Estimation of Glacier Outline and Volume Changes in the Vilcanota Range Snow-Capped Mountains, Peru, Using Temporal Series of Landsat and a Combination of Satellite Radar and Aerial LIDAR Images


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Article

by

Nilton Montoya-Jara

1,

Hildo Loayza

2,3,*,

Raymundo Oscar Gutiérrez-Rosales

4,

Marcelo Bueno

1 and

Roberto Quiroz

5

1

Facultad de Agronomía y Zootecnia, Escuela Profesional de Agronomía, Universidad Nacional San Antonio Abad del Cusco (UNSAAC), Cusco 08003, Peru

2

International Potato Center (CIP), Headquarters P.O. Box 1558, Lima 15024, Peru

3

Programa Académico de Ingeniería Ambiental, Facultad de Ingeniería, Universidad de Huánuco, Huánuco 10001, Peru

4

Facultad de Ingeniería Agrícola, Universidad Nacional Agraria de La Molina, Lima 15012, Peru

5

Instituto de Innovación Agropecuaria de Panamá (IDIAP), Estación Experimental de Cerro Punta—Chiriquí, Panama y Sistema Nacional de Investigación (SNI-SENACYT) Ciudad del Saber, Edificio 161, Clayton, Panama

*

Author to whom correspondence should be addressed.

Remote Sens. 2024, 16(20), 3901; https://doi.org/10.3390/rs16203901 (registering DOI)

Submission received: 23 August 2024
/
Revised: 13 October 2024
/
Accepted: 16 October 2024
/
Published: 20 October 2024

Abstract

The Vilcanota is the second-largest snow-capped mountain range in Peru, featuring 380 individual glaciers, each with its own unique characteristics that must be studied independently. However, few studies have been conducted in the Vilcanota range to monitor and track the area and volume changes of the Suyuparina and Quisoquipina glaciers. Notably, there are only a few studies that have approached this issue using LIDAR technology. Our methodology is based on a combination of optical, radar and LIDAR data sources, which allowed for constructing coherent temporal series for the both the perimeter and volume changes of the Suyuparina and Quisoquipina glaciers while accounting for the uncertainty in the perimeter detection procedure. Our results indicated that, from 1990 to 2013, there was a reduction in snow cover of 12,694.35 m2 per year for Quisoquipina and 16,599.2 m2 per year for Suyuparina. This represents a loss of 12.18% for Quisoquipina and 22.45% for Suyuparina. From 2006 to 2013, the volume of the Quisoquipina glacier decreased from 11.73 km3 in 2006 to 11.04 km3 in 2010, while the Suyuparina glacier decreased from 6.26 km3 to 5.93 km3. Likewise, when analyzing the correlation between glacier area and precipitation, a moderate inverse correlation (R = −0.52, p < 0.05) was found for Quisoquipina. In contrast, the correlation for Suyuparina was low and nonsignificant, showing inconsistency in the effect of precipitation. Additionally, the correlation between the snow cover area and the annual mean air temperature (R = −0.34, p > 0.05) and annual minimum air temperature (R = −0.36, p > 0.05) was low, inverse, and not significant for Quisoquipina. Meanwhile, snow cover on Suyuparina had a low nonsignificant correlation (R = −0.31, p > 0.05) with the annual maximum air temperature, indicating a minimal influence of the measured climatic variables near this glacier on its retreat. In general, it was possible to establish a reduction in both the area and volume of the Suyuparina and Quisoquipina glaciers based on freely accessible remote sensing data.



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