surfing

NASA: The Korean Peninsula; 2005

A pitching deck, the creak of well worn timbers, the cracking of sail and canvas...tied to the mast.  Things have changed a little I guess from when Jack London and  Josef Conrad wrote their haunting Pacific infused epics but it hasnt changed everythwhere. There are corners of this earth where that mythos still holds true, and most of those  corners are here in the South Pacific.

The main source of swell here is from the intense lows that circle the earth south of Australia, these lows spin off northwards with blessed regularity, peppering the entire region with generous SE to SW groundswell from March to September. Australia and New Zealand see the bulk of these swells. These countries cast a very tall shadow across the rest of the Pacific and hence many other islands in their wake can suffer from swell difusion. December to February is cyclone season. Unpredictable cells can deliver swell in a 360 radius, lighting up rarely breaking reefs and points facing every conceivable direction. 

The South Pacific trade winds are some of the most consistent in the world, generally from the East with slight seasonal variation. This is the largest Ocean on the planet and these winds easily generate regular rideable swell. Onshore conditions can be a problem on east facing coastlines but peeling yourself out for an early surf will usually bring some relief.

In the North Pacific it is the intense lows descending from the Aleutians that deliver NE to NW swells from October to March. Hawaii is ideally placed to make best use of this energy but other coastlines in the region have their own less publicised and far less crowded gems.

Jun to October also sees rarer hurricane swell radiate out from southern Mexico. This energy is often felt right throughout Polynesia. With so many energy vectors at work it is very hard not to find a wave in North Korea. It's just a matter of finding the right one. Try to find one away from any military installations while your at it.