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Observations of the Deepening of the Wind-Mixed Layer in the Northeast Pacific Ocean
Northeast Pacific Ocean Wind-Mixed Layer
2009/3/26
Measurements of winds, currents and temperature are used to describe the response of the upper ocean in the northeast Pacific to the passage of an August 1971 synoptic-scale meteorological disturbance...
An Evaluation of the Quality of Sea Surface Temperatures and Salinities Measured at Station P and Line P in the Northeast Pacific Ocean
Sea Surface Temperatures Salinities Measured Northeast Pacific Ocean
2009/2/23
A variety of oceanographic data comprising mainly temperatures collected by bucket, engine-intake, reversing thermometers and thermosalinograph, and salinities obtained with bucket, seawater loop, dee...
The Anticyclonic, Baroclinic Eddy off Sitka, Alaska, in the Northeast Pacific Ocean
Anticyclonic Baroclinic Eddy Northeast Pacific Ocean
2009/2/8
Among the many mesoscale eddies found in the northeast Pacific Ocean is a well-developed, anticyclonic baroclinic eddy, situated within a few hundred kilometers of Sitka, Alaska (57°N. 138°W). It has ...
High-Height Long-Period Ocean Waves Generated by a Severe Storm in the Northeast Pacific Ocean during February 1983
Long-Period Ocean Waves Northeast Pacific Ocean February
2009/1/20
Unusally severe storms occurred in the northeast Pacific Ocean between January and March 1983, and waves from these storms caused extensive erosion and damage along the U.S. west coast. Wave condition...
Annual and Interannual Variability of Steric Sea Level along Line P in the Northeast Pacific Ocean
Steric Sea Level Line P Northeast Pacific Ocean
2009/1/12
Twenty-five and 22 years of hydrographic-STD casts from Station P and Line P, respectively, have been utilized to describe the annual and interannual variability of thermosteric, halosteric and total ...
Wind-forced Variations in Sea Surface Height in the Northeast Pacific Ocean
Sea surface height Northeast Pacific Ocean Wind-forced Variations
2008/12/19
Sea surface height (SSH) anomalies from the Geosat altimeter for the northeast Pacific Ocean were analysed to determine their annual and interannual fluctuations over a 2.5-year period. The interannua...
Circulation within the Ocean Storms Area Located in the Northeast Pacific Ocean Determined by Inverse Methods
Ocean Storms Area Northeast Pacific Ocean Inverse Methods
2008/12/18
An inverse model was applied to hydrographic data obtained from a cruise in the autumn of 1987 in a small area (300 × 250 km) in the northeast Pacific Ocean. The inverse model used geostrophy and a li...
Interdecadal Variability in a Numerical Model of the Northeast Pacific Ocean：1970–89
Interdecadal Variability Northeast Pacific Ocean Numerical Model
2008/12/11
Variations in the thermocline depth of the northeast Pacific Ocean during 1970–1989 are investigated using a reduced-gravity numerical model forced by the local surface wind stress and at the southern...
Bottom Temperature Fluctuations in the Northeast Pacific Ocean at Depth 920 to 1140 m
Bottom Temperature Fluctuations Northeast Pacific Ocean
2008/7/2
Motions of water at medium depths on the continental slopes have seldom been measured. In this experiment, seven thermistors were placed on the ocean bottom at depths from 920 to 1410 m on the contine...
Spatial and temporal patterns in larval supply at hydrothermal vents on the northeast Pacific Ocean
Spatial and temporal patterns larval supply hydrothermal vents northeast Pacific Ocean
2014/5/19
Larval supply in marine benthic invertebrates influences patterns of settlement and recruitment to adult populations. To successfully colonize newly formed or distant hydrothermal vents, which are dis...