Other impacts of human civilization, such as deforestation and other changes to land use, pollution and
black soot landing on Arctic snows also contribute to warming.
Not exact matches
These forcings are spatially heterogeneous and include the effect of aerosols on clouds and associated precipitation [e.g., Rosenfeld et al., 2008], the influence of aerosol deposition (e.g.,
black carbon (
soot)[Flanner et al. 2007] and reactive nitrogen [Galloway et al., 2004]-RRB-, and the role of changes in
land use /
land cover [e.g., Takata et al., 2009].
Recent papers have suggested that various forcings have been significantly underestimated (e.g. various solar influences,
black soot,
land use changes).
Scientific confidence of the occurrence of climate change include, for example, that over at least the last 50 years there have been increases in the atmospheric concentration of CO2; increased nitrogen and
soot (
black carbon) deposition; changes in the surface heat and moisture fluxes over
land; increases in lower tropospheric and upper ocean temperatures and ocean heat content; the elevation of sea level; and a large decrease in summer Arctic sea ice coverage and a modest increase in Antarctic sea ice coverage.
These human forcings include greenhouse gas emissions (e.g. CO2, methane, CFCs), aerosol emissions and deposition [e.g.,
black carbon (
soot), sulfates, and reactive nitrogen], and changes in
land use and
land cover.
«Belching from smokestacks, tailpipes and even forest fires,
soot — or
black carbon — can quickly sully any snow on which it happens to
land.
Using the WRF - chem model, the team first examined how much
soot in the form of so - called
black carbon would
land on snow in the Sierra Nevada, Cascade and Rocky Mountains.