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Snow advisory issued 1st July for New Zealand: Southerly winds by Friday as low pressure moves off the East Coast of the South Island. Widespread snow for the mountains of both islands with snow settling to low levels in the east on Friday night and Saturday. A similar pattern gave Mount Lyford 85 cms of snow last weekend. Update issued Friday 4th July at 6pm NZ time: Snow is already settling to near sea-level in coastal Otago and Southland. Snow will spread quickly north and inland. Windy everywhere with severe gales in exposed eastern parts of South Island and southern North Island and exposed high ground everywhere. Expect dangerous weekend travel conditions over much of South Island and central North Island.

Great Canadian HeliSki, Canada - BC

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6 Day Forecast
(free)
top: 3200m
mid: 2697m
bot: 2194m
2 Day Detail
(subscribers)
top: 3200m
mid: 2697m
bot: 2194m
9 Day Forecast
(subscribers)
top: 3200m
mid: 2697m
bot: 2194m
Piste Map Weather Maps Snowfinder
Printable Forecast
6 Day Weather Forecast for 3200 m altitude, issued (local time): 09 am 04 Jul 2008
  Days 0-3 Great Canadian HeliSki Weather Summary: Light rain (total 3.0mm) at first, then becoming colder with a dusting of snow on Fri afternoon. Freeze-thaw conditions (max 3°C on Fri morning, min -5°C on Sun night). Wind will be generally light. Days 4-6 Great Canadian HeliSki Weather Summary: Mostly dry. Freeze-thaw conditions (max 3°C on Wed morning, min -7°C on Tue night). Wind will be generally light.
Fri
04
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Fri
04
after-
noon
Fri
04
night
Sat
05
morn-
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Sat
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after-
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Sat
05
night
Sun
06
morn-
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Sun
06
after-
noon
Sun
06
night
Mon
07
morn-
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Mon
07
after-
noon
Mon
07
night
Tue
08
morn-
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Tue
08
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Tue
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Wed
09
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Wed
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Wind (km/h)
Summary light rain snow shwrs snow shwrs clear snow shwrs light snow snow shwrs cloudy some clouds clear clear some clouds light snow some clouds clear clear some clouds some clouds
Snow cm - 2 - - - 1 - - - - - - - - - - - -
Rain mm 3 - - - - - - - - - - - - - - - - -
Max °C 3 1 0 2 1 -1 -2 -3 -4 -1 0 0 1 1 0 3 2 1
Min °C 2 1 -1 0 -1 -3 -2 -4 -5 -3 -2 -6 0 -1 -7 2 1 -4
WChill °C -3 -4 -6 -4 -6 -9 -7 -10 -12 -9 -7 -13 -5 -7 -12 -1 -4 -10
Freezing level (m) 3750 3450 3350 3100 3400 3200 2800 2850 2600 2750 3150 3250 3200 3350 3150 3250 3600 3550
Sunrise 3:39 - - 3:40 - - 3:41 - - 3:42 - - 3:43 - - 3:44 - -
Sunset - 20:07 - - 20:07 - - 20:07 - - 20:06 - - 20:05 - - 20:05 -

The above table gives the weather forecast for Great Canadian HeliSki at the specific elevation of 3200 m. Our sophisticated weather models allow us to provide snow forecasts for the top, middle and bottom stations of Great Canadian HeliSki. To access the weather forecasts for the other elevations, use the tab navigation above the table. For a wider view of the weather, check out the Weather Map" of Canada.

NOTE ABOUT FREEZING LEVELS AND TEMPERATURES
The freezing level that we forecast Great Canadian HeliSki is the  free air freezing level. (More specifically, it is the uppermost free air freezing level). This means that all of the air above this elevation is below freezing however it does not necessarily imply that all of the air below it is above freezing.  We provide this because it best describes the level where falling snow first starts to turn to rain. On average, snowflakes only stay frozen for about 100 metres (300 feet) below the free air freezing level. That's because air temperatures usually increase steadily as you descend - but not always.  For example, a temperature inversion describes a pool of cold air near the ground with a layer of warmer air above it. This is a common occurrence in winter when the wind is light. Such pools of dense cold air can vary from a few metres to several kilometres deep and can persist from hours to several weeks. In an inversion, it can be simultaneously below freezing in a mountain valley, and also at a nearby summit, yet above freezing at some elevation in between. Most visitors to the Alps are very familiar with this. Such conditions can allow snow to fall much more than the usual 100 metres below the top freezing level, even reaching the valley, just as long as snow did not pass through enough warm air to melt. Otherwise, freezing rain or re-frozen soft hail (there is even a German word for it - graupel) reaches the valley instead. Our forecasts allow for these possibilities which is why you may see forecasts of snowfall and frost at elevations far below the free-air freezing level, or valley temperatures that are lower than summit temperatures. You may even see forecasts of rain to fall even though it is just below freezing at the surface - that happens if our model predicts that there is a deep warm layer just above. None of these are as contradictory as they may seem at first.

All of our temperature forecasts for Great Canadian HeliSki are for the ground, not the air. These can be very different to free-air temperatures, especially at night. This can lead to what looks like a contradiction. Because the ground is such a good radiator of heat (especially on clear nights when there is a snow cover and the wind is light) surface temperatures often fall more than far below the free air temperatures - sometimes by more than 10 degrees. On such occasions, the snowpack freezes at elevations that are far below the free air freezing level. For example, in the European Alps, snow tends to freeze in valleys on still clear and still nights  even if the free air freezing level is above 3000m simply because snow is so efficient radiating its heat away. In reality there are two freezing levels; one just above the snow surface and another at 3000m with a layer of warmer temperatures in between where the snow may not freeze at all. In summary, the reason we provide surface temperatures is because these determine the condition of the snowpack.


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