The Hokkaido Wilds Guide to the Winter Weather of the Hokkaido Wilds

Posted on Nov 5, 2022
Posted on Nov 5, 2022
0 2
From about mid-December to late February each year, the North-Eastern areas of Japan are absolutely pounded with snowfall. For local Japanese living in yukiguni (雪国, snowy regions), the extent of this snowfall has been a yearly burden for centuries. For many skiers and snowboarders from around the world, it’s a blessing they’ve yet to experience firsthand. Here, we dive deep into what makes Japan such a powder paradise.

Last updated Nov 14, 2022

A deep dive into Japan’s snow

The snowfall in Japan is remarkable not only in quantity but also in reliability; you can certainly get much bigger and deeper snow dumps in coastal systems such as Whistler or New Zealand…. but, what Japan offers is a level of reliability of powder snow that’s unmatched anywhere else in the world. If you’re booking a dream ski holiday, that reliability counts for a lot!

In this post, I’m going to share a bit about the underlying mechanisms that make Japan’s snow system so good. I’ll share some pointers on when and where to make your trip to maximize the chances of daily dumps of deep, dry powder. Finally, I’ll share some resources to use to track the weather while you’re in Japan. We’ll also share some deeper dive reading material such as academic papers if you want to learn more.

Key Points

With a lake effect operating at a massive oceanic scale, Japan produces some of the world’s best snow. Cold, dry Siberian air picks up great amounts of moisture before being dumped on coastal mountains as high quality powder snow. The lowland satoyuki effect in Hokkaido holds the snowclouds in place longer, emphasizing this ‘lake effect’. FYI, Japan offers some excellent weather forecasting tools, from basic to very advanced, including the Japan Met Agency’s ‘nowcasts’.


The key to the massive snow fall in Japan is that it is heavily driven by ‘lake effect’ snow. But, this isn’t like the lake effect snow of North America’s Great Lakes region, or the famous Salt Lake City powder snows of the Wasatch range. Japan’s lake effect snow is really ‘sea effect’ snow… and that means bigger, deeper dumps.

Lake effect snow occurs when cold, dry air passes over a relatively warm water body. Water evaoporates, saturating the air and also warming it. As the air rises, often helped by flowing up and over hills or mountains, it cools and precipitates the moisture as snow.

The recipe is simple:

  1. Cold, dry air
  2. Relatively warm body of water
  3. Wind over hils causing lifting and cooling

Let’s look at these ingredients each in turn.

Author getting deep at Hakkoda Sakeyu Onsen
The author amongst some deep, dry Japanese powder in early 2020

1. Cold, Dry Air

The source of the cold dry air is the Siberian High. This is a large high pressure system over Siberia. In the atmosphere, a high pressure system is generally caused by masses of cold air descendning from higher altitudes. In our case we see this cold air descending and flowing out from Siberia and across the Sea of Japan. The intensity, coverage and variability of the Siberian High is in turn heavily influenced by snow cover across the region (see The role of the Siberian high in northern hemisphere climate variability, Cohen, Saito and Entekhabi, Geophysical Research Letters Volume 28 Issue 2) .

Mean Sea Level Pressure from Reanalysis, Winter Months. Siberian High is the obvious red shaded area on the map. Attribution: Synysee on Wikipedia.
A typical mid-winter setup, high pressure system over Siberia and low pressure system in NE Pacific. Japan Meteorlogical Agency Jan 21st 2022

2. Relatively Warm Body of Water

The Sea of Japan is our ‘lake’; the source of moisture that will go on to become that deep dry powder snow. Becasue it is fed by currents from the South, The Sea of Japan (the sea running along Japan’s NW coast) is relatively warm.  The average temperature in Niigata on the east coast of Honshu never drops much below 10 degrees (celsius!). This large temperature differential with the cool, dry air coming off Siberia allows the air to pickup significant moisture.  The term fetch is used to describe the length of the water over which the wind blows unobstructed. The fetch across the Sea of Japan is anywhere from about 400km between Russia and Hokkaido all the way up to about 900km between China and Honshu. Generally, the greater the fetch the more potential for the evaporation of moisture into the air. But also, the greater the fetch the more the air will warm up… We’ll discuss this when comparing Honshu and Hokkaido snowfall below.

3. Wind Over Hills Causing Lifting and Cooling

The fancy term here is orographic lifting. On making landfall the wind blows up and over some hills. As air rises, it expands. As it expands, it cools. As moist air cools, it’s able to hold less of that moisture, and so the moisture precipitates out of the air. If it’s cold enough, that precipitation falls as snow. In our case, those hills and mountains include areas such as the Japan Alps, the Niseko Range, and the Daisetsuzan Range in Central Hokkaido. Our air is fed full of moisture by the Sea of Japan. And, yes, it’s cold… and it SNOWS! And it SNOWS! And it SNOWS!

One last little gem that is particularly relevant to snowfall in Hokkaido is the presence of satoyuki or lowland snowfall patterns. This occurs when a temperature inversion exists in the atmosphere and the weather system is ‘held down’ by this layer. This allows for additional time spent ***dumping*** all that moisture onto the windward side of the mountains. It’s one of the reasons that the Niseko area does so well, where the altitude at the resort runs from a base elevation of only 260m (850ft) to just 1,200m (4,000ft) at the top. 

A great way to understand how temperature is changing through the vertical atmosphere is to view a ‘sounding‘. This data is either coming from real-world measurements (aircraft, weather balloons) or from a numerical model. As we note below, offers easy access to a forecast atmospheric sounding.

