As part of the USGS Coral Reef Project, the USGS is working on the west coast of Guam to help determine the effects of sedimentation in nearshore waters.

Overview
The Territory of Guam is an organized unincorporated territory of the United States. The island itself is 30 miles (48 km) long and 4 mi (6 km) to 12 mi (19 km) wide. It is the southernmost island in the Marianas island chain and is the largest island in Micronesia. Unlike many of the northern Marianas islands, Guam is not volcanically active. The northern part of the island is a forested coralline limestone plateau while the south contains volcanic peaks covered in forest and grassland. A coral reef surrounds most of the island, except in areas where bays exist that provide access to small rivers and streams that run down from the hills into the Pacific Ocean and Philippine Sea.
Motivation
Human activity has significantly increased the rate of sedimentation along many areas of Guam’s coastline. These human activities are related primarily to land-management practices, including urban development, unregulated use of off-road vehicles, and illegal wildfires. The wildfires, which are intentionally set by hunters to clear lines of sight and draw in new game, remove the grasses and small trees that stabilize the soil. Typhoons strike Guam frequently, commonly dropping more than 30 cm of rain in 24 hours and flushing the unstabilized soil down to the coast and into the nearshore waters.
The USGS is working with the National Park Service on the west coast of the island to help determine the effects of sedimentation in the nearshore waters, including those of War in the Pacific National Historical Park. This is especially significant because the wet season (July to December), during which time large amounts of unstabilized soil wash down to the ocean, coincides with peak coral spawning and larvae settlement. Other partners in these efforts include NOAA, U.S. Coral Reef Task Force (USCRTF) Guam Local Action Strategy (LAS) for Land-Based Pollution (LBP), University of Guam, and Woods Hole Oceanographic Institute (WHOI).
Guam is a U.S. island territory in the Western Pacific, the southernmost island in the Marianas island chain and the largest island in Micronesia. Guam is just one of the USGS Coral Reef Project's study locations.
Reef Hydrodynamics and Sediment Processes
Role of Reefs in Coastal Protection
Reef Resource Assessments - Planning for the Future
Hydrogeology and Reef Health
Climate Change and Land-use Histories
Below are data releases associated with this project.
Projected flooding extents and depths based on 10-, 50-, 100-, and 500-year wave-energy return periods, with and without coral reefs, for the States of Hawaii and Florida, the Territories of Guam, American Samoa, Puerto Rico, and the U.S. Virgin Islands,
Below are publications associated with this project.
The value of US coral reefs for flood risk reduction
Rigorously valuing the role of U.S. coral reefs in coastal hazard risk reduction
A 50-year Sr/Ca time series from an enclosed, shallow-water Guam coral: In situ monitoring and extraction of a temperature trend, annual cycle, and ENSO and PDO signals
Tropical cyclone projections: Changing climate threats for Pacific Island defense installations
Challenges of forecasting flooding on coral reef–lined coasts
The effectiveness of coral reefs for coastal hazard risk reduction and adaptation
Coastal circulation and water-column properties in the War in the Pacific National Historical Park, Guam: measurements and modeling of waves, currents, temperature, salinity, and turbidity, April-August 2012
Historic impact of watershed change and sedimentation to reefs along west-central Guam
Rapid fluctuations in flow and water-column properties in Asan Bay, Guam: implications for selective resilience of coral reefs in warming seas
From ridge to reef—linking erosion and changing watersheds to impacts on the coral reef ecosystems of Hawai‘i and the Pacific Ocean
The use (and misuse) of sediment traps in coral reef environments: Theory, observations, and suggested protocols
Coastal Circulation and Sediment Dynamics in War-in-the-Pacific National Historical Park, Guam; measurements of waves, currents, temperature, salinity, and turbidity, June 2007-January 2008
Below are partners associated with this project.
- Overview
As part of the USGS Coral Reef Project, the USGS is working on the west coast of Guam to help determine the effects of sedimentation in nearshore waters.
Sources/Usage: Public Domain. Visit Media to see details.Satellite photo of Guam from NASA’s Earth Observing-1 (EO-1) satellite's Advanced Land Imager (ALI). Overview
The Territory of Guam is an organized unincorporated territory of the United States. The island itself is 30 miles (48 km) long and 4 mi (6 km) to 12 mi (19 km) wide. It is the southernmost island in the Marianas island chain and is the largest island in Micronesia. Unlike many of the northern Marianas islands, Guam is not volcanically active. The northern part of the island is a forested coralline limestone plateau while the south contains volcanic peaks covered in forest and grassland. A coral reef surrounds most of the island, except in areas where bays exist that provide access to small rivers and streams that run down from the hills into the Pacific Ocean and Philippine Sea.
