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Browse All : Earth of Goddard Space Flight Center (GSFC) and California from 2006

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Hubble's Largest Galaxy Port …
Title Hubble's Largest Galaxy Portrait Offers a New High-Definition View
General Information What is Hubble Heritage? A monthly showcase of new and archival Hubble images. Go to the Heritage site. Giant galaxies weren?t assembled in a day. Neither was this Hubble Space Telescope image of the face-on spiral galaxy Messier 101 (M101). It is the largest and most detailed photo of a spiral galaxy that has ever been released from Hubble. The galaxy?s portrait is actually composed of 51 individual exposures taken with Hubble's Advanced Camera for Surveys and the Wide Field and Planetary Camera 2 in March 1994, September 1994, June 1999, November 2002, and January 2003. The newly composed image also includes elements from images from ground-based photos.
Hubble Finds that Earth is S …
Title Hubble Finds that Earth is Safe from One Class of Gamma-ray Burst
Hubble Finds that Earth is S …
Title Hubble Finds that Earth is Safe from One Class of Gamma-ray Burst
Hubble Finds that Earth is S …
Title Hubble Finds that Earth is Safe from One Class of Gamma-ray Burst
Hubble Finds that Earth is S …
Title Hubble Finds that Earth is Safe from One Class of Gamma-ray Burst
Hubble Finds that Earth is S …
Title Hubble Finds that Earth is Safe from One Class of Gamma-ray Burst
Hubble Snaps Baby Pictures o …
Title Hubble Snaps Baby Pictures of Jupiter's "Red Spot Jr.
Hubble Finds that Earth is S …
Title Hubble Finds that Earth is Safe from One Class of Gamma-ray Burst
Hubble Finds that Earth is S …
Title Hubble Finds that Earth is Safe from One Class of Gamma-ray Burst
Hubble Finds that Earth is S …
Title Hubble Finds that Earth is Safe from One Class of Gamma-ray Burst
Extraterrestrial Fireworks
Title Extraterrestrial Fireworks
General Information What is Hubble Heritage? A monthly showcase of new and archival Hubble images. Go to the Heritage site. NASA's Hubble Space Telescope has captured an image of a cosmic explosion that is quite similar to fireworks on Earth. In the nearby galaxy, the Small Magellanic Cloud, a massive star has exploded as a supernova, and begun to dissipate its interior into a spectacular display of colorful filaments. The greenish-blue supernova remnant, E0102, resides 50 light-years away from the edge of a bright glowing massive star-forming region.
The Carina Nebula: Star Birt …
Title The Carina Nebula: Star Birth in the Extreme
General Information What is Hubble Heritage? A monthly showcase of new and archival Hubble images. Go to the Heritage site. In celebration of the 17th anniversary of the launch and deployment of NASA's Hubble Space Telescope, a team of astronomers is releasing one of the largest panoramic images ever taken with Hubble's cameras. READ: Junior version of this article Amazing Space Learn about this story in the Star Witness, a science newspaper available on our sister site, Amazing Space. [ http://amazing-space.stsci.edu/news/archive/2007/02/ ] It is a 50-light-year-wide view of the central region of the Carina Nebula where a maelstrom of star birth &#151, and death &#151, is taking place. This image is a mosaic of the Carina Nebula assembled from 48 frames taken with Hubble's Advanced Camera for Surveys. The Hubble images were taken in the light of neutral hydrogen during March and July 2005. Color information was added with data taken in December 2001 and March 2003 at the Cerro Tololo Inter-American Observatory in Chile. Red corresponds to sulfur, green to hydrogen, and blue to oxygen emission.
Dusty Planetary Disks Around …
Title Dusty Planetary Disks Around Two Nearby Stars Resemble Our Kuiper Belt
General Information What is a News Nugget? News Nuggets are bulletins from the world of astronomy. These two bright debris disks of ice and dust appear to be the equivalent of our own solar system's Kuiper Belt, a ring of icy rocks outside the orbit of Neptune and the source of short-period comets. The disks encircle the types of stars around which there could be habitable zones and planets for life to develop. The disks seem to have a central area cleared of debris, perhaps by planets.
Hubble Finds that Earth is S …
Title Hubble Finds that Earth is Safe from One Class of Gamma-ray Burst
Hubble Finds that Earth is S …
Title Hubble Finds that Earth is Safe from One Class of Gamma-ray Burst
Antarctic Plumbing: Lake Eng …
Title Antarctic Plumbing: Lake Englehardt's Subglacial Hydraulic System
Abstract ICESat satellite laser altimeter elevation profiles from 2003-2006 collected over West Antarctica reveal numerous regions of temporally varying elevation. MODIS satellite imagery over roughly the same time period collaborates where these subglacial fluctuations have occurred. These observations have led scientists to conclude that subglacial water movement is happening in this lake region, revealing a widespread, dynamic subglacial water system that could provide important insights into ice flow and the mass balance of Antarctica's ice.
Completed 2007-02-13
Five-Year Average Global Tem …
Title Five-Year Average Global Temperature Anomalies from 1880 to 2006
Abstract Because of a rapid warming trend over the past 30 years, the Earth is now reaching and passing through the warmest levels seen in the last 12,000 years. This color-coded map shows a progression of changing global surface temperatures from 1880 to 2006, the warmest ranked year on record.
Completed 2006-09-20
Five-Year Average Global Tem …
Title Five-Year Average Global Temperature Anomalies from 1880 to 2006
Abstract Because of a rapid warming trend over the past 30 years, the Earth is now reaching and passing through the warmest levels seen in the last 12,000 years. This color-coded map shows a progression of changing global surface temperatures from 1880 to 2006, the warmest ranked year on record.
Completed 2006-09-20
Five-Year Average Global Tem …
Title Five-Year Average Global Temperature Anomalies from 1880 to 2006
Abstract Because of a rapid warming trend over the past 30 years, the Earth is now reaching and passing through the warmest levels seen in the last 12,000 years. This color-coded map shows a progression of changing global surface temperatures from 1880 to 2006, the warmest ranked year on record.
