|
|
Satellite Imagery of Hurrica
| Title |
Satellite Imagery of Hurricane Dennis (WMS) |
| Abstract |
Hurricane Dennis started as a tropical depression on August 23, 1999, became a tropical storm on August 24, and was classified as a hurricane early on August 26, near the Bahamas. From August 26 through August 31, Dennis proceeded up the coast of the United States until it stalled off the coast of North Carolina for four days because the pressure trough that was pushing it out to sea left it behind. This animation shows images of Dennis during its hurricane period from August 26 through August 31, 1999, when the stall began. The images were taken by the GOES-8 satellite, a weather satellite in geostationary orbit above the western hemisphere. The continuous white cloud progression came from infrared images from GOES, and the yellowish clouds that come and go with the daylight came from data taken in the visible spectrum, also from GOES. The GOES images were not taken at regular times, so the hurricane appears to slow down when the time between images gets small and speed up when the time between images gets large. |
| Completed |
2004-02-10 |
|
First 3-D Stereo from STEREO
| Title |
First 3-D Stereo from STEREO: EUVI 171 Angstroms (South Pole View) |
| Abstract |
This movie shows the south pole of the Sun from the two STEREO spacecraft using the 171 Angstrom filter in the Extreme UltraViolet Imager (EUVI). This filter reveals ionized iron (Fe+8=Fe IX, Fe+9=Fe X) which forms at temperatures above 1.3x106K, and flows along the magnetic field lines of the solar active regions. New active regions come into view as the Sun rotates. |
| Completed |
2007-04-25 |
|
First 3-D Stereo from STEREO
| Title |
First 3-D Stereo from STEREO: EUVI 284 Angstroms (Full Disk View) |
| Abstract |
This movie shows the Sun from the two STEREO spacecraft using the 284 Angstrom filter in the Extreme UltraViolet Imager (EUVI). This filter reveals ionized iron (Fe+14=Fe XV), which forms at temperatures above 2x106K, and flows along the magnetic field lines of the solar active regions. New active regions come into view as the Sun rotates. |
| Completed |
2007-04-25 |
|
TRMM Tropical Microwave Imag
| Title |
TRMM Tropical Microwave Imager (TMI) sees the power of Hurricane Jeanne On September 25, 2004 |
| Abstract |
NASA's TRMM spacecraft is used by meteorologists to understand Hurricane Jeanne. TRMM saw this view of Hurricane Jeanne on September 25, 2004, just before it made landfall. The cloud cover is taken by TRMM's Visible and Infrared Scanner (VIRS). It looks underneath of the storm's clouds to reveal the underlying rain structure. Blue represents areas with at least 0.25 inches of rain per hour. Green shows at least 0.5 inches of rain per hour. Yellow is at least 1.0 inches of rain and red is at least 2.0 inches of rain per hour. |
| Completed |
2004-09-30 |
|
TRMM Tropical Microwave Imag
| Title |
TRMM Tropical Microwave Imager (TMI) sees the power of Hurricane Jeanne On September 25, 2004 |
| Abstract |
NASA's TRMM spacecraft is used by meteorologists to understand Hurricane Jeanne. TRMM saw this view of Hurricane Jeanne on September 25, 2004, just before it made landfall. The cloud cover is taken by TRMM's Visible and Infrared Scanner (VIRS). It looks underneath of the storm's clouds to reveal the underlying rain structure. Blue represents areas with at least 0.25 inches of rain per hour. Green shows at least 0.5 inches of rain per hour. Yellow is at least 1.0 inches of rain and red is at least 2.0 inches of rain per hour. |
| Completed |
2004-09-30 |
|
TRMM Tropical Microwave Imag
| Title |
TRMM Tropical Microwave Imager (TMI) sees the power of Hurricane Jeanne On September 25, 2004 |
| Abstract |
NASA's TRMM spacecraft is used by meteorologists to understand Hurricane Jeanne. TRMM saw this view of Hurricane Jeanne on September 25, 2004, just before it made landfall. The cloud cover is taken by TRMM's Visible and Infrared Scanner (VIRS). It looks underneath of the storm's clouds to reveal the underlying rain structure. Blue represents areas with at least 0.25 inches of rain per hour. Green shows at least 0.5 inches of rain per hour. Yellow is at least 1.0 inches of rain and red is at least 2.0 inches of rain per hour. |
| Completed |
2004-09-30 |
|
TRMM Tropical Microwave Imag
| Title |
TRMM Tropical Microwave Imager (TMI) sees the power of Hurricane Jeanne On September 25, 2004 |
| Abstract |
NASA's TRMM spacecraft is used by meteorologists to understand Hurricane Jeanne. TRMM saw this view of Hurricane Jeanne on September 25, 2004, just before it made landfall. The cloud cover is taken by TRMM's Visible and Infrared Scanner (VIRS). It looks underneath of the storm's clouds to reveal the underlying rain structure. Blue represents areas with at least 0.25 inches of rain per hour. Green shows at least 0.5 inches of rain per hour. Yellow is at least 1.0 inches of rain and red is at least 2.0 inches of rain per hour. |
| Completed |
2004-09-30 |
|
TRMM Tropical Microwave Imag
| Title |
