Statistical modeling of the long-range-dependent structure of barrier island framework geology and surface geomorphology
Shorelines exhibit long-range dependence (LRD) and have been shown in some environments to be described in the wave number domain by a power-law characteristic of scale independence. Recent evidence suggests that the geomorphology of barrier islands can, however, exhibit scale dependence as a re...
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doaj-c3ac4684201048df8513260268940b792020-11-25T02:44:50ZengCopernicus PublicationsEarth Surface Dynamics2196-63112196-632X2018-06-01643145010.5194/esurf-6-431-2018Statistical modeling of the long-range-dependent structure of barrier island framework geology and surface geomorphologyB. A. Weymer0B. A. Weymer1P. Wernette2M. E. Everett3C. Houser4Department of Geology and Geophysics, Texas A&M University, College Station, Texas 77843, USAnow at: GEOMAR – Helmholtz Center for Ocean Research Kiel, Wischhofstraße 1–3, 24148 Kiel, GermanyDepartment of Geography, Texas A&M University, College Station, Texas 77843, USADepartment of Geology and Geophysics, Texas A&M University, College Station, Texas 77843, USADepartment of Earth and Environmental Sciences, University of Windsor, Windsor, Ontario N9B 3P4, CanadaShorelines exhibit long-range dependence (LRD) and have been shown in some environments to be described in the wave number domain by a power-law characteristic of scale independence. Recent evidence suggests that the geomorphology of barrier islands can, however, exhibit scale dependence as a result of systematic variations in the underlying framework geology. The LRD of framework geology, which influences island geomorphology and its response to storms and sea level rise, has not been previously examined. Electromagnetic induction (EMI) surveys conducted along Padre Island National Seashore (PAIS), Texas, United States, reveal that the EMI apparent conductivity (<i>σ</i><sub>a</sub>) signal and, by inference, the framework geology exhibits LRD at scales of up to 10<sup>1</sup> to 10<sup>2</sup> km. Our study demonstrates the utility of describing EMI <i>σ</i><sub>a</sub> and lidar spatial series by a fractional autoregressive integrated moving average (ARIMA) process that specifically models LRD. This method offers a robust and compact way of quantifying the geological variations along a barrier island shoreline using three statistical parameters (<i>p</i>, <i>d</i>, <i>q</i>). We discuss how ARIMA models that use a single parameter <i>d</i> provide a quantitative measure for determining free and forced barrier island evolutionary behavior across different scales. Statistical analyses at regional, intermediate, and local scales suggest that the geologic framework within an area of paleo-channels exhibits a first-order control on dune height. The exchange of sediment amongst nearshore, beach, and dune in areas outside this region are scale independent, implying that barrier islands like PAIS exhibit a combination of free and forced behaviors that affect the response of the island to sea level rise.https://www.earth-surf-dynam.net/6/431/2018/esurf-6-431-2018.pdf |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
B. A. Weymer B. A. Weymer P. Wernette M. E. Everett C. Houser |
spellingShingle |
B. A. Weymer B. A. Weymer P. Wernette M. E. Everett C. Houser Statistical modeling of the long-range-dependent structure of barrier island framework geology and surface geomorphology Earth Surface Dynamics |
author_facet |
B. A. Weymer B. A. Weymer P. Wernette M. E. Everett C. Houser |
author_sort |
B. A. Weymer |
title |
Statistical modeling of the long-range-dependent structure of barrier island framework geology and surface geomorphology |
title_short |
Statistical modeling of the long-range-dependent structure of barrier island framework geology and surface geomorphology |
title_full |
Statistical modeling of the long-range-dependent structure of barrier island framework geology and surface geomorphology |
title_fullStr |
Statistical modeling of the long-range-dependent structure of barrier island framework geology and surface geomorphology |
title_full_unstemmed |
Statistical modeling of the long-range-dependent structure of barrier island framework geology and surface geomorphology |
title_sort |
statistical modeling of the long-range-dependent structure of barrier island framework geology and surface geomorphology |
publisher |
Copernicus Publications |
series |
Earth Surface Dynamics |
issn |
2196-6311 2196-632X |
publishDate |
2018-06-01 |
description |
Shorelines exhibit long-range dependence (LRD) and have been shown
in some environments to be described in the wave number domain by a power-law
characteristic of scale independence. Recent evidence suggests that the
geomorphology of barrier islands can, however, exhibit scale dependence as a
result of systematic variations in the underlying framework geology. The LRD
of framework geology, which influences island geomorphology and its response
to storms and sea level rise, has not been previously examined.
Electromagnetic induction (EMI) surveys conducted along Padre Island National
Seashore (PAIS), Texas, United States, reveal that the EMI apparent conductivity
(<i>σ</i><sub>a</sub>) signal and, by inference, the framework geology
exhibits LRD at scales of up to 10<sup>1</sup> to 10<sup>2</sup> km. Our study demonstrates
the utility of describing EMI <i>σ</i><sub>a</sub> and lidar spatial series by
a fractional autoregressive integrated moving average (ARIMA) process that
specifically models LRD. This method offers a robust and compact way of
quantifying the geological variations along a barrier island shoreline using
three statistical parameters (<i>p</i>, <i>d</i>, <i>q</i>). We discuss how ARIMA models
that use a single parameter <i>d</i> provide a quantitative measure for
determining free and forced barrier island evolutionary behavior across
different scales. Statistical analyses at regional, intermediate, and local
scales suggest that the geologic framework within an area of paleo-channels
exhibits a first-order control on dune height. The exchange of sediment
amongst nearshore, beach, and dune in areas outside this region are
scale independent, implying that barrier islands like PAIS exhibit a
combination of free and forced behaviors that affect the response of the
island to sea level rise. |
url |
https://www.earth-surf-dynam.net/6/431/2018/esurf-6-431-2018.pdf |
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