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St. Petersburg Coastal and Marine Science Center images.
Hurricane Sandy leveled dunes and moved eroded sediment from the dunes and beach across the island and into the estuary (Great South Bay) at Fire Island, NY.
Hurricane Sandy leveled dunes and moved eroded sediment from the dunes and beach across the island and into the estuary (Great South Bay) at Fire Island, NY.
An aerial view of Dauphin Island, Alabama, shows a thin strip of road partially covered by sand, with undeveloped beach in the foreground and developed beach in the background.
An aerial view of Dauphin Island, Alabama, shows a thin strip of road partially covered by sand, with undeveloped beach in the foreground and developed beach in the background.
A USGS diver beside a Massive Starlet (Siderastrea siderea) coral colony in Dry Tortugas National Park. Scientists used a core from this coral to reconstruct ocean temperatures going back to 1837. Photo: USGS, May 2012
A USGS diver beside a Massive Starlet (Siderastrea siderea) coral colony in Dry Tortugas National Park. Scientists used a core from this coral to reconstruct ocean temperatures going back to 1837. Photo: USGS, May 2012
Scientists used a core from this Massive Starlet (Siderastrea siderea) coral colony in Dry Tortugas National Park to reconstruct ocean temperatures going back to 1837. Photo: USGS
Scientists used a core from this Massive Starlet (Siderastrea siderea) coral colony in Dry Tortugas National Park to reconstruct ocean temperatures going back to 1837. Photo: USGS
The Along-Track Reef-Imaging System (ATRIS), deployed from an adjustable pole mounted to the side of a boat, can provide scientists with information about the condition and type of seafloor.
The Along-Track Reef-Imaging System (ATRIS), deployed from an adjustable pole mounted to the side of a boat, can provide scientists with information about the condition and type of seafloor.
Oblique aerial photographs of Ocracoke Island, NC, from May 6, 2008 (top, pre-storm) and August 30, 2011 (bottom, post-storm, acquired three days after landfall of Hurricane Irene). The yellow arrow in each image points to the same feature. Overwash deposits of sand extend over the road after the storm.
Oblique aerial photographs of Ocracoke Island, NC, from May 6, 2008 (top, pre-storm) and August 30, 2011 (bottom, post-storm, acquired three days after landfall of Hurricane Irene). The yellow arrow in each image points to the same feature. Overwash deposits of sand extend over the road after the storm.
Upper image: Oblique aerial photograph near Rodanthe, NC, looking south along the coast on August 30, 2011, three days after landfall of Hurricane Irene. Center: Oblique aerial photograph of central part of upper image from May 6, 2008, pre-storm; and August 31, 2011, post-storm. The yellow arrow in each image points to the same cottage.
Upper image: Oblique aerial photograph near Rodanthe, NC, looking south along the coast on August 30, 2011, three days after landfall of Hurricane Irene. Center: Oblique aerial photograph of central part of upper image from May 6, 2008, pre-storm; and August 31, 2011, post-storm. The yellow arrow in each image points to the same cottage.
Upper image: Oblique aerial photograph of Pea Island National Wildlife Refuge, NC, looking north along the coast on August 30, 2011, three days after landfall of Hurricane Irene.
Upper image: Oblique aerial photograph of Pea Island National Wildlife Refuge, NC, looking north along the coast on August 30, 2011, three days after landfall of Hurricane Irene.
Photo collage showing researchers on 3 marine field trips. Left, photo of back deck of geophysical survey vessel during collection of bathymetry and seismic data; center, equipment tripod on deck of R/V; right, 2 researchers sit before computer monitors reviewing data as it is collected.
Photo collage showing researchers on 3 marine field trips. Left, photo of back deck of geophysical survey vessel during collection of bathymetry and seismic data; center, equipment tripod on deck of R/V; right, 2 researchers sit before computer monitors reviewing data as it is collected.
Oblique aerial photographs of Hatteras Village, NC, from May 6, 2008 (top, pre-storm) and August 30, 2011(bottom, post-storm, acquired three days after landfall of Hurricane Irene). The yellow arrow in each image points to the same cottage.
Oblique aerial photographs of Hatteras Village, NC, from May 6, 2008 (top, pre-storm) and August 30, 2011(bottom, post-storm, acquired three days after landfall of Hurricane Irene). The yellow arrow in each image points to the same cottage.