Motivation
Human activity has significantly increased the rate of sedimentation along many areas of Guam’s coastline. These human activities are related primarily to land-management practices, including urban development, unregulated use of off-road vehicles, and illegal wildfires. The wildfires, which are intentionally set by hunters to clear lines of sight and draw in new game, remove the grasses and small trees that stabilize the soil. Typhoons strike Guam frequently, commonly dropping more than 30 cm of rain in 24 hours and flushing the unstabilized soil down to the coast and into the nearshore waters.
Underwater photograph of a wave breaking over the shallow fringing coral reef flat in Tumon Bay, Guam. The USGS is working with the National Park Service on the west coast of the island to help determine the effects of sedimentation in the nearshore waters, including those of War in the Pacific National Historical Park. This is especially significant because the wet season (July to December), during which time large amounts of unstabilized soil wash down to the ocean, coincides with peak coral spawning and larvae settlement. Other partners in these efforts include NOAA, U.S. Coral Reef Task Force (USCRTF) Guam Local Action Strategy (LAS) for Land-Based Pollution (LBP), University of Guam, and Woods Hole Oceanographic Institute (WHOI).
- Science
Guam is a U.S. island territory in the Western Pacific, the southernmost island in the Marianas island chain and the largest island in Micronesia. Guam is just one of the USGS Coral Reef Project's study locations.
Reef Hydrodynamics and Sediment Processes
As part of the USGS Coral Reef Project, the overall objective of this research effort is to better understand how circulation and sediment processes impact coral reefs and their adjacent coastlines.Role of Reefs in Coastal Protection
We are combining ocean, engineering, ecologic, social, and economic modeling to provide a high-resolution, rigorous, spatially-explicit valuation of the coastal flood protection benefits provided by coral reefs and the cost effectiveness of reef restoration for enhancing those benefits.Reef Resource Assessments - Planning for the Future
We are mapping and assessing all of the important geologic and oceanographic factors to identify those coral reefs most at risk and those reefs that are potentially the most resilient and the most likely to recover from natural and human-driven impacts.Hydrogeology and Reef Health
As part of the USGS Coral Reef Project, we are conducting geophysical and geochemical research to address questions about coastal groundwater-to-reef flow and coral reef health, with the goal of informing management decisions related to planning and implementing activities in priority watershed-coral reef systems.Climate Change and Land-use Histories
As part of the USGS Coral Reef Project, we are developing new and unique oceanographic and environmental archives from coral skeleton records to better understand the compounding effects of land-use and environmental change on coral reef health. - Data
Below are data releases associated with this project.
Projected flooding extents and depths based on 10-, 50-, 100-, and 500-year wave-energy return periods, with and without coral reefs, for the States of Hawaii and Florida, the Territories of Guam, American Samoa, Puerto Rico, and the U.S. Virgin Islands,
This data release provides flooding extent polygons (flood masks) and depth values (flood points) based on wave-driven total water levels for 22 locations within the States of Hawaii and Florida, the Territories of Guam, American Samoa, Puerto Rico, and the U.S. Virgin Islands, and the Commonwealth of the Northern Mariana Islands. For each of the 22 locations there are eight associated flood mask - Publications
Below are publications associated with this project.
Filter Total Items: 13The value of US coral reefs for flood risk reduction
Habitats, such as coral reefs, can mitigate increasing flood damages through coastal protection services. We provide a fine-scale, national valuation of the flood risk reduction benefits of coral habitats to people, property, economies and infrastructure. Across 3,100 km of US coastline, the top-most 1 m of coral reefs prevents the 100-yr flood from growing by 23% (113 km2), avoiding flooding to 5AuthorsBorja G. Reguero, Curt Storlazzi, Ann E. Gibbs, James B. Shope, Aaron Cole, Kristen A. Cumming, Mike BeckRigorously valuing the role of U.S. coral reefs in coastal hazard risk reduction
The degradation of coastal habitats, particularly coral reefs, raises risks by increasing the exposure of coastal communities to flooding hazards. The protective services of these natural defenses are not assessed in the same rigorous economic terms as artificial defenses, such as seawalls, and therefore often are not considered in decision making. Here we combine engineering, ecologic, geospatialAuthorsCurt D. Storlazzi, Borja G. Reguero, Aaron Cole, Erik Lowe, James B. Shope, Ann E. Gibbs, Barry A. Nickel, Robert T. McCall, Ap R. van Dongeren, Michael W. BeckA 50-year Sr/Ca time series from an enclosed, shallow-water Guam coral: In situ monitoring and extraction of a temperature trend, annual cycle, and ENSO and PDO signals
Located on the northern edge of the West Pacific Warm Pool and having a developed economy and modern infrastructure, Guam is well positioned and equipped for obtaining natural records of the west Pacific maritime paleoclimate. This study was a proof of concept to explore whether useful climate proxy records might be obtained from coral at readily accessible, even if geochemically nonoptimal, coastAuthorsTomoko Bell, Mark Lander, John Jenson, Richard Randall, Judson W. Partin, Nancy G. ProutyTropical cyclone projections: Changing climate threats for Pacific Island defense installations
