BS6399 3 1988
BS6399 3 1988
British Standard
The preparation of this British Standard was entrusted by the Sector Board for
Building and Civil Engineering (B/-) to Technical Committee B/525/1, upon
which the following bodies were represented:
Contents
Page
Committees responsible Inside front cover
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Foreword ii
Section 1. General
1 Scope 1
2 Definitions 1
3 Symbols 1
4 Minimum impose roof loads 2
Section 2. Snow loads
5 Snow load on the roof 4
6 Snow load on the ground 4
7 Snow load shape coefficients 6
8 Snow sliding down roofs 9
Appendix A Annual probabilities of exceedance different from 0.02 21
Appendix B Snow drift load calculations 21
Appendix C Addresses of advisory offices 21
Figure 1 — Basic snow load on the ground 5
Figure 2 — Snow load shape coefficients for flat or monopitch roofs 7
Figure 3 — Snow load shape coefficients for pitched roofs 10
Figure 4 — Snow load shape coefficients for curved roofs 11
Figure 5 — Snow load shape coefficients and drift lengths for
valleys of multi-span pitched or curved roofs 13
Figure 6 — Snow load shape coefficients and drift lengths at
abrupt changes of roof height 14
Figure 7 — Snow load shape coefficients and drift lengths for single
pitch roofs abutting taller structures at 90° 16
Figure 8 — Snow load shape coefficients and drift lengths for
intersecting pitched roofs 17
Figure 9 — Snow load shape coefficients and drift lengths for
local projections and obstructions 19
Table 1 — Values of salt for corresponding values of sb 4
Publications referred to Inside back cover
© BSI 11-1998 i
BS 6399-3:1988
Foreword
This Part of this British Standard Code of practice has been prepared under the
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ii © BSI 11-1998
BS 6399-3:1988
A British Standard does not purport to include all the necessary provisions of a
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contract. Users of British Standards are responsible for their correct application.
Compliance with a British Standard does not of itself confer immunity
from legal obligations.
Summary of pages
This document comprises a front cover, an inside front cover, pages i to iv,
pages 1 to 22, an inside back cover and a back cover.
This standard has been updated (see copyright date) and may have had
amendments incorporated. This will be indicated in the amendment table on
the inside front cover.
iv
blank
BS 6399-3:1988
Section 1. General
1 Scope 2.4
site snow load
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the load intensity of undrifted snow in a sheltered h Assumed maximum height of snow in a
area at an assumed ground level datum of 100 m local drift (valleys of multi-span roofs and
above mean sea level, estimated to have an annual the intersections);
probability of exceedance of 0.02 hoi Vertical height of obstruction,
2.3 suffix i = 1, 2 or 3 to distinguish between
altitude of site several vertical heights on the same
diagram;
the height above mean sea level of the site where the
building is to be located, or is already located for an lsi Horizontal length of snow drift,
existing building suffix i = 1, 2 or 3 to distinguish between
several snow drifts on the same diagram;
salt Coefficient used in correcting basic snow
load on the ground for altitude;
© BSI 11-1998 1
BS 6399-3:1988 Section 1
sb Basic snow load (on the ground); c) a uniformly distributed load of 0.6 kN/m2
measured on plan for roof slopes of 30° or less; or
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2 © BSI 11-1998
Section 1 BS 6399-3:1988
The minimum imposed load on a curved roof should A load of 0.9 kN on any square with a 125 mm side
be calculated in accordance with 4.3. In provides for loads incidental to maintenance on all
evaluating 4.3.1 c), the roof should be divided into self-supporting roof coverings, i.e. those not
not less than five equal segments and the mean requiring structural support over their whole area.
slope of each segment considered to be equivalent to No loads incidental to maintenance are appropriate
the roof slope, a. The snow loads should be to glazing.
determined according to clause 7.
