Curt Storlazzi, PhD
My interests span the coastal zone, from seacliff erosional processes to sediment dynamics in the shallow coastal ocean. My research focuses on the quantitative study of hydrodynamics, sediment transport, and geomorphology in coastal and marine environments.
Research Topics
Coral reef morphology, hydrodynamics, and sediment, nutrient, contaminant, and larval transport
The role of coral reefs and other coastal ecosystems in coastal hazard risk reduction
The interplay between geologic structure, climatic fluctuations, and coastal processes
High-resolution oceanographic instrumentation and coastal mapping techniques
The influence of physical processes on coral reef ecosystems
Many tropical coastal environments have been impacted by infrastructure development, nutrient and contaminant delivery, and natural and human-induced sedimentation. The high geomorphic and hydrodynamic complexity both within and between coral reefs, in conjunction with past technical restrictions, has limited our understanding of the nature of flow and the resulting flux of physical, chemical, and biologic material in these ecosystems. Understanding the physical controls on the timing and magnitude of flow and sediment, larvae, nutrient, and contaminant transport, along with their impact on seafloor geomorphology, stability, and sedimentation in these refugia are essential to assessing modern anthropogenic impacts (climate change, etc.) on these ecosystems and help guide how restoration can increase the resiliency of coral reef-lined coastal communities.
See: Coral Reef Project and The Value of U.S. Coral Reefs for Risk Reduction (links below)
The influence of climate change and sea-level rise on coral reef-lined coasts
Observations show that sea level is rising and recent projections indicate sea level will exceed 1.0 m, and may reach 2.0 m, above 2000 levels by the end of the 21st century. The amount of land and water available for human habitation, water and food sources, and ecosystems along coral reef-lined coasts is limited and vulnerable to wave-driven flooding during storms. Rising sea levels will further exacerbate the impacts of storms on coral reef-lined coasts by reducing wave breaking (and thus energy dissipation) over reefs and result in greater wave energy impacting the shoreline, causing increased flooding and changes to the coast such as erosion. Understanding the physical controls on the timing and magnitude of flooding, along with their impact on coastal geomorphology, are essential to assessing impacts on, and the future sustainability of, coastal infrastructure, agriculture, freshwater availability, and ecosystems.
See: Low-lying areas of tropical Pacific islands (links below)
Professional Experience
2002-present: Research Geologist and Oceanographer, USGS Coastal and Marine Hazards and Resources Program
2002-present: Research Associate, University of California at Santa Cruz (UCSC) Institute for Marine Sciences
Education and Certifications
2002-2004: Research Fellow, Partnership for Interdisciplinary Studies of Coastal Oceans Consortium
2000-2002: Post-doctoral Researcher, UCSC Institute for Marine Sciences
2000: Ph.D., UCSC, Earth Sciences Department
1996: B.Sc., University of Delaware, Geology Department
Science and Products
Rigorously valuing the role of coral reefs in coastal protection: An example from Maui, Hawaii, U.S.A.
Coastal circulation and water-column properties in the National Park of American Samoa, February–July 2015
Doubling of coastal flooding frequency within decades due to sea-level rise
Land-use change and managed aquifer recharge effects on the hydrogeochemistry of two contrasting atoll island aquifers, Roi-Namur Island, Republic of the Marshall Islands
Sources and dispersal of land-based runoff from small Hawaiian drainages to a coral reef: Insights from geochemical signatures
Sediment transport in the presence of large reef bottom roughness
Identification and classification of very low frequency waves on a coral reef flat
Observations of nearshore groundwater discharge: Kahekili Beach Park submarine springs, Maui, Hawaii
Seasonal sediment dynamics shape temperate bedrock reef communities
Changes to extreme wave climates of islands within the Western Tropical Pacific throughout the 21st century under RCP 4.5 and RCP 8.5, with implications for island vulnerability and sustainability
End of the chain? Rugosity and fine-scale bathymetry from existing underwater digital imagery using structure-from-motion (SfM) technology
Observations of wave transformation over a fringing coral reef and the importance of low-frequency waves and offshore water levels to runup, overwash, and coastal flooding
Non-USGS Publications**
**Disclaimer: The views expressed in Non-USGS publications are those of the author and do not represent the views of the USGS, Department of the Interior, or the U.S. Government.
Science and Products
- Science
Filter Total Items: 26
- Data
Filter Total Items: 42No Result Found
- Maps
- Multimedia
Filter Total Items: 26No results found.
- Publications
Filter Total Items: 193
Rigorously valuing the role of coral reefs in coastal protection: An example from Maui, Hawaii, U.S.A.
