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Troposphere
The lowest layer of the atmosphere where weather occurs. 90% of all weather, 10 mi
Stratosphere
The layer of the atmosphere above the troposphere, containing the ozone layer.
Mesosphere
The layer of the atmosphere above the stratosphere.
Thermosphere
The layer of the atmosphere above the mesosphere.
Exosphere
The outermost layer of the atmosphere.
Ozone (O₃)
A molecule found mostly in the stratosphere that traps heat and blocks radiation.
Ionosphere
Part of Earth's upper atmosphere, between 80 and about 600 km, where solar radiation ionizes atoms and molecules.
Aurora
Natural light display in the sky, typically seen in high-latitude regions, caused by the ionosphere.
Magnetosphere
A protective bubble of magnetic field surrounding the planet, shielding it from harmful solar wind and cosmic rays.
Conduction
The process by which heat or electricity is directly transmitted through a substance without movement of the material.
Convection
The movement of particles through a substance, transporting heat energy from hotter areas to cooler areas.
Radiation
The process where energy is transferred from one object to another through electromagnetic waves.
Clouds
Visible masses of tiny water droplets or ice crystals suspended in the atmosphere.
Adiabatic heating/cooling
Processes involving changes in temperature due to work done on or by a system, with no heat transfer occurring.
Cold front
Forms when a cold, dense air mass pushes under a warm, lighter air mass, forcing the warm air to rise.
Warm front
A warm air mass pushes into a cooler air mass, often resulting in small showers.
Occluded front
A weather front formed when a cold front overtakes a warm front, leading to thunderstorms.
Stationary front
A boundary between two air masses where neither is strong enough to displace the other, resulting in fair weather.
Cyclone
An area of low pressure where air masses meet and rise.
Anticyclone
An area of high pressure where air moves apart and sinks.
Hadley cell
Located near the equator, where warm, moist air rises and cools, forming clouds and precipitation.
Ferrell cell
Found between 30 and 60 degrees latitude, driven by the interaction between the Hadley and Polar cells.
Polar cell
Located at high latitudes, where cold, dry air sinks and moves towards the equator.
Thermal Inversion
A phenomenon where a layer of warm air sits above a layer of cooler air, contrary to the normal temperature decrease with altitude.
how did earths atmosphere form?
Volcanic outgassing
what are the most common gasses in the atmosphere
Nitrogen, oxygen, argon
what are some examples of variable atmospheric gasses?
water, carbon dioxide (CO2), methane
Forms of heat transfer
1. Radiation
Temperature inversions
caused by cold, clear, winter nights with calm air when the land does not radiate energy to the lower layers of atmosphere.
Wind
caused by differences in temperature, pressure and density of air
Humidity
is the amount of water vapor in the atmosphere at a given location on Earth's surface.
relative humidity
the % of water vapor in the air relative to the amount needed for 100% saturation
Dew point
the temperature to which air must be cooled at constant pressure to reach full saturation in the atmosphere & condense
latent heat
the extra thermal energy contained in a unit of water vapor compared to its liquid water form.
adiabatic process
An air mass can change temperature without being heated or cooled
Stable air
when a rising air mass cools and sinks back to a level of the same atmospheric density. (Fair weather clouds)
unstable air
occurs when the surrounding air cools faster than the warm rising air mass. (Thunderstorms)
convective lifting
cloud forming when moist air rises expands and cools
Orographic lifting
an air mass is forced to move up over a mountain. as the air rises, it cools reaching dew point and condensing into clouds/precipitation
Convergence
two air masses run into each other, forcing each other upward
nacreous clouds
form at high altitudes(stratosphere) over poles.
noctilucent clouds
form in mesophere in polar regions
meteorology
study of atmospheric phenomina.
weather vs climate
weather = short term
climate = avg over at least 30 yrs
air mass
large body of air that has same characteristics as the source region
front
a collision between two air masses, creating dramatic weather changes
cold front
occurs when dense cold air displaces warm air going under.
warm front
occurs when warm air displaces cold air and can cause light rain
occluded front
when a cold air mass moves rapidly lifting up a warm air mass and makes contact with another cold air mass in front of it. usually heavy storms as a result
stationary front
occurs when cold and warm air masses come into contact but neither advance and the front stalls. generally fair weather as result
climate
climate is a long term average of variations in weather for a particular area.