Modelling the Interactions in Paleoclimate Data from Ice Cores

This paper considers methods for testing directions of causation in the paleoclimate series for temperature and CO2 concentration derived from Antarctic ice cores from 800,000 years BP. These series are well-known to move together in the transitions between glacial and interglacial periods, but the...

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Main Authors: James Davidson, Alemtsehai Turasie
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Published: 2013
Subjects:
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.364.6869
http://people.exeter.ac.uk/jehd201/paleoclimate.pdf
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spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.364.6869 2023-05-15T14:05:28+02:00 Modelling the Interactions in Paleoclimate Data from Ice Cores James Davidson Alemtsehai Turasie The Pennsylvania State University CiteSeerX Archives 2013 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.364.6869 http://people.exeter.ac.uk/jehd201/paleoclimate.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.364.6869 http://people.exeter.ac.uk/jehd201/paleoclimate.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://people.exeter.ac.uk/jehd201/paleoclimate.pdf text 2013 ftciteseerx 2016-01-08T00:59:38Z This paper considers methods for testing directions of causation in the paleoclimate series for temperature and CO2 concentration derived from Antarctic ice cores from 800,000 years BP. These series are well-known to move together in the transitions between glacial and interglacial periods, but the dynamic relationship between the series is open to dispute. Bivariate models are constructed, in the context of which we perform tests for Granger causality, or in other words for asymmetry in the pattern of dynamic interactions. An important question is the stationarity of the series, because di¤erent statistical techniques are called for in stationary and integrated models. Previous work with climate data has focused on a cointegration approach appropriate to integrated series, but a range of tests show no evidence of integrated behaviour in these seres. A second important question is linearity, whether the dynamics in mean can be adequately represented by a high-order vector autoregressive process. This modelling approach is compared with a nonlinear Markov switching mechanism, in which the glacial/interglacial switches are controlled by a common hidden discrete process with …xed conditional probabilities of changes of state. A further characteristic of the data that comes to light is pronounced conditional heteroscedasticity, with much larger disturbances in evidence around the glacial/interglacial transitions.This data feature is e¤ectively accounted for by …tting a GARCH component. 1 Text Antarc* Antarctic Unknown Antarctic
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description This paper considers methods for testing directions of causation in the paleoclimate series for temperature and CO2 concentration derived from Antarctic ice cores from 800,000 years BP. These series are well-known to move together in the transitions between glacial and interglacial periods, but the dynamic relationship between the series is open to dispute. Bivariate models are constructed, in the context of which we perform tests for Granger causality, or in other words for asymmetry in the pattern of dynamic interactions. An important question is the stationarity of the series, because di¤erent statistical techniques are called for in stationary and integrated models. Previous work with climate data has focused on a cointegration approach appropriate to integrated series, but a range of tests show no evidence of integrated behaviour in these seres. A second important question is linearity, whether the dynamics in mean can be adequately represented by a high-order vector autoregressive process. This modelling approach is compared with a nonlinear Markov switching mechanism, in which the glacial/interglacial switches are controlled by a common hidden discrete process with …xed conditional probabilities of changes of state. A further characteristic of the data that comes to light is pronounced conditional heteroscedasticity, with much larger disturbances in evidence around the glacial/interglacial transitions.This data feature is e¤ectively accounted for by …tting a GARCH component. 1
author2 The Pennsylvania State University CiteSeerX Archives
format Text
author James Davidson
Alemtsehai Turasie
spellingShingle James Davidson
Alemtsehai Turasie
Modelling the Interactions in Paleoclimate Data from Ice Cores
author_facet James Davidson
Alemtsehai Turasie
author_sort James Davidson
title Modelling the Interactions in Paleoclimate Data from Ice Cores
title_short Modelling the Interactions in Paleoclimate Data from Ice Cores
title_full Modelling the Interactions in Paleoclimate Data from Ice Cores
title_fullStr Modelling the Interactions in Paleoclimate Data from Ice Cores
title_full_unstemmed Modelling the Interactions in Paleoclimate Data from Ice Cores
title_sort modelling the interactions in paleoclimate data from ice cores
publishDate 2013
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.364.6869
http://people.exeter.ac.uk/jehd201/paleoclimate.pdf
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genre_facet Antarc*
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http://people.exeter.ac.uk/jehd201/paleoclimate.pdf
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