Explicit representation of subgrid heterogeneity in a GCM land surface scheme
By Richard Essery, M. Best, R. Betts, P. Cox, C. Taylor. 2003
450 citations recorded by the source corpus.
Subfields: Civil and Structural Engineering, Global and Planetary Change, Oceanography
View Paper: https://www.semanticscholar.org/paper/4b50133d32e861d43a20df41c42d13a86a8e6845
How researchers see this paper
The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.
In Civil and Structural Engineering
In Global and Planetary Change
- P. Cox
- Paul R. Field
- Chris D. Jones
- C. Charlton-Perez
- Mei Zhao
- R. Wood
- Susan P. Ballard
- Peter A. Clark
In Oceanography
Citations in the corpus
- Convection‐permitting models: a step‐change in rainfall forecasting (2016, background): “…are also a key part of CPMs; in fact, the MetUM, since it is used as a climate model, already possesses a sophisticated surface and sub-surface scheme (Essery et al., 2003), but even this has been refined for mesoscale application, particularly in its treatment of urban surfaces (Porson et al.,…”
- Simulated glacial and interglacial vegetation across Africa: implications for species phylogenies and trans‐African migration of plants and animals (2007, background): “…Publishing Ltd, Global Change Biology, 14, 827–840 TRIFFID (Cox, 2001), the dynamic global vegetation component of the land surface scheme, MOSES-2 (Essery et al., 2003), simulates growth and replacement of vegetation of five functional types: broadleaf trees, needleleaf trees, C3 grasses, C4…”
- Carbon dioxide and climate impulse response functions for the computation of greenhouse gas metrics:a multi-model analysis (2012, unknown): “The terrestrial carbon cycle is represented by the MOSES2 land surface scheme (Essery et al., 2003) which simulates exchange of water, energy and carbon between the land surface and the atmosphere, and the TRIFFID dynamic global vegetation model (Cox, 2001) which simulates the coverage and competiti”
- The BRIDGE HadCM3 family of climate models: HadCM3@Bristol v1.0 (2017, unknown): “2 has major upgrades to all aspects of the land surface exchange and the surface radiation scheme Essery et al. (2003).”
- RAMI4PILPS: An intercomparison of formulations for the partitioning of solar radiation in land surface models (2011, methodology): “The Joint UK Land Environment Simulator (JULES) used here is the radiative transfer scheme of both the TRIFFID (Top‐down Representation of Interactive Foliage and Flora Including Dynamics) and JULES (Joint UK Land Environment Simulator) [Cox, 2001; Essery et al., 2003].”
- GSWP-2 Multimodel Analysis and Implications for Our Perception of the Land Surface (2006, background): “…NASA GSFC/HSB United States 30 m 3W 2T 1S Sg Vs Koster and Suarez (1992) MOSES2 Met Office United Kingdom 30 m 4W 4T 1S Sd Vd Cox et al. (1999); Essery et al. (2003) Noah NOAA/NCEP/ EMC United Sates 15 m 4W 4T 1S Sg Vd Ek et al. (2003) NSIPPCatchment NASA GSFC/ GMAO United States 20 m 3W 6T 3S…”
- The Distribution of Cloud Horizontal Sizes (2011, methodology): “The model includes parameterizations to represent the boundary layer (Lock et al. 2000) cloud cover and condensate (Smith 1990), mixed phase cloud microphysics (Wilson and Ballard 1999), land surface Essery et al. (2003), and convection (Gregory and Rowntree 1990).”