Verified planning context

Snow, weather and avalanche context

Historical patterns help you compare trips. They do not predict your week or replace the operator's daily decisions.

Evidence reviewed 2026-08-26

Typical operating window

July–OctoberSouthern Alps storms begin building winter cover from late autumn; useful glacier skiing normally develops in winter.

Strongest comparable snow evidence

3.95 m published average · 2.58–5.32 m observed rangeMueller Hut electronic weather stationTier B · observed reference · low confidence

Snow character

maritimeStorm snow can be dense near the divide. Cold clear periods preserve dry snow, while spring sun drives fast surface change.

Public avalanche information

NZAA Aoraki/Mount Cook regionNZAA states that its public forecast is not for commercial operators. The heli-ski operator must maintain its own assessment.

Weather and flight context

Strong westerlies produce large precipitation gradients across the Main Divide.

  • Main Divide cloud cap
  • Severe alpine wind
  • Glacier flat light and rapid warming

Meteorological reference area

Tasman Glacier and Aoraki high-alpine context

Includes
Tasman Glacier and nearby Aoraki high-alpine reference sites.
Excludes
Queenstown, Wānaka, and Canterbury profiles.
Elevation
No verified operator-terrain elevation band is public. Each evidence value retains its site elevation.

Evidence pack

Measurements, claims and gaps stay separate.

Tier BObserved winter snowfall reference3.95 m published average · 2.58–5.32 m observed range
Site
Mueller Hut electronic weather station · 1818 m · Distance unavailable — the source summary does not publish station coordinates
Period
Ten winters; exact years are not listed in the published summary
Completeness
Ten-year summary; annual values and missing periods are not published on the source page.
Method
Earth Sciences New Zealand published mean and observed minimum-to-maximum winter snowfall.
Limitation
A short single-point series cannot represent glacier accumulation or every heli-ski elevation.
Tier CModelled snowfall water equivalent729 mm SWE median · 656–831 mm interquartile range
Site
Tasman Glacier ERA5-Land grid cell · -43.6000, 170.2000 · 1.4 km from Tasman Glacier reference point
Period
Calendar years 1991–2020
Completeness
360 monthly means; all 30 calendar years contain 12 values.
Method
ERA5-Land monthly mean daily snowfall accumulation was multiplied by calendar days and 1,000, then summed by calendar year.
Limitation
This reference area supports evidence discovery and comparison. It is not an operating-area or tenure boundary. This unadjusted 0.1° reanalysis grid cell is not an observation, snow depth, or terrain-wide total. Grid elevation and wind redistribution can cause substantial local bias.

Monthly evidence

Each cell keeps its measurement type and unit. Reanalysis water equivalent is not snow depth. Text-only cells preserve a representative data gap.

Modelled snowfall water equivalent
JanFebMarAprMayJunJulAugSepOctNovDec
2.6 mm SWE2.3 mm SWE5.4 mm SWE18 mm SWE54 mm SWE95.8 mm SWE121.9 mm SWE99.8 mm SWE99.6 mm SWE81 mm SWE48.8 mm SWE14.9 mm SWE

Commercial operator assessment

Operator assessment process not independently verified

The operator must assess current snow, avalanche terrain, weather, aircraft limits, and rescue options. No private operational plan is inferred.

Sources and evidence notes

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