Podcast
Questions and Answers
Along a coastline impacted by a hurricane, what synergistic effect amplifies the severity of damage beyond inundation from intense precipitation alone?
Along a coastline impacted by a hurricane, what synergistic effect amplifies the severity of damage beyond inundation from intense precipitation alone?
- The convergence of pre-existing coastal storm systems with the cyclonic circulation, resulting in compound flooding scenarios.
- Localized orographic lift augmenting convective precipitation cells, leading to hyper-localized flash flooding events inland.
- The dynamic interaction of storm surge with astronomical tides and subsequent wave action, exacerbating coastal erosion and infrastructure damage. (correct)
- Intensified electrostatic discharge (lightning) causing ignition of submerged methane hydrates, leading to localized explosions exacerbating structural failures.
Beyond minimal vertical wind shear and sufficient Coriolis force, which critical thermodynamic ingredient, modulated by complex ocean-atmosphere coupling, is indispensable for sustaining and intensifying a tropical cyclone?
Beyond minimal vertical wind shear and sufficient Coriolis force, which critical thermodynamic ingredient, modulated by complex ocean-atmosphere coupling, is indispensable for sustaining and intensifying a tropical cyclone?
- A pre-existing mesoscale convective vortex (MCV) exhibiting robust quasi-geostrophic forcing and upward vertical motion.
- The presence of a deep, highly baroclinic zone characterized by a rapid horizontal temperature gradient propagating from the mid-latitudes.
- An anomalously steep geopotential height gradient within the upper troposphere, fostering enhanced ventilation of the storm's outflow layer.
- Elevated sea surface temperatures coupled with a deep oceanic mixed layer, providing a sustained source of enthalpy flux to fuel the storm's convective engine. (correct)
Quantitatively assessing continental runoff partitioning within the hydrological cycle, how does surface overland flow compare to subsurface groundwater discharge regarding total flux into oceanic reservoirs?
Quantitatively assessing continental runoff partitioning within the hydrological cycle, how does surface overland flow compare to subsurface groundwater discharge regarding total flux into oceanic reservoirs?
- Overland flow and groundwater discharge share a near 1:1 ratio (approximately 50:50) stemming from equilibrium infiltration capacities.
- Overland flow significantly exceeds groundwater discharge (approximately 75%) because of limited vadose zone storage capacity. (correct)
- Overland flow vastly dominates (approximately 95%) due to the impermeable nature of most continental lithologies.
- Groundwater discharge constitutes the majority (approximately 70%) owing to its sustained contribution during inter-storm periods.
Concerning water budget analysis, identify the segment within the presented hydrograph (PET = potential evapotranspiration, AE = actual evapotranspiration, P = precipitation) indicative of soil moisture depletion under conditions where AE persistently lags behind PET.
Concerning water budget analysis, identify the segment within the presented hydrograph (PET = potential evapotranspiration, AE = actual evapotranspiration, P = precipitation) indicative of soil moisture depletion under conditions where AE persistently lags behind PET.
How does the principle of continentality manifest in annual temperature range disparities, specifically contrasting coastal proximity effects against interior continental locations while accounting for advection and specific heat capacity?
How does the principle of continentality manifest in annual temperature range disparities, specifically contrasting coastal proximity effects against interior continental locations while accounting for advection and specific heat capacity?
In alpine glacial geomorphology, differentiate between the formation mechanisms of lateral moraines and terminal moraines, emphasizing source material entrainment, transport processes, and depositional contexts.
In alpine glacial geomorphology, differentiate between the formation mechanisms of lateral moraines and terminal moraines, emphasizing source material entrainment, transport processes, and depositional contexts.
How do synclines impact the hydrological characteristics of a landscape, especially regarding groundwater flow patterns, susceptibility to erosion, and the potential formation of artesian systems compared to other geological structures?
How do synclines impact the hydrological characteristics of a landscape, especially regarding groundwater flow patterns, susceptibility to erosion, and the potential formation of artesian systems compared to other geological structures?
