skip to main content
OSTI.GOV title logo U.S. Department of Energy
Office of Scientific and Technical Information

Title: Vertical fine structure observations in the eastern equatorial Pacific

Journal Article · · J. Geophys. Res.; (United States)

Measurements of vertical displacement and horizontal velocity finestructure near the equator at 110/sup 0/W in the eastern Pacific Ocean are reported. Profiles were scaled to a constant Bruent-Vaeisaelae frequency ocean (N/sub 0/ = 1 cph) in accordance with a WKBJ approximation. A total of 57 CTD casts between 3/sup 0/N and 3/sup 0/S taken during five cruises in 1979 were analyzed. Results show an equatorial enhancement of vertical displacement is similar variance for vertical wavelengths longer than 50 sdbar (stretched decibars). This enhancement is similar to that which has been reported at 125/sup 0/W and 179/sup 0/E. Difference between locations can be accounted for by the observed temporal variability at 110/sup 0/W. Coherence between vertical displacement profiles separated in time by dealys of 2 hours to 120 hour indicate that the high wave number structures were largely associated with time scales of 4 days and less. Meridionally, vertical structures longer than 300 sdbar were coherent within 50 km of the equator. We interpret this vertical displacement fine structure enhancement as high wave number equatorially trapped inertial-gravity waves. The velocity fine structure measurements in July 1979 also indicate equatorially enhanced horizontal kinetic energy for vertical wave lengths longer than 100 sdbar. The velocity structures persisted over the 56 hour of measurement and appeared to have longer time scales than the vertical displacements. Meridional energy measurement and appeared to have longer time scales than the vertical displacements. Meridional energy exceeded zonal energy; however, the two components were coherent. We interpret these velocity structures as inertial-gravity waves which were produced off the equator and are propagating through the equatorial region.

Research Organization:
NOAA Pacific Marine Enviromental Lab., Seattle, Washington 98105
OSTI ID:
5790688
Journal Information:
J. Geophys. Res.; (United States), Vol. 86:C11
Country of Publication:
United States
Language:
English

Similar Records

Deep currents and their interpretation as equatorial waves in the Western Pacific Ocean
Journal Article · Thu Jan 01 00:00:00 EST 1981 · J. Phys. Oceanogr.; (United States) · OSTI ID:5790688

Equatorial currents at semi-annual period in the Indian Ocean
Journal Article · Sat May 01 00:00:00 EDT 1982 · J. Phys. Oceanogr.; (United States) · OSTI ID:5790688

Vertical dispersion of inertial waves in the upper ocean
Journal Article · Fri May 20 00:00:00 EDT 1983 · J. Geophys. Res.; (United States) · OSTI ID:5790688