PPT-Tropical Pacific Ocean forcing of the

1998 99 decadal shift in global precipitation Lyon Barnston DeWitt Climate Dynamics revised MAM 2011 PRCP Anomaly MAM 19992011 AVG PRCP Anomaly East Africa MAM PRCP Anomaly. While written to incorporate computer technology the lesson can be easily adapted to paper and pen Lesson Objective Students will compose a series of slides based on the exhibits at OC The teacher may select one type of exhibit such as those that co and Feedback Processes. Earth. ’. s Climate System. What have we learned?. Earth is a planet. Planetary temperature is determined by . Brightness of our star. Earth-sun distance. Albedo of the planet. 1998. -. 99 . decadal shift in global precipitation. Lyon, . Barnston. , DeWitt, . Climate Dynamics . (revised). MAM 2011. PRCP Anomaly. MAM 1999-2011. AVG PRCP Anomaly. East Africa . MAM PRCP Anomaly. An. Overview . and Prospects for the Future. Michele Rienecker. Global Modeling and Assimilation Office. NASA/GSFC. With many . contributions borrowed . from the Ocean Data Assimilation . Community. Mass Systems. Andrew Makepeace. Penn State Erie, The . Behrend. College. Advisor Dr. Joe . Previte. Forced Spring Mass System. m. y’’ + b y’ + k y = F(t). m. – mass. b. – friction constant. Introduction to the physical climate system. Oliver . Elison. . Timm. . ATM 306 Fall 2016. Lecture 1. Atmospheric Circulation. Objectives. Objectives. The general circulation of the atmosphere. Winds and pressure systems. the Marine Boundary Layer. Henry Potter & Tripp Collins. Raphael Ramos, Neil Williams, Will . Drennan. , Hans Graber. Abstract. Materials & Methods. Results. Conclusions. Objectives. Future Work. Feedbacks. . “Our understanding of the climate system is complicated by . feedbacks. that either . amplify. or . damp. perturbations…”. Feedbacks. . Describe the inter-related growth or decay of the components of a system.. I. nfluencing . . the ITF in the 21. st. Century. Tony Lee. NASA Jet Propulsion Laboratory. California Institute of Technology. ITF: a great challenge to both observations and models. Figure after . :. Potential . Vorticity. :. = 0 for isentropic motions. Equivalent Potential . Vorticity. :. For a horizontally homogeneous atmosphere with vertical wind shear, vortex lines and Theta-E surfaces are initially horizontal (EPV=0). Since EPV is conserved, vortex lines remain on the original theta-E surfaces if they are subsequently tilted up or down…. . The concept of climate forcing, and some Basic understandings of Heat, Temperature, Feedbacks, and physics time scales . The Earth Climate System is Ultimately in Contact with Our Astronomical Surroundings. La gamme de thé MORPHEE vise toute générations recherchant le sommeil paisible tant désiré et non procuré par tout types de médicaments. Essentiellement composé de feuille de morphine, ce thé vous assurera d’un rétablissement digne d’un voyage sur . Analyses are performed of an ocean-only model driven by observed winds, an idealized atmosphere-only model run with observed SSTs with a uniform tropical warming and an additional warming added to the tropical Indian Ocean, and GOGA and TOGA runs. Andrey Proshutinsky. 1. , Eiji Watanabe. 2. , Elena Golubeva. 3. , Christophe Herbaut. 4. , Marie-Noelle Houssais. 4. , . Jiayan. Yang. 1. , Jinlun Zhang. 5. , . Yevgeny. Aksenov. 6. and Beverly de Cuevas.