Completed 2006-09-20
Five-Year Average Global Tem …
Title Five-Year Average Global Temperature Anomalies from 1880 to 2006
Abstract Because of a rapid warming trend over the past 30 years, the Earth is now reaching and passing through the warmest levels seen in the last 12,000 years. This color-coded map shows a progression of changing global surface temperatures from 1880 to 2006, the warmest ranked year on record.
Completed 2006-09-20
Five-Year Average Global Tem …
Title Five-Year Average Global Temperature Anomalies from 1880 to 2006
Abstract Because of a rapid warming trend over the past 30 years, the Earth is now reaching and passing through the warmest levels seen in the last 12,000 years. This color-coded map shows a progression of changing global surface temperatures from 1880 to 2006, the warmest ranked year on record.
Completed 2006-09-20
Five-Year Average Global Tem …
Title Five-Year Average Global Temperature Anomalies from 1880 to 2006
Abstract Because of a rapid warming trend over the past 30 years, the Earth is now reaching and passing through the warmest levels seen in the last 12,000 years. This color-coded map shows a progression of changing global surface temperatures from 1880 to 2006, the warmest ranked year on record.
Completed 2006-09-20
Five-Year Average Global Tem …
Title Five-Year Average Global Temperature Anomalies from 1880 to 2006
Abstract Because of a rapid warming trend over the past 30 years, the Earth is now reaching and passing through the warmest levels seen in the last 12,000 years. This color-coded map shows a progression of changing global surface temperatures from 1880 to 2006, the warmest ranked year on record.
Completed 2006-09-20
Five-Year Average Global Tem …
Title Five-Year Average Global Temperature Anomalies from 1880 to 2006
Abstract Because of a rapid warming trend over the past 30 years, the Earth is now reaching and passing through the warmest levels seen in the last 12,000 years. This color-coded map shows a progression of changing global surface temperatures from 1880 to 2006, the warmest ranked year on record.
Completed 2006-09-20
Five-Year Average Global Tem …
Title Five-Year Average Global Temperature Anomalies from 1880 to 2006
Abstract Because of a rapid warming trend over the past 30 years, the Earth is now reaching and passing through the warmest levels seen in the last 12,000 years. This color-coded map shows a progression of changing global surface temperatures from 1880 to 2006, the warmest ranked year on record.
Completed 2006-09-20
Five-Year Average Global Tem …
Title Five-Year Average Global Temperature Anomalies from 1880 to 2006
Abstract Because of a rapid warming trend over the past 30 years, the Earth is now reaching and passing through the warmest levels seen in the last 12,000 years. This color-coded map shows a progression of changing global surface temperatures from 1880 to 2006, the warmest ranked year on record.
Completed 2006-09-20
Five-Year Average Global Tem …
Title Five-Year Average Global Temperature Anomalies from 1880 to 2006
Abstract Because of a rapid warming trend over the past 30 years, the Earth is now reaching and passing through the warmest levels seen in the last 12,000 years. This color-coded map shows a progression of changing global surface temperatures from 1880 to 2006, the warmest ranked year on record.
Completed 2006-09-20
Five-Year Average Global Tem …
Title Five-Year Average Global Temperature Anomalies from 1880 to 2006
Abstract Because of a rapid warming trend over the past 30 years, the Earth is now reaching and passing through the warmest levels seen in the last 12,000 years. This color-coded map shows a progression of changing global surface temperatures from 1880 to 2006, the warmest ranked year on record.
Completed 2006-09-20
Five-Year Average Global Tem …
Title Five-Year Average Global Temperature Anomalies from 1880 to 2006
Abstract Because of a rapid warming trend over the past 30 years, the Earth is now reaching and passing through the warmest levels seen in the last 12,000 years. This color-coded map shows a progression of changing global surface temperatures from 1880 to 2006, the warmest ranked year on record.
Completed 2006-09-20
Five-Year Average Global Tem …
Title Five-Year Average Global Temperature Anomalies from 1880 to 2006
Abstract Because of a rapid warming trend over the past 30 years, the Earth is now reaching and passing through the warmest levels seen in the last 12,000 years. This color-coded map shows a progression of changing global surface temperatures from 1880 to 2006, the warmest ranked year on record.
Completed 2006-09-20
Five-Year Average Global Tem …
Title Five-Year Average Global Temperature Anomalies from 1880 to 2006
Abstract Because of a rapid warming trend over the past 30 years, the Earth is now reaching and passing through the warmest levels seen in the last 12,000 years. This color-coded map shows a progression of changing global surface temperatures from 1880 to 2006, the warmest ranked year on record.
Completed 2006-09-20
Day Fire in Southern Califor …
Title Day Fire in Southern California
Description While the outline of a fire may be hidden by thick smoke in a photo-like, "natural-color" image, "false-color" images that use visible as well as short-wave or near-infrared light observed by remote-sensing instruments can reveal details on the ground. This pair of images shows the Day Fire in southern California northwest of Los Angeles on September 19, 2006. The images are based on data collected by an aircraft-based sensor called MASTER, [ http://masterweb.jpl.nasa.gov/ ] a simulator for two sensors on NASA's Terra [ http://terra.nasa.gov ] satellite. (NASA uses airborne simulators to cross-check the accuracy of satellite data.) In the natural-color version (bottom), dingy white smoke hangs over most of the scene, hiding the outline of the fire. But in the infrared-enhanced version (top), the actively burning areas around the perimeter of the blaze are obvious as glowing pink and yellow spots, while the smoke fades into a transparent blue. Unburned vegetation appears green, while the burned area appears in shades of brown and gold. The MASTER instrument simulates the Moderate Resolution Imaging Spectroradiometer (MODIS) [ http://modis.gsfc.nasa.gov ] and the Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER) sensors on Terra. The instrument can be mounted on several different aircraft, including NASA's ER-2 [ http://www.nasa.gov/centers/dryden/news/FactSheets/FS-046-DFRC.html ] and WB-57 [ http://jsc-aircraft-ops.jsc.nasa.gov/wb57/index.html ] airplanes. NASA images created by Jesse Allen, Earth Observatory, using data provided by the ER-2/MASTER team.
