'Vorticity' presentation slideshows

Vortex Nernst effect Loss of long-range phase coherence The Upper Critical Field High-temperature Diamagnetism

Vorticity and Phase Coherence in Cuprate Superconductors Yayu Wang, Lu Li, J. Checkelsky, N.P.O. Princeton Univ. M. J. Naughton, Boston College S. Uchida, Univ. Tokyo S. Ono, S. Komiya, Yoichi Ando, CRI, Elec. Power Inst., Tokyo Genda Gu , Brookhaven National Lab. Vortex Nernst effect

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AOSS 401, Fall 2007 Lecture 22 November 02 , 2007

AOSS 401, Fall 2007 Lecture 22 November 02 , 2007. Richard B. Rood (Room 2525, SRB) rbrood@umich.edu 734-647-3530 Derek Posselt (Room 2517D, SRB) dposselt@umich.edu 734-936-0502. Class News November 02 , 2007. Homework 5 (Due Monday) Posted to web

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Wes Junker e-mail: norman.junker@noaa

SEMI-INTELLEGENT USE OF THE NCEP MODELS (FALL 1999). Wes Junker e-mail: norman.junker@noaa.gov. Presented at COMET for Hydromet 00-1 Friday, 15 October 1999. Why models have forecast problems.

690 views • 57 slides

Green Events

Green Events. Aug 3. 2006. Additional Comments: AEJ with 25 m/s jet core at 700 hPa extending from 0-23W. MCS and ITF cyclone appear to develop in phase. Low-level theta e advection on S side of ITF cyclone appears to help MCS.

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The Christmas Day Snowstorm of 2002

496 views • 39 slides

1.16k views • 33 slides

Scaling Laws for Residual Flows and Cross-shelf Exchange at an Isolated Submarine Canyon

Scaling Laws for Residual Flows and Cross-shelf Exchange at an Isolated Submarine Canyon. Dale Haidvogel, IMCS, Rutgers University Don Boyer, Arizona State University. With support from: NSF, ONR, Coriolis Lab. Gordon Research Conference, 2003. Premise and Approach.

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540 views • 29 slides

CEE 262A H YDRODYNAMICS

464 views • 26 slides

Sub Meso scales, Energy Cascades and Energy Dissipation

Sub Meso scales, Energy Cascades and Energy Dissipation. Jeroen Molemaker, Xavier Capet, James McWilliams IGPP, UCLA. Nested modeling (North East Atlantic). South-East Pacific. South West Atlantic. Los Angeles-Long Beach. Santa Monica Bay. Canary Islands (dx = 1 km).

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A model of the flow around bilge keels of FPSO hull sections subject to roll motions

A model of the flow around bilge keels of FPSO hull sections subject to roll motions. The University of Texas at Austin Ocean Engineering Group S. A. Kinnas, Y.-H. Yu, B. Kacham, and H. S. Lee Supported by the Offshore Technology Research Center (OTRC). Introduction. Motivation

537 views • 22 slides

Andy Hulme and J.E. Martin 28 th Hurricane/Tropical Meteorology 30 April 2008

The Role of Upshear Convection in Expediting the Tropical Transition of Atlantic Hurricane Karen (2001). Andy Hulme and J.E. Martin 28 th Hurricane/Tropical Meteorology 30 April 2008. Background. Tropical transition: TCG from a baroclinic precursor

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SO441 Synoptic Meteorology

SO441 Synoptic Meteorology. Vorticity and vorticity advection. What is vorticity ?. Many meteorological web sites include some form of vorticity contours on the 500-mb charts Why? How does having contours of vorticity help a meteorologist understand the atmosphere?.

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Air Masses and Fronts

METR 2413 5 April 2004. Air Masses and Fronts. Air Mass: a large volume of air that has remained over a surface for a long enough period of time to be modified by the surface relatively uniform horizontal temperature and moisture content

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Observed Vorticity Structure in Hurricane Rita (2005) Methodology Improvements

Observed Vorticity Structure in Hurricane Rita (2005) Methodology Improvements. Michael M. Bell National Center for Atmospheric Research/ Earth Observing Laboratory Colorado State University Wen-Chau Lee National Center for Atmospheric Research/ Earth Observing Laboratory.

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SO441 Synoptic Meteorology

SO441 Synoptic Meteorology. Lesson 6: Potential vorticity. Potential Vorticity. Concept of potential vorticity : Take a column of air defined by two potential temperature surfaces ( ? and ? + ?? ). Move this column of air eastward. Force it to go up and over a mountain range.

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b 0 =0

Sverdrup interior. ? 2 p + [(2*H* b 0 )/(d *|f 0 |)] ? x p + [2/d ] f 0 /|f 0 | ? y t (x) = 0. Stommel boundary. Vorticity:. b 0 =0. b 0 >0. -p ( x,y ). t (x). f -plane:. b -plane:. f const x const. f + x -. f const x const. f - x +. f + x = const. f + x = const.

250 views • 7 slides

MAE 5130: VISCOUS FLOWS

MAE 5130: VISCOUS FLOWS. Lecture 2: Introductory Concepts August 19, 2010 Mechanical and Aerospace Engineering Department Florida Institute of Technology D. R. Kirk. IMPORTANT RELATIONSHIPS. If the curl of the velocity field is zero Flow is irrotational

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Lamb LWT2 description method developed by P.James, Hadley Centre

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Practical Course SC & V

Practical Course SC & V. Streamfunction, Vorticity. Dr. Miriam Mehl. Stream Function. volume flow per time step contour lines = streamlines. Vorticity. vortical motion strength positive: clockwise negative: counter clockwise.

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