Modelling the hydrological response of debris-free and debris-covered glaciers to present climatic conditions in the semiarid Andes of central Chile

Author:

Ayala A.1,Pellicciotti F.12,MacDonell S.3,McPhee J.45,Vivero S.3,Campos C.3,Egli P.1

Affiliation:

1. Institute of Environmental Engineering; ETH Zurich; Stefano-Franscini-Platz 5 8093 Zurich Switzerland

2. Department of Geography, Faculty of Engineering and Environment; Northumbria University; Newcastle upon Tyne UK

3. Centro de Estudios Avanzados en Zonas Áridas (CEAZA); Universidad de La Serena; Raúl Bitrán 1305 La Serena Chile

4. Department of Civil Engineering, Faculty of Physical and Mathematical Sciences; University of Chile; Av. Blanco Encalada 2002 Santiago Chile

5. Advanced Mining Technology Centre (AMTC), Faculty of Physical and Mathematical Sciences; University of Chile; Av. Tupper 2007 Santiago Chile

Funder

Chilean Water Authority (Dirección General de Aguas, DGA)

FONDECYT Initiation into Investigation

Fondo Nacional de Desarrollo Científico y Tecnológico

Publisher

Wiley

Subject

Water Science and Technology

Reference99 articles.

1. Distributed energy balance modeling of South Cascade Glacier, Washington and assessment of model uncertainty;Anslow;Journal of Geophysical Research,2008

2. Ayala A Pellicciotti F MacDonell S McPhee J Burlando P 2016 Melt and sublimation on glaciers of the dry Andes: semiarid high-elevation conditions decrease the performance of empirical melt models In Preparation for Water Resources Research

3. Modeling 2 m air temperatures over mountain glaciers: exploring the influence of katabatic cooling and external warming;Ayala;Journal of Geophysical Research, [Atmospheres],2015

4. Hydrological and geomorphological significance of rock glaciers in the dry Andes, Chile (27°-33°S);Azócar;Permafrost and Periglacial Processes,2010

5. Berk A Anderson G Acharya PK Shettle EP 2008 MODTRAN 5.2.0.0 user's manual

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