PPT-Assessing North Atlantic climate variability since the early 1800s through

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historical New England whaling ship logbooks and reanalyses Neele Sander 12 Caroline C Ummenhofer 2 Bastian Münch 3 Timothy D Walker 24 1 ChristianAlbrechtsUniversität

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Assessing North Atlantic climate variability since the early 1800s through: Transcript

historical New England whaling ship logbooks and reanalyses Neele Sander 12 Caroline C Ummenhofer 2 Bastian Münch 3 Timothy D Walker 24 1 ChristianAlbrechtsUniversität zu. Noel . Keenlyside. Geophysical Institute, University of . Bergen. Ingo . Bethke. , Francois . Counillon. , Tor . Eldevik. , Anne Britt . Sandø. , . Øystein. . Skagseth. , . Yongqi. . Gao. , Helene . 10 years of AMOC measurements from the RAPID program and a view to the future. Gerard McCarthy, Darren . Rayner. , Ivan . Haigh. , Joel . Hirschi. and David . Smeed. . National Oceanography Centre. May 16. th. , 2011. U.S. . EAST COAST WINTER STORM VARIABILITY DUE TO NAO AND OTHER LOW-FREQUENCY OSCILLATIONS. By Brandon Meitz. May 16. th. , 2011. L. Outline. What is winter storm variability?. What are ECWS?. System. Stuart A. . Cunningham. Scottish Association for Marine Science. Stuart.Cunningham@sams.ac.uk. . Barbara Berx. 1. , Eleanor Frajka-Williams. 2. and Mark Inall. 3. 1. Marine Laboratory Science, Aberdeen. 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. (. l. inking intra. -seasonal, inter-annual and longer time scales. Alessandra Giannini. , . Seyni. . Salack. , . Tiganadaba. . Lodoun. , . Abdou. . Ali. , . Amadou. . T Gaye and . Ousmane. . Ndiaye. Their . Teleconnection. Patterns. . 2010/ 11/ 16 . Speaker/ Pei-. Ning. Kirsten . Feng. Advisor/ Yu-. Heng. Tseng. Outline . Literature Review. Motivation . Objective. Data and Model. Preliminary work. Objectives. To better understand variability in eastern upwelling regions and the Gulf of Guinea. To enhance climate modelling and prediction capabilities. Improve understanding of marine ecosystems for better prediction and management. Bell Ringer:. Explain . the . meaning behind . this political cartoon in the early 1800s?. It is about Andrew Jackson.. . Veto, king, standing on constitution…. b/w 1815-1860 over 5 million immigrants came to USA. Oliver Elison Timm ATM 306 Fall 2016. Information. ATM 306 . ES 232. Schedule. Monday, Wednesday. 11:00am-12:20pm. Office hours:. Mon 12:30-1:30pm. Thu 9:15-10:15am. Or by appointment. Contact. oelisontimm@albany.edu. Professor Leila M. V. Carvalho. University of California, Santa Barbara. Seventh WMO International Workshop on Monsoons (IWM-7) ONLINE TRAINING WORKSHOP ON SUBSEASONAL TO SEASONAL (S2S) PREDICTION OF MONSOONS. Tony . Doré. , Christian Schiffer, . R. . Foulger. , Dieter Franke, Laurent Geoffroy, Laurent . Gernigon. , Bob . Holdsworth. , Ken McCaffrey, Alex Peace, . Kenni. Petersen, Randell Stephenson, Kim Welford (and others?). Peter Brandt, Marcus Dengler, Rebecca Hummels, Josefine . Herrford. Large Scale . Thermohaline. Circulation. 2. Kuhlbrodt et al. 2007. RACE . Contribution. . to. AMOC . Observing. System. Denmark Strait Overflow. cont. ). High/Positive phase: . the jet is shifted towards higher latitude, the polar vortex is intensified, and cold air is walled off in the polar vortex. . Low/Negative phase. , the vortex is weaker, the jet is shifted southward, and cold air outbreaks are more common.

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