Abstract. 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...
Uncertainties in estimation of albedo-related radiative forcing cause ambiguity in evaluation of net...
The boreal–alpine treeline is a fine-spatial heterogeneous ecotone with small single trees, tree clu...
In the presence of snow, the bias in the prediction of surface albedo by many climate models remains...
Uncertainties in estimation of albedo-related radiative forcing cause ambiguity in evaluation of net...
Uncertainties in estimation of albedo-related radiative forcing cause ambiguity in evaluation of net...
Land surface albedo is an essential climate variable controlling the planetary radiative energy budg...
The importance to consider changes in surface albedo and go beyond simple carbon accounting when ass...
Albedo and fraction of absorbed photosynthetically active radiation (FAPAR) determine the shortwave ...
Predicting the surface albedo of a forest of a given species composition or plant functional type is...
Surface albedo, which is the fraction of reflected radiant energy by earth’s surface to incoming sol...
<p>Land surface albedo is a key parameter of the Earth’s climate system. It has high variability in ...
Albedo and fraction of absorbed photosynthetically active radiation (FAPAR) determine the shortwave ...
Vegetation cover and land-use changes induced by human activities have changed the global surface al...
Vegetation albedo is a critical component of the Earth's climate system, yet efforts to evaluate and...
The relationship of black-sky and white-sky albedo values of snow-covered terrain is studied using e...
Uncertainties in estimation of albedo-related radiative forcing cause ambiguity in evaluation of net...
The boreal–alpine treeline is a fine-spatial heterogeneous ecotone with small single trees, tree clu...
In the presence of snow, the bias in the prediction of surface albedo by many climate models remains...
Uncertainties in estimation of albedo-related radiative forcing cause ambiguity in evaluation of net...
Uncertainties in estimation of albedo-related radiative forcing cause ambiguity in evaluation of net...
Land surface albedo is an essential climate variable controlling the planetary radiative energy budg...
The importance to consider changes in surface albedo and go beyond simple carbon accounting when ass...
Albedo and fraction of absorbed photosynthetically active radiation (FAPAR) determine the shortwave ...
Predicting the surface albedo of a forest of a given species composition or plant functional type is...
Surface albedo, which is the fraction of reflected radiant energy by earth’s surface to incoming sol...
<p>Land surface albedo is a key parameter of the Earth’s climate system. It has high variability in ...
Albedo and fraction of absorbed photosynthetically active radiation (FAPAR) determine the shortwave ...
Vegetation cover and land-use changes induced by human activities have changed the global surface al...
Vegetation albedo is a critical component of the Earth's climate system, yet efforts to evaluate and...
The relationship of black-sky and white-sky albedo values of snow-covered terrain is studied using e...
Uncertainties in estimation of albedo-related radiative forcing cause ambiguity in evaluation of net...
The boreal–alpine treeline is a fine-spatial heterogeneous ecotone with small single trees, tree clu...
In the presence of snow, the bias in the prediction of surface albedo by many climate models remains...