Glacier-melting debate highlights importance of satellites 2 February 2010
The intense public debate on how rapidly the Himalayan glaciers are retreating
highlights the necessity for the constant monitoring of glaciers worldwide by
satellites.
Since glaciers are among the most reliable indicators of climate change and
because they can have a major influence on water availability, knowledge of the
recent changes and future behaviour is of great interest for climate scientists
and governing bodies. A key to assess these changes or to model their future
evolution is the existence of a detailed glacier inventory.
Data from satellites allow scientists to measure glacier extent in detail,
providing authoritative evidence of trends. They also allow local measurements
to be expanded to a regional scale. Considering the valuable role satellites can
play in determining the state of Earth’s glaciers, the Global Climate Observing
System (GCOS) has called for the systematic monitoring of glaciers by satellites
in support of the UN Framework Convention on Climate Change.
In 2007, ESA started the GlobGlacier project as a major effort to develop and
apply existing methodologies to monitor glaciers and contribute to a global
glacier inventory using satellite observations. GlobGlacier, part of ESA’s 'Data
User Element', is adding about 20 000 of the estimated 160 000 glaciers
worldwide to this inventory to allow their histories to be adequately tracked.
Kashmir, part of the Indian Himalayas, is one of the selected regions where
little information is available on overall glacier extent or changes.
GlobGlacier is creating inventory data for more than 1000 glaciers in this
region.
The inventory combines information on glacier outlines based on archived
satellite data from the Landsat Thematic Mapper (TM) and the Enhanced Thematic
Mapper Plus (ETM+) instruments with topographic information from the Shuttle
Radar Topography Mission and the Global Digital Elevation Model (GDEM) from
ASTER (Advanced Spaceborne Thermal Emission and Reflection Radiometer). When a
time series of suitable images are available for a certain region, changes in
glacier length and extent can be calculated. "Such data allow scientists to
assess the overall pattern of changes in a larger region for a better
determination of climatic change impacts," said GlobGlacier Project Manager
Frank Paul from the University of Zurich.
The animation available in the "view images" section, based on data
acquired by Landsat’s TM on 15 November 1990 and by ETM+ on 1 August 2001,
illustrates the changes in glacier extents that occurred during this time in the
region northeast of the Gangotri Glacier, situated in Garwhal Himalaya.
While most of the smaller and debris-free glaciers show considerable retreat in
this period, the larger glaciers with completely covered tongues have not
changed much. Several of the pro-glacial lakes have grown. Quite a few glaciers
at lower altitudes are nearly free of snow in the August 2001 image, indicating
a retreat that year.
ESA’s ERS-1, ERS-2 and Envisat Advanced Synthetic Aperture Radar (ASAR) data
are providing velocity measurements of selected glaciers. The image in the "view
images" section shows the surface velocity field for the Baltoro Glacier in
Pakistan based on Envisat ASAR data from 2003 to 2008.
ESA’s new Climate Change Initiative, which will produce robust long-term
records of essential climate variables, will build on the results of the
GlobGlacier project by further improving the algorithms for glacier monitoring
and continually updating the related glacier inventory information.
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