Life--in Long Beach, a survey of community welfare services and needs ...

Mode of access: Internet.

Long Beach Harbor numerical analysis of harbor oscillations :

"September 1976."

Long Beach Harbor numerical analysis of harbor oscillations :

"September 1976."

Long Beach Harbor numerical analysis of harbor oscillations :

"February 1977."

The ports of Los Angeles, Long Beach, San Diego and San Luis Obispo, California ... (Revised, 1930)

The frontispiece in pt. 2 and part of the plates, maps and tables are folded.

Annual report - Long Beach Water Department.

Report year ends June 30.

Los Angeles and Long Beach Harbors model study : resonant response of the harbors for Phase 1 of the Los Angeles deep-draft dry bulk export terminal /

"January 1984."

Joyce Chapman at Uncle Charlie's birthday party, Long Beach, California,1933

Joyce Chapman at Uncle Charlie's birthday party, an all-day event at C. C. Chapman's home, 4th Street, Long Beach, California, 1933.

Los Angeles-Long Beach (LA-2) ocean dredged material disposal site designation : environmental impact statement.

Mode of access: Internet.

Beach changes at Long Beach Island, New Jersey, 1962-73 /

Beach profile line data collected from 32 profile sites along Long Beach Island, New Jersey. A total of 2,158 profile line surveys were examined, using empirical eigenfunction analysis and other measures of beach variability. Most profile lines have shown an accretionary trend since 1962 with rates between 2.3 and 0.24 meter per year in spite of erosion estimates due to sea level rise on the order of 0.68 meter per year. A great deal of variability in profile line change takes place along the beach, increasing from north to south, due to the location of profile lines relative to structures and offshore linear shoals. Detailed closely spaced profile lines taken over a year in a groin field near the north end of the island indicate littoral transport directions shift from north to south. Evidence of a littoral transport node near the north end of the groin field has been found. Net transport of the node is toward the south, but the rate could not be established due to lack of adequate wave data. Profile line variability within groin cells shows that single profile lines are not sufficient to determine the net change within a cell. The design of future beach monitoring studies should consider coastal structures, offshore bathymetry, the method of analysis, and the scales of processes under study. A coastal storm in November 1968 moved the MSL back as much as 22 meters; however, the beach recovered without artificial measures. The offshore bathymetry shows a series of shoreface-connected linear shoals at several locations along the island. Limited data show that these have remained stable and that most beach variability takes place in water shallower than 3 meters.