Day Fire in Southern Califor …
Title Day Fire in Southern California
Description While the outline of a fire may be hidden by thick smoke in a photo-like, "natural-color" image, "false-color" images that use visible as well as short-wave or near-infrared light observed by remote-sensing instruments can reveal details on the ground. This pair of images shows the Day Fire in southern California northwest of Los Angeles on September 19, 2006. The images are based on data collected by an aircraft-based sensor called MASTER, [ http://masterweb.jpl.nasa.gov/ ] a simulator for two sensors on NASA's Terra [ http://terra.nasa.gov ] satellite. (NASA uses airborne simulators to cross-check the accuracy of satellite data.) In the natural-color version (bottom), dingy white smoke hangs over most of the scene, hiding the outline of the fire. But in the infrared-enhanced version (top), the actively burning areas around the perimeter of the blaze are obvious as glowing pink and yellow spots, while the smoke fades into a transparent blue. Unburned vegetation appears green, while the burned area appears in shades of brown and gold. The MASTER instrument simulates the Moderate Resolution Imaging Spectroradiometer (MODIS) [ http://modis.gsfc.nasa.gov ] and the Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER) sensors on Terra. The instrument can be mounted on several different aircraft, including NASA's ER-2 [ http://www.nasa.gov/centers/dryden/news/FactSheets/FS-046-DFRC.html ] and WB-57 [ http://jsc-aircraft-ops.jsc.nasa.gov/wb57/index.html ] airplanes. NASA images created by Jesse Allen, Earth Observatory, using data provided by the ER-2/MASTER team.
Heat Wave in North America
Title Heat Wave in North America
Description Scorching summer sun, burning pavement, stinging sweat—normal for July. But in July 2006, temperatures climbed above average levels for the previous six years and stayed warm for several days. During mid-July, a heat wave settled over most of the United States, with air temperatures soaring past 100 degrees Fahrenheit (38 Celsius). Land surface temperatures climbed as well, as this image shows. Most of the United States and portions of Canada and Mexico were much warmer than they had been during the same period from 2000 to 2005. Deep red across the Midwest indicates that land surface temperatures were as much as 10 degrees Celsius warmer than the six-year average, and with the exception of the Pacific Northwest and a few other isolated region, the rest of the country was also warmer than average. The heat wave continued past the period shown here, through the end of July. In California alone, the heat killed at least 126 people, reported Reuters on July 29. This image was created from data collected by the Moderate Resolution Imaging Spectroradiometer (MODIS [ http://modis.gsfc.nasa.gov ]) on NASA's Terra [ http://terra.nasa.gov/ ] satellite between July 12 and July 19, 2006. NASA image created by Jesse Allen, Earth Observatory, using data provided courtesy of Zhengming Wan, MODIS Land Surface Temperature Group, Institute for Computational Earth System Science [ http://www.icess.ucsb.edu/ ], University of California, Santa Barbara.
Heat Wave in Western Europe
Title Heat Wave in Western Europe
Description Western Europe continued to bake in late July 2006. Following an unusually warm spell between July 12 and 19, [ http://earthobservatory.nasa.gov/NaturalHazards/natural_hazards_v2.php3?img_id=13743 ] temperatures across most of the region remained much warmer than normal. This image shows land surface (as opposed to air) temperatures collected from July 20-27, 2006, compared to the average temperatures for that period over the past six years (2000-2005). Places that were up to ten degrees Celsius warmer than average are deep red, while places that were up to ten degrees cooler than average are deep blue. Places where the temperatures were average are white. The temperatures were measured by the Moderate Resolution Imaging Spectroradiometer (MODIS) [ http://modis.gsfc.nasa.gov ] on NASA's Terra [ http://terra.nasa.gov ] satellite. In the center of the image, deep red areas of very warm temperatures spread across Germany, as well as France (to the west), and Poland (to the east). To the north (top center), both Norway (west) and Sweden (east) were much warmer than average. Only small pockets of the region were cooler than average: northeastern Spain, the "toe" of Italy's boot and the western half of the island of Sicily, and parts of Greece (lower right). July 2006 was a record-breaking month for heat in many Western European countries, coming in as the hottest July on record in several countries, including Belgium, Denmark, Ireland, the Netherlands, and the United Kingdom. NASA image created by Jesse Allen, Earth Observatory, using data provided courtesy of Zhengming Wan, MODIS Land Surface Temperature Group, Institute for Computational Earth System Science [ http://www.icess.ucsb.edu/ ], University of California, Santa Barbara.
Drought in Southeastern Aust …
Title Drought in Southeastern Australia
Description Deep red paints the coastal mountains of southeastern Australia, hangs over the continent's arid interior, and dots much of the rest of the land in this image, indicating that unusually high temperatures reigned in November 2006. According to the Australian Bureau of Meteorology, the monthly average temperature for the country hit a record high in November. The average temperature for the continent was 2.11 degrees Celsius warmer than average, with local temperatures rising more than 4 degrees C above average for the month in places. These abnormally high air temperatures are reflected in the extreme land surface temperatures shown in this image. The land is usually much warmer to the touch than the temperature recorded by a thermometer hanging above the ground, and so, during November, land surface temperatures in Australia were as much as 10 degrees Celsius above a five-year average. The greatest deviation from normal temperatures is shown in dark red in this image. Average temperatures are white, and cooler-than-average temperatures are blue. The temperature data were collected by the Moderate Resolution Imaging Spectroradiometer (MODIS [ http://modis.gsfc.nasa.gov ]) on NASA's Terra [ http://terra.nasa.gov/ ] satellite. The temperature anomaly was greatest in the Great Dividing Range, which curves along the coasts of Victoria and New South Wales in southeast Australia. The heat and a lack of spring rain may have primed the mountains for devastating wildfires. By the end of December, several large wildfires [ http://earthobservatory.nasa.gov/NaturalHazards/natural_hazards_v2.php3?img_id=14029 ] raced through the mountains, threatening local communities and clouding the skies over much of southeastern Australia with dense smoke. The high temperatures in the Great Dividing Range and elsewhere were just part of an unusually warm and dry spring, [ http://earthobservatory.nasa.gov/NaturalHazards/natural_hazards_v2.php3?img_id=13943 ] which in turn, was an extension of a dry year. Some of the dryness may be linked to a weak El Niñno in the Pacific Ocean. El Niñno is a regular climate pattern during which sea surface temperatures in the eastern Pacific Ocean near the equator heat up and trade winds weaken. Though the effects of El Niñno vary, the phenomenon often changes rainfall patterns around the world. In Australia, El Niñno often brings a dry winter and spring. It is also linked to an increase in the number of extreme fire days, during which conditions are hot, dry, and windy. NASA image created by Jesse Allen, Earth Observatory, using data provided courtesy of Zhengming Wan, MODIS Land Surface Temperature Group, Institute for Computational Earth System Science [ http://www.icess.ucsb.edu/ ], University of California, Santa Barbara.