4.5 Partial loading due to snow removal
In certain cases snow may be artificially removed
from, or redistributed on, a roof, e.g. due to excessive
heat loss through a small section of roof or manually
to maintain access to a service door. This can result
in more severe load imbalances occurring than those
resulting from clause 5 (which have been derived for
natural deposition patterns). To provide for these
situations, if they are likely to occur and if other
information is not available, a load case should be
considered comprising the minimum imposed
uniformly distributed load according to clause 4 on
any portion of the roof area and zero load on the
remainder of the area.
© BSI 11-1998 3
BS 6399-3:1988
The snow load on the roof sd (in kN/m ) is 2 The snow load at ground level increases as the
determined by multiplying the estimated snow load altitude of the ground level increases. As the basic
on the ground at the site location and altitude (the snow load on the ground is given for an assumed
site snow load) by a factor known as the snow load ground level altitude of 100 m, it is necessary to
shape coefficient in accordance with the following adjust the value for locations where the ground level
equation: is above 100 m. The site snow load s0 (in kN/m2)
should be calculated from the following equations:
sd = µ i s0
s0 = sb
where
for sites whose altitude is not greater than 100 m; or
s0 is the site snow load (in kN/m2) (see clause 6);
s0 = sb + salt ((A – 100)/100)
µi is the snow load shape coefficient µ1, µ2, etc. for sites whose altitude is above 100 m but not
(see clause 7). greater than 500 m
Several snow load cases may have to be considered where
in design to check adequately for the different snow
sb is the basic snow load on the ground
load patterns that can occur. Each load case may
require the use of one or more different snow load (in kN/m2) (see 6.1);
shape coefficients. Depending upon the pattern salt = 0.1sb + 0.09 (alternatively see Table 1);
being considered the snow load on the roof should be
treated either as a uniformly distributed load or as A is the altitude of the site (in metres).
a variably distributed load over all or part of the It is not necessary to make any correction for the
roof. It should be assumed to act vertically and refer height of the building. For sites whose altitude is
to a horizontal projection of the area of the roof. For above 500 m specialist advice should be sought
the redistributed snow load cases the distribution of (see clause 1 and appendix C).
the snow in the direction parallel to the obstruction NOTE For simplicity of calculation it is assumed that the same
is normally assumed to be uniform. value for the basic snow load on the ground should apply for
altitudes between 0 and 100 m. If preferred the equation for
The snow load on the roof should be considered to be altitudes greater than 100 m may be used for altitudes between 0
a medium term load for the majority of design in the and 100 m; in these cases the correction term, salt((A - 100)/100),
will automatically be negative.
UK, i.e. to have a notional duration of one month.
Table 1 — Values of salt for
6 Snow load on the ground corresponding values of sb
6.1 Basic snow load (sb) sb salt
4 © BSI 11-1998
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Section 2
© BSI 11-1998
Figure 1 — Basic snow load on the ground
5
BS 6399-3:1988
BS 6399-3:1988 Section 2
7 Snow load shape coefficients NOTE The snow load shape coefficient, being a ratio of two
loads, is non-dimensional. The equations of the form 2h0i/s0 are
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7.1 General principles correct, although apparently having the dimensions kN/m3,
because of the density correction. The correction is based on
Snow is naturally deposited in many different limited information which shows that the snow density is
patterns on a roof depending upon the wind speed, increased when the snow forms in drifts.
the wind direction, the type of snow, the external 7.2 Single span roofs
shape of the roof and the position and height of any
7.2.1 General. These are flat, monopitch, pitched or
surrounding roofs or obstructions. Therefore, it is
curved roofs of single span. The snow load shape
often necessary to consider several loading
coefficients do not include any allowances for
situations to ensure that all the critical load effects
drifting at parapets or other obstructions as these
are determined.
should be treated independently (see 7.4).
