Snow Drift On Roof

For small gaps we have an inconsistency.

Snow drift on 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. Nonetheless information should be sought from locals on drift orientation. Density snow density γ.

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. Leeward snow drifts occur when wind blows snow off of a higher elevation roof down onto an adjacent lower roof. Importance factor i s. This is true of typical smaller roofs but as the roof s plan dimensions become large the roof increasingly emulates the ground.

For ordinary leeward drifts the width is 4hd unless hd hcin which case we set the height at hcand increase the width. Ground snow load s s. Drift height is smallerof hdfor upper roof snow source and h s 6 space below aerodynamic shade line. 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.

There are three elements needed for roof snow drift formation. Version 0 0 3 september 14 2020. Slipperiness of the roof. Snow drift loading adjacent to roof obstructions.

Less snow will accumulate on a slippery roof it will slide off instead. 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. Rain load s r. Horizontal extent is smallerof 6hdor 6h s 30.

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.