Heavy Rains in Hawaii
Title Heavy Rains in Hawaii
Description In March 2006, Hawaii suffered heavy rains, flooding, and severe weather. A series of storms (upper-level low pressure centers) north and west of the islands drew warm moist air up from the tropics. When this flow of moist tropical air passed over Hawaii, the island chain's steep mountains acted as a wringer, releasing torrential rain from the air. As a result, the islands received record-setting rain throughout March 2006. On Kauai, Mount Waialeale (one of the wettest places on earth) set an all-time monthly record of 93.71 inches of rain. Part of the reason for all of the rainfall is the current La Niña. During La Niña conditions, Hawaii is expected to have above-average rainfall totals. The image above is based on data from the Tropical Rainfall Measuring Mission (TRMM). The TRMM-based, near-real time Multi-satellite Precipitation Analysis (MPA) at the NASA Goddard Space Flight Center monitors rainfall over the global Tropics. The above image shows MPA rainfall anomalies between February 19 and April 1, 2006, for the northern East Pacific. Hawaii and the surrounding area had higher-than-average rainfall (green areas) in general, and the western half of the state received much more rain than normal (blue areas). The large-format image also shows a coherent pattern of above-average rainfall anomalies that extend to the West Coast (green streaks) and culminate in well-above-average rainfall (blue areas) over northern California. These trends are consistent with a La Niña pattern. The TRMM satellite was launched in November 1997 to measure rainfall over the tropics. It is equipped with both passive and active sensors, including the first precipitation radar in space. TRMM is a joint mission between NASA and the Japanese space agency, JAXA. Image produced by Hal Pierce (SSAI/NASA GSFC) and caption by Steve Lang (SSAI/NASA GSFC).
Hurricane Daniel
Title Hurricane Daniel
Description On July 18, Daniel became the third hurricane to form in the East Pacific during 2006, setting the pace of hurricane formation at about average for the region. It was already the second major hurricane in the East Pacific, which put 2006 well ahead of the pace set in 2005, during which only two major hurricanes formed for the entire season. After intensifying from a tropical depression that was tracking westward across the eastern Pacific away from land, Daniel became a named tropical storm on July 17, 2006, about 1,400 miles south of Baja California. Daniel continued to strengthen and became a minimal hurricane on the afternoon of July 18 (local time). The Tropical Rainfall Measuring Mission satellite (TRMM [ http://trmm.gsfc.nasa.gov/ ]) captured these images of Hurricane Daniel on July 19 at 3:29 a.m. Pacific Daylight Time (10:29 UTC), just before the storm intensified from Category 1 to a Category 4 storm. The top image shows the horizontal distribution of rain intensity (top-down view) within the storm. Rain rates in the center of the swath are from the TRMM Precipitation Radar, and rain rates in the outer swath are from the TRMM Microwave Imager. These rain rates are overlaid on infrared data from the TRMM Visible Infrared Scanner. Circles of red and green trace out the tight circling bands of rain. This tight banding, along with a nearly complete inner eyewall (innermost green arc), is evidence that Daniel was very well organized with a well-developed circulation. There is also an area of intense rain (dark red) within the eyewall. At the time of this image, the National Hurricane Center [ http://www.nhc.noaa.gov/ ], reported that Daniel was a strong Category 1 hurricane, with maximum sustained winds reported at 150 kilometers per hour (92 mph or 80 knots). The lower image is a three-dimensional depiction of the storm from the same overpass. The image was created from data taken by the TRMM Precipitation Radar, which has the ability to look at vertical precipitation structures. The radar reveals an area of deep convection, where water-laden air is rising high and fast, right near Daniel's center. This area shows up as red peaks that are about 15 kilometers high. The peaks are associated with the area of heavy rain within the eyewall in the previous image. The presence of such towers can be a precursor for intensification when they are near the storm's core. This was indeed the case with Daniel, which steadily increased in intensity after these images were taken, reaching Category 4 intensity on July 20, with maximum sustained winds of 220 km/hr (138 mph or 120 knots) as reported by the National Hurricane Center. Daniel was expected to gradually turn to the northwest and weaken over cooler waters. TRMM was placed into service in November of 1997. From its low-earth orbit, TRMM has been providing valuable images and information on tropical cyclones around the Tropics using a combination of passive microwave and active radar sensors, including the first precipitation radar in space. TRMM is a joint mission between NASA and the Japanese space agency, JAXA. Images produced by Hal Pierce (SSAI/NASA GSFC) and caption by Steve Lang (SSAI/NASA GSFC).
