'Gradient wind' diaporamas de présentation

AOSS 401, Fall 2007 Lecture 15 October 17 , 2007

AOSS 401, Fall 2007 Lecture 15 October 17 , 2007. Richard B. Rood (Room 2525, SRB) rbrood@umich.edu 734-647-3530 Derek Posselt (Room 2517D, SRB) dposselt@umich.edu 734-936-0502. October 17 , 2007. Exam results Roadmap for the next month Introduction to vorticity. Exam Results.

999 views • 59 slides

AOSS 401, Fall 2007 Lecture 15 October 17 , 2007

AOSS 401, Fall 2007 Lecture 15 October 17 , 2007. Richard B. Rood (Room 2525, SRB) rbrood@umich.edu 734-647-3530 Derek Posselt (Room 2517D, SRB) dposselt@umich.edu 734-936-0502. October 17 , 2007. Exam results Roadmap for the next month Introduction to vorticity. Exam Results.

596 views • 59 slides

UHM Course ATMO402 - Ch3 - Gradient Wind Approximation & Thermal Wind

Learn advanced concepts in dynamics include vorticity, cyclogenesis, jet streams, fronts, mesoscale circulations and so on.

408 views • 40 slides

Rip Currents-- Killer Currents Jim Lushine

Rip Currents-- Killer Currents Jim Lushine. Outline of Presentation. Rip Current Fatalities Data Forecasting Verification NWS Products Future Work. Rip Current Fatalities. Southeast Florida Rip Current Fatalities. Florida Rip Current Fatalities.

593 views • 38 slides

Meteorology and the Bronze C

726 views • 34 slides

Meteorology and the Bronze C

477 views • 34 slides

Work presented in collaboration with: Roger Smith, Jun Zhang and Mark Boothe

New insights from GRIP/HS3. HS3. Work presented in collaboration with: Roger Smith, Jun Zhang and Mark Boothe. Overarching NASA-HS3 Science Questions :. How do hurricanes form? What causes rapid intensity change? What is the role of deep convection in intensification?

365 views • 25 slides

Work presented in collaboration with: Roger Smith, Jun Zhang and Mark Boothe

New insights from GRIP/HS3. HS3. Work presented in collaboration with: Roger Smith, Jun Zhang and Mark Boothe. Overarching NASA-HS3 Science Questions :. How do hurricanes form? What causes rapid intensity change? What is the role of deep convection in intensification?

259 views • 25 slides

Chapter 3. Applications of the Basic Equations 3.1 Isobaric Coordinates

Chapter 3. Applications of the Basic Equations 3.1 Isobaric Coordinates. Horizontal Momentum Equation. Total Derivative. Geostrophic Relations. 3.1.2 Continuity Equation In Isobaric Coordinate System. 3.2 Balanced Flow. Several Types of Balanced Flow. n. ds. s(x,y,t). t. stream- lines.

248 views • 23 slides

Work presented in collaboration with: Roger Smith and Jun Zhang

New insights from GRIP/HS3. HS3. Work presented in collaboration with: Roger Smith and Jun Zhang. Overarching NASA-HS3 Science Questions :. How do hurricanes form? What causes rapid intensity change? What is the role of deep convection in intensification?

314 views • 20 slides

The General Circulation of the Atmosphere

306 views • 15 slides

Dynamics: Nov. 11

Dynamics: Nov. 11. Which are non-divergent, irrational ??. Circulation:. =. Circulations often conserved. Orthonormal to div, vort. Deformation:. Flow can be broken down into divergent, rotational, and deformation components. Flow over mountains. Both deformation And shear

236 views • 15 slides

ATOC 4720 class34

ATOC 4720 class34. 1. The horizontal equations of motion: smaller-scale motion 2. The vertical equation of motion 3. The thermal wind. Previous class: GEOSTROPHY:. Northern Hemisphere (NH):. y. L. H. CF. PGF. P1 P2 P3 P4 P5. x. Geostrophic wind value:.

138 views • 13 slides

WIND FIELDS OF TYPHOON SONGDA (2004) OBSERVED BY THE OKINAWA DOPPLER RADAR (COBRA)

970hPa. 08. 07. 945. Ogimi WPR site. 940. 06. 925hPa. 935. 05. 940. Nago COBRA radar site. 945. 04. 935. 03. 998hPa. 935. 02. 945. 980. 975. 01. 27. NICT Okinawa Center (Onna). 31. 29. 28. 30. Yonaguni Island. JST. Ishigaki Island.

158 views • 1 slides