ASAR is an excellent instrument for observing the extent
and dynamics of ice shelves, which are important indicators
of climate change in polar regions. Along the Antarctic
Peninsula the ice shelves can reach 300 m thickness. They
are nourished by glaciers streaming down from the central
ice sheet plateau, which extends as a narrow spine along
the central part of the Peninsula.
Ice shelf animation
Time series climate data from the Peninsula
document an average temperature rise of 2.5 degrees Celsius
over the last 50 years. And as can be seen in this animation
which incorporates data from the last decade by combining
ERS SAR data with the first Envisat data, this warming seems
to have changed the very face of the Peninsula's east coast
once completely ice-shelf bound. This animation was prepared
by Prof. Helmuth Rott and his colleages from the University
of Innsbruck.
During the last 20 years, the duration and extent of surface
melt has increased significantly on the ice shelves of the western
and north-eastern sections of the Peninsula. This has led to
the formation of melt water ponds, weakening the structure of
the ice fabric and producing crevasses and rifts.
Antarctica in January 1999
(image from ERS)
Antarctica in January 1995
(image from ERS)
The ASAR image covers the Antarctic Peninsula, which extends for 1000
km in the south-north direction and is situated between the Bellingshausen
Sea on the west and the Weddell Sea on the east. This is a region
that has experienced exceptional atmospheric warming since the 1950s
and is therefore of key interest for global change research. Over
the last 50 years an average temperature increase of 2.5°C has been
observed at the climate stations on the Peninsula. This has triggered
the retreat and break-up of several ice shelves, culminating in the
collapse of the two northern parts of the Larsen Ice Shelf in January
1995 (Larsen A) and in March 2002 (Larsen B). The launch of Envisat
on 1 March 2002 occurred just in time to capture the dramatic break-up
of Larsen B.