In coral, lake bottom, and
sea bottom cores, δ18O is the primary temperature indicator via CaCO3.
Not exact matches
Measurements of stable isotopes of planktonic and benthic foram and diatom shells have been taken from hundreds of deep -
sea cores around the world to map past surface and
bottom water temperatures.
44 present
sea level (meters) Height above or below Today's
sea level present
sea level (meters) Height above or below Height above or below present
sea level (feet) Figure 20.9 Changes in average
sea level over the past 250,000 years based on data from
cores removed from the ocean
bottom.
Changes in average
sea level over the past 250,000 years based on data from
cores removed from the ocean
bottom.
But a reminder, you are doing V&V on the dynamic
core, the
bottom boundary conditions (like orography), each individual parameterization (e.g. radiative transfer, convection, boundary layer, clouds, etc), and in the case of coupled models the ocean module, the
sea ice module, the land process module, the aerosol module (and in future the ice sheet module), in stand alone mode as well as when coupled in the climate model.
Besides the information about greenhouse - gas levels from the trapped air bubbles at Vostok, a sediment
core from the
bottom of the Red
Sea indicates changes in sea level, which in turn give an approximation of ice sheet ar
Sea indicates changes in
sea level, which in turn give an approximation of ice sheet ar
sea level, which in turn give an approximation of ice sheet area.