Natural Disasters

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Final Exam Review

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63 Terms

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Storm stages

  • tropical wave

  • tropical depression or disturbance

  • tropical storm (gets named from here)

  • hurricane (74 mph winds)

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What is fire?

rapid combustion

  • combination of O2 with carbon, hydrogen, and other elements in a chemical reaction that produces light, heat, and flame

  • exothermic reaction (releases heat) o can think of it as the opposite of photosynthesis

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Fire stages: pre-heating

water is expelled from wood/fuel

this is accomplished through:

  • flames (nearby fires)

  • long periods of dryness (lack of rain, drought)

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Fire stages: pyrolysis

thermal degradation of wood cellulose (stable to about 615 F)

  • gives off flammable gasses and water vapor

  • ash

  • gas movement causing cracks in the wood

  • can BECOME flames

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Fire stages: flaming combustion

pyrolyzed wood burns hot and fast

  • greatest energy released

  • highly efficient; predominates in windy environments

heat transfer through:

  • radiation

  • convection

  • conduction

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Fire stages: glowing combustion

after the active flames die off; coals

  • wood slowly consumed in oxidation reaction

  • lower temperature!

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Fire burn direction

Up!

  • up slope

  • heat rises

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2005 hurricane season

Worst season on record until 2020

  • 27 names storms

  • 7 considered major

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Hurricane seasonal average

10 named storms, 6 hurricanes, 2 major

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Pacific Ocean name for hurricane

Typhoon

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Indian Ocean name for hurricane

Cyclone

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tropical wave

  • initial low pressure disturbance

  • unorganized

  • moving west

  • winds < 20 mph

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tropical depression or disturbance

  • moving mass of thunder storms

  • starting to organize

  • assigned a number

  • winds < 39 mph

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tropical storm

  • gets named

    • alternating male/female names starting with "A"

  • distinct rotary/cyclonic motion

  • winds 39 – 74 mph

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Hurricane

  • well-defined circular structure with large rain bands

  • central "eye" of low pressure first forms

  • winds > 74 mph (increasing to > 150 mph)

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Northern Hemisphere hurricane turn which way??????

Counterclockwise

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Cat 2 hurricane in terms of energy from hydrogen bombs???

Hundreds

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Hurricane conditions in the beginning

calm wind patterns

  • for several days and 100s of miles

warm ocean surface (80 degrees)

  • as well as 200 feet below

vertical disturbance in the atmosphere

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Saffir Simpson scale

measured in categories (1 through 5)

  • function of wind speed and storm surge

    • potential damage

    • potential damage is not linear with category

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Saffir Simpson scale: cat 1

wind: 74-95 mph

effects: No real damage to building structures

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Saffir Simpson scale: cat 2

wind: 96-110 mph

effects: Minor damage to buildings. Considerable damage to vegetation

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Saffir Simpson scale: cat 3

wind: 111-130 mph

effects: Some structural damage to small residences. Mobile homes are destroyed. Flooding near the coast.

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Saffir Simpson scale: cat 4

wind: 131-155 mph

effects: Complete roof structure failure on small residences. Major erosion of beach. Major damage to lower floors of structures.

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Saffir Simpson scale: cat 5

wind: >155 mph

effects: Complete roof failure and major damage to all structures located less than 15 feet ASL

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Storm surge

large volume of rain/runoff prior to landfall of the hurricane

  • 90% of all fatalities in a hurricane caused by storm surge

  • large amounts of erosion

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Storm surge from 3 factors:

  • force of the waves (including debris in the water)

  • hydraulic lift (upward force) under structures

  • reflected wave energy from man-made structures

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Factors in storm surge SEVERITY

  • wind speed

  • tide stage

  • low pressure

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two types of surge:

flood surge: water brought onto the land by the storm

ebb surge: water floods off the land to the sea

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Where is wind moving fastest on that there hurricane moving north?

knowt flashcard image
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Doppler radar

Examines final movements prior to landfall

  • hours to days timescale

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visible and infrared satellite images

  • Every 30 minutes on average

    • can be acquired pretty fast

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Planes flying through hurricane storm center

  • measure vertical structure, wind speeds, pressure, and temperatures

  • use drop-sonde instruments to relay information regarding the change with height

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Hurricane Andrew

Category 4-5

Bahamas —> Florida —> Louisiana

COSTLIEST IN U.S. History (UNTIL KATRINA)

COULD have been worse if it landed a bit more north

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Hurricane Katrina

Costliest Atlantic hurricane in history!!!

  • costliest damage at eye wall

  • mini swirls did happen!

  • Florida, to the gulf, to Louisiana after it regained energy

  • Cat 5 in the Gulf

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NOVA: Flood! (The Great flood of 1993)

Flooding in the Midwest! (Mississippi River)

  • unusually wet Summer

    • JETSTREAM stayed over the Midwest month after month (storm highway)

  • weakening levees

  • all out war against nature

    • bringing in more dam/levee supplies

    • multiple levee breaks/multiple crests

St. Louis

  • big ass floodwall broke!

