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Images of Atlantic Ocean and Goddard Space Flight Center (GSFC)
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Global Large-scale Precipita
| Title |
Global Large-scale Precipitation during Hurricane Frances (WMS) |
| Abstract |
Water vapor is a small but significant constituent of the atmosphere, warming the planet due to the greenhouse effect and condensing to form clouds. As moisture-laden air rises, the relative humidity increases until it saturates the air, at which time precipitation occurs. If the uplift of air is due to large-scale atmospheric motion, then the precipitation is called large-scale, or dynamic. This animation shows the large-scale precipitation for the whole globe from September 1, 2004, through September 5, 2004, during the period of Hurricane Frances in the western Atlantic Ocean and Typhoon Songda in the western Pacific Ocean. Large-scale precipitation tends to be continuous and to come from decks of stratus clouds rather than from thunderstorms. |
| Completed |
2005-07-28 |
|
Global Large-scale Precipita
| Title |
Global Large-scale Precipitation during Hurricane Frances (WMS) |
| Abstract |
Water vapor is a small but significant constituent of the atmosphere, warming the planet due to the greenhouse effect and condensing to form clouds. As moisture-laden air rises, the relative humidity increases until it saturates the air, at which time precipitation occurs. If the uplift of air is due to large-scale atmospheric motion, then the precipitation is called large-scale, or dynamic. This animation shows the large-scale precipitation for the whole globe from September 1, 2004, through September 5, 2004, during the period of Hurricane Frances in the western Atlantic Ocean and Typhoon Songda in the western Pacific Ocean. Large-scale precipitation tends to be continuous and to come from decks of stratus clouds rather than from thunderstorms. |
| Completed |
2005-07-28 |
|
Sequence of Clouds, Snow Cov
| Title |
Sequence of Clouds, Snow Cover, Sea Ice, Sea Surface Temperature and Biosphere |
| Abstract |
This animation is part of an NSF-funded, international project, Exploring Time. The two-hour television special, broadcast on the Discovery Channel in the spring of 2007, explores how the world changes over different timescales ... from billionths of seconds to billions of years. This animation portrays a variety of remotely sensed data elements at different temporal resolutions. Initially, the animation shows cloud cover in motion over North America in half-hour increments from Nov. 26 to Dec. 7, 2005. The temporal pace quickens to show a 5-day moving average of daily MODIS snow cover along with daily AMSR-E sea ice from Dec. 7, 2005 to Mar. 15, 2006. As the view swings south over the Gulf of Mexico, the AMSR-E Sea Surface Temperature reveals warming ocean temperatures from March through August, 2006. As it passes over the Atlantic Ocean, the biosphere fades into view, showing both chlorophyll concentration in the ocean along with Normalized Difference Vegetation Index over the land areas. The biosphere animates over time while the view pans over northern Africa and Europe, showing data collected from September 2002 through February 2006. This program was also broadcast in Japan through a partnership with the NHK international broadcasting service and in France through a partnership with the ARTE television network. |
| Completed |
2006-11-29 |
|
Sequence of Clouds, Snow Cov
| Title |
Sequence of Clouds, Snow Cover, Sea Ice, Sea Surface Temperature and Biosphere |
| Abstract |
This animation is part of an NSF-funded, international project, Exploring Time. The two-hour television special, broadcast on the Discovery Channel in the spring of 2007, explores how the world changes over different timescales ... from billionths of seconds to billions of years. This animation portrays a variety of remotely sensed data elements at different temporal resolutions. Initially, the animation shows cloud cover in motion over North America in half-hour increments from Nov. 26 to Dec. 7, 2005. The temporal pace quickens to show a 5-day moving average of daily MODIS snow cover along with daily AMSR-E sea ice from Dec. 7, 2005 to Mar. 15, 2006. As the view swings south over the Gulf of Mexico, the AMSR-E Sea Surface Temperature reveals warming ocean temperatures from March through August, 2006. As it passes over the Atlantic Ocean, the biosphere fades into view, showing both chlorophyll concentration in the ocean along with Normalized Difference Vegetation Index over the land areas. The biosphere animates over time while the view pans over northern Africa and Europe, showing data collected from September 2002 through February 2006. This program was also broadcast in Japan through a partnership with the NHK international broadcasting service and in France through a partnership with the ARTE television network. |
