Joseph Long (Former Employee)
Science and Products
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Morphodynamic data assimilation used to understand changing coasts
Morphodynamic data assimilation blends observations with model predictions and comes in many forms, including linear regression, Kalman filter, brute-force parameter estimation, variational assimilation, and Bayesian analysis. Importantly, data assimilation can be used to identify sources of prediction errors that lead to improved fundamental understanding. Overall, models incorporating data assim
Authors
Nathaniel G. Plant, Joseph W. Long
Nearshore dynamics of artificial sand and oil agglomerates
Weathered oil can mix with sediment to form heavier-than-water sand and oil agglomerates (SOAs) that can cause beach re-oiling for years after a spill. Few studies have focused on the physical dynamics of SOAs. In this study, artificial SOAs (aSOAs) were created and deployed in the nearshore, and shear stress-based mobility formulations were assessed to predict SOA response. Prediction sensitivity
Authors
P. Soupy Dalyander, Nathaniel G. Plant, Joseph W. Long, Molly R. McLaughlin
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. Thresholds on
Authors
Jacquelyn Rose Smith, Joseph W. Long, Hilary F. Stockdon, Justin J. Birchler
Effects of proposed sediment borrow pits on nearshore wave climate and longshore sediment transport rate along Breton Island, Louisiana
As part of a plan to preserve bird habitat on Breton Island, the southernmost extent of the Chandeleur Islands and part of the Breton National Wildlife Refuge in Louisiana, the U.S. Fish and Wildlife Service plans to increase island elevation with sand supplied from offshore resources. Proposed sand extraction sites include areas offshore where the seafloor morphology suggests suitable quantities
Authors
Patricia (Soupy) Dalyander, Rangley C. Mickey, Joseph W. Long, James G. Flocks
Field observations of artificial sand and oil agglomerates
Oil that comes into the surf zone following spills, such as occurred during the 2010 Deepwater Horizon (DWH) blowout, can mix with local sediment to form heavier-than-water sand and oil agglomerates (SOAs), at times in the form of mats a few centimeters thick and tens of meters long. Smaller agglomerates that form in situ or pieces that break off of larger mats, sometimes referred to as surface re
Authors
Patricia (Soupy) Dalyander, Joseph W. Long, Nathaniel G. Plant, Molly R. McLaughlin, Rangley C. Mickey
A method for determining average beach slope and beach slope variability for U.S. sandy coastlines
The U.S. Geological Survey (USGS) National Assessment of Hurricane-Induced Coastal Erosion Hazards compares measurements of beach morphology with storm-induced total water levels to produce forecasts of coastal change for storms impacting the Gulf of Mexico and Atlantic coastlines of the United States. The wave-induced water level component (wave setup and swash) is estimated by using modeled offs
Authors
Kara S. Doran, Joseph W. Long, Jacquelyn R. Overbeck
Inundation of a barrier island (Chandeleur Islands, Louisiana, USA) during a hurricane: Observed water-level gradients and modeled seaward sand transport
Large geomorphic changes to barrier islands may occur during inundation, when storm surge exceeds island elevation. Inundation occurs episodically and under energetic conditions that make quantitative observations difficult. We measured water levels on both sides of a barrier island in the northern Chandeleur Islands during inundation by Hurricane Isaac. Wind patterns caused the water levels to sl
Authors
Christopher R. Sherwood, Joseph W. Long, Patrick Dickhudt, P. Soupy Dalyander, David M. Thompson, Nathaniel G. Plant
A probabilistic method for constructing wave time-series at inshore locations using model scenarios
Continuous time-series of wave characteristics (height, period, and direction) are constructed using a base set of model scenarios and simple probabilistic methods. This approach utilizes an archive of computationally intensive, highly spatially resolved numerical wave model output to develop time-series of historical or future wave conditions without performing additional, continuous numerical si
Authors
Joseph W. Long, Nathaniel G. Plant, P. Soupy Dalyander, David M. Thompson
Scaling coastal dune elevation changes across storm-impact regimes
Extreme storms drive change in coastal areas, including destruction of dune systems that protect coastal populations. Data from four extreme storms impacting four geomorphically diverse barrier islands are used to quantify dune elevation change. This change is compared to storm characteristics to identify variability in dune response, improve understanding of morphological interactions, and provid
Authors
Joseph W. Long, Anouk T. M. de Bakker, Nathaniel G. Plant
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 sediment with eac
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
Assessing mobility and redistribution patterns of sand and oil agglomerates in the surf zone
Heavier-than-water sand and oil agglomerates that formed in the surf zone following the Deepwater Horizon oil spill continued to cause beach re-oiling 3 years after initial stranding. To understand this phenomena and inform operational response now and for future spills, a numerical method to assess the mobility and alongshore movement of these “surface residual balls” (SRBs) was developed and app
Authors
P. Soupy Dalyander, Joesph W. Long, Nathaniel G. Plant, David M. Thompson
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 unavailable, a
Authors
Hilary F. Stockdon, David M. Thompson, Nathaniel G. Plant, Joseph W. Long
Non-USGS Publications**
Long, J. W., and H. T. Özkan-Haller, 2009, Low-frequency characteristics of wave group–forced vortices, J. Geophys. Res., 114, C08004, doi:10.1029/2008JC004894.
Scott, C.P., Cox, D.T., Maddux, T.B., and Long, J.W., 2005, Large-scale laboratory observations of turbulence on a fixed barred beach: Measurement Science and Technology, v. 16, p. 1903, doi: 10.1088/0957-0233/16/10/004.
Long, J. W., and H. T. Özkan-Haller, 2005, Offshore controls on nearshore rip currents, J. Geophys. Res., 110, C12007, doi:10.1029/2005JC003018.