  • broken levee on the Columbia side relieve pressure on St. Louis and the propane tanks

  • 9 state area

  • costliest flood in U.S. hisotry

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Mini swirls

small localized swirls within the eyewall

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Flood

damaging floods result when the volume of river/stream flow exceeds natural barriers and/or the levels of flood preparedness

 because flow is greater or longer than expected

 because of an incomplete understanding of local hazards

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Natural flood causes

  • heavy rain

  • dam failure

  • rapid snowmelt / ice jams

  • deforestation

  • steep slopes

  • storm surges during tropical storms / hurricanes

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Deadliest flood disaster

Johnstown floods

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Infiltration capacity

capacity of a soil to absorb water

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High infiltration rates

  • coarse soil

  • well-vegetated land

  • low soil moisture

  • porous topsoil

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poor infiltration rates

  • impermeable crusts in the soil

  • salt layers

  • cold weather (frozen soil has poor infiltration)

  • compaction

  • paved (impervious) surfaces

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Hydrograph

discharge rate (Q) in m3/s (plus rainfall amount) versus time

  • measured by a stream gauge

  • varies with infiltration capacity and rainfall amount

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Case Study: Pittsburgh flood 1936

Flood Control Act 1936 and 1938

primary causes

  • prolonged precipitation (snow & rain)

  • high intensity, shorter duration rains

  • certain areas had large flash floods

  • steep slopes, thin soil cover, low vegetation

Power and water cut off; contamination by sewage

Flood Control Act 1936 and 1938

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Flash flooding of Washington Blvd. in Pittsburgh

Aug. 19, 2011 at 4:30pm (rush hour) o 1.79 inches of rain in 30 min

  • volume = 208 Olympic sized swimming pools

  • 10 feet of water rapidly rose on the roadway

  • sewer capacity was exceeded

  • killed 4 people

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Miramichi Fire

October 1825 (Maine & New Brunswick)

  • a summer of sparse rain

  • strong winds spread smaller camp and settler’s fires

  • among the worst wildfires in North American history Page 2/6

  • burned 3.9 million acres

  • killed 160 - 500 people

  • left 15,000 homeless

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Bad trees for fires D:

Ponderosa Pines

  • western U.S.

  • cones don’t open until a certain temperature is reached

Eucalyptus

  • high oil content

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Riskiest area in the world for wildfires

the Mediterranean

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Northern California: Mendocino complex fire

burned more than 459,000 acres

  • the largest complex fire in the state's history

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Diablo winds

Originate inland in areas of high pressure

  • air becomes hotter and drier as it heads west towards the low pressure coast

  • speed up as they are forced through narrow spaces (canyons and mountainsides)

  • if they hit already dry area, they can fan the flames and carry the wildfire overland

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Early earth

was more similar to present-day Venus than what we have today

  • extreme volcanic activity

  • high CO2 in atmosphere (we talking 98% yo) and hotter temperatures

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Where that early earth CO2 go??

Its in the limestone and other organic material!!! (80% of it)

  • resulting from plate tectonics and rock cycle

rest went to oceans and living material

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Oxygen isotopes

we can examine changes in rock and fossil composition over time  for example: O2 isotope ratio in shells (think back to those early lectures!)  there are three isotopes of O2 (16O, 17O, 18O) - 16O is the most common Page 2/6  evaporation from the oceans favors lighter isotopes  therefore, precipitation concentrates 16O and 17O on land (in ice/snow) and 18O gets concentrated in the sea  if the amount of 18O/16O is measured in shells, scientists know about the conditions of the water at the time they were formed - lower 18O meant warmer conditions

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Greenhouse gasses

allow solar energy in but trap the radiant heat from the Earth from escaping

  • water vapor (H2O)

  • carbon dioxide (CO2)

  • methane (CH4)

  • nitrous oxide (N2O)

  • ozone (O3)

  • CFC’s

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Intergovernmental Panel on Climate Change (IPCC)

  • 100’s of scientists meeting and reporting their findings on climate change

  • assess current models/predictions

  • report areas of uncertainty

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High level findings from IPCC

warming of climate is not in question

  • 90% of all warming since 1950 is due to human activity

  • all greenhouse gases are at their highest amount in the past 650,000 years 

  • the probability that this is all from natural causes is < 5% 

  • average world temperatures could rise from 1 to 6° F by 2100 

  • > 60% chance of increased droughts, hurricanes, and extreme tides 

  • > 90% chance of more frequent heat waves and heavy rainfall 

  • a rise in sea level of between 7 – 23 inches 

  • levels now will continue to affect the climate for the next 1,000 years!

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Climate mitigation options

changes in technology o carbon-free or carbon-neutral energy technologies for power plants, cars, etc.

  • takes time (politics) o cap and trade 

limit CO2 emissions through a market-based trading system 

  • CO2 producers pay more for emissions credits 

  • non-CO2 producers gain by selling credits

air scrubbing

  • possible but VERY expensive right now o

fertilizing the oceans with FeSO4 to grow algae (similar to massive tree planting)

  • algae would take up CO2 

  • effects on the ocean’s biosphere unknown?

weathering of rocks

  • pulls CO2 out of atmosphere and makes carbonic acid 

  • also, very slow

geoengineering 

  • inject large amounts of particles into the atmosphere to reflect solar energy 

  • similar to a volcanic eruption 

  • risks unknown? 

carbon sequestration 

  • capturing CO2 and injecting it deep underground in a liquid form

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Taxonomy order

kingdom  phylum  class  order  family  genus  species

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