PPT-U3D13&14 - Ocean Temperature Data & El Nino

U3D13 Bell Ringer 1214 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. s. Warm. . currents flow . away. from the . equator.. Cold. currents flow . toward. the . equator.. Ocean Currents. Sun. Wind. Coriolis. Effect. Gravity. Factors Influencing Currents. Energy from the Sun heats the water.. 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 ocean-atmosphere 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. 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. Currents. Ocean water contains streamlike movements of water called . ocean currents.. Currents can travel extremely far. In ancient times, currents were largely responsible for any human travel across the oceans. It is believed that currents carried the ancient Peruvians over 6,000 km across the south pacific to Polynesia. . By: Hope Stokes, Trey Judge, Aaron Bruney. Coriolis Effect . A mass moving in a rotating system experiences a force called the coriolis force acting perpendicular to the direction of motion and to the axis of rotation. It makes the water on the opposite side of the earth rotate in opposite directions. . Chris Hunt, Joe Salisbury, Doug . Vandemark. Special collaborators: William . Mook. and Meredith White (MSF), Dave Kuhn (VT), AJ Erskine (KCB), Kari Rapine (CAF), Michael . Congrove. (OSH). Northeast Aquaculture Conference and Exposition, Providence RI January 11-13 . 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. By: Hope Stokes, Trey Judge, Aaron Bruney. Coriolis Effect . A mass moving in a rotating system experiences a force called the coriolis force acting perpendicular to the direction of motion and to the axis of rotation. It makes the water on the opposite side of the earth rotate in opposite directions. . 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). 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. https://psl.noaa.gov/data/writ_new/. Presentation given May 2020. . Additional datasets, variables, and features have been added since.. Ocean Datasets. Reanalyses. Original horizontal resolution. Original Time range.