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Icy Bay, Alaska

Icy Bay, Alaska

From NASA's Operation IceBridge campaign in Alaska: A high altitude view of Icy Bay, in the Wrangell-Saint Elias Wilderness. Just a century ago, this body of water was covered in ice.

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On the edge of the Kalahari Desert in Namibia, sand dunes are encroaching onto once-fertile lands in the north. Healthy vegetation appears red in this image; in the center, notice the lone red dot. It is the result of a center-pivot irrigation system, evidence that at least one optimistic farmer continues to work the fields despite the approaching sand. This image was acquired by the Landsat 7 satellite on August 14, 2000. This is a false-color composite image made using near infrared, red and green wavelengths. The image has also been sharpened using the sensor's panchromatic band.
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Manam Volcano in Papua New Guinea, as seen from space on June 16, 2010. Located 13 kilometers (8 miles) off the coast of mainland Papua New Guinea, Manam forms an island 10 kilometers (6 miles) wide. It is a stratovolcano. The volcano has two summit craters, and although both are active, most historical eruptions have arisen from the southern crater. On June 16, the volcano released a thin, faint plume as clouds clustered at the volcano's summit. Rivulets of brown rock interrupt the carpet of green vegetation on the volcano’s slopes. White clouds partially obscure the satellite’s view of Manam. The clouds may be the result of water vapor from the volcano, but they may also have formed independently of volcanic activity. The volcanic plume appears as a thin blue-gray veil extending toward the northwest over the Bismarck Sea.
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These night-shining clouds were spotted over Billund, Denmark on July 15, 2010. These rare clouds are technically called "noctilucent" or "polar mesospheric" clouds, and form at high altitudes, 80 to 85 kilometers (50 to 53 miles) high, where the mesosphere is located. The clouds' high position in the atmosphere allows them to reflect sunlight long after the sun has dropped below the horizon. They only form when the temperature drops below –130 degrees Celsius (-200 degrees Fahrenheit), whereupon the scant amount of water high in the atmosphere freezes into ice clouds. This happens most often in countries at high northern and southern latitudes (above 50 degrees) in the summer, when the mesosphere is coldest. Studies suggest that night-shining clouds are becoming brighter and more common, which is linked to the mesosphere getting colder and more humid. These changes may be happening because of increased levels of heat-trapping greenhouse gases such as carbon dioxide and methane in the atmosphere. In the mesosphere, carbon dioxide radiates heat into space, causing cooling. More methane, on the other hand, puts more water vapor into the atmosphere, because sunlight breaks methane up into water molecules at high altitudes. Research is ongoing.
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The Sierra de Velasco Mountains dominate this image in northern Argentina. The Catamarca province is in the northern part of the image, and the La Rioja province is to the south. The streams are fed by runoff from the snow in the Andes Mountains to the north. These intermittent streams can dry up rapidly. The larger urban area near the bottom of the image is La Rioja, the capital of the province of La Rioja. This image was acquired by the Landsat 5 satellite on February 28, 1985.
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Video: Images created from GRACE data showing changes in Greenland ice mass since 2002.
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This simulated natural-color image shows the North and South Malosmadulu Atolls in the Maldives, an island republic in the northern Indian Ocean, southwest of India. The Maldives consists of a chain of almost 1200 small coral islands that are grouped into clusters of atolls. It is home to about a third of a million people. Arguably the lowest-lying country in the world, the average elevation is 1 meter (3.3 feet) above sea level. Waves triggered by the great tsunami of December 2004 spilled over sea walls to flood the capital with sandy water and then swept out just as suddenly. Residents fear this was a foreboding of disasters to come from sea level rise due to global warming. The image was taken on 22 December 2002, and covers an area of 51 x 90 kilometers (32 x 56 miles).
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Bombetoka Bay in northwestern Madagascar is an inlet of Mozambique Channel, and is at the mouth of the Betsiboka River. Just downstream is the second largest port of Madagascar, the town of Mahajanga, a road terminus and trade center that exports sugar, coffee, spices, cassava, vegetable oils, timber and vanilla. The surrounding area abounds in extensive coffee plantations. Simulated natural color image taken by the Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER) on August 23, 2000.
