Cited by 413Climate variability and modelsHydrology and Drought AnalysisHydrology and Watershed Management Studies

Variability of precipitation in the Atacama Desert: its causes and hydrological impact

Houston, John·2006·International Journal of Climatology

Abstract

An analysis of the variability of rainfall at 27 stations and run-off at 4 stations between 18° and 28°S in the Atacama Desert has been carried out. A diagonal boundary zone between summer- and winter-dominated areas is related to the provenance of the rainfall: Amazonia to the north and east, and Pacific moisture to the south. It is shown that winter rainfall tends to be higher during El Niño years, while heavy summer rainfall tends to be more common during La Niña. However, rather than the precipitation being directly controlled by El Niño-Southern Oscillation (ENSO), previous studies have shown that it is the regional synoptic conditions towards the source areas that largely control temporal precipitation variations, and these are in turn either facilitated or inhibited by ENSO. The spatio-temporal variability of precipitation leads to a complex hydrological regime. Perennial rivers in the north and central Atacama Desert tend to flood in summer, especially during La Niña conditions, from source to sea. Perennial rivers in the south tend to flood in summer, but as a result of melt from the previous years snowfall, especially during El Niño conditions, again from source to sea. However, while inland areas may also experience flooding of ephemeral rivers in summer associated with La Niña, coastal areas on the other hand experience winter flooding of ephemeral rivers associated with El Niño. Surface water flood events, and groundwater recharge events reported in the literature, are generally less frequent than ENSO events, confirming the requirement for specific synoptic conditions and making the use of averages unsound for present-day hydrological studies and water resource evaluations. Copyright © 2006 Royal Meteorological Society.

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Crossref · 10.1002/joc.1359

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  • Fluctuations in water table and brine concentration, influenced by reinjection as well as abstraction, can affect the evaporation rate.

    “Fluctuations in the water table and brine concentration, influenced by reinjection as well as abstraction, can affect the evaporation rate (Houston, 2006;Marazuela et al., 2019bMarazuela et al., , 2020b)).”
  • The evaporation rate increases as brine concentration decreases, and has an exponentially decreasing relationship with depth; once the water table is ≥0.5 m below the surface, evaporation reduces significantly.

    “The evaporation rate increases as brine concentration decreases, and has an exponentially decreasing relationship with depth, once the water table is ≥0.5 m below the surface evaporation reduces significantly (Houston, 2006;Marazuela et al., 2020b).”

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Authors
Houston, J.
Corresponding author
Houston, John
Venue
International Journal of Climatology
Publisher
Wiley
Published
2006
Volume
26
Issue
15
Pages
2181-2198
ISSN
  • 0899-8418 (ISSN-L)
  • 1097-0088
OpenAlex
W2060098961
Cited by
413
References
40
Citations by year
2026: 22 · 2025: 13 · 2024: 31 · 2023: 39 · 2022: 38 · 2021: 30 · 2020: 62 · 2019: 47 · 2018: 21 · 2017: 23 · 2016: 14 · 2015: 13 · 2014: 12 · 2013: 9 · 2012: 10
FWCI
2.76
Type
journal article
Language
en
Open access
closed
Locations
International Journal of Climatology (publishedVersion)
Topics
  • Physical Sciences › Environmental Science › Global and Planetary Change › Climate variability and models
  • Physical Sciences › Environmental Science › Global and Planetary Change › Hydrology and Drought Analysis
  • Physical Sciences › Environmental Science › Water Science and Technology › Hydrology and Watershed Management Studies
Keywords
rainfall variability, Atacama Desert, ENSO, El Niño, La Niña, seasonal rainfall, synoptic conditions, river flooding, ephemeral streams, groundwater recharge, hydrological regime

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