Storms 1: Meteorology Basics
storms account for 75% of natural disasters deaths and damages in the US
1980-2010: 134 weather-related disasters caused > $1 billion in damages each
total damages = >$880 billion
weather: conditions in the atmosphere at a given time and place
temperature
moisture
wind
pressure
occurs in troposphere
first 5-9 miles
energy that powers storms
heat energy from the sun is turned into sensible heat and latent heat
heat we can sense or feel (or measure)
when we measure temperature, we are measuring sensible heat
on an atomic level, this is really particles moving around
“hidden” heat energy
energy absorbed during a state change like melting (ice to water)
can be released as sensible heat if the state change is reversed (ex: condensing, freezing)
if liquid water becomes gaseous: heat is taken from the surroundings
if gaseous water becomes liquid: heat is transferred to the surroundings
therefore, humid air (with lots of gaseous water) can be energy source for storms
absolute humidity: amount of water vapor in air
absolute humidity = mass of water/ mass of air
grams of moisture per m^3
total amount of water vapor in air varies with temperature
more water in warmer air
less water in cooler air
so, the absolute measure is not very useful
relative humidity: percentage of the maximum water vapor that could be in the air at a given temperature
relative humidity = current absolute humidity/highest possible absolute humidity
100% relative humidity = air is completely saturated with water vapor; rain is possible
highest possible absolute humidity changes with temperature
storms account for 75% of natural disasters deaths and damages in the US
1980-2010: 134 weather-related disasters caused > $1 billion in damages each
total damages = >$880 billion
weather: conditions in the atmosphere at a given time and place
temperature
moisture
wind
pressure
occurs in troposphere
first 5-9 miles
energy that powers storms
heat energy from the sun is turned into sensible heat and latent heat
heat we can sense or feel (or measure)
when we measure temperature, we are measuring sensible heat
on an atomic level, this is really particles moving around
“hidden” heat energy
energy absorbed during a state change like melting (ice to water)
can be released as sensible heat if the state change is reversed (ex: condensing, freezing)
if liquid water becomes gaseous: heat is taken from the surroundings
if gaseous water becomes liquid: heat is transferred to the surroundings
therefore, humid air (with lots of gaseous water) can be energy source for storms
absolute humidity: amount of water vapor in air
absolute humidity = mass of water/ mass of air
grams of moisture per m^3
total amount of water vapor in air varies with temperature
more water in warmer air
less water in cooler air
so, the absolute measure is not very useful
relative humidity: percentage of the maximum water vapor that could be in the air at a given temperature
relative humidity = current absolute humidity/highest possible absolute humidity
100% relative humidity = air is completely saturated with water vapor; rain is possible
highest possible absolute humidity changes with temperature