GEOG 103 Midterm

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91 Terms

1
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what are weather and climate results of

Atmospheric pressure gradients and energy imbalances.

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what is Wein’s Law

The principle stating that peak emission wavelength is inversely proportional to absolute temperature (λmax∝1T\lambda_{\text{max}} \propto \frac{1}{T}).

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how far is the Ionosphere & what does it absorb

Extends outward from 80 km80\,\text{km}; absorbs X-rays, gamma rays, and short UV radiation.

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how far out is the Ozonoshere & what is its function

19–50 km19\text{--}50\,\text{km}; absorbs harmful UV rays via ozone (O3O_3) and converts them to heat.

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what is the Atmospheric composition mainly consist of

78%78\% Nitrogen (N2N_2) and 21%21\% Oxygen (O2O_2), making up 99%99\% of atmospheric gases.

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does a negative or positive feedback work in a self regulating manner

Negative feedback (stabilizes systems by counteracting change; positive feedback amplifies change).

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What is the tropospheres atmospheric profile

Surface to 8–15 km8\text{--}15\,\text{km}; temperature decreases with height; site of active weather.

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what is the atmospheric profile of the Stratosphere

15–50 km15\text{--}50\,\text{km}; temperature increases with altitude due to UV absorption by O3O_3.

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What is the atmospheric profile of the Mesosphere

50–85 km50\text{--}85\,\text{km}; coldest atmospheric layer; temperature decreases with altitude; site of meteor burnout.

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what is the atmospheric profile of Thermosphere

85–600 km85\text{--}600\,\text{km}; temperature rises sharply with altitude; contains auroras in extremely low-density air.

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what are the three ways energy is transferred

  1. Radiation

  2. Sensible heat

  3. Latent heat


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what is radiation in heat

Thermal energy transfer via electromagnetic waves requiring no intervening medium.

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what is sensible heat

Heat that causes a measurable temperature change without altering the phase of a substance.

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What Is Latent Heat

Heat absorbed or released during a phase change at constant temperature.

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What is the Meridional Energy Flux

Equator-to-pole transfer of heat via oceanic and atmospheric circulation.

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what are the 4 Principle controls on temperature

  1. Latitude

  2. Altitude/elevation

  3. Cloud cover

  4. Land-water heating contrasts


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what are the 4 reasons the climate changes

  1. Solar cycles

  2. Milankovitch cycles

  3. Atmospheric composition changes

  4. Plate tectonics


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what are solar activity cycles

Periodic fluctuations in solar irradiance driven by sunspots, flares, and solar magnetism.

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What are Milankovitch Cycles

Cyclical variations in Earth's orbit, axial tilt, and precession driving long-term climate shifts.

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what is the source of carbon Dioxide in our atmosphere

Respiration, organic decomposition, volcanism, and fossil fuel combustion.

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What is the sink for Carbon dioxide in our atmosphere

Photosynthesis (biomass), oceanic dissolution, and geologic carbonate burial.

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how do green house gasses increase our planets surface temperature

By absorbing and re-radiating outgoing terrestrial infrared radiation back toward Earth's surface.

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what is the source for methane in our atmosphere

Wetlands, livestock digestion, landfills, termite activity, and fossil fuel extraction.

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what are the sinks for methane in our atmosphere

Oxidation by atmospheric hydroxyl radicals (OHOH) and uptake by soil microorganisms.

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what are the source of aerosols in our atmosphere

Volcanoes, sea spray, windblown dust, industrial emissions, and biomass burning.

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what is the sink for aerosols in our atmosphere

Wet deposition (precipitation scavenging) and dry gravitational sedimentation.

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what are climate variability events

Short- to medium-term regional and global climate deviations (e.g., ENSO: El Niño and La Niña).

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8 main geographic factors that influence climate

  1. Latitude

  2. Altitude

  3. Air masses

  4. Ocean currents

  5. Land-sea distribution

  6. Pressure cells

  7. Mountain barriers

  8. Prevailing winds


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what are air mass influences

Weather alterations brought by large bodies of air carrying distinct temperature and moisture profiles.

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what are global high and low pressure zones

Pressure belts where highs generate clear, dry conditions and lows drive cloudiness and precipitation.

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what are prevailing winds

Dominant regional winds that transport heat, moisture, and air masses globally.

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What is a Isobar

A weather map isoline connecting points of equal atmospheric pressure.

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what is A on the KÖppen Geiger system

Tropical Moist

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what is B on the KÖppen Geiger system

Dry

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what is C on the KÖppen Geiger system

Moist Subtropical Mid-Latitude

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what is D on the KÖppen Geiger system

Moist Continental Mid-Latitude

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what is E on the KÖppen Geiger system

Polar

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what is Primary Circulation

Global wind belts driven by differential solar heating and Earth's rotation.

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what is secondary circulation

Migratory synoptic systems, such as cyclones and anticyclones.

