Hilary Stockdon, Ph.D. (Former Employee)
Science and Products
Filter Total Items: 34
Hydrologic-Enforcement of Lidar DEMs
Hydrologic connectivity of light detection and ranging (lidar)-derived elevation data is critical for coastal hydrologic modeling applications. However, unless hydrologically-enforced, raised structures (i.e. bridges, roads overlaying culverts) can block overland flow to coastal waters. Because highly detailed lidar-derived elevation surfaces include features such as bridge decks and road fill...
Shoreline Definition of Inland Water Bodies Not Hydrologically Connected to the Ocean
Most airborne topographic light detection and ranging (lidar) systems operate within the near-infrared spectrum. Laser pulses from these systems frequently are absorbed by water and do not generate reflected returns on water bodies in the resulting lidar point cloud. Thus, the absence of lidar returns over water is useful for identifying inland water bodies that are not connected by any path to...
Shoreline Definition in Emergent Wetland Environments
Coastal shoreline mapping is a particularly complex issue because of the dynamic nature of water levels at the land-water interface, the various tidal vertical datums in use, and the spatial scale of the shoreline delineation. In addition, the definition of a shoreline varies depending on whether the shoreline will be used for nautical charts and navigation, delineating the legal federal and state...
Storm Surge Hazards
The USGS Coastal National Elevation Database Applications Project organized a workshop in cooperation with the College of Staten Island-City University of New York to discuss storm surge modeling and get input from scientists across a broad community. The workshop, held on April 22-23, 2014 on the College of Staten Island campus, is part of a larger project intended to enhance topobathymetric...
Structure From Motion
Coastal topographic and bathymetric (topobathymetric) data with high spatial resolution (1-meter or better) and high vertical accuracy are needed to assess the vulnerability of Pacific Islands to climate change impacts, including sea-level rise. According to the Intergovernmental Panel on Climate Change reports, low-lying atolls in the Pacific Ocean are extremely vulnerable to king tide events...
Sea-level rise
The accuracy with which coastal topography has been mapped directly affects the reliability and usefulness of elevation-based sea-level rise vulnerability assessments. Recent research has shown that the qualities of the elevation data must be well understood to properly model potential impacts. The cumulative vertical uncertainty has contributions from elevation data error, water level data...
Restoration, Redevelopment, and Protection Projects
The Coastal National Elevation Database Applications Project supports scientific research and applications assessing restoration, redevelopment, and protection projects in the Hurricane Sandy impact areas along New Jersey and New York coastal beaches.
Coastal Multi-Temporal Elevation Database
The U.S. Geological Survey (USGS) National Geospatial Program's 3D Elevation Program (3DEP) aims to collect new light detection and ranging (lidar) data over the same areas on an 8-year return cycle. Between lidar surveys, there may be significant differences in bare- and non-bare earth heights due to both natural and human-induced geomorphic changes that occur. Therefore, research methods are...
Coastal Landscape Change and Vulnerability
Scientific research and applications assessing coastal landscape change and vulnerability are critical for applications such as shoreline mapping, hydrodynamic modeling, coastal vulnerability, and coastal geomorphology studies. However, very little ground truth data are available within the intertidal zone and adjacent beaches.
Satellite-Derived Bathymetry
Defining near-shore water depth (bathymetry) is problematic because ships cannot operate close to the shore while collecting acoustic bathymetric soundings. Alternatively, optical green laser lidar sensors have been used to collect bathymetric points, however, these types of lidar acquisitions are costly for the footprint collected and are subject to bathymetric inaccuracies in turbid water...
River bathymetry
This image is a topobathymetric elevation model of a part of the Mississippi River in New Orleans, Louisiana, and is an example of inland bathymetry in the northern Gulf of America. This regional topobathymetric elevation model includes airborne light detection and ranging (lidar) point clouds, hydrographic surveys, side-scan sonar surveys, and multibeam surveys obtained from USGS, NOAA, the State...
