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Books on the topic 'Global ocean biogeochemical model'

Author: Grafiati

Published: 3 June 2025

Last updated: 31 July 2025

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1

Center, Goddard Space Flight, ed. A coupled ocean general circulation, biogeochemical, and radiative model of the global oceans: Seasonal distributions of ocean chlorophyll and nutrients. National Aeronautics and Space Administration, Goddard Space Flight Center, 2000.

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2

Evans, Geoffrey T., and Michael J. R. Fasham, eds. Towards a Model of Ocean Biogeochemical Processes. Springer Berlin Heidelberg, 1993. http://dx.doi.org/10.1007/978-3-642-84602-1.

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3

1948-, Evans Geoffrey T., Fasham M. J. R, North Atlantic Treaty Organization. Scientific Affairs Division., and NATO Advanced Research Workshop Towards a Model of Ocean Biogeochemical Processes (1992 : Château de Bonas, France), eds. Towards a model of ocean biogeochemical processes. Springer-Verlag, 1993.

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4

Zhou, Tianjun, Yongqiang Yu, Yimin Liu, and Bin Wang, eds. Flexible Global Ocean-Atmosphere-Land System Model. Springer Berlin Heidelberg, 2014. http://dx.doi.org/10.1007/978-3-642-41801-3.

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5

Xu, Yongfu. A study of the biogeochemical cycle of CO2 in the ocean using a parcel model. University of East Anglia, 1990.

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6

Schiller, Andreas. A global ocean general circulation model for climate variability studies. CSIRO Marine Laboratories, 1997.

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7

Center, Goddard Space Flight, ed. A Global Ocean Tide model from TOPEX/POSEIDON altimetry: GOT99.2. National Aeronautics and Space Administration, Goddard Space Flight Center, 1999.

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8

Natural Environment Research Council. Marine Sciences Directorate., ed. Oceans and the global carbon cycle: An introduction to the Biogeochemical Ocean Flux Study of NERC Marine Sciences Directorate. Natural Environment Research Council, 1989.

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9

Tokmakian, Robin Telrud. The assimilation of satellite altimeter data into a global eddy resolving ocean model. Naval Postgraduate School, 1997.

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10

Gordon, Lawrence Joseph. Analysis of a simulation of the seasonal cycle in the tropical Pacific Ocean in an eddy-resolving global ocean model. Naval Postgraduate School, 1992.

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11

Rapp, Richard H. The development of a degree 360 expansion of the dynamic ocean topography of the POCM4̲B global circulation model. National Aeronautics and Space Administration, Goddard Space Flight Center, 1998.

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12

S, Border J., and Jet Propulsion Laboratory (U.S.), eds. Observation model and parameter partials for the JPL geodetic GPS modeling software "GPSOMC". National Aeronautics and Space Administration, Jet Propulsion Laboratory, California Institute of Technology, 1988.

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13

National Aeronautics and Space Administration (NASA) Staff. Coupled Ocean General Circulation, Biogeochemical, and Radiative Model of the Global Oceans: Seasonal Distributions of Ocean Chlorophyll and Nutrients. Independently Published, 2018.

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14

National Aeronautics and Space Administration (NASA) Staff. Technical Report Series on Global Modeling and Data Assimilation. Volume 22; a Coupled Ocean-Atmosphere Radiative Model for Global Ocean Biogeochemical Models. Independently Published, 2018.

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15

Development of ocean biogeochemical general circulation model. [University of Tokyo, Center for Climate System Research], 1996.

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16

Evans, Geoffrey T., and Michael J. R. Fasham. Towards a Model of Ocean Biogeochemical Processes. Springer London, Limited, 2011.

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17

Evans, Geoffrey T., and Michael J. R. Fasham. Towards a Model of Ocean Biogeochemical Processes. Springer London, Limited, 2013.

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18

Iap Global Ocean-Atmosphere-Land System Model. Science Pr, 2000.

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19

One-dimensional coupled ecosystem-carbon flux model for the simulation of biogeochemical parameters at Ocean Weather Station P. National Aeronautics and Space Administration, Goddard Space Flight Center, 2000.

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20

National Aeronautics and Space Administration (NASA) Staff. One-Dimensional Coupled Ecosystem-Carbon Flux Model for the Simulation of Biogeochemical Parameters at Ocean Weather Station P. Independently Published, 2018.

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21

The Assimilation of Satellite Altimeter Data into a Global Eddy Resolving Ocean Model. Storming Media, 1997.

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22

Validation Test Report for the 1/16 Degree Global NRL Layered Ocean Model Nowcast/Forecast System. Storming Media, 2003.

