Understanding drivers of glacier-length variability over the last millennium

@article{Huston2021UnderstandingDO,
  title={Understanding drivers of glacier-length variability over the last millennium},
  author={Alan Huston and Nicholas Siler and Gerard H. Roe and Erin Christine Pettit and Nathan J. Steiger},
  journal={The Cryosphere},
  year={2021},
  volume={15},
  pages={1645-1662}
}
Abstract. Changes in glacier length reflect the integrated response to local fluctuations in temperature and precipitation resulting from both external forcing (e.g., volcanic eruptions or anthropogenic CO 2 ) and internal climate variability. In order to interpret the climate history reflected in the glacier moraine record, the influence of both sources of climate variability must therefore be considered. Here we study the last millennium of glacier-length variability across the globe using a… 

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References

SHOWING 1-10 OF 39 REFERENCES

The response of glaciers to intrinsic climate variability: observations and models of late-Holocene variations in the Pacific Northwest

Abstract Discriminating between glacier variations due to natural climate variability and those due to true climate change is crucial for the interpretation and attribution of past glacier changes,

The effects of interannual climate variability on the moraine record

Valley glacier moraines are commonly used to infer past mean annual precipitation and mean melt-season temperature. However, recent research has demonstrated that, even in steady climates,

The absence of memory in the climatic forcing of glaciers

Glaciers respond to both long-term, persistent climate changes as well as the year-to-year variability that is inherent to a constant climate. Distinguishing between these two causes of length change

Centennial glacier retreat as categorical evidence of regional climate change

The near-global retreat of glaciers over the last century provides some of the most iconic imagery for communicating the reality of anthropogenic climate change to the public. Surprisingly, however,

Influence of North Atlantic climate variability on glacier mass balance in Norway, Sweden and Svalbard

ABSTRACT Climate variability can complicate efforts to interpret any long-term glacier mass-balance trends due to anthropogenic warming. Here we examine the impact of climate variability on the

Committed retreat: controls on glacier disequilibrium in a warming climate

ABSTRACT The widespread retreat of mountain glaciers is a striking emblem of recent climate change. Yet mass-balance observations indicate that many glaciers are out of equilibrium with current

On the attribution of industrial-era glacier mass loss to anthropogenic climate change

Abstract. Around the world, small ice caps and glaciers have been losing mass and retreating since the start of the industrial era. Estimates are that this has contributed approximately 30 % of the

Holocene glacier fluctuations: is the current rate of retreat exceptional?

Abstract Most glaciers in the Northern Hemisphere reached their postglacial maximum in recent times, that is, after the medieval period. During the last 100 or 150 years a significant retreat has

How sensitive are mountain glaciers to climate change? Insights from a block model

ABSTRACT Simple models of glacier volume evolution are important in understanding features of glacier response to climate change, due to the scarcity of data adequate for running more complex models

Trends and variability in the global dataset of glacier mass balance

Glacier mass balance (i.e., accumulation and ablation) is the most direct connection between climate and glaciers. We perform a comprehensive evaluation of the available global network of