Topic outline
Why do ocean observations at Funka Bay?
Funka Bay is an inner bay located in the southwestern part of Hokkaido.
The areas shaded in black in the figure on the left below were once oceans hundreds of thousands of years ago. Funka Bay is thought to have been a strait connecting the Pacific Ocean and the Sea of Japan long ago.
There are many active volcanoes around Funka Bay, hence its name (“Funka” means “eruption” in Japanese[A1] ).
Please look at the ocean current map (left figure below). You can see the cold Oyashio current and the warm Kuroshio current (→Tsugaru Warm Current) flowing nearby.
In early spring, the Oyashio water flows into Funka Bay. In the late summer, the Tsugaru Warm Current flows into Funka Bay.
The water in Funka Bay switches out in early spring and late summer. Hence, the water remains in the bay from spring to summer and autumn to winter.
During that period, it is possible to track water changes over time in the open-ocean water (Oyashio water, Kuroshio water).
（It is almost impossible to observe the same water in areas with an ocean current even if observations are recorded in the same location every month）
We are continuing ocean observations of Funka Bay every month with the idea that we will be able to discover various things.
We have clarified the factors that change the concentration of plant-derived isoprene and the resultant knowledge on the generation of organic iodine gas.
There is a diatom bloom every year for about three weeks starting in early March. Approximately half of the annual primary production in Funka Bay is supported by this diatom bloom in the spring.
The following is a distribution of chlorophyll concentration on the sea surface, which was measured using satellites.
What is measured at Funka Bay?
- For the time being, we measure everything we can. Though we have not fully analyzed everything…
We measure as many basic parameters of ocean chemistry as possible.
Seawater components：dissolved oxygen, total carbonate, alkalinity, nutrients (five components), organic gas components (halocarbons, isoprene, of which methane is included)
Particle components： diatom suspensions during diatom bloom (vertically collected with NORPAC Net) → Carbon, nitrogen, phosphorus, silicon (of which, iodine is also included)
Sediment components： nutrients, organic gas components, carbon, nitrogen, phosphorus, silicon
（This paper focuses on the analysis of organic gas components, which is the main research theme. Of these, carbon, nitrogen, and silicon are included）
Photobook of observations at Funka Bay (some include links to LASBOS YouTube)
A large amount of diatom aggregate is collected and used for the decomposition culture experiments. We always receive the cooperation of members of the Fisheries Science Group. Thank you.
This is a sediment sample.
We attempted to investigate the chemical environment of sediments and the state of benthic organisms.
Ashura sediment core sampler. This can collect three sediment core samples at a time.
The landscape looks beautiful during winter. This is Mt. Yotei.
The picture below shows a sample treatment where the pore water is sucked out on board the Ushio-Maru.
Mr. Miyashita (left) was recording observations with a runny nose like a little kid.
The top two students who conducted the Funka Bay observations. They have both found jobs at an environmental consulting firm.
The dining scene at Ushio-Maru. We want to eat seafood curry on every voyage!
CTD rosette sampler on Ushio-Maru. A miniature size around this scale is easier to use.
Observations from around ten years ago. Professor Emeritus Kuma (right) stood on the front lines of the observation process until just before his retirement.
Water is sampled in narrow spaces.
A short break between observations
