---
res:
  bibo_abstract:
  - Transpiration (T) connects water, energy, and carbon cycles within ecosystems.
    While T has often been reported to increase with soil warming, underlying reasons
    remain poorly understood. Here, using a mechanistic ecohydrological model, T&C‐BG,
    we simulated T responses to soil warming at 30 sites spanning various biomes and
    climates. Consistent with observations, the numerical model reproduces negative,
    insignificant, and predominantly positive T responses under soil warming. Numerical
    results show that soil warming generally increases T for sites with a small Bowen
    ratio. The main mechanisms leading to positive T responses to soil warming are
    complex changes in energy partitioning with modifications of canopy surface temperature
    and aerodynamic, stomatal, and leaf boundary layer conductance. However, soil
    warming can also affect phenology, which might result in either increased or decreased
    T. Our findings shed light on how T changes with warmer soil and help interpret
    outcomes of warming experiments.@eng
  bibo_authorlist:
  - foaf_Person:
      foaf_givenName: Zhaoyang
      foaf_name: Luo, Zhaoyang
      foaf_surname: Luo
  - foaf_Person:
      foaf_givenName: Jianning
      foaf_name: Ren, Jianning
      foaf_surname: Ren
  - foaf_Person:
      foaf_givenName: Qi
      foaf_name: Zhuang, Qi
      foaf_surname: Zhuang
  - foaf_Person:
      foaf_givenName: Simone
      foaf_name: Fatichi, Simone
      foaf_surname: Fatichi
      foaf_workInfoHomepage: http://www.librecat.org/personId=cf8e546b-a9b0-11f0-a43b-aa89ed1b56d6
  bibo_doi: 10.1029/2025gl120046
  bibo_issue: '8'
  bibo_volume: 53
  dct_date: 2026^xs_gYear
  dct_isPartOf:
  - http://id.crossref.org/issn/0094-8276
  - http://id.crossref.org/issn/1944-8007
  dct_language: eng
  dct_publisher: American Geophysical Union@
  dct_title: 'Transpiration changes with soil warming: Insights from a mechanistic
    model@'
...