Abstract. Light transmission into bare glacial ice affects surface
energy balance, biophotochemistry, and light detection and ranging (lidar)
laser elevation measurements but has not previously been reported for the
Greenland Ice Sheet. We present measurements of spectral transmittance at
350–900 nm in bare glacial ice collected at a field site in the western
Greenland ablation zone (67.15∘ N, 50.02∘ W). Empirical irradiance
attenuation coefficients at 350–750 nm are ∼ 0.9–8.0 m−1 for ice at 12–124 cm depth. The absorption minimum is at
∼ 390–397 nm, in agreement with snow transmission
measurements in Antarctica and optical mapping of deep ice at the South
Pole. From 350–530 nm, our empirical attenuation coefficients are nearly
1 order of magnitude larger than theoretical values for optically pure
ice. The estimated absorption coefficient at 400 nm suggests the ice volume
contained a light-absorbing particle concentration equivalent to
∼ 1–2 parts per billion (ppb) of black carbon, which is similar to
pre-industrial values found in remote polar snow. The equivalent mineral
dust concentration is ∼ 300–600 ppb, which is similar to values for
Northern Hemisphere warm periods with low aeolian activity inferred from ice
cores. For a layer of quasi-granular white ice (weathering crust)
extending from the surface to ∼ 10 cm depth, attenuation
coefficients are 1.5 to 4 times larger than for deeper bubbly ice. Owing to
higher attenuation in this layer of near-surface granular ice, optical
penetration depth at 532 nm is 14 cm (20 %) lower than asymptotic
attenuation lengths for optically pure bubbly ice. In addition to the
traditional concept of light scattering on air bubbles, our results imply
that the granular near-surface ice microstructure of weathering crust is
an important control on radiative transfer in bare ice on the Greenland Ice
Sheet ablation zone, and we provide new values of flux attenuation,
absorption, and scattering coefficients to support model development and
validation.