Annual Variability in the Cordillera Blanca Snow Accumulation Area Between 1988 and 2023 Using a Cloud Processing Platform

Tropical glaciers are highly sensitive to climate change, with their mass balance influenced by temperature and precipitation, which affects the accumulation area. In this study, we developed an open-source tool to map the accumulation area of glaciers in the Cordillera Blanca, Peru (1988–2023), usi...

Full description

Saved in:
Bibliographic Details
Main Authors: Júlia Lopes Lorenz, Kátia Kellem da Rosa, Rafael da Rocha Ribeiro, Rolando Cruz Encarnación, Adina Racoviteanu, Federico Aita, Fernando Luis Hillebrand, Jesus Gomez Lopez, Jefferson Cardia Simões
Format: Article
Language:English
Published: MDPI AG 2025-06-01
Series:Geosciences
Subjects:
Online Access:https://www.mdpi.com/2076-3263/15/6/223
Tags: Add Tag
No Tags, Be the first to tag this record!
_version_ 1839653885007888384
author Júlia Lopes Lorenz
Kátia Kellem da Rosa
Rafael da Rocha Ribeiro
Rolando Cruz Encarnación
Adina Racoviteanu
Federico Aita
Fernando Luis Hillebrand
Jesus Gomez Lopez
Jefferson Cardia Simões
author_facet Júlia Lopes Lorenz
Kátia Kellem da Rosa
Rafael da Rocha Ribeiro
Rolando Cruz Encarnación
Adina Racoviteanu
Federico Aita
Fernando Luis Hillebrand
Jesus Gomez Lopez
Jefferson Cardia Simões
author_sort Júlia Lopes Lorenz
collection DOAJ
description Tropical glaciers are highly sensitive to climate change, with their mass balance influenced by temperature and precipitation, which affects the accumulation area. In this study, we developed an open-source tool to map the accumulation area of glaciers in the Cordillera Blanca, Peru (1988–2023), using Landsat images, spectral indices, and the Otsu method. We analyzed trends and correlations between snow accumulation area, meteorological patterns from ERA5 data, and oscillation modes. The results were validated using field data and manual mapping. Greater discrepancies were observed in glaciers with debris cover or small clean glaciers (<1 km<sup>2</sup>). The Amazonian and Pacific sectors showed a significant trend in decreasing accumulation areas, with reductions of 8.99% and 10.24%, respectively, from 1988–1999 to 2010–2023. El Niño events showed higher correlations with snow accumulation, snowfall, and temperature during the wet season, indicating a stronger influence on the Pacific sector. The accumulation area was strongly anti-correlated with temperature and correlated with snowfall in both sectors at a 95% confidence level (α = 0.05). The highest correlations with meteorological parameters were observed during the dry season, suggesting that even minor changes in temperature or precipitation could significantly impact the accumulation area.
format Article
id doaj-art-cc121569d83c4cb7a76584ae1cc968d0
institution Matheson Library
issn 2076-3263
language English
publishDate 2025-06-01
publisher MDPI AG
record_format Article
series Geosciences
spelling doaj-art-cc121569d83c4cb7a76584ae1cc968d02025-06-25T13:54:22ZengMDPI AGGeosciences2076-32632025-06-0115622310.3390/geosciences15060223Annual Variability in the Cordillera Blanca Snow Accumulation Area Between 1988 and 2023 Using a Cloud Processing PlatformJúlia Lopes Lorenz0Kátia Kellem da Rosa1Rafael da Rocha Ribeiro2Rolando Cruz Encarnación3Adina Racoviteanu4Federico Aita5Fernando Luis Hillebrand6Jesus Gomez Lopez7Jefferson Cardia Simões8Centro Polar e Climático, Departamento de Geografia, Instituto de Geociências do Universidade Federal do Rio Grande do Sul, Av. Bento Gonçalves, Porto Alegre 91501-970, RS, BrazilCentro Polar e Climático, Departamento de Geografia, Instituto de Geociências do Universidade Federal do Rio Grande do Sul, Av. Bento Gonçalves, Porto Alegre 91501-970, RS, BrazilCentro Polar e Climático, Departamento de Geografia, Instituto de Geociências do Universidade Federal do Rio Grande do Sul, Av. Bento Gonçalves, Porto Alegre 91501-970, RS, BrazilAutoridad Nacional del Agua, Av. Confraternidad Internacional Oeste No. 167, Independencia, Huaraz 02002, PeruInstitute for Geosciences and Environmental Research (IGE), University Grenoble-Alpes/CNRS/IRD/Grenoble-INP, 38058 Grenoble Cedex 9, FranceCentro Polar e Climático, Departamento de Geografia, Instituto de Geociências do Universidade Federal do Rio Grande do Sul, Av. Bento Gonçalves, Porto Alegre 91501-970, RS, BrazilInstituto Federal de Educação, Ciência