Circulation-induced warm and dry conditions amplify PD-versus-NAT thermodynamic soil-moisture and VPD drying, whereas cold and wet condition
type: CreativeWork
type: ScholarlyArticle
type: Claim
type: RA
abstract: Circulation-induced warm and dry conditions amplify PD-versus-NAT thermodynamic soil-moisture and VPD drying, whereas cold and wet conditions and more frequent heavy precipitation mitigate it.
text: Circulation-induced warm and dry conditions amplify PD-versus-NAT thermodynamic soil-moisture and VPD drying, whereas cold and wet conditions and more frequent heavy precipitation mitigate it.
date created: 2026-07-26T05:58:22.133Z
date published: 2026-07-26T05:58:22.133Z
date modified: 2026-07-26T05:58:22.133Z
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/d23d6159cd9b1ac46875acd0c0c99e1099d903218301ed96299ccccb0cecc86b
has premise: https://www.isonomia.app/c/c0b9f082a8fda004abf817ea92732d14595f61e356197cf8703eb2a57e8f503f
has premise: https://www.isonomia.app/c/fe2df9c6f96d9cf547f58deeb0f0e743948984e5632f82b0af69f5a3952ec837
has premise: https://www.isonomia.app/c/6ccb6bfe34f8d593efd30fb3fbf6675ae34171546550f3f93f14ec8a159ede75
has premise: https://www.isonomia.app/c/3816f80eb0572ad791ae42bd5272ecd2f435736d42e3b6372214324f6f4d9a06
uses scheme: Causal (If cause then effect)
applies scheme key: causal
dialectical status: PropertyValue
  incoming attacks: 0
  incoming attack edges: 0
  incoming supports: 0
  critical questions required: 2
  critical questions answered: 0
  critical questions open: 2
  standing score: 0.5
  is tested: false
attestation: PropertyValue
  permalink: Circulation-induced warm and dry conditions amplify PD-versus-NAT thermodynamic soil-moisture and VPD drying, whereas cold and wet condition
  immutable permalink: https://www.isonomia.app/a/NL3Fw4Ei@d2b8e51516889bd420aa20f35c7b7f5548a65d101002fadcef63f5ff41a38262
  version: 1
  retrieved at: 2026-08-24T19:52:38.093Z

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

https://www.isonomia.app/c/d23d6159cd9b1ac46875acd0c0c99e1099d903218301ed96299ccccb0cecc86b
type: Claim
type: InformationNode
text: Circulation-induced warm and dry conditions amplify PD-versus-NAT thermodynamic soil-moisture and VPD drying, whereas cold and wet conditions and more frequent heavy precipitation mitigate it.

https://www.isonomia.app/c/c0b9f082a8fda004abf817ea92732d14595f61e356197cf8703eb2a57e8f503f
type: Claim
type: InformationNode
text: Under constant PD and NAT forcing, the thermodynamic soil-moisture difference varies substantially from year to year, ranging from −0.39 to −1.00 mm around a −0.72 mm JJA mean difference.

https://www.isonomia.app/c/fe2df9c6f96d9cf547f58deeb0f0e743948984e5632f82b0af69f5a3952ec837
type: Claim
type: InformationNode
text: For every millimetre of negative circulation-induced soil-moisture anomaly, PD has an additional 0.08 mm of drying relative to NAT, an 8% positive amplification effect.

https://www.isonomia.app/c/6ccb6bfe34f8d593efd30fb3fbf6675ae34171546550f3f93f14ec8a159ede75
type: Claim
type: InformationNode
text: Across the domain, circulation-induced summer soil-moisture conditions and the thermodynamic soil-moisture component (PD–NAT) have a significant positive correlation of 0.62.

https://www.isonomia.app/c/3816f80eb0572ad791ae42bd5272ecd2f435736d42e3b6372214324f6f4d9a06
type: Claim
type: InformationNode
text: Even with constant forcing in PD and NAT, the thermodynamic soil-moisture difference varies substantially from year to year: its mean is −0.72 mm, with annual differences from −0.39 to −1.00 mm.

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