'Ocean salinity' diaporamas de présentation

Ocean: Lessons 1 and 2

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Chapter 7: The Ocean General Circulation and Climate

Chapter 7: The Ocean General Circulation and Climate. This chapter discusses: Basic structures and dynamics Ekman transport Geostrophic currents Surface ocean circulation Subtropical gyre Boundary currents Deep ocean circulation Thermohaline conveyor belt

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SSS Science Team Meeting

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What is happening?

What is happening?. Bruce A. McCarl Distinguished Professor of Agricultural Economics Texas A&M University mccarl@tamu.edu http://agecon2.tamu.edu/people/faculty/mccarl-bruce/. Climate Change Adaptation. Energy. Climate Change Effects. Climate Change Mitigation. Basic Resources.

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COSEE-OS is one of 10 Centers and is thematic in nature Principal institutions are University of Maine, UNH & Bi

COSEE-OS is one of 10 Centers and is thematic in nature Principal institutions are University of Maine, UNH & Bigelow Laboratory for Ocean Sciences Long-term goal is to help the COSEE Network reach rural and inland audiences. GUIDING QUESTIONS

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Jean PLA CNES, Toulouse, France

MONITORING OF CLIMATE CHANGE AND MICROWAVE SATELLITE REMOTE SENSING _ Introduction _ Satellite altimetry _ Passive remote sensing _ Earth Exploration Satellite frequencies. Jean PLA CNES, Toulouse, France. INTRODUCTION.

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Jean PLA CNES, Toulouse, France

SPACEBORNE PASSIVE REMOTE SENSING MISSIONS: ? SOIL MOISTURE AND OCEAN SALINITY (SMOS) ? MEGHA TROPIQUE. Jean PLA CNES, Toulouse, France. Summary SMOS: SEA SALINITY AND SOIL MOISTURE, MEASUREMENT TECHNIQUES MEGHA TROPIQUE: DETECTION OF CYCLONES CLIMATE CHANGE AND PASSIVE REMOTE SENSING.

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Chapter 7 Ocean Chemistry

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OCEAN SALINITY

OCEAN SALINITY. OCEAN SALINITY. by Robert Perry. DISCLAIMER: The images, maps and diagrams in this presentation were taken from the public domain on the world wide web. Any privately owned images not available for this non- commercial, educational project will gladly be removed.

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Apollo 17 December 1972

Apollo 17 December 1972. Climate Science in the Space Age. Gary Lagerloef Oceanographer & Climate Scientist Earth & Space Research AZA , 16 September 2009 Portland, OR. NASA Earth Observatories. Atmosphere Temperature Tropical Storms Ozone Humidity Rainfall Cloud structure

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Ocean Water Chemistry

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The Restless Oceans

The Restless Oceans. 23.5. Explain how the properties of ocean water change with depth. Atmosphere & Ocean Circulation. Atmospheric Circulation Depends on density Ocean Surface Circulation Depends on the wind Deep Ocean Circulation Depends on density. Why is Ocean Circulation Important?.

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Gaia Hypothesis

Gaia Hypothesis. Created by James Lovelock in 1969 (but not published until 1979) "the biosphere - atmosphere, oceans, climate, Earth's crust and biota, living organisms, is regulated as a homeostatic system in conditions comfortable for the living organisms".

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