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The Cryosphere An interactive open-access journal of the European Geosciences Union
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
Research article
09 Jun 2016
Review status
This discussion paper is a preprint. It has been under review for the journal The Cryosphere (TC). The revised manuscript was not accepted.
Glacier surface mass balance modeling in the inner tropics using a positive degree-day approach
L. Maisincho1,2, V. Favier3, P. Wagnon2,4, V. Jomelli5, R. Basantes Serrano2,3,8, B. Francou2, M. Villacis6, A. Rabatel3, M. Ménégoz7, L. Mourre2, and B. Cáceres1 1INAMHI, Instituto Nacional de Meteorología e Hidrología, Iñaquito N36-14 y Corea, Quito, Ecuador
2IRD, Univ. Grenoble Alpes, CNRS, INPG, Laboratoire d'étude des Transferts en Hydrologie et Environnement (LTHE), UMR5564, F-38000 Grenoble, France
3Univ. Grenoble Alpes, CNRS, Laboratoire de Glaciologie et Géophysique de l’Environnement (LGGE), UMR5183, F-38000 Grenoble, France
4ICIMOD, GPO Box 3226, Kathmandu, Nepal
5Université Paris 1 Panthéon-Sorbonne, CNRS, Laboratoire de Géographie Physique (LGP), 92195 Meudon, France
6Escuela Politécnica Nacional (EPN), Ladrón de Guevara E11-253, Quito, Ecuador
7Institut Català de Ciènces del Clima (IC3), Doctor Trueta, 203 3a planta 08005 Barcelona (Spain)
8Universidad Regional Amazónica (IKIAM), Km 7, Via Muyuna-Atacapi, Tena, Ecuador
Abstract. We present a basic ablation model combining a positive degree-day approach to calculate melting and a simple equation based on wind speed to compute sublimation. The model was calibrated at point scale (4900 m a.s.l.) on Antizana Glacier 15 (0.28 km2; 0°28' S, 78°09' W) with data from March 2002 to August 2003 and validated with data from January to November 2005. Cross validation was performed by interchanging the calibration and validation periods. Optimization of the model based on the calculated surface energy balance allowed degree-day factors to be retrieved for snow and ice, and suggests that melting started when daily air temperature was still below 0 °C, because incoming shortwave radiation was intense around noon and resulted in positive temperatures for a few hours a day. The model was then distributed over the glacier and applied to the 2000–2008 period using meteorological inputs measured on the glacier foreland to assess to what extent this approach is suitable for quantifying glacier surface mass balance in Ecuador. Results showed that a model based on temperature, wind speed, and precipitation is able to reproduce a large part of surface mass-balance variability of Antizana Glacier 15 even though the melting factors for snow and ice may vary with time. The model performed well because temperatures were significantly correlated with albedo and net shortwave radiation. Because this relationship disappeared when strong winds result in mixed air in the surface boundary layer, this model should not be extrapolated to other tropical regions where sublimation increases during a pronounced dry season or where glaciers are located above the mean freezing level.

Citation: Maisincho, L., Favier, V., Wagnon, P., Jomelli, V., Basantes Serrano, R., Francou, B., Villacis, M., Rabatel, A., Ménégoz, M., Mourre, L., and Cáceres, B.: Glacier surface mass balance modeling in the inner tropics using a positive degree-day approach, The Cryosphere Discuss.,, 2016.
L. Maisincho et al.
Interactive discussionStatus: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
Printer-friendly Version - Printer-friendly version      Supplement - Supplement
RC1: 'Referee's Comments', Anonymous Referee #1, 25 Jun 2016 Printer-friendly Version 
AC1: 'Response to R1', Luis Maisincho, 31 Aug 2016 Printer-friendly Version Supplement 
RC2: 'Review', Anonymous Referee #2, 12 Jul 2016 Printer-friendly Version 
AC2: 'Response to R2', Luis Maisincho, 31 Aug 2016 Printer-friendly Version Supplement 
L. Maisincho et al.
L. Maisincho et al.


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Latest update: 17 Oct 2017
Publications Copernicus
Short summary
Studies performed in the outer tropics suggested that Positive Degree-Day (PDD) model should be used with caution in tropical areas because temperature is not directly linked to the main local melting processes. Using an enhanced PDD model in the inner tropics during nine years allowed an accurate modelling of the glacier-wide mass balances and ablation on the Antizana glacier. This proves the high sensitivity of glaciers to temperature changes in Ecuador.
Studies performed in the outer tropics suggested that Positive Degree-Day (PDD) model should be...