But the fast - motion shift to forests will
likely absorb carbon dioxide, as well.
Not exact matches
Although some lakes can also
absorb CO2 at their surfaces similar to the way oceans do, the increases in these other sources of organic and inorganic
carbon are
likely the dominant factor, says Scott Higgins, a research scientist at the International Institute for Sustainable Development's Experimental Lakes Area, a natural laboratory of 58 small lakes in Ontario.
Its two faces differ strikingly in color,
likely the result of thermal segregation: Over time, darker materials (like
carbon) have
absorbed more heat from the sun, warming up and sending lighter, more volatile materials (like ice) to the colder hemisphere.
The mostly
likely explanation is that the
carbon nanotubes
absorb more sunlight and donate electrons to the photosynthetic process, according to Giraldo and the rest of the team, or the nanotubes may be speeding up the transfer of electrons within the photosynthetic processes.
«We wanted to understand why there is more cis - lycopene in the body, and by mathematically modeling our patients» blood
carbon - 13 lycopene concentration data, we found that it is
likely due to a conversion of all - trans to cis lycopene, which occurs soon after we
absorb lycopene from our food,» she added.
Further, because of the processes highlighted in the Solomon paper and other analyses, including the IPCC AR4, the net removal of CO2 from the atmosphere is
likely to fall as the stocks that
absorb all that
carbon, particularly the oceans, fill up.
One of climate science's main focuses is the capacity of land and sea to
absorb CO2; if «
carbon sinks» lose the ability to sequester
carbon, more CO2 will remain in the atmosphere,
likely escalating warming.
New research shows forests are slow to recover from droughts, and climate models that overlook recovery time are
likely overestimating how much
carbon forests can
absorb after droughts.
This leaves only a few dollars margin to
absorb other factors such as potential
carbon offset costs,
likely inflation in labour, materials and energy costs.
And such corals are
likely to suffer before their tropical counterparts as cold waters
absorb more
carbon dioxide.
Callendar suggested that the top layer of the ocean, that interacts with the atmosphere, would easily become saturated with
carbon dioxide and that would affect its ability to
absorb more, because, he thought, the rate of mixing of shallow and deep oceanic waters was
likely to be very slow.
Black
carbon has
likely played a far more significant role there, because of the contrast between
absorbing aerosols deposited on the ice surface, and the high albedo perennial ice cover, and thus in this particular region black
carbon has
likely been an aggravating factor when it comes to anthropogenic surface warming.