The primary loading conditions to be considered are:
7.2.2 Flat or monopitch roofs. For these roofs it is
a) that resulting from a uniformly distributed necessary to consider a single load case resulting
layer of snow over the complete roof, likely to from a uniform layer of snow over the complete roof.
occur when snow falls when there is little or no The value of the snow load shape coefficient (µi) is
wind; dependent on the angle of the pitch of the roof
b) those resulting from redistributed (or unevenly measured from the horizontal (a) and should be
deposited) snow, likely to occur in windy obtained from Figure 2. This value is assumed to be
conditions. constant over the complete roof area.
Condition b) can be caused by a redistribution of 7.2.3 Pitched roofs
snow which affects the load distribution on the 7.2.3.1 General. For this type of roof it is necessary
complete roof, e.g. snow transported from the to consider two load cases. For both cases the value
windward slope of a pitched roof to the leeward side; of the snow load shape coefficient (µi) is dependent
usually modelled as a uniformly distributed load on on the angle of pitch of the roof measured from the
the leeward side of the roof and zero load on the horizontal (a). For asymmetric pitched roofs, each
windward side. It can also be caused by side of the roof should be treated as one half of a
redistribution of snow which affects the load corresponding symmetric roof.
distribution on only a local part of the roof, e.g. snow
drifting behind a parapet; modelled as a variably 7.2.3.2 Case 1; uniform load. This results from a
distributed load. Both types of redistribution should uniform layer of snow over the complete roof. The
be considered if appropriate. For a complex roof value for the snow load shape coefficient should be
shape there may be several load cases associated obtained from Figure 3(a) ; this value is assumed to
with condition b). be constant over the complete roof area.
In general, load cases should be considered to act 7.2.3.3 Case 2; asymmetric load. This results from
individually and not together. In some transport of snow from one side of the ridge to the
circumstances more than one of the load cases will other side. This situation only needs to be
be applicable for the same location on the roof. When considered for roof slopes greater than 15°. The
this arises they should be treated as alternatives. value for the snow load shape coefficient for one
slope of the roof should be zero, i.e. no snow load.
NOTE However, where, for example, on a lower roof area
sheltered from all wind directions, there is the possibility of The value for the snow load shape coefficient for the
redistribution of snow from a higher roof to form a local drift on other slope should be obtained from Figure 3(b); this
top of a uniform snow load distribution on this lower roof, it value is assumed to be constant over the loaded
would be appropriate to consider the local drift load acting in
combination with the uniform snow load on the lower roof.
slope of the roof.
Redistribution of snow should be considered to occur
on any roof slope and at any obstruction, as it should
be assumed that the wind can blow from any
direction.
The equations given in Figure 2 to Figure 9 for
determining the snow load shape coefficients are
empirical; where they are associated with local
drifting of snow they include a correction to allow for
an increased weight density in the drift. Therefore,
when using the equations the dimensions of the
building and of the obstruction (b1, h01, ls1, b2, etc.)
should be in metres and the site snow load should be
in kN/m2.
6 © BSI 11-1998
Section 2 BS 6399-3:1988
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© BSI 11-1998 7
BS 6399-3:1988 Section 2
7.4 Local drifting of snow on roofs Where simultaneous drifts in several valleys of a
multispan roof are being considered in the design of
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8 © BSI 11-1998
Section 2 BS 6399-3:1988
where b is the larger value of b1 and b2 Drift length ls1 is the lesser value of 5h01 and b1.
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with the restriction: µ1 ≤ 8 Snow load shape coefficient µ1 is the lesser of:
For drifting in a valley behind a parapet at a gable (2h01)/s0 and 5.
end the snow load at the face of the parapet should In addition, for door canopies projecting not more
be assumed to decrease linearly from its maximum than 5 m from the building, the value of snow load
value in the valley to zero at the adjacent ridges, shape coefficient should not exceed:
providing the parapet does not project much higher (2b)/ls1
than the ridge.
where b is the larger of b1 and b2 (see Figure 9).
