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Titan: Larger and Larger Lak …
Description Titan: Larger and Larger Lakes
Full Description This radar image, obtained by Cassini's radar instrument during a near-polar flyby on Feb. 22, 2007, shows a big island smack in the middle of one of the larger lakes imaged on Saturn's moon Titan. This image offers further evidence that the largest lakes are at the highest latitudes. The island is about 90 kilometers (62 miles) by 150 kilometers (93 miles) across, about the size of Kodiak Island in Alaska or the Big Island of Hawaii. The island may actually be a peninsula connected by a bridge to a larger stretch of land. As you go farther down the image, several very small lakes begin to appear, which may be controlled by local topography. This image was taken in synthetic aperture mode at 700 meter (2,300 feet) resolution. North is toward the left. The image is centered at about 79 north degrees north and 310 degrees west. The Cassini-Huygens mission is a cooperative project of NASA, the European Space Agency and the Italian Space Agency. The Jet Propulsion Laboratory, a division of the California Institute of Technology in Pasadena, manages the mission for NASA's Science Mission Directorate, Washington, D.C. The Cassini orbiter was designed, developed and assembled at JPL. The radar instrument was built by JPL and the Italian Space Agency, working with team members from the United States and several European countries. For more information about the Cassini-Huygens mission visit http://saturn.jpl.nasa.gov/home/index.cfm. Credit: NASA/JPL
Date February 27, 2007
A Bright Supernova in the Ne …
Title A Bright Supernova in the Nearby Galaxy NGC 2403
Deadly Earthquake, Xianjing …
Title Deadly Earthquake, Xianjing Province, China
Description A destructive earthquake of magnitude 6.4 rattled China?s Xinjiang province at 10:04 AM (local time) on February 24, 2003. Over 250 people were killed. This remote, flat, and mostly featureless area of western China (called the Tarim Basin by geologists) is different from most other regions with frequent earthquakes. Typical seismically active areas are mountainous, like Alaska and coastal California, and lie along the boundaries of tectonic plates. In contrast, the Tarim Basin (which lies on the Eurasian Plate) remains flat while it is being squeezed by the motion of the Indian Plate?which is 1000 km (620 miles) away. Instead of deforming into belts of mountain ranges, the Tarim Basin is transmitting force applied by the Indian Plate to the interior of Asia, where the Tian Shan mountains are rising. The Tian Shan can be seen at the top edge of the large image. The approximate epicenter of the earthquake is represented by a white dot in this image, acquired on August 29, 2001, (before the earthquake) by the Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER). ASTER is an instrument aboard NASA's Terra [ http://terra.nasa.gov/ ] satellite. The false-color image combines near-infrared, red, and green wavelengths. Crops, almost certainly irrigated, appear red in this scene, while barren landscape appears brown. Image courtesy NASA/GSFC/MITI/ERSDAC/JAROS, and U.S./Japan ASTER Science Team [ http://earthobservatory.nasa.gov/cgi-bin/redirect?http://asterweb.jpl.nasa.gov/ ]
Magnitude 7.9 Earthquake Str …
nasa, nasaimageofthedaygalle …
An intense earthquake struck …
alaska_dem_2002307
mediatype IMAGE
mediatype image
date 2002-11-03
creator NASA -- Image courtesy mapping-ak.wr.usgs.gov/research.html USGS Alaska Science Center
identifier alaska_dem_2002307
Northern Forest Affected by …
nasa, nasaimageofthedaygalle …
823-10827. * Arctic Climate …
forest_tundra_trend_iotd
mediatype IMAGE
mediatype image
date 2003
creator NASA -- (Map adapted from figures provided by Scott Goetz, www.whrc.org/ Woods Hole Research Center )
identifier forest_tundra_trend_iotd
Smoke Signals from the Alask …
nasa, nasaimageofthedaygalle …
Large, lightning-induced fir …
PIA04363
mediatype IMAGE
mediatype image
date 2004-06-30
creator NASA -- Image courtesy NASA/GSFC/LaRC/JPL, www-misr.jpl.nasa.gov/ MISR Team and Dominic Mazzoni (JPL). Text by Clare Averill (Raytheon/JPL).
identifier PIA04363
Warm Ocean Temperatures Blan …
PIA00556
Sol (our sun)
Altimeter
Title Warm Ocean Temperatures Blanket the Far-Western Pacific
Original Caption Released with Image These data, taken during a 10-day collection cycle ending March 9, 2001, show that above-normal sea-surface heights and warmer ocean temperatures(indicated by the red and white areas) still blanket the far-western tropical Pacific and much of the north (and south) mid-Pacific. Red areas are about 10centimeters (4 inches) above normal, white areas show the sea-surface height is between 14 and 32 centimeters (6 to 13 inches) above normal. This build-up of heat dominating the Western Pacific was first noted by TOPEX/Poseidon oceanographers more than two years ago and has outlasted the El Niño and La Niña events of the past few years. See: http://www.jpl.nasa.gov/elnino/990127.html . This warmth contrasts with the Bering Sea, Gulf of Alaska and tropical Pacific where lower-than-normal sea levels and cool ocean temperatures continue (indicated by blue areas). The blue areas are between 5 and 13centimeters (2 and 5 inches) below normal, whereas the purple areas range from 14 to 18 centimeters (6 to 7 inches) below normal. Actually, the near-equatorial ocean cooled through the fall of 2000 and into mid-winter and continues almost La Niña-like. Looking at the entire Pacific basin, the Pacific Decadal Oscillation's warm horseshoe and cool wedge pattern still dominates this sea-level height image. Most recent National Oceanic and Atmospheric Administration (NOAA) sea-surface temperature data also clearly illustrate the persistence of this basin-wide pattern. They are available at http://psbsgi1.nesdis.noaa.gov:8080/PSB/EPS/SST/climo.html The U.S.-French TOPEX/Poseidon mission is managed by JPL for NASA's Earth Science Enterprise, Washington, D.C. JPL is a division of the California Institute of Technology in Pasadena. For more information on the TOPEX/Poseidon project, see: http://topex-www.jpl.nasa.gov
Titan: Larger and Larger Lak …
PIA09180
Saturn
Radar Mapper
Title Titan: Larger and Larger Lakes
Original Caption Released with Image This radar image, obtained by Cassini's radar instrument during a near-polar flyby on Feb. 22, 2007, shows a big island smack in the middle of one of the larger lakes imaged on Saturn's moon Titan. This image offers further evidence that the largest lakes are at the highest latitudes. The island is about 90 kilometers (62 miles) by 150 kilometers (93 miles) across, about the size of Kodiak Island in Alaska or the Big Island of Hawaii. The island may actually be a peninsula connected by a bridge to a larger stretch of land. As you go farther down the image, several very small lakes begin to appear, which may be controlled by local topography. This image was taken in synthetic aperture mode at 700 meter (2,300 feet) resolution. North is toward the left. The image is centered at about 79 north degrees north and 310 degrees west. The Cassini-Huygens mission is a cooperative project of NASA, the European Space Agency and the Italian Space Agency. The Jet Propulsion Laboratory, a division of the California Institute of Technology in Pasadena, manages the mission for NASA's Science Mission Directorate, Washington, D.C. The Cassini orbiter was designed, developed and assembled at JPL. The radar instrument was built by JPL and the Italian Space Agency, working with team members from the United States and several European countries. For more information about the Cassini-Huygens mission visit http://saturn.jpl.nasa.gov/home/index.cfm [ http://saturn.jpl.nasa.gov ].
Shaded Relief Mosaic of Umna …
PIA03509
Sol (our sun)
AirSAR
Title Shaded Relief Mosaic of Umnak Island, Aleutian Islands, Alaska
Original Caption Released with Image This image is a shaded relief mosaic of Umnak Island in Alaska's Aleutian Islands. It was created with Airsar data that was geocoded and combined into this mosaic as part of a NASA-funded Alaska Digital Elevation Model Project at the Alaska Synthetic Aperture Radar Facility (ASF) at the University of Alaska Geophysical Institute in Fairbanks, Alaska. Airsar collected the Alaska data as part of its PacRim 2000 Mission, which took the instrument to French Polynesia, American and Western Samoa, Fiji, New Zealand, Australia, New Guinea, Indonesia, Malaysia, Cambodia, Philippines, Taiwan, South Korea, Japan, Northern Marianas, Guam, Palau, Hawaii and Alaska. Airsar, part of NASA's Airborne Science Program, is managed for NASA's Earth Science Enterprise by JPL. JPL is a division of the California Institute of Technology in Pasadena.
