Using Holocene relative sea-level data to inform future sea-level predictions: An example from southwest England

W. Roland Gehrels; David A. Dawson; Jon Shaw; William A. Marshall

doi:10.1016/j.gloplacha.2011.05.013

Using Holocene relative sea-level data to inform future sea-level predictions: An example from southwest England

W. Roland Gehrels^*
, David A. Dawson
, Jon Shaw
, William A. Marshall

^*Corresponding author for this work

School of Geography, Earth and Environmental Sciences

Research output: Contribution to journal › Article › peer-review

Original language	English
Pages (from-to)	116-126
Number of pages	0
Journal	Global and Planetary Change
Volume	78
Issue number	0
DOIs	https://doi.org/10.1016/j.gloplacha.2011.05.013
Publication status	Published - 2011

Keywords

Sea level
Isostasy
English Channel
Foraminifera
Britain
IPCC
UKCIP

Access to Document

10.1016/j.gloplacha.2011.05.013

Cite this

@article{aa26b5f3639b41afa13be1d3ce6ef505,

title = "Using Holocene relative sea-level data to inform future sea-level predictions: An example from southwest England",

keywords = "Sea level, Isostasy, English Channel, Foraminifera, Britain, IPCC, UKCIP",

author = "Gehrels, \{W. Roland\} and Dawson, \{David A.\} and Jon Shaw and Marshall, \{William A.\}",

year = "2011",

doi = "10.1016/j.gloplacha.2011.05.013",

language = "English",

volume = "78",

pages = "116--126",

journal = "Global and Planetary Change",

issn = "0921-8181",

publisher = "Elsevier B.V.",

number = "0",

}

TY - JOUR

T1 - Using Holocene relative sea-level data to inform future sea-level predictions: An example from southwest England

AU - Gehrels, W. Roland

AU - Dawson, David A.

AU - Shaw, Jon

AU - Marshall, William A.

PY - 2011

Y1 - 2011

KW - Sea level

KW - Isostasy

KW - English Channel

KW - Foraminifera

KW - Britain

KW - IPCC

KW - UKCIP

U2 - 10.1016/j.gloplacha.2011.05.013

DO - 10.1016/j.gloplacha.2011.05.013

M3 - Article

SN - 0921-8181

VL - 78

SP - 116

EP - 126

JO - Global and Planetary Change

JF - Global and Planetary Change

IS - 0

ER -