Levee Crest Elevation Profiles
This study explores the feasibility of using high-resolution digital elevation models (DEMs) constructed from airborne light detection and ranging (lidar) surveys to develop an automated procedure to extract levee longitudinal elevation profiles for both federal levees in Atchafalaya Basin and local levees in Lafourche Parish, south Louisiana. This approach can successfully accommodate abrupt...
Filter Total Items: 58
Dune management challenges on developed coasts Dune management challenges on developed coasts
From October 26-28, 2015, nearly 100 members of the coastal management and research communities met in Kitty Hawk, NC, USA to bridge the apparent gap between the coastal dune research of scientists and engineers and the needs of coastal management practitioners. The workshop aimed to identify the challenges involved in building and managing dunes on developed coasts, assess the extent to...
Authors
Nicole A. Elko, Kate Brodie, Hilary F. Stockdon, Karl F. Nordstrom, Chris Houser, Kim McKenna, Laura Moore, Julie D. Rosati, Peter Ruggiero, Roberta Thuman, Ian J. Walker
National assessment of nor’easter-induced coastal erosion hazards: mid- and northeast Atlantic coast National assessment of nor’easter-induced coastal erosion hazards: mid- and northeast Atlantic coast
Beaches serve as a natural buffer between the ocean and inland communities, ecosystems, and natural resources. However, these dynamic environments move and change in response to winds, waves, and currents. During extreme storms, changes to beaches can be great, and the results are sometimes catastrophic. Lives may be lost, communities destroyed, and millions of dollars spent on...
Authors
Justin J. Birchler, P. Soupy Dalyander, Hilary F. Stockdon, Kara S. Doran
How well can wave runup be predicted? comment on Laudier et al. (2011) and Stockdon et al. (2006) How well can wave runup be predicted? comment on Laudier et al. (2011) and Stockdon et al. (2006)
Laudier et al. (2011) suggested that there may be a systematic bias error in runup predictions using a model developed by Stockdon et al. (2006). Laudier et al. tested cases that sampled beach and wave conditions that differed from those used to develop the Stockdon et al. model. Based on our re-analysis, we found that in two of the three Laudier et al. cases observed overtopping was...
Authors
Nathaniel G. Plant, Hilary F. Stockdon
Enhancing evaluation of post-storm morphologic response using aerial orthoimagery from Hurricane Sandy Enhancing evaluation of post-storm morphologic response using aerial orthoimagery from Hurricane Sandy
Improved identification of morphological responses to storms is necessary for developing and maintaining predictive models of coastal change. Morphological responses to Hurricane Sandy were measured using lidar and orthophotos taken before and after the storm. Changes to dune features measured from lidar were compared to the occurrence of overwash deposits measured using orthophotos...
Authors
Jacquelyn Rose Smith, Joseph W. Long, Hilary F. Stockdon, Justin J. Birchler
National assessment of hurricane-induced coastal erosion hazards: Northeast Atlantic Coast National assessment of hurricane-induced coastal erosion hazards: Northeast Atlantic Coast
Beaches serve as a natural buffer between the ocean and inland communities, ecosystems, and natural resources. However, these dynamic environments move and change in response to winds, waves, and currents. During extreme storms, changes to beaches can be great, and the results are sometimes catastrophic. Lives may be lost, communities destroyed, and millions of dollars spent on...
Authors
Justin J. Birchler, Hilary F. Stockdon, Kara S. Doran, David M. Thompson
Probabilistic estimation of dune retreat on the Gold Coast, Australia Probabilistic estimation of dune retreat on the Gold Coast, Australia
Sand dunes are an important natural buffer between storm impacts and development backing the beach on the Gold Coast of Queensland, Australia. The ability to forecast dune erosion at a prediction horizon of days to a week would allow efficient and timely response to dune erosion in this highly populated area. Towards this goal, we modified an existing probabilistic dune erosion model for...