Perspective View of Umnak Is …
PIA03508
Sol (our sun)
AirSAR
Title Perspective View of Umnak Island, Aleutian Islands, Alaska (#2)
Original Caption Released with Image This image is a perspective view of Umnak Island, one of Alaska's Aleutian Islands. The active Okmok volcano appears in the center of the island. The image was created by draping a Landsat 7 Thematic Mapper image over a digital elevation mosaic derived from Airsar data. This work was conducted as part of a NASA-funded Alaska Digital Elevation Model Project at the Alaska Synthetic Aperture Radar Facility (ASF) at the University of Alaska Geophysical Institute in Fairbanks, Alaska. Airsar collected the Alaska data as part of its PacRim 2000 Mission, which took the instrument to French Polynesia, American and Western Samoa, Fiji, New Zealand, Australia, New Guinea, Indonesia, Malaysia, Cambodia, Philippines, Taiwan, South Korea, Japan, Northern Marianas, Guam, Palau, Hawaii and Alaska. Airsar, part of NASA's Airborne Science Program, is managed for NASA's Earth Science Enterprise by JPL. JPL is a division of the California Institute of Technology in Pasadena.
Perspective View of Umnak Is …
PIA03507
Sol (our sun)
AirSAR
Title Perspective View of Umnak Island, Aleutian Islands, Alaska (#1)
Original Caption Released with Image This image is a perspective view of Umnak Island, one of Alaska's Aleutian Islands. The active Okmok volcano appears in the center of the island. The image was created by draping a Landsat 7 Thematic Mapper image over a digital elevation mosaic derived from Airsar data. This work was conducted as part of a NASA-funded Alaska Digital Elevation Model Project at the Alaska Synthetic Aperture Radar Facility (ASF) at the University of Alaska Geophysical Institute in Fairbanks, Alaska. Airsar collected the Alaska data as part of its PacRim 2000 Mission, which took the instrument to French Polynesia, American and Western Samoa, Fiji, New Zealand, Australia, New Guinea, Indonesia, Malaysia, Cambodia, Philippines, Taiwan, South Korea, Japan, Northern Marianas, Guam, Palau, Hawaii and Alaska. Airsar, part of NASA's Airborne Science Program, is managed for NASA's Earth Science Enterprise by JPL. JPL is a division of the California Institute of Technology in Pasadena.
Mt. Pinatubo, Phillipines - …
PIA03513
Sol (our sun)
AirSAR
Title Mt. Pinatubo, Phillipines - Comparison of November, 1996 and September, 2000
Original Caption Released with Image Built, operated and managed by the Jet Propulsion Laboratory, Pasadena, Calif., AIRSAR is part of NASA's Earth Science Enterprise program. JPL is a division of the California Institute of Technology in Pasadena., The effects of the June 15, 1991, eruption of Mt. Pinatubo continue to affect the lives of people living near the volcano on the island of Luzon in the Philippines. The eruption produced a large amount of volcanic debris that was deposited on the flanks of the volcano as part of pyroclastic flows. This debris consists of unconsolidated ash and boulders, and following heavy rains, it mixes with the rain run-off to form volcanic mudflows called lahars. Lahars are moving rivers of concrete slurry that are highly erosive. They can sweep down existing river valleys, carving deep canyons where the slopes are steep, or depositing a mixture of fine ash and larger rocks on the gentler slopes. The deposits left from a lahar soon solidify into a material similar to concrete, but while they are moving, lahars are dynamic features, and in a single river valley, the active channel may change locations within a few minutes or hours. These changes represent a significant natural hazard to local communities. These images from the NASA's airborne imaging radar AIRSAR instrument show two snapshots in the evolution of the lahars in the lower Pasig-Potrero River, just north of the town of Bacalor, east of the summit of the volcano. These images were collected on November 29, 1996 and September 25, 2000. The radar is particularly good at picking out spatial variations in the average particle size of the lahar deposits, which show up as a variety of different colored units at lower right. The active river channel is dark in both images, and is particularly well-defined in the September 2000 image. In the November 1996 image, the area of the flooded channel is much wider, so that the radar images are quite effective at showing where the drier surface materials are located. Also visible as a series of linear features in both images is a series of concrete dikes that have been constructed to protect the adjacent agricultural land from the lahar deposits. Some of this land has recently been developed as fish ponds, which are visible in the lower left of the 2000 image as a series of small, dark blue rectangles. Scientists have been using airborne radar data collected by NASA's AIRSAR instrument in their studies of the aftereffects of the Mt. Pinatubo eruption. AIRSAR collected imaging radar data over the volcano during a mission to the Pacific Rim region in late 1996 and on a follow-up mission to the area in late 2000. These data sets, along with remote sensing data collected from satellites, provide valuable information about the dynamic landscape and its hazards. AIRSAR collects radar interferometry used to produce digital elevation models. By comparing topographic data collected in 1996 and again in 2000, volcanologists can study how the shape and size of the volcano is changing. The detailed topography is also used to determine the highest risk areas for lahars to flow. AIRSAR flies aboard a NASA DC-8 based at NASA's Dryden Flight Research Center, Edwards, Calif.
Perspective View of Okmok Vo …
PIA03511
Sol (our sun)
AirSAR
Title Perspective View of Okmok Volcano, Aleutian Islands, Alaska (#2)
Original Caption Released with Image This perspective view shows the caldera of the Okmok volcano in Alaska's Aleutian Islands. The shaded relief was generated from and draped over an Airsar-derived digital elevation mosaic. Airsar collected the Alaska data as part of its PacRim 2000 Mission, which took the instrument to French Polynesia, American and Western Samoa, Fiji, New Zealand, Australia, New Guinea, Indonesia, Malaysia, Cambodia, Philippines, Taiwan, South Korea, Japan, Northern Marianas, Guam, Palau, Hawaii and Alaska. Airsar, part of NASA's Airborne Science Program, is managed for NASA's Earth Science Enterprise by JPL. JPL is a division of the California Institute of Technology in Pasadena.
Perspective View of Okmok Vo …
PIA03510
Sol (our sun)
AirSAR
Title Perspective View of Okmok Volcano, Aleutian Islands, Alaska (#1)
Original Caption Released with Image This perspective view shows the caldera of the Okmok volcano in Alaska's Aleutian Islands. The shaded relief was generated from and draped over an Airsar-derived digital elevation mosaic. Airsar collected the Alaska data as part of its PacRim 2000 Mission, which took the instrument to French Polynesia, American and Western Samoa, Fiji, New Zealand, Australia, New Guinea, Indonesia, Malaysia, Cambodia, Philippines, Taiwan, South Korea, Japan, Northern Marianas, Guam, Palau, Hawaii and Alaska. Airsar, part of NASA's Airborne Science Program, is managed for NASA's Earth Science Enterprise by JPL. JPL is a division of the California Institute of Technology in Pasadena.
Mt. Pinatubo, Phillippines - …
PIA03512
Sol (our sun)
AirSAR
Title Mt. Pinatubo, Phillippines - Perspective View
Original Caption Released with Image The effects of the June 15, 1991, eruption of Mt. Pinatubo continue to affect the lives of people living near the volcano on the island of Luzon in the Philippines. The eruption produced a large amount of volcanic debris that was deposited on the flanks of the volcano as part of pyroclastic flows. This perspective view looking toward the east shows the western flank of the volcano where most of these pyroclastic flows were deposited. This debris consists of ash and boulders that mix with water after heavy rains to form volcanic mudflows called lahars. Lahars are moving rivers of concrete slurry that are highly erosive. They can sweep down existing river valleys, carving deep canyons where the slopes are steep, or depositing a mixture of fine ash and larger rocks on the gentler slopes. The deposits left from a lahar soon solidify into a material similar to concrete, but while they are moving, lahars are dynamic features, and in a single river valley the active channel may change locations within a few minutes or hours. These changes represent a significant natural hazard to local communities. The topographic data were collected by NASA's airborne imaging radar AIRSAR instrument on November 29, 1996. Colors are from the French SPOT satellite imaging data in both visible and infrared wavelengths collected in February 1996. Areas of vegetation appear red and areas without vegetation appear light blue. River valleys radiate out from the summit of the volcano (upper center). Since the eruption, lahars have stripped these valleys of any vegetation. The Pasig-Potrero River flows to the northeast off the summit in the upper right of the image. Scientists have been using airborne radar data collected by the AIRSAR instrument in their studies of the aftereffects of the Mt. Pinatubo eruption. AIRSAR collected imaging radar data over the volcano during a mission to the Pacific Rim region in late 1996 and on a follow-up mission to the area in late 2000. These data sets along with remote sensing data collected from satellites provide valuable information on the dynamic landscape and the hazards that it poses. AIRSAR flies aboard a NASA DC-8 based at NASA's Dryden Flight Research Center, Edwards, Calif. Built, operated and managed by the Jet Propulsion Laboratory, Pasadena, Calif., AIRSAR is part of NASA's Earth Science Enterprise program. JPL is a division of the California Institute of Technology in Pasadena.