The degradation of coastal habitats, particularly coral reefs, raises risks by exposing 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 not considered in decision-making. Here we present a new methodology that combines economic, ecological, and enginAuthorsCurt D. Storlazzi, Borja G. Reguero, Erik Lowe, James B. Shope, Ann E. Gibbs, Mike Beck, Barry A. NickelCoastal circulation and water-column properties in the National Park of American Samoa, February–July 2015
There is little information on the oceanography in the National Park of American Samoa (NPSA). The transport pathways for potentially harmful constituents of land-derived runoff, as well as larvae and other planktonic organisms, are driven by nearshore circulation patterns. To evaluate the processes affecting coral reef ecosystem health, it is first necessary to understand the oceanographic procesAuthorsCurt D. Storlazzi, Olivia Cheriton, Kurt J. Rosenberger, Joshua B. Logan, Timothy B. ClarkDoubling of coastal flooding frequency within decades due to sea-level rise
Global climate change drives sea-level rise, increasing the frequency of coastal flooding. In most coastal regions, the amount of sea-level rise occurring over years to decades is significantly smaller than normal ocean-level fluctuations caused by tides, waves, and storm surge. However, even gradual sea-level rise can rapidly increase the frequency and severity of coastal flooding. So far, globalAuthorsSean Vitousek, Patrick L. Barnard, Charles H. Fletcher, Neil Frazer, Li H. Erikson, Curt D. StorlazziLand-use change and managed aquifer recharge effects on the hydrogeochemistry of two contrasting atoll island aquifers, Roi-Namur Island, Republic of the Marshall Islands
Freshwater resources on low-lying atoll islands are highly vulnerable to climate change and sea-level rise. In addition to rainwater catchment, groundwater in the freshwater lens is a critically important water resource on many atoll islands, especially during drought. Although many atolls have high annual rainfall rates, dense natural vegetation and high evapotranspiration rates can limit recharAuthorsMehrdad Hejazian, Jason J. Gurdak, Peter W. Swarzenski, Kingsley Odigie, Curt D. StorlazziSources and dispersal of land-based runoff from small Hawaiian drainages to a coral reef: Insights from geochemical signatures
Land-based sediment and contaminant runoff is a major threat to coral reefs, and runoff reduction efforts would benefit from knowledge of specific runoff sources. Geochemical signatures of small drainage basins were determined in the fine fraction of soil and sediment, then used in the nearshore region of a coral reef-fringed urban embayment on southeast Oahu, Hawaii, to describe sources and dispeAuthorsRenee K. Takesue, Curt D. StorlazziSediment transport in the presence of large reef bottom roughness
The presence of large bottom roughness, such as that formed by benthic organisms on coral reef flats, has important implications for the size, concentration, and transport of suspended sediment in coastal environments. A 3 week field study was conducted in approximately 1.5 m water depth on the reef flat at Ningaloo Reef, Western Australia, to quantify the cross-reef hydrodynamics and suspended seAuthorsAndrew Pomeroy, Ryan J. Lowe, Marco Ghisalberti, Curt D. Storlazzi, Graham Symonds, Dano RoelvinkIdentification and classification of very low frequency waves on a coral reef flat
Very low frequency (VLF, 0.001–0.005 Hz) waves are important drivers of flooding of low-lying coral reef-islands. In particular, VLF wave resonance is known to drive large wave runup and subsequent overwash. Using a 5 month data set of water levels and waves collected along a cross-reef transect on Roi-Namur Island in the Republic of the Marshall Islands, the observed VLF motions were categorizedAuthorsMatthijs Gawehn, Ap van Dongeran, Arnold van Rooijen, Curt D. Storlazzi, Olivia Cheriton, Ad ReniersObservations of nearshore groundwater discharge: Kahekili Beach Park submarine springs, Maui, Hawaii
Study regionThe study region encompasses the nearshore, coastal waters off west Maui, Hawaii. Here abundant groundwater—that carries with it a strong land-based fingerprint—discharges into the coastal waters and over a coral reef.Study focusCoastal groundwater discharge is a ubiquitous hydrologic feature that has been shown to impact nearshore ecosystems and material budgets. A unique combined geoAuthorsPeter W. Swarzenski, H. Dulai, K.D. Kroeger, C.G. Smith, N. Dimova, C. D. Storlazzi, N.G. Prouty, S. B. Gingerich, C. R. GlennSeasonal sediment dynamics shape temperate bedrock reef communities
Mobilized seafloor sediment can impact benthic reef communities through burial, scour, and turbidity. These processes are ubiquitous in coastal oceans and, through their influence on the survival, fitness, and interactions of species, can alter the structure and function of benthic communities. In northern Monterey Bay, California, USA, as much as 30% of the seafloor is buried or exposed seasonallAuthorsJared D. Figurski, Jan Freiwald, Steve I. Lonhart, Curt D. StorlazziChanges to extreme wave climates of islands within the Western Tropical Pacific throughout the 21st century under RCP 4.5 and RCP 8.5, with implications for island vulnerability and sustainability
Waves are the dominant influence on coastal morphology and ecosystem structure of tropical Pacific islands. Wave heights, periods, and directions for the 21st century were projected using near-surface wind fields from four atmosphere-ocean coupled global climate models (GCM) under representative concentration pathways (RCP) 4.5 and 8.5. GCM-derived wind fields forced the global WAVEWATCH-III waveAuthorsJames B. Shope, Curt D. Storlazzi, Li H. Erikson, Christie HegermillerEnd of the chain? Rugosity and fine-scale bathymetry from existing underwater digital imagery using structure-from-motion (SfM) technology
The rugosity or complexity of the seafloor has been shown to be an important ecological parameter for fish, algae, and corals. Historically, rugosity has been measured either using simple and subjective manual methods such as ‘chain-and-tape’ or complicated and expensive geophysical methods. Here, we demonstrate the application of structure-from-motion (SfM) photogrammetry to generate high-resolutAuthorsCurt D. Storlazzi, Peter Dartnell, Gerry Hatcher, Ann E. GibbsObservations of wave transformation over a fringing coral reef and the importance of low-frequency waves and offshore water levels to runup, overwash, and coastal flooding
Many low-lying tropical islands are susceptible to sea level rise and often subjected to overwash and flooding during large wave events. To quantify wave dynamics and wave-driven water levels on fringing coral reefs, a 5 month deployment of wave gauges and a current meter was conducted across two shore-normal transects on Roi-Namur Island in the Republic of the Marshall Islands. These observationsAuthorsOlivia Cheriton, Curt D. Storlazzi, Kurt J. RosenbergerNon-USGS Publications**
**Disclaimer: The views expressed in Non-USGS publications are those of the author and do not represent the views of the USGS, Department of the Interior, or the U.S. Government.
- News
Filter Total Items: 21