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). 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, . Heat and Work transfer. (quantitatively). Thermodynamics & Heat Transfer. Thermodynamics. Heat Transfer. Study of . “How heat flows”. every activity involves heat transfer. . Driving Potential. 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.. MODIS. , TRMM, and ECMWF-Interim Reanalysis Data. TERRA/AQUA PI: . Terry Kubar (UCLA/JIFRESSE). Co-I: . Ali . Behrangi. (JPL). Collaborator: . Graeme Stephens (JPL). MODIS Science Team Meeting – Atmosphere Team Breakout Session. &. 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. . CONVECTION . FIXED . POWER TD1005. Objectives. To find the surface . temperature.. To . compare the . surface. temperature of the heat transfer surfaces in force and free convections for fixed input power.. (mainly deep convection, although issues are broader). Invited review article for JMSJ in preparation. Brian Mapes. University of Miami . WCRP Open Science Conference, Denver . October 2011. B6_Mapes.pptx Plaza C room. By Will Welch. For Jan . Kubelka. CHEM 4560/5560. Spring, 2017. University of Wyoming. Why Molecular Dynamics?. 1. Scale: Large collections of interacting particles that cannot (and should not) be studied by quantum mechanics . 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). Andrey . Vlasenko. , Armin Köhl, Detlef . Stammer. Institut für . Meerskunde. Universität Hamburg. Hamburg. TASK. Task 1.2.1 Identification of the atmospheric response to ocean surface state changes. 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. 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.. Massachusetts Institute of Technology. Two Points of View. Macroscopic. : What sets the frequency of tropical cyclones on the planet? Are tropical cyclones agents in a system that maintains itself in some critical state?.