[{"language":[{"iso":"eng"}],"publication_status":"published","intvolume":"        33","keyword":["Water Science and Technology"],"_id":"12603","date_published":"2018-11-26T00:00:00Z","abstract":[{"text":"We present a field-data rich modelling analysis to reconstruct the climatic forcing, glacier response, and runoff generation from a high-elevation catchment in central Chile over the period 2000–2015 to provide insights into the differing contributions of debris-covered and debris-free glaciers under current and future changing climatic conditions. Model simulations with the physically based glacio-hydrological model TOPKAPI-ETH reveal a period of neutral or slightly positive mass balance between 2000 and 2010, followed by a transition to increasingly large annual mass losses, associated with a recent mega drought. Mass losses commence earlier, and are more severe, for a heavily debris-covered glacier, most likely due to its strong dependence on snow avalanche accumulation, which has declined in recent years. Catchment runoff shows a marked decreasing trend over the study period, but with high interannual variability directly linked to winter snow accumulation, and high contribution from ice melt in dry periods and drought conditions. The study demonstrates the importance of incorporating local-scale processes such as snow avalanche accumulation and spatially variable debris thickness, in understanding the responses of different glacier types to climate change. We highlight the increased dependency of runoff from high Andean catchments on the diminishing resource of glacier ice during dry years.","lang":"eng"}],"type":"journal_article","month":"11","publication_identifier":{"issn":["0885-6087"],"eissn":["1099-1085"]},"main_file_link":[{"open_access":"1","url":"https://doi.org/10.1002/hyp.13354"}],"article_processing_charge":"No","oa_version":"Published Version","date_created":"2023-02-20T08:13:14Z","doi":"10.1002/hyp.13354","title":"Interannual variability in glacier contribution to runoff from a high‐elevation Andean catchment: Understanding the role of debris cover in glacier hydrology","scopus_import":"1","publisher":"Wiley","page":"214-229","citation":{"chicago":"Burger, Flavia, Alvaro Ayala, David Farias, Thomas E. Shaw, Shelley MacDonell, Ben Brock, James McPhee, and Francesca Pellicciotti. “Interannual Variability in Glacier Contribution to Runoff from a High‐elevation Andean Catchment: Understanding the Role of Debris Cover in Glacier Hydrology.” <i>Hydrological Processes</i>. Wiley, 2018. <a href=\"https://doi.org/10.1002/hyp.13354\">https://doi.org/10.1002/hyp.13354</a>.","short":"F. Burger, A. Ayala, D. Farias, T.E. Shaw, S. MacDonell, B. Brock, J. McPhee, F. Pellicciotti, Hydrological Processes 33 (2018) 214–229.","ista":"Burger F, Ayala A, Farias D, Shaw TE, MacDonell S, Brock B, McPhee J, Pellicciotti F. 2018. Interannual variability in glacier contribution to runoff from a high‐elevation Andean catchment: Understanding the role of debris cover in glacier hydrology. Hydrological Processes. 33(2), 214–229.","mla":"Burger, Flavia, et al. “Interannual Variability in Glacier Contribution to Runoff from a High‐elevation Andean Catchment: Understanding the Role of Debris Cover in Glacier Hydrology.” <i>Hydrological Processes</i>, vol. 33, no. 2, Wiley, 2018, pp. 214–29, doi:<a href=\"https://doi.org/10.1002/hyp.13354\">10.1002/hyp.13354</a>.","ama":"Burger F, Ayala A, Farias D, et al. Interannual variability in glacier contribution to runoff from a high‐elevation Andean catchment: Understanding the role of debris cover in glacier hydrology. <i>Hydrological Processes</i>. 2018;33(2):214-229. doi:<a href=\"https://doi.org/10.1002/hyp.13354\">10.1002/hyp.13354</a>","ieee":"F. Burger <i>et al.