Delineate the complex atmospheric dynamics underpinning sea breeze circulation, incorporating roles of differential heating, thermal pressure gradients, Coriolis effects, and the varying influence of synoptic-scale pressure systems.
Delineate the complex atmospheric dynamics underpinning sea breeze circulation, incorporating roles of differential heating, thermal pressure gradients, Coriolis effects, and the varying influence of synoptic-scale pressure systems.
Decipher the intricate relationship between upper-tropospheric jet stream dynamics and the cyclogenesis stage of mid-latitude cyclones, elucidating the impact of zones of convergence and divergence located downstream from the polar front.
Decipher the intricate relationship between upper-tropospheric jet stream dynamics and the cyclogenesis stage of mid-latitude cyclones, elucidating the impact of zones of convergence and divergence located downstream from the polar front.
In the context of volcanic eruptions, differentiate between effusive and explosive styles, linking magma viscosity, gas content, effusion rates, and pyroclastic processes to specific volcano morphologies.
In the context of volcanic eruptions, differentiate between effusive and explosive styles, linking magma viscosity, gas content, effusion rates, and pyroclastic processes to specific volcano morphologies.
Deconstruct the hydrodynamics of sediment transport around coastal structures, particularly jetties, incorporating concepts of wave diffraction, longshore currents, sediment budget, and the equilibrium shoreline profile.
Deconstruct the hydrodynamics of sediment transport around coastal structures, particularly jetties, incorporating concepts of wave diffraction, longshore currents, sediment budget, and the equilibrium shoreline profile.
Dissect the process of wave-cut platform formation, integrating considerations of eustatic sea-level changes, isostatic adjustments, differential weathering, abrasion rates, bioerosion activity, and sediment transport dynamics.
Dissect the process of wave-cut platform formation, integrating considerations of eustatic sea-level changes, isostatic adjustments, differential weathering, abrasion rates, bioerosion activity, and sediment transport dynamics.
Using thermodynamic principles and the Clausius-Clapeyron relation, evaluate the theoretical dew point temperature of an air parcel with a specific humidity of 20 g/kg, referencing an idealized saturation specific humidity chart and considering the effects of atmospheric pressure and hygroscopic aerosol loading.
Using thermodynamic principles and the Clausius-Clapeyron relation, evaluate the theoretical dew point temperature of an air parcel with a specific humidity of 20 g/kg, referencing an idealized saturation specific humidity chart and considering the effects of atmospheric pressure and hygroscopic aerosol loading.
Given an air parcel at 20°C with a specific humidity of 5 g/kg, determine its relative humidity utilizing a psychrometric chart, explicitly accounting for potential hygroscopic influences from aerosol within the boundary layer inversion.
Given an air parcel at 20°C with a specific humidity of 5 g/kg, determine its relative humidity utilizing a psychrometric chart, explicitly accounting for potential hygroscopic influences from aerosol within the boundary layer inversion.
Assess the vertical distribution of atmospheric pressure, taking into account hydrostatic equilibrium, the ideal gas law, and gravitational acceleration in deriving a mathematical relationship that explains observed pressure gradients influenced by heterogeneities from temperature and composition.
Assess the vertical distribution of atmospheric pressure, taking into account hydrostatic equilibrium, the ideal gas law, and gravitational acceleration in deriving a mathematical relationship that explains observed pressure gradients influenced by heterogeneities from temperature and composition.
Within a convective boundary layer undergoing diurnal heating, deduce those atmospheric stratification conditions most conducive to the formation of intense summer thunderstorms, accounting factors such as capping inversions, entrainment zones, and conditional instability parameters.
Within a convective boundary layer undergoing diurnal heating, deduce those atmospheric stratification conditions most conducive to the formation of intense summer thunderstorms, accounting factors such as capping inversions, entrainment zones, and conditional instability parameters.
Given the principles governing atmospheric saturation, articulate the most energetically efficient mechanism by which air reaches saturation, inducing condensate phase transition phenomena leading to precipitation formation across diverse meteorological regimes.
