Due to their high sensitivity to changes in climate, glaciers are one of the best natural indicators of climate change. Despite this, many underlying processes that control glacier response to climate change are poorly understood.
Eric Johnson, S. Rupper
semanticscholar +1 more source
One Decade of Glacier Mass Changes on the Tibetan Plateau Derived from Multisensoral Remote Sensing Data [PDF]
The Tibetan Plateau (TP) with an average altitude of 4,500 meters above sea level is characterized by many glaciers and ice caps. Glaciers are a natural indicator for climate variability in this high mountain environment where meteorological stations are
Neckel, Niklas
core +1 more source
The climatic mass balance of Svalbard glaciers: a 10-year simulation with a coupled atmosphere–glacier mass balance model [PDF]
Abstract. In this study we simulate the climatic mass balance of Svalbard glaciers with a coupled atmosphere–glacier model with 3 km grid spacing, from September 2003 to September 2013. We find a mean specific net mass balance of −257 mm w.e. yr−1, corresponding to a mean annual mass loss of about 8.7 Gt, with large interannual variability. Our results
Kjetil S. Aas +6 more
openaire +4 more sources
Glacier mass balance changes and meltwater discharge [PDF]
Ginot, Patrick (ed.) +1 more
core +4 more sources
We present the first-ever mass-balance (MB) observation (2014–19), reconstruction (between 1978 and 2019) and sensitivity of debris-free Stok glacier (33.98°N, 77.45°E), Ladakh Region, India.
M. Soheb +5 more
semanticscholar +1 more source
Common climatic signal from glaciers in the European Alps over the last 50 years [PDF]
Conventional glacier-wide mass balances are commonly used to study the effect of climate forcing on glacier melt. Unfortunately, the glacier-wide mass balances are also influenced by the glacier's dynamic response.
A. Bauder +12 more
core +1 more source
Modelling the 20th and 21st century evolution of Hoffellsjökull glacier, SE-Vatnajökull, Iceland [PDF]
The Little Ice Age maximum extent of glaciers in Iceland was reached about 1890 AD and most glaciers in the country have retreated during the 20th century.
E. Berthier +7 more
core +4 more sources
Mass-balance reconstruction for Glacier No. 354, Tien Shan, from 2003 to 2014 [PDF]
This study presents a reconstruction of the seasonal mass balance of Glacier No. 354, located in the Akshiirak range, Kyrgyzstan, from 2003 to 2014. We use a distributed accumulation and temperature-index melt model driven by daily air temperature and
Azisov, Erlan +9 more
core +1 more source
Can shrubs help to reconstruct historical glacier retreats?
In the 21st century, most of the world’s glaciers are expected to retreat due to further global warming. The range of this predicted retreat varies widely as a result of uncertainties in climate and glacier models.
Allan Buras +2 more
doaj +1 more source
Modeling the impacts of climate trends and lake formation on the retreat of a tropical Andean glacier (1962–2020) [PDF]
Located in Peru's Cordillera Blanca, the Queshque Glacier (∼9.8° S) has experienced nearly continuous retreat since the mid-20th century. More recently, this trend has accelerated after the glacier transitioned from land to lake terminating.
T. Y. Shutkin +11 more
doaj +1 more source

