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what are weather and climate results of
Atmospheric pressure gradients and energy imbalances.
what is Wein’s Law
The principle stating that peak emission wavelength is inversely proportional to absolute temperature (λmax∝T1).
how far is the Ionosphere & what does it absorb
Extends outward from 80km; absorbs X-rays, gamma rays, and short UV radiation.
how far out is the Ozonoshere & what is its function
19–50km; absorbs harmful UV rays via ozone (O3) and converts them to heat.
what is the Atmospheric composition mainly consist of
78% Nitrogen (N2) and 21% Oxygen (O2), making up 99% of atmospheric gases.
does a negative or positive feedback work in a self regulating manner
Negative feedback (stabilizes systems by counteracting change; positive feedback amplifies change).
What is the tropospheres atmospheric profile
Surface to 8–15km; temperature decreases with height; site of active weather.
what is the atmospheric profile of the Stratosphere
15–50km; temperature increases with altitude due to UV absorption by O3.
What is the atmospheric profile of the Mesosphere
50–85km; coldest atmospheric layer; temperature decreases with altitude; site of meteor burnout.
what is the atmospheric profile of Thermosphere
85–600km; temperature rises sharply with altitude; contains auroras in extremely low-density air.
what are the three ways energy is transferred
Radiation
Sensible heat
Latent heat
what is radiation in heat
Thermal energy transfer via electromagnetic waves requiring no intervening medium.
what is sensible heat
Heat that causes a measurable temperature change without altering the phase of a substance.
What Is Latent Heat
Heat absorbed or released during a phase change at constant temperature.
What is the Meridional Energy Flux
Equator-to-pole transfer of heat via oceanic and atmospheric circulation.
what are the 4 Principle controls on temperature
Latitude
Altitude/elevation
Cloud cover
Land-water heating contrasts
what are the 4 reasons the climate changes
Solar cycles
Milankovitch cycles
Atmospheric composition changes
Plate tectonics
what are solar activity cycles
Periodic fluctuations in solar irradiance driven by sunspots, flares, and solar magnetism.
What are Milankovitch Cycles
Cyclical variations in Earth's orbit, axial tilt, and precession driving long-term climate shifts.
what is the source of carbon Dioxide in our atmosphere
Respiration, organic decomposition, volcanism, and fossil fuel combustion.
What is the sink for Carbon dioxide in our atmosphere
Photosynthesis (biomass), oceanic dissolution, and geologic carbonate burial.
how do green house gasses increase our planets surface temperature
By absorbing and re-radiating outgoing terrestrial infrared radiation back toward Earth's surface.
what is the source for methane in our atmosphere
Wetlands, livestock digestion, landfills, termite activity, and fossil fuel extraction.
what are the sinks for methane in our atmosphere
Oxidation by atmospheric hydroxyl radicals (OH) and uptake by soil microorganisms.
what are the source of aerosols in our atmosphere
Volcanoes, sea spray, windblown dust, industrial emissions, and biomass burning.
what is the sink for aerosols in our atmosphere
Wet deposition (precipitation scavenging) and dry gravitational sedimentation.
what are climate variability events
Short- to medium-term regional and global climate deviations (e.g., ENSO: El Niño and La Niña).
8 main geographic factors that influence climate
Latitude
Altitude
Air masses
Ocean currents
Land-sea distribution
Pressure cells
Mountain barriers
Prevailing winds
what are air mass influences
Weather alterations brought by large bodies of air carrying distinct temperature and moisture profiles.
what are global high and low pressure zones
Pressure belts where highs generate clear, dry conditions and lows drive cloudiness and precipitation.
what are prevailing winds
Dominant regional winds that transport heat, moisture, and air masses globally.
What is a Isobar
A weather map isoline connecting points of equal atmospheric pressure.
what is A on the KÖppen Geiger system
Tropical Moist
what is B on the KÖppen Geiger system
Dry
what is C on the KÖppen Geiger system
Moist Subtropical Mid-Latitude
what is D on the KÖppen Geiger system
Moist Continental Mid-Latitude
what is E on the KÖppen Geiger system
Polar
what is Primary Circulation
Global wind belts driven by differential solar heating and Earth's rotation.
what is secondary circulation
Migratory synoptic systems, such as cyclones and anticyclones.
