The AIM (Aerial Imaging and Mapping group) collected UAS imagery for scientists at The Marine Biological Laboratory (MBL) from the Plum Island estuary in Rowley MA. Inke Forbrich from MBL will lead the analysis looking at the reflectance index NDVI for vegetation surrounding a gas flux tower installed in t
Images
Woods Hole Coastal and Marine Science Center images
The AIM (Aerial Imaging and Mapping group) collected UAS imagery for scientists at The Marine Biological Laboratory (MBL) from the Plum Island estuary in Rowley MA. Inke Forbrich from MBL will lead the analysis looking at the reflectance index NDVI for vegetation surrounding a gas flux tower installed in t
The AIM (Aerial Imaging and Mapping group) collected UAS imagery for scientists at The Marine Biological Laboratory (MBL) from the Plum Island estuary in Rowley MA. Inke Forbrich from MBL will lead the analysis looking at the reflectance index NDVI for vegetation surrounding a gas flux tower installed in t
The AIM (Aerial Imaging and Mapping group) collected UAS imagery for scientists at The Marine Biological Laboratory (MBL) from the Plum Island estuary in Rowley MA. Inke Forbrich from MBL will lead the analysis looking at the reflectance index NDVI for vegetation surrounding a gas flux tower installed in t
Data locations for Ice Island Arctic Ocean Heat Flow Studies
Data locations for Ice Island Arctic Ocean Heat Flow StudiesData locations for Ice Island Arctic Ocean Heat Flow Studies
Data locations for Ice Island Arctic Ocean Heat Flow Studies
Data locations for Ice Island Arctic Ocean Heat Flow StudiesData locations for Ice Island Arctic Ocean Heat Flow Studies
Two red sea urchins (Mesocentrotus franciscanus) sit on the deck of the R/V Falkor. These sea urchins were collected during the #HuntingBubbles research cruise led by the USGS and Schmidt Ocean Institute, which focused on exploring and understanding methane seeps and the communities that depend on them along the Cascadia Margin.
Two red sea urchins (Mesocentrotus franciscanus) sit on the deck of the R/V Falkor. These sea urchins were collected during the #HuntingBubbles research cruise led by the USGS and Schmidt Ocean Institute, which focused on exploring and understanding methane seeps and the communities that depend on them along the Cascadia Margin.
Bike path skirting cobbled beaches of Falmouth, Massachusetts.
Bike path skirting cobbled beaches of Falmouth, Massachusetts.
Low-altitude aerial photograph of Plum Island, Massachusetts
Low-altitude aerial photograph of Plum Island, MassachusettsLow-altitude aerial photograph of Plum Island, Massachusetts, , from USGS field activity 2019-009-FA.
Low-altitude aerial photograph of Plum Island, Massachusetts
Low-altitude aerial photograph of Plum Island, MassachusettsLow-altitude aerial photograph of Plum Island, Massachusetts, , from USGS field activity 2019-009-FA.
USGS pilot landing an unmanned aerial system on Dauphin Island, AL
USGS pilot landing an unmanned aerial system on Dauphin Island, ALUSGS unmanned aerial system (drone) pilot collecting aerial imagery and ground control points for the Coastal Resource Evaulation for Management Applications (CREMA) project on Dauphin Island, Alabama
USGS pilot landing an unmanned aerial system on Dauphin Island, AL
USGS pilot landing an unmanned aerial system on Dauphin Island, ALUSGS unmanned aerial system (drone) pilot collecting aerial imagery and ground control points for the Coastal Resource Evaulation for Management Applications (CREMA) project on Dauphin Island, Alabama
Surficial Geology Map of Nantucket and Marthas Vineyard, MA
Surficial Geology Map of Nantucket and Marthas Vineyard, MAMap showing the surficial geology from this study and Baldwin and others (2016) with equivalent onshore geology (adapted from Stone and DiGiacomo-Cohen, 2009). The areal extents over which offshore subsurface geologic units crop out at the sea floor were interpreted from seismic-reflection data.
