dorsal/arxiv
View SchemaStructural Cointegration of the Paleoclimate: Estimating Earth System Sensitivity
| Authors | Satoshi Nakano, Kazuhiko Nishimura |
|---|---|
| Categories | |
| ArXiv ID | 2601.06986vv1 |
| URL | https://arxiv.org/abs/2601.06986 |
| License | http://arxiv.org/licenses/nonexclusive-distrib/1.0/ |
Abstract
Understanding the long-term relationship between atmospheric $CO_2$ and global temperature is fundamental to assessing Earth's climate sensitivity. This study applies a Structural Vector Error Correction Model (SVECM) to paleoclimate records from the EPICA Dome C and Vostok ice cores, spanning the last 800,000 years. By leveraging the statistical property of cointegration, we identify a robust, long-term equilibrium relationship between temperature and log-transformed $CO_2$ concentrations while controlling for orbital forcing ($N60J$). Our results, based on 854 observations, reveal a strong causal link with a long-term coefficient ($\beta$) of 17.30, characterized by a high level of statistical significance ($z = -3.82$). This corresponds to an Earth System Sensitivity (ESS) of approximately 12.0$^\circ$C per doubling of $CO_2$. Forecast Error Variance Decomposition (FEVD) further demonstrates that $CO_2$ shocks account for approximately 40\% of the long-term temperature variance.
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"abstract": "Understanding the long-term relationship between atmospheric $CO_2$ and global temperature is fundamental to assessing Earth\u0027s climate sensitivity. This study applies a Structural Vector Error Correction Model (SVECM) to paleoclimate records from the EPICA Dome C and Vostok ice cores, spanning the last 800,000 years. By leveraging the statistical property of cointegration, we identify a robust, long-term equilibrium relationship between temperature and log-transformed $CO_2$ concentrations while controlling for orbital forcing ($N60J$). Our results, based on 854 observations, reveal a strong causal link with a long-term coefficient ($\\beta$) of 17.30, characterized by a high level of statistical significance ($z = -3.82$). This corresponds to an Earth System Sensitivity (ESS) of approximately 12.0$^\\circ$C per doubling of $CO_2$. Forecast Error Variance Decomposition (FEVD) further demonstrates that $CO_2$ shocks account for approximately 40\\% of the long-term temperature variance.",
"arxiv_id": "2601.06986",
"authors": [
"Satoshi Nakano",
"Kazuhiko Nishimura"
],
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"physics.ao-ph"
],
"license": "http://arxiv.org/licenses/nonexclusive-distrib/1.0/",
"title": "Structural Cointegration of the Paleoclimate: Estimating Earth System Sensitivity",
"url": "https://arxiv.org/abs/2601.06986",
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