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Kamloops is not one roof climate. It is a valley floor sitting around 350 metres and hillside neighbourhoods nearly seven hundred metres above it — and the City’s own building bylaw treats those two places differently.

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One city, two snow load zones

Most roofing sites treat a city as a single set of conditions. Kamloops demonstrably is not one, and the evidence is in the City’s own building bylaw: it does not apply a single ground snow load across the municipality. It splits it.

The bylaw assigns one value to Mt. Dufferin and the area south of the Trans Canada Highway, excluding Valleyview and Dallas, and a lower one to Valleyview, Dallas and everything north of the highway. Two zones, one city, with a major highway forming part of the boundary.

The design figures themselves are not published on this page, and deliberately so. Structural design values are engineering territory, and a roofing website is the wrong place to put a number that someone might build against. Confirm the design value for your address with the City’s Building Inspection Section or a structural engineer.

What is worth saying plainly is why the split exists, because the reason is the useful part.

The reason is altitude

The national building code publishes climatic design data city by city, and its Kamloops row is keyed to an elevation of 355 metres. That is valley bottom — the elevation of Brocklehurst, North Kamloops, Valleyview and the downtown core, give or take a few metres.

But a great deal of Kamloops is nowhere near 355 metres. The residential hillsides climb to more than two and a half times that height. A single code value keyed to the valley floor cannot describe a roof on Aberdeen, and the City’s higher zone is the local adjustment that acknowledges it.

So the two-zone split is not an administrative quirk. It is an altitude correction, and once you see it that way the map below stops being trivia and starts being a rough guide to how hard a given roof is working.

The Kamloops elevation ladder

Below is the median ground elevation of every one of the City’s twenty-seven official neighbourhoods, derived from the City’s own neighbourhood boundary polygons sampled against national elevation data. The range column matters as much as the median: several neighbourhoods climb hundreds of metres within their own boundary, which means a neighbourhood name alone does not settle the question for a specific house.

Median ground elevation by Kamloops neighbourhood, highest first
NeighbourhoodMedian elevationRange within the neighbourhood
Rose Hill940 m462–1113 m
Aberdeen924 m633–1055 m
Iron Mask861 m501–999 m
Knutsford828 m676–983 m
Pineview754 m724–846 m
Dufferin688 m368–883 m
Upper Sahali642 m531–749 m
Barnhartvale612 m417–1025 m
Batchelor Heights581 m387–988 m
Southgate546 m523–602 m
Juniper Ridge542 m395–722 m
Noble Creek522 m348–872 m
Lower Sahali520 m434–548 m
TRU516 m463–576 m
Westsyde516 m347–899 m
West End430 m358–511 m
Sagebrush406 m364–477 m
Heffley Creek396 m345–756 m
Mission Flats384 m338–604 m
Valleyview377 m339–491 m
Dallas366 m340–487 m
Downtown366 m343–505 m
Rayleigh364 m342–720 m
Campbell Creek358 m346–483 m
North Kamloops350 m339–364 m
Brocklehurst348 m341–430 m
Tranquille346 m335–552 m

Contains information licensed under the Open Government Licence – Kamloops. Elevations derived from City neighbourhood boundaries sampled against national digital elevation data, and are ground elevations for general guidance only.

Read the top and the bottom of that table together. Rose Hill and Aberdeen sit above 900 metres. Tranquille, Brocklehurst and North Kamloops sit below 350. That is a spread of close to six hundred metres inside one municipality, and it is the largest single reason roofs in this city do not age at the same rate.

What six hundred metres actually does to a roof

Altitude is not an abstraction here. It shows up in four concrete ways, and each one maps onto a specific kind of roof failure.

  1. It is colder up the hill — by about four degreesThe average temperature difference between Brocklehurst and Aberdeen runs to roughly four degrees, consistent with the standard rate at which air cools with altitude over that elevation gap. Four degrees does not sound like much until it is the difference between melting and not melting.
  2. Snow stays on the roof longerA hillside roof holds a snowpack after the valley has cleared. Retained snow is retained weight, and it is retained meltwater looking for a way off — or a way in.
  3. The freeze-thaw cycle runs more oftenWhat damages a roof is not cold, it is crossing freezing repeatedly. Meltwater that runs during a sunlit afternoon and refreezes overnight works into every seam and lifts what it can. More crossings per winter means more of that, and it is the mechanism behind ice damming and behind gutters pulling off fascia.
  4. Ultraviolet exposure is stronger with altitudeThe same semi-arid sun that dominates roof ageing across this city is more intense higher up, on roofs that are also enduring the biggest temperature swings. Those two things act on the same material at the same time.

