PPT-Climate variability and change

Author : sherrill-nordquist | Published Date : 2017-05-17

Introduction to the physical climate system Oliver Elison Timm ATM 306 Fall 2016 Lecture 1 Atmospheric Circulation Objectives Objectives The general circulation

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Climate variability and change: Transcript


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. Earth System Sensitivities. Peter Cox. Professor of Climate System Dynamics. University of Exeter. How can we constrain . long-term Earth System Projections . using short-term Observations ?. Climate Sensitivity to Doubling CO. Reasons for recapping progress:. - Present advances in scientific understanding of the climate system. Demonstrate the return on investment of agency funding and interagency coordination of US CLIVAR research. Yu-Fen Huang. Hendricks E. A., B. d. . Mcnoldy. , and Wayne H. Schubert. Introduction. TC intensity change is caused by environmental, oceanic, and internal dynamical factors. (Wang and Wu 2004). . An important internal process is the dynamic instability. . using the WRF-Chem regional model . Anne Boynard, Gabriele Pfister, David Edwards. National Center for Atmospheric Research (NCAR), Boulder, Colorado, USA. NAQC – 9 March 2011. Motivation. Tropospheric CO is a . 3. /. HO. x. ) Abundances. Glacial-Interglacial. Rapid Climate Change. Glacial.  .  . Model-based hypothesis: During large climate transitions, variability in the O. 3. /. HO. x. ratio is determined by . Solubles. Breitling, B.J. and K.J. Herrick . POET LLC, Sioux Falls SD. ABSTRACT. METHODS. Distillers grains with . solubles. (. DDGS. ) is an ingredient that is commonly included in livestock ration formulations. Several reasons for the widespread use of DDGS include a favorable nutrient profile, competitive cost, and availability. However, as with all co-products, one reason for exclusion from ration formulation is a concern regarding variability. It was our objective to address this concern by characterizing the quality of DDGS across 27 ethanol . PM. 2.5. . air quality inferred from a multi-model analysis of meteorological modes. Loretta J. Mickley. Co-Is:. Amos P.K.A. Tai. . and Daniel J. Jacob. School of Engineering and Applied Sciences. Harvard University. Bureau . of Meteorology – R&D Branch. Regional characteristics of tropical expansion and the role of climate variability. Observations vs Models. Observed rate in many metrics is 0.5 – 1.0 degrees/decade of expansion. (AOSS 480 // NRE 480) . Richard B. Rood. Cell: 301-526-8572. 2525 Space Research Building (North Campus). rbrood@umich.edu. http://. aoss.engin.umich.edu. /people/rbrood. Winter 2015. February . 10, . Kuroshio. Extension . System . B. Qiu. 1. , S. Chen. 1. , N. Schneider. 1. and B. Taguchi. 2. 1. Dept of Oceanography, University of Hawaii, USA. 2. Earth Simulator Center, JAMSTEC, Japan. Climate Implications of Frontal Scale Air-Sea Interaction Workshop, Boulder, 5-7 August . Rebecca . Saari. Assistant Professor. Civil & Environmental Engineering. Y.F. Mei, E. . Monier. , F. Garcia-Menendez. CMAS Conference. Chapel Hill, NC, October 23, 2016. 2. Connecting Policies to Air Quality Impacts. Climate Matters in the Newsroom Josh Murphy Center for Climate Change Communication (4C) George Mason University Overview Our Mission (4C) “ We develop and apply social science insights to help society make informed decisions that will stabilize the Earth’s life-sustaining climate, and prevent further harm from climate change.” 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. Productivity. Justin . Sheffield. 1. , . Julio E. Herrera-. Estrada. 2. , . Kelly . Caylor. 1. , . Eric F. . Wood. 1. 1. Dept. Civil and Environmental Engineering, Princeton University, Princeton, NJ.

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