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Frontiers The Snowline and 0°C Isotherm Altitudes During

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Frontiers  The Snowline and 0°C Isotherm Altitudes During
A continuous centennial Lateglacial-Early Holocene (15-10 cal kyr

A continuous centennial Lateglacial-Early Holocene (15-10 cal kyr

Freezing level - Wikipedia

Freezing level - Wikipedia

Spatial and temporal patterns of snowmelt refreezing in a

Spatial and temporal patterns of snowmelt refreezing in a

Chapter 2: High Mountain Areas — Special Report on the Ocean and

Chapter 2: High Mountain Areas — Special Report on the Ocean and

Discrimination of glacier facies using multi-temporal SAR data, Journal of  Glaciology

Discrimination of glacier facies using multi-temporal SAR data, Journal of Glaciology

Why is the snow line higher in the Himalayas than on the equator

Why is the snow line higher in the Himalayas than on the equator

Recent mass-balance changes of Agua Negra glacier (30°S) in the

Recent mass-balance changes of Agua Negra glacier (30°S) in the

Frontiers  Late Quaternary glacier advances in the Andes of Santiago,  central Chile, and paleoclimatic implications

Frontiers Late Quaternary glacier advances in the Andes of Santiago, central Chile, and paleoclimatic implications

Frontiers  Simulation of Long-Term Changes of the Equilibrium Line Altitude  in the Central Chilean Andes Mountains Derived From Atmospheric Variables  During the 1958–2018 Period

Frontiers Simulation of Long-Term Changes of the Equilibrium Line Altitude in the Central Chilean Andes Mountains Derived From Atmospheric Variables During the 1958–2018 Period