Twenty-first Century Glaciers and Climate in the Prokletije Mountains, Albania

2009/11/01 by Philip D. Hughes · 4 citations
Earth and Planetary Sciences · Environmental Science · #Cryospheric studies and observations #Climate change and permafrost #Landslides and related hazards

paper · doi:10.1657/1938-4246-41.4.455

openalex publication_date 2009/11/01 · openalex created_date 2016/06/24 · openalex updated_date 2026/07/02

Abstract

At least four active glaciers are present in the Prokletije Mountains of northern Albania. These glaciers exist at altitudes between 1980 and 2420 m a.s.l.—well below the regional equilibrium line altitude—on shaded northeast-facing slopes prone to avalanche. Glacier-climate modeling suggests that these glaciers require annual accumulation of between 4137 and 5531 mm (water equivalent) to balance melting. A significant proportion of this accumulation is likely to be sourced from windblown snow and, in particular, avalanching snow. It is estimated that the total accumulation needed to balance melting is potentially up to twice the value received from direct precipitation. The presence of these glaciers—some of the southernmost in Europe—at altitudes well below the regional equilibrium line altitude, highlights the importance of local controls on glacier development.

Citations

• Mass balance and equilibrium-line altitudes of glaciers in high-mountain environments
• Estimating equilibrium-line altitude (ELA) from glacier inventory data

Cited by

• Characteristics of mountain glaciers in the northern Japanese Alps
• Europe’s southernmost glaciers: response and adaptation to climate change
• Determining the cooling magnitude in the east of China during the Last Glacial Maximum using a degree-day model
• Albania [wikipedia]

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