| Completed |
2006-11-29 |
|
Sequence of Clouds, Snow Cov
| Title |
Sequence of Clouds, Snow Cover, Sea Ice, Sea Surface Temperature and Biosphere |
| Abstract |
This animation is part of an NSF-funded, international project, Exploring Time. The two-hour television special, broadcast on the Discovery Channel in the spring of 2007, explores how the world changes over different timescales ... from billionths of seconds to billions of years. This animation portrays a variety of remotely sensed data elements at different temporal resolutions. Initially, the animation shows cloud cover in motion over North America in half-hour increments from Nov. 26 to Dec. 7, 2005. The temporal pace quickens to show a 5-day moving average of daily MODIS snow cover along with daily AMSR-E sea ice from Dec. 7, 2005 to Mar. 15, 2006. As the view swings south over the Gulf of Mexico, the AMSR-E Sea Surface Temperature reveals warming ocean temperatures from March through August, 2006. As it passes over the Atlantic Ocean, the biosphere fades into view, showing both chlorophyll concentration in the ocean along with Normalized Difference Vegetation Index over the land areas. The biosphere animates over time while the view pans over northern Africa and Europe, showing data collected from September 2002 through February 2006. This program was also broadcast in Japan through a partnership with the NHK international broadcasting service and in France through a partnership with the ARTE television network. |
| Completed |
2006-11-29 |
|
Sequence of Clouds, Snow Cov
| Title |
Sequence of Clouds, Snow Cover, Sea Ice, Sea Surface Temperature and Biosphere |
| Abstract |
This animation is part of an NSF-funded, international project, Exploring Time. The two-hour television special, broadcast on the Discovery Channel in the spring of 2007, explores how the world changes over different timescales ... from billionths of seconds to billions of years. This animation portrays a variety of remotely sensed data elements at different temporal resolutions. Initially, the animation shows cloud cover in motion over North America in half-hour increments from Nov. 26 to Dec. 7, 2005. The temporal pace quickens to show a 5-day moving average of daily MODIS snow cover along with daily AMSR-E sea ice from Dec. 7, 2005 to Mar. 15, 2006. As the view swings south over the Gulf of Mexico, the AMSR-E Sea Surface Temperature reveals warming ocean temperatures from March through August, 2006. As it passes over the Atlantic Ocean, the biosphere fades into view, showing both chlorophyll concentration in the ocean along with Normalized Difference Vegetation Index over the land areas. The biosphere animates over time while the view pans over northern Africa and Europe, showing data collected from September 2002 through February 2006. This program was also broadcast in Japan through a partnership with the NHK international broadcasting service and in France through a partnership with the ARTE television network. |
| Completed |
2006-11-29 |
|
Sequence of Clouds, Snow Cov
| Title |
Sequence of Clouds, Snow Cover, Sea Ice, Sea Surface Temperature and Biosphere |
| Abstract |
This animation is part of an NSF-funded, international project, Exploring Time. The two-hour television special, broadcast on the Discovery Channel in the spring of 2007, explores how the world changes over different timescales ... from billionths of seconds to billions of years. This animation portrays a variety of remotely sensed data elements at different temporal resolutions. Initially, the animation shows cloud cover in motion over North America in half-hour increments from Nov. 26 to Dec. 7, 2005. The temporal pace quickens to show a 5-day moving average of daily MODIS snow cover along with daily AMSR-E sea ice from Dec. 7, 2005 to Mar. 15, 2006. As the view swings south over the Gulf of Mexico, the AMSR-E Sea Surface Temperature reveals warming ocean temperatures from March through August, 2006. As it passes over the Atlantic Ocean, the biosphere fades into view, showing both chlorophyll concentration in the ocean along with Normalized Difference Vegetation Index over the land areas. The biosphere animates over time while the view pans over northern Africa and Europe, showing data collected from September 2002 through February 2006. This program was also broadcast in Japan through a partnership with the NHK international broadcasting service and in France through a partnership with the ARTE television network. |
