PPT-El Niño-Southern Oscillation

Allie Marquardt Outline Overview of El Niño A Change in the Atmosphere Resulting Changes in the Ocean Sea Surface Temperature Thermocline Rossby Waves and Dissipation What is El Niño El Niño is characterized by warm sea surface temperatures SST in the Pacific Ocean around the equator but is associated with a large scale change in the oceanatmosphere system. NORMAL. :. - Easterly trade winds between ± 30° latitude (Coriolis Force). - Sea Surface Height slant to west. - Warm basin in W. Pacific. - Cool surface in E. (upwelling H. FY14 Review. Jon Gottschalck. Acting Chief, Operational Prediction Branch. NOAA / NWS / Climate Prediction Center. NCEP Production Suite Review. College Park, MD. December 2-3, 2014. Outline. Major climate modes overview, forecast review. Overview. The Slab Ocean El Nino. How good are the CMIP models?. Non-linearity. Seasonality (spring barrier). CP vs. EP. Teleconnections delayed feedback. Climate Change. Overview. The Slab Ocean El Nino. 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. Pam Knox. UGA Agricultural Climatologist. 2016-17 Winter anomalies. http://www.hprcc.unl.edu/maps.php?map=ACISClimateMaps. Rome: 2016 temperature. http://mrcc.isws.illinois.edu/CLIMATE. /. (sign up for free account and pick Monthly/Thermograph). 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 . 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. 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. 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.. pulser. ). B. Quinn. Feb. 23, 2018. 1. Cabling scheme for . HCal. One signal, one HV cable to each tube. (Plus one HV & 6 signal/section for . pulser. ). Cables secured, strain-relieved on gantry behind . Bedo tye nino ducu i ot kwan pire tek 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).