The profile of homing behavior in chum salmon (Oncorhynchus keta) that migr
ate from coastal sea to their natal river was not known well. We thus inves
tigated temporal behavioral profiles of pre-spawning chum salmon in terms o
f water depth and temperature in Ishikari Bay using a micro data logger in
1997 and 1998. Fish were caught by a set net, tagged and attached with a da
ta logger under MS222 anesthesia, and were released at the points 5 and 3 k
m off from the mouth of the Ishikari River in 1997 and 1998, respectively.
A temporal profile of water depth and ambient temperature along the migrato
ry pathway of recaptured salmon indicated that they usually stayed near the
surface where water temperature was relatively low. Conductivity-temperatu
re-depth recorder (CTD) data and the sea surface temperature estimated with
National Oceanic and Atmospheric Administration (NOAA) Advanced Very High
Resolution Radiometer (AVHRR) indicated that the influent of river water fo
rmed a low-temperature brackish subsurface layer near the mouth of the Ishi
kari River. These results indicate that chum salmon homing to the Ishikari
River prefer low water temperature, and wander in the subsurface layer of n
earshore area close to the mouth of the Ishikari River until they are motiv
ated to migrate upstream. The main factor that regulates behavioral pattern
of returned chum salmon in coastal sea should be distribution of water tem
perature.