Global warming gases have hit record levels in the world's atmosphere, with concentrations of carbon dioxide up 39 percent since the start of the industrial era in 1750, the U.N. weather agency said Monday.
The new figures for 2010 from the World Meteorological Organization show that CO2 levels are now at 389 parts per million, up from about 280 parts per million a quarter-millenium ago.
The WMO said the increase of 2.3 parts per million in CO2 in the atmosphere between 2009 and 2010 shows an acceleration from the average 1.5 parts per million increase during the 1990s.
The levels are significant because the greenhouse gases such as CO2, methane and nitrous oxide, trap heat in the atmosphere.
WMO Deputy Secretary-General Jeremiah Lengoasa said CO2 emissions are to blame for about four-fifths of the warming effect on the climate linked to greenhouse gases.
He added that there is a lag between what gets pumped into the atmosphere and its effect on climate.
"With this picture in mind, even if emissions were stopped overnight globally, the atmospheric concentrations would continue for decades because of the long lifetime of these greenhouse gases in the atmosphere," he said.
Negotiators from virtually all the world's nations will gather later this month in South Africa to try to agree on steps to head off the worst of the climate disruptions that researchers say will result if concentrations hit around 450 parts per million.
That could happen within several decades at the current rate, though some climate activists and vulnerable nations say the world has already passed the danger point of 350 parts per million and must somehow undo it.
Since 1750, WMO says, atmospheric concentrations of CO2 have risen 39 percent, those of nitrous oxide have gone up 20 percent and concentrations of methane jumped 158 percent.
Its report Monday cites fossil fuel-burning, loss of forests that absorb CO2 and use of fertilizer as the main culprits.
The levels do show some seasonal fluctuations. During the summer growing season, plants absorb carbon dioxide from the atmosphere. In winter, the concentration of CO2 rises as vegetation and other biomass decompose.