Articles | Volume 10, issue 1
The Cryosphere, 10, 313–328, 2016
https://doi.org/10.5194/tc-10-313-2016
The Cryosphere, 10, 313–328, 2016
https://doi.org/10.5194/tc-10-313-2016
Research article
10 Feb 2016
Research article | 10 Feb 2016

Cloud effects on surface energy and mass balance in the ablation area of Brewster Glacier, New Zealand

J. P. Conway and N. J. Cullen

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Cited articles

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Short summary
Clouds are shown to force fundamental changes in the surface energy and mass balance of Brewster Glacier, New Zealand. Cloudy periods exhibit greater melt due to increased incoming long-wave radiation and higher atmospheric vapour pressure rather than through minimal changes in mean air temperature and wind speed. Surface mass-balance sensitivity to air temperature is enhanced in overcast compared to clear-sky periods due to more frequent melt and a strong precipitation phase to albedo feedback.