'Potential intensity' diaporamas de présentation

First Law of Thermodynamics The internal energy dU changes when:

First Law of Thermodynamics The internal energy dU changes when: 1. heat dQ is exchanged between a parcel and its environment 2. work is done by a parcel on its environment (or vice-versa)

445 views • 38 slides

First Law of Thermodynamics The internal energy dU changes when:

First Law of Thermodynamics The internal energy dU changes when: 1. heat dQ is exchanged between a parcel and its environment 2. work is done by a parcel on its environment (or vice-versa)

459 views • 38 slides

(visiting BMRC/CAWCR, Melbourne, Australia, 8/07-7/08)

Some tests of our understanding of what controls tropical cyclone statistics Adam Sobel Columbia University New York, NY USA. (visiting BMRC/CAWCR, Melbourne, Australia, 8/07-7/08). 11/22/07. Collaborators. Suzana Camargo, Lamont-Doherty Earth Observatory, Columbia

444 views • 36 slides

Hurricanes in other climates: Thermodynamic genesis factors

471 views • 35 slides

Predictability of Tropical Cyclone Intensity Forecasting

Predictability of Tropical Cyclone Intensity Forecasting. Mark DeMaria NOAA/NESDIS/ StAR , Fort Collins, CO CoRP Science Symposium Fort Collins, CO August 2010. Outline. Overview of tropical cyclone intensity forecasting Charlie Neumann (1987) methodology

522 views • 34 slides

Genesis Potential Index and ENSO

Genesis Potential Index and ENSO. Suzana J. Camargo. Collaborators:. Kerry A. Emanuel Program in Atmospheres, Ocean and Climate Massachusetts Institute of Technology, Cambridge, MA Adam H. Sobel Department of Applied Physics and Applied Mathematics

425 views • 26 slides

Genesis Potential Index and ENSO

Genesis Potential Index and ENSO. Suzana J. Camargo. Collaborators:. Kerry A. Emanuel Program in Atmospheres, Ocean and Climate Massachusetts Institute of Technology, Cambridge, MA Adam H. Sobel Department of Applied Physics and Applied Mathematics

267 views • 26 slides

Annual- and zonal-mean climate of the tropics (NCEP)

Annual- and zonal-mean climate of the tropics (NCEP). Relative humidity [%]. Temperature [degC]. subtropical high. subtropical high. surface pressure [mb]. equatorial trough. Angular momentum conservation and zonal acceleration. When parcel moves poleward, r decreases

408 views • 24 slides

Increased Storm Intensity due to Climate Change:

TROPICAL STORMS AND HURRICANES . Increased Storm Intensity due to Climate Change:. Marques Miller Jordan Langworthy. What is climate change?. Substantial increase in global temperatures over a long period of time. Greenhouse effect. Ocean circulation. Climate Change Predictions.

388 views • 15 slides