Global Hydrological Cycle

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Flashcards covering key terms related to the Global Hydrological Cycle.

Last updated 10:48 PM on 4/16/26
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24 Terms

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Global Hydrological cycle

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Evaporation

  • conversion of liquid water to water vapor

  • occurs when a water molecule in a liquid has enough energy to break free of the chemical bonds within the liquid, and enter the atmosphere

    • higher temp = more energy available

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Transpiration

  • The process by which water vapor is released from plants into the atmosphere

  • conversion of liquid water to water vapor by plants (evap through a biological linkage)

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Condensation

  • conversion of water vapor to liquid water

  • occurs when a water molecule in the air comes into contact with a water molecule in the liquid

    • the grater number of vapor water molecules in the air, the greater change that this collision will occur

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water vapor requires a physical substance to form a basis for condensation:

dust particles, chemicals produces by plants, etc. in the atmosphere “seed” the atmosphere

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Precipitation

  • condensation under gravitational pull

  • condensed water vapor falls to Earth due to gravity as rain, snow, sleet, or hail

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Sublimation

  • The direct transition of water molecules from a solid state to a vapor state without becoming liquid

  • movement of water molecules directly from a solid state to a vapor state

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Movement of runoff

  • all water that falls on land as rainfall must eventually drain into the ocean reservoir

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Vapor Pressure

The pressure exerted by water vapor in the air at any given moment.

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evaporation rate

  • how much water is moving from a liquid state to a vapor state over time

    • depends on the temperature of the liquid

      • the warmer to liquid, the faster the rate of evap

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condensation rate

  • how much water is moving from a vapor to a liquid state over time

    • depends on the vapor pressure in the air directly in contact with the liquid water

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Relative Humidity (RH)

  • when rates of condensation and evaporation are equal

    • air is “full” of all the water vapor it can hold

    • air is saturated at 100% RH

      • at this point water will condense in the atmosphere

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what are the two classes of terrestrial reservoirs

Green water and Blue water

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Blue Water

  • all water held temporarily in non-living reservoirs

    • lakes, rivers, ice, soil moisture, groundwater, oceans, and atmosphere

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Green Water

  • all water held temporarily in biological life

  • Major driver of water movement on land

    • the majority of precipitation is initially taken up by plants (green water reservoir)

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what is the major driver of water movement on land?

Green water reservoirs (plants that take up precipitation)

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Glacier

  • masses of ice and snow build up / compressed over hundreds of thousands of years

    • ice and snow persist if local temps do not rise above 0C during the year

    • lower levels of snow get compressed by the weight of upper layers of snow

      • forms solid ice under increasing pressure

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Soil-water zone

  • closest to the surface

  • where plant roots and animal activity take place

  • soil particles have lots of empty space in btw then (room for oxygen and plant roots)

  • contains some water (but water is held tight to the surface of the soil particles)

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Unsaturated Zone

  • The zone within the soil where the spaces between soil particles are filled mainly with air

  • contains very little active biological life aside from soil microbes

  • where water that escapes capture by biological life is carried by gravity (deeper)

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Saturated Zone

  • The zone in which all voids or pores within the soil or rock are filled with water

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Water Table

  • The upper boundary of the saturated zone of groundwater

  • boundary btw saturated and unsaturated zones

  • all space below this is completely filled with water (groundwater)

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Groundwater

  • Water located beneath the Earth's surface, held in soil and rock formations

  • Below water table

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Cryosphere

Frozen water part of the Earth system, including glaciers and polar ice.

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Residence Time

  • The average amount of time water spends in a particular reservoir

  • retention time

  • if the system is in a steady state:

    • can calculate this

    • = reservoir volume / flow rate