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BIOME4

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<span class="search-highlight">BIOME4</span> (see text) experiments forced with temperature, precipitation, and i...
Published: 01 January 2011
Figure 2. BIOME4 (see text) experiments forced with temperature, precipitation, and insolation data from each Community Atmosphere Model–Community Land Model experiment. MODERN is calculated using baseline climatology provided for BIOME4. To facilitate comparison, predicted biomes are reduced
Journal Article
Journal: Geology
Published: 01 January 2011
Geology (2011) 39 (1): 3–6.
...Figure 2. BIOME4 (see text) experiments forced with temperature, precipitation, and insolation data from each Community Atmosphere Model–Community Land Model experiment. MODERN is calculated using baseline climatology provided for BIOME4. To facilitate comparison, predicted biomes are reduced...
FIGURES
Journal Article
Journal: Geology
Published: 01 September 2007
Geology (2007) 35 (9): 771–774.
... event in tropical Pangea. Although late Paleozoic plant types were distinct from their modern counterparts in similar environments ( Gastaldo et al., 1996 ), the floristic biogeography of the late Paleozoic paralleled that of the present ( Ziegler, 1990 ). Thus we contend that BIOME4 likely provides...
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Figure 1. Simulated ecological biomes for ICE-L (A), ICE-I (B), ICE-S (C), ...
Published: 01 September 2007
Figure 1. Simulated ecological biomes for ICE-L (A), ICE-I (B), ICE-S (C), LCO 2 (D), and HCO 2 (E) experiments. BIOME4 simulates 27 different ecological biomes; these biomes were condensed into nine mega-biomes according to Harrison and Prentice (2003) to simplify comparisons between
Journal Article
Journal: Geology
Published: 01 July 2014
Geology (2014) 42 (7): 627–630.
... control on Paleozoic continental-scale glaciation, while paleogeographic configurations and solar irradiance were of secondary importance. We use the GENESIS version 3.0 general circulation model (GCM) coupled to BIOME4, an equilibrium vegetation model, and a three-dimensional dynamic ice sheet model...
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Series: Geological Society, London, Special Publications
Published: 01 January 2010
DOI: 10.1144/SP342.16
EISBN: 9781862395909
... for interpreting ENSO-related signals. We also make use of the BIOME4 vegetation model ( Kaplan 2001 ). BIOME4 employs a detailed vegetation classification scheme by discriminating between 28 potential natural vegetation types. BIOME4 is used to translate the multivariate climate data from our GCM simulations...
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Series: Special Publications
Publisher: Society for Sedimentary Geology
Published: 01 January 2019
DOI: 10.2110/sepmsp.108.08
EISBN: 9781565763470
...–evaporation (SON: September, October, November). Gray shading indicates the underlying high-resolution topography. Fig. 7. —Biomes model results for the A) Albian and B) Aptian: (i) Biome4 CO 2 , (ii) full Köppen, and (iii) basic Köppen. Full Köppen codes: Dwa = cold, dry winter, and hot summer...
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Journal Article
Published: 14 February 2018
Geological Magazine (2019) 156 (2): 208–241.
.... The plate tectonic models will also require coupling with continental vegetation models such as BIOME4 (Kaplan et al. 2003 ) or marine models such as Darwin (Follows & Dutkiewicz, 2011 ; http://darwinproject.mit.edu ). Similarly, the plate tectonic models may constrain evolutionary models...
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