TRMM Tropical Microwave Imager (TMI) sees the power of Hurricane Jeanne On September 25, 2004 |
| Abstract |
NASA's TRMM spacecraft is used by meteorologists to understand Hurricane Jeanne. TRMM saw this view of Hurricane Jeanne on September 25, 2004, just before it made landfall. The cloud cover is taken by TRMM's Visible and Infrared Scanner (VIRS). It looks underneath of the storm's clouds to reveal the underlying rain structure. Blue represents areas with at least 0.25 inches of rain per hour. Green shows at least 0.5 inches of rain per hour. Yellow is at least 1.0 inches of rain and red is at least 2.0 inches of rain per hour. |
| Completed |
2004-09-30 |
|
TRMM Tropical Microwave Imag
| Title |
TRMM Tropical Microwave Imager (TMI) sees the power of Hurricane Jeanne On September 25, 2004 |
| Abstract |
NASA's TRMM spacecraft is used by meteorologists to understand Hurricane Jeanne. TRMM saw this view of Hurricane Jeanne on September 25, 2004, just before it made landfall. The cloud cover is taken by TRMM's Visible and Infrared Scanner (VIRS). It looks underneath of the storm's clouds to reveal the underlying rain structure. Blue represents areas with at least 0.25 inches of rain per hour. Green shows at least 0.5 inches of rain per hour. Yellow is at least 1.0 inches of rain and red is at least 2.0 inches of rain per hour. |
| Completed |
2004-09-30 |
|
GOES-12 Imagery of Hurricane
| Title |
GOES-12 Imagery of Hurricane Katrina: Full Disk Lower Level Temperature (WMS) |
| Abstract |
The GOES-12 satellite sits at 75 degrees west longitude at an altitude of 36,000 kilometers over the equator, in geosynchronous orbit. At this position its Imager instrument takes pictures of cloud patterns in several wavelengths for all of North and South America, a primary measurement used in weather forecasting. Every three hours the Imager takes a picture of the full disk of the Earth. This animation shows a sequence of these full disk images in the wavelength band from 12.9 to 13.8 microns, during the period that Hurricane Katrina passed through the Gulf of Mexico. This wavelength band is useful for determining cloud characteristics such as cloud top pressure. |
| Completed |
2005-08-29 |
|
GOES-12 Imagery of Hurricane
| Title |
GOES-12 Imagery of Hurricane Katrina: Full Disk Water Vapor (WMS) |
| Abstract |
The GOES-12 satellite sits at 75 degrees west longitude at an altitude of 36,000 kilometers over the equator, in geosynchronous orbit. At this position its Imager instrument takes pictures of cloud patterns in several wavelengths for all of North and South America, a primary measurement used in weather forecasting. Every three hours the Imager takes a picture of the full disk of the Earth. This animation shows a sequence of these full disk images in the 6.47 to 7.02 micron wavelength band, during the period that Hurricane Katrina passed through the Gulf of Mexico. This wavelength band is useful for estimating mid-level water vapor content and for observing atmospheric motion in that level. |
| Completed |
2005-08-29 |
|
GOES-12 Imagery of Hurricane
| Title |
GOES-12 Imagery of Hurricane Katrina: Full Disk Longwave Infrared (WMS) |
| Abstract |
The GOES-12 satellite sits at 75 degrees west longitude at an altitude of 36,000 kilometers over the equator, in geosynchronous orbit. At this position its Imager instrument takes pictures of cloud patterns in several wavelengths for all of North and South America, a primary measurement used in weather forecasting. Every three hours the Imager takes a picture of the full disk of the Earth. This animation shows a sequence of these full disk images in the longwave infrared wavelengths, from 10.2 to 11.2 microns, during the period that Hurricane Katrina passed through the Gulf of Mexico. This wavelength band is the most common one for observing cloud motions and severe storms throughout the day and night. |
| Completed |
2005-08-29 |
|
Global Infrared Cloud Cover,
| Title |
Global Infrared Cloud Cover, September 2001 (WMS) |
| Abstract |
This animation is a mosaic of cloud cover data taken by several different satellites in the infrared band. One of the most prominent cloud features during this time was Hurricane Erin near the Atlantic coast of the United States. |
| Completed |
2004-02-11 |
|
SeaWiFS: Typhoon Bilis
| Title |
SeaWiFS: Typhoon Bilis |
| Abstract |
'Super' Typhoon Bilis was one of the largest Typhoons on record. On August 23, 2000, it slammed Taiwan on its way to China. |
| Completed |
2000-08-15 |
|
SeaWiFS: Typhoon Bilis
| Title |
SeaWiFS: Typhoon Bilis |
| Abstract |
'Super' Typhoon Bilis was one of the largest Typhoons on record. On August 23, 2000, it slammed Taiwan on its way to China. |
| Completed |
2000-08-15 |
|
RHESSI and TRACE View of Jan
| Title |
RHESSI and TRACE View of January 20, 2005 Solar Flare |
| Abstract |
RHESSI spacecraft images of gamma-rays (blue) and X-rays (red) thrown off by the hottest part of the flare are shown with UV images from the TRACE spacecraft. The gamma rays are made by energetic protons at the Sun. Scientists were surprised that the gamma rays matched the energy spectrum of protons at Earth: the proton storm may have come directly from the Sun and not from the CME as anticipated. |