Potential changing climate threats in the tropical and subtropical North Pacific Ocean were assessed, using coupled ocean-atmosphere and atmosphere-only general circulation models, to explore their response to projected increasing greenhouse gas emissions. Tropical cyclone occurrence, described by their frequency and intensity, near islands housing major U.S. defense installations was the primaryAuthorsMatthew J. Widlansky, Hariharasubramanian Annamalai, Stephen B. Gingerich, Curt D. Storlazzi, John J. Marra, Kevin I. Hodges, Barry Choy, Akio KitohChallenges of forecasting flooding on coral reef–lined coasts
Understanding wave-driven coastal flooding is a challenging scientific problem; the need for forecasts is becoming more urgent because of sea level rise, climate change, and ever-growing coastal populations. The tools developed for sandy shorelines are generally not applicable to coral reef–lined coasts with their complex bathymetry, hydrodynamically rough reef platforms, steep and poorly sorted bAuthorsCurt D. StorlazziThe effectiveness of coral reefs for coastal hazard risk reduction and adaptation
The world’s coastal zones are experiencing rapid development and an increase in storms and flooding. These hazards put coastal communities at heightened risk, which may increase with habitat loss. Here we analyse globally the role and cost effectiveness of coral reefs in risk reduction. Meta-analyses reveal that coral reefs provide substantial protection against natural hazards by reducing wave enAuthorsFilippo Ferrario, Michael W. Beck, Curt D. Storlazzi, Fiorenza Micheli, Christine C. Shepard, Laura AiroldiCoastal circulation and water-column properties in the War in the Pacific National Historical Park, Guam: measurements and modeling of waves, currents, temperature, salinity, and turbidity, April-August 2012
The U.S. Geological Survey (USGS) Pacific Coastal and Marine Science Center (PCMSC) initiated an investigation in the National Park Service’s (NPS) War in the Pacific National Historical Park (WAPA) to provide baseline scientific information on coastal circulation and water-column properties along west-central Guam, focusing on WAPA’s Agat Unit, as it relates to the transport and settlement of corAuthorsCurt D. Storlazzi, Olivia M. Cheriton, Jamie M.R. Lescinski, Joshua B. LoganHistoric impact of watershed change and sedimentation to reefs along west-central Guam
Using coral growth parameters (extension, density, calcification rates, and luminescence) and geochemical measurements (barium to calcium rations; Ba/Ca) from coral cores collected in west-central Guam, we provide a historic perspective on sediment input to coral reefs adjacent to the Piti-Asan watershed. The months of August through December are dominated by increased coral Ba/Ca values, correspoAuthorsNancy G. Prouty, Curt D. Storlazzi, Amanda L. McCutcheon, John W. JensonRapid fluctuations in flow and water-column properties in Asan Bay, Guam: implications for selective resilience of coral reefs in warming seas
Hydrodynamics and water-column properties were investigated off west-central Guam from July 2007 through January 2008. Rapid fluctuations, on time scales of 10s of min, in currents, temperature, salinity, and acoustic backscatter were observed to occur on sub-diurnal frequencies along more than 2 km of the fore reef but not at the reef crest. During periods characterized by higher sea-surface tempAuthorsCurt D. Storlazzi, Michael E. Field, Olivia M. Cheriton, M.K. Presto, J.B. LoganFrom ridge to reef—linking erosion and changing watersheds to impacts on the coral reef ecosystems of Hawai‘i and the Pacific Ocean
Coral reef ecosystems are threatened by unprecedented watershed changes in the United States and worldwide. These ecosystems sustain fishing and tourism industries essential to the economic survival of many communities. Sediment, nutrients, and pollutants from watersheds are increasingly transported to coastal waters, where these contaminants damage corals. Although pollution from watersheds is onAuthorsJonathan D. Stock, Susan A. Cochran, Michael E. Field, James D. Jacobi, Gordon TribbleThe use (and misuse) of sediment traps in coral reef environments: Theory, observations, and suggested protocols
Sediment traps are commonly used as standard tools for monitoring “sedimentation” in coral reef environments. In much of the literature where sediment traps were used to measure the effects of “sedimentation” on corals, it is clear from deployment descriptions and interpretations of the resulting data that information derived from sediment traps has frequently been misinterpreted or misapplied. DeAuthorsC. D. Storlazzi, M.E. Field, Michael H. BothnerCoastal Circulation and Sediment Dynamics in War-in-the-Pacific National Historical Park, Guam; measurements of waves, currents, temperature, salinity, and turbidity, June 2007-January 2008
Flow in and around coral reefs affects a number of physical, chemical and biologic processes that influence the health and sustainability of coral reef ecosystems. These range from the residence time of sediment and contaminants to nutrient uptake and larval retention and dispersal. As currents approach a coast they diverge to flow around reef structures, causing high horizontal and vertical shearAuthorsCurt D. Storlazzi, M. Katherine Presto, Joshua B. Logan - Partners
Below are partners associated with this project.