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Images of Antarctica and Goddard Space Flight Center (GSFC)
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Antarctica: Allen Hills Fly
| Title |
Antarctica: Allen Hills Fly Over |
| Abstract |
RADARSAT lets Scientist see the frozen continent. |
| Completed |
1999-11-08 |
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Antarctica: Allen Hills Fly
| Title |
Antarctica: Allen Hills Fly Over |
| Abstract |
RADARSAT lets Scientist see the frozen continent. |
| Completed |
1999-11-08 |
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Antarctica: Allen Hills Fly
| Title |
Antarctica: Allen Hills Fly Over |
| Abstract |
RADARSAT lets Scientist see the frozen continent. |
| Completed |
1999-11-08 |
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Antarctica: Allen Hills Fly
| Title |
Antarctica: Allen Hills Fly Over |
| Abstract |
RADARSAT lets Scientist see the frozen continent. |
| Completed |
1999-11-08 |
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ICESat First Light Release:
| Title |
ICESat First Light Release: Antarctica, from Coast to Coast |
| Abstract |
ICESat's first topographic profiles across the continent reveal the textured surfaces of Antarctic ice sheets in unprecedented detail. The following profile spans the entire Antarctic continent from coast to coast. The transect begins near Wrigley Gulf, crosses the Ross Ice Shelf and central Antarctica, finally tapering off at the Amery Ice Shelf. The high flat area in the center of the continent is called the East Antarctic plateau. |
| Completed |
2003-05-23 |
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ICESat First Light Release:
| Title |
ICESat First Light Release: Antarctica, from Coast to Coast |
| Abstract |
ICESat's first topographic profiles across the continent reveal the textured surfaces of Antarctic ice sheets in unprecedented detail. The following profile spans the entire Antarctic continent from coast to coast. The transect begins near Wrigley Gulf, crosses the Ross Ice Shelf and central Antarctica, finally tapering off at the Amery Ice Shelf. The high flat area in the center of the continent is called the East Antarctic plateau. |
| Completed |
2003-05-23 |
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ICESat First Light Release:
| Title |
ICESat First Light Release: Antarctica, from Coast to Coast |
| Abstract |
ICESat's first topographic profiles across the continent reveal the textured surfaces of Antarctic ice sheets in unprecedented detail. The following profile spans the entire Antarctic continent from coast to coast. The transect begins near Wrigley Gulf, crosses the Ross Ice Shelf and central Antarctica, finally tapering off at the Amery Ice Shelf. The high flat area in the center of the continent is called the East Antarctic plateau. |
| Completed |
2003-05-23 |
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ICESat First Light Release:
| Title |
ICESat First Light Release: Antarctica, from Coast to Coast |
| Abstract |
ICESat's first topographic profiles across the continent reveal the textured surfaces of Antarctic ice sheets in unprecedented detail. The following profile spans the entire Antarctic continent from coast to coast. The transect begins near Wrigley Gulf, crosses the Ross Ice Shelf and central Antarctica, finally tapering off at the Amery Ice Shelf. The high flat area in the center of the continent is called the East Antarctic plateau. |
| Completed |
2003-05-23 |
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ICESat First Light Release:
| Title |
ICESat First Light Release: Antarctica, from Coast to Coast |
| Abstract |
ICESat's first topographic profiles across the continent reveal the textured surfaces of Antarctic ice sheets in unprecedented detail. The following profile spans the entire Antarctic continent from coast to coast. The transect begins near Wrigley Gulf, crosses the Ross Ice Shelf and central Antarctica, finally tapering off at the Amery Ice Shelf. The high flat area in the center of the continent is called the East Antarctic plateau. |
| Completed |
2003-05-23 |
|
ICESat First Light Release:
| Title |
ICESat First Light Release: Antarctica, from Coast to Coast |
| Abstract |