MISR Sights the Bering Strai …
PIA02638
Sol (our sun)
Multi-angle Imaging SpectroR …
Title MISR Sights the Bering Strait
Original Caption Released with Image With the Seward Peninsula of Alaska to the east, and Chukotskiy Poluostrov of Siberia to the west, the Bering Strait separates the United States and the Russian Federation by only 90 kilometers. It is named for Danish explorer Vitus Bering, who spotted the Alaskan mainland in 1741 while leading an expedition of Russian sailors. This view of the region was captured by MISR's vertical-viewing (nadir) camera on August 18, 2000 during Terra orbit 3562. The boundary between the US and Russia lies between Big and Little Diomede Islands, which are visible in the middle of the Bering Strait. The Arctic Circle, at 66.5 degrees north latitude, runs through the Arctic Ocean in the top part of this image. This circle marks the southernmost latitude for which the Sun does not rise above the horizon on the day of the winter solstice. At the bottom of this image is St. Lawrence Island. Situated in the Bering Sea, it is part of Alaska and home to Yupik Eskimos. 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 of Technology. For more information: http://www-misr.jpl.nasa.gov
AIRS Storm Front Approaching …
PIA07938
Sol (our sun)
Atmospheric Infrared Sounder …
Title AIRS Storm Front Approaching California (animation)
Original Caption Released with Image Click on the image for the AIRS Storm Front Approaching California Animation NASA's Atmospheric Infrared Sounder instrument is able to peel back cloud cover to reveal 3-D structure of a storm's water vapor content, information that can be used to improve weather forecast models. In this animation the initial visible cloud image series shows a front moving toward the West Coast of the United States as a low pressure area moves into the Pacific Northwest. The "Pineapple Express," a stream of moisture that originates in the tropics South of Hawaii and usually crosses Mexico to enter New Mexico and Texas, has shifted Westward and is also visible moving into Baja California. The area preceding the front appears to be relatively clear in the visible images. As the view shifts from the visible to the infrared wavelengths which highlight water vapor, we see both cloud areas contain heavy burdens of moisture. The area which appears clear in the visible images is seen to contain water vapor near the coastline as well. The viewpoint then rotates so that we can see the vertical cross section of the fronts. The variability of the vertical extent of water vapor and the amount is now clearly visible. The storm moving in from the Gulf of Alaska is more heavily laden with water vapor than that moving in from the Southwest. The moisture is concentrated in the lower atmosphere. The colors indicate the amount of water vapor present. Blue areas denote low water vapor content, green areas are medium water vapor content, red areas signify high water vapor content. The vertical grid for the final frame ranges from 250 millibar pressure at the top to 1000 millibar pressure at the bottom. The top is about 10 km (6.2 miles) above the surface of the Earth. The Atmospheric Infrared Sounder Experiment, with its visible, infrared, and microwave detectors, provides a three-dimensional look at Earth's weather. Working in tandem, the three instruments can make simultaneous observations all the way down to the Earth's surface, even in the presence of heavy clouds. With more than 2,000 channels sensing different regions of the atmosphere, the system creates a global, 3-D map of atmospheric temperature and humidity and provides information on clouds, greenhouse gases, and many other atmospheric phenomena. The AIRS Infrared Sounder Experiment flies onboard NASA's Aqua spacecraft and is managed by NASA's Jet Propulsion Laboratory, Pasadena, Calif., under contract to NASA. JPL is a division of the California Institute of Technology in Pasadena.
MISR Stereo Imaging Distingu …
PIA02625
Sol (our sun)
Multi-angle Imaging SpectroR …
Title MISR Stereo Imaging Distinguishes Smoke from Cloud
Original Caption Released with Image These views of western Alaska were acquired by MISR on June 25, 2000 during Terra orbit 2775. The images cover an area of about 150 kilometers x 225 kilometers, and have been oriented with north to the left. The left image is from the vertical-viewing(nadir) camera, whereas the right image is a stereo "anaglyph" that combines data from the forward-viewing 45-degree and 60-degree cameras. This image appears three-dimensional when viewed through red/blue glasses with the red filter over the left eye. It may help to darken the room lights when viewing the image on a computer screen. The Yukon River is seen wending its way from upper left to lower right. A forest fire in the Kaiyuh Mountains produced the long smoke plume that originates below and to the right of image center. In the nadir view, the high cirrus clouds at the top of the image and the smoke plume are similar in appearance, and the lack of vertical information makes them hard to differentiate. Viewing the righthand image with stereo glasses, on the other hand, demonstrates that the scene consists of several vertically-stratified layers, including the surface terrain, the smoke, some scattered cumulus clouds, and streaks of high, thin cirrus. This added dimensionality is one of the ways MISR data helps scientists identify and classify various components of terrestrial scenes. 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 of Technology.
TOPEX/El Niño Watch - Strong …
PIA02935
Sol (our sun)
Altimeter
Title TOPEX/El Niño Watch - Strong, Long-lasting La Niña Just Fading Away, June 19, 2000
Original Caption Released with Image ."Let's not forget that the legacy of two years of La Niña will be with us this summer and into the fall," said JPL oceanographer Dr. William Patzert. "Much of the nation's farmland is really dry in many regions. The reality is that the atmosphere is still acting as though La Niña remains." The National Oceanic and Atmospheric Administration's (NOAA) National Weather Service has forecasted continuing drought for much of the midwestern and southeastern United States and an active hurricane season for our coming summer. NOAA seasonal forecasts can be found at http://www.cpc.ncep.noaa.gov [ http://www.cpc.ncep.noaa.gov ] . The U.S.-French TOPEX/Poseidon mission is managed by JPL for the NASA's Earth Science Enterprise, Washington, D.C. JPL is a division of the California Institute of Technology in Pasadena. For more information on the TOPEX/Poseidon project, see http://topex-www.jpl.nasa.gov [ http://topex-www.jpl.nasa.gov ], After dominating the tropical Pacific Ocean for more than two years, the 1998-2000 La Niña "cool pool" is continuing its slow fade and seems to be retiring from the climate stage, according to the latest satellite data from the U.S.-French TOPEX/Poseidon mission. These data, taken during a 10-day cycle of collection ending June 9, show that the equatorial Pacific continues to warm up and is returning to normal (green) as this latest, persistent, two-year La Niña episode is coming to an end. Only a few patches of cooler, lower sea levels (seen in blue and purple) remain across the tropics. It should be noted that in June 1999, La Niña barely had a pulse, but was resuscitated in fall 1999. (See June 1999 press release on that topic at http://www.jpl.nasa.gov/elnino/990629.html [ http://www.jpl.nasa.gov/elnino/990629.html ] .) The blue areas are between 5 and 13 centimeters (2 and 5 inches) below normal, whereas the purple areas range from 14 to 18 centimeters (6 to 7 inches) below normal. In the far-western tropical Pacific Ocean, the ocean remains higher and warmer than normal. In summary, it appears that the global climate system is finally emerging from the past three years of dramatic swings from the extra-large El Niño of 1997/1998, which was followed by two unusually cool and persistent La Niña years, according to scientists at NASA's Jet Propulsion Laboratory. But as the northern hemisphere summer begins, above-normal sea surface heights and warmer ocean temperatures (indicated by the red and white areas) still blanket the western equatorial Pacific and much of the north and south mid-Pacific. Red areas are about 10 centimeters (4 inches) above normal, white areas show the sea surface height is between 14 and 32 centimeters (6 to 13 inches) above normal. This contrasts with the Bering Sea and Gulf of Alaska region southward along the western coast of North America, where lower-than-normal sea levels and cool ocean temperatures continue, although this pattern is also weakening. A possible switch in this larger-than-El Niño/La Niña, slower-changing pattern -- the Pacific Decadal Oscillation -- was first noticed by many scientists in late 1998. See a January 2000 press release on that topic at http://www.jpl.nasa.gov/elnino/20000118.html [ http://www.jpl.nasa.gov/elnino/20000118.html ] , or for further information and graphics about the Pacific Decadal Oscillation, see http://topex-www.jpl.nasa.gov/discover/PDO.html [ http://topex-www.jpl.nasa.gov/discover/PDO.html ]
TOPEX El Niño/La Niña - Enti …
PIA01528
Sol (our sun)
Altimeter
Title TOPEX El Niño/La Niña - Entire Pacific is out of Whack, April 7, 1999
Original Caption Released with Image New sea surface height measurements from the TOPEX/Poseidon satellite show that the sea level and temperature of the entire Pacific is "out of balance," including a large area of abnormally cool water along the west coast of North America that scientists say will influence regional weather patterns along the west coast of the Americas this summer. Southern California's seasonal "June gloom" weather, caused by a marine layer that traps smog over the Los Angeles basin, may linger throughout the summer as a result, according to oceanographer Dr. William Patzert of JPL. "Our data certainly show that the unusual oceanic climatic conditions that gave rise to El Niño and La Niña are not returning to a normal state." he said. "Our planet's climate system continues to exhibit rather wild behavior. These large warm and cold, high and low sea levels are slow-developing and long-lasting, and will certainly influence global climate and weather for the coming summer and into next fall." The unusually cool water (areas of lower sea level shown in blue and purple) extends from the Gulf of Alaska along the North American coast, sweeping south-westward from Baja California, where it merges with the remnants of La Niña. The La Niña phenomenon's cool, lower sea levels across the equator continue to weaken and break into (purple) patches. The northwest Pacific continues to be warmer than normal, though the variations from normal are not as great as in recent months. Areas where the Pacific Ocean is normal appear in green. The data represented in the image were collected from May 12-22. TOPEX/Poseidon's sea-surface height measurements have provided scientists with a detailed view of the 1998-99 La Niña and the 1997-98 El Niño because the satellite's altimeter measures the changing sea-surface height with unprecedented precision. In this image, the purple areas are about 18 centimeters (7 inches) below normal, creating a deficit in the heat supply to the surface waters. The white areas show the sea surface is between 14 and 32 centimeters (6 to 13 inches) above normal, in the red areas, it's about 10 centimeters (4 inches) above normal. The TOPEX/Poseidon mission is managed by the Jet Propulsion Laboratory for NASA s Office of Earth Science, Washington, DC. JPL is a division of the California Institute of Technology, Pasadena, CA. For more information, please visit the TOPEX/Poseidon project web page at http://topex-www.jpl.nasa.gov