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Susitna Glacier, Alaska. Like rivers of liquid water, glaciers flow downhill, with tributaries joining to form larger rivers. But where water rushes, ice crawls. As a result, glaciers gather dust and dirt, and bear long-lasting evidence of past movements. Alaska’s Susitna Glacier reveals some of its long, grinding journey in this image, taken from space on August 27, 2009. The satellite image combines infrared, red and green wavelengths to form a false-color picture. Vegetation is red and the glacier’s surface is marbled with dirt-free blue ice and dirt-coated brown ice. Infusions of relatively clean ice push in from tributaries in the north. The glacier surface appears especially complicated near the center of the image, where a tributary has pushed the ice in the main glacier slightly southward. In the lower left corner of this image, meltwater lakes can be seen on top of the ice.
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This map shows the bright lights of cities and wildfires set against the inky black backdrop of night. The image is actually a composite of satellite data collected over a number of days in April 2012 and October 2012, and is the result of 312 orbits and 2.5 TB of information. The lights seen here are not just from cities; they are also from wildifires, lightning, gas flares and reflected moonlight. Because the image is a composite of several days’ worth of data, fires and other points of light may have been picked up by the satellite and integrated into the composite image even though they were temporary, making some rural locations (such as in Australia) seem brighter than they really are on a typical day.
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The beauty of Earth's atmosphere and the setting sun. Photo taken by an Expedition-15 crewmember on the International Space Station on June 3, 2007.
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Perhaps the most impressive of cloud formations, cumulonimbus (from the Latin for “pile” and “rain cloud”) clouds form due to vigorous convection (rising and overturning) of warm, moist and unstable air. Surface air is warmed by the sun-heated ground surface and rises; if sufficient atmospheric moisture is present, water droplets will condense as the air mass encounters cooler air at higher altitudes. The air mass itself also expands and cools as it rises due to decreasing atmospheric pressure, a process known as adiabatic cooling. This type of convection is common in tropical latitudes year-round and during the summer season at higher latitudes. As water in the rising air mass condenses and changes from a gas to a liquid state, it releases energy to its surroundings, further heating the surrounding air and leading to more convection and rising of the cloud mass to higher altitudes. This leads to the characteristic vertical “towers” associated with cumulonimbus clouds, an excellent example of which is visible in this astronaut photograph. If enough moisture is present to condense and heat the cloud mass through several convective cycles, a tower can rise to altitudes of approximately 10 kilometers at high latitudes and to 20 kilometers in the tropics before encountering a region of the atmosphere known as the tropopause—the boundary between the troposphere and the stratosphere. The tropopause is characterized by a strong temperature inversion. Beyond the tropopause, the air no longer gets colder as altitude increases. The tropopause halts further upward motion of the cloud mass. The cloud tops flatten and spread into an anvil shape, as illustrated by this astronaut photograph. The photo was taken from a viewpoint that was at an angle from the vertical, rather than looking straight down towards the Earth’s surface. The image, taken while the International Space Station was located over western Africa near the Senegal-Mali border, shows a fully formed anvil cloud with numerous smaller cumulonimbus towers rising near it. The high energy levels of these storm systems typically make them hazardous due to associated heavy precipitation, lightning, high wind speeds and possible tornadoes.
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Along Greenland's western coast, a small field of glaciers surrounds Baffin Bay. This image was acquired by the Landsat 7 satellite on September 3, 2000. It is a false-color composite image made using near-infrared, red and blue wavelengths. 
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Parts of the Atlantic, Gulf of Mexico and Caribbean Sea as seen from the International Space Station 220 miles above Earth, from the Cupola window. The image was taken on November 9, 2010 by one of the Expedition-25 crew members using a 16-millimeter f/2.8D lens, which gives the image a fish-eye effect.
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