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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...
Numerical Model of Convection Driven by a Surface Stress and Non-Uniform Horizontal Heating
Convection Driven Surface Stress Non-Uniform Horizontal Heating
2009/4/3
This paper examines the two-dimensional convective motion of a nonrotating incompressible Boussinesq fluid heated non-uniformly from below. The fluid container is rectangular; the side and top boundar...
Interannual Variation in Net Heating at the Surface of the Tropical Pacific Ocean
Tropical Pacific Ocean Net Heating tropical Pacific Ocean
2009/2/5
Interannual variations of net surface heating of the tropical Pacific Ocean are analyzed for the period 1957–76. Special emphasis is given to exploring the relationship between these variations and th...
The Role of Local Heating in Producing Temperature Variations in the Offshore Waters of the Eastern Tropical Pacific
Local Heating Temperature Variations Offshore Waters Eastern Tropical Pacific
2009/2/5
The role of local heating in producing annual and interannual sea-surface temperature variations in the eastern tropical Pacific is studied. Removed from the eastern boundary (122°W), and off the equa...
Large Diurnal Heating of the Sea Surface Observed by the HCMR Experiment
Day–night surface temperature Sea Surface HCMR Experiment
2009/1/19
Day–night surface temperature differences measured in the infrared (10.5–12.5 μm channel) by the HCMR satellite experiment frequently show large diurnal heating (several °C) of the upper layer of the ...
Vertical Circulation Revealed by Diurnal Heating of the Upper Ocean in Late Winter. Part II：Modeling
Vertical Circulation Upper Ocean Diurnal Heating
2008/12/30
A heat budget for observations at current meters in the mixing layer beneath a freely drifting spar buoy showed that the buoy must be in a convergence zone, where transport of warm water downwards enh...
Vertical Circulation Revealed by Diurnal Heating of the Upper Ocean in Late Winter：Part I：Observations
Vertical Circulation Upper Ocean Diurnal Heating
2008/12/30
During a 5-day period in late winter 1984, temperature were measured at 9 depths beneath a drifting spar buoy to a relative accuracy of 2 mK. The depths ranged from 15 to 145 m in a mixing layer that ...
Slippery Near-Surface Layer of the Ocean Arising Due to Daytime Solar Heating
Slippery Near-Surface Layer Daytime Solar Heating Ocean Arising
2008/12/27
Measurements made in the Equatorial Atlantic during the 35th cruise of the R/V Akademic Vernadsky using a free-rising profiler and drifters revealed a near-surface slippery layer of the ocean arising ...
The Upper-Ocean Response to Surface Heating
Long-Term Upper-Ocean Study Frontal Air-Sea Interaction Experiment Upper-Ocean Response Surface Heating
2008/12/9
Moored observations of atmospheric variables and upper-ocean temperatures from the Long-Term Upper-Ocean Study (LOTUS) and the Frontal Air-Sea Interaction Experiment (FASINEX) are used to examine the ...
Rotating Convection Driven by Differential Bottom Heating
Rotating Convection Driven Differential Bottom Heating
2008/7/11
Convection experiments were carried out in a rectangular tank as a model of oceanic meridional overturning circulation. The objective was finding a relation between the meridional heat flux and therma...
Radiative transfer calculations are used to quantify the effects of physical and biological processes on variations in the transmission of solar radiation through the upper ocean. Results indicate tha...
Ocean Radiant Heating. Part II: Parameterizing Solar Radiation Transmission through the Upper Ocean
Ocean Radiant Heating Parameterizing Solar Radiation Transmission Upper Ocean
2008/7/2
Accurate determination of sea surface temperature (SST) is critical to the success of coupled ocean–atmosphere models and the understanding of global climate. To accurately predict SST, both the quant...