Authors
Margaret L. Palmsten, Kristen D. Splinter, Nathaniel G. Plant, Hilary F. Stockdon
Topographic lidar survey of the Alabama, Mississippi, and Southeast Louisiana Barrier Islands, from September 5 to October 11, 2012 Topographic lidar survey of the Alabama, Mississippi, and Southeast Louisiana Barrier Islands, from September 5 to October 11, 2012
This Data Series Report contains lidar elevation data collected from September 5 to October 11, 2012, for the barrier islands of Alabama, Mississippi and southeast Louisiana, including the coast near Port Fourchon. Most of the data were collected September 5–10, 2012, with a reflight conducted on October 11, 2012, to increase point density in some areas. Point cloud data—data points...
Authors
Kristy K. Guy, Kara S. Doran, Hilary F. Stockdon, Nathaniel G. Plant
Hurricane Sandy: observations and analysis of coastal change Hurricane Sandy: observations and analysis of coastal change
Hurricane Sandy, the largest Atlantic hurricane on record, made landfall on October 29, 2012, and impacted a long swath of the U.S. Atlantic coastline. The barrier islands were breached in a number of places and beach and dune erosion occurred along most of the Mid-Atlantic coast. As a part of the National Assessment of Coastal Change Hazards project, the U.S. Geological Survey collected...
Authors
Kristin L. Sopkin, Hilary F. Stockdon, Kara S. Doran, Nathaniel G. Plant, Karen L.M. Morgan, Kristy K. Guy, Kathryn E. L. Smith
Predictions of barrier island berm evolution in a time-varying storm climatology Predictions of barrier island berm evolution in a time-varying storm climatology
Low-lying barrier islands are ubiquitous features of the world's coastlines, and the processes responsible for their formation, maintenance, and destruction are related to the evolution of smaller, superimposed features including sand dunes, beach berms, and sandbars. The barrier island and its superimposed features interact with oceanographic forces (e.g., overwash) and exchange...
Authors
Nathaniel G. Plant, James Flocks, Hilary F. Stockdon, Joseph W. Long, Kristy K. Guy, David M. Thompson, Jamie M. Cormier, Christopher G. Smith, Jennifer L. Miselis, P. Soupy Dalyander
Evaluation of wave runup predictions from numerical and parametric models Evaluation of wave runup predictions from numerical and parametric models
Wave runup during storms is a primary driver of coastal evolution, including shoreline and dune erosion and barrier island overwash. Runup and its components, setup and swash, can be predicted from a parameterized model that was developed by comparing runup observations to offshore wave height, wave period, and local beach slope. Because observations during extreme storms are often...
Authors
Hilary F. Stockdon, David M. Thompson, Nathaniel G. Plant, Joseph W. Long
Assessing hazards along our Nation's coasts Assessing hazards along our Nation's coasts
Coastal areas are essential to the economic, cultural, and environmental health of the Nation, yet by nature coastal areas are constantly changing due to a variety of events and processes. Extreme storms can cause dramatic changes to our shorelines in a matter of hours, while sea-level rise can profoundly alter coastal environments over decades. These changes can have a devastating...
Authors
Hilary F. Stockdon, Cheryl J. Hapke, E. Robert Thieler, Nathaniel G. Plant
National assessment of hurricane-induced coastal erosion hazards: Southeast Atlantic Coast National assessment of hurricane-induced coastal erosion hazards: Southeast Atlantic Coast
Beaches serve as a natural barrier between the ocean and inland communities, ecosystems, and natural resources. However, these dynamic environments move and change in response to winds, waves, and currents. During extreme storms, changes to beaches can be large, and the results are sometimes catastrophic. Lives may be lost, communities destroyed, and millions of dollars spent on...
