PPT-Impacts of Shoaling Ocean Waves on Wind Stress and Drag Coefficient in Coastal Waters
Author : murphy | Published Date : 2023-10-30
Isaac Ginis University of Rhode Island Graduate School of Oceanography Coauthors Xuanyu Chen CSU Tetsu Hara URIGSO Workshop on PhysicsDynamics Coupling Princeton
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Impacts of Shoaling Ocean Waves on Wind Stress and Drag Coefficient in Coastal Waters: Transcript
Isaac Ginis University of Rhode Island Graduate School of Oceanography Coauthors Xuanyu Chen CSU Tetsu Hara URIGSO Workshop on PhysicsDynamics Coupling Princeton University June 2 2022 . . . . Waves. When directly generated and affected by local winds, a wind wave system is called a wind sea. After the wind ceases to blow, wind waves are called swells. More generally, a swell consists of wind generated waves that are not significantly affected by the local wind at that time. They have been created elsewhere or a long time ago. Wind waves on the ocean are called ocean waves. These wind waves can also have a negative effect, where on . RELATIONSHIP BETWEEN ROUGHNESS LENGTH, STATIC STABILITY, AND DRAG COEFFICIENT IN A DUNE ENVIRONMENT. Introduction to the subject. Drag (Wind) coefficient- quantifies the drag or resistance of an object in a fluid environment such as air or water. . :. Waves . *Refer to Chapter . 12 . in your Textbook . Learning Goals. : . I can label the anatomy of an ocean wave.. I can differentiate between the various types of waves.. Anatomy of a Wave. :. Crest. Section 3: Currents, Waves, and Tides. Earth Science. Mr. Margetan. . Ocean Currents. Surface Currents – Movement of water on the surface, primarily caused by winds. Ocean Currents. Longshore. Currents – Currents which run parallel to the shoreline due to energy released from waves. Coastal ocean. A short course on:. Modeling IO processes and phenomena . INCOIS. Hyderabad, India. November 16−27, 2015. References. 1) HIGNotes.pdf:. Section 5, pages 53−60.. McCreary, J.P., 1980: Modeling wind-driven ocean circulation. JIMAR 80-0029, HIG 80-3, Univ. of Hawaii, Honolulu, 64 pp. . The Motion of the Ocean…. Marine Science. Day 1: . Atmospheric Circulation . Objectives. :. What is physical oceanography?. What are the layers of the atmosphere?. Explain how the surface of the Earth is heated.. Waves. What You Will Learn. Identify the parts of a wave. . • Explain how the parts of a wave relate to wave movement. . • Describe how ocean waves form and move. . • Classify types of waves. . Ocean Currents. A . horizontal movement . of water in a well-defined pattern is called a . __________.. current. What are the two major categories of ocean currents?. Surface currents. What are the two major categories of ocean currents?. 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. 1Inter-Color Products from GOCI and MODISRuhul Amin1Richard Gould1Sherwin Ladner1 Igor Shulman1Jason Jolliff1Peter Sakalaukus1Adam Lawson1 Paul Martinolich2and Robert Arnone11Naval Research Laboratory eachersWaveThe repeating and periodic disturbance that travels through a medium eg water from one location to another locationWave CharacteristicsWave crestThe highest part of a waveWave troughThe low For much of human history, knowledge of the ocean and its currents was not recorded for many reasons - most sailors could not write and information was passed orally.. European nations began systematic ocean explorations but kept information secret between the 15. Energy is moving, not water. orbital motion. energy is transferred via circular motions. water (and gull) return to original position. the wave form moves forward. Motion decreases with depth. At. a depth of ½ of the wavelength, the motion is not significant.. Richard Kane . Monmouth University. April 1, 2021. Purpose:. Create accurate shoaling model using available wave modeling . Make shoaling tool available to public . Lay groundwork for more complicated water safety analysis .
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