Quiz 1 Flashcards
Precipitation is the primary input of water into a watershed.
True
A watershed can include multiple smaller sub-watersheds.
True
The global water balance ensures that the total amount of water in the cycle remains constant.
True
Snowmelt contributes to runoff in watersheds in colder climates.
True
Water vapor in the atmosphere contributes to the formation of precipitation.
True
Interception by vegetation reduces the amount of precipitation reaching the ground.
True
The hydrologic cycle describes the continuous movement of water on, above, and below the Earth’s surface.
True
Groundwater flow within a watershed is faster than surface runoff.
True
Human activities like deforestation and urbanization can disrupt the natural hydrologic cycle.
True
Snowmelt contributes to surface runoff in colder climates.
True
The cryosphere refers to the frozen components of the Earth’s hydrologic cycle.
True
The movement of water in the hydrologic cycle is unidirectional.
False
Water vapor in the atmosphere does not contribute to the hydrologic cycle.
False
A watershed’s outflow is typically measured at its outlet, such as a river mouth.
True
The hydrologic response of a watershed to precipitation depends on land use and soil type.
True
Infiltration capacity of soil increases as the soil becomes more saturated.
False
Transpiration is the release of water vapor from plants into the atmosphere.
True
Urbanization generally decreases runoff within a watershed.
False
Water storage in glaciers and ice caps is considered a short-term storage component of the hydrologic cycle.
False
The hydrologic cycle has no role in shaping the Earth’s surface features.
False
Evaporation rates increase with higher temperatures, wind speed, and lower humidity.
True
Evaporation occurs only during the daytime when the sun is present.
False
Impervious surfaces in urban areas reduce infiltration in a watershed.
True
Evaporation rates are higher in humid climates than in arid climates.
False
Deserts have a high rate of evapotranspiration compared to humid regions.
False
Watersheds are static and cannot change due to natural or human activities.
False
Overland flow occurs when the infiltration rate of soil is greater than the rainfall intensity.
False
Evaporation rates are higher in areas with dense vegetation.
False
Deforestation within a watershed has no impact on runoff or evaporation rates.
False
Precipitation falling on a watershed is uniformly distributed over its area.
False