Ice Types in the Beaufort Se …
PIA04300
Sol (our sun)
Multi-angle Imaging SpectroR …
Title Ice Types in the Beaufort Sea, Alaska
Original Caption Released with Image Determining the amount and type of sea ice in the polar oceans is crucial to improving our knowledge and understanding of polar weather and long term climate fluctuations. These views from two satellite remote sensing instruments, the synthetic aperture radar (SAR) on board the RADARSAT satellite and the Multi-angle Imaging SpectroRadiometer (MISR), illustrate different methods that may be used to assess sea ice type. Sea ice in the Beaufort Sea off the north coast of Alaska was classified and mapped in these concurrent images acquired March 19, 2001 and mapped to the same geographic area. To identify sea ice types, the National Oceanic and Atmospheric Administration (NOAA) National Ice Center constructs ice charts using several data sources including RADARSAT SAR images such as the one shown at left. SAR classifies sea ice types primarily by how the surface and subsurface roughness influence radar backscatter. In the SAR image, white lines delineate different sea ice zones as identified by the National Ice Center. Regions of mostly multi-year ice (A) are separated from regions with large amounts of first year and younger ice (B-D), and the dashed white line at bottom marks the coastline. In general, sea ice types that exhibit increased radar backscatter appear bright in SAR and are identified as rougher, older ice types. Younger, smoother ice types appear dark to SAR. Near the top of the SAR image, however, red arrows point to bright areas in which large, crystalline "frost flowers" have formed on young, thin ice, causing this young ice type to exhibit an increased radar backscatter. Frost flowers are strongly backscattering at radar wavelengths (cm) due to both surface roughness and the high salinity of frost flowers, which causes them to be highly reflective to radar energy. Surface roughness is also registered by MISR, although the roughness observed is at a different spatial scale. Older, rougher ice areas are predominantly backward scattering to the MISR cameras, whereas younger, smoother ice types are predominantly forward scattering. The MISR map at right was generated using a statistical classification routine (called ISODATA) and analyzed using ice charts from the National Ice Center. Five classes of sea ice were found based upon the classification of MISR angular data. These are described, based on interpretation of the SAR image, by the image key. Very smooth ice areas that are predominantly forward scattering are colored red. Frost flowers are largely smooth to the MISR visible band sensor and are mapped as forward scattering. Areas mapped as blue are predominantly backward scattering, and the other three classes have statistically distinct angular signatures and fall within the middle of the forward/backward scattering continuum. Some areas that may be first year or younger ice between the multi year ice floes are not discernible to SAR, illustrating how MISR potentially can make a unique contribution to sea ice mapping. 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. This data product was generated from a portion of the imagery acquired during Terra orbit 6663. The MISR image has been cropped to include an area that is 200 kilometers wide, and utilizes data from blocks 30 to 33 within World Reference System-2 path 71. 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.
TOPEX/El Niño Watch - Los Ni …
PIA02969
Sol (our sun)
Altimeter
Title TOPEX/El Niño Watch - Los Niños may be Gone, But Pacific Pattern Remains August 14, 2000
Original Caption Released with Image After three years of El Niño and La Niña with their often devastating climate consequences, the Pacific is finally calming down in the tropics but still shows signs of being abnormal elsewhere, according to the latest satellite data from the U.S.-French TOPEX/Poseidon mission. These data, taken during a 10-day cycle of collection ending August 17, show that tropical Pacific sea levels, which indicate how much heat is stored in the ocean, have returned to near-normal (green) after three years of dramatic fluctuations. See http://www.jpl.nasa.gov/elnino/ . But as summer ends in the Northern Hemisphere, remnants of the past few years remain embedded in the upper ocean. Above-normal sea surface heights and warmer ocean temperatures (indicated by the red and white areas) still blanket the far-western tropical Pacific and much of the north (and south) mid-Pacific. Red areas are about 10 centimeters (4 inches) above normal, white areas show the sea surface height is between 14 and 32 centimeters (6 to 13 inches) above normal. This contrasts with the Bering Sea and Gulf of Alaska where lower-than-normal sea levels and cool ocean temperatures continue (indicated by blue areas), although this pattern is also weakening. The blue areas are between 5 and 13 centimeters (2 and 5 inches) below normal, whereas the purple areas range from 14 to 18 centimeters (6 to 7 inches) below normal. Looking at the entire Pacific basin, the Pacific Decadal Oscillation's (PDO) characteristic warm horseshoe and cool wedge pattern is still evident in this sea-level height image. The PDO is a long-term ocean temperature fluctuation of the Pacific Ocean that waxes and wanes approximately every 10 to 20 years. Most recent National Oceanic and Atmospheric Administration (NOAA) sea-surface temperature date also clearly illustrate the persistence of this basin-wide pattern. They are available at: http://psbsgi1.nesdis.noaa.gov:8080/PSB/EPS/SST/climo.html."The present calming started three to four months ago when the La Niña faded away," said oceanographer Dr. William Patzert of NASA's Jet Propulsion Laboratory, Pasadena, Calif. "It appears that the global climate system is finally recovering from the past three years of dramatic swings from the extra-large El Niño of 1997/1998, which was followed by two unusually cool and persistent La Niña years.""The good news is that we're finally out from under the El Niño and La Niña of the past three years," Patzert said. "Unfortunately, in the longer term, the reality is that the PDO pattern still dominates the Pacific and, in the short term, the atmosphere is still acting as though La Niña remains. The western United States continues hot and dry, and a larger than normal number of hurricanes are forecast by NOAA for both the Pacific and the Atlantic. Also for the remainder of the summer and into the fall, we are continuing to experience the legacy or hangover from El Niño and La Niña -- the devastating Western U.S. fires from the, Canadian to Mexican borders are one example." National Oceanic and Atmospheric Administration's (NOAA) National Weather Service has forecasted continuing heat in the Western United States and an active hurricane season for the end of summer and into the fall. NOAA seasonal forecasts can be found at: http://www.cpc.ncep.noaa.gov. This month marks the eighth anniversary of the launch of TOPEX/Poseidon, a mission that had been planned to last only three to five years. The satellite has orbited Earth more than 37,400 times and completed 290 10-day data collection cycles. More than 99 percent of all available mission data has been collected and archived by the operations team at JPL. The U.S.-French TOPEX/Poseidon mission is managed by JPL for the NASA's Earth Science Enterprise, Washington, D.C. JPL is a division of the California Institute of Technology in Pasadena. For more information on the TOPEX/Poseidon project, see http://topex-www.jpl.nasa.gov [ http://topex-www.jpl.nasa.gov ]
TOPEX/El Niño Watch - La Niñ …
PIA01526
Sol (our sun)
Altimeter
Title TOPEX/El Niño Watch - La Niña Hangs On, February 27, 1999
Original Caption Released with Image Propulsion Laboratory for NASA's Office of Earth Science, Washington, DC. JPL is a division of the California Institute of Technology, Pasadena, CA., The cold pool of water in the Pacific known as "La Niña" still persists, although it is slowly weakening, according to scientists studying new data from the U.S.-French TOPEX/Poseidon satellite. A new image, produced using sea-surface height measurements taken by the satellite, is available on the Internet at http://www.jpl.nasa.gov/elnino/. It shows sea-surface height on February 27, 1999 relative to normal ocean conditions, reflecting the heat content of the ocean. The low sea level or cold pool of water along the equator (shown in purple and blue), commonly referred to as La Niña, still dominates the equatorial Pacific Ocean. This La Niña, which first appeared in May through June 1998, still persists, although it is slowly weakening, scientists say. Given its persistence and present strength, the ocean cooling trend is expected to continue to exert a strong influence on global climate systems throughout the spring and into the early summer. This situation is similar to the 1997-1998 El Niño, which extended into early summer 1998. The world's oceans are the great reservoirs of heat that influence global climate because they can cool or heat the atmosphere above. This transfer of heat drives weather patterns across both land and sea. La Niña provides a physical link connecting the large, slow changes in the ocean with predictable changes in day-to-day weather."La Niña shifts the high-altitude weather highway known as the jet stream," said Dr. William Patzert, an oceanographer at NASA's Jet Propulsion Laboratory. "It funnels storm tracks to the Pacific Northwest, which has resulted in heavy rainfall and lots of snow in that region so far, as well as the upper Midwest. Much of the Southwest, by contrast, has been shielded from stormy weather and, as a result, has received significantly less precipitation than normal to date. This year's La Niña was average in its intensity, but at its peak, it was associated with a 15 to 20-centimeter deep trough (6 to 8 inches) in the central tropical Pacific," Patzert said. "The depression was correlated with a 2 to 3-degree Centigrade (about 3.5 to 5.5 degrees Fahrenheit) dip in normal ocean surface temperatures." The image also shows that the very large, unusual area of higher or warmer water (shown here in red and white) in the western Pacific Ocean, from the tropics to the Gulf of Alaska, continues to expand. Although the appearance of this feature is not fully understood, it is recognized as influential to overall weather and climate. The white areas in the image indicate that the sea-surface height is between 14 and 32 centimeters (6 to 13 inches) above normal, in the red areas, sea-surface height is about 10 centimeters (4 inches) above normal. The green areas indicate normal conditions. The purple areas are between 14 to 18 centimeters (6 to 7 inches) below normal, and the blue areas are between 5 to 13 centimeters (2 to 5 inches) below normal. The TOPEX/Poseidon mission is managed by the Jet
