Titlebook: Oceanic Whitecaps; And Their Role in Ai Edward C. Monahan,Gearóid Mac Niocaill Book 1986 Springer Science+Business Media Dordrecht 1986 Clo

察覺

Bubble Populations: Background and Breaking Waves population comes from the decay of the bubble patches, from secondary sources such as biological activity, droplet impact, and sediment outgassing, and from stable microbubbles..Aradio-controlled bubble camera is described, as is its use in following the decay of a laboratory bubble injection event

ORBIT

On Reconciling Optical and Acoustical Bubble Spectra in the Mixed Layer 30 μm (8μm in tap water);numbers fall off slowly with depth. Optically determined estimates, in contrast, show a strong peak above 80 μm; numbers fall off rapidly with depth. Existing theory is insufficiently developed to exclude either of these interpretations. Re-examination of the acoustical and

Hyaluronic-Acid

The Contribution of Bubbles to Gas Transfer Across an Air-Water Interfaceover-pressure leads to water supersaturation at equilibrium, this supersaturation being more significant for less soluble gases. Although the transfer velocity remains roughly constant for a variable concentration far from equilib rium, its range of variation becomes infinite near equilibrium. Atten

CLOUT

Oceanic Air Bubbles as Generators of Marine Aerosols liquid marine aerosols at the sea-surface. Relevant parameters are: bubble size, concentration, injection depth and age. The transfer function giving the liquid droplet production rate in relation to the bubble parameters is of prime interest for any physical modelling..In order to estimate the oce

疏忽

柔軟

instate

A Model of Marine Aerosol Generation Via Whitecaps and Wave Disruptionboundary layer, attempted to define, in terms of aerosol droplet radius (r) and 10m-elevation wind speed (U), a model of open-ocean sea-surface aerosol generation. This source function is represented by the expression dF(r, U)/dr, which states the rate of production of marine aerosol droplets, per u