EXAM 2 Flashcards

Streams and Floods, Climate, Mass Movements, Coastal, Glaciers, Water Resources

1
Q

Define stream load and explain what factors control it.

A

Stream load: materials that are carried and transported by a stream or river
Dissolved load: ions dissolved in the water
Suspended load: particles carried in suspension
Bed load: particles moved along the streambed

Factors:
Stream velocity
Volume of water flowing
Size and density of the particles
Slope of stream channel

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2
Q

Why do stream sediments tend to be well sorted?

A

Stream sediments tend to be well sorted because the sorting process occurs as a result of the varying velocities of water within the stream

Faster-moving water: can transport larger and heavier particles

Slower-moving water: can only transport smaller and lighter particles

Differential transport leads to the sorting of sediment particles by size, resulting in well-sorted sediments.

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3
Q

Explain how migration and enlargement of meanders contribute to floodplain development.

A

Meander migration and enlargement: Alter the shape and size of the river channel

As meanders migrate laterally and enlarge over time, they erode the outer banks and deposit sediment on the inner banks, creating a wider and flatter floodplain

Increases the capacity of the river to accommodate floodwaters

Reduces the risk of flooding in surrounding areas

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4
Q

Describe some of the factors that cause rivers to be braided, rather than meandering.

A

High sediment supply: When a river has more sediment than it can transport, it deposits excess sediment, creating bars and islands within the channel

Variable discharge: Caused by factors like seasonal rainfall or glacial meltwater, can lead to fluctuations in channel capacity, promoting the formation of multiple channels

Steep channel gradient: Increases the energy available for sediment transport.

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5
Q

What is a flood-frequency curve?

A

Flood-frequency curve: graph that illustrates the relationship between the magnitude of floods and their frequency of occurrence

Plots the discharge of a river against the probability of exceedance (chance of a flood of a certain magnitude occurring in a given year)

Essential for assessing flood risk and designing flood control measures

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6
Q

What is recurrence interval and how is it determined?

A

Recurrence interval: Average time interval between floods of a particular magnitude or greater

Determined by analyzing historical flood data and constructing a flood-frequency curve

Recurrence Interval = (N + 1) / M, where N is the number of years of record and M is the rank of the flood event.

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7
Q

Describe how urbanization can affect stream flooding.

A

Increasing the amount of impervious surfaces such as roads, buildings, and parking lots

These surfaces prevent water from infiltrating into the ground, leading to rapid runoff during rainfall events

Urban areas experience higher peak flows and more frequent flooding.

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8
Q

Why does the Earth have seasons?

A

Earth’s axial tilt relative to its orbit around the Sun

As Earth orbits the Sun, different parts of the planet receive varying amounts of sunlight

Leads to differences in temperature and weather patterns

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9
Q

In what way does climate change impact hurricanes?

A

Warmer ocean temperatures provide more energy for hurricanes to intensify, leading to stronger and more destructive storms

Rising sea levels increase the risk of storm surge and coastal flooding during hurricane landfalls.

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10
Q

Describe the “greenhouse effect”.

A

Greenhouse effect: natural process that regulates Earth’s temperature by trapping heat in the atmosphere

Greenhouse gases (carbon dioxide [CO2], methane [CH4], water vapor [H2O]), absorb and re-emit infrared radiation emitted by the Earth’s surface

Warms the lower atmosphere and the surface of the Earth, making it habitable for life.

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11
Q

The sun emits energy in what parts of the electromagnetic spectrum?

A

Electromagnetic radiation:
Ultraviolet (UV)
Visible light
Infrared (IR)

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12
Q

The Earth emits energy in what parts of the electromagnetic spectrum?

A

Infrared radiation: result of the Earth’s surface and atmosphere absorbing solar energy and re-radiating it back into space

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13
Q

What is ‘insolation’ and how does it vary with latitude and season?

A

Insolation: incoming solar radiation received by the Earth’s surface

Varies with latitude and season due to the curvature of the Earth and its axial tilt

At the equator, insolation is generally more intense throughout the year, leading to warmer temperatures

At higher latitudes, insolation decreases, resulting in cooler temperatures.

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14
Q

Describe how global atmospheric circulation patterns affect climates at different latitudes.

A

These circulation patterns transport heat and moisture around the globe, shaping regional climates.

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15
Q

What are the two main mechanisms by which the energy from the sun is transported from the equator toward the poles?

A
  1. Atmospheric circulation (such as Hadley, Ferrel, and Polar cells)
  2. Ocean currents (such as the Gulf Stream and the Antarctic Circumpolar Current)
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16
Q

What drives the thermohaline circulation in the oceans, and how does this “conveyor” affect climate around the North Atlantic?