| Completed |
2006-11-29 |
|
Sequence of Clouds, Snow Cov
| Title |
Sequence of Clouds, Snow Cover, Sea Ice, Sea Surface Temperature and Biosphere |
| Abstract |
This animation is part of an NSF-funded, international project, Exploring Time. The two-hour television special, broadcast on the Discovery Channel in the spring of 2007, explores how the world changes over different timescales ... from billionths of seconds to billions of years. This animation portrays a variety of remotely sensed data elements at different temporal resolutions. Initially, the animation shows cloud cover in motion over North America in half-hour increments from Nov. 26 to Dec. 7, 2005. The temporal pace quickens to show a 5-day moving average of daily MODIS snow cover along with daily AMSR-E sea ice from Dec. 7, 2005 to Mar. 15, 2006. As the view swings south over the Gulf of Mexico, the AMSR-E Sea Surface Temperature reveals warming ocean temperatures from March through August, 2006. As it passes over the Atlantic Ocean, the biosphere fades into view, showing both chlorophyll concentration in the ocean along with Normalized Difference Vegetation Index over the land areas. The biosphere animates over time while the view pans over northern Africa and Europe, showing data collected from September 2002 through February 2006. This program was also broadcast in Japan through a partnership with the NHK international broadcasting service and in France through a partnership with the ARTE television network. |
| Completed |
2006-11-29 |
|
Terra/MOPITT CO South Atlant
| Title |
Terra/MOPITT CO South Atlantic Transport |
| Abstract |
Carbon Monoxide (CO) can be seen flowing across the South Atlantic Ocean in measurements by the Terra/MOPITT instrument. |
| Completed |
2001-05-22 |
|
Terra/MOPITT CO South Atlant
| Title |
Terra/MOPITT CO South Atlantic Transport |
| Abstract |
Carbon Monoxide (CO) can be seen flowing across the South Atlantic Ocean in measurements by the Terra/MOPITT instrument. |
| Completed |
2001-05-22 |
|
Terra/MOPITT CO South Atlant
| Title |
Terra/MOPITT CO South Atlantic Transport |
| Abstract |
Carbon Monoxide (CO) can be seen flowing across the South Atlantic Ocean in measurements by the Terra/MOPITT instrument. |
| Completed |
2001-05-22 |
|
Terra/MOPITT CO South Atlant
| Title |
Terra/MOPITT CO South Atlantic Transport |
| Abstract |
Carbon Monoxide (CO) can be seen flowing across the South Atlantic Ocean in measurements by the Terra/MOPITT instrument. |
| Completed |
2001-05-22 |
|
Terra/MOPITT CO South Atlant
| Title |
Terra/MOPITT CO South Atlantic Transport |
| Abstract |
Carbon Monoxide (CO) can be seen flowing across the South Atlantic Ocean in measurements by the Terra/MOPITT instrument. |
| Completed |
2001-05-22 |
|
Terra/MOPITT CO South Atlant
| Title |
Terra/MOPITT CO South Atlantic Transport |
| Abstract |
Carbon Monoxide (CO) can be seen flowing across the South Atlantic Ocean in measurements by the Terra/MOPITT instrument. |
| Completed |
2001-05-22 |
|
Hurricane Frances Progressio
| Title |
Hurricane Frances Progression with Fixed View |
| Abstract |
Hurricane Frances races towards Florida and both the Terra and Aqua satellite are spectators. |
| Completed |
2004-09-03 |
|
Hurricane Frances Progressio
| Title |
Hurricane Frances Progression with a Fixed View |
| Abstract |
A fixed view of the Atlantic Ocean with Hurricane Frances sprinting towards Florida |
| Completed |
2004-09-07 |
|
Hurricane Frances Progressio
| Title |
Hurricane Frances Progression with a Fixed View |
| Abstract |
A fixed view of the Atlantic Ocean with Hurricane Frances sprinting towards Florida |
| Completed |
2004-09-07 |
|
Hurricane Frances Progressio
| Title |
Hurricane Frances Progression with a Fixed View |
| Abstract |
A fixed view of the Atlantic Ocean with Hurricane Frances sprinting towards Florida |
| Completed |
2004-09-07 |
|
Hurricane Frances Progressio
| Title |
Hurricane Frances Progression with a Fixed View |
| Abstract |
A fixed view of the Atlantic Ocean with Hurricane Frances sprinting towards Florida |
| Completed |
2004-09-07 |
|
Hurricane Frances Progressio
| Title |
Hurricane Frances Progression with a Fixed View |
| Abstract |
A fixed view of the Atlantic Ocean with Hurricane Frances sprinting towards Florida |
| Completed |
2004-09-07 |
|
Hurricane Frances Progressio
| Title |