What is Tertiary circulation
Localized, temporary wind patterns and mesoscale breezes.
what is wind
Moving air characterized as a vector having both velocity (magnitude) and direction.
what are the 4 driving forces of wind
Gravity
Pressure gradient force
Coriolis force
Friction
what is pressure gradient force
The fundamental force driving air directly from high to low pressure.
what is the Coriolis force
An apparent deflective force on moving fluids caused by Earth's planetary rotation.
which way does the Coriolis force act win the northern hemisphere
To the right of the path of motion (clockwise deflection).
which way does the Coriolis force act in the southern hemisphere
To the left of the path of motion (counterclockwise deflection).
what is Geostrophic wind
Upper-level wind flowing parallel to straight isobars where Coriolis balances pressure gradient force.
what is a cyclone
A low-pressure system with convergent, inward-spiraling winds and stormy conditions.
what is an anti cyclone
A high-pressure system with divergent, outward-spiraling winds and clear, stable weather.
convergence of air towards the centre of a low pressure region at the surface results in
Vertical ascent (upward motion).
Divergence of air from the centre of a high pressure region at the surface results in
Subsidence (downward motion).
what are the 4 surface circulation patterns
Doldrums (ITCZ)
Trade winds
Horse latitudes
Prevailing westerlies
what are the circulation patterns in the upper atmosphere
Jet streams
what is an Adiabatic temperature change
Internal temperature change via compression or expansion without heat exchange.
what is Orographic uplift
Forced mechanical ascent of air masses over elevated topography.
what is Orographic precipitation
Precipitation produced when moisture cools and condenses as it rises over mountains.
what is Frontal Precipitation
Precipitation triggered when contrasting air masses collide and the warmer air is forced aloft.
advancing cold front characteristics
Steep frontal slope, rapid warm air displacement, and intense convective storms.
An advancing warmfront characteristics
Gentle frontal slope, warm air gliding over cold air, and widespread, steady stratiform rain.
what is Convergent precipitation
Rainfall caused by converging low-level horizontal airflows forcing vertical uplift.
what is Convective precipitation
Rainfall caused by rapid thermal buoyancy of heated, moist air producing cumulus clouds.
3 main types of storms
Extratropical (mid-latitude) cyclones
Tropical cyclones
Mesoscale convective systems
what is an extratropical cyclone
A frontal, mid-latitude low-pressure storm system driven by horizontal temperature contrasts.
what are tropical storms
Organized, rotating maritime convective systems fueled by latent heat over warm seas.
what are hurricanes
Intense tropical cyclones featuring a non-frontal warm core, low central pressure, and an eyewall.
what are miso-scale convective storms
Organized thunderstorm complexes sustained by latent heat release that produce severe localized weather.
what are specific traits to the three individual phases of water
Ice: rigid, crystalline, lowest density; Liquid: fluid, high specific heat; Gas: highly expansive, lowest density.
how is water distributed around the world
Oceans (≈97%), ice caps/glaciers (≈2%), and freshwater reservoirs (<1%).
how is water stored around the world
Within reservoirs: oceans, ice sheets, groundwater aquifers, surface water, and the atmosphere.
order the gases in our atmosphere from greatest to least
Nitrogen
Carbon dioxide
Methane
Oxygen
Water Vapour
heat transfer through electro magnetic waves is called
radiation
Heat transfer through a flowing medium (like air or ocean currents) is called
Convection
Molecule to molecule heat transfer for molecules in direct contact to each other
Conduction
what is a dynamic equilibrium
A dynamic equilibrium is a state in which opposing forces or influences are balanced, resulting in no net change in a system over time, even though processes are continuously occurring.
Weins law states
the colder an object, the longer the peak wavelength of emitted radiation.
most of the worlds precipitation and evaporation happens
Over the oceans
what are stream discharge patterns determined by
Slope
erodibility or resistance of Bedrock
jointing, folding and faulting of bedrock
what is the ITCZ
The Intertropical Convergence Zone (ITCZ) is a region near the equator where trade winds from both hemispheres meet, resulting in heavy precipitation and cloud formation.
direction of airflow in a cyclone
air moves towards the center
direction of airflow in an anticyclone
away from the center
is a cyclone low or high pressure
Low-pressure
is an anti cyclone high or low pressure
high-pressure
what is interflow
Lateral subsurface movement of water through the soil layer.
What is Surface runoff
Flow of excess water over the land surface toward water bodies.
what is base flow
The portion of streamflow that comes from groundwater seepage into the stream, typically during dry periods.
area of convergence of polar and tropical air masses
Polar Front
NE or SE winds form subtropical highs to the ITCZ
Trade winds
region of low winds and high temperature in equatorial regions
Doldrums
westerlies
Strong winds originating in the subtropical highs and flowing towards the poles
is Coriolis force stronger or weaker at higher latitudes
the Coriolis force is stronger at higher latitudes it has little effect at the equator
which ocean basin receives the highest percentage of total global river discharge
the Pacific