Houser (2009) Summary of beach-dune interactions Flashcards

1
Q

Most barrier islands and spits are in a state of transgression (land- ward retreat), why is this?

A

In response to a combination of eustatic sea-level rise and local land subsidence.

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2
Q

What happens to barrier islands during extreme storms?

A

Barrier islands transgress during extreme storms capable of breaching the fronting dunes and distributing sediment to the back of the island in the form of washover fans.

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3
Q

What does the redistribution of sediment during an extreme storm and the rate of island transgression depend on?

A

The height and alongshore extent of coastal dunes relative to the elevation of the storm surge.

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4
Q

What does storm erosion of the backshore and dunes lead to?

A

A scarped seaward dune slope that promotes sediment transport to the lee slope and the migration of the dune landward.

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5
Q

What does an increase in sea mean for the migration of the the nearshore and beach profile?

A

The landward migration of the nearshore and beach profile, creating the potential for the dune system to retreat landward without loss of height.

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6
Q

What does migration of the beach dune system require?

A

Sediment eroded offshore by the storm surge to be delivered first to the beachface by nearshore (surf and swash) processes and then transported to the back- shore by the wind.

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