Hurricane Frances Progression with a Fixed View |
| Abstract |
A fixed view of the Atlantic Ocean with Hurricane Frances sprinting towards Florida |
| Completed |
2004-09-07 |
|
Rainfall Accumulation from H
| Title |
Rainfall Accumulation from Hurricane Isabel (WMS) |
| Abstract |
Hurricane Isabel generated large amounts of rain over the Atlantic ocean as it approached East coast of the United States in September 2003. In fact, unlike many hurricanes, most of the Isabel's rainfall did not occur over land, flooding on land was caused mainly by storm surge. This animation shows accumulation of rainfall from the hurricane--each frame shows the total amount of rain since the start of the measurement period. Rain from other sources has been masked out, so the hurricane track is clearly visible as the storm moves across the Atlantic. |
| Completed |
2005-04-12 |
|
Hurricane Frances Progressio
| Title |
Hurricane Frances Progression with a Fixed View |
| Abstract |
A fixed view of the Atlantic Ocean with Hurricane Frances sprinting towards Florida |
| Completed |
2004-09-07 |
|
Rainfall Accumulation from H
| Title |
Rainfall Accumulation from Hurricane Isabel (WMS) |
| Abstract |
Hurricane Isabel generated large amounts of rain over the Atlantic ocean as it approached East coast of the United States in September 2003. In fact, unlike many hurricanes, most of the Isabel's rainfall did not occur over land, flooding on land was caused mainly by storm surge. This animation shows accumulation of rainfall from the hurricane--each frame shows the total amount of rain since the start of the measurement period. Rain from other sources has been masked out, so the hurricane track is clearly visible as the storm moves across the Atlantic. |
| Completed |
2005-04-12 |
|
Hurricane Frances Progressio
| Title |
Hurricane Frances Progression with a Fixed View |
| Abstract |
A fixed view of the Atlantic Ocean with Hurricane Frances sprinting towards Florida |
| Completed |
2004-09-07 |
|
Hurricane Frances Progressio
| Title |
Hurricane Frances Progression with a Fixed View |
| Abstract |
A fixed view of the Atlantic Ocean with Hurricane Frances sprinting towards Florida |
| Completed |
2004-09-07 |
|
Global Cloud Cover during Hu
| Title |
Global Cloud Cover during Hurricane Frances (WMS) |
| Abstract |
Water vapor is a small but significant constituent of the atmosphere, warming the planet due to the greenhouse effect and condensing to form clouds which both warm and cool the Earth in different circumstances. Warm, moisture-laden air moving out from the tropics brings clouds and rainfall to the temperate zones. This animation shows the cloud cover for the whole globe from September 1, 2004, through September 5, 2004, during the period of Hurricane Frances in the western Atlantic Ocean and Typhoon Songda in the western Pacific Ocean. The cloud cover in any region significantly affects the energy balance since sunlight reflected from the clouds is not available to heat the surface. The motion of clouds in this animation clearly indicates the speed and direction of winds around the globe. |
| Completed |
2005-07-25 |
|
Global Cloud Cover during Hu
| Title |
Global Cloud Cover during Hurricane Frances (WMS) |
| Abstract |
Water vapor is a small but significant constituent of the atmosphere, warming the planet due to the greenhouse effect and condensing to form clouds which both warm and cool the Earth in different circumstances. Warm, moisture-laden air moving out from the tropics brings clouds and rainfall to the temperate zones. This animation shows the cloud cover for the whole globe from September 1, 2004, through September 5, 2004, during the period of Hurricane Frances in the western Atlantic Ocean and Typhoon Songda in the western Pacific Ocean. The cloud cover in any region significantly affects the energy balance since sunlight reflected from the clouds is not available to heat the surface. The motion of clouds in this animation clearly indicates the speed and direction of winds around the globe. |
| Completed |
2005-07-25 |
|
AMSR-E Anomalous Atlantic Se
| Title |
AMSR-E Anomalous Atlantic Sea Surface Temperature Data Used to Forecast 2003 Hurricane Season |
| Abstract |
Researchers and forecasters often study sea surface temperatures for an indication of hurricane potential. Scientists say above normal Atlantic Ocean temperatures is one reason for the 'above normal' hurricane forecast. Hurricanes convert heat from the tropical atmosphere and oceans to wind and waves, just as a car engine converts gasoline into motion. These animations show a year in the life of global ocean temperatures, June 2, 2002, to May 11, 2003. Blue indicates the coolest water anomaly, red the warmest anomaly. The Advanced Microwave Scanning Radiometer (AMSR-E) on the Aqua satellite takes measurements through clouds to provide sea surface temperatures. |