</i>, “Interannual variability in glacier contribution to runoff from a high‐elevation Andean catchment: Understanding the role of debris cover in glacier hydrology,” <i>Hydrological Processes</i>, vol. 33, no. 2. Wiley, pp. 214–229, 2018.","apa":"Burger, F., Ayala, A., Farias, D., Shaw, T. E., MacDonell, S., Brock, B., … Pellicciotti, F. (2018). Interannual variability in glacier contribution to runoff from a high‐elevation Andean catchment: Understanding the role of debris cover in glacier hydrology. <i>Hydrological Processes</i>. Wiley. <a href=\"https://doi.org/10.1002/hyp.13354\">https://doi.org/10.1002/hyp.13354</a>"},"status":"public","publication":"Hydrological Processes","year":"2018","author":[{"full_name":"Burger, Flavia","first_name":"Flavia","last_name":"Burger"},{"first_name":"Alvaro","last_name":"Ayala","full_name":"Ayala, Alvaro"},{"full_name":"Farias, David","first_name":"David","last_name":"Farias"},{"first_name":"Thomas E.","last_name":"Shaw","full_name":"Shaw, Thomas E."},{"full_name":"MacDonell, Shelley","last_name":"MacDonell","first_name":"Shelley"},{"full_name":"Brock, Ben","first_name":"Ben","last_name":"Brock"},{"full_name":"McPhee, James","first_name":"James","last_name":"McPhee"},{"id":"b28f055a-81ea-11ed-b70c-a9fe7f7b0e70","first_name":"Francesca","last_name":"Pellicciotti","full_name":"Pellicciotti, Francesca"}],"extern":"1","date_updated":"2023-02-28T11:49:36Z","oa":1,"quality_controlled":"1","article_type":"original","user_id":"2DF688A6-F248-11E8-B48F-1D18A9856A87","day":"26","issue":"2","volume":33},{"date_published":"2016-07-28T00:00:00Z","_id":"12615","keyword":["Water Science and Technology"],"publication_status":"published","intvolume":"        30","language":[{"iso":"eng"}],"title":"Modelling the hydrological response of debris-free and debris-covered glaciers to present climatic conditions in the semiarid Andes of central Chile","article_processing_charge":"No","oa_version":"None","doi":"10.1002/hyp.10971","date_created":"2023-02-20T08:14:40Z","publication_identifier":{"issn":["0885-6087"]},"abstract":[{"text":"We apply the process-based, distributed TOPKAPI-ETH glacio-hydrological model to a glacierized catchment (19% glacierized) in the semiarid Andes of central Chile. The semiarid Andes provides vital freshwater resources to valleys in Chile and Argentina, but only few glacio-hydrological modelling studies have been conducted, and its dominant hydrological processes remain poorly understood. The catchment contains two debris-free glaciers reaching down to 3900 m asl (Bello and Yeso glaciers) and one debris-covered avalanche-fed glacier reaching to 3200 m asl (Piramide Glacier). Our main objective is to compare the mass balance and runoff contributions of both glacier types under current climatic conditions. We use a unique dataset of field measurements collected over two ablation seasons combined with the distributed TOPKAPI-ETH model that includes physically oriented parameterizations of snow and ice ablation, gravitational distribution of snow, snow albedo evolution and the ablation of debris-covered ice. Model outputs indicate that while the mass balance of Bello and Yeso glaciers is mostly explained by temperature gradients, the Piramide Glacier mass balance is governed by debris thickness and avalanches and has a clear non-linear profile with elevation as a result. Despite the thermal insulation effect of the debris cover, the mass balance and contribution to runoff from debris-free and debris-covered glaciers are similar in magnitude, mainly because of elevation differences. However, runoff contributions are distinct in time and seasonality with ice melt starting approximately four weeks earlier from the debris-covered glacier, what is of relevance for water resources management. At the catchment scale, snowmelt is the dominant contributor to runoff during both years. However, during the driest year of our simulations, ice