ICESat's first topographic profiles across the continent reveal the textured surfaces of Antarctic ice sheets in unprecedented detail. The following profile spans the entire Antarctic continent from coast to coast. The transect begins near Wrigley Gulf, crosses the Ross Ice Shelf and central Antarctica, finally tapering off at the Amery Ice Shelf. The high flat area in the center of the continent is called the East Antarctic plateau. |
| Completed |
2003-05-23 |
|
ICESat First Light Release:
| Title |
ICESat First Light Release: Antarctica, from Coast to Coast |
| Abstract |
ICESat's first topographic profiles across the continent reveal the textured surfaces of Antarctic ice sheets in unprecedented detail. The following profile spans the entire Antarctic continent from coast to coast. The transect begins near Wrigley Gulf, crosses the Ross Ice Shelf and central Antarctica, finally tapering off at the Amery Ice Shelf. The high flat area in the center of the continent is called the East Antarctic plateau. |
| Completed |
2003-05-23 |
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Antarctica: Larsen Pre-shot
| Title |
Antarctica: Larsen Pre-shot (with box) |
| Abstract |
This animation was used with the Larsen Ice Shelf images in animation #1400. |
| Completed |
1999-11-08 |
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Antarctica: Fimbul Ice Shelf
| Title |
Antarctica: Fimbul Ice Shelf Preview |
| Completed |
1999-11-08 |
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Antarctica: Fimbul Ice Shelf
| Title |
Antarctica: Fimbul Ice Shelf Fly-over |
| Completed |
1999-11-08 |
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Antarctica: Fimbul Ice Shelf
| Title |
Antarctica: Fimbul Ice Shelf Fly-over |
| Completed |
1999-11-08 |
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Total Ozone over Antarctica
| Title |
Total Ozone over Antarctica from TOMS: July 1, 1998 through October 1, 1998 (With Dates) |
| Completed |
1998-10-02 |
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Moving Along Antarctica to t
| Title |
Moving Along Antarctica to the South Pole |
| Abstract |
This animation was originally grouped with animation #1005. |
| Completed |
1999-11-08 |
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Chemical Model Animation of
| Title |
Chemical Model Animation of Chlorine Release from Reservoir Gases over Antarctica |
| Abstract |
Over the Antarctic continent, ice clouds form in the cold winter darkness. On the surface of the cloud particles, chlorine nitrate and hydrogen chloride react and release chlorine. The chlorine then reacts with ozone forming chlorine monoxide and starting the catalytic ozone destruction cycle. The massive ozone loss results in the development of the Antarctic ozone hole. |
| Completed |
1999-04-09 |
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TOMS Ozone over Antarctica:
| Title |
TOMS Ozone over Antarctica: August 1, 2000 to September 6, 2000 |
| Abstract |
In August of 2000, Earth Probe TOMS measured the largest ozone hole ever observed over Antarctica. |
| Completed |
2000-05-30 |
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Antarctica Morph through Tim
| Title |
Antarctica Morph through Time: Continental Zoom |
| Completed |
1998-12-31 |
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Antarctica Morph Through Tim
| Title |
Antarctica Morph Through Time: Ellsworth Land View |
| Completed |
1998-12-31 |
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Antarctica: Snow Dunes
| Title |
Antarctica: Snow Dunes |
| Completed |
1999-11-08 |
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Antarctica: Snow Dunes
| Title |
Antarctica: Snow Dunes |
| Completed |
1999-11-08 |
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Antarctica: Snow Dunes
| Title |
Antarctica: Snow Dunes |
| Completed |
1999-11-08 |
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Total Ozone Over Antarctica
| Title |
Total Ozone Over Antarctica from TOMS: October 3, 1999 |
| Abstract |
Total ozone over Antarctica for October 3, 1999 as measured by Earth Probe TOMS. Dark blue represents regions of low ozone and red represents regions of high ozone. |
| Completed |
2002-10-10 |
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ICESat First Light Release:
| Title |
ICESat First Light Release: Antarctica in Three Dimensions |
