'Latent heating' diaporamas de présentation

Steve Guimond

Tropical Cyclone Inner-Core Dynamics : Part 1. A Latent Heat Retrieval and its Effects on Intensity and Structure Change Part 2. The Impacts of Effective Diffusion on the Axisymmetrization Process. Steve Guimond.

819 views • 69 slides

NOAA/ESRL/GSD/AMB

26 th Conference on Severe Local Storms 06 November 2012. Recent and Future Advancements in Convective-Scale Storm Prediction with the High -Resolution Rapid Refresh ( HRRR) Forecast System. NOAA/ESRL/GSD/AMB

737 views • 36 slides

Heating Profiles Associated with Deep Convection Estimated from TRMM and Future Satellites

Heating Profiles Associated with Deep Convection Estimated from TRMM and Future Satellites. Robert Houze University of Washington. Wei-Kuo Tao Goddard Space Flight Center. 19th Scientific Steering Group Session of the Global Energy and Water Cycle Experiment, January 23, 2007, Honolulu, HI.

378 views • 30 slides

Geostrophic Adjustment

Geostrophic Adjustment. Recall winds adjust to mass for scales larger than L R and mass adjust to wind for scales smaller than L R .

456 views • 30 slides

Stefan Klink, Klaus Stephan and Christoph Schraff stefan.klink@dwd.de

498 views • 30 slides

Methods for Introducing VHTs in Idealized Models: Retrieving Latent Heat

Methods for Introducing VHTs in Idealized Models: Retrieving Latent Heat. Steve Guimond Florida State University. Motivation. Previous theoretical work on TC intensification Many authors (i.e. Montgomery and Enagonio, 1998)

361 views • 28 slides

The general circulation of the atmosphere revisited

The general circulation of the atmosphere revisited. Kevin E. Trenberth NCAR Boulder, CO.

435 views • 26 slides

Hurricane Dynamics: Summer Research Highlights

Hurricane Dynamics: Summer Research Highlights. Steve Guimond Florida State University. Motivation. TC intensification is a complex, non-linear process governed by physics on a multitude of scales Synoptic scale Vortex scale Convective scale Hydrometeor scale

345 views • 26 slides

Intensification and weakening; Formation of eye and evolution of inner core

Intensification and weakening; Formation of eye and evolution of inner core. TC Intensification. Rapid Intensification Factors: High SST/OHC, Moist troposphere- esp. low and mid levels, Cold UL temps

435 views • 26 slides

Latent Heating Estimates from TRMM

370 views • 25 slides

Scott Curtis, PhD 15 October Associate Professor, East Carolina University Virtual Seminar

A Global Perspective on Flood and Landslide Hazards Through Recent Advances in Satellite-Based Research. Scott Curtis, PhD 15 October Associate Professor, East Carolina University Virtual Seminar Assistant Director, Center for Natural Hazards Research CDRE, Millersville University.

379 views • 21 slides

Electrified Simulations of Hurricane Rita (2005) with Comparisons to LASA Data

Electrified Simulations of Hurricane Rita (2005) with Comparisons to LASA Data. Steve Guimond 1,2 , Jon Reisner 2 , Chris Jeffery 2 and Xuan-Min Shao 2 1 Florida State University 2 Los Alamos National Laboratory. Motivation. Improve understanding and forecasting of TC intensification

284 views • 21 slides

Stefan Klink, Klaus Stephan and Christoph Schraff and Daniel Leuenberger

423 views • 20 slides

Spatio-temporal Distribution of Latent Heating in the Southeast Asian Monsoon Region

Spatio-temporal Distribution of Latent Heating in the Southeast Asian Monsoon Region. Manuel Zuluaga, Carlos Hoyos and Peter Webster. School of Earth and Atmospheric Sciences Georgia Institute of Technology Graduate Student Symposium November 2, 2007. Why study Latent Heating?.

283 views • 17 slides

Investigation of deep heating over the Gulf Stream and the linear response

Investigation of deep heating over the Gulf Stream and the linear response. Justin Small Shoshiro Minobe Shang-Ping Xie. Questions. What is the link between the Gulf Stream and deep heating in the atmosphere? and How does it affect the atmospheric, climatological, stationary wave pattern?.

348 views • 16 slides

HOT TOWERS AND HURRICANE INTENSIFICATION

HOT TOWERS AND HURRICANE INTENSIFICATION. Steve Guimond Florida State University. Motivation. TC intensification is a complex, non-linear process governed by physics on a multitude of scales Synoptic scale Vortex scale Convective scale Hydrometeor scale

262 views • 16 slides

210 views • 12 slides

Lightning Observations During NAME

Lightning Observations During NAME. Walt Petersen 1 * , Rich Blakeslee 2 * , Steve Goodman 2 , Phil Krider 3 , Steve Rutledge 4 , and Bob Maddox 3 1 UAH - NSSTC/ESSC; 2 NASA-MSFC/NSSTC; 3 UA; 4 CSU. *Contacts: walt.petersen@msfc.nasa.gov richard.blakeslee@msfc.nasa.gov.

253 views • 11 slides

An overview of the theory behind the Dionysos equations

226 views • 11 slides

William Olson, Mircea Grecu, Chung-Lin Shie JCET/UMBC and NASA/GSFC

168 views • 2 slides