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Mariano Masiokas


Dr. Mariano Masiokas
Assistant Researcher
CCT CONICET Mendoza
Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales (IANIGLA)
Av. Ruiz Leal S/N
Mendoza, 5500
Argentina
Phone: +54 (261) 5244257
Fax: +54 (261) 5244201
E-mail: mmasiokas@mendoza-conicet.gov.ar


Key Publications of Mariano Masiokas (up to five) :
Masiokas, M.H.; Villalba, R.; Luckman, B.; LeQuesne, C.; Aravena, J.C. 2006. Snowpack variations in the central Andes of Argentina and Chile, 1951-2005: Large-scale atmospheric influences and implications for water resources in the region. Journal of Climate 19 (24), 6334-6352.

Masiokas, M.H.; Villalba, R.; Luckman, B.; Delgado, S.; Lascano, M.; Stepanek, P. 2008. 20th-century glacier recession and regional hydroclimatic changes in northwestern Patagonia. Global and Planetary Change 60 (1-2), 85-100.

Masiokas, M.H.; Rivera, A.; Espizua, L.E.; Villalba, R.; Delgado, S.; Aravena, J.C. 2009. Glacier fluctuations in extratropical South America during the past 1000 years. Palaeogeography, Palaeoclimatology, Palaeoecology, doi:10.1016/j.palaeo.2009.08.006.

Masiokas, M.H.; Luckman, B.; Villalba, R.; Delgado, S.; Skvarca, P.; Ripalta, A. 2009. Little Ice Age fluctuations of small glaciers in the Monte Fitz Roy and Lago del Desierto areas, south Patagonian Andes, Argentina. Palaeogeography, Palaeoclimatology, Palaeoecology, doi:10.1016/j.palaeo.2007.10.031.

Masiokas, M.H.; Luckman, B.H.; Villalba, R.; Delgado, S.; Rabassa, J. 2010. Little Ice Age fluctuations of Glaciar Río Manso in the north Patagonian Andes of Argentina. Quaternary Research 73 (1), 96-106.


Expertise of Mariano Masiokas:
Expertise Category Specific Expertise
PAGES TopicsClimate Dynamics
PAGES TimescalesHolocene (10,000 years)
Last Millennium
PAGES LocationSouthern Hemisphere
Americas
PAGES ParametersTemperature
Hydrological Balance
PAGES ArchivesIce Cores/Glaciers
Tree Rings
Documentary Records

Additional Specialties:
Research Thesis: Climatic variability in the north and south Patagonian Andes of Argentina as inferred from instrumental, dendrochronological and glaciological records.

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