Climate-Ocean Interaction
Editat de M.E. Schlesingeren Limba Engleză Paperback – 26 sep 2011
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Specificații
ISBN-13: 9789401074407
ISBN-10: 9401074402
Pagini: 404
Ilustrații: XVI, 386 p.
Dimensiuni: 155 x 235 x 21 mm
Greutate: 0.56 kg
Ediția:Softcover reprint of the original 1st ed. 1990
Editura: SPRINGER NETHERLANDS
Colecția Springer
Locul publicării:Dordrecht, Netherlands
ISBN-10: 9401074402
Pagini: 404
Ilustrații: XVI, 386 p.
Dimensiuni: 155 x 235 x 21 mm
Greutate: 0.56 kg
Ediția:Softcover reprint of the original 1st ed. 1990
Editura: SPRINGER NETHERLANDS
Colecția Springer
Locul publicării:Dordrecht, Netherlands
Public țintă
ResearchCuprins
1: Introduction.- The Ocean as a Component of the Climate System.- 2: Observations of the Climate of the Ocean.- Observed Variations of Sea Surface Temperature.- Can Box Ocean Models Calibrated by Inverse Methods Provide a Means of Testing Ocean Circulation Models?.- 3: Modelling the Atmospheric, Oceanic and Sea Ice Components of the Climatic System.- General Circulation Modelling of the Atmosphere.- An Ocean Modelling System for Supercomputer Architectures of the 1990s.- Modelling Sea Ice for Climate Studies.- 4: Simulating the Variability of Climate on Short, Medium and Long Time Scales.- Interannual Variability in Coupled Tropical Atmosphere-Ocean Models.- Predictability of ENSO.- ENSO Modelling at MPI.- Specification and Variability of the Surface Forcing of the Ocean.- Ocean Models and the Inter—Basin Transport of Heat.- Extratropical Response to SST Anomalies and the Barotropic Model.- Modelling of Geochemical Tracers in the Ocean.- Diapycnal Mixing.- Climatic Change and Ocean Bottom Water Formation: Are We Missing Something?.- Reconstructions of Low and Middle Latitude Export Productivity, 30,000 Years BP to the Present: Implications for Global Carbon Reservoirs.- Global Estimation of Oceanic Eddy Transports from Satellite Altimetry?.- 5: Working Group Reports.- 1 Climate Observations.- 2 Modelling.- 3 ENSO Modelling and Prediction.- 4 Climate-Ocean Interaction on Time Scales of Decades to Centuries.- 5 Impact of Paleoclimatic Proxy Data on Climate Modelling.