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...

Full description

Bibliographic Details
Main Authors: B. A. Weymer, P. Wernette, M. E. Everett, C. Houser
Format: Article
Language:English
Published: Copernicus Publications 2018-06-01
Series:Earth Surface Dynamics
Online Access:https://www.earth-surf-dynam.net/6/431/2018/esurf-6-431-2018.pdf
id doaj-c3ac4684201048df8513260268940b79
record_format Article
spelling 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
work_keys_str_mv AT baweymer statisticalmodelingofthelongrangedependentstructureofbarrierislandframeworkgeologyandsurfacegeomorphology
AT baweymer statisticalmodelingofthelongrangedependentstructureofbarrierislandframeworkgeologyandsurfacegeomorphology
AT pwernette statisticalmodelingofthelongrangedependentstructureofbarrierislandframeworkgeologyandsurfacegeomorphology
AT meeverett statisticalmodelingofthelongrangedependentstructureofbarrierislandframeworkgeologyandsurfacegeomorphology
AT chouser statisticalmodelingofthelongrangedependentstructureofbarrierislandframeworkgeologyandsurfacegeomorphology
_version_ 1724765674860969984