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Listing 1 - 10 of 46 results.

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Photo ID: h2a8w7Subject: PaleontologyDescription
Coelenterata; Corals; Cores; Growth Bands; Paleoclimatology; Pavona clavusCoral skeleton formed in winter has a different density than that formed in summer because of variations in growth rates related to temperature and cloud cover conditions. Thus corals exhibit seasonal growth bands very much like those in trees. Sometimes these bands are visible to the naked eye; usually, however, they are more visible in an X-ray like this. When paleoclimatologists drill a coral core, they can count the growth bands and date samples exactly. Long cores can cover several hundred years; this portion of a core from Urvina Bay in the Galapagos Islands covers the period from 1716 to 1735 A. D. To best understand past climate, scientists need to be able to date their samples as accurately as possible. They need to know exactly when climatic changes occurred so that they can create realistic computer models of the global climate system.
PhotographerLocation
NOAA

Credit Line: Courtesy National Oceanic and Atmospheric Administration
South America; Ecuador; Galapagos Islands; Urvina Bay
Photo Quality | LargeAvailable for Commercial Use

Photo ID: h4vk5wSubject: Satellite ImageryDescription
Clouds; Geologic Hazards; Hurricanes; Hydrosphere; Meteorology; Storms; WeatherHurricane Alberto, the first hurricane of the 2000 season, sustained winds of 75 mph, and was classified as a relatively weak hurricane.
PhotographerLocation
SeaWifs

Credit Line: Copyright © NASA SeaWiFS Project
North America
Photo Quality | LargeAvailable for Commercial Use

Photo ID: h4vli8Subject: Satellite ImageryDescription
Atolls; Basalt; Complexes; Geologic Regions; Hills; Igneous Rock; Islands; Landforms; Massifs; Mountains; Oceans; Plutonic Rocks; SeasThe island of Cyprus is seen in this image taken in 2001. This image shows the three distinctive geologic regions of the island including the Troodos Massif (mountains), the Kyrenia Range (thin arc), and the low lying Lefkosia region.
PhotographerLocation
MODIS

Credit Line: Courtesy MODIS, NASA
Asia; Cyprus; Cyprus Island
Photo Quality | LargeAvailable for Commercial Use

Photo ID: h4vppiSubject: Satellite ImageryDescription
Fluvial Features; Geomorphology; Hydrogeology; Hydrology; Streams; WaterwaysImages of the Nile River fluctuations near Khartoum, Sudan capturing the river's dynamic nature. These images show the river before and after the rainy seasons of 2000 and 2001. In these images it is possible to see the waters of the White Nile and Blue Nile converge and continue to flow northward as the Great Nile. The flooding in this area has dire consequences for the people living along the Nile. Image taken with the Terra Satellite's Multi-angle Imaging SpectroRadiometer (MISR) nadir camera.
PhotographerLocation
NASAVE

Credit Line: Courtesy NASA, Visible Earth
Africa; Sudan; Nubian Desert; Nile River
Photo Quality | LargeAvailable for Commercial Use

Photo ID: h4vtgqSubject: Satellite ImageryDescription
Clouds; Coastlines; Seasons; Snow; WeatherThis true-color image taken in June of 2001 shows snow retreating from much of Alaska. The blues, greens and browns in the water along the coasts are likely a mixture of phytoplankton and sediment running off from rivers. At upper right, you can see the Bering Strait continuing to thaw.
PhotographerLocation
MODIS

Credit Line: Courtesy MODIS, NASA
North America; United States; Alaska
Photo Quality | LargeAvailable for Commercial Use

Photo ID: h4w4ioSubject: GlaciersDescription
Annual Layers; Corew; Electrical Conductivity; Ice Caps; Ice Cores; Layers; Oxygen; Seasonal Variations; Visual StratigraphyThree deep core sections show distinct annual bands produced by the deposition of dust during the dry season (dry season dust layers are represented by triangles). While annual bands provide accurate relative dating (the age of each ice band is known to be a year apart from directly adjacent bands), paleoclimatologists also search for absolute dates within a core chronology. Electrical conductivity measurements (ECM), particle concentrations, and the ratio of heavy to light oxygen molecules are other seasonally-variable core parameters that can be used along with visual stratigraphy in dating ice cores.
PhotographerLocation
NOAA

