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Intraspecific scaling of mass to length in pelagic animals: Ontogenetic shape change and its implications
Intraspecific scaling of mass length in pelagic animals Ontogenetic shape change its implications
2014/4/4
Intraspecific relationships between body mass (M) and length (L) are widely reported using the equation M = aLb. The power term (b) holds fundamental information on how body proportions change with in...
Comment: Temperature, nutrients, and the size-scaling of phytoplankton growth in the sea
Comment Temperature nutrients size-scaling of phytoplankton growth the sea
2014/4/4
Comment: Temperature, nutrients, and the size-scaling of phytoplankton growth in the sea。
Mixing and stratification in lakes of varying horizontal length scales: Scaling arguments and energy partitioning
Mixing stratification varying horizontal length scales Scaling arguments energy partitioning
2014/4/17
This work analyzes the effects that changes in the surface area of stratified lakes have on the partitioning of energy among different pools, and, ultimately, on the strength of thermalstratification....
Scaling statistics in a critical,nonlinear physical model of tropical oceanic rainfall
Scaling statistics critical,nonlinear physical model tropical oceanic rainfall
2009/11/12
Over the last two decades, concepts of scale invariance have come to the fore in both modeling and data analysis in hydrological precipitation research. With the advent of the use of the multiplicativ...
The simple scaling of a tidal bottom boundary layer by the shear velocity, u*, and the wall to the wall describes well the mean Bow field. To test the full extent of this scaling measurements were mad...
Fetch Relations for Wind-Generated Waves as a Function of Wind-Stress Scaling
Canadian Atlantic Storms Program Wind-Stress Scaling Wind-Generated Waves
2008/12/30
We present the variation that results when fetch relations for wind-generated wave spectra are sealed by the friction velocity component in the dominant wave direction rather than the magnitude of the...
Surface Wave–Turbulence Interactions. Scaling （z） near the Sea Surface
Surface Wave Sea Surface turbulent mixing
2008/12/12
A freely rising profiler was used to collect vertical microstructure profiles in the upper oceanic boundary layer under various atmospheric and sea conditions. Near the sea surface, the rate of viscou...
A Nonhydrostatic Mesoscale Ocean Model. Part I：Well-Posedness and Scaling
Mesoscale Ocean Model hydrostatic approximations
2008/12/10
The incompressibility and hydrostatic approximations that are traditionally used in large-scale oceanography to make the hydrodynamic equations more amenable to numerical integration result in the pri...
Recent tests of all generations of numerical wave models indicate that extreme wave heights are significantly underpredicted by these models. This behavior is consistent with the finding by Ewing and ...
Internal Boundary Layer Scaling in “Two Layer” Solutions of the Thermocline Equations
Internal Boundary Layer Scaling Two Layer Thermocline Equations
2008/7/17
The diffusivity dependence of internal boundary layers in solutions of the continuously stratified, diffusive thermocline equations is revisited. If a solution exists that approaches a two-layer solut...
Jet Structure and Scaling in Southern Ocean Models
Jet Structure Scaling Southern Ocean Models
2008/7/11
The jet structure of the Antarctic Circumpolar Current (ACC) simulated by two general circulation models (GCMs), FRAM (Fine Resolution Antarctic Model) and POP (Parallel Ocean Program), is examined in...
Comparison of Thermally Driven Circulations from a Depth-Coordinate Model and an Isopycnal-Layer Model. Part I: Scaling-Law Sensitivity to Vertical Diffusivity
Thermally Driven Circulations Depth-Coordinate Model Isopycnal-Layer Model Scaling-Law Sensitivity
2008/6/30
Two different types of numerical ocean circulation models are used in a classical idealized problem, the thermally induced circulation in an ocean basin bounded by two meridians to the east and west a...
Scaling Analysis for the Interaction between a Buoyant Coastal Current and the Continental Shelf: Experiments and Observations
Buoyant Coastal Current Continental Shelf
2008/6/23
This paper addresses how the geometrical parameters (ambient ocean depth, H; bottom slope, α) of coastal bathymetry affect the evolution of buoyant coastal currents flowing over a sloping continental ...
Scaling Analysis for the Interaction between a Buoyant Coastal Current and the Continental Shelf: Experiments and Observations
Buoyant Coastal Current Continental Shelf
2008/6/23
This paper addresses how the geometrical parameters (ambient ocean depth, H; bottom slope, α) of coastal bathymetry affect the evolution of buoyant coastal currents flowing over a sloping continental ...
Resource levels, allometric scaling of population abundance, and marine phytoplankton diversity
Resource levels allometric scaling population abundance marine phytoplankton diversity
2014/4/21
We analyzed the relationship between population abundance and cell size in phytoplankton assemblages from coastal, shelf, and open-ocean environments. Our results show that across the entire size spec...