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23

Bin, Wang, Yimin Liu, Tianjun Zhou, and Yongqiang Yu. Flexible Global Ocean-Atmosphere-Land System Model: A Modeling Tool for the Climate Change Research Community. Springer London, Limited, 2013.

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24

Bin, Wang, Yimin Liu, Tianjun Zhou, and Yongqiang Yu. Flexible Global Ocean-Atmosphere-Land System Model: A Modeling Tool for the Climate Change Research Community. Springer, 2016.

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25

The Role Of The Ocean In Global Cycling Of Persistent Organic Contaminants Refinement And Application Of A Global Multicompartment Chemistrytransport Model. Springer, 2010.

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26

Stemmler, Irene. Role of the Ocean in Global Cycling of Persistent Organic Contaminants: Refinement and Application of a Global Multicompartment Chemistry-Transport Model. Springer, 2010.

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27

Spinrad, Richard W., Kendall L. Carder, and Mary Jane Perry, eds. Ocean Optics. Oxford University Press, 1994. http://dx.doi.org/10.1093/oso/9780195068436.001.0001.

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Since the publication of Jerlov's classic volume on optical oceanography in 1968, the ability to predict or model the submarine light field, given measurements of the inherent optical properties of the ocean, has improved to the point that model fields are very close to measured fields. In the last three decades, remote sensing capabilities have fostered powerful models that can be inverted to estimate the inherent optical properties closely related to substances important for understanding global biological productivity, environmental quality, and most nearshore geophysical processes. This vo

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28

Gupta, Sunil. The Archaeological Record of Indian Ocean Engagements. Oxford University Press, 2018. http://dx.doi.org/10.1093/oxfordhb/9780199935413.013.46.

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With the Bay of Bengal littoral as its focus, this chapter reviews the archaeological evidence for human expansions, migrations, formation of exchange networks, long-distance trade, political impulses, and transmissions of technocultural traditions in deep time, from around 5000 bc to 500 ad. In doing so, the author offers the idea of the Bay of Bengal Interaction Sphere, a “neutral” model of analysis that sets aside the constraints of the old Indianization debate for South-Southeast Asian interaction and situates the Bay within a broader global framework extending from the Mediterranean to th

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29

Krishnamurti, T. N., H. S. Bedi, and V. M. Hardiker. An Introduction to Global Spectral Modeling. Oxford University Press, 1998. http://dx.doi.org/10.1093/oso/9780195094732.001.0001.

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This book is an indispensable guide to the methods used by nearly all major weather forecast centers in the United States, England, Japan, India, France, and Australia. Designed for senior-level undergraduates and first-year graduate students, the book provides an introduction to global spectral modeling. It begins with an introduction to elementary finite-difference methods and moves on towards the gradual description of sophisticated dynamical and physical models in spherical coordinates. Topics include computational aspects of the spectral transform method, the planetary boundary layer phys

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30

Torres Padrón, María Esther, ed. XXI International Iberian Marine Chemistry (SIQUIMAR 2022). Libro de Abstracts. Universidad de Las Palmas de Gran Canaria. Servicio de Publicaciones y Difusión Científica, 2023. http://dx.doi.org/10.20420/1716.2023.580.

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The XXI International Iberian Seminar on Marine Chemistry (SIQUIMAR) bring marine chemical scientists of multidisciplinary research activities related with chemical oceanography, biogeochemical processes studies, tracers in the ocean, marine ecotoxicology and pollution and global changes related processes.

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31

Worm, Boris, and Derek P. Tittensor. A Theory of Global Biodiversity (MPB-60). Princeton University Press, 2018. http://dx.doi.org/10.23943/princeton/9780691154831.001.0001.

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The number of species found at a given point on the planet varies by orders of magnitude, yet large-scale gradients in biodiversity appear to follow some very general patterns. Little mechanistic theory has been formulated to explain the emergence of observed gradients of biodiversity both on land and in the oceans. Based on a comprehensive empirical synthesis of global patterns of species diversity and their drivers, this book develops and applies a new theory that can predict such patterns from few underlying processes. The book shows that global patterns of biodiversity fall into four consi

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32

Dunlop, Storm. 2. The circulation of the atmosphere. Oxford University Press, 2017. http://dx.doi.org/10.1093/actrade/9780199571314.003.0002.

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‘The circulation of the atmosphere’ outlines the general model of the movement of air around the Earth. There are three circulation cells either side of the equator: the Hadley cell (nearest to the equator) and the polar cell, driven by specific temperature and pressure gradients, and the Ferrel cell between them. It describes global pressure patterns and the Coriolis effect, which results in south-westerly trade winds in the northern hemisphere and north-westerly trade winds in the southern. Also described are the Intertropical Convergence Zone, the polar easterlies, the westerlies, and how a

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