The Sea of Japan is a 978,000-km2 marginal sea, located in the western periphery of the North Pacific. It is bordered by the Eurasian continent to the west and the Japanese archipelago to the east, and is connected to the Okhotsk Sea through the narrow Soya Strait to the north, to the North Pacific through Tsugaru Strait in the east, and to the East China Sea through the narrow Tsushima Strait to the south. The average depth is about 1667 m and its deepest point is 3742 m. The warm Tsushima Current flows into the Sea of Japan through Tsushima Strait from the south and runs along the Japanese coast to the north and flows out through Tsugaru Strait into the North Pacific and through Soya Strait into the Okhotsk Sea. Due to the narrow (ca. 200-km width) and shallow (90–130-m depth) geography of Tsushima Strait, limited water circulation occurs in the upper layers shallower than ca. 300 m depth. Deeper than that, so-called “Japan Sea Proper Water”, which is characterized by extremely cold (0–1 °C) and high salinity (34.1 PSU) water, is distributed throughout the Sea of Japan (http://www.jma-net.go.jp/jsmarine/japansea.html).
Giant squid are estimated to live in mesopelagic waters of temperate open oceans (Clarke 1966; Roper and Boss 1982). Kubodera and Mori (2005) revealed that a giant squid off the Ogasawara Islands in the North Pacific appeared at 900 m depth and swam up to 600 m to escape from a jig on which its tentacle was hooked. They reported that the water temperatures at 900 and 600 m depth were about 4 and 6 °C, respectively. This evidence suggests that giant squid in the Sea of Japan might not be permanent residents but, rather, migrants from the south, passing through bottom layer waters of the Tsushima Strait when the water temperature there decreases to below ca. 6 °C in mid-winter to early spring. Once they have traveled into the Sea of Japan, water temperatures in the deep layer are too cold and they probably move through the water column to the more suitable temperature zone between the warm surface layer and the cold Japan Sea Proper Water during summer to fall.
Okiyama (1993) suggested a possible reason for why giant squid have been occasionally found dead on beaches or caught in fixed nets set in Japanese coastal waters of the Sea of Japan during winter to early spring. At the beginning of winter, the surface water is cooling down from the northern peripheries along the continental coasts and the cold surface water at 0–1 °C subsides into deeper stratum, which is the origin of the Japan Sea Proper Water. Cold water subsidence commences from the north and gradually extends to the south as winter progresses. This cold water movement might reduce the suitable temperature habitat of the giant squid both horizontally and vertically. They are forced to move southward and to shallower depths. Some individuals would be weakened by exposure to extremely cold waters and then transported by eddies of the Tsushima Current and strong northwesterly seasonal winds, which would result in them coming closer to Japanese coastal waters and explain them being trapped in fixed nets and/or becoming stranded on beaches along the Japanese coast.
Although this is one possible explanation for the occurrence of giant squid in Japanese coastal waters of the Sea of Japan, the unusual mass findings of giant squid in 2014 and 2015 are likely due to a different mechanism. Judging from 10-day and monthly mean water temperature anomalies at the surface and 100 m depths during the winter seasons of 2014 and 2015, the water temperatures at these depths were apparently lower in both years than usual, especially in January 2014 and February 2015. Prominent large-scale cold water masses that developed in the middle layer of the central portion of the Sea of Japan in 2014 and 2015 might have worked strongly to carry the giant squid to the surface layer and towards the Japanese coast. In addition, although there were few records of giant squid during 2008–2013 (Kubodera, personal observation), it is possible that a number of giant squid entered the Sea of Japan during these years and survived there until 2014.
One of the important biological findings of giant squid deduced from the recent mass findings is the bimodal size frequency distribution (80–160 cm DML with a mode at 110 cm and 160–190 cm DML with a mode at 170 cm DML) in winter season. The smaller group had a nearly even sex ratio and the larger group was comprised entirely of females. Wada et al. (2015) recently reported that two young giant squid measuring 33 cm DML were caught by purse seine net in the southwestern Sea of Japan on June 14, 2013. Assuming that a young giant squid measuring 33 cm DML in June grows to 110 cm DML by January, the monthly growth rate would be ca. 11 cm DML. This value represents very rapid growth and an inclination towards an S-growth curve, with lower growth rates in earlier and later life stages. The overall size composition of giant squid in the Sea of Japan suggests a longevity of 2 years for males and 3 years for females.
Roper and Shea (2013) reviewed current knowledge on the taxonomy and systematics, distribution, population size, habitat use, age and growth, predation and feeding, reproduction and life cycles, and functional morphology of giant squid and found wide gaps. The present mass findings of 57 individuals within a relatively short period of time, two winter seasons between 2014 and 2015, and a restricted area of Japanese coast of the Sea of Japan have greatly increased the available information necessary to understand the natural history of giant squid.
Roper et al. (2015) investigated records of giant squid that were discovered in the western North Atlantic Ocean between Newfoundland and the Gulf of Mexico and provided detailed information on 28 individuals found during 1952–2011. They recognized a general upwards trend in the number of sightings in the 1990s and 2000s, reflecting the increased scientific awareness and growing popular interest in giant squid. In Japan, we had two large events concerning giant squid in 2013. One was a TV program airing on Japan’s national public broadcasting organization, NHK, in January, which broadcast the first encounter with a live giant squid using a manned submersible in the deep sea off the Ogasawara Islands. The other was a special exhibition entitled “The Deep” held at the National Museum of Nature and Science in Tokyo from July to September, in which a preserved giant squid specimen as well as videos of live giant squid filmed for the first time were introduced. These two events made Japanese people, especially the younger generations, become more interested in the giant squid. Such a boom in attention directed towards giant squid and other deep-sea creatures likely increases the awareness of giant squid among people in coastal regions and encourages them to alert the media and local experts to any findings.
We also suggest that the Sea of Japan may work as a large natural trap for giant squid migrating from the south during early spring. Their distribution spreads widely into the mid-layers, which are within their suitable water temperature zone, and they continue to grow during summer and fall. In winter, the oceanographic characteristics of the Sea of Japan may compel giant squid to move southward and to shallower surface waters, where the coastal eddy of the Tsushima Current and strong westward seasonal winds may carry them to Japanese coastal waters, where they become entangled in fixed nets or stranded on beaches. For future “giant squid” research, the Japanese coasts of the Sea of Japan during the winter months would be the most suitable area to encounter live giant squid.