5Net radiation reaching the forest floor is influenced by vegetation density. Previous studies have 6 confirmed that in mid-latitude conifer forests in Greenville, ME (45.5°N), net radiation decreases 7 and then subsequently increases with increasing vegetation density, for clear sky conditions. This 8 leads to existence of a net radiation minimum at an intermediate vegetation density. With 9 increasing cloud cover, the minimum radiation shifts toward lower densities, sometimes resulting 10 in a monotonically increasing radiation with vegetation density. The net radiation trend, 11 however, is expected to change with location of forests, affecting the magnitude and temporality 12 of individual radiation components. This research explores the variability of net radiation on 13 snow-covered forest floor for different vegetation densities along a latitudinal transect. We 14 especially investigate how the magnitude of minimum/maximum radiation and vegetation 15 density at which they are expressed, changes with site location. To evaluate these, net radiation is 16 calculated using the Forest Radiation Model at six different locations in white spruce (Picea 17 glauca) forests across North America, with latitudes ranging from 45 to 66°N. Results show that 18 the variation of net radiation with vegetation density significantly varies between different 19 latitudes. In higher latitude forests, the magnitude of net radiation is generally smaller, and the 20 minimum radiation is exhibited at relatively sparser vegetation densities, for clear sky conditions. 21For interspersed cloudy sky conditions, net radiation non-monotonically varies with latitude 22 across the sites, depending on the seasonal sky cloudiness and air temperature. Net radiation on 23 north-facing hillslopes is less sensitive to latitudinal location than on south-facing sites. 24 3 1 Introduction 25