Difference between revisions of "Coastal squeeze"
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| − | {{ | + | {{Definition|title=Coastal squeeze |
| + | |definition= intertidal habitat loss which arises due to the high-water mark being fixed by a defence and the low water mark migrating landwards in response to sea level rise<ref>Pontee, N. 2013. Defining coastal squeeze: A discussion. Ocean and Coastal Management 84: 204-207</ref>}} | ||
| − | This article | + | |
| + | This article complements the article '[[Effects of global climate change on European marine biodiversity]]' by Lieven Therry with a shorth introduction to the impact of coastal squeeze on biodiversity. | ||
=Coastal Squeeze= | =Coastal Squeeze= | ||
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| − | Europe accommodates a significant number of shorebirds in winter. Shorebird numbers depend on intertidal areas, so [[Sea level rise|sea-level rise]] could reduce the carrying capacity for these shorebirds | + | Europe accommodates a significant number of shorebirds in winter. Shorebird numbers depend on intertidal areas, so [[Sea level rise|sea-level rise]] could reduce the carrying capacity for these shorebirds<ref name="Nicholls"> Nicholls, R.J.; Klein, R.J.T. (2005). Climate change and coastal management in Europe's coast, '''in''': Vermaat, J.E. ''et al.'' (Ed.) (2005). Manging European coasts: past, present and future. pp. 199-226. </ref> |
| − | Average sea level rise is predicted to be up to 90 cm by the year 2100. | + | Average sea level rise is predicted to be up to 90 cm by the year 2100 compared to 2000. This will not greatly affect the highly adaptable sandy-shore biota for beaches that follow sea level rise, according to the [[Bruun rule]]. Onshore migration is the natural ecosystem response to rising sea levels, but this is stopped by fixed sea defenses. Intertidal zones (e.g. beaches, mudflats, salt marshes) are trapped in a ‘coastal squeeze’ between the impacts of urbanization on the terrestrial side and manifestations of climate change at sea. While unconstrained, these intertidal zones are resilient, changing shape and extent naturally in response to storms and variations in wave climate and currents. However, human modifications of the coastal zone severely limit this flexibility<ref name="Nordstrom"> Nordstrom, K.F. (2000). Beaches and dunes on developed coasts. Cambrige University Press, Cambridge, UK, '''cit. in''': Schlacher, T.A.; Dugan, J.; Schoeman, D.S.; Lastra, M.; Jones, A.; Scapini, F.; McLachlan, A.; Defeo, O. (2007). Sandy beaches at the brink. ''Diversity and Distribution''.</ref>. This raises a fundamental conflict between protecting socio-economic activity and sustaining the ecological functioning of the coastal zone in Europe under rising sea levels. It suggests a need for more soft protection (nourishment), managed retreat, and possibly accommodation strategies. <ref name="Nicholls"> Nicholls, R.J.; Klein, R.J.T. (2005). Climate change and coastal management in Europe's coast, '''in''': Vermaat, J.E. ''et al.'' (Ed.) (2005). Manging European coasts: past, present and future. pp. 199-226. </ref> <ref name="McLachlan"> McLachlan, A.; Brown, A.C. (2006). The ecology of sandy shores. 2nd. Edition. Academic Press: Amsterdam, The Netherlands. 373 pp. </ref> |
| − | + | The ecological consequences of hard engineering interventions on retreating beaches entails the loss of biodiversity, productivity, and critical habitats as well as modifications of the subtidal zone, which is an important [[recruitment]] zone for many sandy beach animals<ref name="Dugan"> Dugan, J.E. & Hubbard, D.M. (2006). Ecological responses to coastal armouring on exposed sandy beaches. ''Shore and Beach'' 74: 10-16. '''cit. in''': Schlacher, T.A.; Dugan, J.; Schoeman, D.S.; Lastra, M.; Jones, A.; Scapini, F.; McLachlan, A.; Defeo, O. (2007). Sandy beaches at the brink. ''Diversity and Distribution''.</ref> <ref name="Peterson1"> Peterson, C.H. & Bishop, M.J. (2005). Assessing the environmental impacts of beach nourishment. ''Bioscience'' 55: 887-896. '''cit. in''': Schlacher, T.A.; Dugan, J.; Schoeman, D.S.; Lastra, M.; Jones, A.; Scapini, F.; McLachlan, A.; Defeo, O. (2007). Sandy beaches at the brink. ''Diversity and Distribution''.