Given the principles governing atmospheric saturation, articulate the most energetically efficient mechanism by which air reaches saturation, inducing condensate phase transition phenomena leading to precipitation formation across diverse meteorological regimes.
Considering the surface radiative budget and solar geometry, analyze the impact of variations in Sun angle contingent on latitudinal position regarding incident energy intensity, atmospheric path length, and planetary albedo response across differing surface types.
Considering the surface radiative budget and solar geometry, analyze the impact of variations in Sun angle contingent on latitudinal position regarding incident energy intensity, atmospheric path length, and planetary albedo response across differing surface types.
Within earth's radiative balance model, critique the diverse impacts of cloud cover regimes on net surface temperature, contrasting both shortwave albedo effects with longwave greenhouse influences and quantifying feedbacks from cloud microphysics and atmospheric convection.
Within earth's radiative balance model, critique the diverse impacts of cloud cover regimes on net surface temperature, contrasting both shortwave albedo effects with longwave greenhouse influences and quantifying feedbacks from cloud microphysics and atmospheric convection.
Considering the influence of seasonal temperature gradients and the conservation of angular momentum, analyze how the latitudinal position and intensity of the Northern Hemisphere jet stream fluctuate during winter, particularly in proximity to the polar front.
Considering the influence of seasonal temperature gradients and the conservation of angular momentum, analyze how the latitudinal position and intensity of the Northern Hemisphere jet stream fluctuate during winter, particularly in proximity to the polar front.
Delineate the surface pressure features governing atmospheric circulation surrounding the equator within the three-cell model, considering factors such as Coriolis effects, Hadley cell dynamics, and resulting precipitation patterns.
Delineate the surface pressure features governing atmospheric circulation surrounding the equator within the three-cell model, considering factors such as Coriolis effects, Hadley cell dynamics, and resulting precipitation patterns.
With respect to adiabatic processes in Earth's troposphere, describe temperature variations governed by air parcel ascent, explicitly incorporating countervailing effects of moisture content, latent heat exchange, and boundary layer mixing dynamics.
With respect to adiabatic processes in Earth's troposphere, describe temperature variations governed by air parcel ascent, explicitly incorporating countervailing effects of moisture content, latent heat exchange, and boundary layer mixing dynamics.
Infer potential upper-level tropospheric wind direction based on given geographic location, employing geostrophic wind principles, isobaric spatial configurations, and accounting for influences from thermal wind and orographic forcing.
Infer potential upper-level tropospheric wind direction based on given geographic location, employing geostrophic wind principles, isobaric spatial configurations, and accounting for influences from thermal wind and orographic forcing.
Characterize texture traits exhibited by intrusive igneous rocks, linking those traits mechanistically to magma cooling history, crustal emplacement depths, mineral nucleation dynamics, and crystal growth kinetics described under Bowen's reaction series.
Characterize texture traits exhibited by intrusive igneous rocks, linking those traits mechanistically to magma cooling history, crustal emplacement depths, mineral nucleation dynamics, and crystal growth kinetics described under Bowen's reaction series.
Relate the hydrologic function and material composition of an aquifer to relevant lithologic properties and hydrogeologic principles.
Relate the hydrologic function and material composition of an aquifer to relevant lithologic properties and hydrogeologic principles.
Quantify the depth-dependence of oscillatory water motion generated by surface waves, integrating deep-water wave theory and relating vertical attenuation of orbital diameter exponentially with respect to wavelength.
Quantify the depth-dependence of oscillatory water motion generated by surface waves, integrating deep-water wave theory and relating vertical attenuation of orbital diameter exponentially with respect to wavelength.
In alpine glacial geomorphology, synthesize the geomorphic processes underpinning cirque formation, involving nivation, frost shattering, abrasion, and glacial plucking acting on pre-existing bedrock weaknesses. Consider slope aspect on insolation and rates of chemical weathering.
