Physical scientist Jackson Currie steers a personal water craft (PWC) equipped with GPS and echo sounder through the waves of the nearshore area of Zmudowski State Beach in Moss Landing, California.
Images
Physical scientist Jackson Currie steers a personal water craft (PWC) equipped with GPS and echo sounder through the waves of the nearshore area of Zmudowski State Beach in Moss Landing, California.
A tidal marsh at Billy Frank Jr. Nisqually National Wildlife Refuge, WA.
A tidal marsh at Billy Frank Jr. Nisqually National Wildlife Refuge, WA.
Photograph showing the impact of a large wave at the south shore of Laysan Island, with endangered Laysan teal in the foreground.
Location: Laysan Islands (Northwestern Hawaiian Islands).
Photograph showing the impact of a large wave at the south shore of Laysan Island, with endangered Laysan teal in the foreground.
Location: Laysan Islands (Northwestern Hawaiian Islands).
Seafloor image at a deepwater (~1400 m water depth) seep site on the New England margin. Seafloor conditions here are well inside the pressure-temperature stability field for methane hydrate. Gas being emitted below the rock overhang has formed gas hydrate (the white ice-like material). Distinct bubbles are visible in the foreground. The red laser scale is 10 cm.
Seafloor image at a deepwater (~1400 m water depth) seep site on the New England margin. Seafloor conditions here are well inside the pressure-temperature stability field for methane hydrate. Gas being emitted below the rock overhang has formed gas hydrate (the white ice-like material). Distinct bubbles are visible in the foreground. The red laser scale is 10 cm.
Two researchers deploying a fishing trawl into Lake Superior while aboard the USGS GLSC's R/V Kiyi
Two researchers deploying a fishing trawl into Lake Superior while aboard the USGS GLSC's R/V Kiyi
Photograph of shallow-water coral bleaching at Sombrero de Pelo reef in Pacific Panama during the 2015-2016 El Nino event. Because of the influence of internal waves, corals growing at deeper locations at this site did not bleach.
Photograph of shallow-water coral bleaching at Sombrero de Pelo reef in Pacific Panama during the 2015-2016 El Nino event. Because of the influence of internal waves, corals growing at deeper locations at this site did not bleach.
Pacific Ocean temperature differences during this winter’s record-setting El Niño. Dark red areas are much warmer than average.
Pacific Ocean temperature differences during this winter’s record-setting El Niño. Dark red areas are much warmer than average.
Sea surface temperature differences on March 1, 2016. Dark red indicates much warmer water.
Sea surface temperature differences on March 1, 2016. Dark red indicates much warmer water.
Kim Yates (left) and Nate Smiley of the USGS St. Petersburg Coastal and Marine Science Center measure acidity, nutrient levels, and other characteristics of water sampled near the coral reef off Kahekili Beach Park, Maui, Hawai‘i, in March 2016.
Kim Yates (left) and Nate Smiley of the USGS St. Petersburg Coastal and Marine Science Center measure acidity, nutrient levels, and other characteristics of water sampled near the coral reef off Kahekili Beach Park, Maui, Hawai‘i, in March 2016.
Preliminary map products derived from the UAS imagery collected near Coast Guard Beach, Cape Cod National Seashore
linkPreliminary map products derived from the UAS imagery collected near Coast Guard Beach, Cape Cod National Seashore on 1 March 2016. Left: shaded relief color contoured digital elevation map on a 0.1-meter grid. Right: orthophotomosaic (0.05-meter resolution) overlaid on the shaded relief map.
Preliminary map products derived from the UAS imagery collected near Coast Guard Beach, Cape Cod National Seashore
linkPreliminary map products derived from the UAS imagery collected near Coast Guard Beach, Cape Cod National Seashore on 1 March 2016. Left: shaded relief color contoured digital elevation map on a 0.1-meter grid. Right: orthophotomosaic (0.05-meter resolution) overlaid on the shaded relief map.
Glacier Bay, Alaska, dive team.
USGS geologist Jamie Conrad uses a map of the seafloor off Southern California to plan high-resolution mapping southwest of Santa Catalina Island. Small inset shows seafloor data collected by the ship that reveals hills, gullies, and basins.
USGS geologist Jamie Conrad uses a map of the seafloor off Southern California to plan high-resolution mapping southwest of Santa Catalina Island. Small inset shows seafloor data collected by the ship that reveals hills, gullies, and basins.
A ship will tow this green cable, which contains underwater microphones that record sound reflected off layers beneath the seafloor. USGS scientists will use the data to pinpoint the location of faults.
A ship will tow this green cable, which contains underwater microphones that record sound reflected off layers beneath the seafloor. USGS scientists will use the data to pinpoint the location of faults.
Large waves breaking on cliffs in western Santa Cruz, California, February 13, 2016.
Large waves breaking on cliffs in western Santa Cruz, California, February 13, 2016.
The USGS Coastal and Estuarine Dynamics Group will be deploying a Nanopod at Pea Island DUNEX experiment site to collect oceanographic information.
The USGS Coastal and Estuarine Dynamics Group will be deploying a Nanopod at Pea Island DUNEX experiment site to collect oceanographic information.
USGS scientists survey a beach near San Francisco to assist with a comparison of data derived from aerial photos and lidar.
USGS scientists survey a beach near San Francisco to assist with a comparison of data derived from aerial photos and lidar.
The coastal bluff along East Cliff Drive in Santa Cruz, California are especially vulnerable to rising sea level during big storms. Sometimes even the rip-rap, put in place to protect roadways and homes, cannot protect the bluffs from erosion.
The coastal bluff along East Cliff Drive in Santa Cruz, California are especially vulnerable to rising sea level during big storms. Sometimes even the rip-rap, put in place to protect roadways and homes, cannot protect the bluffs from erosion.
View of the Santa Cruz Beach Boardwalk amusement park in Santa Cruz, California. Photo was taken from the bluff on East Cliff Drive, east of the San Lorenzo River mouth. Sand on the beach gets eroded, redistributed, and deposited due to the dynamic conditions brought about by storms and changing river flow.
View of the Santa Cruz Beach Boardwalk amusement park in Santa Cruz, California. Photo was taken from the bluff on East Cliff Drive, east of the San Lorenzo River mouth. Sand on the beach gets eroded, redistributed, and deposited due to the dynamic conditions brought about by storms and changing river flow.
Waves flood across a coastal road near Santa Cruz, California.
Waves flood across a coastal road near Santa Cruz, California.
On remote Barter Island, Alaska, Bruce Richmond (right) and Cordell Johnson drill into 500-foot-thick permafrost using a handheld drill with a 2-inch drill bit—a challenging task! It can take 3 hours to drill nearly 20 feet down.
On remote Barter Island, Alaska, Bruce Richmond (right) and Cordell Johnson drill into 500-foot-thick permafrost using a handheld drill with a 2-inch drill bit—a challenging task! It can take 3 hours to drill nearly 20 feet down.
Image of the unstructured finite element mesh model grid encompassing the Atlantic Ocean, Caribbean Sea and Gulf of Mexico
linkThe advanced circulation (ADCIRC) model unstructured finite element mesh spans the western North Atlantic Tidal domain to the 60-degree west meridian, including the Atlantic Ocean, Caribbean Sea and Gulf of Mexico.
Image of the unstructured finite element mesh model grid encompassing the Atlantic Ocean, Caribbean Sea and Gulf of Mexico
linkThe advanced circulation (ADCIRC) model unstructured finite element mesh spans the western North Atlantic Tidal domain to the 60-degree west meridian, including the Atlantic Ocean, Caribbean Sea and Gulf of Mexico.