The General Circulation of the Atmosphere
By Tapio Schneider. Nature, 2006
225 citations recorded by the source corpus.
Subfields: Atmospheric Science, Global and Planetary Change
View Paper: https://www.semanticscholar.org/paper/0f928c94d8be378c9246e7609e73d47f61ac4cbc
How researchers see this paper
The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.
In Atmospheric Science
- Jian Lu
- S. Bordoni
- Tapio Schneider
- B. Galperin
- S. Sukoriansky
- N. Dikovskaya
- T. Reichler
- Gabriel Vecchi
In Global and Planetary Change
- Jian Lu
- Tapio Schneider
- S. Bordoni
- T. Reichler
- B. Galperin
- S. Sukoriansky
- N. Dikovskaya
- Gabriel Vecchi
Citations in the corpus
- Expansion of the Hadley Cell under Global Warming: Winter versus Summer (2012, unknown): “To distinguish the contrasting dynamical regimes between the winter and summer cells, Walker and Schneider (2006) where z is zonal-mean relative vorticity, f is planetary vorticity, u is the zonal-mean zonal wind, and V is the earth’s angular velocity.”
- Eddy Influences on Hadley Circulations: Simulations with an Idealized GCM (2006, unknown): “This latitude, in the small-angle approximation, scales as c ϳ ͑R⌬Ј ͒ 1ր4 ; ͑5͒ see Held (2000) and Schneider (2006).”
- Eddy-Mediated Regime Transitions in the Seasonal Cycle of a Hadley Circulation and Implications for Monsoon Dynamics (2008, methodology): “In all respects other than the radiative-heating formulation , the idealized GCM is the same as that described by Schneider and Walker (2006) and used by Walker and Schneider (2006).”
- Expansion of the Hadley cell under global warming (2007, background): “…GHG is complex, as the HC is influenced by many factors, involving tropical heating processes [e.g., Mitas and Clement, 2006], the atmospheric stability [e.g., Schneider, 1977], extra-tropical eddy dynamics [e.g., Walker and Schneider, 2006], and total atmospheric moisture [Frierson et al., 2006].”
- On the arrest of inverse energy cascade and the rhines scale (2006, background): “In the context of large-scale atmospheric flows, the interaction between turbulence and waves yields dynamically rich macroturbulence (Held 1999; Schneider 2006), the notion that underlies diverse phenomena ranging from a local weather to a global climate.”