Seasonal and isotopic precipitation patterns in the semi-arid and high mountain areas

被引:2
|
作者
Valdivielso, Sonia [1 ]
Murray, Jesica [2 ,3 ]
Custodio, Emilio [4 ,5 ,6 ]
Hassanzadeh, Ashkan [1 ]
Martinez, Daniel Emilio [7 ]
Vazquez-Sune, Enric [1 ]
机构
[1] CSIC, Inst Environm Assessment & Water Res IDAEA, C Jordi Girona 18-26, Barcelona 08034, Spain
[2] Univ Nacl Salta, Inst Bio & Geo Ciencias NOA IBIGEO, CONICET, Salta, Argentina
[3] Univ Strasbourg, Inst Terre & Environm Strasbourg ITES, Strasbourg, France
[4] Engn Tech Univ Catalonia UPC, Engn Tech Univ Catalonia, C Jordi Girona 1-3, Barcelona 08034, Spain
[5] Royal Acad Math Phys & Nat Sci RAC Spain, Barcelona, Spain
[6] Univ Las Palmas Gran Canaria, Univ Palmas Gran Canaria, Las Palmas Gran Canaria, Islas Canarias, Spain
[7] Univ Nacl Mar Del Plata, Inst Geol Costas & Cuaternario, Inst Invest Marinas & Costeras, CONICET, Mar Del Plata, Buenos Aires, Argentina
关键词
Los Pozuelos basin; Stable isotopes; Back trajectories; HYSPLIT; OLR; Convective; STABLE-ISOTOPES; CENTRAL ANDES; VARIANCE TEST; WATER; GROUNDWATER; DELTA-O-18; CLIMATE; VARIABILITY; ENSO; EVAPORATION;
D O I
10.1016/j.scitotenv.2024.171750
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Precipitation plays a crucial role in the natural hydrological cycle. Understanding the spatial and temporal variations of precipitation isotopes is essential for identifying hydrological, meteorological, and ecological processes. In high mountain areas with arid and semi-arid conditions, especially in regions with endorheic basins, the portion of precipitation that infiltrates the groundwater as the primary source of water recharge. However, estimating this recharge is challenging and prone to high uncertainty. The main objective of this study was to implement a robust and detailed methodology to analyze the influence of meteorological variables and the origin of moisture sources on the stable isotopic composition (8 18 O and 8 2 H) of precipitation. As an illustrative case, we focused on the Los Pozuelos Basin, an endorheic basin in the Altiplano-Puna region of the Andes. The analysis incorporated precipitation samples collected over a 3-year period (January 2020 to April 2023) along with comprehensive monitoring of local atmospheric variables, satellite imagery, and HYSPLIT backward trajectory models. The examination involved a multivariate analysis of meteorological and stable isotope data and atmospheric transport pattern. Precipitation characteristics exhibited seasonal variability, with summer precipitation being depleted in heavy isotopes due to its extended continental journey and the recycling it undergoes while crossing the Amazon basin with convective activity. Another moisture path from the Atlantic Ocean, via the Rio de la Plata or Gran Chaco basin, represented an intermediate isotopic stage. La Nin a events intensified westerly winds, drawing moist air masses from the Pacific Ocean and causing rainfall in the study area. In winter, precipitation comes from the Pacific Ocean and isotopically enriched due to the low amount of precipitation and lower convective activity. By employing a meticulous methodology and multivariate statistical analysis, the study contributes positively to the broader discourse on water resource management and conservation in arid and semi -arid environments.
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页数:14
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