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What is Tertiary circulation

Localized, temporary wind patterns and mesoscale breezes.

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what is wind

Moving air characterized as a vector having both velocity (magnitude) and direction.

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what are the 4 driving forces of wind

  1. Gravity

  2. Pressure gradient force

  3. Coriolis force

  4. Friction


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what is pressure gradient force

The fundamental force driving air directly from high to low pressure.

44
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what is the Coriolis force

An apparent deflective force on moving fluids caused by Earth's planetary rotation.

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which way does the Coriolis force act win the northern hemisphere

To the right of the path of motion (clockwise deflection).

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which way does the Coriolis force act in the southern hemisphere

To the left of the path of motion (counterclockwise deflection).

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what is Geostrophic wind

Upper-level wind flowing parallel to straight isobars where Coriolis balances pressure gradient force.

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what is a cyclone

A low-pressure system with convergent, inward-spiraling winds and stormy conditions.

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what is an anti cyclone

A high-pressure system with divergent, outward-spiraling winds and clear, stable weather.

50
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convergence of air towards the centre of a low pressure region at the surface results in

Vertical ascent (upward motion).

51
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Divergence of air from the centre of a high pressure region at the surface results in

Subsidence (downward motion).

52
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what are the 4 surface circulation patterns

  1. Doldrums (ITCZ)

  2. Trade winds

  3. Horse latitudes

  4. Prevailing westerlies


53
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what are the circulation patterns in the upper atmosphere

Jet streams

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what is an Adiabatic temperature change

Internal temperature change via compression or expansion without heat exchange.

55
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what is Orographic uplift

Forced mechanical ascent of air masses over elevated topography.

56
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what is Orographic precipitation

Precipitation produced when moisture cools and condenses as it rises over mountains.

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what is Frontal Precipitation

Precipitation triggered when contrasting air masses collide and the warmer air is forced aloft.

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advancing cold front characteristics

Steep frontal slope, rapid warm air displacement, and intense convective storms.

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An advancing warmfront characteristics

Gentle frontal slope, warm air gliding over cold air, and widespread, steady stratiform rain.

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what is Convergent precipitation

Rainfall caused by converging low-level horizontal airflows forcing vertical uplift.

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what is Convective precipitation

Rainfall caused by rapid thermal buoyancy of heated, moist air producing cumulus clouds.

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3 main types of storms

  1. Extratropical (mid-latitude) cyclones

  2. Tropical cyclones

  3. Mesoscale convective systems


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what is an extratropical cyclone

A frontal, mid-latitude low-pressure storm system driven by horizontal temperature contrasts.

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what are tropical storms

Organized, rotating maritime convective systems fueled by latent heat over warm seas.

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what are hurricanes

Intense tropical cyclones featuring a non-frontal warm core, low central pressure, and an eyewall.

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what are miso-scale convective storms

Organized thunderstorm complexes sustained by latent heat release that produce severe localized weather.

67
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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.

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how is water distributed around the world

Oceans (≈97%\approx 97\%), ice caps/glaciers (≈2%\approx 2\%), and freshwater reservoirs (<1%< 1\%).

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how is water stored around the world

Within reservoirs: oceans, ice sheets, groundwater aquifers, surface water, and the atmosphere.

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order the gases in our atmosphere from greatest to least

  1. Nitrogen

  2. Carbon dioxide

  3. Methane

  4. Oxygen

  5. Water Vapour


71
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heat transfer through electro magnetic waves is called

radiation

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Heat transfer through a flowing medium (like air or ocean currents) is called

Convection

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Molecule to molecule heat transfer for molecules in direct contact to each other

Conduction

74
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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.

75
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Weins law states

the colder an object, the longer the peak wavelength of emitted radiation.

76
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most of the worlds precipitation and evaporation happens

Over the oceans

77
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what are stream discharge patterns determined by

  1. Slope

  2. erodibility or resistance of Bedrock

  3. jointing, folding and faulting of bedrock


78
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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.

79
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direction of airflow in a cyclone

air moves towards the center

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direction of airflow in an anticyclone

away from the center

81
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is a cyclone low or high pressure

Low-pressure

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is an anti cyclone high or low pressure

high-pressure

83
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what is interflow

Lateral subsurface movement of water through the soil layer.

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What is Surface runoff

Flow of excess water over the land surface toward water bodies.

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what is base flow

The portion of streamflow that comes from groundwater seepage into the stream, typically during dry periods.

86
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area of convergence of polar and tropical air masses

Polar Front

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NE or SE winds form subtropical highs to the ITCZ

Trade winds

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region of low winds and high temperature in equatorial regions

Doldrums

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westerlies

Strong winds originating in the subtropical highs and flowing towards the poles

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is Coriolis force stronger or weaker at higher latitudes

the Coriolis force is stronger at higher latitudes it has little effect at the equator

91
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which ocean basin receives the highest percentage of total global river discharge

the Pacific