Snow Drift On Roof

This is true of typical smaller roofs but as the roof s plan dimensions become large the roof increasingly emulates the ground.

Snow drift on roof.

Horizontal extent is smallerof 6hdor 6h s 30. 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. 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. There are three elements needed for roof snow drift formation.

Snow drift loading adjacent to roof obstructions. If your roof is located in windswept areas or even north of the treeline the wind will cause snow drifting making less of it accumulate on your roof. Nonetheless information should be sought from locals on drift orientation. For small gaps we have an inconsistency.

Asce standard 7 requires designers to assume that the high winds that cause snow to drift could come from any direction. Slipperiness of the roof. Windward snow drifts occur when wind blows snow from a lower elevation roof towards the wall of an adjacent higher roof. Rain load s r.

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. Density snow density γ. Version 0 0 3 september 14 2020.

Leeward drift results from snow blown off a high roof onto a lower roof. Leeward snow drifts occur when wind blows snow off of a higher elevation roof down onto an adjacent lower roof. Less snow will accumulate on a slippery roof it will slide off instead. Importance factor i s.

Ground snow load s s.