Water Cycle Flashcards
Define Atmospheric Water:
Water found in the atmosphere mainly water vapour with some liquid water (cloud and rain droplets) and ice crystals.
Define Cryospheric Water:
The water locked up on the Earth’s surface as ice.
Define Hydrosphere:
A discontinous layer of water at or near the Earth’s surface. It includes all liquid and frozen surface waters, groundwater held in soil and rock and atmospheric water vapour.
Define Oceanic Water:
The water contained in the Earth’s oceans and seas but no including such inland seas as the Caspian Sea.
Define Terrestrial Water:
This consist of groundwater, soil moisture, lakes, wetlands, and rivers.
Define Condensation:
The process by which water vapour changes into liquid water.
Define Cryospheric Processes:
Those processes that affect the total mass of ice at any scale from local patches of frozen ground to global ice amounts. They include accumulation (the build-up of ice mass) and ablation the loss of ice mass).
Define Drainage Basin:
This is an area of land drained by a river and its tributaries. It includes water found on the surface, in the soil and in near-surface geology.
Define Evaporation:
The process by which liquid water changes to a gas. This requires energy, which is provided by the sun and aided by wind.
Define Evapotranspiration
The total output of water from the drainage basin directly back into the atmosphere.
Define Groundwater Flow:
The slow movement of water through underlying rocks.
Define Infiltration
The downward movement of water from the surface into soil.
Define Interception Storage:
The precipitation that falls on the vegetation surfaces or human-made cover and is temporarily stored on these surfaces. This water is then either evaporated or transferred to the ground.
Define Overland flow:
The tendency of water to flow horizontally across land surfaces when rainfall has exceeded the infiltration capacity of the soil and all surface stores are full to overflowing.
Define Percolation:
The downard movement of water within the rock under the soil surface. Rates vary depending on the type of geoglogy.