Coastal Dunes Flashcards

1
Q

What are snow dunes?

A

Wind blown snow can form dunes just like sand, and 11% of the Earth (mostly at the poles) is covered by them

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2
Q

Where can you find snow dunes?

A

On a coastal plain of the Arctic Ocean

Greenland, Antarctica, Alaska, etc.

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3
Q

What are the essential ingredients for a dune?

A

Sediment input from offshore to build a beach (sediment supply)
Availability of sediment on beach (lack of stabilisers)
Wind (transport capacity) to transport sediment from beach onshore
Space onshore for dunes to grow (lack of houses/cliffs)
Time for dunes to build between destructive storms

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4
Q

What type of beach is required for a dune?

A
High wave energy, wide surf zone, lots of bars
Low and wide beach
Least flow disturbance (flat beach)
Large sediment availability
Steepness reduces transport capacity
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5
Q

The angle the wind is blowing out compared where your beach is a vital dune formation consideration

A

Some way to get the sand from the intertidal zone (longshore transport and cross shore important), onto the beach and into the dune building area
Wind beach alignment crucial
Amount of beach exposure

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6
Q

Sediment movement processes

A

Saltation
Threshold wind speed required to entrain sediment
Very fine sediment more cohesive
Large sediment harder to entrain
Round quartz vs irregular shell fragments

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7
Q

Transport (dry vs. wet thresholds)

A

Wet sand is harder to entrain than dry sand

More cohesion so higher wind speed required

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8
Q

Meso-scale influences

A

An experiment to see how beach input to dunes varies over time:
Sediment availability- high tides and snow cover
The perfect conditions: when it is windy from the right direction, at low tide without any rain/snow
Strong winds often come with big waves, and/or rain
Moderate winds do the most work

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9
Q

Typical wind profile on a foredune

A

Wind speed up
Increase in wind speed close to dune crest
Particularly in larger dunes
Increased potential to transport sediment

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10
Q

Sometimes an Offshore wind is important

A

Recirculating wind within recirculation zone, or deflected from crest may be strong enough to transport sediment from the beach onto the dune.

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11
Q

Terrestrial laser scanning (TLS)

A
3D imprint of landscape
High resolution (~1.2 mm) 
Surface topography
Sand movement 
Vegetation
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12
Q

Sand transport on Protodune

A

Switch from erosion to deposition at 0.95m, upwind of crest
Reduced transport on strip lee; downwind
A bedform, only ~ 6 cm height can significantly influence transport!

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13
Q

Main coastal dune types

A
Foredunes (most common type)
Blowouts (typically in association with foredunes)
Parabolic dunes (more common on coasts with moderate to high wave/wind energy and sediment supply)
Transgressive dunes (similar environments to parabolic, but limited vegetation e.g. aridity/cold)
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14
Q

Dunes have many uses

A

Natural resources (mining, water storage, crops)
Coastal protection
Tourism

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15
Q

Sand fences

A

Trap sand
Create new dunes, or fill in gaps Inexpensive and easy to construct
Different fence configurations

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16
Q

What is an example of an artificial dune?

A

Sand fences

17
Q

What is an artificial dune?

A

Mimic natural protection processes

18
Q

Who writes a good paper on dunes (look up flashcards and remember them).

A

Hesp (2011)

Houser (2009)