A1 Vertaisarvioitu alkuperäisartikkeli tieteellisessä lehdessä
Effect of small-scale snow surface roughness on snow albedo and reflectance
Tekijät: Manninen Terhikki, Anttila Kati, Jääskeläinen Emmihenna, Riihelä Aku, Peltoniemi Jouni, Räisänen Petri, Lahtinen Panu, Siljamo Niilo, Thölix Laura, Meinander Outi, Kontu Anna, Suokanerva Hanne, Pirazzini Roberta, Suomalainen Juha, Hakala Teemu, Kaasalainen Sanna, Kaartinen Harri, Kukko Antero, Hautecoeur Olivier, Roujean Jean-Louis
Kustantaja: COPERNICUS GESELLSCHAFT MBH
Julkaisuvuosi: 2021
Journal: Cryosphere
Tietokannassa oleva lehden nimi: CRYOSPHERE
Lehden akronyymi: CRYOSPHERE
Vuosikerta: 15
Numero: 2
Aloitussivu: 793
Lopetussivu: 820
Sivujen määrä: 28
ISSN: 1994-0416
eISSN: 1994-0424
DOI: https://doi.org/10.5194/tc-15-793-2021
Verkko-osoite: https://tc.copernicus.org/articles/15/793/2021/
Rinnakkaistallenteen osoite: https://research.utu.fi/converis/portal/detail/Publication/53693386
The primary goal of this paper is to present a model of snow surface albedo accounting for small-scale surface roughness effects. The model is based on photon recollision probability, and it can be combined with existing bulk volume albedo models, such as Two-streAm Radiative Trans-fEr in Snow (TARTES). The model is fed with in situ measurements of surface roughness from plate profile and laser scanner data, and it is evaluated by comparing the computed albedos with observations. It provides closer results to empirical values than volume-scattering-based albedo simulations alone. The impact of surface roughness on albedo increases with the progress of the melting season and is larger for larger solar zenith angles. In absolute terms, small-scale surface roughness can decrease the total albedo by up to about 0.1. As regards the bidirectional reflectance factor (BRF), it is found that surface roughness increases backward scattering especially for large solar zenith angle values.
Ladattava julkaisu This is an electronic reprint of the original article. |  |