TOPEX/El Niño Watch - La Niñ …
PIA01586
Sol (our sun)
Altimeter
Title TOPEX/El Niño Watch - La Niña Barely Has a Pulse, June 18, 1999
Original Caption Released with Image Lingering just a month ago in the eastern Pacific Ocean, the La Niña phenomenon, with its large volume of chilly water, barely has a pulse this month, according to new satellite data from the U.S.-French TOPEX/Poseidon mission. The data, taken during a 10-day cycle of data collection ending June 18, show that the equatorial Pacific Ocean is warming up and returning to normal (green) as La Niña all but vanishes. The warming trend is most apparent in the equatorial Pacific Ocean, where only a few patches of cooler, low sea levels (seen in blue and purple) remain. The blue areas are between 5 and 13 centimeters (2 and 5 inches) below normal, whereas the purple areas range from 14 to 18 centimeters (6 to 7 inches) below normal. Like its counterpart, El Niño, a La Niña condition will influence global climate and weather until it has completely subsided. As summer begins in the northern hemisphere, lower-than-normal sea surface levels and cool ocean temperatures persist in the northeastern Gulf of Alaska and along the western coast of North America. In contrast, the trend is the opposite over most of the Pacific, where above-normal sea surface heights and warmer ocean temperatures (indicated by the red and white areas) appear to be increasing and dominating the overall Pacific Ocean. Red areas are about 10 centimeters (4 inches) above normal, white areas show the sea surface height is between 14 and 32 centimeters (6 and 13 inches) above normal. Scientists are not ready to administer last rites to La Niña, though. In the last 12 months, the pool of unusually cold water in the Pacific has shrunk (warmed) several times before cooling (expanding) again. This summer's altimeter data will help them determine whether La Niña has truly dissipated or whether they will see another resurgence of cool water in the Pacific. The TOPEX/Poseidon mission is managed by the Jet Propulsion Laboratory for NASA's Office of Earth Science, Washington, DC. JPL is a division of the California Institute of Technology, Pasadena, CA. For more information, please visit the TOPEX/Poseidon project web page at http://topex-www.jpl.nasa.gov/ [ http://topex-www.jpl.nasa.gov/ ]
Anchorage, AK
PIA02675
Sol (our sun)
ASTER
Title Anchorage, AK
Original Caption Released with Image Anchorage, Alaska and Cook Inlet are seen in this 30 by 30 km(19 by 19 miles) sub-image, acquired May 12, 2000 by the Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER). Orbiting at an altitude of 705 km (430 miles) on board NASA's Terra satellite, ASTER provides data at a resolution of 15 m (47 feet) and allows creation of this simulated natural color image. At the center of the image is the Ted Stevens Anchorage International Airport, in the upper right corner is Elmendorf Air Force Base. Dark green coniferous forests are seen in the northwest part of the image. A golf course, with its lush green fairways, is just south of the Air Force Base. Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER) is one of five Earth-observing instruments launched December 18, 1999, on NASA's Terra satellite. The instrument was built by Japan's Ministry of International Trade and Industry. A joint U.S./Japan science team is responsible for validation and calibration of the instrument and the data products. Dr. Anne Kahle at NASA's Jet Propulsion Laboratory, Pasadena, California, is the U.S. science team leader, Moshe Pniel of JPL is the project manager. ASTER is the only high-resolution imaging sensor on Terra. The primary goal of the ASTER mission is to obtain high-resolution image data in 14 channels over the entire land surface, as well as black and white stereo images. With revisit time of between 4 and 16 days, ASTER will provide the capability for repeat coverage of changing areas on Earth's surface. The broad spectral coverage and high spectral resolution of ASTER will provide scientists in numerous disciplines with critical information for surface mapping and monitoring dynamic conditions and temporal change. Examples of applications include monitoring glacial advances and retreats, potentially active volcanoes, thermal pollution, and coral reef degradation, identifying crop stress, determining cloud morphology and physical properties, evaluating wetlands, mapping surface temperature of soils and geology, and measuring surface heat balance.
Pacific Dictates Droughts an …
PIA05071
Sol (our sun)
Altimeter
Title Pacific Dictates Droughts and Drenchings
Original Caption Released with Image The latest remote sensing data from NASA's Jason satellite show that the equatorial Pacific sea surface levels are higher, indicating warmer sea surface temperatures in the central and west Pacific Ocean. This pattern has the appearance of La Niña rather than El Niño. This contrasts with the Bering Sea, Gulf of Alaska and U.S. West Coast where lower-than-normal sea surface levels and cool ocean temperatures continue (indicated by blue and purple areas). The image above is a global map of sea surface height, accurate to within 30 millimeters. The image represents data collected and composited over a 10-day period, ending on Jan 23, 2004. The height of the water relates to the temperature of the water. As the ocean warms, its level rises, and as it cools, its level falls. Yellow and red areas indicate where the waters are relatively warmer and have expanded above sea level, green indicates near normal sea level, and blue and purple areas show where the waters are relatively colder and the surface is lower than sea level. The blue areas are between 5 and 13 centimeters (2 and 5 inches) below normal, whereas the purple areas range from 14 to 18 centimeters (6 to 7 inches) below normal. The Jason satellite carries a dual-frequency radar altimeter. This instrument beams microwave pulses-at 13.6 and 5.3 Gigahertz, respectively-downward toward the Earth. To determine the ocean's height, the instrument precisely measures the time it takes for the microwave pulses to bounce off the surface and return to the spacecraft. This measure, multiplied by the speed of light, gives the range from the satellite to the ocean surface. (For more details, visit the Jason Website [ http://topex-www.jpl.nasa.gov ].) The joint U.S.-French Topex/Poseidon mission is managed by the JPL for NASA's Earth Science Enterprise, NASA Headquarters, Washington, D.C. JPL is a division of the California Institute of Technology in Pasadena. Research on Earth's oceans using Jason and other space-based capabilities is conducted by NASA's Earth Science Enterprise to better understand and protect our home planet. For more information on Topex/Poseidon, see http://topex-www.jpl.nasa.gov.
Smoke Signals from the Alask …
PIA04363
Sol (our sun)
Multi-angle Imaging SpectroR …
Title Smoke Signals from the Alaska and Yukon Fires
Original Caption Released with Image . Some of the smoke from these fires was detected as far away as New Hampshire. These visualizations were captured on June 30th by the Multi-angle Imaging SpectroRadiometer (MISR) on NASA's Terra spacecraft. Here, MISR distinguishes clouds from smoke and retrieves heights and optical depths for the smoke -- information which will help to improve models of how smoke aerosols are transported. The images cover an area extending from the Mackenzie Bay in northwest Canada, through the Alaskan Interior and along the Alaska-Yukon border, south to the Wrangell Mountains. The first panel in the series is a natural-color image from MISR's 60° forward viewing camera. Smoke plumes notable along the right-hand edge are situated southwest of the Peel River in the Yukon Territory, and plumes extending west from the left-hand edge are situated in the vicinity of the Yukon River and the town of Eagle at the Alaska-Canada border. In the lower portion of the image, thick smoke obscures the Wrangell Mountain range. The next panel in the series is a stereoscopic height field, in which topography, smoke plumes and clouds are all being detected. Analysis indicates that most of the smoke and many low clouds are situated at heights between about 1 and 4 kilometers above the surface, while a few high clouds attained much greater altitudes. The third panel from the left is a smoke mask, in which the image is classified as either non-smoke, or as smoke with low confidence (lc) or high confidence (hc), represented by the blue, red and green pixels, respectively. Many of the actual smoke "plumes" were identified as high-confidence smoke, including parts of plumes in the Peel River region (upper right) and Yukon River/Alaska-Canada border region (left-hand edge). This smoke mask is produced by a computerized "machine-learning" classifier which detects smoke by examining the spectral, textural, and angular features in the radiances from three oblique-viewing MISR cameras. Ultimately, the classifier will be trained to identify plume-like shapes, thus making it possible to automatically isolate plume heights from the stereo product. The right-hand panel displays MISR's aerosol optical depth retrieval, in which the brightness and contrast changes of the surface at different view angles are used to measure the attenuation of sunlight as it passes through a column of the atmosphere. Increasing amounts of smoke aerosol appear as green, yellow, orange and red pixels, and clearer skies are indicated by blue pixels. Areas where the aerosol optical depth could not be retrieved, either because the smoke was too thick to see the surface contrast or because the presence of clouds precluded a retrieval, are shown in dark gray. 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. The non-animated data products were generated from a portion of the imagery acquired, Large lightning-induced fires were active in Alaska and the Yukon Territory from mid-June to mid-July, 2004. Thick smoke particles filled the air during these fires, prompting Alaskan officials to issue air quality warnings [ http://airnow.gov/ ], during Terra orbits 24123. The still panels cover an area of about 400 kilometers 898 kilometers, and use data from blocks 35 to 41 within World Reference System-2 path 64. MISR was built and is managed by NASA's Jet Propulsion Laboratory, Pasadena, Calif., 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 of Technology.
