Quiz 1 Flashcards

1
Q

Precipitation is the primary input of water into a watershed.

A

True

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2
Q

A watershed can include multiple smaller sub-watersheds.

A

True

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3
Q

The global water balance ensures that the total amount of water in the cycle remains constant.

A

True

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4
Q

Snowmelt contributes to runoff in watersheds in colder climates.

A

True

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5
Q

Water vapor in the atmosphere contributes to the formation of precipitation.

A

True

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6
Q

Interception by vegetation reduces the amount of precipitation reaching the ground.

A

True

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7
Q

The hydrologic cycle describes the continuous movement of water on, above, and below the Earth’s surface.

A

True

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8
Q

Groundwater flow within a watershed is faster than surface runoff.

A

True

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9
Q

Human activities like deforestation and urbanization can disrupt the natural hydrologic cycle.

A

True

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10
Q

Snowmelt contributes to surface runoff in colder climates.

A

True

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11
Q

The cryosphere refers to the frozen components of the Earth’s hydrologic cycle.

A

True

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12
Q

The movement of water in the hydrologic cycle is unidirectional.

A

False

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13
Q

Water vapor in the atmosphere does not contribute to the hydrologic cycle.

A

False

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14
Q

A watershed’s outflow is typically measured at its outlet, such as a river mouth.

A

True

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15
Q

The hydrologic response of a watershed to precipitation depends on land use and soil type.

A

True

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16
Q

Infiltration capacity of soil increases as the soil becomes more saturated.

17
Q

Transpiration is the release of water vapor from plants into the atmosphere.

18
Q

Urbanization generally decreases runoff within a watershed.

19
Q

Water storage in glaciers and ice caps is considered a short-term storage component of the hydrologic cycle.

20
Q

The hydrologic cycle has no role in shaping the Earth’s surface features.

21
Q

Evaporation rates increase with higher temperatures, wind speed, and lower humidity.

22
Q

Evaporation occurs only during the daytime when the sun is present.

23
Q

Impervious surfaces in urban areas reduce infiltration in a watershed.

24
Q

Evaporation rates are higher in humid climates than in arid climates.

25
Q

Deserts have a high rate of evapotranspiration compared to humid regions.

26
Q

Watersheds are static and cannot change due to natural or human activities.

27
Q

Overland flow occurs when the infiltration rate of soil is greater than the rainfall intensity.

28
Q

Evaporation rates are higher in areas with dense vegetation.

29
Q

Deforestation within a watershed has no impact on runoff or evaporation rates.

30
Q

Precipitation falling on a watershed is uniformly distributed over its area.