In alpine glacial geomorphology, synthesize the geomorphic processes underpinning cirque formation, involving nivation, frost shattering, abrasion, and glacial plucking acting on pre-existing bedrock weaknesses. Consider slope aspect on insolation and rates of chemical weathering.
In fluvial geomorphology, relate point bar formation along meandering river reaches to secondary circulation cells, sediment transport rates, flow separation zones, bank erosion dynamics, and the concept of dynamic equilibrium.
In fluvial geomorphology, relate point bar formation along meandering river reaches to secondary circulation cells, sediment transport rates, flow separation zones, bank erosion dynamics, and the concept of dynamic equilibrium.
Discriminate among disparate sediment transport mechanisms operating within fluvial systems, emphasizing conditions governing traction, saltation, suspension load, and dissolved load as a function of grain size, fluid shear stress, particle Reynolds number, and electrochemical interactions.
Discriminate among disparate sediment transport mechanisms operating within fluvial systems, emphasizing conditions governing traction, saltation, suspension load, and dissolved load as a function of grain size, fluid shear stress, particle Reynolds number, and electrochemical interactions.
Propose a plausible mechanism that allows permanent rock deformation without fracture.
Propose a plausible mechanism that allows permanent rock deformation without fracture.
Analyze the thermodynamics governing the formation of sleet, relating it uniquely to the tropospheric temperature profiles, ice nucleation dynamics, adiabatic processes, and latent heat exchange associated with atmospheric phase transitions.
Analyze the thermodynamics governing the formation of sleet, relating it uniquely to the tropospheric temperature profiles, ice nucleation dynamics, adiabatic processes, and latent heat exchange associated with atmospheric phase transitions.
Interpret fault plane geometry, differentiating the hanging wall from the footwall, and relate these structural components to the broader context of stress regimes and displacement histories.
Interpret fault plane geometry, differentiating the hanging wall from the footwall, and relate these structural components to the broader context of stress regimes and displacement histories.
Deconstruct the modern atmospheric composition regarding key trace gas abundancies, and identify a component that exists outside of the top three constituents.
Deconstruct the modern atmospheric composition regarding key trace gas abundancies, and identify a component that exists outside of the top three constituents.
Relate the distinctive geomorphic characteristics of drumlins to glacial processes, emphasizing till deformation mechanics, subglacial hydraulics, and the role of eskers in their formation.
Relate the distinctive geomorphic characteristics of drumlins to glacial processes, emphasizing till deformation mechanics, subglacial hydraulics, and the role of eskers in their formation.
Relate floodplain topography to fluvial channel dynamics, differentiating between primary river flows and secondary parallel flows that do not join, accounting for discharge dynamics and sediment transport capacities.
Relate floodplain topography to fluvial channel dynamics, differentiating between primary river flows and secondary parallel flows that do not join, accounting for discharge dynamics and sediment transport capacities.
Infer upper-level wind patterns and pressure gradients given surface wind directional biases, considering the convergence zones, the effects of Coriolis force, and considering the role of angular momentum.
Infer upper-level wind patterns and pressure gradients given surface wind directional biases, considering the convergence zones, the effects of Coriolis force, and considering the role of angular momentum.
Flashcards
Storm surge
Storm surge
The most significant damage along a coastline during a hurricane is usually due to this.
Little wind shear, Coriolis force, warm ocean water
Little wind shear, Coriolis force, warm ocean water
Conditions where hurricane formation is most likely.
95% overland; 5% groundwater
95% overland; 5% groundwater
Runoff distribution in the hydrologic cycle.
