Snow Drift On Roof

This accounts for the wind s tendency to remove snow from the roof by drifting while snow is generally not able to drift up onto the building from the ground.
Snow drift on roof. Importance factor i s. Leeward drift results from snow blown off a high roof onto a lower roof. Density snow density γ. Leeward snow drifts occur when wind blows snow off of a higher elevation roof down onto an adjacent lower roof.
Windward snow drifts occur when wind blows snow from a lower elevation roof towards the wall of an adjacent higher roof. Snow drift loading adjacent to roof obstructions. Version 0 0 3 september 14 2020. The peak snow load on the lower roof is about nine times the load on the upper roof.
Snow drift loading adjacent to roof obstructions. An area of aerodynamic shade geometric irregularity on the roof where the drift can form and grow a source of driftable snow upwind of the geometric irregularity and wind speed sufficient to cause transport of driftable snow across the aerodynamic shade region. Less snow will accumulate on a slippery roof it will slide off instead. For ordinary leeward drifts the width is 4hd unless hd hcin which case we set the height at hcand increase the width.
Drift height is smallerof hdfor upper roof snow source and h s 6 space below aerodynamic shade line. Rain load s r. This is true of typical smaller roofs but as the roof s plan dimensions become large the roof increasingly emulates the ground. Asce standard 7 requires designers to assume that the high winds that cause snow to drift could come from any direction.
For small gaps we have an inconsistency. Slipperiness of the roof. Nonetheless information should be sought from locals on drift orientation. Asce 7 specifies drifts for simple geometries based on the size of the upwind snow source area fetch and ground snow drift is a 2 hfor more complex geometries a reasonable approach is to match the cross sectional area of the odd shaped drift to that for a roof step with the same fetch and ground load 50 faq 4 odd drift geometries.
Ground snow load s s.