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Spatial and temporal changes of aridity in Argentina and its relationship with some oceanic-atmospheric teleconnection patterns

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Abstract

This paper analyzes spatial and temporal changes of aridity in Argentina (1961–2022). The aridity degree, using Climatic Research Unit (CRU) monthly data, was defined through six climate types classified by De Martonne Aridity Index (DMI). Argentina presents a very arid, arid and semiarid region that extends from Puna to Patagonia, alongside two humid and very humid regions: one located in the Chaco-Pampas Plains and Mesopotamia, and another in the Patagonian Andes. Between these regions, there are subhumid areas with marked aridity variations. These structures persist over time, but advances or setbacks were observed in their bordering areas, with significant changes in the Andes (leading to more arid conditions) and the southwestern Pampas Plains (leading to more humid conditions) during the historical period. The contribution of temperature and precipitation changes to these DMI changes was quantified, indicating that precipitation modulated the DMI spatial changes, while temperature intensified or weakened the change magnitudes. The extension variations of the arid and semiarid regions in Argentina were related to three climate variability modes (El Niño – Southern Oscillation [ENSO], Pacific Decadal Oscillation [PDO] and South Atlantic Ocean Dipole [SAOD]). Significant correlations were found with PDO (r < 0) and SAOD (r > 0), which indicate that an increase in the area occupied by arid and semiarid climates are associated with PDO negative phase or SAOD positive phase. Moreover, when these phases occur simultaneously, the expansion of arid and semiarid regions is larger than under the action of an individual forcing.

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Acknowledgements

This work has been supported by FONCYT Grant PICT2018-02496 and PIP grant KE2 11220210100752CO. The authors would like to thank Cerne Bibiana Ph.D. (DCAO/UBA) for her recommendations to improve this paper. The authors also express gratitude for the comments from the editors and reviewers that have been valuable in enhancing the research quality.

Funding

The research has been funded by National Agency for Scientific and Technological Promotion of Argentina, under FONCYT Grant PICT2018-02496 and by the National Council of Scientific and Technological Research of Argentina under PIP grant KE2 11220210100752CO.

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The first author (P.S.B.) as well as the co-author (M.E.D.) of this work have equally contributed to the preparation of the manuscript, creating the relevant figures/tables and conducting their respective analyses.

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Correspondence to Pedro S. Blanco or Moira E. Doyle.

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Blanco, P.S., Doyle, M.E. Spatial and temporal changes of aridity in Argentina and its relationship with some oceanic-atmospheric teleconnection patterns. Theor Appl Climatol (2024). https://doi.org/10.1007/s00704-024-04909-7

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  • DOI: https://doi.org/10.1007/s00704-024-04909-7

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