Scale dependence of bubble creation mechanisms in breaking waves

By G. Deane, M. Stokes. Nature, 2002

728 citations recorded by the source corpus.

View Paper: https://www.semanticscholar.org/paper/40b024b4c70667afac7ca0f1a6b40f2e048adc82

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Oceanography

In Pollution

Citations in the corpus

Ageing and burst of surface bubbles (2018, background): “While bubbles responsible for film drops are suspected to be less numerous than those responsible for jet drops at the surface of oceans (Deane & Stokes 2002), most sea surface droplets are nevertheless thought to originate from film drops (Lewis & Schwartz 2004; de Leeuw et al. 2011; Wang et al.…”
Air entrainment and bubble statistics in breaking waves (2016, positive): “Figure 1 shows the bubble size distribution from various laboratory studies, using diﬀerent measurement methods: cameras and bubble interface detection technique (Deane & Stokes 2002), ﬁber optical probes (Rojas & Loewen 2007; (2010), ( × ) L1996 for Loewen et al. (1996), ( (cid”
Void fraction measurements in breaking waves (2007, background): “…factor for all of these processes is the spectrum of bubble sizes, and numerous authors have attempted to make measurements of this distribution (including Medwin (1970), Johnson & Cooke (1979), Cartmill & Su (1993), Deane (1997), Farmer et al. (1998), Deane & Stokes (2002) and Leifer & Proc.”
A physically based framework for modeling the organic fractionation of sea spray aerosol from bubble film Langmuir equilibria (2014, background): “20–30 cm or more (Melville, 1996; Deane and Stokes, 2002), so if equilibrium is reached within less than 1 s, the exposure time will be sufficient to reach or nearly reach equilibrium for many ocean bubbles.”
Bubbly and Buoyant Particle–Laden Turbulent Flows (2020, neutral): “Data adapted from Aliseda and Lasheras (2011). importantly, deformable (Deane and Stokes 2002; Duineveld 1995).”
Inertial scaling of dissipation in unsteady breaking waves (2008, background): “Results from Loewen (1991) (see also Deane & Stokes 2002 ) showed that there was still significant energy in the hydrophone signal for frequencies above 5 kHz.”
Three-dimensional vortex structures under breaking waves (2005, background): “…breaks, it is acoustically active inside the wave crest owing to newly created bubbles – with those smaller than the Hinze scale (about 1 mm) subject to jet and drop entrainment, and larger bubbles fragmenting in the turbulent and sheared ﬂow during the wave cavity collapse (Deane & Stokes 2002).”
Dynamics of Winds and Currents Coupled to Surface Waves (2010, background): “Bubbles range in size from tens of micrometers to centimeters with void fractions up to 10% (Deane & Stokes 2002).”