Surficial Geology Map of Nantucket and Marthas Vineyard, MA
Surficial Geology Map of Nantucket and Marthas Vineyard, MAMap showing the surficial geology from this study and Baldwin and others (2016) with equivalent onshore geology (adapted from Stone and DiGiacomo-Cohen, 2009). The areal extents over which offshore subsurface geologic units crop out at the sea floor were interpreted from seismic-reflection data.
Northeast Region Photo Contest Winner | February 2019 | Honorable Mention
Steve Suttles (L) and John Borden (R) onboard Muddy Waters research boat removing meter in Wellfleet, MA used to quantify critical sediment transport parameters of diverse wetland complexes within 4 NCBN parks in order to inform management efforts.
Northeast Region Photo Contest Winner | February 2019 | Honorable Mention
Steve Suttles (L) and John Borden (R) onboard Muddy Waters research boat removing meter in Wellfleet, MA used to quantify critical sediment transport parameters of diverse wetland complexes within 4 NCBN parks in order to inform management efforts.
Simulation of wave-driven flooding on Marshall Island
Simulation of wave-driven flooding on Marshall IslandReefs provide protection from waves and wave-driven flooding. A snapshot from the simulation of wave-driven flooding and island overwash for an annual storm at the Republic of the Marshall Islands is shown.
Simulation of wave-driven flooding on Marshall Island
Simulation of wave-driven flooding on Marshall IslandReefs provide protection from waves and wave-driven flooding. A snapshot from the simulation of wave-driven flooding and island overwash for an annual storm at the Republic of the Marshall Islands is shown.
First arrival times of contaminants at each location (lighter colors indicate longer time since the storm) for conditions observed during Hurricane Florence (top), and two hypothetical events: one with smaller rainfall (middle) and another with a different post-storm wind pattern (bottom).
First arrival times of contaminants at each location (lighter colors indicate longer time since the storm) for conditions observed during Hurricane Florence (top), and two hypothetical events: one with smaller rainfall (middle) and another with a different post-storm wind pattern (bottom).
Elevation data for land and submerged areas, Barnegat Bay, NJ
Elevation data for land and submerged areas, Barnegat Bay, NJCoastal storms can severely alter the topography and ecosystems along heavily populated coastal regions. Seamless integrated elevation data for both land and submerged areas in Barnegat Bay, New Jersey, are fundamental to coastal planning of the northeastern U.S. Atlantic coast.
Elevation data for land and submerged areas, Barnegat Bay, NJ
Elevation data for land and submerged areas, Barnegat Bay, NJCoastal storms can severely alter the topography and ecosystems along heavily populated coastal regions. Seamless integrated elevation data for both land and submerged areas in Barnegat Bay, New Jersey, are fundamental to coastal planning of the northeastern U.S. Atlantic coast.
Cave passage and diver (Bil Philips, cave explorer) in Ox Bel Ha Cave System of the northeastern Yucatan Peninsula.
Cave passage and diver (Bil Philips, cave explorer) in Ox Bel Ha Cave System of the northeastern Yucatan Peninsula.
Storm and sea level rise scenario model for Dauphin Island, Alabama
Storm and sea level rise scenario model for Dauphin Island, AlabamaStorm and sea level rise scenario models, like the one shown here, can be used to explore the future. This model shows what Dauphin Island may look like 10 years from now if storms become stronger and more frequent (Passeri and others, 2018).
Storm and sea level rise scenario model for Dauphin Island, Alabama
Storm and sea level rise scenario model for Dauphin Island, AlabamaStorm and sea level rise scenario models, like the one shown here, can be used to explore the future. This model shows what Dauphin Island may look like 10 years from now if storms become stronger and more frequent (Passeri and others, 2018).
Gas hydrate (orange material) and gas bubbles near the seafloor in the northern Gulf of America. As the methane bubbles are emitted, a rind of gas hydrate immediately forms around some of them. If more bubbles continue to feed from below, gas hydrate forms.