| Completed |
2005-05-19 |
|
Scene Identification Compare
| Title |
Scene Identification Compared to Clouds (WMS) |
| Abstract |
The Earth's climate is determined by energy transfer from the sun to the Earth's land, oceans, and atmosphere. As the Earth rotates, the sun lights up only part of the Earth at a time, and some of that incoming solar energy is reflected and some is absorbed, depending on type of area it lights. The amount of reflection and absorption is critical to the climate. An instrument named CERES orbits the Earth every 99 minutes and measures the reflected solar energy. This animation shows the scene identification as measured by CERES during 29 orbits on June 20 and 21 of 2003. By comparing the incoming solar radiation with the outgoing reflected and thermal radiation, it is possible to identify the type of area being viewed, whether it be land, clouds, ocean, or ice. This scene identification is used together with the radiation flux measurements to build up a complete picture of the Earth's energy budget over time. |
| Completed |
2005-06-21 |
|
Scene Identification Compare
| Title |
Scene Identification Compared to Clouds (WMS) |
| Abstract |
The Earth's climate is determined by energy transfer from the sun to the Earth's land, oceans, and atmosphere. As the Earth rotates, the sun lights up only part of the Earth at a time, and some of that incoming solar energy is reflected and some is absorbed, depending on type of area it lights. The amount of reflection and absorption is critical to the climate. An instrument named CERES orbits the Earth every 99 minutes and measures the reflected solar energy. This animation shows the scene identification as measured by CERES during 29 orbits on June 20 and 21 of 2003. By comparing the incoming solar radiation with the outgoing reflected and thermal radiation, it is possible to identify the type of area being viewed, whether it be land, clouds, ocean, or ice. This scene identification is used together with the radiation flux measurements to build up a complete picture of the Earth's energy budget over time. |
| Completed |
2005-06-21 |
|
Hurricane Rita Sea Surface T
| Title |
Hurricane Rita Sea Surface Temperature and Clouds |
| Abstract |
This visualization shows the sea surface temperatures during Hurricane Rita. The data is from Septemeber 17 through 22, 2005. The colors on the ocean represent the sea surface temperatures, and satellite images of the hurricane clouds are laid over the temperatures to clearly show the hurricane positions. Orange and red depict regions that are 82 degrees F and higher, where the ocean is warm enough for hurricanes to form. Hurricane winds are sustained by the heat energy of the ocean, so the ocean is cooled as the hurricane passes and the energy is extracted to power the winds. The sea surface temperatures are 3-day moving averages based on the AMSR-E instrument on the Aqua satellite, while the cloud images were taken by the Imager on the GOES-12 satellite. |
| Completed |
2005-09-22 |
|
Hurricane Rita Sea Surface T
| Title |
Hurricane Rita Sea Surface Temperature and Clouds |
| Abstract |
This visualization shows the sea surface temperatures during Hurricane Rita. The data is from Septemeber 17 through 22, 2005. The colors on the ocean represent the sea surface temperatures, and satellite images of the hurricane clouds are laid over the temperatures to clearly show the hurricane positions. Orange and red depict regions that are 82 degrees F and higher, where the ocean is warm enough for hurricanes to form. Hurricane winds are sustained by the heat energy of the ocean, so the ocean is cooled as the hurricane passes and the energy is extracted to power the winds. The sea surface temperatures are 3-day moving averages based on the AMSR-E instrument on the Aqua satellite, while the cloud images were taken by the Imager on the GOES-12 satellite. |
| Completed |
2005-09-22 |
|
Hurricane Rita Sea Surface T
| Title |
Hurricane Rita Sea Surface Temperature and Clouds |
| Abstract |
This visualization shows the sea surface temperatures during Hurricane Rita. The data is from Septemeber 17 through 22, 2005. The colors on the ocean represent the sea surface temperatures, and satellite images of the hurricane clouds are laid over the temperatures to clearly show the hurricane positions. Orange and red depict regions that are 82 degrees F and higher, where the ocean is warm enough for hurricanes to form. Hurricane winds are sustained by the heat energy of the ocean, so the ocean is cooled as the hurricane passes and the energy is extracted to power the winds. The sea surface temperatures are 3-day moving averages based on the AMSR-E instrument on the Aqua satellite, while the cloud images were taken by the Imager on the GOES-12 satellite. |
| Completed |
2005-09-22 |
|
Hurricane Rita Sea Surface T
| Title |
Hurricane Rita Sea Surface Temperature and Clouds |
| Abstract |