</ref>. Even beach nourishment is not free of negative ecological consequences, especially if the grainsize of the fill material does not correspond to the original beach sediment<ref name="Peterson2"> Peterson, C.H.; Bishop, M.J., Johnson, G.A.; D’Anna, L.M. & Manning, L.M. (2006). Exploiting beach filling as an unaffordable experiment: benthic intertidal impacts propagating upwards to shorebirds. ''Journal of Experimental Marine Biology and Ecology'' 338: 205-221. '''cit. in''': Schlacher, T.A.; Dugan, J.; Schoeman, D.S.; Lastra, M.; Jones, A.; Scapini, F.; McLachlan, A.; Defeo, O. (2007). Sandy beaches at the brink. ''Diversity and Distribution''.</ref><ref name="Speybroeck"> Speybroeck, J.; Bonte, D.; Courtens, W.; Gheskiere, T.; Grootaert, P.; Maelfait, J.P.; Mathys, M.; Provoost, S.; Sabbe, K.; Stienen, E.W.M.; Van Lancker, V.; Vincx, M. & Degraer, S. (2006). Beach nourishment: an ecologically sound coastal defence alternative? A review. Aquatic conservation – Marine and Freshwater Ecosystems 16: 419-435. '''cit. in''': Schlacher, T.A.; Dugan, J.; Schoeman, D.S.; Lastra, M.; Jones, A.; Scapini, F.; McLachlan, A.; Defeo, O. (2007). Sandy beaches at the brink. ''Diversity and Distribution''.</ref>. | |
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[[Image:coastalsqueeze.jpg|centre|300px|Coastal squeeze SOURCE: www3.hants.gov.uk|frame]] | [[Image:coastalsqueeze.jpg|centre|300px|Coastal squeeze SOURCE: www3.hants.gov.uk|frame]] | ||
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| + | ==Solutions to coastal squeeze== | ||
| + | Solutions to coastal squeeze are described in the article [[Climate adaptation measures for the coastal zone]]. Three types of measures are discussed: | ||
| + | * Seaward extension of the coast: see [[Climate adaptation measures for the coastal zone#Foreland creation|Foreland creation]]. | ||
| + | * Moving the flood defense inland: see [[Climate adaptation measures for the coastal zone#Foreland restoration - managed realignment|Foreland restoration - managed realignment]]. | ||
| + | * Managed retreat: see [[Climate adaptation measures for the coastal zone#Preparing for retreat|Preparing for retreat]]. | ||
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:[[Shoreline management]] | :[[Shoreline management]] | ||
:[[Sea level rise]] | :[[Sea level rise]] | ||
| − | :[[Climate adaptation | + | :[[Bruun rule for shoreface adaptation to sea-level rise]] |
| + | :[[Effect of climate change on coastline evolution]] | ||
| + | :[[Climate adaptation measures for the coastal zone]] | ||
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==References== | ==References== | ||
Latest revision as of 12:09, 6 March 2022
Definition of Coastal squeeze:
intertidal habitat loss which arises due to the high-water mark being fixed by a defence and the low water mark migrating landwards in response to sea level rise[1]
This is the common definition for Coastal squeeze, other definitions can be discussed in the article
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This article complements the article 'Effects of global climate change on European marine biodiversity' by Lieven Therry with a shorth introduction to the impact of coastal squeeze on biodiversity.
Contents
Coastal Squeeze
A significant threat for coastal organisms is loss of habitat. This may be due to direct loss through coastal land claim. This often involves building structures to protect the land and/or infrastructure from erosion and sea defences to prevent erosion and/or flooding. These and other techniques effectivley 'fix' the coastline. This is particlularly important where it effects habitats and ecosystems that would normally move landward in response to erosive forces. Where there is a rise in sea level relative to the land a coastal squeeze[2] takes place. This is exacerbated by global warming, which not only leads to higher sea levels, but also an increase of the storm frequency. Increased storminess results in coastal erosion including cliff erosion, retreat of beaches, loss of salt marsh and dune scarping with vegetation loss.
