It is equally urgent to strengthen the monitoring network in those regions which at the moment have sparse coverage and to include the latest technologies such as high-resolution remote sensing to compliment the traditional field observations," said Mr Gilruth and Professor Haeberli. The call was made during the 20th anniversary celebrations of the Intergovernmental Panel on Climate Change (IPCC)-the scientific body established by UNEP and the World Meteorological Organisation to advise governments on global warming. Here UNEP and the WGMS released the report Global Glacier Changes: Facts and Figures. The report presents the latest fluctuations of glaciers and ice caps and underlines the overall trend of glaciers' retreat. Indeed the report confirms that the average annual melting rate of glaciers appears to have doubled after the turn of the millennium, with record losses posted in 2006 for a key network of reference sites. If the trend continues and governments fail to agree on deep and decisive emission reductions at the crucial UN climate convention meeting in Copenhagen in 2009, it is possible that glaciers may completely disappear from many mountain ranges in the 21st century. Background
By looking at glaciers or what is left of them, future generations will be able to discern clearly which climate scenario is being played out at the present time. The consequences of ice disappearance for landscape characteristics in high mountain areas will be felt at local to regional scales, while the changes in the water cycle will also affect continental-scale water supply and global-scale sea levels. Glacier
monitoring
The database on glacier fluctuations includes 36 240 length change observations from 1803 glaciers as far back as the late 19th century, as well as about 3 400 annual mass balance measurements from 226 glaciers covering the past six decades. In 2006, a new record annual mass loss was measured on the reference glaciers under long-term observation. The average annual melting rate of mountain glaciers appears to have doubled after the turn of the millennium, in comparison with the already accelerated melting rates observed in the two decades before. The previous record loss in the year 1998 has already been exceeded three times, i.e., in the years 2003, 2004 and 2006, with the losses in 2004 and 2006 being almost twice as high as the previous 1998 record loss. Early measurements indicate strong ice losses as early as the 1940s and 1950s, followed by a moderate ice loss between 1966 and 1985, and accelerating ice losses until present. The global average annual mass loss of more than half a metre during the decade of 1996 to 2005 represents twice the ice loss of the previous decade (1986-95) and over four times the rate of the decade from 1976 to 1985. Prominent periods of regional mass gains are found in the Alps in the late 1970s and early 1980s and in coastal Scandinavia and New Zealand in the 1990s. Glaciers
and climate
Under current IPCC climate scenarios, the ongoing trend of worldwide and rapid, if not accelerating, glacier shrinkage on the century time scale is most likely to be of a non-periodic nature, and may lead to the de-glaciation of large parts of many mountain ranges this century. New
efforts needed
The internationally coordinated glacier monitoring was initiated in 1894, following the example of the Swiss national observation network, and has been mainly under Swiss leadership since then. Today, the World Glacier Monitoring Service (WGMS) is responsible for the collection and publication of standardized glacier data from around the world. The WGMS is located at the University of Zurich, Switzerland, and maintains a collaborative network of national correspondents and principal investigators in the countries involved in glacier monitoring. The long-term measurement series of glacier mass balance produces one of the essential variables within the international climate-related monitoring programmes.
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