This visualization shows the sea surface temperatures during Hurricane Rita. The data is from Septemeber 17 through 22, 2005. The colors on the ocean represent the sea surface temperatures, and satellite images of the hurricane clouds are laid over the temperatures to clearly show the hurricane positions. Orange and red depict regions that are 82 degrees F and higher, where the ocean is warm enough for hurricanes to form. Hurricane winds are sustained by the heat energy of the ocean, so the ocean is cooled as the hurricane passes and the energy is extracted to power the winds. The sea surface temperatures are 3-day moving averages based on the AMSR-E instrument on the Aqua satellite, while the cloud images were taken by the Imager on the GOES-12 satellite. |
| Completed |
2005-09-22 |
|
Hurricane Rita Sea Surface T
| Title |
Hurricane Rita Sea Surface Temperature and Clouds |
| Abstract |
This visualization shows the sea surface temperatures during Hurricane Rita. The data is from Septemeber 17 through 22, 2005. The colors on the ocean represent the sea surface temperatures, and satellite images of the hurricane clouds are laid over the temperatures to clearly show the hurricane positions. Orange and red depict regions that are 82 degrees F and higher, where the ocean is warm enough for hurricanes to form. Hurricane winds are sustained by the heat energy of the ocean, so the ocean is cooled as the hurricane passes and the energy is extracted to power the winds. The sea surface temperatures are 3-day moving averages based on the AMSR-E instrument on the Aqua satellite, while the cloud images were taken by the Imager on the GOES-12 satellite. |
| Completed |
2005-09-22 |
|
TRMM Tropical Microwave Imag
| Title |
TRMM Tropical Microwave Imager (TMI) sees the power of Hurricane Jeanne On September 26, 2004 |
| Abstract |
NASA's TRMM spacecraft is used by meteorologists to understand It looks underneath of the storm's clouds to reveal the underlying rain structure. Blue represents areas with at least 0.25 inches of rain per hour. Green shows at least 0.5 inches of rain per hour. Yellow is at least 1.0 inches of rain and red is at least 2.0 inches of rain per hour. |
| Completed |
2004-09-27 |
|
TRMM Tropical Microwave Imag
| Title |
TRMM Tropical Microwave Imager (TMI) sees the power of Hurricane Jeanne On September 26, 2004 |
| Abstract |
NASA's TRMM spacecraft is used by meteorologists to understand It looks underneath of the storm's clouds to reveal the underlying rain structure. Blue represents areas with at least 0.25 inches of rain per hour. Green shows at least 0.5 inches of rain per hour. Yellow is at least 1.0 inches of rain and red is at least 2.0 inches of rain per hour. |
| Completed |
2004-09-27 |
|
TRMM Tropical Microwave Imag
| Title |
TRMM Tropical Microwave Imager (TMI) sees the power of Hurricane Jeanne On September 26, 2004 |
| Abstract |
NASA's TRMM spacecraft is used by meteorologists to understand It looks underneath of the storm's clouds to reveal the underlying rain structure. Blue represents areas with at least 0.25 inches of rain per hour. Green shows at least 0.5 inches of rain per hour. Yellow is at least 1.0 inches of rain and red is at least 2.0 inches of rain per hour. |
| Completed |
2004-09-27 |
|
TRMM Tropical Microwave Imag
| Title |
TRMM Tropical Microwave Imager (TMI) sees the power of Hurricane Jeanne On September 26, 2004 |
| Abstract |
NASA's TRMM spacecraft is used by meteorologists to understand It looks underneath of the storm's clouds to reveal the underlying rain structure. Blue represents areas with at least 0.25 inches of rain per hour. Green shows at least 0.5 inches of rain per hour. Yellow is at least 1.0 inches of rain and red is at least 2.0 inches of rain per hour. |
| Completed |
2004-09-27 |
|
TRMM Tropical Microwave Imag
| Title |
TRMM Tropical Microwave Imager (TMI) sees the power of Hurricane Jeanne On September 26, 2004 |
| Abstract |
NASA's TRMM spacecraft is used by meteorologists to understand It looks underneath of the storm's clouds to reveal the underlying rain structure. Blue represents areas with at least 0.25 inches of rain per hour. Green shows at least 0.5 inches of rain per hour. Yellow is at least 1.0 inches of rain and red is at least 2.0 inches of rain per hour. |
| Completed |
2004-09-27 |
|
TRMM Tropical Microwave Imag
| Title |
TRMM Tropical Microwave Imager (TMI) sees the power of Hurricane Jeanne On September 26, 2004 |
| Abstract |
NASA's TRMM spacecraft is used by meteorologists to understand It looks underneath of the storm's clouds to reveal the underlying rain structure. Blue represents areas with at least 0.25 inches of rain per hour. Green shows at least 0.5 inches of rain per hour. Yellow is at least 1.0 inches of rain and red is at least 2.0 inches of rain per hour. |
| Completed |
2004-09-27 |
|
South Pole Sea Ice 1990-1999
| Title |
South Pole Sea Ice 1990-1999 |
| Abstract |
Animation of ten years of sea ice data, from the Defense Meteorological Satellite Program (DMSP) Special Sensor Microwave Imager (SSMI). |
| Completed |
2002-03-28 |
|
South Pole Sea Ice 1990-1999
