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Twenty-eighth Report Adapting Institutions to Climate Change Cm ...

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2.73<br />

BOX 2D FACTORS AFFECTING THE CHARACTER AND SHAPE OF COASTLINES 43<br />

Geology<br />

Nature of rocks/sediments onshore and offshore<br />

Rock structure – bedding, joints, faults<br />

Position of water-table in coastal cliffs<br />

Rate of sediment supply <strong>to</strong> coastal areas<br />

<strong>Change</strong>s in the Earth’s crust<br />

Physical processes<br />

Waves – largely influenced by wind and water depth<br />

Tides<br />

Rates of relative sea level change<br />

Rainfall<br />

Frequency and intensity of s<strong>to</strong>rms<br />

Human interference<br />

Coastal construction<br />

Aggregate extraction<br />

Flood and coastal defences against erosion<br />

Coastal reclamation<br />

Agricultural land drainage<br />

There can be no doubt, therefore, that climate change will have a profound impact on the shape<br />

of the coastline just through the operation of natural forces. Coastal infrastructure, including<br />

coastal defences, ports and harbours, not only alters the appearance of the coastline but also has<br />

an influence on natural processes. More than 40% of the coastline of England and Wales has<br />

some form of coastal defence. Our present suite of coastal protection structures will be stretched<br />

<strong>to</strong> its full capacity under the conditions predicted for climate change and many may no longer be<br />

effective. The Commission saw evidence in south Wales from the National Trust on the scale and<br />

extent of the challenges confronting that organisation as it attempts <strong>to</strong> defend coastal sites and<br />

properties under its jurisdiction. 44 <strong>Adapting</strong> <strong>to</strong> the changed conditions presents a major institutional<br />

challenge.<br />

Coastal squeeze<br />

2.74 Low-lying coastlines with sandy or muddy seashores result from the gradual accretion of sediment<br />

deposited by tidal action. Because the slope of the seashore is so shallow, the extent of the intertidal<br />

zone can vary considerably with changes in sea level. Under natural conditions this can result in<br />

the coastline retreating inland as sea levels rise or moving further offshore where sea levels fall.<br />

Coastal development tends <strong>to</strong> form a barrier <strong>to</strong> this dynamic repositioning of the coastline so that<br />

there is no possibility of the coastline retreating inland. As a consequence, coastal habitats such<br />

as saltmarshes get squeezed and may eventually be lost al<strong>to</strong>gether. This in turn means that there<br />

25<br />

Chapter 2

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