PPT-The Coupling of Convection, Large-Scale Atmospheric Dynamics, and Sea-Surface Temperature

MODIS TRMM and ECMWFInterim Reanalysis Data TERRAAQUA PI Terry Kubar UCLAJIFRESSE CoI Ali Behrangi JPL Collaborator Graeme Stephens JPL MODIS Science Team Meeting Atmosphere Team Breakout Session. Peter J Minnett, Robert H Evans and . Gui. Podestá. Meteorology and Physical Oceanography. Rosenstiel School of Marine and Atmospheric Science. University of Miami. Overview. Sea-surface temperature (SST) as an Essential Climate Variable (ECV), and Climate Data Record (CDR). Aim. Calculate local natural convection heat-transfer coefficients for a sphere. Calculate the local boundary layer . Calculate experimental mean Nusselt number. Compare experimental and theoretical Nusselt numbers. By Ross . Nuechterlein. Convection. Convection.  is the movement of molecules within fluids and is one of the major modes of heat and mass transfer in liquids and gas.. Buoyancy . Buoyancy.  is an upward acting force exerted by a fluid , that opposes an object's weight.. For a constant property, laminar flow a . similarity solution. exists for the flow field . u. (. y. ). local boundary layer thickness. local skin friction coefficient. average skin friction coefficient. By Will Welch. For Jan . Kubelka. CHEM 4560/5560. Fall, 2014 . University of Wyoming. Forces on each particle are calculated at time t. The forces provide trajectories, which are propagated for a . small duration of time, . Explore: p. 672 - 678. Learning Targets. I can use simple models to simulate the forces acting on tectonic plates.. I can compare directions of plate motions with locations of hot spots, spreading ridges, and trenches. spectroradiometry. . Peter J Minnett. Meteorology and Physical Oceanography. Rosenstiel School of Marine and Atmospheric Science. University of Miami. 2. What is SST?. The infrared emission from the ocean originates from the uppermost <1mm of the ocean – the skin layer.. Where is Bullying happening at AMS?. The Results. Hot Spot. Percentage Bullied Here. Ranking. School Bus. 30%. 4. th. Hallways. 49%. 1. st. Class (Teacher in room). 41%. 2. nd. . Class (Teacher. not in room). &. related issues. P. . Mukhopadhyay. Climate v. Numerical Weather Prediction. NWP: . Initial state is CRITICAL. Don’t really care about whole PDF, just probable phase space. conservation of mass/energy to match observed state. 1. Aim : . develop an appreciation for the physical phenomena associated with internal flow and to obtain convection coefficients. Contents:. Entrance region . vs. fully developed region. Hydrodynamic effect consideration. Peter J Minnett, Robert H Evans and . Gui. Podestá. Meteorology and Physical Oceanography. Rosenstiel School of Marine and Atmospheric Science. University of Miami. Overview. Sea-surface temperature (SST) as an Essential Climate Variable (ECV), and Climate Data Record (CDR). Xiaoming Hu. 1. , Sergio A. Sejas. 2. , Ming Cai. 3. , . Zhenning. Li. 4. and Song Yang. 1. 1. School of Atmospheric Sciences, Sun . Yat-sen. University, Guangzhou, China. 2. NASA Langley Research Center, Climate Science Branch, Hampton, Virginia, USA. EARTH SURFACE. gravity. random. motion. Weight of all air molecules is propagated to surface by random motion of molecules. Random motion of molecules causes pressure to be applied in all directions. Why is it windy at the seaside?. Cold air sinks. Where is the freezer compartment put in a fridge?. Freezer compartment. It is put at the top, because cool air sinks, so it cools the food on the way down..