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Mir Dreams
| Title |
Mir Dreams |
| Explanation |
This dream-like image of Mir [ http://www.hq.nasa.gov/osf/mir/ ] was recorded by astronauts as the Space Shuttle Atlantis [ http://kids.msfc.nasa.gov/Rockets/ShuttleNames.asp ] approached the Russian space station prior to docking during the STS-76 mission [ http://spaceflight.nasa.gov/shuttle/archives/sts-76/ index.html ]. Sporting spindly appendages and solar panels, Mir resembles a whimsical flying insect hovering about 350 kilometers above New Zealand's [ http://www.rasnz.org.nz/index.htm ] South Island and the city of Nelson [ http://webnz.com/nelsonarts/foundations.html ], near Cook Strait [ http://www.south-pole.com/p0000071.htm ]. In late March 1996, Atlantis shuttled astronaut Shannon W. Lucid [ http://www.jsc.nasa.gov/Bios/htmlbios/lucid.html ] to Mir for a five month visit, increasing Mir's occupancy from 2 to 3. It returned to pick Lucid up and drop off astronaut John Blaha [ http://www.jsc.nasa.gov/Bios/htmlbios/blaha.html ] during the STS-79 mission [ http://www.ksc.nasa.gov/shuttle/missions/sts-79/mission-sts-79.html ] in August of that year. Since becoming operational in 1986, Mir has [ http://www.hq.nasa.gov/osf/mir/mirvis.html ] been visited by over 100 spacefarers from the nations of planet Earth including, Russia, the United States, Great Britain, Germany, France, Japan, Austria, Kazakhstan and Slovakia. After joint Shuttle-Mir [ http://spaceflight.nasa.gov/history/shuttle-mir/ ] training missions in support of the International Space Station [ http://spaceflight.nasa.gov/station/index.html ], continuous occupation of Mir ended in August 1999. Mir is still in orbit and its operation is now being pursued by commercial interests [ http://www.mirstation.com/index.html ]. |
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Mir Dreams
| Title |
Mir Dreams |
| Explanation |
This dream [ http://www.pbs.org/wgbh/nova/mir/day.html ]-like image of Mir [ http://www.pbs.org/wgbh/nova/mir/tour.html ] was recorded by astronauts as the Space Shuttle Atlantis [ http://kids.msfc.nasa.gov/Rockets/ShuttleNames.asp ] approached the Russian space station prior to docking during the STS-76 mission. Sporting spindly appendages and solar panels, Mir resembles a whimsical flying insect hovering about 350 kilometers above New Zealand's [ http://www.rasnz.org.nz/index.htm ] South Island and the city of Nelson near Cook Strait [ http://www.south-pole.com/p0000071.htm ]. In late March 1996, Atlantis shuttled astronaut Shannon W. Lucid [ http://www.jsc.nasa.gov/Bios/htmlbios/lucid.html ] to Mir for a five month visit, increasing Mir's occupancy from 2 to 3. It returned to pick Lucid up and drop off astronaut John Blaha [ http://www.jsc.nasa.gov/Bios/htmlbios/blaha.html ] during the STS-79 mission [ http://www.ksc.nasa.gov/shuttle/missions/sts-79/mission-sts-79.html ] in August of that year. Since becoming operational in 1986, Mir has [ http://www.cosmicimages.com/Mir/index.html ] been visited by over 100 spacefarers from the nations of planet Earth including, Russia, the United States, Great Britain, Germany, France, Japan, Austria, Kazakhstan and Slovakia. After joint Shuttle-Mir [ http://spaceflight.nasa.gov/history/shuttle-mir/ ] training missions in support of the International Space Station [ http://spaceflight.nasa.gov/station/index.html ], continuous occupation of Mir ended in August 1999. The Mir was deorbited [ http://antwrp.gsfc.nasa.gov/apod/ap010323.html ] in March 2001. |
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Mir Dreams
| Title |
Mir Dreams |
| Explanation |
This dream [ http://www.pbs.org/wgbh/nova/mir/day.html ]-like image of Mir [ http://www.pbs.org/wgbh/nova/mir/tour.html ] was recorded by astronauts as the space shuttle orbiter Atlantis [ http://kids.msfc.nasa.gov/Rockets/ShuttleNames.asp ] approached the Russian space station prior to docking during the STS-76 mission in 1996. Sporting spindly appendages and solar panels, Mir resembles a whimsical flying insect hovering about 350 kilometers above New Zealand's [ http://www.rasnz.org.nz/index.htm ] South Island and the city of Nelson near Cook [ http://www.south-pole.com/p0000071.htm ] Strait. Mir was launched 20 years ago [ http://www.russianspaceweb.com/mir.html ] this week, and served as a continuously occupied orbital outpost [ http://spaceflight.nasa.gov/history/shuttle-mir/ ] until August 1999. Mir was visited by over 100 spacefarers from the nations of planet Earth including, Russia, the United States, Great Britain, Germany, France, Japan, Austria, Kazakhstan and Slovakia. The Mir was deorbited [ http://antwrp.gsfc.nasa.gov/apod/ap010323.html ] in March 2001. |
