Understanding the Susceptibility of the Tropical Proglacial Environment in Peru Using Optical Imagery and Radon Measurements

The tropical glaciers of the Cordillera Blanca have played host to some of the most significant mass movements ever recorded in the world and Peru; many proglacial lakes formed in this mountain range have natural dikes made of moraine material, which, if they collapse, would present a risk for the c...

Full description

Bibliographic Details
Main Authors: Diego Antonio García-Tadeo, Modesto Montoya-Zavaleta, Yumin Tan
Format: Article
Language:English
Published: MDPI AG 2023-03-01
Series:Atmosphere
Subjects:
Online Access:https://www.mdpi.com/2073-4433/14/3/568
_version_ 1797613543009288192
author Diego Antonio García-Tadeo
Modesto Montoya-Zavaleta
Yumin Tan
author_facet Diego Antonio García-Tadeo
Modesto Montoya-Zavaleta
Yumin Tan
author_sort Diego Antonio García-Tadeo
collection DOAJ
description The tropical glaciers of the Cordillera Blanca have played host to some of the most significant mass movements ever recorded in the world and Peru; many proglacial lakes formed in this mountain range have natural dikes made of moraine material, which, if they collapse, would present a risk for the cities located downstream of a proglacial lake, where the proglacial lake Palcacocha has a remarkable background regarding floods. The Sentinel-2 MSI (Multi-Spectral Instrument, Level-2A) has a specific band for snow probability mapping that indicates glaciers and snow cover; this is effective for recognizing proglacial lakes by calculating the <i>NDWI<sub>ice</sub></i>. It is also helpful for lithology with <i>SWIR</i> for granite moraine deposits and slate moraines in the proglacial environment Palcacocha; these deposits surround the proglacial lake, with <i>NDWI<sub>ice</sub></i> determining the perimeter where sediment interacts with the rocks and meltwater. In addition, there are high radon concentrations made by ice avalanche impacts on the proglacial lake. Unstable glacier blocks cause ice avalanches into this proglacial lake, and the radon responds to flow variations from these high-impact avalanches. We used the device RadonEye PLus2, which allows real-time detection of radon flux changes in the proglacial environment. Our results indicated that ice avalanches making a high impact in the proglacial lake cause turbulent flow and generate radon concentration marks with a rising magnitude, while the absence of ice avalanches in the lake will cause the values to go down. The relationships of radon concentrations in the atmosphere for a tropical proglacial environment are radon and temperature (R<sup>2</sup> = 0.364), radon and humidity (R<sup>2</sup> = 0.469). In a passive proglacial environment with prolonged rainfall, radon concentrations tend to decrease, with an inversely proportional relationship between humidity and radon in the tropical proglacial environment. Proglacial lakes in the tropical zone often have large volumes of freshwater with high slopes from tropical glaciers, and climate change effects are an imminent danger for nearby cities.
first_indexed 2024-03-11T06:56:14Z
format Article
id doaj.art-223fa29d0597432292d99c72988f3472
institution Directory Open Access Journal
issn 2073-4433
language English
last_indexed 2024-03-11T06:56:14Z
publishDate 2023-03-01
publisher MDPI AG
record_format Article
series Atmosphere
spelling doaj.art-223fa29d0597432292d99c72988f34722023-11-17T09:33:34ZengMDPI AGAtmosphere2073-44332023-03-0114356810.3390/atmos14030568Understanding the Susceptibility of the Tropical Proglacial Environment in Peru Using Optical Imagery and Radon MeasurementsDiego Antonio García-Tadeo0Modesto Montoya-Zavaleta1Yumin Tan2School of Transportation Science and Engineering, Beihang University, No. 37 Xueyuan Road, Haidian District, Beijing 100191, ChinaGraduate School of Science, Universidad Nacional de Ingeniería, Av. Túpac Amaru 210, Lima 15333, PeruSchool of Transportation Science and Engineering, Beihang University, No. 37 Xueyuan Road, Haidian District, Beijing 100191, ChinaThe tropical glaciers of the Cordillera Blanca have played host to some of the most significant mass movements ever recorded in the world and Peru; many proglacial lakes formed in this mountain range have natural dikes made of moraine material, which, if they collapse, would present a risk for the cities located downstream of a proglacial lake, where the proglacial lake Palcacocha has a remarkable background regarding floods. The Sentinel-2 MSI (Multi-Spectral Instrument, Level-2A) has a specific band for snow probability mapping that indicates glaciers and snow cover; this is effective for recognizing proglacial lakes by calculating the <i>NDWI<sub>ice</sub></i>. It is also helpful for lithology with <i>SWIR</i> for granite moraine deposits and slate moraines in the proglacial environment Palcacocha; these deposits surround the proglacial lake, with <i>NDWI<sub>ice</sub></i> determining the perimeter where sediment interacts with the rocks and meltwater. In addition, there are high radon concentrations made by ice avalanche impacts on the proglacial lake. Unstable glacier blocks cause ice avalanches into this proglacial lake, and the radon responds to flow variations from these high-impact avalanches. We used the device RadonEye PLus2, which allows real-time detection of radon flux changes in the proglacial environment. Our results indicated that ice avalanches making a high impact in the proglacial lake cause turbulent flow and generate radon concentration marks with a rising magnitude, while the absence of ice avalanches in the lake will cause the values to go down. The relationships of radon concentrations in the atmosphere for a tropical proglacial environment are radon and temperature (R<sup>2</sup> = 0.364), radon and humidity (R<sup>2</sup> = 0.469). In a passive proglacial environment with prolonged rainfall, radon concentrations tend to decrease, with an inversely proportional relationship between humidity and radon in the tropical proglacial environment. Proglacial lakes in the tropical zone often have large volumes of freshwater with high slopes from tropical glaciers, and climate change effects are an imminent danger for nearby cities.https://www.mdpi.com/2073-4433/14/3/568tropical glacierproglacial environmentremote sensingradonPeru
spellingShingle Diego Antonio García-Tadeo
Modesto Montoya-Zavaleta
Yumin Tan
Understanding the Susceptibility of the Tropical Proglacial Environment in Peru Using Optical Imagery and Radon Measurements
Atmosphere
tropical glacier
proglacial environment
remote sensing
radon
Peru
title Understanding the Susceptibility of the Tropical Proglacial Environment in Peru Using Optical Imagery and Radon Measurements
title_full Understanding the Susceptibility of the Tropical Proglacial Environment in Peru Using Optical Imagery and Radon Measurements
title_fullStr Understanding the Susceptibility of the Tropical Proglacial Environment in Peru Using Optical Imagery and Radon Measurements
title_full_unstemmed Understanding the Susceptibility of the Tropical Proglacial Environment in Peru Using Optical Imagery and Radon Measurements
title_short Understanding the Susceptibility of the Tropical Proglacial Environment in Peru Using Optical Imagery and Radon Measurements
title_sort understanding the susceptibility of the tropical proglacial environment in peru using optical imagery and radon measurements
topic tropical glacier
proglacial environment
remote sensing
radon
Peru
url https://www.mdpi.com/2073-4433/14/3/568
work_keys_str_mv AT diegoantoniogarciatadeo understandingthesusceptibilityofthetropicalproglacialenvironmentinperuusingopticalimageryandradonmeasurements
AT modestomontoyazavaleta understandingthesusceptibilityofthetropicalproglacialenvironmentinperuusingopticalimageryandradonmeasurements
AT yumintan understandingthesusceptibilityofthetropicalproglacialenvironmentinperuusingopticalimageryandradonmeasurements