Authors
Hilary F. Stockdon, Kara S. Doran, David M. Thompson, Kristin L. Sopkin, Nathaniel G. Plant
Science and Products
Filter Total Items: 34
Hydrologic-Enforcement of Lidar DEMs
Hydrologic connectivity of light detection and ranging (lidar)-derived elevation data is critical for coastal hydrologic modeling applications. However, unless hydrologically-enforced, raised structures (i.e. bridges, roads overlaying culverts) can block overland flow to coastal waters. Because highly detailed lidar-derived elevation surfaces include features such as bridge decks and road fill...
Shoreline Definition of Inland Water Bodies Not Hydrologically Connected to the Ocean
Most airborne topographic light detection and ranging (lidar) systems operate within the near-infrared spectrum. Laser pulses from these systems frequently are absorbed by water and do not generate reflected returns on water bodies in the resulting lidar point cloud. Thus, the absence of lidar returns over water is useful for identifying inland water bodies that are not connected by any path to...
Shoreline Definition in Emergent Wetland Environments
Coastal shoreline mapping is a particularly complex issue because of the dynamic nature of water levels at the land-water interface, the various tidal vertical datums in use, and the spatial scale of the shoreline delineation. In addition, the definition of a shoreline varies depending on whether the shoreline will be used for nautical charts and navigation, delineating the legal federal and state...
Storm Surge Hazards
The USGS Coastal National Elevation Database Applications Project organized a workshop in cooperation with the College of Staten Island-City University of New York to discuss storm surge modeling and get input from scientists across a broad community. The workshop, held on April 22-23, 2014 on the College of Staten Island campus, is part of a larger project intended to enhance topobathymetric...
Structure From Motion
Coastal topographic and bathymetric (topobathymetric) data with high spatial resolution (1-meter or better) and high vertical accuracy are needed to assess the vulnerability of Pacific Islands to climate change impacts, including sea-level rise. According to the Intergovernmental Panel on Climate Change reports, low-lying atolls in the Pacific Ocean are extremely vulnerable to king tide events...
Sea-level rise
The accuracy with which coastal topography has been mapped directly affects the reliability and usefulness of elevation-based sea-level rise vulnerability assessments. Recent research has shown that the qualities of the elevation data must be well understood to properly model potential impacts. The cumulative vertical uncertainty has contributions from elevation data error, water level data...
Restoration, Redevelopment, and Protection Projects
The Coastal National Elevation Database Applications Project supports scientific research and applications assessing restoration, redevelopment, and protection projects in the Hurricane Sandy impact areas along New Jersey and New York coastal beaches.
Coastal Multi-Temporal Elevation Database
The U.S. Geological Survey (USGS) National Geospatial Program's 3D Elevation Program (3DEP) aims to collect new light detection and ranging (lidar) data over the same areas on an 8-year return cycle. Between lidar surveys, there may be significant differences in bare- and non-bare earth heights due to both natural and human-induced geomorphic changes that occur. Therefore, research methods are...
Coastal Landscape Change and Vulnerability
Scientific research and applications assessing coastal landscape change and vulnerability are critical for applications such as shoreline mapping, hydrodynamic modeling, coastal vulnerability, and coastal geomorphology studies. However, very little ground truth data are available within the intertidal zone and adjacent beaches.
Satellite-Derived Bathymetry
Defining near-shore water depth (bathymetry) is problematic because ships cannot operate close to the shore while collecting acoustic bathymetric soundings. Alternatively, optical green laser lidar sensors have been used to collect bathymetric points, however, these types of lidar acquisitions are costly for the footprint collected and are subject to bathymetric inaccuracies in turbid water...
River bathymetry
This image is a topobathymetric elevation model of a part of the Mississippi River in New Orleans, Louisiana, and is an example of inland bathymetry in the northern Gulf of America. This regional topobathymetric elevation model includes airborne light detection and ranging (lidar) point clouds, hydrographic surveys, side-scan sonar surveys, and multibeam surveys obtained from USGS, NOAA, the State...
