'Surface ocean' diaporamas de présentation

Radiocarbon Course Students:

Radiocarbon Course Students: These slides are provided for your reference. If you wish to use any of these slides, please make sure to contact the appropriate lecturer first for permission and attribution. Thank you. UCI AMS Short Course 2011 14 C in the Oceans. Outline

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Eco/Phyical Enviro

Eco/Phyical Enviro. Population. Major Ecosystems. Eco/Energy. Grab bag. 10. 10. 10. 10. 10. 20. 20. 20. 20. 20. 30. 30. 30. 30. 30. 40. 40. 40. 40. 40. 50. 50. 50. 50. 50. Ecosystem/Physical Enviro - 10.

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Ocean Surface Circulation

Ocean Surface Circulation. Motion in the Ocean, Part I, or Why does the ocean have currents, and why do they move in circles?. Jack Barth (barth@coas.oregonstate.edu). NASA web site: http://oceanmotion.org. Two types of Ocean Circulation:. Surface Circulation -- Wind-driven

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Ocean Movement

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Chapter 5 Surface Ocean/ Deep Ocean Circulation

Chapter 5 Surface Ocean/ Deep Ocean Circulation. Physiographic features of the world’s seafloor. Tharp and Heezen bathymetric map of the seafloor (1959). Seafloor Structure. Winds cause large gyres (circular patterns) in the surface ocean…. Simplified geometry. Ocean basin. 60.

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Climatology Review

Climatology Review. Question 1. Why do gyres form?. Question 2. Name three factors that controls the movement of surface currents. Question 3.

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IMDIS, LUCCA, Italy, 25.09.2013

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Ocean Surface Circulation

Ocean Surface Circulation. Motion in the Ocean, Part I, or Why does the ocean have currents, and why do they move in circles?. Two types of Ocean Circulation:. Surface Circulation -- Wind-driven Deep Circulation -- Density (T,S) driven. Atmospheric Circulation. Temperature and Pressure.

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23 April 2004 Tokyo, Japan

Carbon Theme Report and Implementation IGOS-P Side Event at GEO4 in Tokyo. Berrien Moore III Institute for the Study of Earth, Oceans, and Space University of New Hampshire. 23 April 2004 Tokyo, Japan. 370. 360. 350. 340. 330. 320. 310. 1957. 1963. 1969. 1975. 1981. 1987.

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Third Workshop on Air-Ice Chemical Interactions Columbia University, New York, June 6, 2011

Email: marcelo.guzman uky.edu. Third Workshop on Air-Ice Chemical Interactions Columbia University, New York, June 6, 2011. A Photochemical Mechanism of Model Organic Matter in Ice. Marcelo I. Guzman 1 and Michael Hoffmann 2

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Who Wants to Be a Millionaire?

Who Wants to Be a Millionaire?. Click the appropriate dollar amount at right to proceed to the question. _________________________ _____________________ _____________________ _____________________ ___________________ ___________________ __________________ _________________

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Eastern Pacific surface fluxes observed and simulated by coupled GCMs

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Determining the magnitude and variability of the anthropogenic CO 2 uptake rate by the oceans.

Determining the magnitude and variability of the anthropogenic CO 2 uptake rate by the oceans. Dick Feely (NOAA/PMEL/JISAO) Chris Sabine (NOAA/PMEL/JISAO) Rolf Sonnerup (JISAO/PMEL) Paul Quay (UW/JISAO). JISAO/PMEL/UW Collaboration. Observational Program (Feely, Sabine, Quay)

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Unit 10: Circulation of the World Ocean Surface ocean currents Geography of currents; gyres

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Water and Weather

Water and Weather. Chapter Seven: Oceans. 7.1 Introduction to Oceans 7.2 Waves 7.3 Shallow Marine Environments 7.4 The Ocean Floor. Investigation 7A. Global Winds and Ocean Currents. How do temperature and salinity cause ocean layering?. 7.1 Introduction to Oceans.

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Life on Europa?

This moon of Jupiter might have life in a subsurface ocean. Life on Europa?. For life to be present the three basic requirements are: 1) liquid water, 2) chemical building blocks, and 3) a source of energy. Europa is assumed to have all three.

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Dolphins

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Soil Respiration (Decomposition)

Volcanoes. Photosynthesis. Soil Respiration (Decomposition). 120. 0.1. Atmosphere. 750. 58. Deforestation and Land Use Change. Plant Respiration. Ocean Loss. Burning Fossil Fuels. 1.1. 59. Ocean Uptake. 90. 7.7. 92. Plants. 560. 725. Litterfall. 59. Rivers. Soils.

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