PPT-Detection of SST fronts from high-resolution model

hindcast results and its preliminary evaluation in the South China Sea Shihe Ren a Xueming Zhu a and Drevillon Marie b a National Marine Environmental Forcasting Center Beijing China. Impact . Objectives . Develop a regionalization framework to improve sampling of extreme events. Assess the simulations of stationary and non-stationary climate extremes in ultra high-resolution global climate model simulations. James Cummings Naval Research Laboratory. Monterey, CA 93943. 2013 Sea Surface Temperature Science Team Meeting. Seattle, Washington, USA. Global HYCOM . The role of model resolution and synoptic SST variability. Guidi Zhou, Mojib . Latif. , . Wonsun. . Park*, . Richard . Greatbatch. GEOMAR Helmholtz Centre for Ocean Research Kiel, Germany. *presenting. Craig Donlon and Kenneth S. Casey on behalf of the SST-VC members. ESA and NOAA. CEOS SIT-29 Meeting. C. NES, Toulouse, France. 9. th. -10. th. April 2014. GPM/GMI. SST-VC Status and Issues. Relatively healthy space segment but:. Chris Brierley & . Alexey. . Fedorov. Yale University. Outline. When was the Pliocene?. What did the Pliocene climate look like?. Why was the Pliocene climate like that?. Carbon dioxide increase. Evaluation: See worksheet. A - Cold Front B = Warm Front B1. Cool air mas - warm air mass moves in. A2. Warm air mass - cool air mass moves in. B3. Bri Meridional. Overturning Circulation . and the. Prediction . of North Atlantic . Sea Surface Temperature. Mojib. . Latif. , Helmholtz Centre for Ocean Research . and . Kiel . University. Klöwer. , M., et al. (. Global ENSO-TC Teleconnection . Ray . Bell . With thanks to. . Kevin Hodges, Pier Luigi Vidale, Jane Strachan and Malcolm Roberts. @. RayBell_Met. Introduction. Motivation. It . is important to evaluate the ability of GCMs to simulate . warm. path”. A. Czaja. , L. Sheldon, B. . Vanniere. & R. . Parfitt. Imperial College, London & Grantham Institute for Climate Change. All papers mentioned in the talk can be found at:. http://www.sp.ph.ic.ac.uk/~aczaja. One (biased) look at progress. Gary A. Wick. NOAA ESRL/PSD. October 29, 2013. Physical Basis – Priority Topics. Diurnal Variability. Spatial/Temporal Variability. Skin effect. Physical Basis – Priority Topics. Andrey . Vlasenko. , Armin Köhl, Detlef . Stammer. Institut für . Meerskunde. Universität Hamburg. Hamburg. TASK. Task 1.2.1 Identification of the atmospheric response to ocean surface state changes. Suzana J. Camargo,. Mingfang. Ting and . Yochanan. . Kushnir. LDEO, Columbia University. GloDecH. Meeting, OCP, LDEO, December 14, 2011.. Atlantic PDI . (power dissipation index ~. . V. 3. max. ) . Lisha. M. . Roubert. University of Wisconsin-Madison. Department of Atmospheric & Oceanic Sciences. Fronts: The Boundaries between Air Masses. A front is defined as the transition zone between two air masses of different density. . Adeetya's Kitchen & Furniture in Pune offers a selection of top-quality kitchen trolleys to maximize storage space and improve the functionality of any kitchen. https://adeetyas.com/high-quality-kitchen-trolleys-in-pune.php