Since 2010, multiple high Snowline years have been observed.
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At the permanent" Snowline a further abrupt fall occurs and
we find hardly a tenth of what is found at the forestline.
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The Snowline is an imaginary line running across the mountain
range above which the snow falls, and differs for different parts of the Himalayas.
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To assess how human-induced climate influences and natural variability affect New Zealand
glaciers requires the use of climate models, Snowline observations and other datasets.
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Continuing the Snowline photograph work will allow us to better
identify climate change tipping points and warning signs for our water resources- and therefore better prepare New Zealand for an uncertain future.