COASTAL HAZARDS Flashcards

1
Q

often called shorelines, are a critical component of the biosphere because a large number of species are connected in some way or another to the unique habitats found at this interface between the land and sea.

A

Coastlines

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2
Q

are areas where tectonic forces deform and uplift the land. They are usually rugged and irregular, with beaches sometimes being restricted to coves and inlets.

A

Active shorelines

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3
Q

are areas with
little to no tectonic activity,
commonly resulting in a relatively
straight coastline with flat-lying
terrain. Ex. U.S. Gulf and Atlantic

A

Passive shorelines

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4
Q

The periodic rise and fall of sea level is known as

A

ocean tides

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5
Q

This complex interaction creates a net outward force, called

A

tidal force,

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6
Q

high tides and two low tides each day (approximately __________ passes
between two high tides). Note that tides also occur on large lakes, but the rise and fall is

A

12 hours and 25 minutes

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7
Q

refers to the difference in sea level between high and low tides.

A

Tidal range

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8
Q

occurs when the Moon and Sun periodically line up such that their gravitational
effects reinforce one another.

A

Spring tide

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9
Q

occurs when the gravitational pull of the Moon and Sun are at right angles which
tend to cancel their tidal effects on one another.

A

Neap tide

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10
Q

++In addition to orbital influences, tidal range varies depending on latitude, water depth, shape
of the shoreline, and the presence of large storms.++

A
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11
Q

are strong localized currents during high tide formed by the surface of
the sea sloping towards the shore which generates mechanical energy that forces
water to funnel up into inlets and river channels.

A

Tidal currents

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12
Q

involve the physical movement of water molecules from one
location to another

A

Ocean currents

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13
Q

are large-scale currents in the open water near the surface of the
sea which are driven mainly by winds blowing consistently in the same direction.

A

Surface currents

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14
Q

are formed in response to differences in ocean temperature and salinity. Cooler and more saline water is relatively dense which causes it to sink and
flow toward areas where water is less dense.

A

Density currents

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15
Q

refer to density-driven currents that circulate enormous volumes
of water, both vertically and horizontally, in a convective manner between tropical and polar regions.

A

Ocean Conveyor

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16
Q

++Density and wind-driven currents transfer vast amounts of heat energy from the Tropics toward higher latitudes (influence the global climate system) and also transport nutrients into the ocean.+++

A
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17
Q

transport energy through water such that water molecules move or vibrate in a circular manner.

A

Water waves

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18
Q

As the wave continues toward shore, this causes a progressive decrease in velocity along the length of the wave, forcing it to bend in a process called

A

wave refraction

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19
Q

is a wave whose amplitude reaches a critical level at which some process can suddenly start causing large amounts of wave energy to be transformed into turbulent kinetic energy.

A

Breaking wave

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20
Q

refers to the area where the waves break

A

Surf zone

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21
Q

is an ocean current that flows parallel to the shore and is caused by large swells Iseries of waves) sweeping into the shoreline at an angle and pushing down the length of the beach in one direction.

A

Longshore current

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22
Q

is the process of transporting material along a coast by waves that approach at an angle to the shore but recede perpendicular from it.

A

Longshore drift or beach drift

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23
Q

interaction between waves and a landmass can cause the shoreline to slowly move landward, a process referred to as

A

shoreline retreat

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24
Q

are points of land that are just seaward and areas where waves first make contact with land

A

Headlands

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25
Q

are elongate deposits of sediment that parallel the shore and are separated from the mainland by open water, lagoons, tidal mudflats, or saltwater marshes

A

Barrier islands

26
Q

result from the complex interaction between waves, sea level change, and sediment supply

A

Barrier islands

27
Q

In general, most barrier islands are no
higher than _____ above sea level, but their shape varies depending on the relative

A

6m

28
Q

are elongated sediment deposits separated from the mainland by open water or wetlands.

A

Barrier islands

29
Q

to refer to large, rotating low-pressure storm systems that originate in tropical oceans.