A

Thermohaline circulation: primarily driven by differences in temperature and salinity

Warm, less dense surface waters move towards the poles, where they cool and become denser, sinking to deeper ocean layers

Global “conveyor belt” of ocean currents helps regulate climate by redistributing heat around the Earth, particularly affecting climate in the North Atlantic region.

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17
Q

What is upwelling and why does it occur?

A

Upwelling: process by which cold, nutrient-rich waters rise from the ocean depths to the surface

Occurs along coastlines where surface winds blow offshore, causing surface waters to move away from the shore and be replaced by cold, nutrient-rich waters from below

Supports high biological productivity and fisheries in coastal regions.

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18
Q

El Nino and la Nina are naturally occurring variations in the climate. Describe the conditions that lead to El Nino and its effects on weather patterns in the Pacific.

A

El Niño: characterized by the warming of sea surface temperatures in the central and eastern Pacific Ocean, disrupting normal atmospheric circulation patterns

Occurs irregularly every 2-7 years and can lead to changes in weather patterns worldwide.

Effects of El Niño include droughts in some regions, heavy rainfall and flooding in others, and disruptions to marine ecosystems.

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19
Q

What is the ‘Snowball Earth” hypothesis? Describe two of the feedback loops that it assumes.

A

The Snowball Earth Hypothesis: Earth experienced periods of extreme glaciation in its past, during which the entire planet was covered in ice

Feedback loops involving the following factors initiate and maintain these glaciations:

Ice-albedo feedback (reflectivity of ice)
Carbon dioxide levels

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20
Q

What are the three components of Milankovitch cycles? Name and describe them in some detail.

A

Milankovitch cycles: long-term variations in Earth’s orbit and axial tilt that influence climate over tens to hundreds of thousands of years

Eccentricity: changes in the shape of Earth’s orbit

Axial tilt: changes in the tilt of Earth’s axis

Precession: changes in the orientation of Earth’s axis

*These cycles affect the distribution and intensity of solar radiation received by the Earth, influencing climate patterns such as ice ages.

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21
Q

What are some expected changes to climate in New Hampshire in the coming decades? Be specific.

A

Warmer temperatures

Changes in precipitation patterns (including more intense rainfall events)

Increased frequency of heatwaves

Changes in the distribution of plant and animal species

Rising sea levels on coastal areas

22
Q

What are two primary factors that contribute to the uncertainty in climate change projections (like those from the IPCC)?

A

Complexity of Earth’s climate system:

Climate is influenced by numerous interconnected processes and feedback mechanisms, making accurate predictions challenging

Uncertainties in future human activities and emissions:

Uncertainties in future greenhouse gas emissions, technological advancements, and policy decisions contribute to uncertainty in future climate scenarios.

23
Q

Factors influencing slope stability - Geology and Rock Type

A

Different types of rock and soil have varying degrees of cohesion and internal strength, affecting their stability on slopes.

24
Q

Factors influencing slope stability - Slope Angle and Height

A

Steeper slopes are generally less stable than gentler slopes, especially when combined with greater height.

25
Q

Factors influencing slope stability - Vegetation Cover

A

Vegetation helps stabilize slopes by reinforcing soil with roots, reducing erosion, and absorbing excess moisture.

26
Q

Factors influencing slope stability - Water Content

A

Excess water can decrease soil cohesion, increase weight, and lubricate surfaces, making slopes more prone to failure.

27
Q

Factors influencing slope stability - Climate and Weathering

A

Climate conditions and weathering processes can weaken rock and soil over time, reducing slope stability.

28
Q

Factors influencing slope stability - Human Activities

A

Construction, mining, deforestation, and other human activities can alter natural slope conditions, increasing the risk of instability.

29
Q

What is “angle of repose”?

A

Angle of Repose: maximum angle at which loose material, such as sand, soil, or rock fragments, can remain stable on a slope without collapsing or sliding

Represents the equilibrium angle between the force of gravity pulling the material downhill and the resistance of the material to movement.

30
Q

Name and describe three different types of mass wasting.

A

Landslides: Rapid downslope movement of rock, soil, or debris along a discrete surface, often triggered by heavy rainfall, earthquakes, or human activities.

Slumps: Movement of material along a curved surface, typically characterized by rotational movement and internal deformation.

Rockfalls: Sudden detachment and free-fall movement of individual rock fragments or blocks from a steep cliff or slope.

31
Q

Describe why heavy rains increase the risk of landslides in some areas.

A

Saturation: Excessive rainfall saturates the soil, reducing its cohesion and increasing pore water pressure, making it more prone to failure.

Increased Weight: The added weight of water can increase the stress on slopes, especially on already unstable or weakened slopes.

Lubrication: Water acts as a lubricant, reducing friction between soil particles and rock surfaces, facilitating slope movement.

Erosion: Heavy rainfall can erode slope materials, undercutting the base of slopes and triggering mass wasting events.

