MEDIA RELATIONS OFFICE 
JET PROPULSION LABORATORY 
CALIFORNIA INSTITUTE OF TECHNOLOGY 
NATIONAL AERONAUTICS AND SPACE ADMINISTRATION 
PASADENA, CALIF. 91109 TELEPHONE (818) 354-5011 
http://www.jpl.nasa.gov 
 
Contacts:  Colleen Sharkey (818) 354-0372 
 
IMAGE ADVISORY                          April 11, 2002        
                                
 
CHANGING ANTARCTICA VIEWED BY NASA SATELLITE

     NASA instruments flying on the Terra satellite have 
observed the calving of an iceberg and the breakup of an ice 
shelf in Antarctica, roughly 2,100 kilometers (1,300 miles) 
from one another.  

     Last month, a large crack developed in the Thwaites 
Tongue, a large sheet of glacial ice that extends from the 
West Antarctica mainland into the southern Amundsen Sea.  A 
piece broke away, or calved, forming an iceberg designated B-
22 by the National Ice Center.  In February, a section of the 
Larsen B ice shelf, located on the familiar finger-like 
Antarctic Peninsula, collapsed and broke away from the 
peninsula.

     The progression of both breakups were initially observed 
by NASA's Moderate Resolution Imaging Spectroradiometer.  
Images of the subsequent calving and ice shelf breakup were 
captured by NASA's Multi-angle Imaging SpectroRadiometer.  

     The B-22 iceberg images are available at: 

http://www-misr.jpl.nasa.gov/gallery/galhistory/2002_mar_27a.html .

     The B-22 iceberg measures approximately 82 kilometers 
(about 32 miles) long by 62 kilometers (about 24 miles) wide.  
Comparison of the images shows the iceberg, located below and 
to the left of center, has drifted away from the ice shelf.  
The breakup of ice near the shelf edge, in the area 
surrounding B-22, is also visible in the later image.  

     These natural-color images were acquired on March 10 and 
24, 2002, respectively.  Antarctic researchers have reported 
an increase in the frequency of iceberg calving in recent 
years.  It has not yet been established if this is a result of 
regional climate variation or the global warming trend.

     The two views of the ice shelf breakup, acquired on March 
7, 2002, provide helpful chemical and topographical 
perspectives.  In the left-hand image, near-infrared, red and 
blue data from the Multi-angle Imaging SpectroRadiometer's 
nadir (vertical-viewing) camera causes water ice within the 
ice shelf to appear vibrant blue.  Water has an intrinsic blue 
color due to the selective absorption of longer wavelengths 
such as red and infrared, and the translucent properties of 
ice within the collapsing shelf enables this absorption to be 
observed.  

     The ice shelf images are available at:

http://photojournal.jpl.nasa.gov/cgi-bin/PIAGenCatalogPage.pl?PIA03702

     Data from three different cameras on the instrument and 
one color channel were combined to create the multi-angle 
composite on the right.  Because vertical protrusions or 
depressions within textured surfaces appear brighter on their 
illuminated faces, the orange color in the multi-angle 
composite suggests a rough ice surface.  

     The Multi-angle Imaging SpectroRadiometer, built and 
managed by NASA's Jet Propulsion Laboratory, Pasadena, Calif., 
is one of several Earth-observing experiments aboard Terra, 
launched in December 1999. The instrument acquires images of  
Earth at nine angles simultaneously, using nine separate 
cameras pointed forward, downward, and backward along its 
flight path.  The Terra mission supports NASA's Earth Science 
Enterprise, a long-term research effort designed to help 
better understand and protect our home planet.  More 
information about the radiometer is available at 

     http://www-misr.jpl.nasa.gov .

     JPL is a division of the California Institute of 
Technology in Pasadena.

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