'Coriolis' presentation slideshows

Physical Processes Responsible for the Squall Line Dynamics

Physical Processes Responsible for the Squall Line Dynamics. We described the observed features and evolutions of squall lines earlier, questions remain, as to: Why does the strength and longevity of an MCS depend on the strength of environmental vertical wind shear?

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608 views • 50 slides

WHAT IS THE CORIOLIS EFFECT?

WHAT IS THE CORIOLIS EFFECT?. The Apparent Deflection of Objects Moving Across the Surface of the Earth from Their Intended Path. Derives from objects (air) moving across a moving frame of reference (the rotating latitude longitude grid of the world). Earth Rotating in

621 views • 50 slides

Thundersnow Apr 1, 2010

Thundersnow Apr 1, 2010. ATS 351 Lecture 10. Winds, Fronts, and Cyclogenesis. Outline . Atmospheric pressure Forces that affect the wind PGF, Coriolis, Centripetal, Friction Vertical Motion Fronts Mid-Latitude Cyclogenesis. Atmospheric Pressure. Ideal Gas Law p = ? RT

533 views • 44 slides

Lecture 10

1.03k views • 38 slides

Jason Hogan Stanford University January 17, 2013

Prospects for gravitational wave detection with atom interferometry. Seoul National University Seoul, Korea. Jason Hogan Stanford University January 17, 2013. Topics. Atom interferometry in a 10 meter tower. Gravitational wave detection with atoms. Cold Atom Inertial Sensors.

575 views • 36 slides

Chapter 22 Study Notes

Chapter 22 Study Notes. The Atmosphere. Chapter 22 Section 1. Characteristics of the Atmosphere. atmosphere. 1. The __________ is a mixture of ______, primarily nitrogen, oxygen, and argon, that surrounds Earth. gases. compounds.

434 views • 35 slides

Meteorology of Windstorms

601 views • 33 slides

Ocean Circulation

Ocean Circulation. Ocean Circulation. Ocean currents are affected by two kinds of forces; the primary forces that start water moving and determines its velocity. Secondary forces are factors that influence the direction and nature of its flow. Ocean Circulation.

603 views • 32 slides

Tim Oke and the extension-upwards of UHI-observations into the PBL

Prof. Robert Bornstein Dept. of Meteorology, San Jose State University San Jose, CA, USA, pblmodel@hotmail.com Prof. Julian Hunt University College, London, UK Presented at the T. R. Oke Symposium AMS Annual Meeting, Phoenix AZ Jan 2009 Funding source: NSF.

402 views • 26 slides

Convection, Wind, and the Coriolis Effect

427 views • 23 slides

cattaneo@flash.uchicago.edu

Chicago 2003. The solar dynamo(s). Fausto Cattaneo Center for Magnetic Self-Organization in Laboratory and Astrophysical Plasmas. cattaneo@flash.uchicago.edu. Chicago 2003. The solar dynamo problem. The solar dynamo is invoked to explain the origin magnetic activity

313 views • 22 slides

ODINAFRICA/GLOSS Sea Level Training Course

366 views • 22 slides

Effects to consider on oscillation frequencies

293 views • 21 slides

Steve Joiner, Technical Committee Chair John McDonough, Member OIF Board of Directors

Optical Internetworking Forum. Steve Joiner, Technical Committee Chair John McDonough, Member OIF Board of Directors. www.oiforum.com. What is the OIF?. Why the OIF? Organization of Working Groups Possible Interaction OIF / ITU-T Summary. What is OIF?. Launched in April of 1998

441 views • 18 slides

Salinity, Temperature, Density

? temp = ? density ? salinity = ? densit Thermocline Zone of rapid temp decrease Does this correlate with density and salinity?. Salinity, Temperature, Density. Below the surface waters (>500m) it is cold, dense, and saline.

351 views • 17 slides

SO441 Synoptic Meteorology

SO441 Synoptic Meteorology. Vorticity and vorticity advection. Vorticity : objectives. Develop a conceptual model of vorticity

303 views • 17 slides

Physical Oceanography

Physical Oceanography. Physical Characteristics of Water. Water displays the bizarre trait of increasing, then decreasing and later increasing its density with steadily lowered temperature. ( the range oceanographers use however is a simple inverse relationship .)

319 views • 16 slides

Gulf stream, recirculation, and other western boundary layer currents

Gulf stream, recirculation, and other western boundary layer currents. 1. the Gulf Stream 2. the coriolis force ant the gyre 3.the western boundary current layer. The Gulf Stream. powerful, warm, and swift Atlantic ocean current

351 views • 15 slides

Introduction

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