Hurricane Daniel
Title Hurricane Daniel
Description On July 18, Daniel became the third hurricane to form in the East Pacific during 2006, setting the pace of hurricane formation at about average for the region. It was already the second major hurricane in the East Pacific, which put 2006 well ahead of the pace set in 2005, during which only two major hurricanes formed for the entire season. After intensifying from a tropical depression that was tracking westward across the eastern Pacific away from land, Daniel became a named tropical storm on July 17, 2006, about 1,400 miles south of Baja California. Daniel continued to strengthen and became a minimal hurricane on the afternoon of July 18 (local time). The Tropical Rainfall Measuring Mission satellite (TRMM [ http://trmm.gsfc.nasa.gov/ ]) captured these images of Hurricane Daniel on July 19 at 3:29 a.m. Pacific Daylight Time (10:29 UTC), just before the storm intensified from Category 1 to a Category 4 storm. The top image shows the horizontal distribution of rain intensity (top-down view) within the storm. Rain rates in the center of the swath are from the TRMM Precipitation Radar, and rain rates in the outer swath are from the TRMM Microwave Imager. These rain rates are overlaid on infrared data from the TRMM Visible Infrared Scanner. Circles of red and green trace out the tight circling bands of rain. This tight banding, along with a nearly complete inner eyewall (innermost green arc), is evidence that Daniel was very well organized with a well-developed circulation. There is also an area of intense rain (dark red) within the eyewall. At the time of this image, the National Hurricane Center [ http://www.nhc.noaa.gov/ ], reported that Daniel was a strong Category 1 hurricane, with maximum sustained winds reported at 150 kilometers per hour (92 mph or 80 knots). The lower image is a three-dimensional depiction of the storm from the same overpass. The image was created from data taken by the TRMM Precipitation Radar, which has the ability to look at vertical precipitation structures. The radar reveals an area of deep convection, where water-laden air is rising high and fast, right near Daniel's center. This area shows up as red peaks that are about 15 kilometers high. The peaks are associated with the area of heavy rain within the eyewall in the previous image. The presence of such towers can be a precursor for intensification when they are near the storm's core. This was indeed the case with Daniel, which steadily increased in intensity after these images were taken, reaching Category 4 intensity on July 20, with maximum sustained winds of 220 km/hr (138 mph or 120 knots) as reported by the National Hurricane Center. Daniel was expected to gradually turn to the northwest and weaken over cooler waters. TRMM was placed into service in November of 1997. From its low-earth orbit, TRMM has been providing valuable images and information on tropical cyclones around the Tropics using a combination of passive microwave and active radar sensors, including the first precipitation radar in space. TRMM is a joint mission between NASA and the Japanese space agency, JAXA. Images produced by Hal Pierce (SSAI/NASA GSFC) and caption by Steve Lang (SSAI/NASA GSFC).
Hurricane Daniel
Title Hurricane Daniel
Description On July 18, Daniel became the third hurricane to form in the East Pacific during 2006, setting the pace of hurricane formation at about average for the region. It was already the second major hurricane in the East Pacific, which put 2006 well ahead of the pace set in 2005, during which only two major hurricanes formed for the entire season. After intensifying from a tropical depression that was tracking westward across the eastern Pacific away from land, Daniel became a named tropical storm on July 17, 2006, about 1,400 miles south of Baja California. Daniel continued to strengthen and became a minimal hurricane on the afternoon of July 18 (local time). The Tropical Rainfall Measuring Mission satellite (TRMM [ http://trmm.gsfc.nasa.gov/ ]) captured these images of Hurricane Daniel on July 19 at 3:29 a.m. Pacific Daylight Time (10:29 UTC), just before the storm intensified from Category 1 to a Category 4 storm. The top image shows the horizontal distribution of rain intensity (top-down view) within the storm. Rain rates in the center of the swath are from the TRMM Precipitation Radar, and rain rates in the outer swath are from the TRMM Microwave Imager. These rain rates are overlaid on infrared data from the TRMM Visible Infrared Scanner. Circles of red and green trace out the tight circling bands of rain. This tight banding, along with a nearly complete inner eyewall (innermost green arc), is evidence that Daniel was very well organized with a well-developed circulation. There is also an area of intense rain (dark red) within the eyewall. At the time of this image, the National Hurricane Center [ http://www.nhc.noaa.gov/ ], reported that Daniel was a strong Category 1 hurricane, with maximum sustained winds reported at 150 kilometers per hour (92 mph or 80 knots). The lower image is a three-dimensional depiction of the storm from the same overpass. The image was created from data taken by the TRMM Precipitation Radar, which has the ability to look at vertical precipitation structures. The radar reveals an area of deep convection, where water-laden air is rising high and fast, right near Daniel's center. This area shows up as red peaks that are about 15 kilometers high. The peaks are associated with the area of heavy rain within the eyewall in the previous image. The presence of such towers can be a precursor for intensification when they are near the storm's core. This was indeed the case with Daniel, which steadily increased in intensity after these images were taken, reaching Category 4 intensity on July 20, with maximum sustained winds of 220 km/hr (138 mph or 120 knots) as reported by the National Hurricane Center. Daniel was expected to gradually turn to the northwest and weaken over cooler waters. TRMM was placed into service in November of 1997. From its low-earth orbit, TRMM has been providing valuable images and information on tropical cyclones around the Tropics using a combination of passive microwave and active radar sensors, including the first precipitation radar in space. TRMM is a joint mission between NASA and the Japanese space agency, JAXA. Images produced by Hal Pierce (SSAI/NASA GSFC) and caption by Steve Lang (SSAI/NASA GSFC).