32
Q

What human activities contribute to slope instability? Explain these activities create instabilities.

A

Deforestation: Removal of vegetation reduces slope stability by removing root reinforcement and increasing surface runoff, leading to erosion.

Construction and Excavation: Alteration of slopes through excavation, grading, or construction activities can disturb natural slope conditions, leading to instability.

Mining: Excavation and blasting associated with mining operations can weaken slopes, leading to slope failures and landslides.

Poor Land Use Practices: Improper land use practices such as overloading slopes with structures, roads, or landfills can increase stress on slopes and contribute to instability.

33
Q

Name and describe the methods that humans employ to prevent instabilities.

A

Vegetation Management: Planting and maintaining vegetation on slopes to stabilize soil with roots, reduce erosion, and absorb excess moisture

Engineering Structures: Constructing retaining walls, rock buttresses, or soil reinforcement structures to stabilize slopes and prevent erosion.

Drainage Systems: Installing drainage systems such as French drains or surface water diversion channels to reduce excess water infiltration and pore pressure buildup.

Slope Grading and Terracing: Modifying slope angles and creating terraces to reduce slope steepness and redistribute weight, improving stability.

Slope Monitoring and Early Warning Systems: Implementing monitoring techniques such as inclinometers, GPS, and rainfall gauges to detect changes in slope stability and provide early warnings of potential failures.

34
Q

Name and describe the major parts of a beach (beach face, berm, foreshore, backshore)

A

Beach Face: The sloping portion of the beach that extends from the water’s edge to the berm. It is continually reshaped by wave action and tides.

Berm: A raised area of sand or gravel running parallel to the shoreline, marking the highest point reached by normal high tides. It serves as a buffer against wave erosion during storms.

Foreshore: The area of the beach that is exposed during low tide and submerged during high tide. It experiences constant wave action and erosion.

Backshore: The upper portion of the beach that is only submerged during extreme high tides or storm surges. It is usually dry and subject to wind-driven processes.

35
Q

What causes waves? As waves approach a shoreline, they ‘break’. Why?

A

Waves: Primarily caused by the transfer of energy from the wind to the water’s surface

As wind blows across the ocean, it creates ripples that develop into waves

As waves approach the shoreline, they begin to feel the ocean bottom, causing the wave crests to become steeper and eventually break

Wave breaking occurs when the wave height exceeds the depth of the water, causing the wave to collapse and release its energy.

36
Q

What causes tides? What is the difference between neap and spring tides? What causes the so-called “King tide”?

A

Tides: primarily caused by the gravitational pull of the Moon and, to a lesser extent, the Sun, on Earth’s oceans

Neap tides: gravitational forces of the Sun and Moon are perpendicular to each other, resulting in lower high tides and higher low tides

Spring tides: gravitational forces of the Sun and Moon are aligned, resulting in higher high tides and lower low tides

King tides: (perigean spring tides) the Moon is at its closest point to Earth (perigee), amplifying the gravitational pull and causing especially high tides

37
Q

How do longshore currents impact shorelines? What is littoral drift?

A

Longshore currents: currents that flow parallel to the shoreline, transporting sediment along the coast

Littoral drift: movement of sediment along the shoreline due to the combined action of waves and currents

Longshore currents and littoral drift can impact shorelines by redistributing sediment, shaping beaches, and forming coastal landforms such as spits and barrier islands.

38
Q

What is a storm surge and what are its components?

A

Wind Setup: increase in sea level caused by strong onshore winds pushing water towards the shore.
Barometric Pressure Drop: decrease in atmospheric pressure associated with the storm, causing water to pile up.
Wave Setup: The increase in sea level caused by large waves riding on top of the storm surge.

39
Q

What is a wave-cut platform? How does it form?

A

Wave cut platform: gently sloping, flat surface eroded by wave action at the base of a cliff or headland

Forms through a process of abrasion and hydraulic action, where waves undercut and erode the base of the cliff, causing it to retreat inland

Over time, the exposed bedrock is worn down into a flat platform by continued wave action.

40
Q

Why do drowned valleys form?

A

Drowned valleys: form when sea level rises or land subsides, flooding river valleys that were previously exposed

As sea level rises, river valleys are inundated with seawater, forming estuaries or drowned river mouths

Process can be accelerated by glacial melting or tectonic activity.

41
Q

Name and describe two methods of coastal stabilization.

A

Beach Nourishment: Adding sand or sediment to eroded beaches to widen the shoreline and protect coastal structures.

Seawalls and Revetments: Hard structures built along the shoreline to deflect wave energy and prevent erosion of the coast.

Dune Restoration: Planting vegetation and building dunes to stabilize shorelines, absorb wave energy, and protect inland areas from storm surges.

42
Q

How does wave refraction work to erode points of land jutting out into the sea?

