Images

Near vertical (top, middle) and low angle oblique (bottom) aerial photographs of Rodanthe, North Carolina. View looking west along the North Carolina shore. High waves and storm surge from Hurricane Joaquin eroded the beach, exposing the pilings of the homes to wave attack (green and orange arrows).

Near vertical (top, middle) and low angle oblique (bottom) aerial photographs of Salvo, North Carolina. View looking west along the North Carolina shore. Waves and surge from Hurricane Joaquin eroded the beach, causing significant shoreline retreat and a narrower beach, leaving deposits of darker sand at the base of the dune (green arrow).

Near vertical (top, middle) and low angle oblique (bottom) aerial photographs of Hatteras, North Carolina. View looking north along the North Carolina shore. Waves and surge from Hurricane Joaquin eroded the beach, causing significant shoreline retreat and a narrower beach at the location of the Hurricane Isabel breach in 2003 (green arrow).

Near vertical (top, middle) and low angle oblique (bottom) aerial photographs of New Drum Inlet, Core Banks, North Carolina. View looking northwest along the North Carolina shore.

Near vertical (top, middle) and low angle oblique (bottom) aerial photographs of Bear Inlet, North Carolina. View looking northwest along the North Carolina shore. High waves and storm surge from Hurricane Joaquin eroded the beaches, moving sand inland (green arrow) and reshaping the flood-tidal shoals.

Near vertical (top, middle) and low angle oblique (bottom) aerial photographs of Camp Lejeune, North Carolina. View looking northwest along the North Carolina shore. Waves and surge from Hurricane Joaquin eroded the beach, causing significant shoreline retreat and a narrower beach.

Near vertical (top, middle) and low angle oblique (bottom) aerial photographs of Topsail, North Carolina. View looking northwest along the North Carolina shore. Elevated storm-induced water levels overtopped the low dunes here causing the dune to overwash. Sand was transported landward, burying the marsh (green arrow).

Personal watercraft were utilized to collect bathymetry in the surf zone and shore face (top left), setup on the beach (top right), instrument configuration (bottom left) and Pelican case hardware configuration (bottom right).

The relatively new camera stations at Santa Cruz and Madeira Beach have not yet imaged many rip channels, so this is an example from the U.S. Army Corps of Engineers Field Research Facility in Duck, North Carolina. In this time-averaged image from video taken September 1, 2015, the dark horizontal bands perpendicular to the beach indicate rip channels.

Maps showing (A) acoustic backscatter and (B) bathymetry collected with the inteferomentric sonar

Graphics and photos showing the overwash characteristics of 3 locations at Fire Island, NY

Photo showing the complex geomorphology of the marsh landscape of the Grand Bay National Wildlife Refuge/Grand Bay National Estuarine Research Reserve in coastal Alabama and Mississippi. (1) Geology—a tidal creek that at lower sea level than present served as a distributary channel of a river-delta system. (2) Hydrodynamics—wave erosion of the marsh edge.

Photo showing multiple geomorphic environments including from left to right: the Atlantic Ocean, beach, dunes, and island interior.

This USGS vessel acquires single-beam bathymetry in shallow nearshore environments. We acquire repeat bathymetry surveys over multiple years and compute changes in bathymetry, thus allowing us to identify hotspots of erosion and deposition on short timescales.

Waves breaking over offshore reefs on Kwajalein Atoll, in the Marshall Islands, where reefs are protecting developed land from flooding.

Aerial image showing beach and offshore reef

Aerial image showing beach and offshore reef

View of Hanauma Bay Nature Preserve in Hawaii. Hanauma is located along the southeast coast of the Island of Oʻahu. It is known for its abundance of marine life and is a popular snorkeling location.

Two colonies of the mustard hill coral, Porites astreoides, one apparently healthy (left) and one visibly bleached (right) during a coral-bleaching event at Hen and Chickens Sanctuary Preservation Area, Plantation Key, FL, USA. When ocean temperatures were unusually warm in the Florida Keys National Marine Sanctuary in October 2015, coral ble

Concrete and stainless-steel marker photographed 17 years after being installed into the reef in 1998 by Harold Hudson, NOAA. Scraping and grazing by parrotfish, chemical erosion from sponges, and wave action all combine to winnow away the dead skeletons of coral—a process known as reef erosion.

Here are shown two mustard hill corals (Porites astreoides) growing side-by-side, one (right) that has succumbed to heat stress and lost its symbiotic algae, and one (left) that has not.