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Perspective View of Budapest
…
nasa, nasaimageofthedaygalle
…
After draining the northern
…
PIA04952
| mediatype |
IMAGE |
| mediatype |
image |
| date |
2000-02-11 |
| creator |
NASA -- Image Courtesy www.jpl.nasa.gov/srtm/ SRTM Team NASA/JPL/NIMA |
| identifier |
PIA04952 |
|
Aerosols over Central and Ea
…
nasa, nasaimageofthedaygalle
…
Particulate air pollution is
…
PIA04325
| mediatype |
IMAGE |
| mediatype |
image |
| date |
2003-02-23 |
| creator |
NASA -- Image courtesy NASA/GSFC/LaRC/JPL, www-misr.jpl.nasa.gov/ MISR Team. Text by Clare Averill (Acro Service Corporation/JPL) |
| identifier |
PIA04325 |
|
Haze over Europe: Natural Ha
…
nasa, nasanaturalhazards
Particulate air pollution is
…
MISR_PIA04325
| mediatype |
IMAGE |
| mediatype |
image |
| date |
2003-03-28 |
| creator |
NASA -- NASA Image Of The Day |
| identifier |
MISR_PIA04325 |
|
Aerosols over Central and Ea
…
PIA04325
Sol (our sun)
Multi-angle Imaging SpectroR
…
| Title |
Aerosols over Central and Eastern Europe |
| Original Caption Released with Image |
Particulate air pollution is a complex mixture of particles of varying origins and compositions. Determining the type and abundance of tiny airborne particles, known as aerosols, is needed for monitoring air quality and for understanding climate change. During the last weeks of March 2003, unusually high and widespread aerosol pollution was detected over Europe by several satellite-borne instruments. The Multi-angle Imaging SpectroRadiometer (MISR) instrument aboard NASA's Terra satellite determines aerosol amount and information about particle properties by examining the variation in scene brightness at different view angles. These images and data products illustrate the amount of aerosols on two dates over parts of Central and Eastern Europe, from the Baltic Sea in the north to the Adriatic Sea in the south. Two groups of three panels are shown. Within each group, the left and center views are natural-color images from MISR's vertical-viewing (nadir) and most obliquely forward-viewing cameras, respectively, and the right-hand panel is a map of retrieved aerosol amount, parameterized by a quantity called the optical depth. A color scale is used to represent this quantity, and high aerosol amount is indicated by yellow or green pixels, and clearer skies are indicated by blue pixels. The left-hand group of panels is comprised of data acquired on February 23, 2003, when most of the land area was still partially frozen. The right-hand group of panels portrays the same area about one month later, on March 27. The nadir camera enables surface features to stand out most clearly, whereas MISR's oblique cameras enhance sensitivity to even thin layers of aerosols. In the March image, the only strong indications of haze from the nadir view are the thin tendrils of grayish pixels over the dark waters of the Baltic Sea. Although aerosols are conventionally difficult to discern over bright surfaces, MISR is able to produce an aerosol abundance map for both the earlier snow-covered scene and for the later date, though fewer successful retrievals were obtained in the winter data. Skies were relatively clear in the earlier view, and the high optical depths implied by the red pixels are probably blunders due either to the homogeneity of the underlying snow-covered surface or the presence of unscreened clouds. In contrast, the March data show a thick haze over most of the lower-elevation parts of the observed area. Optical depths are relatively lower over the Julian Alps and the mountains of western Croatia (just north of the Adriatic), whereas higher abundances are observed to the north of the mountains and over eastern Croatia. There is a gradual transition from higher optical depths in western Poland to lower optical depths in Lithuania and along the eastern coast of the Baltic. Higher optical depths are also indicated over much of Hungary, Slovakia and eastern Austria. Places where clouds or other factors precluded