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Marine geochemistry: ocean circulation, carbon cycle and climate change
Marine geochemistry uses chemical elements and their isotopes to study how the ocean works. It brings quantitative answers to questions such as: What is the deep ocean mixing rate? How much atmospheric CO2 is pumped by the ocean? How fast are pollutants removed from the ocean? How do ecosystems reac...
Autores principales: | , |
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Lenguaje: | eng |
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Oxford University Press
2016
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Acceso en línea: | https://dx.doi.org/10.1093/acprof:oso/9780198787495.001.0001 http://cds.cern.ch/record/2241037 |
Sumario: | Marine geochemistry uses chemical elements and their isotopes to study how the ocean works. It brings quantitative answers to questions such as: What is the deep ocean mixing rate? How much atmospheric CO2 is pumped by the ocean? How fast are pollutants removed from the ocean? How do ecosystems react to the anthropogenic pressure? The book provides a simple introduction to the concepts (environmental chemistry, isotopes), the methods (field approach, remote sensing, modeling) and the applications (ocean circulation, carbon cycle, climate change) of marine geochemistry with a particular emphasis on isotopic tracers. Marine geochemistry is not an isolated discipline: numerous openings on physical oceanography, marine biology, climatology, geology, pollutions and ecology are proposed and provide a global vision of the ocean. It includes new topics based on ongoing research programs such as GEOTRACES, Global Carbon Project, Tara Ocean. It provides a complete outline for a course in marine geochemistry. To favor a hands-on approach, application exercises are worked out throughout the book and each chapter concludes with a set of problems based on the recent scientific literature (with solutions given at the end of the book). |
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