melt contributes 42 ± 8% and 67 ± 6% of the annual and summer runoff, respectively. Sensitivity analyses show that runoff is most sensitive to temperature and precipitation gradients, melt factors and debris cover thickness. ","lang":"eng"}],"type":"journal_article","month":"07","date_updated":"2023-02-24T11:29:28Z","extern":"1","year":"2016","author":[{"full_name":"Ayala, A.","first_name":"A.","last_name":"Ayala"},{"last_name":"Pellicciotti","first_name":"Francesca","full_name":"Pellicciotti, Francesca","id":"b28f055a-81ea-11ed-b70c-a9fe7f7b0e70"},{"full_name":"MacDonell, S.","first_name":"S.","last_name":"MacDonell"},{"first_name":"J.","last_name":"McPhee","full_name":"McPhee, J."},{"last_name":"Vivero","first_name":"S.","full_name":"Vivero, S."},{"full_name":"Campos, C.","first_name":"C.","last_name":"Campos"},{"first_name":"P.","last_name":"Egli","full_name":"Egli, P."}],"publication":"Hydrological Processes","status":"public","page":"4036-4058","citation":{"mla":"Ayala, A., et al. “Modelling the Hydrological Response of Debris-Free and Debris-Covered Glaciers to Present Climatic Conditions in the Semiarid Andes of Central Chile.” <i>Hydrological Processes</i>, vol. 30, no. 22, Wiley, 2016, pp. 4036–58, doi:<a href=\"https://doi.org/10.1002/hyp.10971\">10.1002/hyp.10971</a>.","ieee":"A. Ayala <i>et al.</i>, “Modelling the hydrological response of debris-free and debris-covered glaciers to present climatic conditions in the semiarid Andes of central Chile,” <i>Hydrological Processes</i>, vol. 30, no. 22. Wiley, pp. 4036–4058, 2016.","ama":"Ayala A, Pellicciotti F, MacDonell S, et al. Modelling the hydrological response of debris-free and debris-covered glaciers to present climatic conditions in the semiarid Andes of central Chile. <i>Hydrological Processes</i>. 2016;30(22):4036-4058. doi:<a href=\"https://doi.org/10.1002/hyp.10971\">10.1002/hyp.10971</a>","apa":"Ayala, A., Pellicciotti, F., MacDonell, S., McPhee, J., Vivero, S., Campos, C., &#38; Egli, P. (2016). Modelling the hydrological response of debris-free and debris-covered glaciers to present climatic conditions in the semiarid Andes of central Chile. <i>Hydrological Processes</i>. Wiley. <a href=\"https://doi.org/10.1002/hyp.10971\">https://doi.org/10.1002/hyp.10971</a>","ista":"Ayala A, Pellicciotti F, MacDonell S, McPhee J, Vivero S, Campos C, Egli P. 2016. Modelling the hydrological response of debris-free and debris-covered glaciers to present climatic conditions in the semiarid Andes of central Chile. Hydrological Processes. 30(22), 4036–4058.","chicago":"Ayala, A., Francesca Pellicciotti, S. MacDonell, J. McPhee, S. Vivero, C. Campos, and P. Egli. “Modelling the Hydrological Response of Debris-Free and Debris-Covered Glaciers to Present Climatic Conditions in the Semiarid Andes of Central Chile.” <i>Hydrological Processes</i>. Wiley, 2016. <a href=\"https://doi.org/10.1002/hyp.10971\">https://doi.org/10.1002/hyp.10971</a>.","short":"A. Ayala, F. Pellicciotti, S. MacDonell, J. McPhee, S. Vivero, C. Campos, P. Egli, Hydrological Processes 30 (2016) 4036–4058."},"scopus_import":"1","publisher":"Wiley","volume":30,"issue":"22","day":"28","user_id":"2DF688A6-F248-11E8-B48F-1D18A9856A87","quality_controlled":"1","article_type":"original"},{"citation":{"ista":"Rodriguez M, Ohlanders N, Pellicciotti F, Williams MW, McPhee J. 2016. Estimating runoff from a glacierized catchment using natural tracers in the semi-arid Andes cordillera. Hydrological Processes. 30(20), 3609–3626.","chicago":"Rodriguez, Maximiliano, Nils Ohlanders, Francesca Pellicciotti, Mark W. Williams, and James McPhee. “Estimating Runoff from a Glacierized Catchment Using Natural Tracers in the Semi-Arid Andes Cordillera.” <i>Hydrological Processes</i>. Wiley, 2016. <a href=\"https://doi.org/10.1002/hyp.10973\">https://doi.org/10.1002/hyp.10973</a>.","short":"M. Rodriguez, N. Ohlanders, F. Pellicciotti, M.W. Williams, J. McPhee, Hydrological Processes 30 (2016) 3609–3626.","ama":"Rodriguez M, Ohlanders N, Pellicciotti F, Williams MW, McPhee J. Estimating runoff from a glacierized catchment using natural tracers in the semi-arid Andes cordillera. <i>Hydrological Processes</i>. 