| Title |
South Pole Sea Ice 1990-1999 |
| Abstract |
Animation of ten years of sea ice data, from the Defense Meteorological Satellite Program (DMSP) Special Sensor Microwave Imager (SSMI). |
| Completed |
2002-03-28 |
|
Hurricane Ivan Rainfall Stru
| Title |
Hurricane Ivan Rainfall Structure on September 13, 2004 |
| Completed |
2004-09-13 |
|
Hurricane Ivan Rainfall Stru
| Title |
Hurricane Ivan Rainfall Structure on September 13, 2004 |
| Completed |
2004-09-13 |
|
Hurricane Ivan Rainfall Stru
| Title |
Hurricane Ivan Rainfall Structure on September 13, 2004 |
| Completed |
2004-09-13 |
|
Hurricane Ivan Rainfall Stru
| Title |
Hurricane Ivan Rainfall Structure on September 13, 2004 |
| Completed |
2004-09-13 |
|
Hurricane Ivan Rainfall Stru
| Title |
Hurricane Ivan Rainfall Structure on September 13, 2004 |
| Completed |
2004-09-13 |
|
Outgoing Shortwave Flux Comp
| Title |
Outgoing Shortwave Flux Compared to Clouds (WMS) |
| Abstract |
The Earth's climate is determined by energy transfer from the sun to the Earth's land, oceans, and atmosphere. As the Earth rotates, the sun lights up only part of the Earth at a time, and some of that incoming solar energy is reflected and some is absorbed, depending on type of area it lights. The amount of reflection and absorption is critical to the climate. An instrument named CERES orbits the Earth every 99 minutes and measures the reflected solar energy. This animation shows the reflected solar radiation measured by CERES during 29 orbits on June 20 and 21 of 2003 over infrared cloud images for the same period. Reflected solar radiation is shortwave radiation, and the most intense reflection comes from clouds. |
| Completed |
2005-06-20 |
|
Outgoing Shortwave Flux Comp
| Title |
Outgoing Shortwave Flux Compared to Clouds (WMS) |
| Abstract |
The Earth's climate is determined by energy transfer from the sun to the Earth's land, oceans, and atmosphere. As the Earth rotates, the sun lights up only part of the Earth at a time, and some of that incoming solar energy is reflected and some is absorbed, depending on type of area it lights. The amount of reflection and absorption is critical to the climate. An instrument named CERES orbits the Earth every 99 minutes and measures the reflected solar energy. This animation shows the reflected solar radiation measured by CERES during 29 orbits on June 20 and 21 of 2003 over infrared cloud images for the same period. Reflected solar radiation is shortwave radiation, and the most intense reflection comes from clouds. |
| Completed |
2005-06-20 |
|
NASA Scientists Research Glo
| Title |
NASA Scientists Research Global Precipitation |
| Abstract |
The Global Precipitation Climatology Project (GPCP) is an element of the Global Energy and Water Cycle Experiment (GEWEX) of the World Climate Research program (WCRP). It was established by the WCRP in 1986 with the initial goal of providing monthly mean precipitation data on a 2.5°× 2.5°latitude -longitude grid. Monthly mean precipitation estimates are being produced beginning in 1979 and planned to go through 2005. The GPCP has accomplished this by merging infrared and microwave satellite estimates of precipitation with rain gauge data from more than 6,000 stations. Infrared precipitation estimates are obtained from GOES (United States), GMS (Japan) and Meteosat (European Community) geostationary satellites and National Oceanic and Atmospheric Administration (NOAA) operational polar orbiting satellites. Microwave estimates are obtained from the U.S. Defense Meteorological Satellite Program (DMSP) satellites using the Special Sensor Microwave Imager (SSM/I). These data sets will be used to validate general circulation and climate models, study the global hydrological cycle and diagnose the variability of the global climate system. Data sets have been expanded so that in addition to the monthly mean product available, the GPCP now has a 2.5°×2.5° degree pentad data set starting in 1979 and a 1°×1° daily data set starting in 1997. |
| Completed |
2007-09-14 |
|
NASA Scientists Research Glo
| Title |
NASA Scientists Research Global Precipitation |
| Abstract |
The Global Precipitation Climatology Project (GPCP) is an element of the Global Energy and Water Cycle Experiment (GEWEX) of the World Climate Research program (WCRP). It was established by the WCRP in 1986 with the initial goal of providing monthly mean precipitation data on a 2.5°× 2.5°latitude -longitude grid. Monthly mean precipitation estimates are being produced beginning in 1979 and planned to go through 2005. The GPCP has accomplished this by merging infrared and microwave satellite estimates of precipitation with rain gauge data from more than 6,000 stations. Infrared precipitation estimates are obtained from GOES (United States), GMS (Japan) and Meteosat (European Community) geostationary satellites and National Oceanic and Atmospheric Administration (NOAA) operational polar orbiting satellites. Microwave estimates are obtained from the U.S. Defense Meteorological Satellite Program (DMSP) satellites using the Special Sensor Microwave Imager (SSM/I). These data sets will be used to validate general circulation and climate models, study the global hydrological cycle and diagnose the variability of the global climate system. Data sets have been expanded so that in addition to the monthly mean product available, the GPCP now has a 2.5°×2.5° degree pentad data set starting in 1979 and a 1°×1° daily data set starting in 1997. |
