Lecture 11: Coastal Hazards Flashcards
Hazard does not always equal
risk
Hazards are usually measured based on their…
frequency and magnitude
large events occur far less frequently than small events
Risk =
H x E x V
(hazard x vulnerability x exposure)
Vulnerability and exposure can change over time
Hazards happen in the absence of
humans
Risk happens in the presence of
humans
Exposure =
££ value of infrastructure or number of people within a coastal zone
Vulnerability =
“susceptibility to harm”
event-driven (episodic)
tsunamis hurricanes, storms & cyclones storm "clusters" rip currents rock fall (cliffs)
chronic
shoreline erosion (sediment delivery) nuisance flooding climate-related hazards (slow, very large-scale drivers) relative sea-level rise ocean acidification ocean temperature hypoxia (nutrient loading)
What is a tsunami caused by fundamentally?
caused by water displacement usually at a tectonic boundary offshore (earthquake, lg landslide…).
An earthquake pushes up or drops down one part of the seafloor relative to another.
This displaces a volume of water, pushing it up.
Sets of an oscillation, which develops underwater at great speed.
Sea water is sucked back from the shore.
Waves get bigger as water gets shallower.
What direction do cyclones turn in the northern hemisphere?
Anti-clockwise
What direction do cyclones turn in the southern hemisphere?
Clockwise
What is a tropical cyclone?
A rotating low-pressure weather system that has organized thunderstorms but no fronts (a boundary separating two air masses of different densities).
tropical depression max sustained wind =
max sustained surface winds < 39 mph
tropical storm max sustained wind =
maximum sustained winds of > 39 mph
hurricane max sustained wind =
maximum sustained winds > 74 mph
What is the Coriolis effect?
The Earth’s rotation means that we experience an apparent force known as the Coriolis force. This deflects the direction of the wind to the right in the northern hemisphere and to the left in the southern hemisphere.
What is rip current?
An intermittent strong surface current flowing seaward from the shore.
A self organised feedback (in time and space)
Can also be geologically controlled
How does a rip current form?
Rip starts (1) with slight difference in beach morphology (like a gap between sand bars) or a difference in wave forcing onshore
2) larger waves on either side of the incipient rip push farther up the beach creates a lateral gradient: at rip, less onshore forcing means easier for water to flow offshore…
(3) fed by gradient in flow, feedback strengthens if strong enough, can carve a channel in the beach (a “rip channel”)
Why are rip currents temporary?
Rip is temporary because wave forcing tends to be variable and rip will die out if the flow gradient weakens enough
climate-related (large, slow…)
relative sea-level rise (makes all other elevated water levels worse – e.g., trend!)
CO2 input
ocean acidification
ocean temperature
hypoxia (nutrient loading) – algal blooms that use up all available dissolved oxygen in nearshore waters