This animation displays one year of Outgoing Long-wave Radiation (OLR) Terra-CERES data ...
This animation displays one year of Outgoing Long-wave Radiation (OLR) Terra-CERES data (March 1, 2000 to May 25, 2001) with a 14-day boxcar average. Endpoints have the average re-weighted for the smaller amount of data. The data are 2.5 degree resolution.
This animation displays one year of Reflected Solar Radiation (RSR) Terra-CERES data ...
This animation displays one year of Reflected Solar Radiation (RSR) Terra-CERES data (March 1, 2000 to May 25, 2001) with a 14-day boxcar average. Endpoints have the average re-weighted for the smaller amount of data. The data are 2.5 degree resolution.
In this animation of total ozone, the luminance values of the colors ...
In this animation of total ozone, the luminance values of the colors bounding areas of missing data are used in interpolating over these regions. The missing data are mapped to the grayscale portion of the color map.
In this animation of total ozone, the luminance values of the colors ...
In this animation of total ozone, the luminance values of the colors bounding areas of missing data are used in interpolating over these regions. The missing data are mapped to the grayscale portion of the color map.
In this animation of total ozone, the luminance values of the colors ...
In this animation of total ozone, the luminance values of the colors bounding areas of missing data are used in interpolating over these regions. The missing data are mapped to the grayscale portion of the color map.
El Nino, a periodic warming of the Eastern Pacific Ocean, is among ...
El Nino, a periodic warming of the Eastern Pacific Ocean, is among Earths most powerful phenomena. Satellite, ship, and buoy observations show the 1997-98 event as the strongest on record. Visualizing how sea-surface height, sea-surface temperature, and sea-surface winds differ from normal conditions reveals the events magnitude.
TOMS provides dramatic visual evidence of the annual growth and decay of ...
TOMS provides dramatic visual evidence of the annual growth and decay of the Antarctic ozone hole. The ozone losses over Antarctica result from reactions with the products of man-made chlorine and bromine compounds. Because of the tilt of the Earths axis, continuous darkness falls at the South Pole from March 21 to September 21. The dark region in the middle of the July 1 total ozone picture is polar night, where TOMS cannot make measurements. Ozone losses are in blue. Beginning in August, returning sunlight reaches the edges of Antarctica providing chlorine and bromine compounds with energy to rapidly destroy ozone. By mid September, the ozone loss peaks, creating an ozone hole over Antarctic. For more information see www.gsfc.nasa.gov-topstory-2003-1208toms.html
Here the 20-year seasonal surface temperature trend for the autumn is shown ...
Here the 20-year seasonal surface temperature trend for the autumn is shown over the Arctic region. This animation shows the warming and cooling regions in steps from the regions of least change to the areas of greatest change. Blue hues indicate cooling regions; red hues depict warming. Light regions indicate less change while darker regions indicate more. The temperature scale used ranges from -0.4 to +0.4 degrees Celsius in increments of .02 degrees. (See color bar below)
Here the 20-year seasonal surface temperature trend for the spring is shown ...
Here the 20-year seasonal surface temperature trend for the spring is shown over the Arctic region. This animation shows the warming and cooling regions in steps from the regions of least change to the areas of greatest change. Blue hues indicate cooling regions; red hues depict warming. Light regions indicate less change while darker regions indicate more. The temperature scale used ranges from -0.4 to +0.4 degrees Celsius in increments of .02 degrees. (See color bar below)
Here the 20-year seasonal surface temperature trend for the summer is shown ...
Here the 20-year seasonal surface temperature trend for the summer is shown over the Arctic region. This animation shows the warming and cooling regions in steps from the regions of least change to the areas of greatest change. Blue hues indicate cooling regions; red hues depict warming. Light regions indicate less change while darker regions indicate more. The temperature scale used ranges from -0.4 to +0.4 degrees Celsius in increments of .02 degrees. (See color bar below)
Here the 20-year surface temperature trend is shown over the Arctic region. ...
Here the 20-year surface temperature trend is shown over the Arctic region. This animation shows the warming and cooling regions in steps from the regions of least change to the areas of greatest change. Blue hues indicate cooling regions; red hues depict warming. Light regions indicate less change while darker regions indicate more. The temperature scale used ranges from -0.4 to +0.4 degrees Celsius in increments of .02 degrees. (See color bar below)
Here the 20-year seasonal surface temperature trend for the winter is shown ...
Here the 20-year seasonal surface temperature trend for the winter is shown over the Arctic region. This animation shows the warming and cooling regions in steps from the regions of least change to the areas of greatest change. Blue hues indicate cooling regions; red hues depict warming. Light regions indicate less change while darker regions indicate more. The temperature scale used ranges from -0.4 to +0.4 degrees Celsius in increments of .02 degrees. (See color bar below)
This image shows the 22-year surface temperature trend over the Arctic region. ...
This image shows the 22-year surface temperature trend over the Arctic region. Blue hues indicate areas that are cooling; gold hues depict areas that are warming. Lighter colors indicate less change while darker colors indicate more. The temperature scale steps from zero degrees Celsius in increments of .02 degrees. (See color bar below) The data ranges from -0.162 to +0.487 degrees Celsius.
This series of animations shows a two-dimensional unstructured mesh particle-magneto-hydrodynamic solar wind ...
This series of animations shows a two-dimensional unstructured mesh particle-magneto-hydrodynamic solar wind flow simulation of the interaction of the solar wind with the Earths magnetosphere.
This series of animations shows a two-dimensional unstructured mesh particle-magneto-hydrodynamic solar wind ...
This series of animations shows a two-dimensional unstructured mesh particle-magneto-hydrodynamic solar wind flow simulation of the interaction of the solar wind with the Earths magnetosphere.
Zoom in showing true color, then changing to daytime thermal, then nighttime ...
Zoom in showing true color, then changing to daytime thermal, then nighttime thermal, using mountain top, Landsat, ATLAS thermal, land use, and clouds-convection data
Teaching sign language using two-dimensional images can be difficult due to the ...
Teaching sign language using two-dimensional images can be difficult due to the fact that manual signing is both three-dimensional and time dependent. A prototype demonstration was created to teach the manual alphabet using web-based VRML objects.
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