Subtropical Anticyclones and Summer Monsoons

By Mark J. W. Rodwell, B. Hoskins. 2001

718 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change

View Paper: https://www.semanticscholar.org/paper/6569487a629fd8a3ae7f145a7219dd997f105b92

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Citations in the corpus

Dynamics and chemistry of marine stratocumulus - DYCOMS II (2003, background): “sol (cf. Twomey 1974; Albrecht 1989; Brenguier et al. 2000b), or the large-scale environment ( Rodwell and Hoskins 2001 ), can still project significantly onto the overall radiative budget.”
Role of tropics in changing the response to Milankovich forcing some three million years ago (2003, background): “In the case of a shallow thermocline that allows winds to bring cold water to the surface, feedbacks between the ocean, atmosphere and land come into play [Hoskins, 1996; Rodwell and Hoskins, 2001].”
The role of increasing temperature variability in European summer heatwaves (2004, background): “The sequence of feedbacks involves substantial uncertainties due to large-scale anticyclonic forcin”
The importance of precessional signals in the tropical climate (2004, background): “The work of Rodwell and Hoskins (1996, 2001) demonstrated that the dryness of Mediterranean climate, and the strength of the north Pacific subtropical high could be related to the Asian monsoon heating.”
The formation mechanism of the Bonin high in August (2003, background): “Recently, Rodwell and Hoskins (1996, hereafter RH), Rodwell and Hoskins (2001) and Hoskins (1996) suggested a mechanism for the intensi cation of summer subtropical anticyclones.”
The Probability Distribution of Sea Surface Wind Speeds. Part I: Theory and SeaWinds Observations (2006, background): “In the Taylor and Yelland (2001) parameterization, the roughness length depends on the significant wave height and dominant wave period, both of which are taken to depend on local wind speed; these dependences are combined to yield the first term on the right-hand side of Eq.”
Seamless Poleward Atmospheric Energy Transports and Implications for the Hadley Circulation (2003, background): “The latter arise from the distribution of land and surface topography, in particular, and give rise to regional monsoons and subtropical anticyclones (Trenberth et al. 2000; Rodwell and Hoskins 2001; Chen et al. 2001).”