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FS 3.164

Andean glaciers and their role in the high mountain water cycle

Details

  • Full Title

    FS 3.164: Andean glaciers and their role in the high mountain water cycle
  • Scheduled

    Talks:
    2025-09-16, 10:00 - 12:00 (LT), SOWI – HS 2
  • Assigned to Synthesis Workshop

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  • Thematic Focus

    Cryo- & Hydrosphere, Ecosystems, Water Cycle, Water Resources
  • Keywords

    Andean glaciers, snow, glaciology, hydrology, Andean ecosystems

Description

Andean glaciers cover an extensive latitudinal range and provide vital meltwater for downstream populations and fragile ecosystems. Understanding the past, present, and future conditions of the mass and energy balance of Andean glaciers, as well as their impacts on ecosystems and water resources, is therefore vital. We invite contributions which increase the understanding of the glaciological processes controlling the energy and mass balance of Andean glaciers, particularly those which attempt to understand the important tipping points in the future evolution of these glaciers or quantify their temporal evolution. We also encourage submissions which determine the role of snow and glacier melt in high-elevation Andean catchments, especially in the face of drought conditions and projected climate warming. Research which defines how future glacier change might impact downstream water resources and ecosystem health would also be welcome, and we encourage holistic approaches that integrate disciplines. Contributions are also invited which bridge gaps between changes in the Andean cryosphere and sustainable water and ecosystem management strategies. We encourage abstracts based on methodologies including field measurements, remote sensing and modelling approaches.

Registered Abstracts

ID: 3.9107

Towards co-produced water management pathways to counteract deteriorating mountain water quality in the deglaciating Andes of Peru

Fabian Drenkhan
Castro-Salvador, Sofía; Leyva, Martín; Figueres, Leisel; Herrera, Eyvind; Fernández, Christian

Abstract/Description

In the seasonally dry tropical Andes, glacier retreat has led to widespread downstream impacts increasing mountain water insecurity. A growing number of catchments in the deglaciating Andes of Peru is currently exposed to acid rock drainage which severely affects downstream biota and human health. In combination with poor water governance, this situation of increasing hydrological risk urgently requires effective and long-term solutions to counteract decreasing water availability and poor quality. Yet, this challenging endeavour has barely been addressed in an integrated way in science and public policies. We showcase the deglaciating Negro river catchment (Cordillera Blanca, Peru), to disentangle the complex spatio-temporal interactions between specific catchment characteristics, glacier retreat and changes in water quality in the context of long-term human health. Therefore, in-situ measurements of changing water quality are analysed against specific geologic feature mapping and multi-annual glacier retreat using a supervised machine learning model. To expand our knowledge, a diverse set of participatory methods to determine local perceptions on water quality were applied in one affected community of the Negro river catchment and with decision-makers of the region. This co-produced knowledge framework builds a baseline to evaluate effective long-term strategies for adaptive management and policy in the context of long-term mountain water security.

ID: 3.10647

Glacier buffering of past streamflow droughts in a changing climate: Insights from the Andes

Rodrigo Aguayo
Zekollari, Harry; van Tiel, Marit; Bolibar, Jordi

Abstract/Description

Global warming exacerbates water scarcity by increasing the frequency of hydrological droughts. These droughts can be buffered by glaciers, which mitigate runoff variability across multiple timescales. However, as glaciers retreat, the reliability of this unique natural water reserve becomes increasingly uncertain, potentially intensifying drought stress. While the fields of hydrological modelling and glacier change modelling have advanced considerably, they are often treated independently, resulting in high levels of uncertainty. To address this, we leverage recent advances in regional and global datasets and propose a hybrid modelling approach that combines Long Short-Term Memory (LSTM) neural networks with process-based glacier modelling. Unlike traditional glacio-hydrological models that require parameterisations and basin-specific calibration, the proposed approach can leverage data-driven relationships between meteorological inputs, basin characteristics, and streamflow. We present a proof of concept in the Andes that examines the role of glaciers in the propagation of meteorological to streamflow drought. Furthermore, we explore potential changes in this influence by employing “what-if” storyline scenarios that incorporate projected glacier states. Our hybrid modelling approach improves the representation of the complex interactions between glacier dynamics and streamflow droughts. Preliminary results indicate that glaciers play a crucial role in buffering streamflow droughts, delaying and reducing drought severity under historical climate conditions. However, under “what-if” storyline scenarios, this buffering capacity declines considerably, leading to more frequent and prolonged drought events. The storyline-based analysis further suggests that the most pronounced changes occur in basins with a high dependency on glacier meltwater, particularly in arid regions. The results underscore the potential of hybrid modelling in enhancing our understanding of glacier-drought interactions, offering valuable insights for climate change communication and informing adaptation strategies in high mountain regions such as the Andes.