NOTE For the purpose of this subclause, when considering a
parapet across the end of a valley the snow load at the ridge can
be assumed to be zero providing that the parapet does not project 8 Snow sliding down roofs
more than 300 mm above the ridge.
Under certain conditions snow may slide down a
7.4.4 Tee intersections. For intersecting pitched pitched or curved roof. The force Fs (in kN per metre
roofs the snow load shape coefficients and the drift width) exerted by a sliding mass of snow in the
lengths should be obtained from Figure 8. For this direction of slide is calculated from the following
case the variation in the direction parallel to the equation:
obstruction is non-uniform.
Fs = sdb sina
7.4.5 Local projections and obstructions. The effect
of drifting can be ignored if the vertical elevation where
area against which the drift could form is not
greater than 1 m2. The drifts which occur at local sd is the snow load on the roof (in kN/m2 );
projections and obstructions affect a relatively small b is the distance on plan from the gutter to the
area of roof only. Included in this category is drifting ridge (in metres);
against local obstructions not exceeding 1 m in
height and also drifting on canopies (projecting not a is the angle of pitch of the roof measured from
more than 5 m from the face of the building) over the horizontal.
doors and over loading bays, irrespective of the
height of the obstruction formed. A relatively tall, The appropriate value for sd is obtained from
slender obstruction over 1 m high but not more clause 5. It should be the most onerous value arising
than 2 m wide, may also be considered as a local from uniformly distributed snow on the roof slope
projection. For that specific case, the height against under consideration. It may result from either the
which the drift may form, h0i may be taken as the uniform load case or the asymmetric load case.
lesser of the projection width and the projection This force should be taken into account in the design
height. For parapets, see 7.4.3.3. of snowguards or snowfences if snow is likely to slide
The appropriate snow load shape coefficient at the off the roof endangering people or property below. It
face of the obstruction and the drift length should be should also be taken into account in the design of
obtained from Figure 9 or the following in which all any obstruction on a roof which may prevent snow
parameters are as defined in Figure 9. sliding off the roof.
© BSI 11-1998 9
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10
BS 6399-3:1988
© BSI 11-1998
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Section 2
© BSI 11-1998
Figure 4 — Snow load shape coefficients for curved roofs
11
BS 6399-3:1988
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12
BS 6399-3:1988
© BSI 11-1998
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Section 2
© BSI 11-1998
Figure 5 — Valleys of multi-span pitched or convex curved roofs
13
BS 6399-3:1988
BS 6399-3:1988 Section 2
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Figure 6 — Snow load shape coefficients and drift lengths at abrupt changes
in roof height and parapets
14 © BSI 11-1998
Section 2 BS 6399-3:1988
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Figure 6 — Snow load shape coefficients and drift lengths at abrupt changes
in roof height and parapets (concluded)
© BSI 11-1998 15
BS 6399-3:1988 Section 2
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Figure 7 — Snow load shape coefficients and drift lengths for single pitch roofs
abutting taller structures at 90°
16 © BSI 11-1998
Section 2 BS 6399-3:1988
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Figure 8 — Snow load shape coefficients and drift lengths for intersecting pitched roofs
© BSI 11-1998 17
BS 6399-3:1988 Section 2
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Figure 8 — Snow load shape coefficients and drift lengths for intersecting pitched
roofs (concluded)
18 © BSI 11-1998
Section 2 BS 6399-3:1988
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Figure 9 — Snow load shape coefficients and drift lengths for local
projections and obstructions
© BSI 11-1998 19
BS 6399-3:1988 Section 2
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Figure 9 — Snow load shape coefficients and drift lengths for local
projections and obstructions (concluded)
20 © BSI 11-1998
BS 6399-3:1988
© BSI 11-1998 21
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22
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BS 6399-3:1988
Publications referred to
BS 5555, Specification for SI units and recommendations for the use of their multiples and of certain other
units1).
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1)
Referred to in the foreword only.
2)
Withdrawn.
© BSI 11-1998
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