water and carbon cycle Flashcards
water can be stored in four areas?
hydrosphere, lithosphere, cryosphere, atmosphere
what is the cryosphere
any water that is frozen
what is the lithosphere?
water stored in the crust and upper mantle.
how much of earth’s fresh water is stored in the cryosphere and lithosphere store?
cryosphere- 69%
lithosphere- 30%
evaporation
when liquid changes state in to a gas
what affects the magnitude of evaporation.
it is dependent on season and location, as large levels of solar radiation combined with a large supply of water and warm dry air.
condensation
when water vapour changes state to a liquid. happens when the air cools to its dew point. e.g at night.
what affects the magnitude of condensation
amount of water vapour in the atmosphere and the temperature.
cloud formation
clouds form when warm air cools down, causing the water vapour In it to condense into water droplets, which gather as clouds.
what causes warm air to cool
topography, convection, other air masses.
topography
when warm air meets mountains, its forced to rise, causing it to cool. This results in orographic precipitation.
convection
when the sun heats up the ground, moisture on the ground evaporates and rises up in a column of warm air. as it gets higher it cools, resulting in precipitation.
other air masses
warm air is less dense than cool air. as a result when the two contrasting airs meet, the warm air is forced above the cool air. As this warm air rises it cools down causing frontal precipitation.
what is a drainage basin?
is the area surrounding the river where the rain falling on the land flows into that river. they are OPEN systems.
watershed
the watershed is the dividing ridge, any precipitation falling beyond the water shed enters a different drainage basin.
where can be water be stored on a local scale ?
interception,
vegetation storage,
surface storage,
groundwater storage,
soil storage.
what are the flows in the water cycle?
infiltration,
overland flow,
through fall,
stemflow,
through flow,
percolation,
groundwater flow,
baseflow,
interflow,
channel flow.
overland flow
water flowing over the land because of saturated soil.
through fall
water dropping from one leaf to another.
Throughflow
water moving slowly downhill through the soil.
percolation
water seeping down through the soil into the water table.
baseflow
groundwater flow that feeds into river banks and beds.