This study reports on the radiation and energy balance of three sites (rural, suburban, and urban) located along an urbanization gradient in the Montreal, QC, region for two winters (December-March) with contrasting snow regimes. The urban and suburban sites had similar albedo which was about half that at the rural site during the snow-cover period. Temporal variability in albedo was attributable to the presence of snow on rooftops at the urban site and to a site-specific response to cloudiness at the suburban site. As compared to the suburban site, the urban site showed higher albedo inducing lower net radiation (Q * ) which was compensated for by greater anthropogenic heat flux (Q F ), so that the urban site had highest total available energy (Q * + Q F ). Hourly Q F estimates were a significant term in the winter energy budget analysis. Q F was dominated by building heating at both urbanized sites, while vehicular traffic contributed to rush hour peaks. Daytime total available energy was mostly dissipated as sensible heat flux (Q H ) at the beginning of the winter season and mostly stored ( Q S ) towards the end of the winter at both urbanized sites. Daytime energy partitioning into Q H and Q S was correlated with air temperature with no significant differences between urbanized sites. On a daily time scale, available energy was mostly stored before noon and dissipated as Q H in the afternoon at both urbanized sites. Urbanized sites showed differences in diurnal variability of Q H and Q S occurring in the afternoon and evening. Latent heat flux (Q E ) was low throughout winter and accounted for 10% of the total available energy during daytime at the urbanized sites. Water vapour emissions showed intra-urban differences in their response to wintertime climatic conditions.