Gas hydrate (orange material) and gas bubbles near the seafloor in the northern Gulf of America. As the methane bubbles are emitted, a rind of gas hydrate immediately forms around some of them. If more bubbles continue to feed from below, gas hydrate forms.
Part of the Akumal coastline in Quintana Roo, Mexico, near where the Ox Bel Ha cave system is located.
Part of the Akumal coastline in Quintana Roo, Mexico, near where the Ox Bel Ha cave system is located.
SEABed Observation and Sampling System (SEABOSS) (center image) and the MiniSEABOSS (right) designed for rapid, inexpensive, and effective collection of seabed imagery (photographs and video) as well sediment samples from the coastal/inner-continental shelf regions.
SEABed Observation and Sampling System (SEABOSS) (center image) and the MiniSEABOSS (right) designed for rapid, inexpensive, and effective collection of seabed imagery (photographs and video) as well sediment samples from the coastal/inner-continental shelf regions.
Department of Interior UAS pilots from left to right – Elizabeth Pendleton (USGS, Woods Hole, MA), Colin Milone (Office of Aviation Services, AK), John Vogel (USGS; Flagstaff, AZ), Sandy Brosnahan (USGS, Woods Hole, MA), Brandon Forbes (USGS; Tucson, AZ), Chris Holmquist-Johnson (USGS; Fort Collins, CO),&nb
Department of Interior UAS pilots from left to right – Elizabeth Pendleton (USGS, Woods Hole, MA), Colin Milone (Office of Aviation Services, AK), John Vogel (USGS; Flagstaff, AZ), Sandy Brosnahan (USGS, Woods Hole, MA), Brandon Forbes (USGS; Tucson, AZ), Chris Holmquist-Johnson (USGS; Fort Collins, CO),&nb
Sediment textures distribution from Nantucket and Marthas Vineyard, MA
Sediment textures distribution from Nantucket and Marthas Vineyard, MAThe distribution of sediment textures within the study area. The bottom-type classification is from Barnhardt and others (1998) and is based on 16 sediment classes. The classification is based on four sediment units that include gravel (G), mud (M), rock (R), and sand (S). If the texture is greater than 90 percent, it is labeled with a single letter.
Sediment textures distribution from Nantucket and Marthas Vineyard, MA
Sediment textures distribution from Nantucket and Marthas Vineyard, MAThe distribution of sediment textures within the study area. The bottom-type classification is from Barnhardt and others (1998) and is based on 16 sediment classes. The classification is based on four sediment units that include gravel (G), mud (M), rock (R), and sand (S). If the texture is greater than 90 percent, it is labeled with a single letter.
Scientist surveying the behavior of birds at Pelican Island, Alabama
Scientist surveying the behavior of birds at Pelican Island, AlabamaScientist surveying the presence and behavior of birds at Pelican Island, Alabama. The CMHRP is working with personnel within the Ecosystems Mission Area on this project to identify how physical characteristics of barrier islands influence use by wintering shorebirds.
Scientist surveying the behavior of birds at Pelican Island, Alabama
Scientist surveying the behavior of birds at Pelican Island, AlabamaScientist surveying the presence and behavior of birds at Pelican Island, Alabama. The CMHRP is working with personnel within the Ecosystems Mission Area on this project to identify how physical characteristics of barrier islands influence use by wintering shorebirds.
Waapumeequan (Rising Feather) and Neesweekokotywak (Two Crows)
Waapumeequan (Rising Feather) and Neesweekokotywak (Two Crows)Waapumeequan (Rising Feather) and Neesweekokotywak (Two Crows), otherwise known as Kendall Currence and Troy Currence.
Waapumeequan (Rising Feather) and Neesweekokotywak (Two Crows)
Waapumeequan (Rising Feather) and Neesweekokotywak (Two Crows)Waapumeequan (Rising Feather) and Neesweekokotywak (Two Crows), otherwise known as Kendall Currence and Troy Currence.