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Woods Hole Coastal and Marine Science Center images

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Photograph of flooded airport runway  in Barter Island, Alaska
Flooded airport runway in Barter Island, Alaska
Flooded airport runway in Barter Island, Alaska
Preview image of swath bathymetric grid collected offshore of Fire Island, NY
Swath Bathymetric Grid
Swath Bathymetric Grid
Swath Bathymetric Grid

This bathymetric grid represents approximately 3900 kilometers of bathymetric data collected in 2014. These data were collected using a dual-head R2Sonic 2024 multibeam echosounder (MBES) by Alpine Ocean Seismic Survey, Inc., during USGS field activity 2014-072-FA.

This bathymetric grid represents approximately 3900 kilometers of bathymetric data collected in 2014. These data were collected using a dual-head R2Sonic 2024 multibeam echosounder (MBES) by Alpine Ocean Seismic Survey, Inc., during USGS field activity 2014-072-FA.

USGS scientists walk through a tern colony USGS scientists walk through a tern colony
USGS scientists walk through a tern colony
USGS scientists walk through a tern colony
USGS scientists walk through a tern colony

USGS scientists walk through a tern colony on the Monomoy National Wildlife Refuge (MA). Here, these scientists are using ecogeomorphological models to predict how this refuge will be impacted by sea-level rise and how that will ultimately effect shorebirds.

USGS scientists walk through a tern colony on the Monomoy National Wildlife Refuge (MA). Here, these scientists are using ecogeomorphological models to predict how this refuge will be impacted by sea-level rise and how that will ultimately effect shorebirds.

small hole in the ground surrounded by grass
Soil core from coastal wetland
Soil core from coastal wetland
Soil core from coastal wetland

Scientists collect soil cores in coastal wetland by removing a section of peat, the organic-rich material that makes up salt marshes. After the soil is removed, water quickly fills in the void. This water-logged environment underground is devoid of oxygen and is an important reason that salt marsh peat preserves a record of historical changes.

Scientists collect soil cores in coastal wetland by removing a section of peat, the organic-rich material that makes up salt marshes. After the soil is removed, water quickly fills in the void. This water-logged environment underground is devoid of oxygen and is an important reason that salt marsh peat preserves a record of historical changes.

a woman scientist in a baseball hat standing in a marsh holding a long piece of equipment
Meagan Eagle, USGS Research Scientist, collecting elevation points in Quivett Creek, Brewster, MA
Meagan Eagle, USGS Research Scientist, collecting elevation points in Quivett Creek, Brewster, MA
Meagan Eagle, USGS Research Scientist, collecting elevation points in Quivett Creek, Brewster, MA

Meagan Eagle, Research Scientists at the U.S. Geological Survey, collects an elevation point along the edge of Quivett Creek in Brewster, MA. This salt marsh was restored in 2005 by replacing a narrow culvert to allow full tidal flow once again.

Image of Piping Plover nest
Piping Plover Nest
Piping Plover Nest
Piping Plover Nest

USGS scientists are working to model shorebird habitat availability both today and in the future, given processes like sea-level rise, in an effort to support the efficient management of beaches for both people and nesting shorebirds.

USGS scientists are working to model shorebird habitat availability both today and in the future, given processes like sea-level rise, in an effort to support the efficient management of beaches for both people and nesting shorebirds.

Barnegat Bay residence times in days
Barnegat Bay residence times in days
Barnegat Bay residence times in days
Barnegat Bay residence times in days

Barnegat Bay residence times in days for (a) scenario T, only tidal forcing; (b) scenario TB, combined offshore hydrodynamic forcing; (c) scenario TBR, streamflow with combined hydrodynamic forcing; and (d) scenario TBRM, full suite with meteorological forcing

Barnegat Bay residence times in days for (a) scenario T, only tidal forcing; (b) scenario TB, combined offshore hydrodynamic forcing; (c) scenario TBR, streamflow with combined hydrodynamic forcing; and (d) scenario TBRM, full suite with meteorological forcing

Aerial image of a beach.
Sandwich Town Neck Beach composite aerial view
Sandwich Town Neck Beach composite aerial view
Sandwich Town Neck Beach composite aerial view

Composite aerial view of Sandwich Town Neck Beach. The imagery was obtained from an unmanned aerial system (UAS) flown by Peter Traykovski in February, 2015, a few days after winter storm Juno. The background topography is from USGS and U.S. Army Corps of Engineers lidar data, with missing-data areas shown in white.

Composite aerial view of Sandwich Town Neck Beach. The imagery was obtained from an unmanned aerial system (UAS) flown by Peter Traykovski in February, 2015, a few days after winter storm Juno. The background topography is from USGS and U.S. Army Corps of Engineers lidar data, with missing-data areas shown in white.

Preview image of multi-channel seismic data collected by the USGS
Multi-channel seismic data preview image
Multi-channel seismic data preview image
Multi-channel seismic data preview image

Preview image of multi-channel seismic data collected by the USGS off the US Seaboard Atlantic as part of the US Extended Continental Shelf project.

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