Shifting the diurnal cycle of parameterized deep convection over land
By C. Rio, Frederic Hourdin, J. Grandpeix, J. Lafore. 2009
173 citations recorded by the source corpus.
Subfields: Atmospheric Science, Global and Planetary Change
View Paper: https://www.semanticscholar.org/paper/d53329179f4adb47fbf6cd0291218fba88511ab4
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In Atmospheric Science
- A. D. Del Genio
- Jingbo Wu
- Sandrine Bony
- Anton Beljaars
- J. Dufresne
- J. Vial
- J. Grandpeix
- Frederic Hourdin
In Global and Planetary Change
Citations in the corpus
- LMDZ5B: the atmospheric component of the IPSL climate model with revisited parameterizations for clouds and convection (2013, background): “The singlecolumn result of Rio et al (2009) are confirmed in 3D as illustrated in Fig.”
- Tropospheric water vapor, convection, and climate (2010, background): “This is likely due to deficiencies in the convective parameterization schemes, although “superparameterization”‐based models where convection is explicitly calculated also show problems [Zhang et al., 2008], while improvement is evident in some recent parameterizations [Rio et al., 2009].”
- Influence of the subcloud layer on the development of a deep convective ensemble (2012, background): “Rio et al. (2009) show how a parameterization of the dynamic effects of the wake can contribute to a more realistic timing of parameterized deep convection.”
- The Role of Entrainment in the Diurnal Cycle of Continental Convection (2010, methodology): “Rio et al. (2009) use a different approach, employing separate shallow and deep convection schemes in a single-column model to produce a realistic mid-”
- Representing Equilibrium and Nonequilibrium Convection in Large-Scale Models (2014, background): “It has been shown that CRMs with resolutions of order 2.5 km or higher are able to reproduce the observed diurnal cycle (e.g., Petch et al. 2002; Sato et al. 2008; Stirling and Stratton 2012), but a strong resolution sensitivity exists with respect to both amplitude and phase for coarser horizontal…”
- Presentation and Evaluation of the IPSL‐CM6A‐LR Climate Model (2020, methodology): “The “episodic mixing and buoyancy sorting” scheme originally developed by Emanuel (1991) used for deep convection wasmodified to make the closure and triggering rely on the description of the subcloud vertical motions by thermal plumes and wakes (Rio et al., 2009).”