| Completed |
2007-09-14 |
|
NASA Scientists Research Glo
| Title |
NASA Scientists Research Global Precipitation |
| Abstract |
The Global Precipitation Climatology Project (GPCP) is an element of the Global Energy and Water Cycle Experiment (GEWEX) of the World Climate Research program (WCRP). It was established by the WCRP in 1986 with the initial goal of providing monthly mean precipitation data on a 2.5°× 2.5°latitude -longitude grid. Monthly mean precipitation estimates are being produced beginning in 1979 and planned to go through 2005. The GPCP has accomplished this by merging infrared and microwave satellite estimates of precipitation with rain gauge data from more than 6,000 stations. Infrared precipitation estimates are obtained from GOES (United States), GMS (Japan) and Meteosat (European Community) geostationary satellites and National Oceanic and Atmospheric Administration (NOAA) operational polar orbiting satellites. Microwave estimates are obtained from the U.S. Defense Meteorological Satellite Program (DMSP) satellites using the Special Sensor Microwave Imager (SSM/I). These data sets will be used to validate general circulation and climate models, study the global hydrological cycle and diagnose the variability of the global climate system. Data sets have been expanded so that in addition to the monthly mean product available, the GPCP now has a 2.5°×2.5° degree pentad data set starting in 1979 and a 1°×1° daily data set starting in 1997. |
| Completed |
2007-09-14 |
|
NASA Scientists Research Glo
| Title |
NASA Scientists Research Global Precipitation |
| Abstract |
The Global Precipitation Climatology Project (GPCP) is an element of the Global Energy and Water Cycle Experiment (GEWEX) of the World Climate Research program (WCRP). It was established by the WCRP in 1986 with the initial goal of providing monthly mean precipitation data on a 2.5°× 2.5°latitude -longitude grid. Monthly mean precipitation estimates are being produced beginning in 1979 and planned to go through 2005. The GPCP has accomplished this by merging infrared and microwave satellite estimates of precipitation with rain gauge data from more than 6,000 stations. Infrared precipitation estimates are obtained from GOES (United States), GMS (Japan) and Meteosat (European Community) geostationary satellites and National Oceanic and Atmospheric Administration (NOAA) operational polar orbiting satellites. Microwave estimates are obtained from the U.S. Defense Meteorological Satellite Program (DMSP) satellites using the Special Sensor Microwave Imager (SSM/I). These data sets will be used to validate general circulation and climate models, study the global hydrological cycle and diagnose the variability of the global climate system. Data sets have been expanded so that in addition to the monthly mean product available, the GPCP now has a 2.5°×2.5° degree pentad data set starting in 1979 and a 1°×1° daily data set starting in 1997. |
| Completed |
2007-09-14 |
|
NASA Scientists Research Glo
| Title |
NASA Scientists Research Global Precipitation |
| Abstract |
The Global Precipitation Climatology Project (GPCP) is an element of the Global Energy and Water Cycle Experiment (GEWEX) of the World Climate Research program (WCRP). It was established by the WCRP in 1986 with the initial goal of providing monthly mean precipitation data on a 2.5°× 2.5°latitude -longitude grid. Monthly mean precipitation estimates are being produced beginning in 1979 and planned to go through 2005. The GPCP has accomplished this by merging infrared and microwave satellite estimates of precipitation with rain gauge data from more than 6,000 stations. Infrared precipitation estimates are obtained from GOES (United States), GMS (Japan) and Meteosat (European Community) geostationary satellites and National Oceanic and Atmospheric Administration (NOAA) operational polar orbiting satellites. Microwave estimates are obtained from the U.S. Defense Meteorological Satellite Program (DMSP) satellites using the Special Sensor Microwave Imager (SSM/I). These data sets will be used to validate general circulation and climate models, study the global hydrological cycle and diagnose the variability of the global climate system. Data sets have been expanded so that in addition to the monthly mean product available, the GPCP now has a 2.5°×2.5° degree pentad data set starting in 1979 and a 1°×1° daily data set starting in 1997. |
| Completed |
2007-09-14 |
|
NASA Scientists Research Glo
| Title |
NASA Scientists Research Global Precipitation |
| Abstract |
