Evaluation of Techniques for Numerical Calculation of Storm Surges

Prepared with the Support of Dames and Moore, Inc. Cranford, New Jersey, and Sea Grant Office National Oceanic and Atmospheric Administration Department of Commerce Washington, D.C.

Bibliographic Details
Main Authors: Pagenkopf, James R., Pearce, Bryan R.
Published: Cambridge Massachusetts Institute of Technology. Ralph M. Parsons Laboratory for Water Resources and Hydrodynamics 2022
Online Access:https://hdl.handle.net/1721.1/142972
_version_ 1811081579102994432
author Pagenkopf, James R.
Pearce, Bryan R.
author_facet Pagenkopf, James R.
Pearce, Bryan R.
author_sort Pagenkopf, James R.
collection MIT
description Prepared with the Support of Dames and Moore, Inc. Cranford, New Jersey, and Sea Grant Office National Oceanic and Atmospheric Administration Department of Commerce Washington, D.C.
first_indexed 2024-09-23T11:48:56Z
id mit-1721.1/142972
institution Massachusetts Institute of Technology
last_indexed 2024-09-23T11:48:56Z
publishDate 2022
publisher Cambridge Massachusetts Institute of Technology. Ralph M. Parsons Laboratory for Water Resources and Hydrodynamics
record_format dspace
spelling mit-1721.1/1429722022-06-14T03:26:56Z Evaluation of Techniques for Numerical Calculation of Storm Surges Pagenkopf, James R. Pearce, Bryan R. Prepared with the Support of Dames and Moore, Inc. Cranford, New Jersey, and Sea Grant Office National Oceanic and Atmospheric Administration Department of Commerce Washington, D.C. Two numerical models are employed to describe the water motion in a coastal region associated with the passage of a hurricane or severe storm. The first is two-dimensional, employs the vertically integrated or "tidal" equations of motion and utilizes a finite-difference scheme. The second is also two-dimensional, also employs the vertically integrated conservation of mass and momentum equations and utilizes a finite element solution scheme. Model results are compared and evaluated through various parametric studies such as computer time and accuracy. Boundary condition sensitivity is investigated. In application, storm surge heights are computed for various hurricane systems at the Atlantic Generating Station site using both models. Results are also compared to bathystrophic calculations. It is concluded that under certain instances of storm size and speed the bathystrophic approach may be non-conservative due to the ignoring of inertial terms and two-dimensional effects. The resulting storm surge calculations indicate no significant advantage in using the finite element method over the finite difference method or vice versa, although the same may not be true for other hydrodynamic applications. Other results include maximum surge heights as a function of forward velocity and angle of incidence, as well as historical verification studies for the hurricane of September 14, 1974. 2022-06-13T13:06:24Z 2022-06-13T13:06:24Z 1975-02 199 https://hdl.handle.net/1721.1/142972 2021310 18364 R (Massachusetts Institute of Technology. Department of Civil Engineering) ; 75-12. Report (Ralph M. Parsons Laboratory for Water Resources and Hydrodynamics) ; 199. application/pdf Cambridge Massachusetts Institute of Technology. Ralph M. Parsons Laboratory for Water Resources and Hydrodynamics
spellingShingle Pagenkopf, James R.
Pearce, Bryan R.
Evaluation of Techniques for Numerical Calculation of Storm Surges
title Evaluation of Techniques for Numerical Calculation of Storm Surges
title_full Evaluation of Techniques for Numerical Calculation of Storm Surges
title_fullStr Evaluation of Techniques for Numerical Calculation of Storm Surges
title_full_unstemmed Evaluation of Techniques for Numerical Calculation of Storm Surges
title_short Evaluation of Techniques for Numerical Calculation of Storm Surges
title_sort evaluation of techniques for numerical calculation of storm surges
url https://hdl.handle.net/1721.1/142972
work_keys_str_mv AT pagenkopfjamesr evaluationoftechniquesfornumericalcalculationofstormsurges
AT pearcebryanr evaluationoftechniquesfornumericalcalculationofstormsurges