| Abstract |
ICESat's orbit was designed to maximize coverage over the great polar ice sheets, where ground tracks overlap to create an intricate grid of data points. The accumulation of these data points in the Southern Hemisphere results in a new three-dimensional elevation model of Antarctica. ICESat repeats its orbital pattern every eight days, allowing the GLAS instrument to measure changes over time in the same location. In order to measure ice sheet mass balance, the satellite's advanced technology is providing data on the critically important third dimension, elevation. |
| Completed |
2003-05-15 |
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ICESat First Light Release:
| Title |
ICESat First Light Release: Antarctica in Three Dimensions |
| Abstract |
ICESat's orbit was designed to maximize coverage over the great polar ice sheets, where ground tracks overlap to create an intricate grid of data points. The accumulation of these data points in the Southern Hemisphere results in a new three-dimensional elevation model of Antarctica. ICESat repeats its orbital pattern every eight days, allowing the GLAS instrument to measure changes over time in the same location. In order to measure ice sheet mass balance, the satellite's advanced technology is providing data on the critically important third dimension, elevation. |
| Completed |
2003-05-15 |
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Total Ozone over Antarctica
| Title |
Total Ozone over Antarctica from TOMS: Jul 1, 1998 through Oct 1, 1998 (Rotation to Pole with Dates) |
| Completed |
1998-10-02 |
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Antarctica: Dry Valleys
| Title |
Antarctica: Dry Valleys |
| Abstract |
Using the RADARSAT dataset of Antarctica, Scientist can visit the Dry Valleys, a cold and desert like area. |
| Completed |
1999-11-08 |
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Antarctica: Dry Valleys
| Title |
Antarctica: Dry Valleys |
| Abstract |
Using the RADARSAT dataset of Antarctica, Scientist can visit the Dry Valleys, a cold and desert like area. |
| Completed |
1999-11-08 |
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Antarctica: Dry Valleys
| Title |
Antarctica: Dry Valleys |
| Abstract |
Using the RADARSAT dataset of Antarctica, Scientist can visit the Dry Valleys, a cold and desert like area. |
| Completed |
1999-11-08 |
|
Total Ozone over Antarctica
| Title |
Total Ozone over Antarctica from TOMS: Jul 1, 1998 through Oct 1, 1998 Rotation to Pole without Dates |
| Completed |
1998-10-02 |
|
Great Zoom into Don Juan Pon
| Title |
Great Zoom into Don Juan Pond, Antarctica (treatment #2) |
| Abstract |
Antarctica is the coldest and most remote continent on Earth. It is also home to one of the most Mars-like places that scientists can study without actually traveling to the fourth planet. In this sequence we plunge from space down to a remarkably detailed view of a unique part of the Dry Valleys. By studying this place researchers think they might gain insight into how life on Mars might either survive now or have developed in the past. It is called the Don Juan Pond, and it's one of the saltiest, coldest bodies of water on Earth. The zoom passes through four different resolution data sets including data from Terra, Landsat, and IKONOS. This treatment uses an IKONOS inset that's enhanced to show detail. |
| Completed |
2003-12-18 |
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Great Zoom into Don Juan Pon
| Title |
Great Zoom into Don Juan Pond, Antarctica (treatment #2) |
| Abstract |
Antarctica is the coldest and most remote continent on Earth. It is also home to one of the most Mars-like places that scientists can study without actually traveling to the fourth planet. In this sequence we plunge from space down to a remarkably detailed view of a unique part of the Dry Valleys. By studying this place researchers think they might gain insight into how life on Mars might either survive now or have developed in the past. It is called the Don Juan Pond, and it's one of the saltiest, coldest bodies of water on Earth. The zoom passes through four different resolution data sets including data from Terra, Landsat, and IKONOS. This treatment uses an IKONOS inset that's enhanced to show detail. |
