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Photographing the Earth from the International Space Station

Astronaut Photography of Earth - Display Record

STS41B-41-2347

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File NameFile Size (bytes)WidthHeightAnnotatedCroppedPurposeComments
View STS41B-41-2347.JPG 37265640480 No No ISD 1
View STS41B-41-2347.JPG 44368540405 Yes Yes NASA's Earth Observatory web site
View STS41B-41-2347.JPG 99695639639 No No Earth From Space collection
View STS41B-41-2347.JPG 151281957005900 No No From ISD TIFF images
View STS41B-41-2347.JPG 706824352665266 No No Earth From Space collection

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Electronic Image Data

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Identification

Mission: STS41B Roll: 41 Frame: 2347 Mission ID on the Film or image: 41B
Country or Geographic Name: BRAZIL
Features: THUNDERSTORMS
Center Point: Latitude: -23.5 Longitude: -52.5 (Negative numbers indicate south for latitude and west for longitude)

Stereo: No (Yes indicates there is an adjacent picture of the same area)
ONC Map ID: P27 JNC Map ID:

Camera

Camera Tilt: Low Oblique
Camera Focal Length: 250mm
Camera: HB: Hasselblad
Film: 6017 : Kodak Ektachrome 64, 220 Roll Format.

Quality

Film Exposure: Under Exposed
Percentage of Cloud Cover: 60 (51-75)

Nadir

GMT Date: 198402__ (YYYYMMDD) GMT Time: (HHMMSS)
Nadir Point Latitude: , Longitude: (Negative numbers indicate south for latitude and west for longitude)
Nadir to Photo Center Direction:
Sun Azimuth: (Clockwise angle in degrees from north to the sun measured at the nadir point)
Spacecraft Altitude: nautical miles (0 km)
Sun Elevation Angle: (Angle in degrees between the horizon and the sun, measured at the nadir point)
Orbit Number: 21

Captions

Thunderstorms over Brazil
This photograph, acquired in February 1984 by an astronaut aboard the space shuttle, shows a series of mature thunderstorms located near the Parana River in southern Brazil. With abundant warm temperatures and moisture-laden air in this part of Brazil, large thunderstorms are commonplace. A number of overshooting tops and anvil clouds are visible at the tops of the clouds. Storms of this magnitude can drop large amounts of rainfall in a short period of time, causing flash floods.

However, a NASA-funded researcher has discovered that tiny airborne particles of pollution may modify developing thunderclouds by increasing the quantity and reducing the size of the ice crystals within them. These modifications may affect the clouds’ impact on the Earth’s “radiation budget,” or the amount of radiation that enters and leaves our planet.

Steven Sherwood, a professor at Yale University, found that airborne aerosols reduce the size of ice crystals in thunderclouds and may reduce precipitation as well. Using several satellites and instruments including NASA’s Total Ozone Mapping Spectrometer (TOMS) and NASA’s Tropical Rainfall Measuring Mission (TRMM) satellite, Sherwood observed how airborne pollution particles (aerosols) affect large thunderstorms, or cumulonimbus clouds in the tropics. Common aerosols include mineral dust, smoke, and sulfates. An increased number of these particles create a larger number of smaller ice crystals in cumulonimbus clouds. As a result of their smaller size, the ice crystals evaporate from a solid state directly into a gas, instead of falling as rain. Sherwood noted that this effect is more prevalent over land than open ocean areas.

Previous research by Daniel Rosenfeld of Hebrew University revealed that aerosols and pollution reduced rainfall in shallow cumulus clouds of liquid water, which do not have the capability to produce as much rainfall. Sherwood expanded on that research by looking at cumulonimbus clouds with more ice particles. Studies have also proven that ice particles are smaller in the upper reaches of thunderclouds when there is more pollution and when the rising air in the clouds (convection) is stronger. Aerosols seem to have the most influence on seasonal and longer timescales such as during the warmer months when plants and undergrowth are burned to clear fields.

Over areas where biomass burning occurs, such as South America, aerosols have been found to reduce the diameter of ice crystals in the clouds by as much as 20 percent. Areas over deserts, such as Africa's Sahel Region where dust is a primary aerosol, there was a 10 percent decrease in the diameter of ice crystals in cumulonimbus clouds. Aerosol particles are necessary for clouds to form, and it has been suspected that clouds might be altered by large concentrations of them. By looking at ten years of aerosol data and statistically analyzing many thunderclouds, Sherwood was able to confirm that they were affected.

Sherwood found that ice crystals are smaller in clouds over continents than oceans, which could be attributed to the amount of pollution generated over land. The highest values occur widely over Northern Africa, where desert dust and smoke from agricultural burning occur. Intermediate values prevail over much of Asia, through the Indonesia region and into the south Pacific. The largest ice crystal sizes were found over the eastern Pacific and southern Indian Oceans.

Sherwood’s article, “Aerosols and Ice Particle Size in Tropical Cumulonimbus,” appears in the May 1, 2002, issue of the American Meteorological Society Journal of Climate. This work was performed under the NASA Earth Observing System/Interdisciplinary Science (IDS) program under the Earth Science Enterprise (ESE).

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