| Completed |
2003-05-20 |
|
AMSR-E Anomalous Atlantic Se
| Title |
AMSR-E Anomalous Atlantic Sea Surface Temperature Data Used to Forecast 2003 Hurricane Season |
| Abstract |
Researchers and forecasters often study sea surface temperatures for an indication of hurricane potential. Scientists say above normal Atlantic Ocean temperatures is one reason for the 'above normal' hurricane forecast. Hurricanes convert heat from the tropical atmosphere and oceans to wind and waves, just as a car engine converts gasoline into motion. These animations show a year in the life of global ocean temperatures, June 2, 2002, to May 11, 2003. Blue indicates the coolest water anomaly, red the warmest anomaly. The Advanced Microwave Scanning Radiometer (AMSR-E) on the Aqua satellite takes measurements through clouds to provide sea surface temperatures. |
| Completed |
2003-05-20 |
|
Global Atmospheric Water Vap
| Title |
Global Atmospheric Water Vapor during Hurricane Frances (WMS) |
| Abstract |
Water vapor is a small but significant constituent of the atmosphere, warming the planet due to the greenhouse effect and condensing to form clouds which both warm and cool the Earth in different circumstances. Warm, moisture-laden air moving out from the tropics brings rainfall to the temperate zones. This animation shows the atmospheric water vapor for the whole globe from September 1, 2004, through September 5, 2004, during the period of Hurricane Frances in the western Atlantic Ocean and Typhoon Songda in the western Pacific Ocean. The band of water vapor over the tropics is the intertropical convergence zone, where converging trade winds and high temperatures force large amounts of water high into the atmosphere. Both Hurricane Frances and Typhoon Songda exhibit significant spiral bands of high water vapor. |
| Completed |
2005-07-25 |
|
Global Atmospheric Water Vap
| Title |
Global Atmospheric Water Vapor during Hurricane Frances (WMS) |
| Abstract |
Water vapor is a small but significant constituent of the atmosphere, warming the planet due to the greenhouse effect and condensing to form clouds which both warm and cool the Earth in different circumstances. Warm, moisture-laden air moving out from the tropics brings rainfall to the temperate zones. This animation shows the atmospheric water vapor for the whole globe from September 1, 2004, through September 5, 2004, during the period of Hurricane Frances in the western Atlantic Ocean and Typhoon Songda in the western Pacific Ocean. The band of water vapor over the tropics is the intertropical convergence zone, where converging trade winds and high temperatures force large amounts of water high into the atmosphere. Both Hurricane Frances and Typhoon Songda exhibit significant spiral bands of high water vapor. |
| Completed |
2005-07-25 |
|
Global Convective Precipitat
| Title |
Global Convective Precipitation during Hurricane Frances (WMS) |
| Abstract |
Water vapor is a small but significant constituent of the atmosphere, warming the planet due to the greenhouse effect and condensing to form clouds. As moisture-laden air rises, the relative humidity increases until it saturates the air, at which time precipitation occurs. If the uplift of air is due to strong updrafts and unstable air systems, as in thunderstorms, then the precipitation is called convective. This animation shows the convective precipitation for the whole globe from September 1, 2004, through September 5, 2004, during the period of Hurricane Frances in the western Atlantic Ocean and Typhoon Songda in the western Pacific Ocean. Convective precipitation is more intense but less long-lasting than large-scale precipitation. |
| Completed |
2005-07-28 |
|
Global Convective Precipitat
| Title |
Global Convective Precipitation during Hurricane Frances (WMS) |
| Abstract |
Water vapor is a small but significant constituent of the atmosphere, warming the planet due to the greenhouse effect and condensing to form clouds. As moisture-laden air rises, the relative humidity increases until it saturates the air, at which time precipitation occurs. If the uplift of air is due to strong updrafts and unstable air systems, as in thunderstorms, then the precipitation is called convective. This animation shows the convective precipitation for the whole globe from September 1, 2004, through September 5, 2004, during the period of Hurricane Frances in the western Atlantic Ocean and Typhoon Songda in the western Pacific Ocean. Convective precipitation is more intense but less long-lasting than large-scale precipitation. |
