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Numerical and Dimensional Analysis for Prediction of Line Heating Residual Deformations
dimensional analysis 3-D finite element analysis elasto-plastic analysis residual deformations multiple regression analysis oxy-acetylene gas flame
2011/9/8
Line heating process is a very complex phenomenon as a variety of factors affects the amount of residual deformations. Numerical thermal and mechanical analysis of line heating for prediction of resid...
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...
Hydrographic Observations along the CODE Central Line off Northern California, 1981
CODE Central Line CTD Northern California
2009/1/21
Repeated CTD observations were made along a single section spanning the continental shelf off northern California at 38°40′N during 1981. The section consisted of nine standard stations between 1 and ...
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 ...
Interannual Westward-Propagating Baroclinic Long-Wave Activity on Line P in the Eastern Midlatitude North Pacific
Baroclinic Long-Wave Interannual Westward-Propagating
2009/1/7
For the period 1959–81, quasi-zonal hydrographic sections have been made between the southern coast of Vancouver Island (49°N, 126°W) and Ocean Station P (50°N, 145°W) approximately every two months. ...
Rossby Wave Scattering by a Meridional Line Barrier in an Infinitely Long Zonal Channel
Rossby Wave Scattering Meridional Line Barrier Infinitely Long Zonal Channel
2008/12/23
The interaction of a prescribed channel mode Rossby wave with a meridional line barrier situated in an infinitely long, zonally aligned channel is considered. An analytical solution for the scattered ...
Effects of Rotation on Convective Plumes from Line Segment Sources
three-dimensional nonhydrostatic numerical model Line Segment Sources Convective Plumes
2008/12/10
Effects of rotation on finite-length line plumes are studied with a three-dimensional nonhydrostatic numerical model. Geophysical convection with this source geometry occurs, for example, as the resul...
Interaction between Multiple Line Plumes：A Model Study with Applications to Leads
Laboratory experiments Interaction Multiple Line Plumes
2008/12/9
Laboratory experiments were performed to investigate the aggregate behavior of two identical parallel line turbulent plumes that were discharged to either a homogeneous water column or a two-layer flu...
A Numerical Investigation of Effects of a Tilt of the Zero Wind Stress Curl Line on the Subduction Process
three-dimensional ocean general circulation model nonzonal wind stress curl
2008/11/18
A three-dimensional ocean general circulation model is used to investigate the effects of an idealized, nonzonal wind stress curl on the subduction process in the subtropical gyre. Idealized zonal win...
The Effects of Decadal Oscillations of the Curl τ = 0 Line on Intergyre Water Exchange and Temperature Variability
Decadal Oscillations τ = 0 Intergyre Water Exchange Temperature Variability
2008/6/20
The effect of meridional movement of the curl τ = 0 line on the intergyre transport is investigated by passive tracer experiments in a double gyre circulation. Furthermore, the contribution to tempera...