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Albedo over the boreal forest.

Using the Boreal Ecosystem‐Atmosphere Study mesonet data, we show the annual cycle of albedo for 1994 and 1995 at 10 sites; two over grass, one over an aspen forest, and an average of seven over coniferous forests. Representative daily average albedo values in summer are 0.2 over grass, 0.15 for aspen, and 0.083 for the conifer sites. In winter the corresponding mean albedo for snow‐covered grass, aspen, and conifer sites with snow under the canopy are 0.75, 0.21, and 0.13. The jack pine sites have a higher mean winter albedo of 0.15 than the predominantly spruce sites for which mean albedo is only 0.11. Forest albedo increases at all sites in winter (with snow on the ground under the canopy) as the ratio of diffuse to total solar flux increases. The albedo of the conifer sites in winter rarely reaches 0.3.

NOTE: The published paper has 4 typographic errors in Table 2 [which was typeset very late, without me correcting the proofs]. These should be visible as corrections with recent versions of Acrobat.

Table 2 corrections

-#3 aspen snow: missing count is (260)

-#10 snow: 0.129 ± 0.110

-#6 no snow: 0.085 ± 0.009

-#8 snow: 0.097 ± 0.076

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Full Citation

Betts A. K. and J. H. Ball, 1997: Albedo over the boreal forest. J. Geophys. Res., 102, 28901-28910.