**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
Filter Total Items: 13
Filter Total Items: 17
No Result Found
Filter Total Items: 41
Morphodynamic data assimilation used to understand changing coasts
Morphodynamic data assimilation blends observations with model predictions and comes in many forms, including linear regression, Kalman filter, brute-force parameter estimation, variational assimilation, and Bayesian analysis. Importantly, data assimilation can be used to identify sources of prediction errors that lead to improved fundamental understanding. Overall, models incorporating data assim
Authors
Nathaniel G. Plant, Joseph W. Long
Nearshore dynamics of artificial sand and oil agglomerates
Weathered oil can mix with sediment to form heavier-than-water sand and oil agglomerates (SOAs) that can cause beach re-oiling for years after a spill. Few studies have focused on the physical dynamics of SOAs. In this study, artificial SOAs (aSOAs) were created and deployed in the nearshore, and shear stress-based mobility formulations were assessed to predict SOA response. Prediction sensitivity
Authors
P. Soupy Dalyander, Nathaniel G. Plant, Joseph W. Long, Molly R. McLaughlin
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. Thresholds on
Authors
Jacquelyn Rose Smith, Joseph W. Long, Hilary F. Stockdon, Justin J. Birchler
Effects of proposed sediment borrow pits on nearshore wave climate and longshore sediment transport rate along Breton Island, Louisiana
As part of a plan to preserve bird habitat on Breton Island, the southernmost extent of the Chandeleur Islands and part of the Breton National Wildlife Refuge in Louisiana, the U.S. Fish and Wildlife Service plans to increase island elevation with sand supplied from offshore resources. Proposed sand extraction sites include areas offshore where the seafloor morphology suggests suitable quantities
Authors
Patricia (Soupy) Dalyander, Rangley C. Mickey, Joseph W. Long, James G. Flocks
Field observations of artificial sand and oil agglomerates
Oil that comes into the surf zone following spills, such as occurred during the 2010 Deepwater Horizon (DWH) blowout, can mix with local sediment to form heavier-than-water sand and oil agglomerates (SOAs), at times in the form of mats a few centimeters thick and tens of meters long. Smaller agglomerates that form in situ or pieces that break off of larger mats, sometimes referred to as surface re
Authors
Patricia (Soupy) Dalyander, Joseph W. Long, Nathaniel G. Plant, Molly R. McLaughlin, Rangley C. Mickey
A method for determining average beach slope and beach slope variability for U.S. sandy coastlines
The U.S. Geological Survey (USGS) National Assessment of Hurricane-Induced Coastal Erosion Hazards compares measurements of beach morphology with storm-induced total water levels to produce forecasts of coastal change for storms impacting the Gulf of Mexico and Atlantic coastlines of the United States. The wave-induced water level component (wave setup and swash) is estimated by using modeled offs
Authors
Kara S. Doran, Joseph W. Long, Jacquelyn R. Overbeck
Inundation of a barrier island (Chandeleur Islands, Louisiana, USA) during a hurricane: Observed water-level gradients and modeled seaward sand transport
Large geomorphic changes to barrier islands may occur during inundation, when storm surge exceeds island elevation. Inundation occurs episodically and under energetic conditions that make quantitative observations difficult. We measured water levels on both sides of a barrier island in the northern Chandeleur Islands during inundation by Hurricane Isaac. Wind patterns caused the water levels to sl
Authors
Christopher R. Sherwood, Joseph W. Long, Patrick Dickhudt, P. Soupy Dalyander, David M. Thompson, Nathaniel G. Plant
A probabilistic method for constructing wave time-series at inshore locations using model scenarios
Continuous time-series of wave characteristics (height, period, and direction) are constructed using a base set of model scenarios and simple probabilistic methods. This approach utilizes an archive of computationally intensive, highly spatially resolved numerical wave model output to develop time-series of historical or future wave conditions without performing additional, continuous numerical si
Authors
Joseph W. Long, Nathaniel G. Plant, P. Soupy Dalyander, David M. Thompson
Scaling coastal dune elevation changes across storm-impact regimes
Extreme storms drive change in coastal areas, including destruction of dune systems that protect coastal populations. Data from four extreme storms impacting four geomorphically diverse barrier islands are used to quantify dune elevation change. This change is compared to storm characteristics to identify variability in dune response, improve understanding of morphological interactions, and provid
Authors
Joseph W. Long, Anouk T. M. de Bakker, Nathaniel G. Plant
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 sediment with eac
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
Assessing mobility and redistribution patterns of sand and oil agglomerates in the surf zone
Heavier-than-water sand and oil agglomerates that formed in the surf zone following the Deepwater Horizon oil spill continued to cause beach re-oiling 3 years after initial stranding. To understand this phenomena and inform operational response now and for future spills, a numerical method to assess the mobility and alongshore movement of these “surface residual balls” (SRBs) was developed and app
Authors
P. Soupy Dalyander, Joesph W. Long, Nathaniel G. Plant, David M. Thompson
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 unavailable, a
Authors
Hilary F. Stockdon, David M. Thompson, Nathaniel G. Plant, Joseph W. Long
Non-USGS Publications**
Long, J. W., and H. T. Özkan-Haller, 2009, Low-frequency characteristics of wave group–forced vortices, J. Geophys. Res., 114, C08004, doi:10.1029/2008JC004894.
Scott, C.P., Cox, D.T., Maddux, T.B., and Long, J.W., 2005, Large-scale laboratory observations of turbulence on a fixed barred beach: Measurement Science and Technology, v. 16, p. 1903, doi: 10.1088/0957-0233/16/10/004.
Long, J. W., and H. T. Özkan-Haller, 2005, Offshore controls on nearshore rip currents, J. Geophys. Res., 110, C12007, doi:10.1029/2005JC003018.
**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.