4.6 Article

Contemporary glacial lakes in the Peruvian Andes

Journal

GLOBAL AND PLANETARY CHANGE
Volume 204, Issue -, Pages -

Publisher

ELSEVIER
DOI: 10.1016/j.gloplacha.2021.103574

Keywords

Hazard; Glacier; Lake; GLOF; Climate; Method

Funding

  1. UK Natural Environment Research Council (NERC) [NE/S01330X/1]
  2. Consejo Nacional de Ciencia, Tecnologia e Innovacion (CONCYTEC) [007-2019]
  3. Fondo Nacional de Desarrollo Cientifico y Tecnologico (FONDECYT) [59397]
  4. NERC [NE/S01330X/1] Funding Source: UKRI

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Glacier recession due to climate warming has led to the growth in size and number of glacial lakes, impacting water resources and glacier mass balance, as well as posing risks of glacial lake outburst floods. By creating a comprehensive inventory of glacial lakes in Peru, this study addresses knowledge gaps and provides reproducible methods for consistent monitoring in other mountainous regions. The inventory reveals that the majority of glacial lakes are detached from glaciers, with different dam types affecting lake size variations. This inventory serves as a crucial first step in understanding glacial lakes and assessing risks associated with glacial lake outburst floods.
Glacier recession in response to climate warming has resulted in an increase in the size and number of glacial lakes. Glacial lakes are an important focus for research as they impact water resources, glacier mass balance, and some produce catastrophic glacial lake outburst floods (GLOFs). Glaciers in Peru have retreated and thinned in recent decades, prompting the need for monitoring of ice- and water-bodies across the cordilleras. These monitoring efforts have been greatly facilitated by the availability of satellite imagery. However, knowledge gaps remain, particularly in relation to the formation, temporal evolution, and catastrophic drainage of glacial lakes. In this paper we address this gap by producing the most current and detailed glacial lake inventory in Peru and provide a set of reproducible methods that can be applied consistently for different time periods, and for other mountainous regions. The new lake inventory presented includes a total of 4557 glacial lakes covering a total area of 328.85 km(2). In addition to detailing lake distribution and extent, the inventory includes other metrics, such as dam type and volume, which are important for GLOF hazard assessments. Analysis of these metrics showed that the majority of glacial lakes are detached from current glaciers (97%) and are classified as either embedded (i.e. bedrock dammed; similar to 64% of all lakes) or (moraine) dammed (similar to 28% of all lakes) lakes. We also found that lake size varies with dam type; with dammed lakes tending to have larger areas than embedded lakes. The inventory presented provides an unparalleled view of the current state of glacial lakes in Peru and represents an important first step towards (1) improved understanding of glacial lakes and their topographic and morphological characteristics and (2) assessing risk associated with GLOFs.

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