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29 Cards in this Set

  • Front
  • Back
3 types of disasters

Natural


Technological


Stealth

Hazard probability


Hazard versus Disasters

Risk = Hazard * (Vulnerability - Preparedness)


Hazards are sources of disasters

Magnitude and Frequency

As magnitude increases, frequency decreases


As magnitude increases, return period increases.

Energy Sources for Natural Disasters

Sun: causes differential heating, weather, ocean currents


Internal heat: convection --> plate tectonics --> earthquakes


Gravity: erosion --> landslides


Extraterrestrial Impacts --> tsunamis

Lava Types

Basalt


Andesite


Rhyolite

Volcano Types

Shield/Fissure


Stratovolcanoes


Caldera

4 Types of Eruptions

Pahoehoe


Stromboli


Volcan


Plinian

Volcanic Explosivity Index takes into account 3 things:

volume of material erupted


height of eruption column


length of the blast

Volcano Hazards

pyroclastic flow


lahar


earthquakes


tsunamis


lava


famine


climate change

Quantifying Lava Flows

Velocity = ((density * gravity * sine of the slope) / viscosity) * (thickness * elevation - elevation^2 / 2)

Types of Landslides

Creep- slow


Slump


Debris flow- high liquid content


Rockfall

Basic Factor of Safety Equation

resisting forces / driving forces ; shear strength / shear stress


mgcos(x)/ mgsin(x)

Crazy Factor of Safety Equation

Cohesion + ((density * distance to surface * cos(angle of slope) - pore pressure) * tan(internal friction) / (density * distance to surface * sin(angle of slope)

Causes of Slope Failure

Saturated Soils (lots of rain, makes pore pressure positive, decreases effective normal stress)


Increase the slope angle (theta)


Change the material (influences how it retains water, grain size --> internal friction


Earthquakes


Undercutting


Erosion


Construction (adding mass to the slope)


Dip of the bedrock (interlocking friction good, plane friction bad)



Liquefaction

Mud volcanoes


Sand Boils


Quicksand

Normal wind patterns, effects on ocean

towards equator, east to west, pushes warm water towards Australia, creates upwelling (nutrient-rich cold water)

ENSO wind patterns, effects on ocean

weaker trade winds, water doesn't get pushed over, prevents upwelling,


increases temps by more than 0.5 degrees celsius for at least 3 consecutive months


occurs around December


lots of rain, flooding

La Nina

temperatures decrease by more than 0.5 degrees for 3 consecutive months

2 Ways to Monitor El Nino

SSTa - positive values = El Nino


SSta - negative values = La Nina


SOI - positive values = La Nina


SOI - negative values = El Nino




They are INVERSELY RELATED. If SSTa is positve, SOI is negative



Fire Chemical Reaction

C6H12O6 + O2 --> 6H2O + 6CO2 + release of heat

Fire Triangle

Oxygen, Fuel, Heat



Smother it, remove fuel source/prescribed burns



Types of Stuff that Burns

Slash


Ladder Fuel

4 Stages of Fire

Preheating- heat capacity


Pyrolosis- chemical reaction begins


Flaming Combustion- bursts into flame


Glowing Combustion- charcoals, dying down



2 Types of Spreading

Wind- more oxygen, dry air dries everything out


Wall of Fire- in a line


Crown spreading- from treetop to treetop



4 Types of Drought

Meteorological- department of precipitation from normal


Agricultural- amount of moisture in the soil no longer meets the needs of a crop


Hydrological- surface and subsurface water supplies are lower


Socioeconomical- physical water shortages affect people

Palmer Index

Good for identifying long-term drought

Palmer Hydrologic Drouht Index

How much rain you need to end a drought

Crop Moisture Index

How much moisture you need for specific crops

Dendroclimatology

Study of trees using rings