**Acknowledgements**

The authors would like to acknowledge the Fondap 15110009 project, Center for Climate and Resilience Research [CR2] and to the Fondecyt project Nº 3180682, for their economic support.

**References**

Resiliencia (CR2). 2015:28

University of Chile; 2015

Discussions. 2012;**9**(10)

2013;**17**(3):1035

[1] Bradley R. Projected temperature changes along the American cordillera and the planned

Hydro-Geochemical Water Inputs Identification in Glacierized Basin Hydrology

http://dx.doi.org/10.5772/intechopen.75390

47

[2] Stocker T, Qin D, Plattner G, Tignor M, Allen S, Boschung J, et al. Climate Change 2013:

[3] CR2. Informe a la nación. La megasequía 2010 – 2015. Centro de Ciencia del Clima y la

[4] Crespo S. Conocimiento del aporte hídrico de las precipitaciones y los cuerpos de hielo en la cuenca alta del río Mendoza, Andes centrales de Argentina [PhD Thesis]. National

[5] Cornwell E, Molotch N, McPhee J. Spatio-temporal variability of snow water equivalent in the extra-tropical Andes cordillera from distributed energy balance modeling and remotely sensed snow cover. Hydrology and Earth System Sciences. 2016;**20**(1):411-430

[6] Peña H, Nazarala B. Snowmelt-runoff simulation model of a Central Chile Andean basin with relevant orographic effects. Large scale effects of seasonal snow cover (Proceedings

[7] Castillo Avalos YA. Caracterización de la hidrología glaciar de la cuenca del río Maipo mediante la implementación de un modelo glaciohidrológico semi-distribuido físicamente basado [Thesis]. Santiago: Faculty of Physical Sciences and Mathematics,

[8] Leiva JC, Cabrera G, Lenzano LE. Glacier mass balance in the Cajon del Rubio, Argentinean Central Andes. Cold Regions Science and Technology. 1986;**13**:83-90

[9] Ohlanders N, Rodriguez M, McPhee J. Stable water isotope variation in a central Andean watershed dominated by glacier-and snowmelt. Hydrology & Earth System Sciences

[10] Hoke GD, Aranibar JN, Viale M, Araneo DC, Llano CL. Isotopic characterization of mountain precipitation along the eastern flank of the Andes between 32.5-35°S. Amer

[11] Rodriguez M, McPhee J. Stable water isotope variation in a central Andean watershed dominated by glacier and snowmelt. Hydrology and Earth System Sciences.

[12] Crespo S, Aranibar J, Gomez L, Schwikowski M, Bruetsch S, Cara L, Villalba R. Ionic and stable isotope chemistry as indicators of water sources to the Upper Mendoza River basin, Central Andes of Argentina. Hydrological Sciences Journal. 2017;**62**(4):588-605

[13] Hoefs J. Stable Isotope Geochemistry. Cham: Springer International Publishing; 2015

Geophysical Union; Geochemistry Geophysics Geosystems. 2013;**14**:962-978

The Physical Science Basis. Cambridge: Cambridge University Press; 2013

GCOS network. Geophysical Research Letters. 2004;**31**(16)

University of Luján, Buenos Aires, Argentina. 2016

of the Vancouver symposium). IAHS Publication. 1987:166