The Global Precipitation Climatology Project (GPCP) is an element of the Global Energy and Water Cycle Experiment (GEWEX) of the World Climate Research program (WCRP). It was established by the WCRP in 1986 with the initial goal of providing monthly mean precipitation data on a 2.5°× 2.5°latitude -longitude grid. Monthly mean precipitation estimates are being produced beginning in 1979 and planned to go through 2005. The GPCP has accomplished this by merging infrared and microwave satellite estimates of precipitation with rain gauge data from more than 6,000 stations. Infrared precipitation estimates are obtained from GOES (United States), GMS (Japan) and Meteosat (European Community) geostationary satellites and National Oceanic and Atmospheric Administration (NOAA) operational polar orbiting satellites. Microwave estimates are obtained from the U.S. Defense Meteorological Satellite Program (DMSP) satellites using the Special Sensor Microwave Imager (SSM/I). These data sets will be used to validate general circulation and climate models, study the global hydrological cycle and diagnose the variability of the global climate system. Data sets have been expanded so that in addition to the monthly mean product available, the GPCP now has a 2.5°×2.5° degree pentad data set starting in 1979 and a 1°×1° daily data set starting in 1997. |
| Completed |
2007-09-14 |
|
NASA Scientists Research Glo
| Title |
NASA Scientists Research Global Precipitation |
| Abstract |
The Global Precipitation Climatology Project (GPCP) is an element of the Global Energy and Water Cycle Experiment (GEWEX) of the World Climate Research program (WCRP). It was established by the WCRP in 1986 with the initial goal of providing monthly mean precipitation data on a 2.5°× 2.5°latitude -longitude grid. Monthly mean precipitation estimates are being produced beginning in 1979 and planned to go through 2005. The GPCP has accomplished this by merging infrared and microwave satellite estimates of precipitation with rain gauge data from more than 6,000 stations. Infrared precipitation estimates are obtained from GOES (United States), GMS (Japan) and Meteosat (European Community) geostationary satellites and National Oceanic and Atmospheric Administration (NOAA) operational polar orbiting satellites. Microwave estimates are obtained from the U.S. Defense Meteorological Satellite Program (DMSP) satellites using the Special Sensor Microwave Imager (SSM/I). These data sets will be used to validate general circulation and climate models, study the global hydrological cycle and diagnose the variability of the global climate system. Data sets have been expanded so that in addition to the monthly mean product available, the GPCP now has a 2.5°×2.5° degree pentad data set starting in 1979 and a 1°×1° daily data set starting in 1997. |
| Completed |
2007-09-14 |
|
NASA Scientists Research Glo
| Title |
NASA Scientists Research Global Precipitation |
| Abstract |
The Global Precipitation Climatology Project (GPCP) is an element of the Global Energy and Water Cycle Experiment (GEWEX) of the World Climate Research program (WCRP). It was established by the WCRP in 1986 with the initial goal of providing monthly mean precipitation data on a 2.5°× 2.5°latitude -longitude grid. Monthly mean precipitation estimates are being produced beginning in 1979 and planned to go through 2005. The GPCP has accomplished this by merging infrared and microwave satellite estimates of precipitation with rain gauge data from more than 6,000 stations. Infrared precipitation estimates are obtained from GOES (United States), GMS (Japan) and Meteosat (European Community) geostationary satellites and National Oceanic and Atmospheric Administration (NOAA) operational polar orbiting satellites. Microwave estimates are obtained from the U.S. Defense Meteorological Satellite Program (DMSP) satellites using the Special Sensor Microwave Imager (SSM/I). These data sets will be used to validate general circulation and climate models, study the global hydrological cycle and diagnose the variability of the global climate system. Data sets have been expanded so that in addition to the monthly mean product available, the GPCP now has a 2.5°×2.5° degree pentad data set starting in 1979 and a 1°×1° daily data set starting in 1997. |
| Completed |
2007-09-14 |
|
NASA Scientists Research Glo
| Title |
NASA Scientists Research Global Precipitation |
| Abstract |
The Global Precipitation Climatology Project (GPCP) is an element of the Global Energy and Water Cycle Experiment (GEWEX) of the World Climate Research program (WCRP). It was established by the WCRP in 1986 with the initial goal of providing monthly mean precipitation data on a 2.5°× 2.5°latitude -longitude grid. Monthly mean precipitation estimates are being produced beginning in 1979 and planned to go through 2005. The GPCP has accomplished this by merging infrared and microwave satellite estimates of precipitation with rain gauge data from more than 6,000 stations. Infrared precipitation estimates are obtained from GOES (United States), GMS (Japan) and Meteosat (European Community) geostationary satellites and National Oceanic and Atmospheric Administration (NOAA) operational polar orbiting satellites. Microwave estimates are obtained from the U.S. Defense Meteorological Satellite Program (DMSP) satellites using the Special Sensor Microwave Imager (SSM/I). These data sets will be used to validate general circulation and climate models, study the global hydrological cycle and diagnose the variability of the global climate system. Data sets have been expanded so that in addition to the monthly mean product available, the GPCP now has a 2.5°×2.5° degree pentad data set starting in 1979 and a 1°×1° daily data set starting in 1997. |
