PPT-Approach Observations of sea level and surface winds are analyzed to document observed

Analyses are performed of an oceanonly model driven by observed winds an idealized atmosphereonly model run with observed SSTs with a uniform tropical warming and an additional warming added to the tropical Indian Ocean and GOGA and TOGA runs. Objective. Reconcile the . conflicting evidence of the meridional westerly wind shift during the Last Glacial Maximum (LGM) indicated . by proxy-records from the . atmosphere . and . ocean. Approach. i. What causes wind? . Caused by a difference in air pressure due to. unequal heating of the atmosphere.. Winds are created by. ….. • . Heating the air, decreases pressure (warm. air rises creating a low pressure). Unit 5: Sixth Grade. http://www.youtube.com/watch?v=uBqohRu2RRk. https://games.ciconline.org/windward/content/sailing.html#record. Windward Online Sailing around the world game. Whooosh. !!!!!. When you open the valve on a bicycle tube, the air rushes out.. Ethan Campbell . . intern. Department of Geosciences. Princeton University. Princeton, NJ. Prof. Stephen Riser . mentor. School of Oceanography. University of Washington. Seattle, WA. The Antarctic Circumpolar Current (ACC) and Weddell Sea. Frederick Bingham. UNC Wilmington. Collaborators: Julius . Busecke. ,. Arnold Gordon and Claudia . Giulivi. (LDEO), . Zhijin. Li (JPL). Also thanks to J. . D’Addezio. !. Work funded by NASA. Journal of Geophysical Research Oceans doi:10.1002/2014JC009825. Air and Sea: Interdependency. Atmosphere and ocean are one . interconnected. system.. Change in atmosphere affects the ocean.. Change in ocean affects the . atmosphere. .. Unequal Solar Heating. Greatest amount of solar radiation is at the equator.. © U.S. Coast Guard . Auxiliary Association. No attempts to add, modify or delete information contained within this document shall be made. If errors are discovered, please contact the U.S. Coast Guard Auxiliary’s National Training . Objective. Reconcile the . conflicting evidence of the meridional westerly wind shift during the Last Glacial Maximum (LGM) indicated . by proxy-records from the . atmosphere . and . ocean. Approach. Compare & contrast an idealized hurricane life cycle with a real life example from the past. Understand how the angle of approach of a storm impacts regional damage. Objectives. Hurricane Structure. Category 5? typical gusts over open flat land of more than 280km/h. These winds correspond to the highest category on the Beaufort Scale. Extremely dangerous with widespread destruction. One of the Wind is the movement . of air caused by an uneven heating of the Earth’s . surface.. What HEATS EARTH’S SURFACE?. Heat from the sun heats the surface of the Earth.. This heat arrives to Earth in the form of radiation.. Local winds are caused by the movement of air between low-pressure and high-pressure systems within small areas. As there are so many different types of winds, each one takes on a unique form. Local winds frequently have a significant impact on climate in local regions, so it is critical to understand what causes them.. Lucrezia Ricciardulli, Thomas Meissner, Frank Wentz. Remote Sensing Systems, Santa Rosa, CA, USA. INTERNATIONAL WORKSHOP ON MEASURING. HIGH WIND SPEEDS OVER THE OCEAN. November 2016, UK MET OFFICE, Exeter, UK. April 19 and 20, 2018. Mark A. Bourassa. 1. Ernesto Rodriguez. 2. . and Sarah Gille. 3. Center for Ocean-Atmospheric Prediction Studies. and Department of Earth, Ocean and Atmospheric Science, Florida State University.