PPT-Heat Flux Sensors Isaac T. Leventon

6252014 Heat Flux Measurements Thermal management of materials and manufacturing processes Annealing film drying surface processing Heat exchangers dryers boilers condensers Fire Applications. Jacob Adams. ME 340 Winter 2010. The Problem:. Long complex boiling equations. Numerous cases and different variations can be confusing. Evaluation takes a lot of time. The Solution:. A Calculator!. Makes calculations quick and easy. Convection in the boundary layer occurs to transport heat moisture, and momentum from surface to free atmosphere. Two common scenarios:. 1) Daytime solar heating 2) cold-air outbreaks, lake effect. intraseaonal. and . interdecadal. time scales. Steven Feldstein. The Pennsylvania State University. September 11, 2012. Collaborators: . Sukyoung. Lee, . Tingting. . Gong, Nat Johnson. ,, . Changhyun. Linear Transport Model. Non-Linear phenomenon. Exponential Change. Capacitors. Orpheus Mall – Physics 7B. 1. Linear Transport Model: Flux = . j. Flux is the Amount of stuff (Fluid, Current, Thermal Energy, Particles, Fields – 7C) passing through a given area in a given amount of time. More simply, flux is the flow per unit area. . model . intercomparison. project (FAFMIP). Steering committee. :. Jonathan Gregory (U Reading and Met Office),. . Stephen . Griffies. . (GFDL),. . Detlef. Stammer (U Hamburg), Oleg . Saenko. (. V. A. Soukhanovskii (LLNL). Acknowledgements: . NSTX Team. NSTX Results Review. Princeton, NJ. Wednesday, 1 December . 2010. NSTX. Supported by . College W&M. Colorado Sch Mines. Columbia U. CompX. model . intercomparison. project (FAFMIP). Steering committee. :. Jonathan Gregory (U Reading and Met Office),. . Stephen . Griffies. . (GFDL),. . Detlef. Stammer (U Hamburg), Oleg . Saenko. (. Basics. The . global hydrological cycle. Precipitation. Soil water (lab work). Surface energy . fluxes. Evaporation . and transpiration. Snowpack. Groundwater. Streamflow. Floods . & . Droughts. Water management. 6/25/2014. Heat Flux Measurements. Thermal management of materials and manufacturing processes. Annealing, film drying, surface processing. Heat exchangers, dryers, boilers, condensers. Fire Applications. Jacob Adams. ME 340 Winter 2010. The Problem:. Long complex boiling equations. Numerous cases and different variations can be confusing. Evaluation takes a lot of time. The Solution:. A Calculator!. Makes calculations quick and easy. flow structure of the interaction shows but clearly defined complex shock seen to underexpanded and “plumes” into a barrel with the terminal shock resulting into a supersonic been observed T Qnet. = (. Downwelling. Shortwave + Upwelling Shortwave (albedo)) + (. Downwelling. . Longwave – Upwelling Longwave). Substituting the GEOS-5 expressions for each of these fields gives:. Sfc. . Aim: . To record soil temperature at different depths and computation of soil heat flux. Instruments required. : . Soil thermometer for 5,10, and 20cm depths. Computation of soil heat flux (. q. T. ). Basic Meteorological Direct fluxes:. Sensible Heat, H. s. Latent Heat, H. l. Momentum, . τ. Kinetic Energy=-. τ. *U(z). Fluxes on Ocean Side. Momentum and Energy (waves and currents). Thermodynamic .