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Mass loss on Himalayan glacier endangers water resources

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TLDR
In this paper, the authors collected in 2006 from Naimona'nyi Glacier in the Himalaya (Tibet) lack these distinctive marker horizons suggesting no net accumulation of mass (ice) since at least 1950.
Abstract
[1] Ice cores drilled from glaciers around the world generally contain horizons with elevated levels of beta radioactivity including 36 Cl and 3 H associated with atmospheric thermonuclear bomb testing in the 1950s and 1960s. Ice cores collected in 2006 from Naimona'nyi Glacier in the Himalaya (Tibet) lack these distinctive marker horizons suggesting no net accumulation of mass (ice) since at least 1950. Naimona'nyi is the highest glacier (6050 masl) documented to be losing mass annually suggesting the possibility of similar mass loss on other high-elevation glaciers in low and mid-latitudes under a warmer Earth scenario. If climatic conditions dominating the mass balance of Naimona'nyi extend to other glaciers in the region, the implications for water resources could be serious as these glaciers feed the headwaters of the Indus, Ganges, and Brahmaputra Rivers that sustain one of the world's most populous regions.

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Climate change in mountains: a review of elevation-dependent warming and its possible causes

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Monitoring lake level changes on the Tibetan Plateau using ICESat altimetry data (2003-2009)

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References
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Journal ArticleDOI

Potential impacts of a warming climate on water availability in snow-dominated regions

TL;DR: In a warmer world, less winter precipitation falls as snow and the melting of winter snow occurs earlier in spring, which leads to a shift in peak river runoff to winter and early spring, away from summer and autumn when demand is highest.
Journal ArticleDOI

Climatic warming in the Tibetan Plateau during recent decades

TL;DR: In this paper, the authors collected monthly surface air temperature data from almost every meteorological station on the Tibetan Plateau (TP) since their establishment, and analyzed the temperature series to show that the main portion of the TP has experienced statistically significant warming since the mid-1950s, especially in winter, but the recent warming in the central and eastern TP did not reach the level of the 1940s warm period until the late 1990s.
Journal ArticleDOI

Tropical Climate Instability: The Last Glacial Cycle from a Qinghai-Tibetan Ice Core

TL;DR: An ice core record from the Guliya ice cap on the Qinghai-Tibetan Plateau provides evidence of regional climatic conditions over the last glacial cycle as discussed by the authors.
Journal ArticleDOI

Late glacial stage and holocene tropical ice core records from huascaran, peru.

TL;DR: Two ice cores from the col of Huascar�n in the north-central Andes of Peru contain a paleoclimatic history extending well into the Wisconsinan (W�rm) Glacial Stage and include evidence of the Younger Dryas cool phase, implying that a strong warming has dominated the last two centuries.
Journal ArticleDOI

A High-Resolution Millennial Record of the South Asian Monsoon from Himalayan Ice Cores

TL;DR: A high-resolution ice core record from Dasuopu, Tibet, reveals that this site is sensitive to fluctuations in the intensity of the South Asian Monsoon, and suggests a large-scale, plateau-wide 20th-century warming trend that appears to be amplified at higher elevations.
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