STS-102 Earth Sciences and Image Analysis Photographic Highlights

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View larger image for STS102-303-17
STS102-303-17
Aswan High Dam in 6-meter Resolution from the International Space Station: Astronaut photography of the Earth from the International Space Station has achieved resolutions close to those available from commercial remote sensing satellites—with many photographs having spatial resolutions of less than six meters.

Astronauts take the photographs by hand and physically compensate for the motion of the spacecraft relative to the Earth while the images are being acquired. The achievement was highlighted in an article entitled “Space Station Allows Remote Sensing of Earth to within Six Meters” published in this week’s edition of Eos, Transactions of the American Geophysical Union. Lines painted on airport runways at the Aswan Airport served to independently validate the spatial resolution of the camera sensor.

For press information, read: International Space Station Astronauts Set New Standard for Earth Photography

For details, see Robinson, J. A. and Evans, C. A. 2002. Space Station Allows Remote Sensing of Earth to within Six Meters. Eos, Transactions, American Geophysical Union 83(17):185, 188.

See some of the other detailed photographs posted to Earth Observatory:
Pyramids at Giza
Bermuda
Downtown Houston

View larger image for STS102-331-12
STS102-331-12
Distributary Channels of the Orinoco River: Several meandering distributary channels of the Orinoco River are seen draining northward into the south side of the Gulf of Paria in eastern Venezuela. These sediment-laden channels carry a tremendous quantity of fluvial material that constantly changes the size and shapes of the shoreline and adjacent islands. An assortment of mud flats and sand bars, seen here as lighter colored features in the water, are affected both by stream flow and tidal forces. Although some sunglint (the sun's reflection off of the water surface) is evident in the image, there may also be some evidence of a sheen on the surface of the water that is caused by the oil drilling operations in the gulf. The extensive dark landscape identifies the flat, swampy coastal plains of northeast Venezuela that is covered by dense stands of vegetation.
View larger image for STS102-336-35
STS102-336-35
New England Area: The moderating influence of the Atlantic Ocean is visible along the coastline in this synoptic, southeast view of several New England states. The southern limit of the snow covered landscape can be traced from southeast Massachusetts (left center) westward along the northern shore of Long Island Sound and includes the northern end of New Jersey (right center). In addition to Long Island (center), other prominent features on this image includes: Cape Cod; Martha's Vineyard, Nantucket, and Block Islands; and the Hudson River (bottom center). Several southerly draining river systems are discernible in Connecticut and extensive wetlands are observed along New York and New Jersey coastal areas.
View larger image for STS102-716-25
STS102-716-25
Another New Lake in Egypt: As the Space Shuttle Atlantis passed over southern Egypt in mid-March 2001, the STS-102 astronauts were able to document new flooding in the Toshka region west of Lake Nasser. The formation of the Toshka Lakes in southern Egypt is part of Egypt's New Valley Project. The flooding of the region has been monitored by astronauts since 1998, and continues to show rapid changes.

An animation in a previous posting on the Earth Observatory links together several photographs of the region taken by astronauts to show the sequence of flooding in the Toshka depression. The last image of that sequence was acquired in September, 2000 (Image number STS106-716-96), and is included here for reference. Since September, flooding has occurred over a large area at the western end of the Toshka lakes. The region will be the location of large Egyptian agricultural developments that will support millions of people.

Compare to earlier images posted on Earth Observatory:
October 10, 2000 from the Moderate Resolution Imaging Spectroradiometer
December 1999 from the Space Shuttle.

View larger image for STS102-708-10
STS102-708-10
Salt Evaporation Ponds, Dead Sea: The complex of Jordanian salt evaporation ponds at the southern end of the Dead Sea has expanded significantly over the past dozen years. The western margin of the salt ponds marks the Jordan-Israel border. In August 1989, when the crew of Space Shuttle mission STS28 photographed the region, the northern extension did not exist and the large polygonal ponds in the northwestern and northeastern sectors had not been subdivided. In the view taken by the STS102 crew in March 2001, one can see that there has also been expansion at the southeastern end, and that levees now segment the northeastern wedge into four ponds.

Both sodium chloride and potassium salts are produced from the Dead Sea ponds. Salt-evaporation works are expanding throughout the world in response to increased manufacture of polyvinyl chloride (PVC) and other chemicals, for which salt is a principal feedstock. About 22.4 million metric tons of salt (sodium chloride) were consumed by the chemical industry in 1996. Other uses are in human and animal nutrition, water conditioning, and road de-icing.

View larger image for STS102-344-23
STS102-344-23
Mount Ararat (Agri Dagi), Turkey: Mount Ararat (16,940 feet, 5165 m) is the largest volcano in Turkey. Although not currently active, its most recent eruption has probably been within the last 10,000 years. It is located in extreme northeastern Turkey, near the borders with Iran and Armenia. Southwest of the main peak lies Little Ararat (12,877 feet, 3896 m). Ahora Gorge is a northeast-trending chasm dropping 6000feet from the top of the mountain and was the focus of a major earthquake in 1840. A number of claims by different explorers to have found remnants of Noah’s Ark on Mt. Ararat have led to continuing expeditions to the mountain, many of which have focused their searches on the gorge area.
View larger image for STS102-349-35
STS102-349-35
St. Vincent Island, Apalachicola River Delta, Florida: Beach ridges sweep in bands across St. Vincent Island, a coastal barrier about 120 km southwest of Tallahassee, Florida. These depositional features have accumulated over time on the barrier island, and chronicle the island's evolution. The swales between the ridges some of which are water-filled, creating elongated lakes represent periods of island accretion between intervals of beach ridge development. Each ridge in the series marks the location of the island shoreline. The oldest ridge, approximately 3000 years old, is on the north side. The youngest the berm of the modern beach is on the south-facing portion of the present-day Gulf beach.

The crew of Space Shuttle 102 used the reflection of the sun off water that lies in the swales between ridges to emphasize the variable topography of the beach ridge plain. Similar topography -- although formed in a different manner, combining river and marine deposition -- can be seen on the Po and Ebro river deltas of Italy and Spain, respectively, and on the Mississippi river coast of Louisiana.

St. Vincent Island, which lies between Cape San Blas and the town of Apalachicola on the Florida Panhandle, is a national wildlife refuge and an important breeding ground for loggerhead turtles. Sambar deer, a variety of Asian elk that can weigh as much as 700 pounds, roam the marshlands, and eastern gray wolves have been bred there. The deer were introduced in the early 1900s, when the island was a privately owned hunting ground for exotic game.

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