PDF-DECADAL VARIATIONS IN CLIMATE ASSOCIATED WITH THE NORTH ATLANTIC OSCILLATION JAMES W
Author : liane-varnes | Published Date : 2014-12-21
HURRELL and HARRY VAN LOON National Center for Atmospheric Research Abstract Large changes in the wintertime atmospheric circulation have occurred over the past
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DECADAL VARIATIONS IN CLIMATE ASSOCIATED WITH THE NORTH ATLANTIC OSCILLATION JAMES W: Transcript
HURRELL and HARRY VAN LOON National Center for Atmospheric Research Abstract Large changes in the wintertime atmospheric circulation have occurred over the past two decades over the ocean basins of the Northern Hemisphere and these changes have had. Daniel Nielsen. Motivation/Goals. Existence of year-to-year variability in tornado count. Bias toward recent years due to increased storm spotting capabilities. Improvements in radar network and deployment of NEXRAD. 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?. Can decadal prediction anticipate events such as the warming hiatus?. Danny Barandiaran, Shih-Yu Wang. Utah State University. The “warming hiatus”. r. 2. < 0?. No slowdown in increase of ocean heat content. Past Climates. Past Climates. Climate History. Types of records. Climate reconstruction for Earth. Climate variables. Ocean/Atmosphere variations. ENSO, PDO, NAO, AMO, Thermohaline circulation. Interannual. -to-Decadal Predictions Experiments. . L. Goddard. , on behalf of the . US CLIVAR Decadal Predictability Working Group & Collaborators. : . Lisa Goddard, . Arun. Kumar, Amy Solomon, James Carton, Clara . 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. Daniel N. Baker. Laboratory for Atmospheric and Space Physics. CU-Boulder. e. GY. Declaration. . We have a shared responsibility to create and implement strategies to realize the full potential of digital information for present and future generations. In the 21. the capacity of seasonal-to-decadal predictions in the Arctic and over the Northern . Hemisphere. Daniela Matei (MPI) and Noel . Keenlyside. (. UiB. ). Motivation:. Observations . and ocean, atmosphere, and coupled modelling studies indicate a two-way link between the North Atlantic and Nordic Seas/Arctic that implies. SO 442 . – . Tropical Meteorology. Space and time-scales of dynamical atmospheric processes. SOURCE: UCAR. Climate. : PDO. Years. : ENSO. Seasons:. Monsoons. Months/Weeks:. MJO. Atmospheric Scales of Motion. Past and Present. Art McDonald. Queen’s University. And. SNOLAB. 1940’s to 1960’s:. Neutrino oscillations were proposed by . Pontecorvo. in 1957 motivated by initial reports of measurements by Davis with a Chlorine detector at a reactor. At that point, the transitions being considered were electron neutrino to electron anti-neutrino.. 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. and . Simultaneous . Estimation of . Forced . Oscillations and . Modes. John . Pierre, U of Wyoming. pierre@uwyo.edu. Dan . Trudnowski. , Montana Tech. dtrudnowski@mtech.edu. Jim Follum, PNNL (formerly at U of Wyoming).
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