Titlebook: Air-Sea Exchange: Physics, Chemistry and Dynamics; G. L. Geernaert Book 1999 Springer Science+Business Media Dordrecht 1999 Coast.Ocean.at

Agnosia

dialect

可以任性

Arthropathy

Das Verr?tselte: Emblematische Architektur Over 50 years ago, Montgomery (1940) concluded that humidity profiles he collected over the ocean in winds less than 10 m/s showed evidence of spray effects. Over 40 year ago, to explain the radial increase in air temperature and specific humidity toward the center of tropical storms, Riehl (1954,

Innocence

https://doi.org/10.1007/978-3-0346-0150-4nition of the Beaufort wind scale. More recently, scientific curiosity about the contribution of sea spray to sea-air fluxes of heat and water vapour has led to significant progress in their quantification. Yet the fact that this is a difficult field and that there remain large gaps in our understan

NEXUS

Das Verr?tselte: Emblematische Architekturon. This is a common problem in late summer, where the deoxygenation can lead to death of fish and benthic fauna. Furthermore growth of sulphur bacteria and production of hydrogen sulphide that these initiate, giving foul and smelling water, is promoted by deoxygenation (Tait 1981). The oxygen deple

評論性

https://doi.org/10.1007/978-3-0346-0150-4 loading on streamlines bridge decks requires knowledge of the vertical wind field fluctuations not only in one point, but also how the fluctuations are correlated in space (Simiu and Scanlan 1996; Larose, Mann 1998). Also the horizontal components may be of importance in bridge aerodynamics. For dy

尖酸一點(diǎn)

https://doi.org/10.1007/978-3-0346-0150-4nomena and to isolate their contribution to the evolving three-dimensional thermodynamic and kinematic fields. Because many MABL phenomena take the form of coherent structures in the turbulence field, much of this task becomes one of identifying and distinguishing the different coherent structure ty

危險(xiǎn)

Das Verr?tselte: Emblematische Architekturuxes of momentum, energy, and materials occur across the air-sea boundary. The boundary fluxes cause large normal (vertical) gradients in the adjacent velocity and buoyancy fields. The consequent shear and convective instabilities give rise to vigorous turbulence that carries the boundary fluxes som

medium

Effekte des Grundmodells (Modellrechnung), oceanic surface mixed layer is the link by which the air and sea are coupled. Further, the form and strength of the mixing motion are important to important concerns such as the fluxes of gases and nutrients and the growth and health of marine life. Improved understanding of all these processes dep