TOPEX/El Niño Watch - Pacifi …
PIA02403
Sol (our sun)
Altimeter
Title TOPEX/El Niño Watch - Pacific ocean conditions are split: cold in east, hot in west, July 27, 1999
Original Caption Released with Image The North Pacific Ocean continues to run hot and cold, with abnormally low sea levels and cool waters in the northeastern Pacific contrasting with unusually high sea levels and warm waters in the northwestern Pacific. New imagery from the joint NASA and French space agency's TOPEX/Poseidon orbiting satellite, which celebrates its 7th launch anniversary next week, shows strongly contrasting ocean levels and temperatures on opposite sides of the north Pacific. This pattern was locked in more than four months ago, when a very strong, high-pressure system began to dominate northern Pacific atmospheric and ocean patterns. Present conditions will be slow to change, according to oceanographer Dr. William Patzert of NASA's Jet Propulsion Laboratory, Pasadena, CA, and will influence climate over North America into the fall."The north Pacific, which drives U.S. climate, is still extremely out of balance, with warm waters in the west and cool waters in the east," Patzert said. "When we see these large contrasts in the ocean, the weather delivery system -- the jet stream coming out of the north Pacific -- will do very unusual things. Like the stock market, we have a very volatile situation brought on by the persistence of these ocean imbalances." The latest sea-surface height measurements, available at http://www.jpl.nasa.gov/elnino/, reveal unusually cool water (shown in blue and purple) and lower sea levels (5 to 18 centimeters or 2 to 7 inches below normal) extending from the Gulf of Alaska along the coast of North America. The lower sea levels sweep south-southwest from Baja California, to merge with the remnants of La Niña. Cool, lower equatorial sea levels from La Niña remain weak, but are still evident along the equator. On the other side of the north Pacific, sea levels remain high (10 to 32 centimeters or 4 to 13 inches above normal) and temperatures are warm (shown in red and white). Normal sea levels appear in green. The data were collected on a 10-day data-gathering cycle taken July 18-27. Since its launch on August 10, 1992, TOPEX/Poseidon has performed nearly flawlessly, collecting information about the height of the sea's surface at an unprecedented accuracy of 4 centimeters (15 inches). Using this information, scientists from NASA and the Centre National d'Etudes Spatiales have been able to map and forecast the impact of the 1997-1998 El Niño and the La Niña that followed and continues to hang on."These highly accurate global measurements of the sea-surface height of our oceans have vastly improved our understanding of the oceans and how they exchange energy with Earth's atmosphere to alter the weather and climate," said Charles Yamarone, manager of JPL's Earth Science Flight Projects office. "The satellite has, in fact, produced the longest record of precision global ocean topography to date and given us a wealth of new information about ocean circulation.""Additionally, in the last seven years, we have seen many societal benefits, from TOPEX/Poseidon observations," Yamarone said. "Our data are being used to support a wide range of activities, including ship routing, cable laying, fisheries management and hurricane forecasting." Although La Niña appears to be waning, Patzert added, the ocean abnormality is probably not gone for good. "La Niña might be temporarily down, but she's definitely not out," he said. "What we are seeing from space in these wildly fluctuating sea levels and temperature variations is a continuing hangover from La Niña." The U.S./French TOPEX/Poseidon mission is managed by the Jet Propulsion Laboratory for NASA's Office of Earth Sciences, Washington, DC. JPL is a division of the California Institute of Technology, Pasadena, CA. For more information, please visit the TOPEX/Poseidon project web page at http://topex-www.jpl.nasa.gov/ [ http://topex-www.jpl.nasa.gov/ ]
TOPEX/El Niño Watch - La Niñ …
PIA02436
Sol (our sun)
Altimeter
Title TOPEX/El Niño Watch - La Niña Conditions Likely to Prevail, October 10, 1999
Original Caption Released with Image A repeat of last year's mild La Niña conditions -- with a stormy winter in the Pacific Northwest and a dry winter in the southwestern United States -- will be the likely outcome of sea-surface heights observed by NASA's TOPEX/Poseidon satellite, scientists say. TOPEX/Poseidon has detected lower than normal sea-surface heights in the eastern North Pacific and unusually high sea-surface heights in the western and mid-latitude Pacific. The height of the sea surface over a given area is an indicator of ocean temperature and other factors that influence climate. The latest measurements, taken during a 10-day data cycle October 5-15, are available at http://www.jpl.nasa.gov/elnino . Sea-surface height is shown relative to normal (green) and reveals cooler water (blue and purple) measuring about 14 centimeters (6 inches) lower in the eastern North Pacific, from the Gulf of Alaska to central Alaska, and along the equator. The cooling trend sets the stage for another La Niña this winter."A mirror image of that oceanic profile prevails in the western and mid-latitude Pacific Ocean, where higher than normal sea-surface heights (red and white) are currently about 20 centimeters or 8 inches. Unusually warm temperatures (shown in red and white) have persisted and topped last year's temperatures," said Dr. William Patzert, an oceanographer at NASA's Jet Propulsion Laboratory, Pasadena, CA."These unbalanced conditions will undoubtedly exert a very strong influence on climate over North America this fall and winter," Patzert said. "Our profile of high sea-surface heights and warm temperatures in the western Pacific Ocean contrasts with low sea-surface heights and cool conditions in the eastern and equatorial Pacific. Those conditions will have a powerful impact on the weather system delivering jet streams out of the North Pacific." Conditions are ripe for a stormy, wet winter in the Pacific Northwest and a dry, relatively rainless winter in Southern California and the Southwest, the data show. "Clearly, these unusual conditions, which have persisted for 2 1/2 years, will not be returning to normal any time soon," Patzert said. "This climate imbalance is big and we're definitely going through a decade of wild climatic behavior. But when we look back at the climate record over the past century, we've seen behavior like this before." The TOPEX/Poseidon satellite's measurements have provided scientists with a detailed view of the 1997-1999 El Niño/La Niña climate pattern by measuring the changing sea-surface height with unprecedented precision. For more information, please visit the TOPEX/Poseidon project web page at http://topex-www.jpl.nasa.gov/
TOPEX/El Niño Watch - Mild L …
PIA02437
Sol (our sun)
Altimeter
Title TOPEX/El Niño Watch - Mild La Niña Conditions Developing, November 12, 1999
Original Caption Released with Image Unusually warm ocean temperatures off Asia and cool waters in the eastern and equatorial Pacific are signaling La Niña's mild return, according to the latest sea-surface heights observed by the joint NASA-French space agency's TOPEX/Poseidon satellite. Lower than normal sea-surface heights in the eastern North Pacific and abnormally high sea-surface heights in the western and mid-latitude Pacific are expected to drive storms coming out of the Pacific this winter, the mission data indicate. Those conditions will most likely steer storms north into the Pacific Northwest and keep the southwestern United States dryer than normal. The latest measurements, processed after a 10-day data cycle November 4-13 at NASA's Jet Propulsion Laboratory, Pasadena, CA, are available at http://www.jpl.nasa.gov/elnino . Sea-surface height is shown relative to normal (green) and reveals cooler water(blue and purple) measuring between 8 and 24 centimeters (3 to 9 inches) lower than average in the eastern North Pacific, from the Gulf of Alaska to central Alaska, and along the equator. Unusual conditions persist in the western and mid-latitude Pacific Ocean as well, with higher than average sea-surface heights(red and white) of between 8 and 24 centimeters (3 to 9 inches). These areas of increased sea-surface height and unusually warm water were present last year, but the increase in height has surpassed last year's measurements. The TOPEX/Poseidon satellite's measurements over the last seven and a half years have provided scientists with a comprehensive record of the 1997-1999 El Niño/La Niña climate pattern by measuring changing sea-surface heights to within 4centimeters (1.5 inches) precision. The U.S./French mission is managed by the Jet Propulsion Laboratory for NASA's Earth Sciences Enterprise, Washington, DC. JPL is a division of the California Institute of Technology, Pasadena, CA. For more information, please visit the TOPEX/Poseidon project web page at http://topex-www.jpl.nasa.gov/
Summer in the Arctic Nationa …
PIA03419
Sol (our sun)
Multi-angle Imaging SpectroR …
Title Summer in the Arctic National Wildlife Refuge