2016;30(20):3609-3626. doi:<a href=\"https://doi.org/10.1002/hyp.10973\">10.1002/hyp.10973</a>","ieee":"M. Rodriguez, N. Ohlanders, F. Pellicciotti, M. W. Williams, and J. McPhee, “Estimating runoff from a glacierized catchment using natural tracers in the semi-arid Andes cordillera,” <i>Hydrological Processes</i>, vol. 30, no. 20. Wiley, pp. 3609–3626, 2016.","apa":"Rodriguez, M., Ohlanders, N., Pellicciotti, F., Williams, M. W., &#38; McPhee, J. (2016). Estimating runoff from a glacierized catchment using natural tracers in the semi-arid Andes cordillera. <i>Hydrological Processes</i>. Wiley. <a href=\"https://doi.org/10.1002/hyp.10973\">https://doi.org/10.1002/hyp.10973</a>","mla":"Rodriguez, Maximiliano, et al. “Estimating Runoff from a Glacierized Catchment Using Natural Tracers in the Semi-Arid Andes Cordillera.” <i>Hydrological Processes</i>, vol. 30, no. 20, Wiley, 2016, pp. 3609–26, doi:<a href=\"https://doi.org/10.1002/hyp.10973\">10.1002/hyp.10973</a>."},"page":"3609-3626","status":"public","publication":"Hydrological Processes","publisher":"Wiley","scopus_import":"1","extern":"1","date_updated":"2023-02-24T11:26:54Z","author":[{"full_name":"Rodriguez, Maximiliano","last_name":"Rodriguez","first_name":"Maximiliano"},{"full_name":"Ohlanders, Nils","last_name":"Ohlanders","first_name":"Nils"},{"id":"b28f055a-81ea-11ed-b70c-a9fe7f7b0e70","first_name":"Francesca","last_name":"Pellicciotti","full_name":"Pellicciotti, Francesca"},{"full_name":"Williams, Mark W.","last_name":"Williams","first_name":"Mark W."},{"full_name":"McPhee, James","first_name":"James","last_name":"McPhee"}],"year":"2016","article_type":"original","quality_controlled":"1","issue":"20","volume":30,"user_id":"2DF688A6-F248-11E8-B48F-1D18A9856A87","day":"22","intvolume":"        30","publication_status":"published","language":[{"iso":"eng"}],"date_published":"2016-07-22T00:00:00Z","keyword":["Water Science and Technology"],"_id":"12616","publication_identifier":{"issn":["0885-6087"]},"month":"07","type":"journal_article","abstract":[{"lang":"eng","text":"This paper presents a methodology for hydrograph separation in mountain watersheds, which aims at identifying flow sources among ungauged headwater sub-catchments through a combination of observed streamflow and data on natural tracers including isotope and dissolved solids. Daily summer and bi-daily spring season water samples obtained at the outlet of the Juncal River Basin in the Andes of Central Chile were analysed for all major ions as well as stable water isotopes, δ18O and δD. Additionally, various samples from rain, snow, surface streams and exfiltrating subsurface water (springs) were sampled throughout the catchment. A principal component analysis was performed in order to address cross-correlation in the tracer dataset, reduce the dimensionality of the problem and uncover patterns of variability. Potential sources were identified in a two-component U-space that explains 94% of the observed tracer variability at the catchment outlet. Hydrograph separation was performed through an Informative-Bayesian model. Our results indicate that the Juncal Norte Glacier headwater sub-catchment contributed at least 50% of summer flows at the Juncal River Basin outlet during the 2011–2012 water year (a hydrologically dry period in the Region), even though it accounts for only 27% of the basin area. Our study confirms the value of combining solute and isotope information for estimating source contributions in complex hydrologic systems, and provides insights regarding experimental design in high-elevation semi-arid catchments. The findings of this study can be useful for evaluating modelling studies of the hydrological consequences of the rapid decrease in glacier cover observed in this region, by providing insights into the origin of river water in basins with little hydrometeorological information."