Palaeoclimates and their Modelling

With special reference to the Mesozoic era

Häftad, Engelska, 2013

AvJ.R.L. Allen,B.J. Hoskins,P.J. Valdes,B.W. Sellwood,R. Spicer

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This was a time during which the single continent Pangea disintegrated into continental units similar to those of today, a time when there were no significant polar ice caps and sea level was generally much higher than at the present time, and a time when dinosaurs apparently dominated terrestrial faunas and the flowering plants evolved.

Produktinformation

Utgivningsdatum2013-10-03
Mått210 x 297 x 9 mm
Vikt424 g
FormatHäftad
SpråkEngelska
Antal sidor140
FörlagSpringer
ISBN9789401045469

Tillhör följande kategorier

1 The climate system in the recent geological past.- 2 The use of climate response surfaces to reconstruct palaeoclimate from Quaternary pollen and plant macrofossil data.- 3 Sedimentary facies as indicators of Mesozoic palaeoclimate.- 4 Palaeowind: geological criteria for direction and strength.- 5 Fossils and fossil climate: the case for equable continental interiors in the Eocene.- 6 Water vapour, CO2 and insolation over the last glacial-interglacial cycles.- 7 A brief discussion of the history, strengths and limitations of conceptual climate models for pre-Quaternary time.- 8 Modelling of palaeoclimates: examples from the recent past.- 9 Cretaceous phytogeography and climate signals.- 10 Jurassic climates as inferred from the sedimentary and fossil record.- 11 Early Mesozoic phytogeography and climate.- 12 Model simulations of Cretaceous climates: the role of geography and carbon dioxide.- 13 Atmospheric general circulation models of the Jurassic.- 14 Simulation of Late Permian climate and biomes with an atmosphere-ocean model: comparisons with observations.- 15 The role of palaeoclimate studies: modelling.- 16 The role of palaeoclimate studies: geological indicators.