A Global Climatology of Wind–Wave Interaction

By K. Hanley, S. Belcher, P. Sullivan. 2010

193 citations recorded by the source corpus.

Subfields: Atmospheric Science, Oceanography

View Paper: https://www.semanticscholar.org/paper/d5917ca630d00554e90d0678acdbfce0cb2e085c

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Citations in the corpus

Projection of Global Wave Climate Change toward the End of the Twenty-First Century (2012, methodology): “Compared to wave climate projections using dynamical models, statistical approaches are computationally less demanding andmay be used to sample a larger range of emission and climate model uncertainties but may encounter difficulties in reproducing the observed wave field in regions where wind and w”
The form and orientation of Langmuir cells for misaligned winds and waves (2012, background): “Swell waves, in particular, are susceptible to misalignment with the wind direction [Hanley et al., 2010].”
On the exchange of momentum over the open ocean (2013, unknown): “The third-order ﬁt also highlights the observation that the wage age goes to a ﬁnite positive value under very low wind conditions because of the ubiquitous nature of swell (Hanley et al. 2010) and the role of gustiness in maintaining momentum exchange under these conditions (Fairall et al. 1996).”
How do albatrosses fly around the world without flapping their wings (2011, background): “Thus, typical average wind speeds in the Southern Ocean are 6–11 m/s and typical average wave heights are 2–5 m (Young, 1999; Hanley et al., 2010).”
A global perspective on Langmuir turbulence in the ocean surface boundary layer (2012, unknown): “[2008] and Hanley et al. [2010] show that wind and waves are rarely in equilibrium.”
The physical oceanography of the transport of floating marine debris (2020, background): “However, waves are slower to build to strength and are more persistent than winds, and, once they have evolved into swell waves, they can travel long distances with low dissipation (Ardhuin et al 2009a, Hanley et al 2010,Webb and Fox-Kemper 2015).”
Wind Waves in the Coupled Climate System (2012, background): “On one hand, albeit 1653november 2012AmerICAn meTeoroLoGICAL SoCIeTY | limited, there is a transfer of momentum from waves to the atmosphere, leading to the so-called swell wind (e.g., Hanley et al. 2010).”