}],"date_created":"2023-02-20T08:14:45Z","doi":"10.1002/hyp.10973","oa_version":"None","article_processing_charge":"No","title":"Estimating runoff from a glacierized catchment using natural tracers in the semi-arid Andes cordillera"},{"volume":28,"issue":"23","day":"06","user_id":"2DF688A6-F248-11E8-B48F-1D18A9856A87","article_type":"original","quality_controlled":"1","date_updated":"2023-02-24T08:48:40Z","extern":"1","author":[{"full_name":"Ragettli, S.","last_name":"Ragettli","first_name":"S."},{"full_name":"Cortés, G.","last_name":"Cortés","first_name":"G."},{"first_name":"J.","last_name":"McPhee","full_name":"McPhee, J."},{"first_name":"Francesca","last_name":"Pellicciotti","full_name":"Pellicciotti, Francesca","id":"b28f055a-81ea-11ed-b70c-a9fe7f7b0e70"}],"year":"2013","status":"public","publication":"Hydrological Processes","page":"5674-5695","citation":{"ista":"Ragettli S, Cortés G, McPhee J, Pellicciotti F. 2013. An evaluation of approaches for modelling hydrological processes in high-elevation, glacierized Andean watersheds. Hydrological Processes. 28(23), 5674–5695.","chicago":"Ragettli, S., G. Cortés, J. McPhee, and Francesca Pellicciotti. “An Evaluation of Approaches for Modelling Hydrological Processes in High-Elevation, Glacierized Andean Watersheds.” <i>Hydrological Processes</i>. Wiley, 2013. <a href=\"https://doi.org/10.1002/hyp.10055\">https://doi.org/10.1002/hyp.10055</a>.","short":"S. Ragettli, G. Cortés, J. McPhee, F. Pellicciotti, Hydrological Processes 28 (2013) 5674–5695.","ieee":"S. Ragettli, G. Cortés, J. McPhee, and F. Pellicciotti, “An evaluation of approaches for modelling hydrological processes in high-elevation, glacierized Andean watersheds,” <i>Hydrological Processes</i>, vol. 28, no. 23. Wiley, pp. 5674–5695, 2013.","apa":"Ragettli, S., Cortés, G., McPhee, J., &#38; Pellicciotti, F. (2013). An evaluation of approaches for modelling hydrological processes in high-elevation, glacierized Andean watersheds. <i>Hydrological Processes</i>. Wiley. <a href=\"https://doi.org/10.1002/hyp.10055\">https://doi.org/10.1002/hyp.10055</a>","ama":"Ragettli S, Cortés G, McPhee J, Pellicciotti F. An evaluation of approaches for modelling hydrological processes in high-elevation, glacierized Andean watersheds. <i>Hydrological Processes</i>. 2013;28(23):5674-5695. doi:<a href=\"https://doi.org/10.1002/hyp.10055\">10.1002/hyp.10055</a>","mla":"Ragettli, S., et al. “An Evaluation of Approaches for Modelling Hydrological Processes in High-Elevation, Glacierized Andean Watersheds.” <i>Hydrological Processes</i>, vol. 28, no. 23, Wiley, 2013, pp. 5674–95, doi:<a href=\"https://doi.org/10.1002/hyp.10055\">10.1002/hyp.10055</a>."},"publisher":"Wiley","scopus_import":"1","title":"An evaluation of approaches for modelling hydrological processes in high-elevation, glacierized Andean watersheds","doi":"10.1002/hyp.10055","date_created":"2023-02-20T08:16:39Z","oa_version":"None","article_processing_charge":"No","publication_identifier":{"issn":["0885-6087"]},"month":"09","type":"journal_article","abstract":[{"lang":"eng","text":"We use two hydrological models of varying complexity to study the Juncal River Basin in the Central Andes of Chile with the aim to understand the degree of conceptualization and the spatial structure that are needed to model present and future streamflows. We use a conceptual semi-distributed model based on elevation bands [Water Evaluation and Planning (WEAP)], frequently used for water management, and a