Levee Crest Elevation Profiles
This study explores the feasibility of using high-resolution digital elevation models (DEMs) constructed from airborne light detection and ranging (lidar) surveys to develop an automated procedure to extract levee longitudinal elevation profiles for both federal levees in Atchafalaya Basin and local levees in Lafourche Parish, south Louisiana. This approach can successfully accommodate abrupt...
Filter Total Items: 58
Dune management challenges on developed coasts Dune management challenges on developed coasts
From October 26-28, 2015, nearly 100 members of the coastal management and research communities met in Kitty Hawk, NC, USA to bridge the apparent gap between the coastal dune research of scientists and engineers and the needs of coastal management practitioners. The workshop aimed to identify the challenges involved in building and managing dunes on developed coasts, assess the extent to...
Authors
Nicole A. Elko, Kate Brodie, Hilary F. Stockdon, Karl F. Nordstrom, Chris Houser, Kim McKenna, Laura Moore, Julie D. Rosati, Peter Ruggiero, Roberta Thuman, Ian J. Walker
National assessment of nor’easter-induced coastal erosion hazards: mid- and northeast Atlantic coast National assessment of nor’easter-induced coastal erosion hazards: mid- and northeast Atlantic coast
Beaches serve as a natural buffer between the ocean and inland communities, ecosystems, and natural resources. However, these dynamic environments move and change in response to winds, waves, and currents. During extreme storms, changes to beaches can be great, and the results are sometimes catastrophic. Lives may be lost, communities destroyed, and millions of dollars spent on...
Authors
Justin J. Birchler, P. Soupy Dalyander, Hilary F. Stockdon, Kara S. Doran
How well can wave runup be predicted? comment on Laudier et al. (2011) and Stockdon et al. (2006) How well can wave runup be predicted? comment on Laudier et al. (2011) and Stockdon et al. (2006)
Laudier et al. (2011) suggested that there may be a systematic bias error in runup predictions using a model developed by Stockdon et al. (2006). Laudier et al. tested cases that sampled beach and wave conditions that differed from those used to develop the Stockdon et al. model. Based on our re-analysis, we found that in two of the three Laudier et al. cases observed overtopping was...
Authors
Nathaniel G. Plant, Hilary F. Stockdon
Enhancing evaluation of post-storm morphologic response using aerial orthoimagery from Hurricane Sandy Enhancing evaluation of post-storm morphologic response using aerial orthoimagery from Hurricane Sandy
Improved identification of morphological responses to storms is necessary for developing and maintaining predictive models of coastal change. Morphological responses to Hurricane Sandy were measured using lidar and orthophotos taken before and after the storm. Changes to dune features measured from lidar were compared to the occurrence of overwash deposits measured using orthophotos...
Authors
Jacquelyn Rose Smith, Joseph W. Long, Hilary F. Stockdon, Justin J. Birchler
National assessment of hurricane-induced coastal erosion hazards: Northeast Atlantic Coast National assessment of hurricane-induced coastal erosion hazards: Northeast Atlantic Coast
Beaches serve as a natural buffer between the ocean and inland communities, ecosystems, and natural resources. However, these dynamic environments move and change in response to winds, waves, and currents. During extreme storms, changes to beaches can be great, and the results are sometimes catastrophic. Lives may be lost, communities destroyed, and millions of dollars spent on...
Authors
Justin J. Birchler, Hilary F. Stockdon, Kara S. Doran, David M. Thompson
Probabilistic estimation of dune retreat on the Gold Coast, Australia Probabilistic estimation of dune retreat on the Gold Coast, Australia
Sand dunes are an important natural buffer between storm impacts and development backing the beach on the Gold Coast of Queensland, Australia. The ability to forecast dune erosion at a prediction horizon of days to a week would allow efficient and timely response to dune erosion in this highly populated area. Towards this goal, we modified an existing probabilistic dune erosion model for...
