搜索结果: 1-15 共查到“海洋科学 diffusive”相关记录25条 . 查询时间(0.046 秒)
Diffusive boundary layers do not limit the photosynthesis of the aquatic macrophyte Vallisneria americanaat moderate flows and saturating light levels
Diffusive boundary layers do not limit the photosynthesis the aquatic macrophyte Vallisneria americana moderate flows saturating light levels
2014/4/17
Hydrodynamic models of mass transport assume that diffusive processes next to the surface limit transport and that there are no biological and chemical processes that control the supply and demand of ...
Double-diffusive staircases with a total of 230–350 mixed layers and sharp interfaces were observed in nine microstructure temperature profiles measured during February 2004 in Lake Kivu. The presence...
Note on the Occurrence of Double-Diffusive Convection in the Baltic Proper
Note Occurrence Double-Diffusive Convection Baltic Proper
2009/6/15
Note on the Occurrence of Double-Diffusive Convection in the Baltic Proper.
Double-Diffusive Convection and its Implications for the Temperature and Salinity Structure of the Ocean and Lake Vanda
Double-Diffusive Convection Salinity Structure Temperature Lake Vanda
2009/4/3
Recently, Fedorov has attempted to interpret some temperature and salinity profiles in the northeast Atlantic, as reported by Zenk, in terms of the results of laboratory experiments in double-diffusiv...
Form of the Temperature-Salinity Relationship in the Central Water：Evidence for Double-Diffusive Mixing
Temperature-Salinity Double-Diffusive Mixing Central Water
2009/2/10
Ingham (1966) reported that the temperature-salinity relationships in the Central Waters were much better described by a curve of constant density ratio (Rρ = αΔT/βΔS) than by a straight line. His res...
On the Parameterization of Diapycnal Fluxes due to Double-Diffusive Intrusions
Diapycnal Fluxes Double-Diffusive Intrusions
2009/2/8
An attempt is made to Parameterized the large-Scale average diapycnal (cross-isopycnal) mixing that presumably occurs in the thermohaline fronts that develop when large-scale epipycnal (along-isopycna...
Double-Diffusive Interleaving. Part II：Finite Amplitude, Steady State Interleaving
Double-Diffusive Interleaving Finite Amplitude Steady State Interleaving
2009/1/16
The exponentially growing solutions of the linear stability analysis of double-diffusive interleaving are allowed to grow to finite amplitude. At this stage the double-diffusive fluxes across the intr...
Double-Diffusive Interleaving. Part I：Linear Stability Analysis
Double-Diffusive Interleaving Linear Stability Analysis
2009/1/16
Quasi-horizontal interleaving between water masses is frequently observed in the frontal regions between different water masses where there are significant compensating isopycnal gradients of temperat...
Oceanographic implications of Laboratory Experiments on Diffusive Interfaces
Oceanographic implications Diffusive Interfaces Laboratory Experiments
2009/1/5
This paper contains a summary of the results from some laboratory and theoretical studies on the diffusive interface in double diffusive convection, paying particular attention to the recent work of F...
Double-Diffusive Interleaving at the Equator
Double-Diffusive Interleaving Equator water masses
2008/12/24
A theory for the observed interleaving of water masses at the equator is presented. Unlike layers at midlatitudes, individual layers are observed to be coherent over horizontal scales of hundreds of k...
Microstructure in and around a Double-Diffusive Interface
Double-Diffusive Interface Microstructure
2008/12/22
The microstructure of temperature and velocity were measured for 35 km with a towed vehicle that moved in and around a single interface in a well-developed thermohaline staircase with a density ratio ...
Labrador Sea Water in the Eastern North Atlantic. Part II：Mixing Dynamics and the Advective–Diffusive Balance
Labrador Sea Water Mixing Dynamics Advective–Diffusive Balance
2008/12/11
Deep wintertime convection in the Labrador Basin produces Labrador Sea Water (LSW), which spreads throughout the North Atlantic. The LSW is not formed with constant characteristics but varies on decad...
Study on the Effects of Bottom Topography on Deep Circulation with a Diffusive Reduced-Gravity Model
Bottom Topography Diffusive Reduced-Gravity Model Deep Circulation
2008/12/11
Abyssal circulation around a sea mountain and a depression in a midlatitude basin is investigated with a reduced-gravity model characterized by vertical and horizontal diffusion of both momentum and d...
Double-Diffusive Interleaving：The Influence of Nonconstant Diffusivities
Double-Diffusive Interleaving Nonconstant Diffusivities
2008/12/11
The influence of nonconstant diffusivity and viscosity on double-diffusive interleaving is examined using a simple model. The analysis allows a prediction of the slope, vertical wavenumber, and growth...
Effect of Baroclinicity on Double-Diffusive Interleaving
Double-Diffusive Interleaving Baroclinicity
2008/11/26
Although ocean fronts are often baroclinic, existing models of double-diffusive interleaving have ignored such baroclinic effects as velocity shear and horizontal density gradients. To determine the i...
