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Volume 10, issue 1
The Cryosphere, 10, 313–328, 2016
https://doi.org/10.5194/tc-10-313-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
The Cryosphere, 10, 313–328, 2016
https://doi.org/10.5194/tc-10-313-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.

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  
Ackerley, D., Lorrey, A., Renwick, J. A., Phipps, S. J., Wagner, S., Dean, S., Singarayer, J., Valdes, P., Abe-Ouchi, A., Ohgaito, R., and Jones, J. M.: Using synoptic type analysis to understand New Zealand climate during the Mid-Holocene, Clim. Past, 7, 1189–1207, https://doi.org/10.5194/cp-7-1189-2011, 2011.
Ambach, W.: The influence of cloudiness on the net radiation balance of a snow surface with high albedo, J. Glaciol., 13, 73–84, 1974.
Anderson, B., Lawson, W., Owens, I., and Goodsell, B.: Past and future mass balance of “Ka Roimata o Hine Hukatere” Franz Josef Glacier, New Zealand, J. Glaciol., 52, 597–607, https://doi.org/10.3189/172756506781828449, 2006.
Anderson, B., Mackintosh, A., Stumm, D., George, L., Kerr, T., Winter-Billington, A., and Fitzsimons, S.: Climate sensitivity of a high-precipitation glacier in New Zealand, J. Glaciol., 56, 114–128, https://doi.org/10.3189/002214310791190929, 2010.
Blonquist, J. M., Tanner, B. D., and Bugbee, B.: Evaluation of measurement accuracy and comparison of two new and three traditional net radiometers, Agr. For. Meteorol., 149, 1709–1721, https://doi.org/10.1016/j.agrformet.2009.05.015, 2009.
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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.
Clouds are shown to force fundamental changes in the surface energy and mass balance of Brewster...
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