| Completed |
2005-07-28 |
|
Hurricane Olga: 28 November
| Title |
Hurricane Olga: 28 November 2001 |
| Abstract |
SeaWiFS captures this image of Hurricane Olga in the Atlantic Ocean. |
| Completed |
2001-11-28 |
|
Hurricane Olga: 28 November
| Title |
Hurricane Olga: 28 November 2001 |
| Abstract |
SeaWiFS captures this image of Hurricane Olga in the Atlantic Ocean. |
| Completed |
2001-11-28 |
|
Hurricane Olga: 28 November
| Title |
Hurricane Olga: 28 November 2001 |
| Abstract |
SeaWiFS captures this image of Hurricane Olga in the Atlantic Ocean. |
| Completed |
2001-11-28 |
|
Sea Surface Wind Anomalies i
| Title |
Sea Surface Wind Anomalies in the North Atlantic |
| Abstract |
Sea surface wind anomalies (based on QuikSCAT data) from 31 December 2002 illustrate the wind patterns that exist during a North Atlantic Oscillation. The wind data has been processed using the Variational Analysis Method (VAM). |
| Completed |
2003-02-03 |
|
Sea Surface Wind Anomalies i
| Title |
Sea Surface Wind Anomalies in the North Atlantic |
| Abstract |
Sea surface wind anomalies (based on QuikSCAT data) from 31 December 2002 illustrate the wind patterns that exist during a North Atlantic Oscillation. The wind data has been processed using the Variational Analysis Method (VAM). |
| Completed |
2003-02-03 |
|
Transatlantic Dust from Nort
| Title |
Transatlantic Dust from North Africa (WMS) |
| Abstract |
Desert storms in northern Africa raise dust that is carried in the upper atmosphere across the Atlantic Ocean. The dust, which may carry potentially hazardous bacteria and fungi, can land as far west as the Carribean and the Americas. |
| Completed |
2005-03-14 |
|
Transatlantic Dust from Nort
| Title |
Transatlantic Dust from North Africa (WMS) |
| Abstract |
Desert storms in northern Africa raise dust that is carried in the upper atmosphere across the Atlantic Ocean. The dust, which may carry potentially hazardous bacteria and fungi, can land as far west as the Carribean and the Americas. |
| Completed |
2005-03-14 |
|
African Dust Sequence
| Title |
African Dust Sequence |
| Abstract |
A 48-hour dust storm on March 1 and 2, 2003, is responsible for a very large dust transport over the Atlantic Ocean from March 2 through March 6, 2003. |
| Completed |
2003-03-06 |
|
African Dust Sequence
| Title |
African Dust Sequence |
| Abstract |
A 48-hour dust storm on March 1 and 2, 2003, is responsible for a very large dust transport over the Atlantic Ocean from March 2 through March 6, 2003. |
| Completed |
2003-03-06 |
|
African Dust Sequence
| Title |
African Dust Sequence |
| Abstract |
A 48-hour dust storm on March 1 and 2, 2003, is responsible for a very large dust transport over the Atlantic Ocean from March 2 through March 6, 2003. |
| Completed |
2003-03-06 |
|
African Dust Sequence
| Title |
African Dust Sequence |
| Abstract |
A 48-hour dust storm on March 1 and 2, 2003, is responsible for a very large dust transport over the Atlantic Ocean from March 2 through March 6, 2003. |
| Completed |
2003-03-06 |
|
African Dust Sequence
| Title |
African Dust Sequence |
| Abstract |
A 48-hour dust storm on March 1 and 2, 2003, is responsible for a very large dust transport over the Atlantic Ocean from March 2 through March 6, 2003. |
| Completed |
2003-03-06 |
|
African Dust Sequence
| Title |
African Dust Sequence |
| Abstract |
A 48-hour dust storm on March 1 and 2, 2003, is responsible for a very large dust transport over the Atlantic Ocean from March 2 through March 6, 2003. |
| Completed |
2003-03-06 |
|
African Dust Sequence
| Title |
African Dust Sequence |
| Abstract |
A 48-hour dust storm on March 1 and 2, 2003, is responsible for a very large dust transport over the Atlantic Ocean from March 2 through March 6, 2003. |
| Completed |
2003-03-06 |
|
African Dust Sequence
| Title |
African Dust Sequence |
| Abstract |
A 48-hour dust storm on March 1 and 2, 2003, is responsible for a very large dust transport over the Atlantic Ocean from March 2 through March 6, 2003. |
| Completed |
2003-03-06 |
|
African Dust Sequence
| Title |
African Dust Sequence |
| Abstract |
A 48-hour dust storm on March 1 and 2, 2003, is responsible for a very large dust transport over the Atlantic Ocean from March 2 through March 6, 2003. |
| Completed |
2003-03-06 |
|
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