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Resolving the Impacts and Feedback of Ocean Optics on Upper Ocean Ecology
Resolving the Impacts and Feedback Ocean Optics Upper Ocean Ecology
2015/8/4
The abundance and fecundity of life on this planet is directly related to the energy supplied by the sun. The pyramid of life starts with the absorption of a fraction of this energy, followed by its c...
Feedback effects in a coastal canopy-forming submersed plant bed
coastal canopy-forming submersed plant bed Feedback
2014/4/17
Although physical and biogeochemical properties of an environment determine distribution and health of
biota, some organisms modify habitat conditions through complex interactions with their surround...
Extraction of Mixed Layer Advection Velocities, Diffusion Coefficients, Feedback Factors and Atmospheric Forcing Parameters from the Statistical Analysis of North Pacific SST Anomaly Fields
sea surface temperature Mixed Layer Advection Velocities Diffusion Coefficients
2009/1/9
The statistical properties of observed North Pacific sea surface temperature (SST) anomalies are simulated by a simple mixed layer advection and diffusion model with stabilizing feedback and local sto...
The Role of Temperature Feedback in Stabilizing the Thermohaline Circulation
Temperature Feedback Thermohaline Circulation surface heat flux
2008/12/11
Ocean climate models traditionally compute the surface heat flux with a restoring boundary condition of the form Q = λ(T* − To). This implies an atmosphere of fixed temperature and breaks down w...
Fuzzy-PID controlled lift feedback fin stabilizer
lift fin stabilizer lift force feedback control fuzzy control PID self-adjusting
2011/9/14
Conventional PID controllers are widely used in fin stabilizer control systems,but they have time-variations,nonlinearity,and uncertainty influencing their control effects.A lift feedback fuzzy-PID co...
The Stabilization of the Thermohaline Circulation by the Temperature–Precipitation Feedback
Stabilization Thermohaline Circulation Temperature–Precipitation Feedback
2008/6/13
The meridional freshwater flux in the atmosphere, and hence the strength of the hydrological cycle, undergoes variations on glacial–interglacial as well as on some shorter timescales. A significant po...
Long-term changes in the areal hypolimnetic oxygen deficit (AHOD) of Onondaga Lake: Evidence of sediment feedback
Long-term changes areal hypolimnetic oxygen
2014/4/30
Long-term trends in the rate of depletion of hypolimnetic dissolved oxygen (DO) are documented for ionically
enriched hypereutrophic Onondaga Lake, New York, for the 1978–2002 interval. Depletion rat...