نتایج جستجو برای: total heat flux

تعداد نتایج: 1060876  

2016
Anil Lal

DSMC simulation of re-entry of an object with shape and size close to that of ISRO’s Space Recovery Experiment (SRE) capsule has been analysed using the open-source tool dsmcFoam for three altitude conditions, viz. 85 km, 100 km and 115 km, and for three angles of attack, viz. 0, 20&40. The hypersonic free stream velocity of 8000 m/s and boundary surface temperature of 300 K have been used for ...

2012
Richard Pokorny Pavel Hrma

0022-3115/$ see front matter 2012 Elsevier B.V. A http://dx.doi.org/10.1016/j.jnucmat.2012.06.013 ⇑ Corresponding author at: Division of Advanced University of Science and Technology, Pohang, Repub E-mail address: [email protected] (P. Hrma The ultimate goal of studies of cold cap behavior in glass melters is to increase the rate of glass processing in an energy-efficient manner. Regretta...

Journal: :Agricultural and Forest Meteorology 2010

Journal: :Nano letters 2018
Qingyang Wang Renkun Chen

Phase change heat transfer is fundamentally important for thermal energy conversion and management, such as in electronics with power density over 1 kW/cm^2. The critical heat flux (CHF) of phase change heat transfer, either evaporation or boiling, is limited by vapor flux from the liquid-vapor interface, known as the upper limit of heat flux. This limit could in theory be greater than 1 kW/cm2...

2000
Gerd Krahmann Friedrich Schott

The semienclosed western Mediterranean Sea has proven to be a useful location to evaluate surface heat flux estimates. In the past the directly measured average oceanic heat transport from the Atlantic into the Mediterranean Sea through the Strait of Gibraltar of ;5.2 6 1.3 W m has been compared to estimates of the average heat flux across the surface of the Mediterranean Sea. On long timescale...

2012
Mohammad Valipour Seyyed Morteza Mousavi Reza Valipour Ehsan Rezaei

Usually the energy balance equation is used to estimate evapotranspiration. To calculating the potential evapotranspiration for long periods of time (more than a day), soil heat flux is assumed equal to zero. But in a catchment, the energy balance equation should be in terms of actual evapotranspiration is less than the potential. In this state, the amount of soil heat flux is not equal to zero...

2005
A.Yu. Gelfgat A. Rubinov P. Z. Bar-Yoseph A. Solan

The three-dimensional instability of the thermocapillary convection in cylindrical undeformable floating zones heated laterally is studied numerically. Different types of the boundary conditions, including radiation heating, linearized radiation and prescribed heat flux are used in the calculation. Stability diagrams showing the Prandtl number dependence of the critical Marangoni numbers that r...

2008
M. R. Myers

Ultrasonic time of flight measurements have been used to estimate the interior temperature of propulsion systems remotely. All that is needed is acoustic access to the boundary in question and a suitable model for the heat transfer along the path of the pulse train. The interior temperature is then deduced from a change in the time of flight and the temperature dependent velocity factor, which ...

2011
Melanie R. Fewings Steven J. Lentz

[1] In summer on the shallow New England continental shelf, near the coast the water temperature is much cooler than the observed surface heat flux suggests. Using depth‐integrated heat budgets in 12 and 27 m water depth calculated from observed surface heat flux, water temperature, and velocity, we demonstrate that on time scales of weeks to months the water is persistently cooled due to a mea...

Journal: :The New phytologist 2012
Andy VanLoocke Amy M Betzelberger Elizabeth A Ainsworth Carl J Bernacchi

• Here, we investigated the effects of increasing concentrations of ozone ([O(3)]) on soybean canopy-scale fluxes of heat and water vapor, as well as water use efficiency (WUE), at the Soybean Free Air Concentration Enrichment (SoyFACE) facility. • Micrometeorological measurements were made to determine the net radiation (R(n)), sensible heat flux (H), soil heat flux (G(0)) and latent heat flux...

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