《预订 The Near-Surface Layer of the Ocean: Structure, [ISBN:9789400776203]》,作者:预订 The Near-Surface Layer of the Ocean: Structure, [ISBN:9789400776203]Soloviev 著,出版社:Springer,ISBN:9789400776203。
Small-scale turbulence parameters in the layer below a wind-blown surface of the oc ocean can be measured by means of a tethered free-rising profiler. Spectral analysis of the velocity pulsations, measured in the Atlantic Ocean, shows the presence of a frequency band corresponding to the spectru...
The ocean near-surface layers, such as the mixed and mixing layers, the entrainment layer, and the log layer, contain the oceans' most energetic turbulence and are critical to understanding and prediction of the oceans and the earth system. This chapter covers the foundational dynamical insights ...
Here, we compare measured biological oxidation rates of methane with the diffusional fluxes computed from concentration gradients in the surface layer of the ocean and show that oxidation of methane in sea water is a mechanism which modulates the flux of methane from marine waters to the atmosphere...
The generation and destruction of stratification in the surface mixed layer of the ocean is understood to result from vertical turbulent transport of buoyancy and momentum driven by air–sea fluxes and stresses. In this paper, it is shown that the magnitude and penetration of vertical fluxes are ...
Elemental composition of suspended matter in the Scotia-Weddell Confluence area during spring and summer 1988 (EPOS leg 2) During austral spring and summer 1988 the upper 500 m of water column in the Scotia-Weddell Confluence was sampled for the elemental composition of total s... F Dehairs,...
The interaction of turbulent ocean surface boundary layer (OSBL) currents and the surface waves' Stokes drift generates Langmuir turbulence (LT), which enhances OSBL mixing. This study investigates the response of LT to extreme wind and complex wave forcing under tropical cyclones (TCs), using a ...
In the northwest equatorial Atlantic, it is hypothesized that high salinity waters are subducted at the subtropics during winter and advected westward as a salinity maximum in the upper layers of the tropics, resulting in the barrier layer. In the eastern equatorial Indian Ocean, monsoonal related...
distribution. The timescale for half of the deep water to upwell from 30° S to the mixed layer is ~60–90 years. Introduction The global overturning circulation moves waters around the world’s oceans, connecting surface and deep waters through two interlinked overturning cells, one with ...
4) Ocean Mixed Layer Experiment 海洋混合层实验5) upper ocean 上层海洋 1. The cyclonic stress on the sea surface and the strong mixing processes forced by the typhoon play an important role in the processes of the heat, energy and mass exchange between the upper ocean and the deep ocean...