For 1980–2024, circulation-induced dynamics account for 45% of summer warming, dominate the European precipitation decline, and account for
type: CreativeWork
type: ScholarlyArticle
type: Claim
type: RA
abstract: For 1980–2024, circulation-induced dynamics account for 45% of summer warming, dominate the European precipitation decline, and account for 55% of continental soil-moisture drying, with particularly large regional shares.
text: For 1980–2024, circulation-induced dynamics account for 45% of summer warming, dominate the European precipitation decline, and account for 55% of continental soil-moisture drying, with particularly large regional shares.
date created: 2026-07-26T05:57:57.258Z
date published: 2026-07-26T05:57:57.258Z
date modified: 2026-07-26T05:57:57.258Z
author: Paper Reconstruction Agent
publisher: Isonomia
is part of: Paper reconstruction — Dunkl, Bastos & Sippel (2026), European summer drying
has conclusion: https://www.isonomia.app/c/9f1c37dd3270609bb1265228dcae155d622bd0cae79138000897a5875a42f1f7
has premise: https://www.isonomia.app/c/ccd6befe27317624468389ea6f5a9a4f363982085eba3eb4c615a44f0ddaaec6
has premise: https://www.isonomia.app/c/f6bc4a951b0bedc108826553c6ce813cbbc38b0ee5df99d6e107e8951fe4c36a
has premise: https://www.isonomia.app/c/967db0d559bfa0779121d1e95b402e032851195f4dc7c72d52f56c4cf9fcef1a
has premise: https://www.isonomia.app/c/364b930b1c08dbe59dfe38ecd467228c42d8ee807a91ed0113a0f30f9fdfb936
uses scheme: Causal (If cause then effect)
applies scheme key: causal
dialectical status: PropertyValue
  incoming attacks: 2
  incoming attack edges: 2
  incoming supports: 0
  critical questions required: 2
  critical questions answered: 0
  critical questions open: 2
  standing score: 0.1
  is tested: false
attestation: PropertyValue
  permalink: For 1980–2024, circulation-induced dynamics account for 45% of summer warming, dominate the European precipitation decline, and account for
  immutable permalink: https://www.isonomia.app/a/AdCkM2P5@53acaef680d1088345331b59383f29d81535c870c2ff52e04523bfc6ab8e0cc3
  version: 1
  retrieved at: 2026-08-24T19:45:11.643Z

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Paper reconstruction — Dunkl, Bastos & Sippel (2026), European summer drying
type: CreativeWork

https://www.isonomia.app/c/9f1c37dd3270609bb1265228dcae155d622bd0cae79138000897a5875a42f1f7
type: Claim
type: InformationNode
text: For 1980–2024, circulation-induced dynamics account for 45% of summer warming, dominate the European precipitation decline, and account for 55% of continental soil-moisture drying, with particularly large regional shares.

https://www.isonomia.app/c/ccd6befe27317624468389ea6f5a9a4f363982085eba3eb4c615a44f0ddaaec6
type: Claim
type: InformationNode
text: Dynamic soil-moisture trends closely correspond spatially to dynamic precipitation trends (Pearson correlation = 0.80), indicating precipitation trends drive much of the overall drying pattern.

https://www.isonomia.app/c/f6bc4a951b0bedc108826553c6ce813cbbc38b0ee5df99d6e107e8951fe4c36a
type: Claim
type: InformationNode
text: From 1980 to 2024, warming is 0.64 °C per decade in HIST and 0.29 °C per decade in NAT, so the circulation-induced component accounts for 45% of total summer warming.

https://www.isonomia.app/c/967db0d559bfa0779121d1e95b402e032851195f4dc7c72d52f56c4cf9fcef1a
type: Claim
type: InformationNode
text: European precipitation declines by −0.028 mm d−1 per decade through the dynamic component, while the thermodynamic component offsets this drying by only 6% (0.002 mm d−1 per decade).

https://www.isonomia.app/c/364b930b1c08dbe59dfe38ecd467228c42d8ee807a91ed0113a0f30f9fdfb936
type: Claim
type: InformationNode
text: Soil moisture declines by −0.41 mm per decade in HIST and −0.23 mm per decade in NAT, implying a 55% dynamic contribution.

Causal (If cause then effect)
type: DefinedTerm
type: Scheme
term code: causal