The CCL assessment integrates data describing coastal characteristics, landscape composition, and the level of resistance to change, with data defining the drivers of change that impact the coast, such as waves and flooding. These data types are known as fabric and hazards, respectively.
Images
Woods Hole Coastal and Marine Science Center images
The CCL assessment integrates data describing coastal characteristics, landscape composition, and the level of resistance to change, with data defining the drivers of change that impact the coast, such as waves and flooding. These data types are known as fabric and hazards, respectively.
Data defining the drivers of change that impact the coast, such as waves and flooding are synthesized in hazards layers.
Data defining the drivers of change that impact the coast, such as waves and flooding are synthesized in hazards layers.
The assessment integrates data describing coastal characteristics, landscape composition, and the level of resistance to change to produce the initial fabric layer.
The assessment integrates data describing coastal characteristics, landscape composition, and the level of resistance to change to produce the initial fabric layer.
The U.S. Geological Survey, in cooperation with the National Park Service, developed the Coastal Change Likelihood assessment to determine the future likelihood of coastal change along the Northeast U.S. coastline in the next decade. Here is the CCL map for Chesapeake, Va.
The U.S. Geological Survey, in cooperation with the National Park Service, developed the Coastal Change Likelihood assessment to determine the future likelihood of coastal change along the Northeast U.S. coastline in the next decade. Here is the CCL map for Chesapeake, Va.
The CCL is an updated version of the older Coastal Vulnerability Index, first published in 1999. While the original product was focused on change in the next 50-100 years based solely on sea level rise, the new CCL is more near-term, focusing on change over the next decade as a result of multiple coastal hazards.
The CCL is an updated version of the older Coastal Vulnerability Index, first published in 1999. While the original product was focused on change in the next 50-100 years based solely on sea level rise, the new CCL is more near-term, focusing on change over the next decade as a result of multiple coastal hazards.
The U.S. Geological Survey, in cooperation with the National Park Service, developed the Coastal Change Likelihood assessment to determine the future likelihood of coastal change along the Northeast U.S. coastline in the next decade.
The U.S. Geological Survey, in cooperation with the National Park Service, developed the Coastal Change Likelihood assessment to determine the future likelihood of coastal change along the Northeast U.S. coastline in the next decade.
The U.S. Geological Survey, in cooperation with the National Park Service, developed the Coastal Change Likelihood assessment to determine the future likelihood of coastal change along the Northeast coastline in the next decade. Pictured here is coastal change likelihood on Cape Cod.
The U.S. Geological Survey, in cooperation with the National Park Service, developed the Coastal Change Likelihood assessment to determine the future likelihood of coastal change along the Northeast coastline in the next decade. Pictured here is coastal change likelihood on Cape Cod.
Where are coastal landscapes likely to change?
Where are coastal landscapes likely to change?
The U.S. Geological Survey, in cooperation with the National Park Service, developed the Coastal Change Likelihood assessment to determine the future likelihood of coastal change along the Northeast U.S. coastline in the next decade. The CCL data displayed here are for the mid-Atlantic Bight, and extend from the shoreline to 10m elevation inland.
The U.S. Geological Survey, in cooperation with the National Park Service, developed the Coastal Change Likelihood assessment to determine the future likelihood of coastal change along the Northeast U.S. coastline in the next decade. The CCL data displayed here are for the mid-Atlantic Bight, and extend from the shoreline to 10m elevation inland.
The CCL is an updated version of the older Coastal Vulnerability Index, first published in 1999. While the original product was focused on change in the next 50-100 years based solely on sea level rise, the new CCL is more near-term, focusing on change over the next decade as a result of multiple coastal hazards.
The CCL is an updated version of the older Coastal Vulnerability Index, first published in 1999. While the original product was focused on change in the next 50-100 years based solely on sea level rise, the new CCL is more near-term, focusing on change over the next decade as a result of multiple coastal hazards.