A

Wave refraction: occurs when waves approach a coastline at an angle, causing them to bend and concentrate their energy on headlands or points of land jutting out into the sea

Concentrated wave energy accelerates erosion on the sides of headlands, forming sea cliffs, sea caves, and other erosional landforms.

43
Q

Briefly describe the fate of the Hampton Beach community under the climate scenario coinciding with net zero by 2050?

A

Reduced risks of coastal erosion and flooding due to decreased sea level rise and storm intensity

Challenges related to:
sea level rise
increased temperatures
changes in precipitation patterns

Combat challenges with:
shoreline protection
flood defenses
infrastructure improvements.

44
Q

What is a glacier? How do glaciers form?

A

Glacier: large mass of ice that moves slowly over land under its own weight

Form through the accumulation and compaction of snow over many years

Successive layers of snow accumulate, weight of the overlying snow compresses the lower layers into dense ice

Ice becomes thick enough to flow downhill under the force of gravity, forming a glacier

45
Q

What are the differences between continental and alpine glaciers?

A

Continental Glaciers (ice sheets):
Vast ice masses that cover extensive areas of land
Found in polar regions such as Antarctica and Greenland
Characterized by their immense size and relatively flat topography

Alpine Glaciers (mountain glaciers):
Occur in mountainous regions
Confined to valleys or cirques
Smaller in size compared to continental glaciers
Often found in high-altitude areas
Flow down valleys, sculpting the landscape as they move

46
Q

What part of a glacier flows fastest? Slowest? Why?

A

Fastest-flowing: center/axis of the glacier (ice experiences the least resistance to flow)
- “zone of maximum flow” or “zone of velocity.”

Slowest-flowing: edges/margins (ice encounters frictional resistance from the valley walls or surrounding terrain)

*base of a glacier may also flow faster than the surface due to the presence of meltwater acting as a lubricant, reducing friction.

47
Q

Define and describe the following: striations, till, outwash, drift, moraine.

A

Striations: parallel scratches/grooves on bedrock surfaces caused by the movement of glaciers; formed as glaciers transport rock fragments and debris, which scrape and scratch the underlying bedrock as the glacier moves.

Till: unsorted and unstratified sediment deposited directly by glaciers; consists of a mixture of clay, silt, sand, gravel, and boulders, deposited as the glacier retreats or melts.

Outwash: sediment deposited by meltwater streams flowing from glaciers; usually well-sorted and stratified, consisting of sand, gravel, and finer sediment transported and sorted by meltwater.

Drift: all sedimentary deposits, including till and outwash, left behind by glaciers.

Moraine: accumulations of till deposited by glaciers; can be classified as:
- Lateral moraines: deposited along the sides of glaciers
- Medial moraines: formed where two glaciers merge
- Terminal moraines: deposited at the furthest extent of a glacier
- Recessional moraines: deposited as a glacier temporarily stalls during retreat

48
Q

How does a ‘wineglass valley’ form?

A

Wineglass valley (U-shaped valley): forms through the erosional action of glaciers

V-shaped river valley carved by the flow of water

Glacier erodes valley floor and walls through abrasion and plucking, widening and deepening the valley into a wineglass valley

After the glacier retreats, the valley may be further modified by other erosional processes such as rivers or weathering

49
Q

What is the “Water Budget Equation” and use it to explain the fall of the Aral Sea.

A

Water budget equation: method used to analyze the inflow, outflow, and changes in water storage of a particular system

Inflow - Outflow ± Changes in Storage = 0.

Aral Sea: received water from two main sources (Amu Darya and Syr Darya rivers).

Inflow of water into the Aral Sea drastically decreased due to water diversion for agriculture

Inflow of water into Aral Sea decreased

Increased evaporation due to higher temperatures and reduced surface area lead to higher outlow

Factors resulted in in negative change in storage, leading to dessication of Aral Sea

50
Q

In what region of the United States are water resources analogous to those of the Aral Sea? Briefly explain how the two are similar.

A

Colorado River Basin and Aral Sea Similarities:

Significant water diversion for agricultural irrigation and human consumption

Reduced inflow

Increased water demand due to population growth and economic development

Environmental degredation

Loss of biodiversity

Socio-economic impacts on local communities

51
Q

How do we commonly measure the quantity of “Renewable Fresh Water Resources” in a region and how is this quantification used to determine ‘Water Scarcity’?

A

Renewable freshwater resources indicators:
- Total annual precipitation
- Surface water runoff
- Groundwater recharge.

Water scarcity: determined by comparing availability of renewable freshwater resources to water demand of a region’s population and economy
- Occurs when water demand exceeds supply of renewable resources
- Regions facing high water scarcity may experience water shortages, competition for water resources, and socio-economic challenges related to water access and management

Water Stress Index: compares water withdrawals to renewable resources, or the Falkenmark Indicator (assesses water availability per capita)