Area B
Area B
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Principle of Continentality
Principle of Continentality
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Lateral moraine
Lateral moraine
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Syncline
Syncline
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Sea breeze
Sea breeze
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Below divergence
Below divergence
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Effusive eruption
Effusive eruption
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Jetty
Jetty
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Wave-cut platform
Wave-cut platform
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33%
33%
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Decreases with height
Decreases with height
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Humid and unstable
Humid and unstable
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Cool air by lifting it
Cool air by lifting it
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Solar angle and day length
Solar angle and day length
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Above, stronger and south
Above, stronger and south
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Equatorial Low
Equatorial Low
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Decreases with height
Decreases with height
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Northeast
Northeast
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Intrusive
Intrusive
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Aquifer
Aquifer
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One-half the wavelength
One-half the wavelength
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Cirque
Cirque
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Point bar
Point bar
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Traction
Traction
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Plastic deformation
Plastic deformation
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Sleet
Sleet
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Footwall
Footwall
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Drumlin
Drumlin
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Yazoo tributary
Yazoo tributary
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Polar easterlies
Polar easterlies
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Descending air
Descending air
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3
3
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4
4
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Liquefaction
Liquefaction
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Latent heat
Latent heat
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Study Notes
- The most significant hurricane damage along a coastline is generally due to storm surge
- Hurricane formation is most likely where there is little wind shear, some Coriolis force to provide spin, and warm ocean water to provide energy
- In the hydrologic cycle, runoff from continent to ocean is about 95% overland and about 5% through groundwater
- In a water budget graph, the area between the potential evapotranspiration and actual evapotranspiration curves refers to a period of soil moisture withdrawal
- According to the Principle of Continentality, coastal locations have smaller annual and daily temperature ranges than inland locations
- A lateral moraine will form parallel to the glacier along the edge of the ice mass
- A folded feature that resembles a dip or trough in the rock layers is called a syncline
- Along a coast, when the inland area warms up during the day, there is likely to be a sea breeze
- A mid-latitude cyclone will form along the polar front, below a region of divergence in the jet stream
- An effusive type of eruption will tend to build shield volcanoes
- A coastal structure that is built to protect the mouth of a harbor, which extends out from the coast to interrupt sediment movement, is a jetty
- A flat surface formed by erosion at sea level, which may be covered by water at high tide and fully exposed at low tide, is a wave-cut platform
EC Practice Quiz 02
- Using the saturation specific humidity chart, the dew point of a parcel of air with a measured specific humidity of 20 g/kg, is 25° C
- The relative humidity of a parcel of air at a temperature of 20° C and a measured specific humidity of 5 g/kg is 33%
- Atmospheric pressure is highest at the surface and decreases with elevation
- Both air mass thunderstorms are most likely to form when the lower troposphere is humid and unstable
- To get condensation(cloud and rain drops), the air must be saturated, cooling the air by lifting is the way to produce rain
- In terms of surface temperature and energy, latitude is important because solar energy hits the surface less directly at higher latitudes (latitude determines the sun angle)
- In terms of surface temperature, clouds might cool the surface by reflecting sunlight, warm the surface by absorbing longwave radiation and re-radiating energy downward, and decrease the diurnal temperature range
- In the Northern Hemisphere, the jet stream is found above the polar front and is stronger and shifted south during the winter
- In the three-cell model of global circulation, the dominant surface pressure feature near the Equator is the Equatorial Low
- In the troposphere, temperature decreases the higher you go
EC Practice Quiz 03
- In Figure 2, upper level divergence is most likely occurring at point C
- In Figure 2, the upper-level winds at Point A is blowing from the northeast
- An igneous rock that cools and solidifies below ground and will usually have a texture characterized by intrusive; large crystals (coarse grain)
- An underground formation of rock, sand, or gravel that contains water is An aquifer
- As an ocean wave travels through the water, the movement of water molecules due to the passages of the wave is detectable down to a depth of approximately one-half the wavelength
- In an alpine glacial environment, a cirque is formed when ice erodes a bowl-shaped depression in the mountainside, near the upper part of the mountain glacier
- In a river meander, the depositional feature that forms on the inside of the curve is called a point bar
- In a stream, the form of transportation in which particles are rolled or slid along the bottom is traction
- Stress applied to a block of crust involves a permanent deformation of the rock, but not an actual break involving plastic (ductile) deformation
