«New satellite method enables undersea estimates from space: Statistical advance quantifies
important ocean parameters in the illuminated ocean.»
Not exact matches
As the science develops, it is
important for managers to design select examples of coral reef areas in a variety of
ocean chemistry and oceanographic regimes (e.g., high and low pH and aragonite saturation state; areas with high and low variability of these
parameters) for inclusion in MPAs.
Since OHC uptake efficiency associated with surface warming is low compared with the rate of radiative restoring (increase in energy loss to space as specified by the climate feedback
parameter), an
important internal contribution must lead to a loss rather than a gain of
ocean heat; thus the observation of OHC increase requires a dominant role for external forcing.