ID: 3.11200

Landsystems of the tropical high Peruvian Andes: glaciers, lakes, wetlands (bofedales) and catchment hydrology in Cordillera Vilcanota (Southern Peru)

Bethan Davies
Gribbin, Tom; King, Owen; Matthews, Tom; Baiker, Jan; Becker, Rike; Buytaert, Wouter; Carrivick, Jonathan; Drenkhan, Fabian; Garcia, Juan-Luis; Montoya, Nilton; Perry, Baker; Ely, Jeremy

Abstract/Description

Andean tropical glaciers are important indicators of climate change, provide freshwater resources for downstream communities, and form an important component of the hydrological cycle, supporting some 90 million people. Today, with highly seasonal precipitation and drought, Andean glacier ice, snow, wetlands (bofedales) and lakes play a crucial role in delaying water release, sustaining baseflows and water quality. Glacier shrinkage and changing precipitation patterns and water availability here impacts both high Andean pastoralist systems and other, downstream productive systems, including bigger cities in the inter-Andean valleys. Here we outline the hydrological and geomorphological relationships between glaciers, high-altitude wetlands and downstream hydrology in the Cordillera Vilcanota, Cuzco region, Peru. We present a new geomorphological map of glacial and hydrological features within the Vilcanota catchment. Across this domain we mapped ~23,000 features across seven key landform assemblages: topographic, glacier, subglacial, ice-marginal, fluvial, lacustrine and paraglacial. Our reconstructed maximum icefield covers 2660 km2 and was drained by 11 topographically constrained ice lobes across the region. Our geomorphic mapping reveals seven clear ice margins, morphostratigraphically correlated across the study region, reflecting at least seven palaeoglacier advances during the last glacial cycle, Late Glacial period and the Holocene. Understanding the dynamics and patterns of behaviour of tropical palaeoglaciers is important for interpreting their sensitivities and vulnerabilities. Furthermore, we investigate the way in which the mapped geomorphic features such as moraines, talus slopes and sandar interact with catchment hydrology and impact hydrogeological processes. Bofedales are well developed within glacial limits, with glacial processes such as erosion and formation of moraines providing the poorly drained conditions suitable for their development. The majority of the bofedales are largely hydrologically independent of contemporary glaciers, and could partially buffer water supplies as glaciers dwindle and disappear. This analysis enables an improved understanding of the timeframe for the formation of bofedal wetlands and for them to provide their key ecosystem services of water retention capacity, buffering drought, providing forage for high-Andean livestock herding, carbon storing and sequestration. These insights have implications for the

ID: 3.11657

Holocene moraines indicate a strong topographic control on glacier change in the Olivares Basin (33°S), Chile

Charlotte S. Curry
Rowan, Ann V.; Livingstone, Stephen J.; Diemont, Christiaan R.; Bravo, Claudio; Gheorghiu, Delia M.; Robson, Benjamin A.; Bryant, Robert G.

Abstract/Description

Satellite observations indicate that glaciers in the Olivares Basin (33°S) of the Central Andes are changing rapidly, with terminus recession of 0.5 – 2.5 km documented between 1973 and the present day. To understand recent changes in the context of longer-term glacier behaviour during the Holocene, we constrained past changes in glacier extent and dynamics using high-resolution geomorphological mapping and 36-Cl whole rock cosmogenic nuclide exposure age dating of ice-marginal moraines. These findings are collated into a reconstruction of the spatio-temporal evolution of the Olivares glaciers, and compared against regional palaeoclimate records.
Geomorphological mapping across the Olivares Basin has identified thirty-three distinct ice-marginal extents, six of which are located in the Salto del Olivares. The Salto del Olivares (2,750 – 2,900 m a.s.l.) is situated -33.10°S, -70.07°W, and surrounded by high-relief topography including a large topographic step of 600 – 650 m which separates the Salto del Olivares from the Upper Olivares and Juncal Sur glacier basins. From terminal moraines M2 (n=3), M3 (n=4), and M5 (n=1) in the Salto del Olivares, we collected and analysed eight samples. All eight 36-Cl ages give a Gaussian weighted mean age of 9.7 ± 4.84 ka and are interpreted collectively due overlapping exposure age distributions. Our results suggest a period of glacier stability at the start of the Holocene or the end of the late glacial period, followed by 5 – 9 km of terminal retreat until 1973. This coincides with retreat over the topographic step, which appears to have affected glacial dynamics as evidenced by ice-marginal moraines. When compared to regional and southern-hemispheric climate of the early Holocene, these results suggest that the Olivares glaciers responded to climate change later than similar sites in Patagonia and Northern Chile. This delayed response, coupled with contrasting spatial extents of retreat through time, indicates that local topographic factors, particularly a large topographic step, have played a significant role in modulating the timing and spatial distribution of moraine exposure across the Olivares Basin, competing against the influence of climate.