- When a falling precipitate particle melts into liquid, then refreezes into solid ice before hitting the ground, it is a form of precipitation that is referred to as sleet
- When a fault plane dips down below the Earth's surface at an angle other than vertical, the side of the fault, that is underneath the other is known as the footwall
- Carbon dioxide is NOT one of the three largest constituents of the atmosphere
EC Practice Quiz 04
- A tapered, elongated hill formed when a continental ice sheet deposits and rearranges sediment is a drumlin
- In a floodplain, a secondary river flowing parallel to the main river but not joining it is a yazoo tributary
- In the figure, the band of winds labeled H is the Polar easterlies
- The figure below is a surface high pressure feature produced dynamically by sinking air
Weekly Quiz 01
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If the concentration of a gas in the atmosphere significantly changes from season to season or from place to place, then variable gas concludes that this is a variable gas
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The Earth makes its closest annual approach to the sun on January 4, the date of perihelion
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The most common gas in the Earth's atmosphere is nitrogen
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The ozone layer is located in the stratosphere
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When the sun angle is low, the intensity of radiation arriving at the surface will be reduced because the radiation is spread out over a larger area when it hits obliquely., and the longer path diagonally down through the atmosphere means more of the energy is prevented from reaching the surface
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The latitudes that will have the largest seasonal range of day length are 75° S
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At the Tropic of Capricorn, on 1 day per year, the sun will be directly overhead at solar noon
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Two layers of the atmosphere are characterized by inversions, which is the thermosphere and the stratosphere
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The atmosphere is most dense near the surface because it is cooler in the lower layers, and the density increases(a basis gas law)
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100 mb is the pressure level will be found farthest above the Earth's surface
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The four basic spheres of physical geography refers to the upper layers of the solid planet (i.e., the rock and landforms of the Earth's surface) is the lithosphere
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The Earth is warmer in summer than in winter because the Earth's tilt allows the sun's rays to hit more directly
Weekly Quiz 02/3
- According to the Principle of Continentality, an inland location has higher seasonal temperature variability than a coastal site at the same latitude
- Deserts tend to be hot during the day and cool at night because during the day, most surplus energy goes into sensible heating of the atmosphere, and at night, the lack of clouds and water vapor allows longwave energy to escape easily
- In the local radiation balance, clouds may cool the surface by reflecting incoming solar radiation, warm the surface by absorbing/trapping outgoing longwave radiation and decrease the diurnal temperature range
- The latitudinal gradient of temperature is weakest in summer because in summer, sun angles are higher the farther poleward you go
- Day lengths are always shorter as you go poleward, which does NOT help to explain why high-latitude (polar) locations are cooler than lower latitudes throughout the year
- The Earth emits most of its radiation at longer wavelengths than the sun
- The energy that is required when water evaporates, which is then released into the atmosphere when the water vapor condenses, is latent heat
- The method of energy transfer in which heat is moved by the mixing (or turbulence) of a liquid or gas is called convection
- The percentage of radiation striking an object that is reflected away is the albedo
- Carbon dioxide, methane, and water vapor are important greenhouse gases
- clouds are the largest overall contributor to the planetary albedo
- Over a wet surface, latent heat transferring energy to the atmosphere accounts for the most net radiation received during the day
Weekly Quiz 05
- Referenced by the letters on the figure, L indicates the location of the Southeasterly Trades
- When a mT air mass advances into a cP air mass, there will be a warm front
- Sinking air, you would not expect to find at the Intertropical Convergence Zone (ITCZ)
- An air mass formed over the open ocean in the Icelandic Low (North Atlantic) very likely has cool temperatures and moderate humidity
- Mid-latitude cyclones form when a low surface-pressure center develops along the polar front underneath upper-level divergence in the Polar Front Jet Stream
- During the Northern Hemisphere summer, the large-scale circulation feature that will have the most significant and direct impact on California is the Pacific (Hawaiian) High
- The Lakes are frozen over, and thus can't warm and humidify the passing air masses, is why Lake Effect snows in Buffalo get fewer in later January
- The large curves (meanders) in the flow of the upper-level westerlies are called Rossby Waves
- Referenced by the letters of the idealized Three-Cell Model, region C and D contains the Hadley Cell
- Typically, a surface anticyclone (high pressure cell) is characterized by descending air, diverging surface winds, and clear, sunny conditions
- In the northern hemisphere, the Coriolis force turns winds right and is stronger near the pole
- Santa Ana Winds are warm winds because They are warmed adiabatically by compression as they descend from higher elevations
Week 06 Quiz
- In an unconfined aquifer, the top of the zone of saturation is the water table
- In the soil column, the water that is loosely held against the pull of gravity, and thus is available to plants and evaporation, is capillary water
- Potential evapotranspiration (PET) is primarily determined by temperature
- In the water budget graph below, region B refers to a period of soil moisture withdrawal
- The oceans contain about 97% of all the water on the planet
- Hurricanes are large, cyclonically (counter-clockwise) rotating storms, with rotation source from the Coriolis Effect
- Air mass thunderstorms are short-lived because the downdrafts caused by falling rain tend to snuff out the updrafts that produced the storm.
