PPT-Evolution of the electric potential and turbulence in OH and ECRH low-density plasmas

Author : amari687 | Published Date : 2024-09-18

Profiles of plasma potential in the OH and ECRH plasmas n е   10 10 19  m 3 T i   lt   06   keV and with switch on various groups of gyrotrons

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Evolution of the electric potential and turbulence in OH and ECRH low-density plasmas: Transcript


Profiles of plasma potential in the OH and ECRH plasmas n е   10 10 19  m 3 T i   lt   06   keV and with switch on various groups of gyrotrons. Captain Rocky Stone. . Chief Technical Pilot - Surveillance. FPAW - Oct. 24, 2013. Overview. Turbulence information, what do we do with it?. Turbulence information needs. Pilot and dispatcher training. Objective: TSW understand, transfer and apply energy concepts to electric fields and charges by solving problems involving electric fields and forces.. Let’s revisit energy concepts for a gravitational field. A 250 gram baseball is thrown upward with an initial velocity of 25m/s. What is the maximum height reached by the ball?. A.S. 5.1.1 – 5.1.4 due Monday. Reading reference: chapter 16. Question 16.1a. . Electric Potential Energy I . a). . proton. b). . electron. c). . both feel the same force. d) neither – there is no force. A. A. Tuccillo . on behalf of FTU Team. Since last ITPA in . Culham. Main Experimental . Programme. ended . in May . due to: . Explosion of two secondary breakers (20kV) on LH. Failure of McPherson UV spectrometer . Katherine McCaffrey. PhD Candidate, Fox-Kemper Research Group. Department of Atmospheric and Oceanic Sciences. Cooperative Institute for Research in Environmental Sciences. 1. Thank you to my advisor and collaborators:. A. Najmi – University of Maryland. B. . Eliasson. – University of . StrathClyde. X. Shao, G. . Milikh. , S. Sharma, K. Papadopoulos – University of Maryland. Introduction. Observation of DAILs (Descending Artificial Ionized Layers) (Pedersen et al 2009, 2011). local winds. Scales of Atmospheric Motion vs. Lifespan. We’ve already started to investigate some of the synoptic-scale features…. Topics for today’s discussion. Basically here’s our roadmap for the rest of the course.. Floating potential and envelop of ion saturation . current fluctuations are . correlated. Mode frequency:. 16 kHz: 50 kW ECRH. (ion transit frequency). 37 kHz: 100 kW ECRH . (GAM frequency). 2 D image of the mode. local winds. Scales of Atmospheric Motion vs. Lifespan. We’ve already started to investigate some of the synoptic-scale features…. Topics for today’s discussion. Basically here’s our roadmap for the rest of the course.. Bas van de . Wiel. , . Ivo. van . Hooijdonk. & Judith . Donda. in collaboration with:. Fred . Bosveld. , Peter Baas, . Arnold . Moene. , Harm . Jonker. , . Jielun. Sun, Herman Clercx, . e.a. .. Rick Curtis. Southwest Airlines Meteorology. ADF – 10/9/18. Turbulence Issues. Many Causes. CAT. Mountain Wave. Convection. Wake. Thermal. Difficult to Forecast. Difficult to Verify. Quiz. Question 1:. Katherine McCaffrey. PhD Candidate, Fox-Kemper Research Group. Department of Atmospheric and Oceanic Sciences. Cooperative Institute for Research in Environmental Sciences. 1. Thank you to my advisor and collaborators:. 3- Buoyant . Production/Consumption . Production. Term . III is large and positive near the ground, corresponding to a large generation rate of turbulence whenever the . underlying . surface is warmer than the air. this term represents the effects of thermals in the ML. It's with sunny days . . tokamaks. Michael . Barnes. University . of . Oxford. Culham. Centre for Fusion Energy. F. I. Parra, E. G. . Highcock. , A. A. . Schekochihin. , . S. C. Cowley, and C. M. Roach. Objective. Connor et al. (2004).

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