A

Topical cyclones

30
Q

Winds and low pressure within a hurricane produce a rise in sea level called a

A

storm surge

31
Q

The unusually strong winds associated with hurricanes result from the circulating air masses within the storm.

A

High Winds

32
Q

the lowest category has winds of at least 74 miles per hour anything less is called a

A

tropical storm or depression.

33
Q

used to rank hurricanes based on their wind speed. Note how wind speed is related to the level of air pressure within the eye of a hurricane and its associated storm surge.

A

Saffir Simpson scale

34
Q

rapid rise in sea level called a ________ that inundates
areas above the normal high tide line (up to ___ rise in
sea level)

A

storm surge
9 m

35
Q

commonly leads to inland flooding far from where a storm makes landfall.

A

Intense precipitation

36
Q

the primary source of energy for tropical cyclones

A

ocean

37
Q

In addition to a storm’s precipitation rate, another key factor affecting the level of
flooding is a __________ as it moves over land. Slow moving storms

A

storm’s forward speed

38
Q

Slow-moving storms less than
___________

A

(16 km/ hr)

39
Q

Slow moving storm is particularly more dangerous since ________________

A

more rain will fall on a
given area compared to a storm that passes more rapidly .

40
Q

Rainfall intensity will also increase
when an ocean storm moves inland and encounters____________________

A

rugged or mountainous terrain

41
Q

The rapid elevation gain results in faster cooling rates, which, in turn, increases
the __________________

A

condensation and precipitation rates.

42
Q

The oldest mitigation strategy goes back to ancient cultures, where they___________________

A

avoided locating large settlements directly on the coasts

43
Q

the use of radio technology by ocean-going ships in the early 1900s to report weather conditions back to land-based stations.

A

Development of early warning systems

44
Q

combined with aircraft data allow scientists to use computer models to predict the path of hurricanes with
impressive accuracy.

A

weather satellites continuously track the storms’ location

45
Q

can now commonly predict out to 48 hours in advance where a hurricane
will make landfall and do so with a fairly high degree of accuracy.

A

Forecasting models

46
Q

which allows wave energy to pass beneath the structure rather
than smashing it completely off its foundation.

A

elevate a building above the
expected storm surge level

47
Q

These are unusually high-energy waves that form not from the wind, but rather by the transfer of energy from earthquakes, volcanic eruptions, landslides, or asteroids to a body of water.

A

Tsunamis

48
Q

Tsunamis traveling through deep ocean waters have exceptionally long wavelengths, typically from___________, and their wave base can be rather deep.

A

(10 - 500 km)

49
Q

Tsunamis travel at speeds of over _____________

A

(800 km/ hr ).

50
Q

December 26, 2004, wherein a magnitude 9.1 earthquake
occurred in the subduction zone located off the Indonesian coast of Sumatra which caused the______________

A

seafloor to suddenly shift

51
Q

passing tsunami waves are detected
based on their unusually long wavelength and high velocity.

A

deep ocean buoys

52
Q

are strong currents that flow away from the shore, sometimes inappropriately referred to as a

A

rip tide.

53
Q

Is a physical barrier made of concrete, steel, or large rocks built against the
shore. It is also called a bulkhead or revetment.

A

Seawall

54
Q

Often referred to as
hard stabilization or “armoring a shoreline” because it
physically prevents waves from directly impacting the shoreline.

A

Seawall

55
Q

made of large rocks or steel sheets and is built perpendicular to the shore.

A

groin

56
Q

refers to a group of groins.

A

groin field

57
Q

built-in perpendicular
to the shore in order to trap sand
moving with the longshore
current.

A

Groins

58
Q

barriers made of large rocks and are installed at the mouth of an
inlet to keep sediment from longshore current to clog channels,
thereby reducing dredging costs.

A

Jetties

59
Q

normally come in pairs
and are placed at the mouth
of inlets to help keep the
longshore movement of sand
from clogging navigational
channels.

A

Jetties

60
Q

barrier placed just offshore and is used to keep waves from
directly impacting the shoreline.

A

breakwater

61
Q

In many cases, the only real solution to beach starvation is to manually add
sand to the beach in a process called

A

beach nourishment.