ID: 3.13109

Ecohydrological Characteristics of Wetlands of the Pastoruri and Qorikalis Catchments in thein the Peruvian Andes

Gimi Cristian Mamani Ramos
Diaz Aguilar, Renny Daniel; Fyffe, Catriona; Castro, Joshua; Mallqui, Helder; Quispe, Cristian

Abstract/Description

Bofedales or high-altitude wetlands are delicate ecosystems distributed across the Andean region. They offer multiple ecosystem services for local populations by providing hydrological regulation, important especially for subsistence grazing activities. Understanding their ecohydrological processes is crucial for choosing appropriate conservation and recovery measures for the sustainable management of these ecosystems. In this study, we analyzed and compared the ecohydrological characteristics (soil properties, vegetation characteristics, water chemistry and hydrological fluctuations) of two bofedales located in the northern and southern Peru. These measurements allow us to understand the differing bofedal characteristics and link them to their climate settings and catchment water inputs. Our results show that organic matter content correlates positively with variables such as field capacity, permanent wilting point, and porosity. We find notable differences in the water chemistry characteristics between the bofedales, especially pH, which could indicate differences in dominant water sources. We also found much higher values of hydraulic conductivity in the Pastoruri wetland compared to Qorikalis, which we believe may be that the variation in this parameter is likely due to the difference in terrain slope. The highest variations of water level were recorded in the Pastoruri Wetland, unlike the Qorikalis wetland where water level variations were more subdued. We aim to further analyse the link between precipitation events and water level response to allow direct comparison of the bofedal hydrological functioning. Through this work we plan to reveal new understanding of the factors driving differences in soil properties, water quality, vegetation and wetland hydrology.

ID: 3.13330

Horcones Superior Glacier: Monitoring the Role of Debris Cover at the Top of the Americas

Juan Cruz Ghilardi Truffa
Ruiz, Lucas; Falaschi, Daniel; Lo Vecchio, Andres

Abstract/Description

Glaciers in the Central Andes of Argentina are vital in the mountain hydrological system, contributing up to 60% of river flow during drought periods. This region contains 82% of the country’s debris-covered glaciers. Using remote sensing data, we observed a 21% increase in debris-covered areas over the past 40 years, with 62% of this growth occurring in the last decade. Despite their significance, the processes controlling mass loss and climate change responses by debris-covered glaciers are still poorly understood. To explore how debris cover affects surface ablation and ice dynamics, we recently installed monitoring equipment on the Horcones Superior Glacier (32° 4′ S, 70° 3′ W), located at the base of Aconcagua (6,962 m a.s.l.), the highest peak in the Southern and Western Hemispheres. Our setup includes an ablation stake network along the transition from debris-covered (0.5 m thick debris layer) to debris-free ice, temperature sensors to study heat transfer through the debris, and an Automatic Weather Station close to the glacier. Ground-penetrating radar (GPR) surveys were conducted to map debris layer thickness and ice thickness, and we used GNSS measurements to track surface velocity through boulders and stakes displacement. Additionally, we plan to conduct annual UAV surveys to monitor surface elevation and morphological changes in detail. We expect this monitoring approach to help us better understand the complex interactions between debris and ice and calibrate energy balance models. Our findings will improve our understanding of Andean debris-covered glaciers and their response to climate change.

ID: 3.13755

Impact of Black Carbon on the Surface Energy and Mass Balance of the Huaytapallana Glacier in the Junín Region, Peru

Viankcor Henry Cashpa Carrion
Villalobos Puma, Elver; Fashé Raymundo, Octavio; Silva Vidal, Fey Yamina; Torres Ramos, Christian; Cruz Encarnación, Rolando

Abstract/Description

Recent research conducted on various glaciers worldwide has revealed a significant increase in Black Carbon (BC) concentrations, reaching up to 500% compared to pre-industrial times. In addition, there is still considerable uncertainty regarding the effects of these concentrations on mountain ecosystems such as glaciers and water resources. Therefore, in order to address this issue, the present research aims to estimate the impact of BC on the Surface Energy Balance (SEB) and Surface Mass Balance (SMB) of the Huaytapallana glacier, located in the department of Junín – Peru, during the period from May 2022 to October 2024. To achieve this, in situ BC observations were used alongside a Snow and ice albedo modelling in Python (BioSNICAR) and a Coupled snowpack and ice Surface energy and mass balance model in Python (COSIPY). Furthermore, meteorological and atmospheric BC data measured at over 4700 m a.s.l., as well as ERA5 reanalysis data were used to force the models. The results reveal that the presence of BC on the glacier surface increased the SEB by up to 35 W/m², leading to a more negative SMB of up to 50 cm water equivalent. In conclusion, this research demonstrates that it is feasible to quantify the impact of BC on the dynamics of Peruvian glaciers and shows that the presence of BC causes a significant loss of glacier mass.

