'Large scale circulation' diaporamas de présentation

Statistical Projection of Global Climate Change Scenarios onto Hawaiian Rainfall

Statistical Projection of Global Climate Change Scenarios onto Hawaiian Rainfall. Oliver Timm, International Pacific Research Center, SOEST, University of Hawai'i at Manoa Henry Diaz, NOAA/ESRL/CIRES, Boulder, Colorado. Climate Change in the News.

648 views • 37 slides

Tropical Cyclones and Climate Change in a High Resolution General Circulation Model, HiGEM

Tropical Cyclones and Climate Change in a High Resolution General Circulation Model, HiGEM. Ray Bell Supervisors: Prof. Pier Luigi Vidale, Dr. Kevin Hodges and Dr. Jane Strachan. Introduction. Motivation Socio-economic impacts and changing risk with climate change.

424 views • 33 slides

A new Convection Parameterization: Some Achievements and Some Challenges

A new Convection Parameterization: Some Achievements and Some Challenges. Hans-F Graf, Cambridge Till M Wagner, Oxford (was Cambridge ). IPAM, UCLA, May 2010. Convective clouds Radiation Layered clouds Turbulence. Some motivation:. - Clouds are beautiful.

477 views • 33 slides

Ocean transports of heat and freshwater: How good are our estimates? Has WOCE changed the values and uncertainties?

434 views • 31 slides

NCAS Seasonal Climate Discussion, 2 April 2012

420 views • 31 slides

What happens when Ra grows large: Turbulent convection Statistical approach

What happens when Ra grows large: Turbulent convection Statistical approach Dynamics of individual (coherent) plumes. Turbulent convection ( s =0.71, a =2 p , Ra=10 7 ). Turbulent convection ( s =0.71, a =2 p , Ra=10 7 ). Turbulent convection ( s =0.71, a =2 p , Ra=10 7 ).

464 views • 31 slides

Learning from the crisis: Is there a model for global banking?

Learning from the crisis: Is there a model for global banking? . C.P. Chandrasekhar. Introduction. Crisis not restricted to the mortgage periphery of the financial system or to Wall Street. Afflicts Banking as well. Two contradictory reasons why this was not expected:

354 views • 24 slides

June 16th, 2009

274 views • 15 slides

Building a Portuguese Coastal Operational Modelling System

218 views • 11 slides

5.3 What control occurrence, intensity, type and life-time of the convective systems?

5.3 What control occurrence, intensity, type and life-time of the convective systems?. Central questions What control the occurrence of convection? What control convective type (intensity, lift time, dynamic structure)?. What control occurrence of convection?. Question:

196 views • 8 slides

Climate and the Hydrological Cycle (MO408M)

Climate and the Hydrological Cycle (MO408M). Bart van den Hurk ( www.knmi.nl/~hurkvd ) IMAU (Wednesday): B614 KNMI (other days): B3.36 hurkvd@knmi.nl Aarnout van Delden (IMAU) Geert Jan Roelofs (IMAU). Material. Lecture notes Land processes in climate models Presentations Articles

193 views • 8 slides

Experiment Design:

Mesoscale Variability on The Eastern Brazilian Shelf through a Roms Nested Model L. F. Rezende a, b ; P. Silva a ; A. Peliz a ; J. Dubert a & M. Cirano c

125 views • 1 slides

? CAM simulation underestimates the dry and wet events over central US.

66 views • 1 slides