Page 1© Crown copyright 2007 Constraining the range of climate sensitivity through the diagnosis of cloud regimes Keith Williams 1 and George Tselioudis.
Institute for Biodiversity and Ecosystem Dynamics Universiteit van Amsterdam Research group Palaeoecology and Landscape ecology (P&L) Temperate – Palaeoecology:
Wilks 1992 - Adapting Atochastic Weather Generation Algorithms for Climate Change Studies
International Workshop on Advancement of Typhoon Track Forecast Technique (Nov. 30-Dec. 2, 2009) 1 / 21 Satoru YOKOI 1, Y. N. TAKAYABU 1,2, J. C. L. CHAN.
The other Harvard 3-D model: CACTUS Chemistry, Aerosols, Climate: Tropospheric Unified Simulation Objective: to improve understanding of the interaction.
(SGA / M&D / MPI-M) DEWEK 2008, Bremen 26.11.2008 Change of Wind Speed in Europe in Regional Climate Model Scenario Projections B. Hennemuth, H.-D. Hollweg,
Performance of high resolution global model over La Plata Basin Mario N. Nuñez CIMA-DCAO CONICET / UBA UMI IFAECI 2nd Meeting Buenos Aires, Argentina April.
A Regional Ice-Ocean Simulation Of the Barents and Kara Seas W. Paul Budgell Institute of Marine Research and Bjerknes Centre for Climate Research Bergen,
Synthesising Model Projections of Future Climate Change Mat Collins, Exeter Climate Systems, College of Engineering, Mathematics and Physical Sciences,
Title Meeting Name/Presenter Date. OVERARCHING GOAL To develop a useful downscaled regional climate dataset to enable a variety of sectors to assess the.
GLOBAL CHANGE AND AIR POLLUTION (GCAP):
Continental Drift Drifting Continents Continental drift is the idea that continents are moving very slowly, parallel to Earth’s surface. Alfred Wegener.