Local moisture recycling across the globe

Abstract ∘ (typically 50 km) of its source, identify variables that correlate with it over land globally, and study its model dependency. We derive the seasonal and annual LMR using a 10-year climatology (2008–2017) of monthly averaged atmospheric moisture connections at a scale of 0.5∘ obtained from a Lagrangian atmospheric moisture tracking model. We find that, annually, an average of 1.7 % (SD of 1.1 %) of evaporated moisture returns as precipitation locally, although with large temporal and spatial variability, and the LMR peaks in summer and over wet and mountainous regions. Our results show that wetness, orography, latitude, convective available potential energy, wind speed, and total cloud cover correlate clearly with the LMR, indicating that wet regions with little wind and strong ascending air are particularly favourable for a high LMR. Finally, we find that spatial patterns of local recycling are consistent between different models, yet the magnitude of recycling varies. Our results can be used to study the impacts of evaporation changes on local precipitation, with implications for, for example, regreening and water management.

Standort
Deutsche Nationalbibliothek Frankfurt am Main
Umfang
Online-Ressource
Sprache
Englisch

Erschienen in
Local moisture recycling across the globe ; volume:27 ; number:7 ; year:2023 ; pages:1457-1476 ; extent:20
Hydrology and earth system sciences ; 27, Heft 7 (2023), 1457-1476 (gesamt 20)

Urheber
Theeuwen, Jolanda J. E.
Staal, Arie
Tuinenburg, Obbe A.
Hamelers, Bert V. M.
Dekker, Stefan C.

DOI
10.5194/hess-27-1457-2023
URN
urn:nbn:de:101:1-2023040605164639608931
Rechteinformation
Open Access; Der Zugriff auf das Objekt ist unbeschränkt möglich.
Letzte Aktualisierung
14.08.2025, 10:49 MESZ

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Beteiligte

  • Theeuwen, Jolanda J. E.
  • Staal, Arie
  • Tuinenburg, Obbe A.
  • Hamelers, Bert V. M.
  • Dekker, Stefan C.

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