- In a hurricane, the most severe weather will be found in the eyewall
- Tornadoes occurs most annually in the United States
- Fujita Scale is used to describe the intensity of a tornado
- When a hurricane makes landfall, the local rise in sea level results from water being pushed up against the shoreline is storm surge
- Hurricanes are most likely to form in the summer in the tropical Atlantic
Week 07 Quiz
- Slow vertical movement of the Earth’s crust, that can occur when a weight such as an ice sheet is removed, describes Isostatic rebound
- Exogenous is a geomorphic process that is driven by energy outside of the Earth system
- Both radioactive decay and collisions with other objects are the sources of partial melting to the Earth originally solid based on the nebular hypothesis
- Convergent, between two oceanic plates, describes the formation of island arcs
- Ancient, stable core of a continental landmass is the craton
- Soft or 'plastic-y' internal layer of the Earth on which the continents float describes the asthenosphere
- The type of rock that makes up oceanic crust is said to be mafic, which has high concentrations of magnesium and iron, and is relatively dense
- Middle Mantle NOT a layer of the Earth’s mantle
- Sill is an intrusive igneous structure that is tabular and concordant
- Diverging plates of the Earth, new oceanic crust is produced
- Batholith will generally cover the largest spatial extent
- Transform, is a description that fits the San Andreas Fault in California
Week 09 Quiz
- Horizontal displacement along the line of the fault describes strike-slip
- elastic deformation of rock stores the released energy in an earthquake
- A long ridge in a folded landscape is an anticline
- Seismic waves radiate out in all directions from the point where an earthquake occurs; the fastest waves are the P-waves
- Deposition around a curve in a meandering river is likely to occur on the inside of the curve, forming a point bar
- Flood deposits made up of the coarsest (heaviest) materials may form a natural levee along the edge of the overflowing river
- Saltation refers to the stream form of transportation in which particles are bounced along the bottom
- Oxbow lake results from water trapped in an altered curve of a river
- A tilted fault-block mountain or range can be found in the Sierra Nevada
- Refers to the size of the objects that the stream can maintain in transport
- Pothole is formed in a stream uses rock and gravel to abrade and scour the stream bed in times of flood
- At the fault called hanging wall, one would be crawling down into a normal fault with a dip of 45°
Week 10 Quiz
- On the east coast in the mid-latitudes, a warm current flows towards the pole
- Different parts of a wave slow down at different times producing wave refraction and concentrates energy on points and headlands
- When Earth, Sun, and Moon are in a straight line, spring tides
- Beach drift sediments are in zig-zag movement across a beach and as breaking waves swash diagonally up and down along the sand
- Esker is formed by a sediment deposit from a stream flowing along and beneath a glacier
- The water depth is less than one-half of the wavelength to begin the wave break
- Tombolo is a depositional feature formed in the coastal environment
- Moraines are not an erosional features of glaciers
- Changing tilt of Earth's axis is one of the factors that has controlled the expansion and contraction of continental scale ice sheets in the ongoing Ice Age of the last ~2 million years
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