Chapter 7 (atmosphere) Flashcards
tornado
violently rotating column of air associated with extreme horizontal winds
work
force times distance (joules)
power
rate at which work is done (watts)
current global energy consumption
13 tW per year
potential energy
stored energy
kinetic energy
energy of motion
heat energy
energy of random motion of atoms and molecules
sensible heat
heat that may be sensed or monitored by a thermometer
latent heat
amount of heat that is either absorbed or released when a substance changes phase
latent heat of vaporization
energy required for vaporization of water
conduction
transfer of heat through a substance by means of atomic or molecular interactions
relies on temp differences
convection
transfer of heat by the mass movement of a fluid
convection cell
rising and falling currents due to differences in temperature
radiation
wave like energy that is emitted by any substance that possesses heat
earth’s energy balance
equillibrium between incoming and outgoing energy
wavelength
distance between tops of two successive waves
radiation and absorption of electromagnetic energy is affected by both
temp and reflectivity
hotter objects
emit more electromagnetic energy
if surface temp doubles,
radiated energy increases 16 times
hotter objects radiate energy
more rapidly and at shorter wavelengths
sun emits
short wave radiation
gamma x rays visible UV light
earth’s land surface, oceans, and clouds emit
long wave radiation
infrared
dark or black surfaces
absorb or radiate EM energy readily
light or white surfaces
tend to reflect EM energy rather than absorb it
atmosphere
gaseous envelope that surrounds earth
made up of gas molecules, suspended particles of soild and liquid, and falling precipitation
atmosphere is mainly composes of
nitrogen and oxygen
also argon, water vapor, and carbon dioxide
humidity
amount of water vapor in the atmosphere at a given temperature
relative humidity
ratio of water vapor present in the atmosphere to the maximum amount of water vapor that could be there
lowest layer of the atmosphere
troposphere
troposphere
extends about 8-16km above earths surface
rapid upward decrease in temperature
clouds at the very top
contains most of atmospheric carbon dioxide and methane
ozone is significantly less abundant
tropopause
upper boundary of the troposphere
cumulus clouds
puffy, fair weather, look like cotton
cumulonimbus clouds
thunderstorm clouds, release a lot of energy
atmospheric pressure (barometric pressure)
weight of column of air that is above any given point
force exerted by gas molecules on a surface
atmospheric pressure decreases rapidly at
higher elevations
air rises in areas of
low atmospheric pressure
dry air descends and sky conditions remain clear in
areas of high atmospheric pressure
cold, dry, converging air movement creates
low pressure
warm, moist, diverging air movement results in
high pressure
changes in atmospheric pressure are
a major driving force for wind
parcel
small volume of air
atmospheric stability
tendency of a parcel to remain in place or change its vertical position
an air mass is stable if
its parcels of air resist vertical movement or return to their original position after they have moved