Hurricane Daniel
Title Hurricane Daniel
Description Hurricane Daniel formed in the eastern Pacific Ocean on July 16, 2006, off the Mexican coast south of Baja California. The tropical depression strengthened to storm status in the next day, and as the fourth storm in the Eastern Pacific, was named Daniel. By early morning on July 18, winds in the storm reached 120 kilometers per hour (75 miles per hour), bringing Daniel to hurricane strength, just as the previous three storms of the Eastern Pacific had already done in 2006. Like most hurricanes that form in this region, Daniel tracked out into the Pacific farther away from land. It headed west-northwest, where there is little in the way of barriers to its gathering strength, but also little prospect for it to strike inhabited areas. This photo-like image was acquired by the Moderate Resolution Imaging Spectroradiometer (MODIS) [ http://modis.gsfc.nasa.gov/ ] on the Aqua [ http://aqua.nasa.gov/ ] satellite on July 18, 2006, at 2:10 p.m. local time (21:10 UTC). Daniel has a very well-defined spiral shape and active thunderstorm systems close to the eyewall. At the time the Aqua satellite passed overhead, Daniel had a closed eye: the center of the storm still had cloud cover. Open-eye hurricanes are generally well-developed and powerful systems, a status that Daniel had not yet achieved, though forecasts called for the hurricane to continue to grow in size and strength over the next few days. Sustained winds in the storm system were estimated to be around 120 kilometers per hour (75 miles per hour) around the time the image was captured, according to the University of Hawaii's Tropical Storm Information Center, [ http://www.solar.ifa.hawaii.edu/Tropical/tropical.html ] very similar to its strength earlier in the day when it first achieved hurricane status. By July 20, though, the apparent pause in the storm's gathering power was long over, and sustained winds were reported to be 200 km/hr (125 mph). NASA image by Jesse Allen, Earth Observatory, using data obtained from the Goddard Earth Sciences DAAC.
Hurricane John
Title Hurricane John
Description As of September 1, 2006, Hurricane John had been lashing Mexico's Pacific coast for several days. The storm system center remained offshore, and forecasts predicted that it would only briefly come ashore as it clipped the southern tip of Mexico's Baja California on its track up the Pacific coast. It is unusual for an eastern Pacific hurricane to come ashore without breaking apart into a lesser storm system because of prevailing wind patterns and cold water upwelling along the coast. Hurricane John, however, managed to run parallel to the Mexico coast for several days. The most powerful hurricane-force winds were not over land, but the Category Four hurricane [ http://www.nhc.noaa.gov/aboutsshs.shtml ] was large enough to bring strong winds and heavy surf to the coastal areas. This photo-like image was acquired by the Moderate Resolution Imaging Spectroradiometer (MODIS) [ http://modis.gsfc.nasa.gov/ ] on the Aqua [ http://aqua.nasa.gov/ ] satellite on August 31, 2006, at 2:10 p.m. local time (20:10 UTC). Hurricane John at the time of this image had a well-defined if widespread shape, spiral-arm structure, and a cloud-filled ("closed") eye. Hurricane John had sustained winds of around 165 kilometers per hour (105 miles per hour) at the time this satellite image was acquired, according to the University of Hawaii's Tropical Storm Information Center. [ http://www.solar.ifa.hawaii.edu/Tropical/tropical.html ] This stregnth was somewhat less powerful than two days earlier when Category 4-strength winds were measured in the central parts of the hurricane. NASA image created by Jesse Allen, Earth Observatory, using data provided courtesy of the MODIS Rapid Response [ http://rapidfire.sci.gsfc.nasa.gov/ ] team.
Hurricane Paul
Title Hurricane Paul
Description Hurricane Paul formed on October 21, 2006, in the eastern Pacific near the coast of Mexico. It grew quickly to hurricane strength as it spun off the coast near Baja California for the next several days. The sixteenth named storm of the Pacific storm season, Paul remained offshore as of October 24, though residents of southern Baja California were eyeing it warily for signs it might shift and come ashore there. This photo-like image was acquired by the Moderate Resolution Imaging Spectroradiometer (MODIS) [ http://modis.gsfc.nasa.gov/ ] on the Aqua [ http://aqua.nasa.gov/ ] satellite on October 23, 2006, at 12:30 p.m. local time (20:30 UTC). Paul at the time of this image was a small, well-defined swirl. However, cloud patterns over a wide area appear to be under the storm's influence, with clouds reaching as far as southern Baja. Winds around the center of Hurricane Paul were whipping around at 160 kilometers per hour (100 miles per hour), according to the University of Hawaii's Tropical Storm Information Center. [ http://www.solar.ifa.hawaii.edu/Tropical/ ] In 2005, the record-breaking Atlantic hurricane season was the focus of attention, with the number of named storms exhausting the letters of the alphabet. But as of late October 2006, the hurricane activity in the eastern Pacific Ocean was outpacing the Atlantic: 16 named storms (9 of them hurricanes) versus 9 named storms (5 of them hurricanes). On average, the eastern Pacific Ocean experiences more tropical storms and hurricanes than the Atlantic Basin, 16.4 compared to 10.1. Powerful hurricanes in the eastern Pacific rarely make landfall in the western United States. Persistent easterly winds not only tend to steer storms away from the coast, but they also "shove" the ocean's surface water westward, away from the coast, allowing cool water to well up to replace it. The cool water weakens any storms that do approach the coast. NASA image created by Jesse Allen, Earth Observatory, using data obtained courtesy of the MODIS Rapid Response [ http://rapidfire.sci.gsfc.nasa.gov/ ] team.
