Scientists have compiled a record of snowfall in Antarctica going back 200 years, reports BBC from Austria. The study shows there has been a significant increase in precipitation over the period, up 10per cent. Some 272 billion tonnes more snow were being dumped on the White Continent annually in the decade 2001-2010 compared with 1801-1810. This yearly extra is equivalent to twice the water volume found today in the Dead Sea.

Put another way, it is the amount of water you would need to cover New Zealand to a depth of 1m. Dr Liz Thomas presented the results of the study at the European Geosciences Union (EGU) General Assembly here in Vienna, Austria.

The British Antarctic Survey (BAS) researcher said the work was undertaken to try to put current ice losses into a broader context. "The idea was to get as comprehensive a view of the continent as possible," she told BBC News.

"There's been a lot of focus on the recent era with satellites and how much mass we've been losing from big glaciers such as Pine Island and Thwaites. But, actually, we don't have a very good understanding of how the snowfall has been changing.

"The general assumption up until now is that it hasn't really changed at all - that it's just stayed stable. Well, this study shows that's not the case.”

Dr Thomas and colleagues examined 79 ice cores drilled from across Antarctica. These long cylinders of frozen material are essentially just years of compacted snow.

By analysing the cores' chemistry, it is possible to determine not only when their snows fell but also how much precipitation came down. For

example, one key marker used to differentiate one year from the next, even seasons, is hydrogen peroxide.

This is a photochemical product that forms in the atmosphere when water vapour encounters sunlight.

"For us, that's perfect. Antarctica works like an on-off switch with the long 'polar nights' in winter and long periods of daylight in summer," Dr Thomas explained.

The previous, most extensive survey of this kind assessed just 16 cores. The new study is therefore much more representative of snowfall behaviour across the entire continent.

It found the greater precipitation delivered additional mass to the Antarctic ice sheet at a rate of 7 billion tonnes per decade between 1800 and 2010 and by 14 billion tonnes per decade when only the period from 1900 is considered.

Most of this extra snow has fallen on the Antarctic Peninsula, which saw significant increases in temperature during the 20th Century.