PPT-The Coupling of Convection, Large-Scale Atmospheric Dynamic
Author : conchita-marotz | Published Date : 2016-12-06
MODIS TRMM and ECMWFInterim Reanalysis Data TERRAAQUA PI Terry Kubar UCLAJIFRESSE CoI Ali Behrangi JPL Collaborator Graeme Stephens JPL MODIS Science Team Meeting
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The Coupling of Convection, Large-Scale Atmospheric Dynamic: Transcript
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. We regard the problem as a twodimensional resource allo cation problem for which different algorithms are pro posed Results from simulation experiments indicate the performance that can be achieved in terms of fragmentation and throughput 1 The Prob By. Chi . Bemieh. . Fule. August 6, 2013. THESIS PRESENTATION . Outline. . of. . today’s. presentation. Justification of the study. Problem . statement. Hypotheses. Conceptual. . framework. Research . extratropical. circulation. Steven Feldstein and Michael Goss. The Pennsylvania State University. IUGG, Prague, June 25, 2015. Questions. :. . 1. . What is the relationship between interference, Arctic sea ice, and tropical convection and how does it impact the . Brian Mapes, U of Miami. with. Baohua Chen (UM). Richard Neale (NCAR). Emily Riley (UM). Organ-ization. From Greek organon. about . instrumentality . or . working order. "Organized" convection. (weak) Something is making it patterned . Ceiling System K.P. RyuA.M. Reinhorn A. Filiatrault University at Buffalo, USA The two square frames were respectively mounted on each of two 7m7m shake table extensions. A 7.0m bridge structure was i Yuri Kovchegov. The Ohio State University. Outline. General concepts. Classical gluon fields, . parton. saturation. Quantum (small-x) evolution. Linear BFKL evolution. Non-linear BK and JIMWLK evolution. . of. the Standard . Model. : . r. enormalisation. FK8022, . Lecture. 2. Core. text:. Quarks. and . leptons. : an . introductory. . course. in modern . physics. , . Halzen. and Martin. Further. &. 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. Doswell C.A. III, 2001: Severe Convective Storms – An Overview. Severe Convective Storms, Meteor. Monogr., 28, no. 50, Amer. Meteor. Soc., 13-26. General Outline of this Review. Severe Convection Definitions & Distinctions. 1. Proposal: . Compact KE activity (3 months):. communicate SINATRA . work on FFIR precursor . indices. contribute to flood risk tool. d. efine optimal index/lead times. To discuss: . Since key scientist involved (Adrian Champion) is not joining TENDERLY and SINATRA ST1.3 outputs are ongoing, what is the most profitable use of this resource? . Model. : . r. enormalisation. FK8022, . Lecture. 2. Core. text:. Quarks. and . leptons. : an . introductory. . course. in modern . physics. , . Halzen. and Martin. Further. . reading. :. Basics . (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. P. Song and J. Tu . University of Massachusetts Lowell. Acknowledgments: V. M. Vasyliūnas. . . Conventional M-I-T Coupling: E-J paradigm . . New M-I-T Coupling: B-V paradigm. Physical differences. 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.
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