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Study demonstrates strong potential of seagrass to curb erosion（图）
strong potential seagrass curb erosion
2019/10/30
Most people's experience with seagrass, if any, amounts to little more than a tickle on their ankles while wading in shallow coastal waters. But it turns out that these ubiquitous plants, varieties of...
Populations of Symbiodinium muscatinei Show Strong Biogeographic Structuring in the Intertidal Anemone Anthopleura elegantissima
Symbiodinium muscatinei Anthopleura elegantissima
2015/12/11
Among temperate cnidarian symbioses, the
partnership between the intertidal anemone Anthopleura
elegantissima and its dinoflagellate and chlorophyte symbionts is one of the most well character...
A Feasibility Study on a New Trimaran PCC in Medium Speed –Performance in Still Water and Strong Wind
trimaran Pure Car Carrier EHP drift angle speed reduction
2011/9/9
In the present paper, a new trimaran Pure Car Carrier (PCC) is proposed and a feasibility study on the ship is carried out. In this study, first, the effective horse power (EHP)/car of the PCC running...
Life history, ecology and the biogeography of strong genetic breaks among 15 species of PaciWc rockWsh, Sebastes
Life history ecology
2015/12/11
Strong genetic change over short spatial scales
is surprising among marine species with high dispersal
potential. Concordant breaks among several species signals
a role for geographic barriers to d...
Oceanic Thermal Response to Strong Atmospheric Forcing II. The Role of One-Dimensional Processes
Oceanic Thermal Response Strong Atmospheric Forcing One-Dimensional Processes
2009/2/23
The oceanic response to individual atmospheric forcing events during September to December is studied using ocean weather ship observations supplemented by simulations with a bulk turbulent kinetic en...
Oceanic Thermal Response to Strong Atmospheric Forcing I. Characteristics of Forcing Events
Oceanic Thermal Response Strong Atmospheric Forcing Forcing Events
2009/2/23
Long time series of meteorological data from Ocean Weather Ships P, V and N in the North Pacific Ocean are used to test the hypothesis that significant oceanic thermal response during September to Dec...
Boundary-Forced Planetary Waves：A Simple Model Mid-Ocean Response to Strong Current Variability
Boundary-Forced Planetary Waves Mid-Ocean Response Strong Current Variability
2009/2/13
A simple linear model of the barotropic basin response to forcing imposed along the northern boundary is described. The dependence on latitude of the response may include oscillatory behavior or not, ...
Meanders and Detached Eddies of a Strong Eastward-Flowing Jet Using a Two-Layer Quasi-Geostrophic Model
Detached Eddies Two-Layer Quasi-Geostrophic Model Strong Eastward-Flowing Jet
2009/2/9
The process of meander growth on and eddy detachment from an eastward flowing oceanic jet, which is modeled after the Gulf Stream east of Cape Hatteras, is studied using numerical solutions of nonline...
Open Ocean Momentum Flux Measurements in Moderate to Strong Winds
Ocean Momentum Flux Measurements Strong Winds
2009/2/9
Measurements of the momentum flux were made by the Reynolds flux and dissipation methods on a deep water stable tower operated by the Bedford Institute of Oceanography, A modified Gill propeller-vane ...
On Wind-Driven Mixed Layers with Strong Horizontal Gradients—A Theory with Application to Coastal Upwelling
Wind-Driven Mixed Layers Horizontal Gradients Coastal Upwelling
2009/1/19
A theory of a two-dimensional wind-driven diabatic ocean mixed layer with strong horizontal gradients is formulated analytically. An equation that allows the relaxation of the strict Ekman balance—Cor...
The Response of Intense Oceanic Current Systems Entering Regions of Strong Cooling
Intense Oceanic Current Systems Strong Cooling
2009/1/16
The three-dimensional response of strong currents to cross-stream gradients of surface cooling is studied using numerical simulations. In particular, surface cooling is explored as a possible mechanis...
Upper Ocean Temperature Structure, Inertial Currents, and Richardson Numbers Observed during Strong Meteorological Forcing
Upper Ocean Temperature Inertial Currents Meteorological Forcing
2009/1/16
Upper ocean currents and temperature in the northeastern Pacific were measured during a 14-day period in November 1980 as part of STREX. Velocities in the upper ocean are dominated by near-inertial fr...
Strong Current Events Related to a Subtropical Front in the Northeast Atlantic
Strong Current Events Northeast Atlantic Subtropical Front
2009/1/16
Long-term temperature and current-meter records from moorings in the northern Canary Basin display strong current events with time scales between one and three months and large vertical scales of seve...
Upper Ocean Thermal Response to Strong Autumnal Forcing of the Northeast Pacific
Upper Ocean Thermal Northeast Pacific Storm Transfer and Response Experiment
2009/1/13
CASID free-drifting thermistor chain buoys that utilized Service ARGOS positioning and data collection were deployed in the northeast Pacific Ocean in the vicinity of OWS-P in late autumn in both 1980...
Analytical solutions are found for topographic waves propagating over step bottom slopes in a two-layer infinite channel. From the inviscid unforced long-wave equation for a two-layer fluid on an f-pl...