Earthquake Raises Reefs in t …
Title Earthquake Raises Reefs in the Solomon Islands
Description When people talk about change happening on a geologic time scale, most of the time, they mean that the change happens over the course of millions of years: the Colorado River gradually cuts through the soft rock of the Colorado Plateau until it has made a 4,000-foot-deep chasm, the Grand Canyon, continents drift centimeters at a time, slowly changing the shape and position of landmasses on the Earth. Most of the time, change is slow, but sometimes, geologic change happens all at once. This was the case on Ranongga Island in the Solomon Islands. In the early morning hours of April 2, 2007, a magnitude 8.1 earthquake shook the Solomon Islands, its epicenter southwest of Ranongga Island. The huge quake pushed much of the island up, raising the coral reefs that ringed the island above the water. In the course of a few minutes, Ranongga Island acquired several meters of new beach. The newly exposed reef forms a gray rim along the eastern shore of the island in the left image, acquired by the Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER) on April 12, 2007. In the right image, taken on March 31, 2006, the shallowly submerged reefs color the water a lighter shade of blue. The uplift may be more dramatic than the images show. When ASTER took the 2007 image, the tide was 29.4 centimeters higher than it was when the 2006 image was taken, and yet the uplift is still visible. The lush vegetation that covers the tropical island is bright red in this image, which is made from both visible and infrared light. Out of its aquatic environment, the reef died, becoming the foundation of new land. Such evolution is common in earthquake zones in the Pacific and Indian Oceans. During the December 26, 2004, earthquake that generated the massive Indian Ocean tsunami, Simeulue Island was lifted as much as 150 centimeters (4.9 feet), exposing the reef that surrounded it. A similar set of exposed fossilized reefs on the shores of Papua New Guinea, near the Solomon Islands, provided proof that wobbles in the Earth's orbit trigger ice ages. NASA image created by Jesse Allen, using data provided courtesy of the NASA/GSFC/MITI/ERSDAC/JAROS, and U.S./Japan ASTER Science Team. [ http://asterweb.jpl.nasa.gov/ ]Thanks to Aron Meltzner, California Institute of Technology, for help with image interpretation.
Earthquake Raises Reefs in t …
Title Earthquake Raises Reefs in the Solomon Islands
Description When people talk about change happening on a geologic time scale, most of the time, they mean that the change happens over the course of millions of years: the Colorado River gradually cuts through the soft rock of the Colorado Plateau until it has made a 4,000-foot-deep chasm, the Grand Canyon, continents drift centimeters at a time, slowly changing the shape and position of landmasses on the Earth. Most of the time, change is slow, but sometimes, geologic change happens all at once. This was the case on Ranongga Island in the Solomon Islands. In the early morning hours of April 2, 2007, a magnitude 8.1 earthquake shook the Solomon Islands, its epicenter southwest of Ranongga Island. The huge quake pushed much of the island up, raising the coral reefs that ringed the island above the water. In the course of a few minutes, Ranongga Island acquired several meters of new beach. The newly exposed reef forms a gray rim along the eastern shore of the island in the left image, acquired by the Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER) on April 12, 2007. In the right image, taken on March 31, 2006, the shallowly submerged reefs color the water a lighter shade of blue. The uplift may be more dramatic than the images show. When ASTER took the 2007 image, the tide was 29.4 centimeters higher than it was when the 2006 image was taken, and yet the uplift is still visible. The lush vegetation that covers the tropical island is bright red in this image, which is made from both visible and infrared light. Out of its aquatic environment, the reef died, becoming the foundation of new land. Such evolution is common in earthquake zones in the Pacific and Indian Oceans. During the December 26, 2004, earthquake that generated the massive Indian Ocean tsunami, Simeulue Island was lifted as much as 150 centimeters (4.9 feet), exposing the reef that surrounded it. A similar set of exposed fossilized reefs on the shores of Papua New Guinea, near the Solomon Islands, provided proof that wobbles in the Earth's orbit trigger ice ages. NASA image created by Jesse Allen, using data provided courtesy of the NASA/GSFC/MITI/ERSDAC/JAROS, and U.S./Japan ASTER Science Team. [ http://asterweb.jpl.nasa.gov/ ]Thanks to Aron Meltzner, California Institute of Technology, for help with image interpretation.
Earthquake Raises Reefs in t …
Title Earthquake Raises Reefs in the Solomon Islands
Description When people talk about change happening on a geologic time scale, most of the time, they mean that the change happens over the course of millions of years: the Colorado River gradually cuts through the soft rock of the Colorado Plateau until it has made a 4,000-foot-deep chasm, the Grand Canyon, continents drift centimeters at a time, slowly changing the shape and position of landmasses on the Earth. Most of the time, change is slow, but sometimes, geologic change happens all at once. This was the case on Ranongga Island in the Solomon Islands. In the early morning hours of April 2, 2007, a magnitude 8.1 earthquake shook the Solomon Islands, its epicenter southwest of Ranongga Island. The huge quake pushed much of the island up, raising the coral reefs that ringed the island above the water. In the course of a few minutes, Ranongga Island acquired several meters of new beach. The newly exposed reef forms a gray rim along the eastern shore of the island in the left image, acquired by the Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER) on April 12, 2007. In the right image, taken on March 31, 2006, the shallowly submerged reefs color the water a lighter shade of blue. The uplift may be more dramatic than the images show. When ASTER took the 2007 image, the tide was 29.4 centimeters higher than it was when the 2006 image was taken, and yet the uplift is still visible. The lush vegetation that covers the tropical island is bright red in this image, which is made from both visible and infrared light. Out of its aquatic environment, the reef died, becoming the foundation of new land. Such evolution is common in earthquake zones in the Pacific and Indian Oceans. During the December 26, 2004, earthquake that generated the massive Indian Ocean tsunami, Simeulue Island was lifted as much as 150 centimeters (4.9 feet), exposing the reef that surrounded it. A similar set of exposed fossilized reefs on the shores of Papua New Guinea, near the Solomon Islands, provided proof that wobbles in the Earth's orbit trigger ice ages. NASA image created by Jesse Allen, using data provided courtesy of the NASA/GSFC/MITI/ERSDAC/JAROS, and U.S./Japan ASTER Science Team. [ http://asterweb.jpl.nasa.gov/ ]Thanks to Aron Meltzner, California Institute of Technology, for help with image interpretation.
