Tuesday, November 29, 2011

This year has been warmer than 11 of history, but the figures confirm the trend of global warming

that spring bulbs burst into life in the gardens around the United Kingdom, and the plants bloom in one second by the end of this fall has been mild temperatures prevailing in the United Kingdom and many regions in Europe.

Despite these unusual scenes, however, this year, in general, is not likely to be a world record holder. The Bureau of Meteorology figures released Tuesday shows that in 2011 was 11 th in the list of warmest years in records of global average temperature that dates back to 1850.

The UK was hardly the only - Weather in Russia since January was several degrees above normal, and Central America also had a warmer season. However, La Niña - a weather system in the Pacific that bring colder water to the surface - pushed down the global average, ie, this year was colder than 2010, which broke records in the climate World

Met Office estimates that the global average temperature from January to October 2011 was 14.36C, 0.36C above the 1961-1990 long-term averages. Complete data for the year will be available next March.

According to NASA, last year was the warmest in history, but there is a slight variation in the data collected by the various national centers for climate science, and according to data used by the Bureau of Meteorology and its partners at the University of East Anglia, last year global average temperature was slightly lower than in 1998.


Phil Jones, director of the Climatic Research Unit, University of East Anglia, said that due to natural variability, did not expect to see each year hotter than before, but the long-term trend clear. "The record HadCRUT3 [compiled by the Met Office and UEA], with the support of other albums, is one indicator among many that provide overwhelming evidence that the climate warmed," he said. " independent researchers to analyze the long-term trends of these indicators, there was an increase in temperature of air, sea and ground-level rise and the decline of Arctic sea ice, the accumulation of spring snow in the northern hemisphere and the extension of glaciers. "



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