Original Caption Released with Image This colorful image of the Arctic National Wildlife Refuge and the Beaufort Sea was acquired by the Multi-angle Imaging SpectroRadiometer's nadir (vertical-viewing) camera on August 16, 2000, during Terra orbit 3532. The swirling patterns apparent on the Beaufort Sea are small ice floes driven by turbulent water patterns, or eddies, caused by the interactions of water masses of differing salinity and temperature. By this time of year, all of the seasonal ice which surrounds the north coast of Alaska in winter has broken up, although the perennial pack ice remains further north. The morphology of the perennial ice pack's edge varies in response to the prevailing wind. If the wind is blowing strongly toward the perennial pack (that is, to the north), the ice edge will be more compact. In this image the ice edge is diffuse, and the patterns reflected by the ice floes indicate fairly calm weather. The Arctic National Wildlife Refuge (often abbreviated to ANWR) was established by President Eisenhower in 1960, and is the largest wildlife refuge in the United States. Animals of the Refuge include the 130,000-member Porcupine caribou herd, 180 species of birds from four continents, wolves, wolverine, polar and grizzly bears, muskoxen, foxes, and over 40 species of coastal and freshwater fish. Although most of ANWR was designated as wilderness in 1980, the area along the coastal plain was set aside so that the oil and gas reserves beneath the tundra could be studied. Drilling remains a topic of contention, and an energy bill allowing North Slope oil development to extend onto the coastal plain of the Refuge was approved by the US House of Representatives on August 2, 2001. The Refuge encompasses an impressive variety of arctic and subarctic ecosystems, including coastal lagoons, barrier islands, arctic tundra, and mountainous terrain. Of all these, the arctic tundra is the landscape judged most important for wildlife. From the coast inland to an average of 30-60 kilometers, arctic tundra dominates the coastal plain, until reaching the foothills of the Brooks Mountain Range. Beneath the tundra, a layer of permafrost reaches an average depth of 600 meters, restricting water drainage through the soil, and increasing the sensitivity of tundra vegetation to disturbance. Precipitation is scarce (less than 16 centimeters per year) and the small amount of melt water or rain that soaks into the tundra remains near the surface. This is why the coastal plain can be classified as a wetland. The western boundary of the Refuge is marked by the Canning River, about halfway between the center and left-hand side of the image, and the eastern boundary is near the right-hand edge at the US/Canadian border. The two permanent human settlements within the image area are Kaktovic near the tip of the large rounded peninsula, and Arctic Village south of the Brooks Range near the southern Refuge boundary. The area represented by the image is approximately 380 kilometers x 540, kilometers. 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 of Technology.
Pacific Decadal Oscillation
PIA03460
Sol (our sun)
Altimeter
Title Pacific Decadal Oscillation
Original Caption Released with Image Like fall and winter of 2000, this year's Topex/Poseidon satellite data shows that the Pacific ocean continues to be dominated by the strong Pacific Decadal Oscillation, which is larger than the El Niño/La Niña pattern. The data, taken during a ten-day collection cycle ending Oct. 29,2001, show that the near-equatorial ocean has been very quiet in the past year, and sea levels and sea surface temperatures are near normal. Above-normal sea surface heights and warmer ocean temperatures, indicated by the red and white areas, still blanket the far western tropical Pacific and much of the north mid-Pacific. Red areas are about 10 centimeters (4inches) above normal, white areas show the sea surface height is between 14 and 32 centimeters (6 to 13 inches) above normal. In the western Pacific, the buildup of the Pacific Decadal Oscillation pattern, first noted by Topex/Poseidon oceanographers more than three years ago, has outlasted both the El Niño and La Niña of the past few years. This warmth contrasts with the Bering Sea, Gulf of Alaska and the west coast of the United States, where lower than normal sea surface levels and cool ocean temperatures continue, as indicated by the blue areas. The blue areas are between 5 and 13 centimeters (2 and 5 inches) below normal, while the purple areas range from 14 to 18 centimeters (6 to 7 inches) below normal. According to oceanographer Dr. William Patzert of NASA's Jet Propulsion Laboratory, Pasadena, Calif., the striking similarity between data taken in 2000 and the same time period in 2001 indicates that winter weather forecasts for this year will be similar to last year. The joint U.S.-French Topex/Poseidon mission is managed by the JPL for NASA's Earth Science Enterprise, NASA Headquarters, Washington, D.C. JPL is a division of the California Institute of Technology in Pasadena. For more information on Topex/Poseidon, see the Topex/Poseidon Web Site [ http://topex-www.jpl.nasa.gov ].
Pacific Decadal Oscillation …
PIA03457
Sol (our sun)
Altimeter
Title Pacific Decadal Oscillation Still Rules in Pacific, No Niño Anytime Soon
Original Caption Released with Image These data, taken during a 10-day collection cycle ending August 18, 2001, show that above-normal sea-surface heights and warmer ocean temperatures(indicated by the red and white areas) still blanket the far-western tropical Pacific and much of the north (and south) mid-Pacific. Red areas are about 10 centimeters (4 inches) above normal, white areas show the sea-surface height is between 14 and 32 centimeters (6 to 13 inches) above normal. This build-up of heat dominating the Northern and Western Pacific was first noted by Topex/Poseidon oceanographers almost three years ago and has outlasted the El Niño and La Niña events of the past few years. Seehttp://www.jpl.nasa.gov/elnino/990127.html [ http://www.jpl.nasa.gov/elnino/990127.html ] . This warmth contrasts with the Bering Sea, Gulf of Alaska and Eastern tropical Pacific where lower-than-normal sea levels and cool ocean temperatures continue (indicated by blue areas). The blue areas are between 5 and 13 centimeters (2 and 5 inches) below normal, whereas the purple areas range from 14 to 18 centimeters (6 to 7 inches) below normal. Across the tropics, the equatorial ocean remains calm with no indication of any El Niño developing. Looking at the entire Pacific basin, the Pacific Decadal Oscillation's warm horseshoe in the North and West Pacific and cool wedge pattern in the Eastern Tropical Pacific still dominates this sea-level height image. Most recent National Oceanic and Atmospheric Administration sea-surface temperature data also clearly illustrate the persistence of this basin-wide pattern. They are available athttp://psbsgi1.nesdis.noaa.gov:8080/PSB/EPS/SST/climo.html [ http://psbsgi1.nesdis.noaa.gov:8080/PSB/EPS/SST/climo.html ] For more information on the TOPEX/Poseidon project, visit:http://sealevel.jpl.nasa.gov [ http://sealevel.jpl.nasa.gov ]. The U.S.-French TOPEX/Poseidon mission is managed by JPL for NASA's Earth Science Enterprise, Washington, D.C. JPL is a division of the California Institute of Technology in Pasadena.
Where is La Niña?
PIA04622
Sol (our sun)
Altimeter
Title Where is La Niña?
Original Caption Released with Image Since the weak El Niño event of last winter, the equatorial Pacific has cooled and oceanographers have been on a La Niña "watch." Thus far, equatorial waters have seesawed between cooling and the present slight warming. Elsewhere, the northern and northeastern Pacific Ocean remains quite cool and sea levels are much lower than normal. These cooler ocean waters off the U.S. West Coast have driven a cooler and foggier spring and early summer along the coast, and guided the North Pacific Jet Stream north, keeping the West and Southwest in the grip of a 5-year drought. Sea-surface heights are a measure of how much heat is stored in the ocean below to influence future planetary climate events. Jason scientists will continue to monitor the Pacific closely for further signs of La Niña formation and intensity, or not. These Jason data were taken during a 10-day collection cycle ending July 3, 2003. The near-equatorial ocean has been very quiet, although sea levels and sea-surface temperatures are near normal or slightly warmer throughout the far western and central equatorial Pacific. Red areas are about 10 centimeters (4 inches) above normal, white areas show the sea-surface height is between 14 and 32 centimeters (6 to 13 inches) above normal. This slight rise in sea levels (warming) contrasts with the Bering Sea, Gulf of Alaska and U.S. West Coast, where lower-than-normal sea-surface levels (blue areas) and cool ocean temperatures continue. The blue areas are between 5 and 13 centimeters (2 and 5 inches) below normal, and the purple areas range from 14 to 18 centimeters (6 to 7 inches) below normal. The joint U.S.-French Topex/Poseidon mission is managed by the JPL for NASA's Earth Science Enterprise, NASA Headquarters, Washington, D.C. JPL is a division of the California Institute of Technology in Pasadena. Research on Earth's oceans using Jason and other space-based capabilities is conducted by NASA's Earth Science Enterprise to better understand and protect our home planet. For more information on Topex/Poseidon, see http://topex-www.jpl.nasa.gov [ http://topex-www.jpl.nasa.gov ].