| Completed |
2003-12-18 |
|
Great Zoom into Don Juan Pon
| Title |
Great Zoom into Don Juan Pond, Antarctica (treatment #2) |
| Abstract |
Antarctica is the coldest and most remote continent on Earth. It is also home to one of the most Mars-like places that scientists can study without actually traveling to the fourth planet. In this sequence we plunge from space down to a remarkably detailed view of a unique part of the Dry Valleys. By studying this place researchers think they might gain insight into how life on Mars might either survive now or have developed in the past. It is called the Don Juan Pond, and it's one of the saltiest, coldest bodies of water on Earth. The zoom passes through four different resolution data sets including data from Terra, Landsat, and IKONOS. This treatment uses an IKONOS inset that's enhanced to show detail. |
| Completed |
2003-12-18 |
|
Great Zoom into Don Juan Pon
| Title |
Great Zoom into Don Juan Pond, Antarctica (treatment #2) |
| Abstract |
Antarctica is the coldest and most remote continent on Earth. It is also home to one of the most Mars-like places that scientists can study without actually traveling to the fourth planet. In this sequence we plunge from space down to a remarkably detailed view of a unique part of the Dry Valleys. By studying this place researchers think they might gain insight into how life on Mars might either survive now or have developed in the past. It is called the Don Juan Pond, and it's one of the saltiest, coldest bodies of water on Earth. The zoom passes through four different resolution data sets including data from Terra, Landsat, and IKONOS. This treatment uses an IKONOS inset that's enhanced to show detail. |
| Completed |
2003-12-18 |
|
Great Zoom into Don Juan Pon
| Title |
Great Zoom into Don Juan Pond, Antarctica (treatment #2) |
| Abstract |
Antarctica is the coldest and most remote continent on Earth. It is also home to one of the most Mars-like places that scientists can study without actually traveling to the fourth planet. In this sequence we plunge from space down to a remarkably detailed view of a unique part of the Dry Valleys. By studying this place researchers think they might gain insight into how life on Mars might either survive now or have developed in the past. It is called the Don Juan Pond, and it's one of the saltiest, coldest bodies of water on Earth. The zoom passes through four different resolution data sets including data from Terra, Landsat, and IKONOS. This treatment uses an IKONOS inset that's enhanced to show detail. |
| Completed |
2003-12-18 |
|
Great Zoom into Don Juan Pon
| Title |
Great Zoom into Don Juan Pond, Antarctica (treatment #2) |
| Abstract |
Antarctica is the coldest and most remote continent on Earth. It is also home to one of the most Mars-like places that scientists can study without actually traveling to the fourth planet. In this sequence we plunge from space down to a remarkably detailed view of a unique part of the Dry Valleys. By studying this place researchers think they might gain insight into how life on Mars might either survive now or have developed in the past. It is called the Don Juan Pond, and it's one of the saltiest, coldest bodies of water on Earth. The zoom passes through four different resolution data sets including data from Terra, Landsat, and IKONOS. This treatment uses an IKONOS inset that's enhanced to show detail. |
| Completed |
2003-12-18 |
|
Antarctica: Lake Vostok
| Title |
Antarctica: Lake Vostok |
| Abstract |
Using RADARSAT data of Antarctica, one can see the abandoned Russian station that is on top of a frozen Lake Vostok. |
| Completed |
1999-11-08 |
|
Antarctica: Lake Vostok
| Title |
Antarctica: Lake Vostok |
| Abstract |
Using RADARSAT data of Antarctica, one can see the abandoned Russian station that is on top of a frozen Lake Vostok. |
| Completed |
1999-11-08 |
|
Antarctica: Lake Vostok
| Title |
Antarctica: Lake Vostok |
| Abstract |
Using RADARSAT data of Antarctica, one can see the abandoned Russian station that is on top of a frozen Lake Vostok. |
| Completed |
1999-11-08 |
|
Antarctica: Larsen Ice Shelf
| Title |
Antarctica: Larsen Ice Shelf Side by Side Comparison |
| Abstract |