The CCL is an updated version of the older Coastal Vulnerability Index, first published in 1999. While the original product was focused on change in the next 50-100 years based solely on sea level rise, the new CCL is more near-term, focusing on change over the next decade as a result of multiple coastal hazards.
The CCL is an updated version of the older Coastal Vulnerability Index, first published in 1999. While the original product was focused on change in the next 50-100 years based solely on sea level rise, the new CCL is more near-term, focusing on change over the next decade as a result of multiple coastal hazards.
The CCL is an updated version of the older Coastal Vulnerability Index, first published in 1999. While the original product was focused on change in the next 50-100 years based solely on sea level rise, the new CCL is more near-term, focusing on change over the next decade as a result of multiple coastal hazards.
The CCL is an updated version of the older Coastal Vulnerability Index, first published in 1999. While the original product was focused on change in the next 50-100 years based solely on sea level rise, the new CCL is more near-term, focusing on change over the next decade as a result of multiple coastal hazards.
The U.S. Geological Survey, in cooperation with the National Park Service, developed the Coastal Change Likelihood assessment to determine the future likelihood of coastal change along the Northeast U.S. coastline in the next decade.
The U.S. Geological Survey, in cooperation with the National Park Service, developed the Coastal Change Likelihood assessment to determine the future likelihood of coastal change along the Northeast U.S. coastline in the next decade.
Headshot of Neil Kamal Ganju, a Research Oceanographer with the USGS Woods Hole Coastal and Marine Science Center.
Headshot of Neil Kamal Ganju, a Research Oceanographer with the USGS Woods Hole Coastal and Marine Science Center.
The year of 2022 was big for the Sea-Floor Mapping Group at the Woods Hole Coastal and Marine Science Center! These data were collected as part of a collaborative research program and include data collected by USGS and our partners.
The year of 2022 was big for the Sea-Floor Mapping Group at the Woods Hole Coastal and Marine Science Center! These data were collected as part of a collaborative research program and include data collected by USGS and our partners.
USGS scientists collect core samples from marsh to explore the drives of wetland accretion in the face of rising seas and human impacts impact the evolution on salt marshes.
USGS scientists collect core samples from marsh to explore the drives of wetland accretion in the face of rising seas and human impacts impact the evolution on salt marshes.
USGS scientists collect core samples from marsh to explore the drives of wetland accretion in the face of rising seas and human impacts impact the evolution on salt marshes.
USGS scientists collect core samples from marsh to explore the drives of wetland accretion in the face of rising seas and human impacts impact the evolution on salt marshes.
As sea levels rise, salt water extends further up tidal rivers. As sea-level rise accelerates, vegetation transitions are increasingly observed and USGS scientists are busy assessing those changes. USGS scientists take soil cores in the marsh.
As sea levels rise, salt water extends further up tidal rivers. As sea-level rise accelerates, vegetation transitions are increasingly observed and USGS scientists are busy assessing those changes. USGS scientists take soil cores in the marsh.
Observational data are key to identify landscape change tipping points and the role of invasive species on coastal change. Photo of USGS staff mapping invasive Phragmites on Assateague Island National Seashore. Photo by Seth Ackerman.
Observational data are key to identify landscape change tipping points and the role of invasive species on coastal change. Photo of USGS staff mapping invasive Phragmites on Assateague Island National Seashore. Photo by Seth Ackerman.
USGS scientists working on FLACC study coastal change, and develop techniques and metrics to measure past, present, and future shoreline change rates along the sandy coasts of the U.S.
USGS scientists working on FLACC study coastal change, and develop techniques and metrics to measure past, present, and future shoreline change rates along the sandy coasts of the U.S.
Test track from 1970’s commercial dredging equipment trials through a nodule field on the Blake Plateau, imaged in 2022 from an autonomous underwater vehicle (BOEM/USGS).
Test track from 1970’s commercial dredging equipment trials through a nodule field on the Blake Plateau, imaged in 2022 from an autonomous underwater vehicle (BOEM/USGS).