Esperanza Fire
Title Esperanza Fire
Description Waves of gray-brown smoke washed over the mountains southeast of Los Angeles and out over the Pacific on October 26, 2006. West of Palm Springs, California, the Esperanza Fire had ballooned under the influence of Santa Ana winds to more than 19,000 acres as of the morning of October 27, according to the daily report from the National Interagency Fire Center. [ http://www.nifc.gov/information.html ] Racing through grass, brush, and timber, the blaze had forced hundreds to evacuate, and it killed several firefighters who were working to protect homes. Fire officials are reporting the cause of the blaze as arson. This photo-like image shows the fire and surrounding area captured by the Moderate Resolution Imaging Spectroradiometer (MODIS) [ http://modis.gsfc.nasa.gov ] on NASA's Aqua [ http://aqua.nasa.gov ] satellite on October 26. Places where MODIS detected actively burning fire are outlined in red. The Santa Ana Mountains peek out from beneath the smoke near the southeastern suburbs of Los Angeles. Santa Ana winds are a California firefighter's nightmare. These blustery, dry, and often hot winds blow out of the desert and race through canyons and passes in the mountains on their way toward the coast. The air is hot not because it is bringing heat from the desert, but because it is flowing downslope from higher elevations. As fall progresses, cold air begins to sink into the Great Basin deserts to the east of California. As the air piles up at the surface, high pressure builds, and the air begins to flow downslope toward the coast. When winds blow downslope, the air gets compressed, which causes it to warm and dry out. In fact, the air can warm at a rate of 10 degrees Celsius per kilometer of descent (29 degrees Fahrenheit per mile). Canyons and passes funnel the winds, which increases their speed. Not only do the winds spread the fire, but they also dry out vegetation, making it even more flammable. A 250-meter-resolution KMZ file [ http://earthobservatory.nasa.gov/NaturalHazards/Archive/Oct2006/Esperanza_AMO_2006299.kmz ] of the Esperanza Fire is available for use with Google Earth. [ http://earth.google.com/download-earth.html ] NASA image by Jeff Schmaltz, MODIS Rapid Response Team, [ http://rapidfire.sci.gsfc.nasa.gov ] Goddard Space Flight Center.
Esperanza Fire
Title Esperanza Fire
Description In late October, a fierce forest fire flared up in the mountainous terrain west of Palm Springs, California. The Esperanza Fire started in the foothills at the southern outskirts of the town of Cabazon, apparently as an act of arson. Driven by Santa Ana winds out of Great Basin deserts to the east, the fire raced over more than 40,000 acres in a matter of days, destroying 34 homes and 20 outbuildings in the area. Several firefighters died while battling the blaze.This high-resolution satellite image of the fire was captured on October 26, 2006, by the Thematic Mapper sensor on NASA's Landsat 5 satellite. The image was captured at 11:16 a.m. Pacific Daylight Time, roughly 10 hours after fire officials believe the fire began. At the top of the scene, the towns of Banning and Cabazon line Interstate 10, which appears as a thick, gray ribbon running through the dry, brown valley of San Gorgino Pass. Regular geometric shapes—straight lines and rectangles—are roads and buildings. Meandering, pale tracings show the paths of dry creeks and rivers. To the south, the foothill ranges of the San Jacinto Mountains begin. Fire was burning along ridgelines near McMullen and Hurley Flats. Gray-brown smoke stretches southwest in long plumes. A towering column of smoke west-southwest of McMullen flat casts a dramatic black shadow to the northwest. At the time of this image, the fire had already burned almost the entire landscape between Hurley Flat and the valley floor to the north, as well as nearly all the terrain bounded by the smoke plumes. Although the difference is subtle, burned areas appear charcoal-tinged when compared to unburned vegetation, such as the forested slopes of the Black Mountain Scenic Area at lower right. Unburned vegetation appears brownish-green. NASA image created by Jesse Allen, Earth Observatory, using data provided courtesy of Laura Rocchio, Landsat Project Science Office. [ http://landsat.gsfc.nasa.gov/ ]
Fires in California
Title Fires in California
Description According to news reports, the Sawtooth and Millard Complex Fires in southern California east of San Bernardino merged on Friday afternoon, July 14, 2006. This pair of images of the two fires was captured on July 14 before the two fires joined. The top image is a photo-like, natural-color satellite image captured by the Enhanced Thematic Mapper Plus sensor on NASA's Landsat satellite. The dull vegetation of this semi-arid region at the western edge of the Mojave Desert appears brownish, while canyons and bare spots appear tan. The false-color image below includes satellite observations of shortwave and near-infrared light reflected from the ground. In this view, vegetation appears bright green, burned areas appear deep red, and actively flaming fire fronts appear hot pink. Smoke appears blue. These fires were burning in an area with large expanses of dead trees that were killed by pine bark beetles. As of July 19, 2006, the Sawtooth Complex Fire was 61,700 acres and fully contained, while the Millard Complex Fire was about 24,210 acres and 57 percent contained. According to reports from the National Interagency Fire Center, [ http://www.nifc.gov/information.html ] 221 structures were lost in the Sawtooth Fire. NASA images created by Jesse Allen, Earth Observatory, using data provided courtesy of Laura Rocchio, Landsat Project Science Office. [ http://landsat.gsfc.nasa.gov/ ]
Fires in California
Title Fires in California
Description According to news reports, the Sawtooth and Millard Complex Fires in southern California east of San Bernardino merged on Friday afternoon, July 14, 2006. This pair of images of the two fires was captured on July 14 before the two fires joined. The top image is a photo-like, natural-color satellite image captured by the Enhanced Thematic Mapper Plus sensor on NASA's Landsat satellite. The dull vegetation of this semi-arid region at the western edge of the Mojave Desert appears brownish, while canyons and bare spots appear tan. The false-color image below includes satellite observations of shortwave and near-infrared light reflected from the ground. In this view, vegetation appears bright green, burned areas appear deep red, and actively flaming fire fronts appear hot pink. Smoke appears blue. These fires were burning in an area with large expanses of dead trees that were killed by pine bark beetles. As of July 19, 2006, the Sawtooth Complex Fire was 61,700 acres and fully contained, while the Millard Complex Fire was about 24,210 acres and 57 percent contained. According to reports from the National Interagency Fire Center, [ http://www.nifc.gov/information.html ] 221 structures were lost in the Sawtooth Fire. NASA images created by Jesse Allen, Earth Observatory, using data provided courtesy of Laura Rocchio, Landsat Project Science Office. [ http://landsat.gsfc.nasa.gov/ ]
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