PPT-Does El Niño Intensity Matter for California Precipitation

Andy Hoell Marty Hoerling Jon Eischeid Klaus Wolter Randy Dole Judith Perlwitz Taiyi Xu Linyin Cheng NOAAESRLPSD. El Nino conditions are characterized by above normal sea surface temperatures near the equator in the eastern and central portions of the equatorial Pacific Ocean While these conditions exist many thousands of miles away from Iowa impacts from El Ni Crystal K Williams. Department of Geography-Geology. Illinois State University. Outline. Introduction/Background. Mesoscale Convective Systems. Squall Lines. Precipitation. Conclusions. Introduction. Why is it so important to understand this climatic event?. How can . poplet. give you 4 levels of progress.. Changing Water currents?. What are the impacts of El Nino around the world?. "Most El . Ninos. The following presentation was used to review for the test.. 9. -17-15. topics. . .. Density. Salinity. Ocean currents. Conveyor Belt. El . N. ino. What to study . . .. Notebook entries. Lab: Density. Nino Events. Chip Konrad. Director of the NOAA Southeast Regional Climate Center. University of North Carolina at Chapel Hill. A. cknowledgement: Jordan McLeod, the new regional climatologist at SERCC. Dan Bikos, Edward Szoke, Steven Miller, Stanley Kidder, Christian Kummerow,. . Cindy Combs,. Scott Longmore. . *. Paula Brown. Cooperative Institute for Research in the Atmosphere (CIRA). *. Department of Atmospheric Science. Ocean_4_ENSO Lecture. Objectives/Agenda. Objective:. L. earn about El Nino and La Nina the two phases of the ENSO (El Nino Southern Oscillation) . cycle. Apply our understanding to your island. ENSO cycle. Michelle L’Heureux (. NOAA CPC). ENSO Forecast team (A. . Barnston. , E. Becker, G. Bell, T. Di . Liberto. , J. Gottschalk, M. . Halpert. , Z. Hu, N. Johnson, W. Wang, Y. . Xue. ), M. . Tippett. Niño-3.4 Forecasts from the NMME. A. n abnormal warming of surface ocean waters in the eastern tropical Pacific. A quasi-periodic climate pattern that occurs across the tropical Pacific Ocean roughly every five years. . average period length is 5 years. Walker circulation. ) that typically finds rising air and heavy rain over the western Pacific and sinking air and generally dry weather over the eastern Pacific. When the trades are exceptionally strong, water along the equator in the eastern Pacific becomes quite cool. This cool event is called La Nino . Pages 484-487. EL NINO. . Go to this website and read this background information first:. http://oceanservice.noaa.gov/facts/ninonina.html. You may need to come back to this website to fill in any notes that you missed. U3D13 – Bell Ringer – 12/14. Short Answer Practice: Cloud Formation. Fill in the blanks of the explanation using the word bank:. Cloud, condenses, dew point, rise, humidity, expand, condensation nuclei, pressure. Voxel-Based Morphometry. Ged . Ridgway, FIL/WTCN. With . thanks to John . Ashburner. Overview. Unified segmentation recap. Voxel-based morphometry (VBM). Spatial normalisation with . Dartel. Tissue segmentation. Precipitation mechanisms. Rainall. maps. Rainfall hyetographs. Nexrad. measurement of rainfall. Reading: Applied Hydrology Sections . 3.5 . to . 3.6 . on . Evaporation for Thursday. Precipitation. Precipitation: water falling from the atmosphere to the earth..