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Snowiest city/ where can one find the best powder


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So the snowiest metropolis (1million+ population)on Earth would be Sapporo with an annual snowfall of approximately 600cm? No any other city in Europe or in North America has such high amount of snowfall?

 

And the best powder(lowest water content?) in the world would be at Niseko?

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I can almost see word for word, member for member, how this thread will go...

I can only talk from experience in Niseko having lived there for 7 years and spent 8 whole winters there. I've not been to the Alps and have yet to ski in Utah unfortunately. In a general sense though

'Cities' such as Tokamachi and Myoko in Niigata will embarrass Sapporo for amounts of snowfall. But they don't have populations of over 1 million. I can't see what the point is myself.

 

I would guess for people in a big city, snow is almost a nuisance than something to actually want more of.

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Sapporo would be the snowiest city with a population of more than 1 million. No other major city even comes close.

 

I doubt very much that Niseko has anywhere near the driest snow though. Resorts just in central Hokkaido would have drier snow and resorts like in Utah and other arid regions of the US would definitely have drier.

It might not have the lowest water content but it does have a great combination of quantity and quality that few other resorts worldwide can match. The quality is more to do with the predominant type of snowflake that falls in Niseko rather than it being some extroadinarily dry snow. Due to the combination of altitude (low) and average temperature (cold but not really cold), Niseko predominantly gets flakes called fernlike stellar dendrites. These types of flakes (pictured below) are the ultimate flakes for producing blower powder. Because of their shape there's a very large surface area and as the flakes fall the fernlike fronds interlock with other flakes. That's why in Niseko you often get what appear to be huge flakes of snow coming down. They are actually conglomerates of smaller flakes all interlocked together. So if there isn't too much wind to deform the flakes this sort of snow settles very lightly with huge amounts of space and air within the fresh snow layer. This is what makes it so incredibly light and fluffy, the blower powder that Niseko is famous for. All hail the fernlike stella dendrite!! :worship:

 

article-1236779-0787691F000005DC-516_196x293_popup.jpg

 

I also believe this is why Niseko has what can only be described as an amazingly stable snowpack. Few other similarly snowy regions in the world have so few avalanches as the Niseko region (maybe few others are so flat? :p ). I believe it's because the interlocking flakes help to hold it all together.

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I guess the difference is that Sapporo must include what act as its "suburbs". Nagoya has loads of satellite cities with separate populations, Kobe has Akashi and Nishinomiya.

 

Nearly two million people is a lot of economic activity. It's also quite far away from the mega city that extends from Tokyo to Kobe.

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It's not like Tokyo actually stretches to Kobe. It's broken up by quite a bit of countryside and greenery. After Odawara the Tanzawa mountains and Mount Fuji do a good job of breaking up any continuous conurbation

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Sapporo would be the snowiest city with a population of more than 1 million. No other major city even comes close.

 

I doubt very much that Niseko has anywhere near the driest snow though. Resorts just in central Hokkaido would have drier snow and resorts like in Utah and other arid regions of the US would definitely have drier.

It might not have the lowest water content but it does have a great combination of quantity and quality that few other resorts worldwide can match. The quality is more to do with the predominant type of snowflake that falls in Niseko rather than it being some extroadinarily dry snow. Due to the combination of altitude (low) and average temperature (cold but not really cold), Niseko predominantly gets flakes called fernlike stellar dendrites. These types of flakes (pictured below) are the ultimate flakes for producing blower powder. Because of their shape there's a very large surface area and as the flakes fall the fernlike fronds interlock with other flakes. That's why in Niseko you often get what appear to be huge flakes of snow coming down. They are actually conglomerates of smaller flakes all interlocked together. So if there isn't too much wind to deform the flakes this sort of snow settles very lightly with huge amounts of space and air within the fresh snow layer. This is what makes it so incredibly light and fluffy, the blower powder that Niseko is famous for. All hail the fernlike stella dendrite!! :worship:

 

article-1236779-0787691F000005DC-516_196x293_popup.jpg

 

I also believe this is why Niseko has what can only be described as an amazingly stable snowpack. Few other similarly snowy regions in the world have so few avalanches as the Niseko region (maybe few others are so flat? :p ). I believe it's because the interlocking flakes help to hold it all together.

 

wow, impressive! What type of snow would be found in Utah and the lofty Alps?

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Even after the cold Siberian air passes through the Sea of Japan and gets saturated with water they barely rise above the freezing point(supersaturated)? Is that right as it seldom rains even on the low lying cities like Otaru and Kutchan. Am I right?

 

Why dont the conifers in Niseko form tree monsters (juhyo) as big as those found in Zao? And why the snow found in Zao isnt as powdrous as those in Niseko? Because its warmer at Zao?

 

Would strong winds inhibit the growth of fernlike crystals??

 

So based on such fact the snow found in western coast of Sakhalin island would be more or less the same as those found in Niseko? But I hv never heard of any ski resorts there :confused:

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On the formation of snow monsters at Zao, an NHK documentary I came across few weeks back explained why. As the wind blow off the Sea of Japan towards Zao mountain range, it encounters the Asahi mountain range first. The crucial factor is that both Zao and Asahi mountain ranges are of similar heights. The heavier clouds dumped most of the moisture upon hitting Asahi mountain range. The lighter clouds with less moisture are pushed over Asahi towards Zao. Upon hitting the trees at Zao, the ice crystals are formed (the video below explains this phenomenon). If the Zao mountains are much lower than Asahi, the clouds would not hit the trees and no snow monsters will be formed. If Zao mountains are much higher, it will cause the moisture to be dumped between the 2 mountains and snow monster would not form. Hence snow monsters will only be formed in places where cold moisture laden winds hit 2 parallel mountain ranges of similar heights. This is based on my memory of that show, so I could have gotten some facts wrong.

 

http://www.youtube.com/watch?v=9NCCD8eLMcI

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It's not like Tokyo actually stretches to Kobe. It's broken up by quite a bit of countryside and greenery. After Odawara the Tanzawa mountains and Mount Fuji do a good job of breaking up any continuous conurbation

 

You're right about your area and :thumbsup: for sticking up for it. Theres about 100km of respite with Shizuoka in the middle.

Once you reach Hamamatsu though, it starts sprawling into the Toyota-supported cities then into Nagoya, there's a brief bit of mountain, and then Kyoto to Himeji is pretty much city all the way.

 

Just another comparison, but Sapporo has nearly half the population of New Zealand, or more folks than Niigata City and Sendai put together. Hokkaido itself is depopulating as fast as anywhere in Japan, but it hasn't hit Sapporo yet.

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It probably snows more in Sapporo than in Denver or Salt Lake City if you're talking about downtown, but for access to great powder skiing from a million+ population center there's really no comparison. Sapporo is a terrific metro area for skiers/boarders, but no better than places like Zurich/Milan/Munich and many others.

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