PPT-Reduction of Temporal Discretization Error in an Atmospheric General Circulation Model

Author Daisuke Hotta hottaumdedu Advisor Prof Eugenia Kalnay Dept of Atmospheric and Oceanic Science University of Maryland College Park ekalnayatmosumdedu Numerical Weather Prediction NWP. Lu J, L Sun, Y Wu, and G Chen. 2014. “The Role of Subtropical Irreversible PV Mixing in the Zonal Mean Circulation Response to Global Warming-Like Thermal Forcing.” . Journal of Climate, . early online. DOI:10.1175/JCLI-D-13-00372.1.. Dr. John Krasting. NOAA/GFDL – Princeton, NJ. John.Krasting@noaa.gov. Rutgers Physical Climatology. October 18, 2012. Why is there circulation to begin with?. The Earth has to maintain its radiative balance!. Part II: Effect of Earth. ’. s rotation. Reference: . Rotunno. (1983, . J. Atmos. Sci.. ). Rotunno (1983). Quasi-2D analytic linear model. Heating function specified over land. Becomes cooling function after sunset. 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. Marvin L. Adams. Texas A&M University. CRASH Annual Review. Ann Arbor, MI. October 28-29, 2010. The integrated team has produced significant results this year.. Collaboration has been fruitful and essential.. and Climate (Chap 6). Atmospheric General Circulation. Also: Global or planetary circulation. . The general circulation (GC) of the atmosphere is the totality of motions that characterize the . large scale. Hydrodynamics. Fall 2011 Review. PDT and radiation transport. Marvin L. Adams. We continue to develop and PDT . and apply it to CRASH problems.. Assessing diffusion model error is a CRASH priority.. Eric Myra will discuss . Daisuke . Hotta. hotta@umd.edu. Advisor: Prof. Eugenia . Kalnay. Dept. of Atmospheric and Oceanic Science, . University of Maryland, College Park. ekalnay@atmos.umd.edu. Numerical Weather Prediction (NWP):. AOS 101 Weather and Climate. Lisha. M. . Roubert. University of Wisconsin-Madison. Department of Atmospheric & Oceanic Sciences. Today’s Lab. Today we will be using the tank lab to simulate the general circulation of the atmosphere. .  . Ismail B. Celik. Mechanical and Aerospace Engineering Department. West Virginia University (. WVU. ), Morgantown WV 26506. ibcelik@mail.wvu.edu. Contributors:. . Zhiyuan . Ma* Sofiane Benyahia**, . do they . make . r. ain . and . how . can we . more accurately simulate that?. Dr. Andrew Martin, anmarti2@pdx.edu. Research Assistant . Professor. Department of Geography, Portland State University. Andrew Cross. Jay Gambetta. Supported by ARO W911NF-14-1-0124. Simulating and Correcting . Qubit. Leakage. 2. What is . Qubit. Leakage?. Physical . qubits. are not ideal two-level systems and may leak out of the computational space. Case . of Santa Olalla pond (SW . Spain. ). . Serrano-Hidalgo, C., Heredia-Díaz J. ., Guardiola-Albert C. . and . Elorza-Tenreiro. F.J.. METODOLOGY. T. o identify the adequate numerical representation of the lagoon using a finer spatial discretization.. E. vidence is presented (typical of recent versions of the AGCM) that the T2m warm bias over Asia and North Americ. a. in AGCMs is in part dynamically driven from above (linked to zonal mean wind bias) and amplified at the surface via possible land model issues.