e Tecnologia do Rio Grande do Sul (IFRS), Campus Rolante, Rolante 95690-000, RS, BrazilInstituto Nacional de Investigación en Glaciares y Ecosistemas de Montaña, Av. Centenario 2656—Sector Palmira, Independencia, Huaraz 02002, PeruCentro Polar e Climático, Departamento de Geografia, Instituto de Geociências do Universidade Federal do Rio Grande do Sul, Av. Bento Gonçalves, Porto Alegre 91501-970, RS, BrazilTropical glaciers are highly sensitive to climate change, with their mass balance influenced by temperature and precipitation, which affects the accumulation area. In this study, we developed an open-source tool to map the accumulation area of glaciers in the Cordillera Blanca, Peru (1988–2023), using Landsat images, spectral indices, and the Otsu method. We analyzed trends and correlations between snow accumulation area, meteorological patterns from ERA5 data, and oscillation modes. The results were validated using field data and manual mapping. Greater discrepancies were observed in glaciers with debris cover or small clean glaciers (<1 km<sup>2</sup>). The Amazonian and Pacific sectors showed a significant trend in decreasing accumulation areas, with reductions of 8.99% and 10.24%, respectively, from 1988–1999 to 2010–2023. El Niño events showed higher correlations with snow accumulation, snowfall, and temperature during the wet season, indicating a stronger influence on the Pacific sector. The accumulation area was strongly anti-correlated with temperature and correlated with snowfall in both sectors at a 95% confidence level (α = 0.05). The highest correlations with meteorological parameters were observed during the dry season, suggesting that even minor changes in temperature or precipitation could significantly impact the accumulation area.https://www.mdpi.com/2076-3263/15/6/223El Niño—ENSOglacial faciestropical glaciersclimate changeLandsat
spellingShingle Júlia Lopes Lorenz
Kátia Kellem da Rosa
Rafael da Rocha Ribeiro
Rolando Cruz Encarnación
Adina Racoviteanu
Federico Aita
Fernando Luis Hillebrand
Jesus Gomez Lopez
Jefferson Cardia Simões
Annual Variability in the Cordillera Blanca Snow Accumulation Area Between 1988 and 2023 Using a Cloud Processing Platform
Geosciences
El Niño—ENSO
glacial facies
tropical glaciers
climate change
Landsat
title Annual Variability in the Cordillera Blanca Snow Accumulation Area Between 1988 and 2023 Using a Cloud Processing Platform
title_full Annual Variability in the Cordillera Blanca Snow Accumulation Area Between 1988 and 2023 Using a Cloud Processing Platform
title_fullStr Annual Variability in the Cordillera Blanca Snow Accumulation Area Between 1988 and 2023 Using a Cloud Processing Platform
title_full_unstemmed Annual Variability in the Cordillera Blanca Snow Accumulation Area Between 1988 and 2023 Using a Cloud Processing Platform
title_short Annual Variability in the Cordillera Blanca Snow Accumulation Area Between 1988 and 2023 Using a Cloud Processing Platform
title_sort annual variability in the cordillera blanca snow accumulation area between 1988 and 2023 using a cloud processing platform
topic El Niño—ENSO
glacial facies
tropical glaciers
climate change
Landsat
url https://www.mdpi.com/2076-3263/15/6/223
work_keys_str_mv AT julialopeslorenz annualvariabilityinthecordillerablancasnowaccumulationareabetween1988and2023usingacloudprocessingplatform
AT katiakellemdarosa annualvariabilityinthecordillerablancasnowaccumulationareabetween1988and2023usingacloudprocessingplatform
AT rafaeldarocharibeiro annualvariabilityinthecordillerablancasnowaccumulationareabetween1988and2023usingacloudprocessingplatform
AT rolandocruzencarnacion annualvariabilityinthecordillerablancasnowaccumulationareabetween1988and2023usingacloudprocessingplatform
AT adinaracoviteanu annualvariabilityinthecordillerablancasnowaccumulationareabetween1988and2023usingacloudprocessingplatform
AT federicoaita annualvariabilityinthecordillerablancasnowaccumulationareabetween1988and2023usingacloudprocessingplatform
AT fernandoluishillebrand annualvariabilityinthecordillerablancasnowaccumulationareabetween1988and2023usingacloudprocessingplatform
AT jesusgomezlopez annualvariabilityinthecordillerablancasnowaccumulationareabetween1988and2023usingacloudprocessingplatform
AT jeffersoncardiasimoes annualvariabilityinthecordillerablancasnowaccumulationareabetween1988and2023usingacloudprocessingplatform