Post Hurricane Irene: Beach state after Hurricane Irene showing the exposure of a groin from loss of beach elevation (foreground) and beach and dune scarping due to elevated water levels (background).
Post Hurricane Irene: Beach state after Hurricane Irene showing the exposure of a groin from loss of beach elevation (foreground) and beach and dune scarping due to elevated water levels (background).
During Hurricane Irene, sand eroded from the beach and dunes was transported landward, burying a walkway near the Fire Island lighthouse.
During Hurricane Irene, sand eroded from the beach and dunes was transported landward, burying a walkway near the Fire Island lighthouse.
Oblique aerial photograph near Rodanthe, North Carolina, looking south along the coast on August 30, 2011, three days after landfall of Hurricane Irene.
Oblique aerial photograph near Rodanthe, North Carolina, looking south along the coast on August 30, 2011, three days after landfall of Hurricane Irene.
Christina Kellogg and David Zawada using SCUBA gear to sample the microbiomes of corals at Loggerhead Key, Dry Tortugas, Florida. Chris Kellogg studies corals to understand coral heath and potential diseases.
Christina Kellogg and David Zawada using SCUBA gear to sample the microbiomes of corals at Loggerhead Key, Dry Tortugas, Florida. Chris Kellogg studies corals to understand coral heath and potential diseases.
U.S. Geological Survey scientist collecting elevation data on the bluff of Alaska’s north coast.
U.S. Geological Survey scientist collecting elevation data on the bluff of Alaska’s north coast.
Eider duck eggs in a nest on Arey Island, Alaska.
Eider duck eggs in a nest on Arey Island, Alaska.
The large white radar dome is a former Distant Early Warning Line site, which sits atop a permafrost bluff on Barter Island, Alaska.
The large white radar dome is a former Distant Early Warning Line site, which sits atop a permafrost bluff on Barter Island, Alaska.
Top: Big Bay along the Long Beach trail, looking east along the Long Beach trail on Big Pine Key, Florida (FL). Note the angled shape of the vegetation caused by salt pruning from the prevailing sea breeze. Bottom: Red mangrove on the Long Beach trail, looking east along Long Beach trail on Big Pine Key, FL. Red mangroves provide critical coastal protection.
Top: Big Bay along the Long Beach trail, looking east along the Long Beach trail on Big Pine Key, Florida (FL). Note the angled shape of the vegetation caused by salt pruning from the prevailing sea breeze. Bottom: Red mangrove on the Long Beach trail, looking east along Long Beach trail on Big Pine Key, FL. Red mangroves provide critical coastal protection.
The Moderate Resolution Imaging Spectroradiometer (MODIS) instrument on NASA’s Aqua satellite captured this natural-color image on July 28, 2010. Around the location of the oil leak, and around the Mississippi Delta, relatively light swirls and patches appear on the ocean surface.
The Moderate Resolution Imaging Spectroradiometer (MODIS) instrument on NASA’s Aqua satellite captured this natural-color image on July 28, 2010. Around the location of the oil leak, and around the Mississippi Delta, relatively light swirls and patches appear on the ocean surface.
Sea Level Rise, Subsidence, and Wetland Loss. This video describes causes of wetland loss in the Mississippi River Delta. Rapid land subsidence due to sediment compaction and dewatering increases the rate of submergence in this deltaic system.
Sea Level Rise, Subsidence, and Wetland Loss. This video describes causes of wetland loss in the Mississippi River Delta. Rapid land subsidence due to sediment compaction and dewatering increases the rate of submergence in this deltaic system.
Estimating volume of water discharged from fish sampling locations within mangrove forests is necessary to derive fish density estimates per volume. Fish density was found to be greater in waters draining natural tidal forests than in waters from mudflats formed as a result of landfall of a Category 5 hurricane on Cape Sable, Everglades National Park in 1935.&
Estimating volume of water discharged from fish sampling locations within mangrove forests is necessary to derive fish density estimates per volume. Fish density was found to be greater in waters draining natural tidal forests than in waters from mudflats formed as a result of landfall of a Category 5 hurricane on Cape Sable, Everglades National Park in 1935.&