TY - GEN
T1 - Cobertura glaciar de los nevados del distrito de Catac, Ancash y su relación con la precipitación y temperatura durante el periodo 1988-2022
AU - Roberto, Chuquilín Goicochea
AU - Alberto, Palacios Miñano
AU - Rosnell, Domínguez Marchena
N1 - Publisher Copyright:
© 2024 Latin American and Caribbean Consortium of Engineering Institutions. All rights reserved.
PY - 2024
Y1 - 2024
N2 - The objective of this research was to analyze how precipitation and temperature affect changes in the glacial coverage of the snow-capped mountains of the Catac district during the period from 1988 to 2022. An applied study was carried out with an explanatory level and a longitudinal design. non-experimental, since the period from 1988 to 2022 was temporally analyzed. The remote sensing technique and the NDSI index (Normalized Differential Snow Index) were used to recognize the glacier, and the climate information was obtained from the PISCO-SENAMHI grid product. A decrease in glacier coverage was observed at a rate of 0.73 km2 per year. The statistical correlation analysis revealed that temperature is the only factor that significantly influences changes in glacier cover, while precipitation is part of the glaciological balance system, but its influence on surface changes is not significant due to a superficial and non-volumetric analysis. In conclusion, the increase in temperature has a notable impact on glacier coverage, through the melting and instability of the ice.
AB - The objective of this research was to analyze how precipitation and temperature affect changes in the glacial coverage of the snow-capped mountains of the Catac district during the period from 1988 to 2022. An applied study was carried out with an explanatory level and a longitudinal design. non-experimental, since the period from 1988 to 2022 was temporally analyzed. The remote sensing technique and the NDSI index (Normalized Differential Snow Index) were used to recognize the glacier, and the climate information was obtained from the PISCO-SENAMHI grid product. A decrease in glacier coverage was observed at a rate of 0.73 km2 per year. The statistical correlation analysis revealed that temperature is the only factor that significantly influences changes in glacier cover, while precipitation is part of the glaciological balance system, but its influence on surface changes is not significant due to a superficial and non-volumetric analysis. In conclusion, the increase in temperature has a notable impact on glacier coverage, through the melting and instability of the ice.
KW - Remote sensing
KW - glacier coverage
KW - precipitation
KW - satellite images
KW - temperature
UR - https://www.scopus.com/pages/publications/85217213238
U2 - 10.18687/LEIRD2024.1.1.218
DO - 10.18687/LEIRD2024.1.1.218
M3 - Contribución a la conferencia
AN - SCOPUS:85217213238
T3 - Proceedings of the LACCEI international Multi-conference for Engineering, Education and Technology
BT - Proceedings of the 4th LACCEI International Multiconference on Entrepreneurship, Innovation and Regional Development
A2 - Larrondo Petrie, Maria M.
A2 - Texier, Jose
A2 - Matta, Rodolfo Andres Rivas
T2 - 4th LACCEI International Multiconference on Entrepreneurship, Innovation and Regional Development, LEIRD 2024
Y2 - 2 December 2024 through 4 December 2024
ER -