physically oriented, fully distributed model [Topographic Kinematic Wave Approximation and Integration ETH Zurich (TOPKAPI-ETH)] developed for research purposes mainly. We evaluate the ability of the two models to reproduce the key hydrological processes in the basin with emphasis on snow accumulation and melt, streamflow and the relationships between internal processes. Both models are capable of reproducing observed runoff and the evolution of Moderate-resolution Imaging Spectroradiometer snow cover adequately. In spite of WEAP's simple and conceptual approach for modelling snowmelt and its lack of glacier representation and snow gravitational redistribution as well as a proper routing algorithm, this model can reproduce historical data with a similar goodness of fit as the more complex TOPKAPI-ETH. We show that the performance of both models can be improved by using measured precipitation gradients of higher temporal resolution. In contrast to the good performance of the conceptual model for the present climate, however, we demonstrate that the simplifications in WEAP lead to error compensation, which results in different predictions in simulated melt and runoff for a potentially warmer future climate. TOPKAPI-ETH, using a more physical representation of processes, depends less on calibration and thus is less subject to a compensation of errors through different model components. Our results show that data obtained locally in ad hoc short-term field campaigns are needed to complement data extrapolated from long-term records for simulating changes in the water cycle of high-elevation catchments but that these data can only be efficiently used by a model applying a spatially distributed physical representation of hydrological processes."}],"date_published":"2013-09-06T00:00:00Z","_id":"12633","keyword":["Water Science and Technology"],"intvolume":"        28","publication_status":"published","language":[{"iso":"eng"}]},{"date_published":"2008-09-15T00:00:00Z","_id":"12656","keyword":["Water Science and Technology"],"intvolume":"        22","publication_status":"published","language":[{"iso":"eng"}],"title":"A study of the energy balance and melt regime on Juncal Norte Glacier, semi-arid Andes of central Chile, using melt models of different complexity","doi":"10.1002/hyp.7085","oa_version":"None","date_created":"2023-02-20T08:18:45Z","article_processing_charge":"No","publication_identifier":{"issn":["0885-6087"],"eissn":["1099-1085"]},"type":"journal_article","month":"09","abstract":[{"text":"We use meteorological data from two automatic weather stations (AWS) on Juncal Norte Glacier, central Chile, to investigate the glacier–climate interaction and to test ablation models of different complexity. The semi-arid Central Andes are characterized by dry summers, with precipitation close to zero, low relative humidity and intense solar radiation. We show that katabatic forcing is dominant both on the glacier tongue and in the fore field, and that low humidity and absence of clouds cause strong radiative cooling of the glacier surface. Surface albedo is basically constant for snow and ice, because of the scarcity of solid precipitation. The energy balance of the glacier is simulated for a 2-month period in austral summer using two models of different complexity, which differ in the inclusion of the heat conduction flux into the snowpack and in the parameterization of the incoming longwave radiation. Net shortwave radiation is the dominant component of the energy balance. The sensible heat flux is always positive, while both the net longwave radiation and latent heat flux are negative. Neglecting the subsurface heat flux and corresponding variations in surface temperature leads to an overestimation of ablation of 2% over a total of 3695 mm water equivalent (w.e.) at the end of the season. Correct