ID: 3.13913

Advancing water security in Andean Glacier-Fed Basins through an upward interdisciplinary approach from communities, monitoring and modeling implementation to local informed decisions

Kimberly Karime Visitación Bustamante
Rau, Pedro; Estrada, Yulissa; Cordova, Marco; Mamani, Albert; Montoya, Nilton; Horna, Daniel; Antiporta, Javier; Ross, Anthony ; Matanó, Alessia; Frappart, Frederic; Bourrel, Luc

Abstract/Description

Water security in the Peruvian Andean region is increasingly threatened by climate change, glacier retreats, and anthropogenic influences. This study focuses on advancing water security through the implementation of the hydrological instrumentation and monitoring systems of two contrasting glacial-fed catchments – Qasqara (Upper Amazon drainage side in Cusco) and Yuracmayo (Upper Pacific drainage side in Lima), both based on local communities needs and requirements to establish a foundational understanding of their hydrological dynamics and the relevance of monitoring towards an effective water resource management strategies. By deploying low-cost hydrological sensors and collecting a high temporal resolution database of streamflow and precipitation, this research formulates hydrological conditions based on hydrological modelling and enhances understanding of their water storage and regulation capacities. Qasqara, located in the upper Vilcanota – Urubamba river basin, features high-altitude lagoons and wetlands fed retreating glaciers, acting as natural regulators of streamflows. These ecosystems could reduce peak discharge by 77 – 87% during extreme events, proving their flood mitigation and water storage capacities. In contrast, Yuracmayo, in the upper Rimac River basin within the Pacific basin, corresponds to one of the most important water reservoirs supplying Lima, Peru’s capital and largest city. Despite increased precipitation, inflows into the Yuracmayo reservoir fed by a nearly extinct glacier, have significantly declined, accompanied by a 39% loss in wetland coverage between 2016 and 2024, raising concerns about long-term water availability. While Qasqara Lagoons act as buffers, Yuracmayo’s bofedals are threatened, putting their regulatory functions at risk. Instrumentation in Qasqara enhances local monitoring, deepens community knowledge of water regulation, and evidences ecosystem resilience in buffering hydrological variability. Meanwhile, Yuracmayo, crucial for Lima’s water security, faces risks from wetland loss and growing water demand. By comparing hydrological responses of Amazon and Pacific glacier-fed catchments with lagoons and water storage capacities, this study establishes the first comparative hydrological dataset for these basins and emphasizes the need for long-term monitoring to track changes in water availability, and provides information about advancing water security in Andean Glacier-Fed Basins to enhance local monitoring.

ID: 3.13948

Comparative Analysis of Light-Absorbing Particles (LAP) and Albedo on the Vallunaraju Glacier: Impact of Forest Fires and Fresh Snow Quality (2024-2025)

Marisol Mariory Julca Cadillo
Valdez Vega, Gilber Froilan; Valverde Fructuoso, Magaly Betsabe; Cruz Encarnacion, Rolando

Abstract/Description

Forest fires release large amounts of atmospheric pollutants, which can be carried by the wind to remote regions, such as glaciers, altering their surface properties. This study assesses the influence of a record number of forest fires on the concentrations of total particulate matter on the glacier surface (TPM), light-absorbing particles (LAP), and albedo, comparing these parameters with those recorded during recent snowfall events.
Sixteen snow and ice samples were collected along an altitudinal profile. In the laboratory, the total particle concentrations were determined, and the LAMH method was used for LAP quantification. Additionally, low-cost sensors were installed on the glacier surface to monitor the variation of albedo along an altitudinal gradient.
During the study period, 396 forest fires were recorded in the Cordillera Blanca region. The TPM on the glacier surface ranged between 140 and 1355 g/m², with a mean of 655 g/m², while LAP concentrations varied from 472 to 683 µg/m², reaching an average of 573.25 µg/m². Consequently, albedo values ranged between 0.21 and 0.48 (mean: 0.35). In contrast, during snowfall episodes, significantly lower TPM values were observed (range: 0.14–1.32 g/m²; mean: 0.45 g/m²) and LAP (range: 13.8–38.6 µg/m²; mean: 21.85 µg/m²), accompanied by a progressive increase in albedo in fresh snow (range: 0.61–0.73; mean: 0.68).
The results indicate that the deposition of TPM and LAP associated with forest fires exceeds, respectively, more than 30,000 and 40 times the concentrations observed during snowfall events, which could favor an accelerated glacier melting process due to the decrease in albedo and the consequent increase in radiation absorption.