an aerosol retrieval are otherwise shown in, dark gray. An overview [ http://earthobservatory.nasa.gov/NaturalHazards/natural_hazards_v2.php3?img_id=8637 ] of the haze extent and meteorological conditions for March 28, 2003 is also available from the Sea-viewing Wide Field-of-view Sensor (SeaWiFS) sensor. The Multi-angle Imaging SpectroRadiometer observes the daylit Earth continuously and every 9 days views the entire globe between 82 degrees north and 82 degrees south latitude. These data products were generated from a portion of the imagery acquired during Terra orbits 16937 and 17403. The panels cover an area of about 380 kilometers x 1775 kilometers, and use data from blocks 43 to 55 within World Reference System-2 path 190. MISR was built and is managed by NASA's Jet Propulsion Laboratory,Pasadena, CA, for NASA's Office of Earth Science, Washington, DC. The Terra satellite is managed by NASA's Goddard Space Flight Center,Greenbelt, MD. JPL is a division of the California Institute ofTechnology. |
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Budapest, Hungary, Perspecti
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PIA04952
Sol (our sun)
C-Band Interferometric Radar
| Title |
Budapest, Hungary, Perspective View, SRTM Elevation Model with Landsat Overlay |
| Original Caption Released with Image |
(Landsat), After draining the northern flank of the Alps Mountains in Germany and Austria, the Danube River flows east as it enters this west-looking scene (upper right) and forms the border between Slovakia and Hungary. The river then leaves the border as it enters Hungary and transects the Transdanubian Mountains, which trend southwest to northeast. Upon exiting the mountains, the river turns southward, flowing past Budapest (purplish blue area) and along the western margin of the Great Hungarian Plain. South and west of the Danube, the Transdanubian Mountains have at most only about 400 meters (about 1300 feet) of relief but they exhibit varied landforms, which include volcanic, tectonic, fluvial (river), and eolian (wind) features. A thick deposit of loess (dust deposits likely blown from ancient glacial outwash) covers much of this area, and winds from the northwest, funneled between the Alps and the Carpathian Mountains, are apparently responsible for a radial pattern of erosional streaks across the entire region. This image was generated from a Landsat satellite image draped over an elevation model produced by the Shuttle Radar Topography Mission (SRTM). The view uses a 3-times vertical exaggeration to enhance topographic expression. The false colors of the scene result from displaying Landsat bands 1, 4, and 7 in blue, green, and red, respectively. Band 1 is visible blue light, but bands 4 and 7 are reflected infrared light. This band combination maximizes color contrasts between the major land cover types, namely vegetation (green), bare ground (red), and water (blue). Shading of the elevation model was used to further highlight the topographic features. Elevation data used in this image was acquired by the Shuttle Radar Topography Mission (SRTM) aboard the Space Shuttle Endeavour, launched on February 11, 2000. SRTM used the same radar instrument that comprised the Spaceborne Imaging Radar-C/X-Band Synthetic Aperture Radar (SIR-C/X-SAR) that flew twice on the Space Shuttle Endeavour in 1994. SRTM was designed to collect three-dimensional measurements of the Earth's surface. To collect the 3-D data, engineers added a 60-meter-long (200-foot) mast, installed additional C-band and X-band antennas, and improved tracking and navigation devices. The mission is a cooperative project between the National Aeronautics and Space Administration (NASA), the National Geospatial-Intelligence Agency (NGA) of the U.S. Department of Defense (DoD), and the German and Italian space agencies. It is managed by NASA's Jet Propulsion Laboratory, Pasadena, CA, for NASA's Earth Science Enterprise, Washington, DC. View Size: 133 kilometers (82 miles) wide, 90 kilometers (56 miles) distance Location: 47.5 degrees North latitude, 19.0 degrees East longitude Orientation: Looking West, 15 degrees down from horizontal, 3X vertical exaggeration Image Data: Landsat Bands 1, 4, 7 as blue, green, red respectively Date Acquired: February 2000 (SRTM), October 11, 1990 |
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