Effects on coastal organisms
Europe accommodates a significant number of shorebirds in winter. Shorebird numbers depend on intertidal areas, so sea-level rise could reduce the carrying capacity for these shorebirds[3]
Average sea level rise is predicted to be up to 90 cm by the year 2100 compared to 2000. This will not greatly affect the highly adaptable sandy-shore biota for beaches that follow sea level rise, according to the Bruun rule. Onshore migration is the natural ecosystem response to rising sea levels, but this is stopped by fixed sea defenses. Intertidal zones (e.g. beaches, mudflats, salt marshes) are trapped in a ‘coastal squeeze’ between the impacts of urbanization on the terrestrial side and manifestations of climate change at sea. While unconstrained, these intertidal zones are resilient, changing shape and extent naturally in response to storms and variations in wave climate and currents. However, human modifications of the coastal zone severely limit this flexibility[4]. This raises a fundamental conflict between protecting socio-economic activity and sustaining the ecological functioning of the coastal zone in Europe under rising sea levels. It suggests a need for more soft protection (nourishment), managed retreat, and possibly accommodation strategies. [3] [5]
The ecological consequences of hard engineering interventions on retreating beaches entails the loss of biodiversity, productivity, and critical habitats as well as modifications of the subtidal zone, which is an important recruitment zone for many sandy beach animals[6] [7]. Even beach nourishment is not free of negative ecological consequences, especially if the grainsize of the fill material does not correspond to the original beach sediment[8][9].
Coastal squeeze SOURCE: www3.hants.gov.uk
Solutions to coastal squeeze
Solutions to coastal squeeze are described in the article Climate adaptation measures for the coastal zone. Three types of measures are discussed:
- Seaward extension of the coast: see Foreland creation.
- Moving the flood defense inland: see Foreland restoration - managed realignment.
- Managed retreat: see Preparing for retreat.
Related articles
- Shoreline management
- Sea level rise
- Bruun rule for shoreface adaptation to sea-level rise
- Effect of climate change on coastline evolution
- Climate adaptation measures for the coastal zone
References
- ↑ Pontee, N. 2013. Defining coastal squeeze: A discussion. Ocean and Coastal Management 84: 204-207
- ↑ Doody, J.P. (2004) 'Coastal squeeze' - an historical perspective. Journal of Coastal Conservation, 10/1-2, 129-138.
- ↑ 3.0 3.1 Nicholls, R.J.; Klein, R.J.T. (2005). Climate change and coastal management in Europe's coast, in: Vermaat, J.E. et al. (Ed.) (2005). Manging European coasts: past, present and future. pp. 199-226.
- ↑ Nordstrom, K.F. (2000). Beaches and dunes on developed coasts. Cambrige University Press, Cambridge, UK, cit. in: Schlacher, T.A.; Dugan, J.; Schoeman, D.S.; Lastra, M.; Jones, A.; Scapini, F.; McLachlan, A.; Defeo, O. (2007). Sandy beaches at the brink. Diversity and Distribution.
- ↑ McLachlan, A.; Brown, A.C. (2006). The ecology of sandy shores. 2nd. Edition. Academic Press: Amsterdam, The Netherlands. 373 pp.
- ↑ Dugan, J.E. & Hubbard, D.M. (2006). Ecological responses to coastal armouring on exposed sandy beaches. Shore and Beach 74: 10-16. cit. in: Schlacher, T.A.; Dugan, J.; Schoeman, D.S.; Lastra, M.; Jones, A.; Scapini, F.; McLachlan, A.; Defeo, O. (2007). Sandy beaches at the brink. Diversity and Distribution.
- ↑ Peterson, C.H. & Bishop, M.J. (2005). Assessing the environmental impacts of beach nourishment. Bioscience 55: 887-896. cit. in: Schlacher, T.A.; Dugan, J.; Schoeman, D.S.; Lastra, M.; Jones, A.; Scapini, F.; McLachlan, A.; Defeo, O. (2007). Sandy beaches at the brink. Diversity and Distribution.
- ↑ Peterson, C.H.; Bishop, M.J., Johnson, G.A.; D’Anna, L.M. & Manning, L.M. (2006). Exploiting beach filling as an unaffordable experiment: benthic intertidal impacts propagating upwards to shorebirds. Journal of Experimental Marine Biology and Ecology 338: 205-221. cit. in: Schlacher, T.A.; Dugan, J.; Schoeman, D.S.; Lastra, M.; Jones, A.; Scapini, F.; McLachlan, A.; Defeo, O. (2007). Sandy beaches at the brink. Diversity and Distribution.
- ↑ Speybroeck, J.; Bonte, D.; Courtens, W.; Gheskiere, T.; Grootaert, P.; Maelfait, J.P.; Mathys, M.; Provoost, S.; Sabbe, K.; Stienen, E.W.M.; Van Lancker, V.; Vincx, M. & Degraer, S. (2006). Beach nourishment: an ecologically sound coastal defence alternative? A review. Aquatic conservation – Marine and Freshwater Ecosystems 16: 419-435. cit. in: Schlacher, T.A.; Dugan, J.; Schoeman, D.S.; Lastra, M.; Jones, A.; Scapini, F.; McLachlan, A.; Defeo, O. (2007). Sandy beaches at the brink. Diversity and Distribution.
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