A Sandhill Crane searches fo …
Description A Sandhill Crane searches for food with its still-fuzzy fledgling by its side. The two, along with another adult crane, have been seen wandering the grassy areas in the KSC Launch Complex 39 area. Sandhill cranes range from Siberia, Alaska and Arctic islands to Michigan, Minnesota and California, from Florida to Texas. They prefer large freshwater marshes, prairie ponds and marshy tundra. KSC shares a boundary with the Merritt Island National Wildlife Refuge, which encompasses 92,000 acres that are a habitat for more than 331 species of birds, 31 mammals, 117 fishes, and 65 amphibians and reptiles. The marshes and open water of the refuge provide wintering areas for 23 species of migratory waterfowl, as well as a year-round home for great blue herons, great egrets, wood storks, cormorants, brown pelicans and other species of marsh and shore birds, as well as a variety of insects
Release Date 05/08/2000
While the sandhill crane par …
Description While the sandhill crane parents search for food in front of the Vehicle Assembly Building, their still-featherless baby nearby tests its voice. The cranes have been a constant sight in the Launch Complex 39 area during the month of May. Sandhill cranes range from Siberia, Alaska and Arctic islands to Michigan, Minnesota and California, from Florida to Texas. They prefer large freshwater marshes, prairie ponds and marshy tundra. KSC shares a boundary with the Merritt Island National Wildlife Refuge, which encompasses 92,000 acres that are a habitat for more than 331 species of birds, 31 mammals, 117 fishes, and 65 amphibians and reptiles. The marshes and open water of the refuge provide wintering areas for 23 species of migratory waterfowl, as well as a year-round home for great blue herons, great egrets, wood storks, cormorants, brown pelicans and other species of marsh and shore birds, as well as a variety of insects
Release Date 05/18/2000
A family of sandhill cranes …
Description A family of sandhill cranes searches for food on the grounds near the Vehicle Assembly Building. The cranes have been a constant sight in the Launch Complex 39 area during the month of May. Sandhill cranes range from Siberia, Alaska and Arctic islands to Michigan, Minnesota and California, from Florida to Texas. They prefer large freshwater marshes, prairie ponds and marshy tundra. KSC shares a boundary with the Merritt Island National Wildlife Refuge, which encompasses 92,000 acres that are a habitat for more than 331 species of birds, 31 mammals, 117 fishes, and 65 amphibians and reptiles. The marshes and open water of the refuge provide wintering areas for 23 species of migratory waterfowl, as well as a year-round home for great blue herons, great egrets, wood storks, cormorants, brown pelicans and other species of marsh and shore birds, as well as a variety of insects
Release Date 05/18/2000
A pair of Sandhill Cranes se …
Description A pair of Sandhill Cranes searches for food with their still-fluffy fledgling close by. The trio have been seen wandering the grassy areas in the KSC Launch Complex 39 area. Sandhill cranes range from Siberia, Alaska and Arctic islands to Michigan, Minnesota and California, from Florida to Texas. They prefer large freshwater marshes, prairie ponds and marshy tundra. KSC shares a boundary with the Merritt Island National Wildlife Refuge, which encompasses 92,000 acres that are a habitat for more than 331 species of birds, 31 mammals, 117 fishes, and 65 amphibians and reptiles. The marshes and open water of the refuge provide wintering areas for 23 species of migratory waterfowl, as well as a year-round home for great blue herons, great egrets, wood storks, cormorants, brown pelicans and other species of marsh and shore birds, as well as a variety of insects
Release Date 05/08/2000
KENNEDY SPACE CENTER, FLA. - …
Description KENNEDY SPACE CENTER, FLA. - White pelicans swim in a lake north of Kennedy Space Center. In the distance, at right, is a great blue heron. White pelicans winter from Florida and southern California south to Panama. Great blue herons range across the breadth of the United States, as well as north to Alaska and Canada and south to Mexico and the West Indies. The Center shares a boundary north, south and west with the 92,000-acre Merritt Island National Wildlife Refuge, which is a habitat for more than 310 species of birds, 25 mammals, 117 fishes and 65 amphibians and reptiles. The marshes and open water of the refuge also provide wintering areas for 23 species of migratory waterfowl, as well as a year-round home for great blue herons, great egrets, wood storks, cormorants, brown pelicans and other species of marsh and shore birds.
Release Date 04/05/2004
KENNEDY SPACE CENTER, FLA. - …
Description KENNEDY SPACE CENTER, FLA. -- This adult bald eagle rests on the ground near a pond close to S.R. 3 in NASA's Kennedy Space Center. Bald eagles live near large bodies of open water such as lakes, marshes, seacoasts and rivers, where there are plenty of fish to eat and tall trees for nesting and roosting. Bald eagles feed primarily on fish, but also eat small animals (ducks, coots, muskrats, turtles, rabbits, snakes, etc.) and occasional carrion (dead animals). They are sometimes seen among a gathering of vultures at the site of a fresh meal. Bald eagles have a presence in every U. S. state except Hawaii. Bald eagles use a specific territory for nesting (they mate for life), winter feeding or a year-round residence. Its natural domain is from Alaska to Baja, California, and from Maine to Florida. There are a dozen eagle nests both in KSC and in the Merritt Island National Wildlife Refuge, which surrounds KSC. The refuge includes several wading bird rookeries, many osprey nests, up to 400 manatees during the spring, and approximately 2,500 Florida scrub jays. It also is a major wintering area for migratory birds. More than 500 species of wildlife inhabit the refuge, with 15 considered federally threatened or endangered. Photo credit: NASA/George Shelton
Release Date 04/20/2007
KENNEDY SPACE CENTER, FLA. - …
Description KENNEDY SPACE CENTER, FLA. -- This adult bald eagle rests on the ground near a pond close to S.R. 3 in NASA's Kennedy Space Center. Bald eagles live near large bodies of open water such as lakes, marshes, seacoasts and rivers, where there are plenty of fish to eat and tall trees for nesting and roosting. Bald eagles feed primarily on fish, but also eat small animals (ducks, coots, muskrats, turtles, rabbits, snakes, etc.) and occasional carrion (dead animals). They are sometimes seen among a gathering of vultures at the site of a fresh meal. Bald eagles have a presence in every U. S. state except Hawaii. Bald eagles use a specific territory for nesting (they mate for life), winter feeding or a year-round residence. Its natural domain is from Alaska to Baja, California, and from Maine to Florida. There are a dozen eagle nests both in KSC and in the Merritt Island National Wildlife Refuge, which surrounds KSC. The refuge includes several wading bird rookeries, many osprey nests, up to 400 manatees during the spring, and approximately 2,500 Florida scrub jays. It also is a major wintering area for migratory birds. More than 500 species of wildlife inhabit the refuge, with 15 considered federally threatened or endangered. Photo credit: NASA/George Shelton
Release Date 04/20/2007
KENNEDY SPACE CENTER, FLA. - …
Description KENNEDY SPACE CENTER, FLA. -- The broad, distinctive bill is a primary feature of this northern shoveler, paddling in the waters of the Merritt Island National Wildlife Refuge at Kennedy Space Center. Typically found in western Canada, Alaska, Colorado and Southern California, it can also be found farther east and south, wintering in the United States along the southeast coast. The marshes and open water of the refuge provide wintering areas for 23 species of migratory waterfowl, as well as a year-round home for great blue herons, great egrets, wood storks, cormorants, brown pelicans and other species of marsh and shore birds. The 92,000-acre refuge is also habitat for more than 310 species of birds, 25 mammals, 117 fishes and 65 amphibians and reptiles
Release Date 01/25/1999
KENNEDY SPACE CENTER, FLA. - …
Description KENNEDY SPACE CENTER, FLA. -- A Rough-legged hawk stares at the landscape from a perch in a tree in the Merritt Island National Wildlife Refuge. This type of hawk is rarely seen in Florida, ranging from northern Alaska through Manitoba and Newfoundland and wintering from California east to Virginia. The 92,000-acre refuge, which shares a boundary with the Kennedy Space Center, is habitat for more than 310 species of birds, 25 mammals, 117 fishes and 65 amphibians and reptiles
Release Date 02/23/1999
KENNEDY SPACE CENTER, FLA. - …
Description KENNEDY SPACE CENTER, FLA. -- A Rough-legged Hawk fans its wings as it gently lands in a tree in the Merritt Island National Wildlife Refuge. This type of hawk is rarely seen in Florida, ranging from northern Alaska through Manitoba and Newfoundland and wintering from California east to Virginia. The 92,000-acre refuge, which shares a boundary with the Kennedy Space Center, is habitat for more than 310 species of birds, 25 mammals, 117 fishes and 65 amphibians and reptiles
Release Date 02/23/1999
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