Credit Line: Courtesy National Oceanic and Atmospheric Administration
South America; Peru; Altiplano; Quelccaya Ice Cap
Photo Quality | LargeAvailable for Commercial Use

Photo ID: h4w4z8Subject: Sedimentary RocksDescription
Accumulation Layers; Ice Caps; Ice Cores; Paleoclimatology; Visual StratigraphyThe Quelccaya cap terminates abruptly and spectacularly in a 55 m ice cliff. The annual accumulation layers clearly visible in the photograph are an average of .75 m thick. While snow can fall during any season on the altiplano, most of it (80-90 percent) arrives between the months of November and April. The distinct seasonality of precipitation at Quelccaya results in the deposition of the dry season dust bands seen in the ice cliff. These layers are extremely useful to the paleoclimatologist because they allow ice core records to be dated very accurately using visual stratigraphy, which is simply the visual identification of annual dust layers in ice records
PhotographerLocation
NOAA

Credit Line: Courtesy National Oceanic and Atmospheric Administration
South America; Peru; Altiplano; Quelccaya Ice Cap
Photo Quality | LargeAvailable for Commercial Use

Photo ID: h4w56oSubject: WeatherDescription
Hurricane Allison; Hurricanes; Natural Hazards; Photometeorology; Remote Sensing; Satellite Imagery; Tropical CyclonesThis is a thermal infrared image of Hurricane Allison, the first named storm of the 1995 season. The 1995 Atlantic hurricane season was the second most active season in recorded history. During 1995, 12 named tropical cyclones formed in the Atlantic before the end of August, and by the end of the season 19 tropical cyclones had received names. 11 of the 19 reached hurricane strength. The 1886 to 1994 seasonal average is 8.4 tropical storms with 4.9 reaching hurricane strength.
PhotographerLocation
NOAA

Credit Line: Courtesy National Oceanic and Atmospheric Administration
Oceans; United States; North Atlantic; Hurricane Allison
Photo Quality | LargeAvailable for Commercial Use

Photo ID: h4w596Subject: WeatherDescription
Hurricane Allison; Hurricanes; Natural Hazards; Photometeorology; Remote Sensing; Satellite Imagery; Tropical CyclonesThis satellite image is a visible spectrum image of the first named storm of the 1995 season, Allison. The 1995 Atlantic hurricane season was the second most active season in recorded history. During 1995, 12 named tropical cyclones formed in the Atlantic before the end of August, and by the end of the season 19 tropical cyclones had received names. 11 of the 19 reached hurricane strength. The 1886 to 1994 seasonal average is 8.4 tropical storms with 4.9 reaching hurricane strength.
PhotographerLocation
NOAA

Credit Line: Courtesy National Oceanic and Atmospheric Administration
Oceans; United States; North Atlantic
Photo Quality | LargeAvailable for Commercial Use

Photo ID: h4w5b7Subject: WeatherDescription
Hurricanes; Natural Hazards; Photometeorology; Remote Sensing; Satellite Imagery; Tropical CyclonesThis satellite thermal infrared image is of Hurricane Erin in August of 1995. The 1995 Atlantic hurricane season was the second most active season in recorded history. During 1995, 12 named tropical cyclones formed in the Atlantic before the end of August, and by the end of the season 19 tropical cyclones had received names. 11 of the 19 reached hurricane strength. The 1886 to 1994 seasonal average is 8.4 tropical storms with 4.9 reaching hurricane strength.
PhotographerLocation
NOAA

Credit Line: Courtesy National Oceanic and Atmospheric Administration
North America; United States; Florida; Hurricane Erin
Photo Quality | LargeAvailable for Commercial Use

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