2008
DOI: 10.2112/06-0820.1
|View full text |Cite
|
Sign up to set email alerts
|

Hurricane Degradation—Barrier Development Cycles, Northeastern Gulf of Mexico: Landform Evolution and Island Chain History

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
2
1
1

Citation Types

2
72
0

Year Published

2009
2009
2017
2017

Publication Types

Select...
6
2
1

Relationship

1
8

Authors

Journals

citations
Cited by 78 publications
(74 citation statements)
references
References 7 publications
2
72
0
Order By: Relevance
“…In December of 2015, the island had a subaerial area of about 13.6 km 2 [31]. The barrier island comprises a portion of a 105-km long Mississippi-Alabama wave-dominated barrier island chain that is backed by the shallow (<4-m depth) Mississippi Sound [32]. A tide gauge, first established in 1966 and operated by the National Oceanic and Atmospheric Administration (NOAA) (station ID: 8735180), is located on the eastern side of the island (Figure 2).…”
Section: Study Sitementioning
confidence: 99%
“…In December of 2015, the island had a subaerial area of about 13.6 km 2 [31]. The barrier island comprises a portion of a 105-km long Mississippi-Alabama wave-dominated barrier island chain that is backed by the shallow (<4-m depth) Mississippi Sound [32]. A tide gauge, first established in 1966 and operated by the National Oceanic and Atmospheric Administration (NOAA) (station ID: 8735180), is located on the eastern side of the island (Figure 2).…”
Section: Study Sitementioning
confidence: 99%
“…The island chain is backed by the shallow (less than 4 meters [m] deep) Mississippi Sound (Otvos and Carter, 2008). Dauphin Island is the only barrier island located offshore of coastal Alabama.…”
Section: Dauphin Islandmentioning
confidence: 99%
“…2). Dauphin Island was formed about 3,500 to 5,000 years ago when the rising sea levels during the mid-to late Holocene Epoch led to the engulfment of a Pleistocene beach ridge (that is, a higher ridge on the eastern side of Dauphin Island) (Otvos and Carter, 2008). Barrier islands in the Mississippi Sound have experienced a strong westward movement due to longshore drift and westward littoral transport (Otvos, 1970;Morton, 2008).…”
Section: Dauphin Islandmentioning
confidence: 99%
“…With access to fresh water, bare sand is colonized by pioneering species, leading to foredune growth and gradual transitions to shrubland and maritime forest [3,8,9]. On barrier islands in the northern Gulf of Mexico, the extent of total land area and drier habitat types, which form at higher elevations, such as shrubland and woodland, is declining relative to lower-elevation, wetter habitat types, such as marsh, at a time scale of a few decades [3,10,11]. This appears to be a combined effect of relative sea level rise and navigational shipping channels impeding natural littoral drift, ultimately affecting sediment replenishment along these islands [11].…”
Section: Introductionmentioning
confidence: 99%