Data from 1971 to 1993 are used to examine characteristics and variabi
lity of the subsurface temperature maximum in the Aleutian Basin of th
e Bering Sea. The temperature of this feature varies from similar to 3
5 degrees C to 4.6 degrees C at depths of similar to 150-400 m, and si
gma-t density is usually in the range 26.6-26.9. The variability is ca
used mainly by the absence or presence of inflow of warm, low-density
Alaskan Stream water through Amukta Pass. Thus the environment of fish
stocks is far from uniform.