Seasonal variability in velocity and ablation of Te Moeka o Tuawe/Fox Glacier, south Westland, New Zealand |
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Authors: | Heather L Purdie Martin S Brook Ian C Fuller John Appleby |
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Institution: | School of Geography, Environment and Earth Sciences, Victoria University of Wellington, Wellington, New Zealand,;Geography Programme, School of People, Environment and Planning, Massey University, Palmerston North, New Zealand |
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Abstract: | Abstract: Seasonal variations in ablation and surface velocity were investigated on the lower Fox Glacier. Variations occur between summer and winter ablation, with surface velocity also showing marked seasonality. Recent advance has resulted in the glacier gaining around 200 m length since late 2004. Longer term, Fox Glacier appears linked to the Southern Oscillation Index, with positive glacier mass balances associated with negative Southern Oscillation Index (El Niño). An estimated glacier response time of approximately 9–14 years suggests the current terminus advance was linked to mass gains in the mid-1990s. Recent collapses at the terminal face continue to prove a hazard at this busy tourist destination. |
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Keywords: | ablation climate Fox Glacier hazards velocity |
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