Journal
JOURNAL OF GLACIOLOGY
Volume 66, Issue 258, Pages 543-555Publisher
CAMBRIDGE UNIV PRESS
DOI: 10.1017/jog.2020.23
Keywords
Debris-covered glaciers; ice/atmosphere interactions; glacier meteorology
Funding
- Austrian Science Fund [V309, P28521, T781-N32]
- Austrian Science Fund (FWF) [P28521] Funding Source: Austrian Science Fund (FWF)
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We present the first direct comparison of turbulence conditions measured simultaneously over exposed ice and a 0.08 m thick supraglacial debris cover on Suldenferner, a small glacier in the Italian Alps. Surface roughness, sensible heat fluxes (similar to 20-50 W m(-2)), latent heat fluxes (similar to 2-10 W m(-2)), topology and scale of turbulence are similar over both glacier surface types during katabatic and synoptically disturbed conditions. Exceptions are sunny days when buoyant convection becomes significant over debris-covered ice (sensible heat flux similar to -100 W m(-2); latent heat flux similar to -30 W m(-2)) and prevailing katabatic conditions are rapidly broken down even over this thin debris cover. The similarity in turbulent properties implies that both surface types can be treated the same in terms of boundary layer similarity theory. The differences in turbulence between the two surface types on this glacier are dominated by the radiative and thermal contrasts, thus during sunny days debris cover alters both the local surface turbulent energy fluxes and the glacier component of valley circulation. These variations under different flow conditions should be accounted for when distributing temperature fields for modeling applications over partially debris-covered glaciers.
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