Cruise three of the N.B. Scofield for 1956. Cruise Report 56-S-3

(PDF contains 3 pages.)

Cruise four of the N.B. Scofield for 1956. Cruise Report 56-S-4

(PDF contains 2 pages.)

Cruise 5 of the N.B. Scofield for 1956. Cruise Report 56-S-5

(PDF contains 2 pages.)

Cruise 6 of the N.B. Scofield for 1956. Cruise Report 56-S-6

(PDF contains 2 pages.)

Cruise 7 of the N.B. Scofield for 1956. Cruise Report 56-S-7

(PDF contains 2 pages.)

Cruise 8 of the N.B. Scofield for 1956. Cruise Report 56-S-8

(PDF contains 2 pages.)

Cruise 57-S-1 of the N.B. Scofield

(PDF contains 1 page.)

Cruise 3 of the N.B. Scofield for 1957.

(PDF contains 3 pages.)

Cruise 4 of the M/V N.B. Scofield for 1957.

(PDF contains 3 pages.)

Cruise 5 of the N.B. Scofield for 1957.

(PDF contains 4 pages.)

A Baseline Study of the Moss Landing/Elkhorn Slough Environment

In July, 1974 we began a baseline study of the Moss Landing-Elkhorn Slough marine environment for PG&E as mandated by the Coastal Commission. This report constitutes results of the first year's program. It is divided into three sections, oceanography, benthic invertebrate ecology, and fish and zooplankton ecology. (PDF contains 226 pages)

Some aspects of the temperature, oxygen and nutrient distributions in Monterey Bay, California. Annual Report, Part 1, 1973

Seasonal variations in temperature, dissolved oxygen, and nutrients in the nearshore areas and in the canyon area of Monterey Bay, California during 1971-1972 were similar~ During upwelling periods, however, water in the nearshore areas was higher in temperature and oxygen and lower in nutrients than water in the canyon area~ This was caused by upwelled water moving north and south of the canyon into counterclockwise and clockwise flow in the northern and southern ends of the bay respectively. The water was heated by insolation and depleted of its nutrients by photosynthesis during this movement. The residence time of water in the nearshore northern and southern bay during upwelling is estimated to be 3 to 8 days, and this fits well into the above circulation pattern and average measured current velocities of 10 to 15 cm/sec~ There is sorne evidence that this circulation pattern and the estimated residence time may be also valid for on-upwelling periods. Upwelling apparently occurred in Monterey Submarine Canyon at rates of 0.4 to 2.9 m/day and was stronger in 1971 than 1972. (PDF contains 107 pages)

A Comparison of the Range and Movements of Acmaea digitalis Eschscholtz, Acmaea scutum Eschscholtz, Acmaea limatula Carpenter and Lottia gigantea Sowerby

Ten limpets (4 Acmaea digitalis , 4 Acmaea scutum, 1 Acmaea limatula, and 1 Lottia gigantea) were marked and their movements observed over a thirteen day period. Recordings of positions were made on a map, and the path of each was drawn on the map from day to day. Acmaea digitalis showed the greatest range, mostly in a vertical direction, and moved usually at night during high tide. Acmaea scutum showed a more limited range in a horizontal direction, and moved both day and night during high tide. Acmaea limatula had a horizontal range similar to A. scutum,, but exhibited no movement during the day time. Lottia gigantea had the most restricted range of any limpet studied, and moved only at night during high tide. This is a student paper done for a University of California Berkeley Zoology class. Since UCB didn't have its own marine lab at the time, it rented space at Hopkins Marine Station where this work was done. Gene Haderlie went on to earn his Ph.D. from Berkeley and later became a Professor at the Naval Post Graduate School in Monterey. (PDF contains 23 pages)

Status of the fisheries report - an update through 2006

(PDF contains 153 pages.)