The practical upshot is that two identical houses, built the same year with the same shingle, in Brocklehurst and in Aberdeen, are not on the same replacement schedule — and the one up the hill is usually not the one that lasts longer.

Within a neighbourhood, exposure still varies

Elevation is the large effect, but it is not the only one, and the table’s range column hints at the rest. Aspect matters: a south-facing plane takes substantially more ultraviolet and thermal load than a north-facing one on the same house, which is why the normal condition of a mature Kamloops roof is asymmetric rather than uniform. So does shelter, and so does whether a building next door shades a plane for half the day.

This is the reason a neighbourhood page is not a substitute for looking at a roof. It sets expectations; it does not diagnose. Getting the actual condition of a specific roof recorded is what a written inspection is for, and a decent report separates the roof plane by plane rather than issuing a single verdict for the whole thing.

Areas covered

Requests are passed to local roofing companies working across the whole of Kamloops and the surrounding area, including the outlying neighbourhoods in the table above — Knutsford, Heffley Creek, Rayleigh, Campbell Creek and Barnhartvale among them.

If you are not sure which neighbourhood you are technically in, it does not matter for getting a quote. It matters for the snow load question, and that one is answered by address rather than by neighbourhood name in any case. Confirm the design values for your address with the City or a structural engineer.

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Kamloops neighbourhoods and roofing — common questions

Why would my roof be different from a roof across town?

Elevation, mostly. The difference between the valley floor and the highest residential neighbourhoods in Kamloops is nearly six hundred metres, which is enough to change how cold it gets, how long snow stays on a roof, and how many times a winter the surface crosses freezing and back. A roof at the top of the hill and a roof by the river are exposed to measurably different conditions despite being in the same city and often the same age.

Which Kamloops neighbourhoods are in the higher snow load zone?

The City’s building bylaw draws the line geographically rather than by neighbourhood list. It assigns one ground snow load to Mt. Dufferin and the area south of the Trans Canada Highway, excluding Valleyview and Dallas, and a lower one to Valleyview, Dallas and everything north of the highway. Because the boundary follows the highway rather than neighbourhood edges, an address near it can sit either side. Confirm the design value for your specific address with the City or a structural engineer.

How much colder is Aberdeen than Brocklehurst?

Roughly four degrees on average, which is what you would expect from the elevation difference between them under the standard rate at which air cools with altitude. Brocklehurst sits in the low 340s of metres; Aberdeen’s median is above 900. That gap is why snow lingers on a hillside roof after the valley has cleared, and why the freeze-thaw cycling that loosens fasteners and sealants runs at different rates in the two places.

Does elevation change what roofing material I should choose?

It changes what the choice has to cope with rather than dictating an answer. A roof that holds snow longer, cycles through freezing more often and sits under stronger sun at altitude is working harder than one that does not. That pushes the conversation toward how the assembly handles retained snow, meltwater and movement. It does not translate into a single material recommendation, and anyone offering one without having seen the roof is guessing.

Where does the two-zone boundary actually run?

Part of it follows the Trans Canada Highway, with Mt. Dufferin and the area south of the highway in one zone and Valleyview, Dallas and everything north of it in the other. That is the bylaw’s own description. It is not a smooth contour line and it does not follow neighbourhood boundaries, which is exactly why an address rather than a neighbourhood name is the right unit for the question.

Do you cover areas outside the Kamloops city limits?

The neighbourhoods listed here are the City’s own official set, which already includes outlying areas such as Knutsford, Heffley Creek, Rayleigh, Campbell Creek and Barnhartvale. Requests from the surrounding area are passed on in the same way; whether a given contractor travels to a specific address is their call and it is worth asking early rather than late.

Covering every Kamloops neighbourhood

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