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Hydrology variables

The TEMS directory contains ten core variables related to terrestrial fresh water, these are:

Surface water discharge
The volume of water flowing through a river channel cross-section per unit of time.
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Surface water storage fluxes
The change in volume and extension of inland water bodies.
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Groundwater storage fluxes
The groundwater topographic flow that changes over time in the volume of groundwater that is held in a certain aquifer.
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Precipitation
All deposits on the earth of hail, mist, rain, sleet, snow, dew, fog, frost, and dust.
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Evapotranspiration
The loss of water to the atmosphere from a given area during a specified time by evaporation from the soil surface and by transpiration from plants.
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Relative (air) humidity
It is the ratio, in percent, of the actual amount of water vapour in a body of air in relation to the maximum amount that the body can hold at a given temperature. Relative humidity varies with temperature and atmospheric pressure for a given amount of water vapour. There is no more evaporation at 100 percent relative humidity.
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Soil moisture
The water content of a defined soil sample.
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Snow water equivalent
The water content obtained from melting a defined sample of snow.
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Biogeochemical transport from land to ocean
The amount of carbon (C), nitrogen (N), phosphorus (P), sulphur (S) and other elements that are transported from land to ocean as dissolved or suspended particles in streams and rivers.
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Sediment Load at large river mouths
Freshwater sediment load is the sum of the framework bedload, the matrix bedload and the suspended solids of an aquatic system. Framework bedload refers to the larger particles that are moved only during large flow events. The matrix bedload refers to that part of the bed material that is small enough to be frequently entrained by low to moderate flows but is large enough to settle out of the water column in lower velocities. The suspended load is held in the water column as suspended material for extended periods of time.

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