In 1978, scientists predicted that global warming would lead to a disintegration of Antarctic Peninsula ice shelves. Spaceborne data indicate that this prediction may be coming true. In these before and after images, note the dramatic change in the apparent shoreline. Scientists captured the first image using the ERS-1 satellite in 1992. As seen in the second image, collected by RADARSAT in 1997, huge changes have come to the coastline. In 1995, a 2000 square kilometer section of the ice shelf collapsed into thousands of fragments that eventually drifted out to sea. Researchers are still debating why the ice shelf broke up so dramatically, and what significance the break up has for interpreting local versus global changes to the environment. Theories include a series of warmer than usual summers which may have caused high levels of surface melting, or an overall climate warming trend. |
| Completed |
1999-11-08 |
|
Antarctica: Larsen Ice Shelf
| Title |
Antarctica: Larsen Ice Shelf Side by Side Comparison |
| Abstract |
In 1978, scientists predicted that global warming would lead to a disintegration of Antarctic Peninsula ice shelves. Spaceborne data indicate that this prediction may be coming true. In these before and after images, note the dramatic change in the apparent shoreline. Scientists captured the first image using the ERS-1 satellite in 1992. As seen in the second image, collected by RADARSAT in 1997, huge changes have come to the coastline. In 1995, a 2000 square kilometer section of the ice shelf collapsed into thousands of fragments that eventually drifted out to sea. Researchers are still debating why the ice shelf broke up so dramatically, and what significance the break up has for interpreting local versus global changes to the environment. Theories include a series of warmer than usual summers which may have caused high levels of surface melting, or an overall climate warming trend. |
| Completed |
1999-11-08 |
|
MODIS Mosaic of Antarctica v
| Title |
MODIS Mosaic of Antarctica view of Pine Island and Thwaites Glacier without ICESat Topography |
| Abstract |
NASA has released a digital image map of the Antarctic continent and surrounding islands. The Moderate Resolution Imaging Spectroradiometer (MODIS) Mosaic of Antarctica (MOA) image map is a composite of 260 swaths comprised of both Terra and Aqua MODIS images acquired between November 20, 2003 and February 29, 2004. MOA provides a cloud-free view of the ice sheet, ice shelves, and land surfaces at a grid scale of 125 m and an estimated resolution of 150 m. All land areas south of 60° S that are larger than a few hundred meters are included in the mosaic. Also included are several persistent fast ice areas and grounded icebergs. |
| Completed |
2005-11-30 |
|
Antarctica: Amery Ice Shelf
| Title |
Antarctica: Amery Ice Shelf and Lambert Glacier fly-over |
| Completed |
1999-11-08 |
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Antarctica: Amery Ice Shelf
| Title |
Antarctica: Amery Ice Shelf and Lambert Glacier fly-over |
| Completed |
1999-11-08 |
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Antarctica: Amery Ice Shelf
| Title |
Antarctica: Amery Ice Shelf and Lambert Glacier fly-over |
| Completed |
1999-11-08 |
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Average October Ozone Levels
| Title |
Average October Ozone Levels Over Antarctica for 1979 to 1999 |
| Abstract |
For more information and related images, please go to (http://svs.gsfc.nasa.gov/stories/toms/index.html). Average September ozone levels over Antarctica for these years can be found in animation 710. |
| Completed |
1999-12-28 |
|
Average October Ozone Levels
| Title |
Average October Ozone Levels Over Antarctica for 1979 to 1999 |
| Abstract |
For more information and related images, please go to (http://svs.gsfc.nasa.gov/stories/toms/index.html). Average September ozone levels over Antarctica for these years can be found in animation 710. |
| Completed |
1999-12-28 |
|
Average October Ozone Levels
| Title |
Average October Ozone Levels Over Antarctica for 1979 to 1999 |
| Abstract |
For more information and related images, please go to (http://svs.gsfc.nasa.gov/stories/toms/index.html). Average September ozone levels over Antarctica for these years can be found in animation 710. |
| Completed |
1999-12-28 |
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