The Greenland ice sheet is a unique archive of the climate and
atmospheric composition far back in time.
Not exact matches
The relevance to
atmospheric composition is that silica - rich rocks have
far less iron and sulfur than silica - poor rocks, and iron and sulfur react with oxygen and form a sink for oxygen.
However, elevated
atmospheric CO2 concentrations and ocean acidification may also have an adverse impact on diatom growth, causing a decrease in cell size and possible
further changes in phytoplankton
composition.
This inertia implies that there is additional climate change «in the pipeline» even without
further change of
atmospheric composition.
Current concentrations of
atmospheric carbon dioxide and methane
far exceed pre-industrial values found in polar ice core records of
atmospheric composition dating back 650,000 years.
The data were
further revised in 2008 to account for variations in the satellite weighting functions over time due to changes in
atmospheric composition.
Implications include (i) the expectation of additional global warming of about 0.6 °C without
further change of
atmospheric composition; (ii) the confirmation of the climate system's lag in responding to forcings, implying the need for anticipatory actions to avoid any specified level of climate change; and (iii) the likelihood of acceleration of ice sheet disintegration and sea level rise.
The experiments were performed with ModelE2, a new version of the NASA Goddard Institute for Space Sciences (GISS) coupled general circulation model that includes three different versions for the
atmospheric composition components: a noninteractive version (NINT) with prescribed
composition and a tuned aerosol indirect effect (AIE), the TCAD version with fully interactive aerosols, whole - atmosphere chemistry, and the tuned AIE, and the TCADI version which
further includes a parameterized first indirect aerosol effect on clouds.
The WGI
FAR codified the key physical and biogeochemical processes in the Earth system that relate a changing climate to
atmospheric composition, chemistry, the carbon cycle and natural ecosystems.