Index Catalog // ScholarsArchive@OSU

Creator:: Moum, J. N. and Osborn, T. R.
Abstract:: A series of profiles of velocity microstructure along 152°E in the western North Pacific Ocean were collected in May–June 1982. Large, averaged turbulent dissipation rates, ϵ, found in the main thermocline (400 to 1000 m) were determined by a combination of large independent estimates of ϵ and a greater rate...
Resource Type:: Article

Creator:: Paulson, Clayton A., Baumann, R. J., deWitt, L. M., Spoering, T. J., and Wagner, J. D.
Abstract:: Observations of temperature and pressure in the upper 100 m were taken with a towed thermistor chain in January 1980 north of Hawaii. The observations were taken as a part of a cooperative investigation of the North Pacific subtropical front entitled FRONTS-80. The chain was towed on four occasions over...
Resource Type:: Technical Report
Full Text:: Observations in FRONTS-80 by C. A. Paulson, R. J. Baumann, L. M. deWitt, T. J. Spoering and J. D. Wagner

Creator:: Dillon, T. M., Moum, J. N., Chereskin, T. K., and Caldwell, D. R.
Abstract:: The conventional view of equatorial dynamics requires that the zonal equatorial wind stress be balanced, in the mean, by the vertical integral of “large-scale” terms, such as the zonal pressure gradient, mesoscale eddy flux, and mean advection, over the upper few hundred meters. It is usually presumed that the surface...
Resource Type:: Article

Creator:: Moum, J. N., Osborn, T. R., and Crawford, W. R.
Abstract:: Turbulence measurements from the central equatorial Pacific in February 1982 have been analyzed and compared to synoptic CTD and current velocity profiles and current meter data. These suggest considerably more time (if not space) variability than had previously been anticipated. Above 300 m at the equator the turbulence levels were...
Resource Type:: Article

Creator:: Dewey, R. K., Moum, J. N., Caldwell, D. R., Sullivan, T. C., Baer, J. T., Kreth, R. D., and Neeley-Brown, M. D.
Abstract:: Temperature, salinity, density and turbulent dissipation profiles measured using the Rapid Sampling Vertical Profiler during the Coastal Transition Zone Experiment, July 1988.
Resource Type:: Technical Report
Full Text:: . Neeley- N00014-87-K-0009 J. N. Moum J. T. Baer Brown D. R. Caldwell R. D. Kreth 9. PERFORMING

Creator:: Jackson, T. L., Gardner, E. Hugh, Mansour, N. S., and Mack, H. J.
Abstract:: Facts and recommendations in this publication may no longer be valid. Please look for up-to-date information in the OSU Extension Catalog: http://extension.oregonstate.edu/catalog
Resource Type:: Technical Report

Creator:: Mansour, N. S., Mack, H. J., Gardner, E. Hugh, and Doerge, T. A.
Abstract:: Facts and recommendations in this publication may no longer be valid. Please look for up-to-date information in the OSU Extension Catalog: http://extension.oregonstate.edu/catalog
Resource Type:: Technical Report

Creator:: Mansour, N. S., Mack, H. J., Gardner, E. Hugh, and Jackson, T. L
Abstract:: Facts and recommendations in this publication may no longer be valid. Please look for up-to-date information in the OSU Extension Catalog: http://extension.oregonstate.edu/catalog
Resource Type:: Technical Report

Creator:: Chereskin, T. K., Levine, Murray D., Harding, A. J., and Regier, L. A.
Abstract:: Measurements of upper ocean shear made during the Mixed Layer Dynamics Experiment (MILDEX) provide evidence of large horizontal scale motion at near‐inertial frequency. The measurements consist of shipboard acoustic Doppler current profiles. Four large‐scale spatial surveys of 2–4 days duration were made by the R/V Wecoma as a set of...
Resource Type:: Article
Full Text:: , J. _Phys. Oceano•r., 10, 385-398, 1980. Sanford, T. B., R. G. Drever, and J. H. Dunlap, A

Creator:: Moum, J. N., Caldwell, D. R., Paulson, C. A., Chereskin, T. V., and Regier, L. A.
Abstract:: A 3°N to 3°S transect of the equator at 140°15'W was made in November 1984. Vertical profiles of temperature, conductivity and turbulent dissipation were obtained at approximately 1 km intervals. Contrary to previous results, we found no obvious peak in dissipation either at the equator or clearly associated with the...
Resource Type:: Article

ScholarsArchive@OSU