geography lab review Flashcards

1
Q

Title:

A

Describes what the map represents.

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2
Q

Legend:

A

Explains the symbols used on the map.

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3
Q

Scale:

A

Indicates the relationship between distances on the map and the real world.

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4
Q

Mercator Projection:

A

Distorts area, especially near the poles.Preserves angles and shapes for navigation.

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5
Q

Peters Projection:

A

Equal-area projection; preserves relative sizes of landmasses.
Distorts shapes.

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6
Q

Robinson Projection:

A

Balances distortions in area, shape, distance, and direction.

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7
Q

Latitude:

A

Horizontal lines measuring distance north or south of the Equator (0° to 90°).

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8
Q

Longitude:

A

Vertical lines measuring distance east or west of the Prime Meridian (0° to 180°).

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9
Q

Passive sensors

A

depend on sunlight or thermal energy from the surface.

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10
Q

Active sensors

A

have their energy source, allowing data collection day or night.

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11
Q

Satellite Imagery Interpretation

A

Different surfaces reflect light in unique ways, like a fingerprint. Urban areas reflect a lot of light in both visible and infrared ranges, making them easy to identify.

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12
Q

GIS Layers:

A

Each layer represents a type of data (e.g., physical, social, environmental).

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13
Q

Understanding Solar Declination

A

The solar declination influences the intensity and duration of sunlight received at different latitudes, driving seasonal variations.

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14
Q

Solar Angle

A

The solar angle determines the intensity of sunlight at a location. Higher angles correspond to more direct sunlight, increasing energy absorption.

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15
Q

Solar Altitude:

A

The angle of the Sun above the horizon at a specific time and location.

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16
Q

Insolation (Incoming Solar Radiation):

A

The amount of solar energy received per unit area, which depends on the angle of incidence and atmospheric conditions.

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16
Q

Seasonal Changes:

A

Caused by Earth’s axial tilt and orbit around the Sun, resulting in varying day lengths and solar angles.

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17
Q

Energy Budget:

A

Balance between incoming solar radiation (shortwave) and outgoing terrestrial radiation (longwave).

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18
Q

Cloud Formation:

A

Clouds form when air cools to its dew point, and water vapor condenses onto aerosols.
Factors influencing cloud formation include temperature, humidity, and atmospheric lifting.

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19
Q

Air Masses:

A

Large bodies of air with uniform temperature and moisture characteristics.

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20
Q

Atmospheric Lifting Mechanisms:

A

Convergent Lifting: Air flows toward a central point and rises.
Convectional Lifting: Warm air rises due to heating from the surface.
Orographic Lifting: Air is forced upward by mountains.
Frontal Lifting: Warm air rises over cold air along a front.

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21
Q

Precipitation Processes:

A

Collision-Coalescence: Droplets collide and merge to form larger raindrops.
Bergeron Process: Ice crystals grow in cold clouds at the expense of supercooled droplets.

22
Q

Absolute Humidity:

A

The actual amount of water vapor in the air, measured in grams per cubic meter.

23
Q

Relative Humidity (RH):

A

The ratio of the actual water vapor in the air to the maximum amount it can hold at a given temperature, expressed as a percentage

24
Q

Dew Point:

A

The temperature at which air becomes saturated, and condensation begins.

25
Q

Atmospheric Stability:

A

Determines whether air will rise or sink.

26
Q

Stable Atmosphere:

A

Air returns to its original position after being displaced.

27
Q

Unstable Atmosphere:

A

Air continues to rise after being displaced.

28
Q

Neutral Atmosphere:

A

Air remains where it is displaced.

29
Q

Environmental Lapse Rate (ELR):

A

The rate at which temperature decreases with altitude in the surrounding air.

30
Q

Dry Adiabatic Lapse Rate (DALR):

A

The rate at which unsaturated air cools as it rises (
1
0

C/km
10

C/km).

31
Q

Moist Adiabatic Lapse Rate (MALR):

A

The rate at which saturated air cools as it rises (varies, typically
6

C/km
6

C/km).

32
Q

Adiabatic Processes

A

When air expands and cools or compresses and warms without exchanging heat with its surroundings.

33
Q

Fluvial Processes: Erosion:

A

The removal of material from the riverbed and surrounding landscape

34
Q

Fluvial Processes: Hydraulic action:

A

Water forces air into cracks, breaking apart rocks.

35
Q

Fluvial Processes: Abrasion:

A

Abrasion: Eroding material (like sand) wears down riverbed surfaces.

36
Q

Fluvial Processes: Attrition:

A

Attrition: The process of rocks and particles colliding and breaking down into smaller pieces.

37
Q

Transportation:

A

The movement of eroded material along the river, including:
Bed load: Larger particles (rocks, gravel) that roll or slide along the riverbed.
Suspended load: Finer particles (sand, silt) carried by the water.
Dissolved load: Ions and dissolved substances in the water, like minerals and salts.

38
Q

Deposition:

A

The process where transported materials are dropped when the water’s velocity decreases.

39
Q

Stream Discharge:

Streamflow:

A

The volume of water flowing through a river or stream, usually measured in cubic meters per second (m³/s).

40
Q

Types of Fluvial Landforms:

Valleys:

A

V-shaped valleys are formed by erosion, whereas U-shaped valleys are shaped by glacial activity.

41
Q

Types of Fluvial Landforms: Floodplains:

A

Floodplains: Areas adjacent to a river, frequently flooded, formed by the deposition of sediments during flooding events.

42
Q

Types of Fluvial Landforms: Deltas:

A

Formed where a river meets a standing body of water, such as a lake or ocean, and deposits sediment carried from upstream.

43
Q

Types of Fluvial Landforms: Meanders:

A

Meanders: Curves in a river that form over time as the river erodes its banks.

44
Q

Types of Fluvial Landforms: Oxbow Lakes:

A

Oxbow Lakes: Formed when a meander is cut off from the main river flow, leaving behind a crescent-shaped lake.

45
Q

Waves:

A

Waves are caused by wind blowing across the surface of the water. The energy of the wave affects the coastline, causing erosion, transportation, and deposition.

46
Q

Wave erosion:

A

Waves attack the coastline, eroding cliffs and rocks.

47
Q

Wave refraction:

A

Waves bend as they approach the shore, focusing energy on headlands and reducing energy in bays.

48
Q

Longshore drift:

A

The movement of sand along the shore, caused by waves hitting the beach at an angle, transports sediment parallel to the coast.

49
Q

Tides:

A

The rise and fall of sea levels caused by the gravitational pull of the moon and the sun. Tides affect the distribution of sediment and the formation of coastal features.

50
Q

Currents:

A

Ocean currents are large-scale flows of water that move through the world’s oceans. Coastal currents can influence the movement of sand and other sediments.

51
Q

Longshore current:

A

A current that moves parallel to the shore, caused by waves hitting the coastline at an angle.

52
Q

Rip currents:

A

Narrow, fast-moving currents that flow from the shore to deeper water.