'Tropical convection' presentation slideshows

Scale Interactions in Organized Tropical Convection

Scale Interactions in Organized Tropical Convection. George N. Kiladis Physical Sciences Division ESRL, NOAA. Why Study Tropical Convective Variability?. Tropical Convection acts as a primary “heat engine” for the atmospheric circulation

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The Asian-Australian Monsoon affect more than one half od the world population.

The Asian-Australian Monsoon affect more than one half od the world population. Monsoon prediction remains a major challenge for the scientific community for the 21 st centuary. Panel:

560 views • 42 slides

Signal to Noise Ratios for Global Modes of Subseasonal Atmospheric Variability

Signal to Noise Ratios for Global Modes of Subseasonal Atmospheric Variability . Edward Berry NOAA/NWS Dodge City, Kansas Klaus Weickmann NOAA/ESRL/PSD Boulder, Colorado . Climate Prediction Center November 16, 2007. Purpose .

551 views • 41 slides

Outline

Winter Storms by Paul Kocin Winter Storm Expert The Weather Channel and Dr. Gerry Bell Climate Prediction Center. Outline. Winter Weather Impacts Winter Forecast Issues Northeastern U.S. Snowfall Impact Scale Climate factors influencing winter storms. Winter Weather Impacts.

598 views • 41 slides

PCU3 Teletraining on LONG RANGE FORECASTING

PCU3 Teletraining on LONG RANGE FORECASTING. By Mike Halpert Climate Prediction Center. LRF Training Parts. Introduction (Audio VisitView presentation) Basis, Tools, Forecast Process (online tutorial) FORECAST CASE STUDY (this training)

528 views • 38 slides

ATM 521 Tropical Meteorology FALL 2009

ATM 521 Tropical Meteorology FALL 2009. ATM 521 Tropical Meteorology SPRING 2008. Instructor: Chris Thorncroft Room: ES226 Phone: 518 442 4555 E-mail: chris@atmos.albany.edu Aim of Course:

523 views • 37 slides

Primitive Equations

Primitive Equations. PRIMITIVE EQUATIONS. Definition. The so called primitive equations are those that govern the evolution of the large-scale motions. In other words, are the equations that describe the horizontal and vertical movement of the atmosphere and changes in temperature

879 views • 31 slides

High resolution models: Tropical Convection and Transport through the Tropical Tropopause Layer

High resolution models: Tropical Convection and Transport through the Tropical Tropopause Layer. Maria Russo, Scott Hosking, Peter Braesicke, John Pyle. TROPICS. ? (K). P (hPa). Height km. 17. 380. 90. Cold point Tropopause. 15. 360. 130. Q=0. TTL. 12. 350. 200.

377 views • 24 slides

Duane Waliser, JPL/Caltech Mitch Moncrieff, NCAR Co-chairs, Science Planning Group

Year of Tropical Convection Coordinating Observing, modeling and Forecasting to Addressing the Challenge of Organized Tropical Convection. Duane Waliser, JPL/Caltech Mitch Moncrieff, NCAR Co-chairs, Science Planning Group.

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Aerosol and chemical transport in tropical convection ACTIVE

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The Asian-Australian Monsoon affect more than one half od the world population.

The Asian-Australian Monsoon affect more than one half od the world population. Monsoon prediction remains a major challenge for the scientific community for the 21 st century. Panel: Co-Chair: Bin Wang and Harry Hendon

387 views • 21 slides

World Weather Research Programme (WWRP) Report Gilbert Brunet WWRP/JSC Chair

World Weather Research Programme (WWRP) Report Gilbert Brunet WWRP/JSC Chair. THORPEX 9th Session of ICSC, WMO, Geneva, 21-22 September 2011. Highlights of WWRP.

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Year of Tropical Convection (YOTC)

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Version: July 26, 2006

Version: July 26, 2006. Year of coordinated Observing, modeling and Forecasting: Addressing the Challenge of Organized Tropical Convection.

278 views • 14 slides

Liquid Water and Homogeneous Ice Nucleation in Tropical Convection

Liquid Water and Homogeneous Ice Nucleation in Tropical Convection. Importance. LWC=0.5 g/m 3 , 15 ? m diam. droplets ---- ?????? km -1 IWC=1 g/m 3 , 1 mm graupel, ?? 0.4 g/cm 3 ??????? m -1 _____________________________________________ Graupel collects cloud droplets ??????? m -1.

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An important constraint on tropical cloud-climate feedback

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TARGET 1 Improved scientific understanding, modelling and prediction of climate.

CL-01 Climate information for Adaptation Task Coordinator: Michel Rixen Task Liaison IB: Stephan Bojinski GEO Secretariat POC: EspenVolden. TARGET 1 Improved scientific understanding, modelling and prediction of climate.

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CFMIP/GCSS Boundary Layer WG Workshop on Evaluation and Understanding of Cloud Processes in GCMs

108 views • 3 slides