:https://doi.org/10.1007/s00382-009-0590-z
https://doi.org/10.34657/4080
https://oa.tib.eu/renate/handle/123456789/5451
op_rights CC BY-NC 2.0 Unported
https://creativecommons.org/licenses/by-nc/2.0/
frei zugänglich
op_rightsnorm CC-BY-NC
op_doi https://doi.org/10.34657/4080
https://doi.org/10.1007/s00382-009-0590-z
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