2022
DOI: 10.1016/j.scitotenv.2021.150271
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Characterization of precipitation and recharge in the peripheral aquifer of the Salar de Atacama

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Cited by 10 publications
(8 citation statements)
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“…Tracking water flows beyond the plants and soils can build on these insights (te Wierik et al., 2021). To track the flows of moisture in the atmosphere, isotopes can also play a role (e.g., Valdivielso et al., 2024). However, interpreting the isotopic composition of atmospheric moisture is challenging because of atmosphere mixing and fractionation during condensation and (re‐) evaporation (e.g., Sun et al., 2024).…”
Section: Discussionmentioning
confidence: 99%
“…Tracking water flows beyond the plants and soils can build on these insights (te Wierik et al., 2021). To track the flows of moisture in the atmosphere, isotopes can also play a role (e.g., Valdivielso et al., 2024). However, interpreting the isotopic composition of atmospheric moisture is challenging because of atmosphere mixing and fractionation during condensation and (re‐) evaporation (e.g., Sun et al., 2024).…”
Section: Discussionmentioning
confidence: 99%
“…The distribution of isotopic precipitation samples is heterogeneous in time, space and type of sample. Specific rain samples are taken in the basin, and permanent rain collectors are installed close to automatic meteorological stations 91 . Isotopic samples are mostly collected during the summer months (January, February and March) since this is the period containing important precipitation events (during the so-called "Altiplanic winter").…”
Section: Application To the Example Of Salar De Atacamamentioning
confidence: 99%
“…The climate of Salar de Atacama is hyperarid because of the geographical barrier that the Andean range represents to the humid air masses coming from Amazonia [20]. The annual precipitation ranges from 20 mm/year in the nucleus to 160 mm/year in the eastern summits and presents a clear seasonal cyclicity [20,21]. Most of the annual precipitation (87%) occurs during the austral summer (December-March), when the more intense easterly winds bring humid air masses coming from the Atlantic Ocean via Amazonia and the Gran Chaco [21].…”
Section: Case Studymentioning
confidence: 99%
“…The annual precipitation ranges from 20 mm/year in the nucleus to 160 mm/year in the eastern summits and presents a clear seasonal cyclicity [20,21]. Most of the annual precipitation (87%) occurs during the austral summer (December-March), when the more intense easterly winds bring humid air masses coming from the Atlantic Ocean via Amazonia and the Gran Chaco [21]. In addition to the altitudinal gradient, this precipitation also presents a latitudinal gradient decreasing from north to south due to the shadow effect of the Andes [22].…”
Section: Case Studymentioning
confidence: 99%
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