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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...
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 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 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...
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 ...
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...
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 ...
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 ...
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 ...
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...
Ocean Radiant Heating. Part I: Optical Influences     Ocean Radiant Heating  Optical Influences       font style='font-size:12px;'> 2008/7/2
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...
Accurate determination of sea surface temperature (SST) is critical to the success of coupled oceanatmosphere models and the understanding of global climate. To accurately predict SST, both the quant...

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