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Agric For Meteorol. 2016 Oct 15;226-227:37-49. doi: 10.1016/j.agrformet.2016.05.012.

On the energy balance closure and net radiation in complex terrain.

Author information

1
Institute of Ecology, University of Innsbruck, Sternwartestr. 15, 6020 Innsbruck, AUSTRIA; Institute for Alpine Environment, European Academy of Bolzano, Drususalle 1, 39100 Bolzano, ITALY; Institute for Applied Remote Sensing, European Academy of Bolzano, Drususalle 1, 39100 Bolzano, ITALY.
2
Institute of Ecology, University of Innsbruck, Sternwartestr. 15, 6020 Innsbruck, AUSTRIA.
3
Institute for Alpine Environment, European Academy of Bolzano, Drususalle 1, 39100 Bolzano, ITALY.
4
Institute for Applied Remote Sensing, European Academy of Bolzano, Drususalle 1, 39100 Bolzano, ITALY.

Abstract

In complex, sloping terrain, horizontal measurements of net radiation are not reflective of the radiative energy available for the conductive and convective heat exchange of the underlying surface. Using data from a grassland site on a mountain slope characterised by spatial heterogeneity in inclination and aspect, we tested the hypothesis that a correction of the horizontal net radiation measurements which accounts for the individual footprint contributions of the various surfaces to the measured sensible and latent heat eddy covariance fluxes will yield more realistic slope-parallel net radiation estimates compared to a correction based on the average inclination and aspect of the footprint. Our main result is that both approaches led to clear, but very similar improvements in the phase between available energy and the sum of the latent and sensible heat fluxes. As a consequence the variance in the sum of latent and sensible heat flux explained by available radiation improved by >10 %, while energy balance closure improved only slightly. This is shown to be mainly due to the average inclination and aspect corresponding largely with the inclination and aspect of the main flux source area in combination with a limited sensitivity of the slope correction to small angular differences in, particularly, inclination and aspect. We conclude with a discussion of limitations of the present approach and future research directions.

KEYWORDS:

eddy covariance; footprint; grassland; slope

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