modelling of incoming longwave radiation is crucial, and we suggest that parameterizations based on vapour pressure and air temperature should be used rather than on computed cloud amount. We also used an enhanced temperature-index model incorporating the shortwave radiation flux, which has two empirical parameters. We apply it both with values of parameters obtained for Alpine glaciers and recalibrated on Juncal Norte. The model recalibrated against the correct energy balance simulations performs very well. The model parameters respond to the meteorological conditions typical of this climatic setting.","lang":"eng"}],"date_updated":"2024-10-14T12:00:17Z","extern":"1","author":[{"first_name":"Francesca","last_name":"Pellicciotti","full_name":"Pellicciotti, Francesca","orcid":"0000-0002-5554-8087","id":"b28f055a-81ea-11ed-b70c-a9fe7f7b0e70"},{"full_name":"Helbing, Jakob","first_name":"Jakob","last_name":"Helbing"},{"full_name":"Rivera, Andrés","last_name":"Rivera","first_name":"Andrés"},{"last_name":"Favier","first_name":"Vincent","full_name":"Favier, Vincent"},{"full_name":"Corripio, Javier","first_name":"Javier","last_name":"Corripio"},{"first_name":"José","last_name":"Araos","full_name":"Araos, José"},{"first_name":"Jean-Emmanuel","last_name":"Sicart","full_name":"Sicart, Jean-Emmanuel"},{"full_name":"Carenzo, Marco","first_name":"Marco","last_name":"Carenzo"}],"year":"2008","status":"public","publication":"Hydrological Processes","citation":{"chicago":"Pellicciotti, Francesca, Jakob Helbing, Andrés Rivera, Vincent Favier, Javier Corripio, José Araos, Jean-Emmanuel Sicart, and Marco Carenzo. “A Study of the Energy Balance and Melt Regime on Juncal Norte Glacier, Semi-Arid Andes of Central Chile, Using Melt Models of Different Complexity.” <i>Hydrological Processes</i>. Wiley, 2008. <a href=\"https://doi.org/10.1002/hyp.7085\">https://doi.org/10.1002/hyp.7085</a>.","short":"F. Pellicciotti, J. Helbing, A. Rivera, V. Favier, J. Corripio, J. Araos, J.-E. Sicart, M. Carenzo, Hydrological Processes 22 (2008) 3980–3997.","ista":"Pellicciotti F, Helbing J, Rivera A, Favier V, Corripio J, Araos J, Sicart J-E, Carenzo M. 2008. A study of the energy balance and melt regime on Juncal Norte Glacier, semi-arid Andes of central Chile, using melt models of different complexity. Hydrological Processes. 22(19), 3980–3997.","mla":"Pellicciotti, Francesca, et al. “A Study of the Energy Balance and Melt Regime on Juncal Norte Glacier, Semi-Arid Andes of Central Chile, Using Melt Models of Different Complexity.” <i>Hydrological Processes</i>, vol. 22, no. 19, Wiley, 2008, pp. 3980–97, doi:<a href=\"https://doi.org/10.1002/hyp.7085\">10.1002/hyp.7085</a>.","apa":"Pellicciotti, F., Helbing, J., Rivera, A., Favier, V., Corripio, J., Araos, J., … Carenzo, M. (2008). A study of the energy balance and melt regime on Juncal Norte Glacier, semi-arid Andes of central Chile, using melt models of different complexity. <i>Hydrological Processes</i>. Wiley. <a href=\"https://doi.org/10.1002/hyp.7085\">https://doi.org/10.1002/hyp.7085</a>","ama":"Pellicciotti F, Helbing J, Rivera A, et al. A study of the energy balance and melt regime on Juncal Norte Glacier, semi-arid Andes of central Chile, using melt models of different complexity. <i>Hydrological Processes</i>. 2008;22(19):3980-3997. doi:<a href=\"https://doi.org/10.1002/hyp.7085\">10.1002/hyp.7085</a>","ieee":"F. Pellicciotti <i>et al.</i>, “A study of the energy balance and melt regime on Juncal Norte Glacier, semi-arid Andes of central Chile, using melt models of different complexity,” <i>Hydrological Processes</i>, vol. 22, no. 19. Wiley, pp. 3980–3997, 2008."},"page":"3980-3997","publisher":"Wiley","scopus_import":"1","volume":22,"issue":"19","day":"15","user_id":"2DF688A6-F248-11E8-B48F-1D18A9856A87","article_type":"original","quality_controlled":"1"}]