Authors
Margaret L. Palmsten, Kristen D. Splinter, Nathaniel G. Plant, Hilary F. Stockdon
Topographic lidar survey of the Alabama, Mississippi, and Southeast Louisiana Barrier Islands, from September 5 to October 11, 2012 Topographic lidar survey of the Alabama, Mississippi, and Southeast Louisiana Barrier Islands, from September 5 to October 11, 2012
This Data Series Report contains lidar elevation data collected from September 5 to October 11, 2012, for the barrier islands of Alabama, Mississippi and southeast Louisiana, including the coast near Port Fourchon. Most of the data were collected September 5–10, 2012, with a reflight conducted on October 11, 2012, to increase point density in some areas. Point cloud data—data points...
Authors
Kristy K. Guy, Kara S. Doran, Hilary F. Stockdon, Nathaniel G. Plant
Hurricane Sandy: observations and analysis of coastal change Hurricane Sandy: observations and analysis of coastal change
Hurricane Sandy, the largest Atlantic hurricane on record, made landfall on October 29, 2012, and impacted a long swath of the U.S. Atlantic coastline. The barrier islands were breached in a number of places and beach and dune erosion occurred along most of the Mid-Atlantic coast. As a part of the National Assessment of Coastal Change Hazards project, the U.S. Geological Survey collected...
Authors
Kristin L. Sopkin, Hilary F. Stockdon, Kara S. Doran, Nathaniel G. Plant, Karen L.M. Morgan, Kristy K. Guy, Kathryn E. L. Smith
Predictions of barrier island berm evolution in a time-varying storm climatology Predictions of barrier island berm evolution in a time-varying storm climatology
Low-lying barrier islands are ubiquitous features of the world's coastlines, and the processes responsible for their formation, maintenance, and destruction are related to the evolution of smaller, superimposed features including sand dunes, beach berms, and sandbars. The barrier island and its superimposed features interact with oceanographic forces (e.g., overwash) and exchange...
Authors
Nathaniel G. Plant, James Flocks, Hilary F. Stockdon, Joseph W. Long, Kristy K. Guy, David M. Thompson, Jamie M. Cormier, Christopher G. Smith, Jennifer L. Miselis, P. Soupy Dalyander
Evaluation of wave runup predictions from numerical and parametric models Evaluation of wave runup predictions from numerical and parametric models
Wave runup during storms is a primary driver of coastal evolution, including shoreline and dune erosion and barrier island overwash. Runup and its components, setup and swash, can be predicted from a parameterized model that was developed by comparing runup observations to offshore wave height, wave period, and local beach slope. Because observations during extreme storms are often...
Authors
Hilary F. Stockdon, David M. Thompson, Nathaniel G. Plant, Joseph W. Long
Assessing hazards along our Nation's coasts Assessing hazards along our Nation's coasts
Coastal areas are essential to the economic, cultural, and environmental health of the Nation, yet by nature coastal areas are constantly changing due to a variety of events and processes. Extreme storms can cause dramatic changes to our shorelines in a matter of hours, while sea-level rise can profoundly alter coastal environments over decades. These changes can have a devastating...
Authors
Hilary F. Stockdon, Cheryl J. Hapke, E. Robert Thieler, Nathaniel G. Plant
National assessment of hurricane-induced coastal erosion hazards: Southeast Atlantic Coast National assessment of hurricane-induced coastal erosion hazards: Southeast Atlantic Coast
Beaches serve as a natural barrier between the ocean and inland communities, ecosystems, and natural resources. However, these dynamic environments move and change in response to winds, waves, and currents. During extreme storms, changes to beaches can be large, and the results are sometimes catastrophic. Lives may be lost, communities destroyed, and millions of dollars spent on...
Authors
Hilary F. Stockdon, Kara S. Doran, David M. Thompson, Kristin L. Sopkin, Nathaniel G. Plant