Not exact matches
Combustion of coal, oil, and natural gas, and to a lesser extent deforestation, land - cover change, and emissions of
halocarbons and
other greenhouse gases, are rapidly increasing the atmospheric concentrations of climate - warming gases.
In 1990, emissions of
halocarbons and
other halogenated compounds occurred almost exclusively in the OECD90 region, which contributed 95 % to the world total (Figure 5 - 19).
Results show that the globally and annually averaged radiative forcing caused by the observed loss of sea ice in the Arctic between 1979 and 2007 is approximately 0.1 W m − 2; a complete removal of Arctic sea ice results in a forcing of about 0.7 W m − 2, while a more realistic ice - free - summer scenario (no ice for one month, decreased ice at all
other times of the year) results in a forcing of about 0.3 W m − 2, similar to present - day anthropogenic forcing caused by
halocarbons.
Other aspects (temperature, winds, etc.) of the atmospheric environment and chemicals other than halocarbons can also influence the ozone l
Other aspects (temperature, winds, etc.) of the atmospheric environment and chemicals
other than halocarbons can also influence the ozone l
other than
halocarbons can also influence the ozone layer.
At this time, there will be a lesser offset of the positive greenhouse effects of the
halocarbons and the
other well - mixed greenhouse gases (WMO, 1999).
Moreover, there are a number of entirely human - made greenhouse gases in the atmosphere, such as the
halocarbons and
other chlorine - and bromine - containing substances, dealt with under the Montreal Protocol.
Water vapor is a highly variable gas and has long been recognized as an important player in the cocktail of greenhouse gases — carbon dioxide, methane,
halocarbons, nitrous oxide, and
others — that affect climate.