Satoyuki (lowland) snow system. Figure from Magono et al. Journal of the Faculty of Science, Hokkaido University. Series 7, Geophysics, 2(3), 287-308 (URL)


If you’re used to the weather in New Zealand, Australia, Europe, or the Western US and Canada, then our ‘snow storms’ in Japan are going to feel quite different. Those other regions of the world are dominated by large weather systems where massive storms blow through, dump a whole load of snow (quality variable… Sierra cement anyone?), and then there’s a few days of clear still weather. The snow systems in Japan, particularly in Hokkaido, tend to be gentler and more consistent. Rather than massive storms rolling through, the cold air outflow from Siberia kind of gets turned on like a tap and so it just dumps consistently and often day-after-day-after-day. It’s not unheard of to go a week or two at a time with 20-40cm (8-16inches) every day.

So then, when does the tap go on?
And when does the tap go off?

Japan generally has a shorter and more intense season of peak snowfall than other parts of the world. My friends in Utah are emailing me photos of their first day out touring in late October… and I’m still out riding my mountain bike. Expect to be getting solid snowfall from mid-December through to early March. Obviously you want a bit of a base built up so the best time to visit is probably about mid January through end of February.

Hokkaido vs Honshu

This section will probably get me some hate, but, it’s ultimately a game of probability.  Honshu, and particularly the Japanese Alps, can receive massive amounts of snow each year. The higher elevation and higher moisture content in the air (that fetch remember) means that when it dumps… it really dumps. But, you are playing a bit more dice with the temperatures and so the snowfall, and resulting snowpack, can be a bit more variable. There’s obviously much bigger terrain in the Alps and it’s easy enough to tag on some time there before or after a trip to Hokkaido. You’ll find the northern parts of Honshu, the likes of Aomori, are closer to Hokkaido in their overall weather patterns.


Most of the weather forecasts that we see from day to day are the result of numerical weather forecast models. These models involve simulating the behaviour of the atmosphere on super computers and then using the forcasts of those simulations to forcast the weather. Many of the world’s largest meteorological agencies make their forecast model data available for free or for a free nominal cost. This means that the data is very available on 3rd party websites. A few of my favorites.

  • Windy
    Windy was originally focused on providing data for sailors and windsurfers but these days it provides a really nice user experience to view data from a number of weather models. The user experience is Spatio-temporal; this means that you can look at the outputs of the models on a map and scroll back and forth through time. Models supported include the NOAA (USA) GFS model, the German ICON model, and the European ECMWF model. This last model is one that is paid-for and so Windy is unique in providing access to it for free in this format. Another great feature from Windy is that it provides access to an atmospheric sounding view. TO access the sounding view, click on a location and select the airgram view.

  • Spot WX
    This site allows you to see the same sort of weather model data but in a different user experience. This time plotted as charts and graphs. It has a different set of weather models including high-resolution models in North America and global models elsewhere. It can be a bit hit or miss as to whether the non-US data is working at any point in time, but, it is a great service when it’s working.

  • Source Data
    You can also go to the source data for these sites. This includes the NOAA models, the ICON model and also more localized models from the Korean Met Agency NEMA model and Japanese Met Agency GSM, MSM and other models. The exact format the data takes will vary by agency; typically this is the underlying model (sometimes with some human intervention or interpretation) that’s being used to produce forecast synoptic charts.

Keep in mind that all of the ‘special’ snow forecast sites such as or will be using one or more of the off the shelf weather models as the basis of their forecasts. Taking the time to learn to work with the source data is a great investment. If you want to learn more about numerical weather prediction then The Weather Machine is a great book to read. 

Weather Maps, Sattelite and Radar

If you like to read a more typical weather map then my favorite for the region are the forecast and analysis charts from the Korean Met agency. The Japan Met Agency also does a great set of forecast charts in aviation style.

The JMA provides excellent real-time data from its network of weather radars, probably amongst the best in the world. This is available in both a general precipitation mode as well as a snowfall-specific mode. These ‘NowCasts’ are also worth keeping an eye on when flying into or out of Sapporo or Asahikawa airport as they give a good indication of delay/cancellation risk too.

JMA Snowfall Nowcast Site


And one last resource to really geek out on. Jim Steenburgh is a Professor at the University of Utah. He teaches both undergraduate and graduate-level atmospheric sciences including a course on “The Greatest Snow on Earth”. He’s a Japan fan and so there’s plenty of content and commentary on Japan in general and Hokkaido in particular. Key resources from Jim include:

Maybe you’ve got other great resources that we’ve missed. Would love to hear from you in the comments and we can update this article with inputs.

Comments | Queries | Discussion

2 thoughts on “The Hokkaido Wilds Guide to the Winter Weather of the Hokkaido Wilds”

  1. Hi guys,
    quick question. If you are heading out for a day ski tour in Hokkaido what do you take in in your pack as far as safety gear for night out should things go wrong late in the day?

    1. Hi Julian.
      Most stuff here is ‘ski back to the car’ type touring. So, I don’t take a huge amount (as I might in Canada). I have two different aid kits which I will take one depending on how big the day is. But both have fire starting stuff and some energy gels. I carry a little Rab brand silnylon tarp that can be used to make shelter or improvised into a rescue sled/tarp. And I have a heavy weight (but still light) Sol Brand emergency blanket. Then it’s just usual touring stuff. Extra clothing, down jacket etc.

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The Hokkaido Wilds Guide to the Winter Weather of the Hokkaido Wilds Difficulty Rating





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GRADES range from A (very difficult) to D (easy). Hazards include exposure to avalanche and fall risk. More details here. Rating rubric adapted from Hokkaido Yukiyama Guidebook 北海道雪山ガイド.