| Completed |
2007-09-14 |
|
NASA Scientists Research Glo
| Title |
NASA Scientists Research Global Precipitation |
| Abstract |
The Global Precipitation Climatology Project (GPCP) is an element of the Global Energy and Water Cycle Experiment (GEWEX) of the World Climate Research program (WCRP). It was established by the WCRP in 1986 with the initial goal of providing monthly mean precipitation data on a 2.5°× 2.5°latitude -longitude grid. Monthly mean precipitation estimates are being produced beginning in 1979 and planned to go through 2005. The GPCP has accomplished this by merging infrared and microwave satellite estimates of precipitation with rain gauge data from more than 6,000 stations. Infrared precipitation estimates are obtained from GOES (United States), GMS (Japan) and Meteosat (European Community) geostationary satellites and National Oceanic and Atmospheric Administration (NOAA) operational polar orbiting satellites. Microwave estimates are obtained from the U.S. Defense Meteorological Satellite Program (DMSP) satellites using the Special Sensor Microwave Imager (SSM/I). These data sets will be used to validate general circulation and climate models, study the global hydrological cycle and diagnose the variability of the global climate system. Data sets have been expanded so that in addition to the monthly mean product available, the GPCP now has a 2.5°×2.5° degree pentad data set starting in 1979 and a 1°×1° daily data set starting in 1997. |
| Completed |
2007-09-14 |
|
NASA Scientists Research Glo
| Title |
NASA Scientists Research Global Precipitation |
| Abstract |
The Global Precipitation Climatology Project (GPCP) is an element of the Global Energy and Water Cycle Experiment (GEWEX) of the World Climate Research program (WCRP). It was established by the WCRP in 1986 with the initial goal of providing monthly mean precipitation data on a 2.5°× 2.5°latitude -longitude grid. Monthly mean precipitation estimates are being produced beginning in 1979 and planned to go through 2005. The GPCP has accomplished this by merging infrared and microwave satellite estimates of precipitation with rain gauge data from more than 6,000 stations. Infrared precipitation estimates are obtained from GOES (United States), GMS (Japan) and Meteosat (European Community) geostationary satellites and National Oceanic and Atmospheric Administration (NOAA) operational polar orbiting satellites. Microwave estimates are obtained from the U.S. Defense Meteorological Satellite Program (DMSP) satellites using the Special Sensor Microwave Imager (SSM/I). These data sets will be used to validate general circulation and climate models, study the global hydrological cycle and diagnose the variability of the global climate system. Data sets have been expanded so that in addition to the monthly mean product available, the GPCP now has a 2.5°×2.5° degree pentad data set starting in 1979 and a 1°×1° daily data set starting in 1997. |
| Completed |
2007-09-14 |
|
NASA Scientists Research Glo
| Title |
NASA Scientists Research Global Precipitation |
| Abstract |
The Global Precipitation Climatology Project (GPCP) is an element of the Global Energy and Water Cycle Experiment (GEWEX) of the World Climate Research program (WCRP). It was established by the WCRP in 1986 with the initial goal of providing monthly mean precipitation data on a 2.5°× 2.5°latitude -longitude grid. Monthly mean precipitation estimates are being produced beginning in 1979 and planned to go through 2005. The GPCP has accomplished this by merging infrared and microwave satellite estimates of precipitation with rain gauge data from more than 6,000 stations. Infrared precipitation estimates are obtained from GOES (United States), GMS (Japan) and Meteosat (European Community) geostationary satellites and National Oceanic and Atmospheric Administration (NOAA) operational polar orbiting satellites. Microwave estimates are obtained from the U.S. Defense Meteorological Satellite Program (DMSP) satellites using the Special Sensor Microwave Imager (SSM/I). These data sets will be used to validate general circulation and climate models, study the global hydrological cycle and diagnose the variability of the global climate system. Data sets have been expanded so that in addition to the monthly mean product available, the GPCP now has a 2.5°×2.5° degree pentad data set starting in 1979 and a 1°×1° daily data set starting in 1997. |
| Completed |
2007-09-14 |
|
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