The Climate Deep: Tipping Cascades, Stranded Assets, and the Joint Topology of Physical and Financial Risk
気候の深層:ティッピングカスケード、座礁資産、物理的リスクと金融リスクの結合位相 (AI 翻訳)
Buckley, Ian R. C.
🤖 gxceed AI 要約
日本語
本論文は、気候変動と金融リスクの相互作用を位相幾何学(層係数コホモロジー)を用いて理論化する。TCFDやNGFSが扱う個別リスクでは捉えられない「気候の深層」と呼ばれる結合サイクルが存在し、個別に管理可能なシステムでも結合部で解決不能な対立サイクルが生じることを示す。座礁資産の具体例を通じて、既存の規制では対応できないため、超国家的な解決機関が必要と主張する。
English
This paper theorizes the interaction between climate and financial risk using sheaf cohomology. It argues that TCFD and NGFS treat climate risk as an input, missing the coupling topology that creates irresolvable conflict cycles ('Climate Deep'). Using stranded assets as an example, it shows that individually manageable systems can form globally unresolvable cycles, requiring a supranational resolution authority.
Unofficial AI-generated summary based on the public title and abstract. Not an official translation.
📝 gxceed 編集解説 — Why this matters
日本のGX文脈において
日本ではSSBJ開示や有報での気候関連情報開示が進むが、本論文は開示の枠組みを超えたシステムレベルのリスクを提起。金融庁や日銀のストレステスト設計に示唆を与えるが、実務適用には距離がある。
In the global GX context
This paper challenges the global climate-finance regulatory paradigm (TCFD, NGFS, ECB scenarios) by arguing that coupling effects create unresolvable conflict cycles. It offers a novel theoretical lens for transition risk and stranded assets, relevant to ISSB and transition finance discussions, though it lacks empirical validation.
👥 読者別の含意
🔬研究者:Provides a novel topological framework for climate-finance coupling, opening new research directions in systemic risk.
🏢実務担当者:Limited direct applicability; may inform scenario analysis design but lacks operational guidance.
🏛政策担当者:Highlights the need for supranational coordination beyond current instruments like the Paris Agreement.
📄 Abstract(原文)
Current climate-finance regulation — TCFD scenario analysis, NGFS stress tests, ECB climate scenarios — treats climate risk as an input to financial risk: a scenario that stresses asset values. It does not model the coupling topology: the feedback between the physical climate system and the financial obligation network. This feedback creates irresolvable conflict cycles — the Climate Deep — that are invisible to both climate modellers (who treat finance as exogenous) and financial regulators (who treat climate as a scenario). This paper extends the Deep Framework (Islands/$H^0$, Flatland/$H^1$, The Deep/$H^2$) to the joint climate-finance system. The three strata become: Islands risk ($H^0$), the physical viability of assets under climate change (stranded assets, physical damage), partially addressed by TCFD and NGFS; Flatland risk ($H^1$), the carbon and supply-chain loops that couple financial flows to emissions (fossil fuel debt, transition loops), addressed by carbon pricing and supply-chain due diligence but not their network topology; and the Climate Deep ($H^2$), tipping cascade conflict cycles — the irresolvable interactions between climate tipping elements and financial obligations that no bilateral instrument can resolve. The central result is the Climate-Finance Coupling Theorem : $H^2(\mathcal{F}_{\mathrm{climate}} \times \mathcal{F}_{\mathrm{finance}})$ can be non-zero even when $H^2(\mathcal{F}_{\mathrm{climate}}) = 0$ and $H^2(\mathcal{F}_{\mathrm{finance}}) = 0$ separately. A conflict cycle can form at the coupling between two individually manageable systems. Managing financial obligations and climate outcomes separately — however rigorously — can still produce a globally irresolvable conflict cycle at the interface. The proof follows from the Mayer-Vietoris long exact sequence: the connecting homomorphism $\delta: H^1 \to H^2$ can be non-trivial even when both factors have trivial $H^2$. The canonical example is the stranded asset conflict cycle: fossil fuel revenues fund sovereign debt service ($A \to B$), sovereign carbon policy determines the rate of Amazonian deforestation ($B \to C$), and Amazonian tipping accelerates physical risk to the fossil fuel sector ($C \to A$). Each bilateral link is individually manageable; the triangle is not. Carney's three channels — physical, liability, and transition risk — map precisely onto the three strata: Islands, Flatland, and The Deep. Existing instruments address the first two. Transition risk at the network level is the Climate Deep, and no regulatory instrument currently measures or addresses it. The resolution instrument required to fill $H^2$ holes in the joint sheaf is a Level 6 supranational authority: an institution that can simultaneously restructure sovereign debt, fossil fuel obligations, and climate commitments. The Paris Agreement is the closest approximation — but it has no balance sheet, no enforcement mechanism, and cannot force the quadrilateral resolution that the Climate Deep requires. Companion papers: Beyond Basel — the Deep Framework for Systemic Risk Regulation (doi:10.5281/zenodo.20700006), Systemic Risk as $H^2$ (doi:10.5281/zenodo.20642908), Tipping Points are Topological (doi:10.5281/zenodo.20653285). Keywords : climate finance, tipping cascades, stranded assets, Deep Framework, sheaf cohomology, systemic risk, Tragedy of the Horizon, Mark Carney, TCFD, NGFS, Paris Agreement, Mayer-Vietoris, coupling theorem, Islands Flatland Deep, physical risk, transition risk, liability risk, supranational resolution, fossil fuel, sovereign debt
🔗 Provenance — このレコードを発見したソース
- Zenodo https://zenodo.org/records/20733943first seen 2026-06-18 04:15:23 · last seen 2026-07-01 04:17:42
- openalex https://doi.org/10.5281/zenodo.20733942first seen 2026-07-08 04:59:30 · last seen 2026-07-09 04:55:09
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