Liste des variables
|
Parameter / Parameter Tree |
Definition |
Reference |
|
Planetary Boundary Layer Height |
The height of the atmospheric layer from the Earth's surface up
to an altitude of about 1 kilometer in which wind speed and
direction are affected by frictional interaction with objects on
the Earth's surface. |
Glossary of Meteorology, American Meteorological Society, 1998. |
|
Latent Heat Flux |
The flux of energy, per unit area, which leaves the surface as
water is transformed into vapor. |
|
|
Sensible Heat Flux |
The flux of energy, per unit area , associated to the diffusion
of heat away from the surface. |
|
|
Sea Level Pressure |
The atmospheric pressure at mean sea level, either directly
measured, or, most commonly, empirically determined from the
observed station pressure. |
Glossary of Weather and Climate, American Meteorological Society, 1996. |
|
Surface Pressure |
In meteorology, the atmospheric pressure at a given location on
the earth's surface. |
Glossary of Weather and Climate, American Meteorological Society, 1996. |
|
Incident Surface SW |
The amount of short wave radiation arriving at the surface.
Most of the short wave energy is in the spectral band 0.2µm
to 4µm. |
|
|
Reflected Surface SW |
The amount of short wave radiation reflected by the
surface. |
|
|
Surface Incoming LW Radiation |
The long wave flux emitted by the atmosphere and reaching the
surface. The energy is concentrated at wavelength greater than
4µm. |
|
|
Surface Net Radiation |
The net radiative energy absorbed at the surface. This
comprises the net short wave as well as the net long wave flux at
the surface. |
|
|
Surface Net SW Radiation |
Short wave radiative energy absorbed at the surface. |
|
|
TOA Net LW Radiation |
Long wave radiative energy lost to space by the Earth. |
|
|
TOA Net SW Radiation |
Net Short wave energy absorbed by the Earth system as seen from
the top of the atmosphere. |
|
|
Lowest Level Temperature |
Temperature in the lowest layer of the soil model. This layer
has a zero flux closure and thus only exchanges energy with the
layer above. |
|
|
Maximum Surface Air Temperature |
Highest air temperature attained during a specific time
interval, here 24 hours. |
Glossary of Weather and Climate, American Meteorological Society, 1996. |
|
Minimum Surface Air Temperature |
Lowest surface air temperature attained during a specific time
interval, here 24 hours. |
Glossary of Weather and Climate, American Meteorological Society, 1996. |
|
Surface Air Temperature |
In meteorology, the temperature of the ambient air near the
surface of the earth, almost invariably determined by a
thermometer in an instrument shelter. In a model this is the
result of an interpolation between the surface temperature and the
temperature of the lowest atmospheric level. |
Glossary of Weather and Climate, American Meteorological Society, 1996. |
|
Evapotranspiration |
The sum of evaporation from bare soil, transpiration from
plants and sublimation of snow covered areas. |
|
|
Surface Air Humidity |
The humidity of the air at about 2m above the ground. Again in
a model this is an interpolation between saturated humidity at the
surface and the value in the lowest layer of the atmospheric
model. |
|
|
Wind Stress |
Energy lost to friction at the surface by the wind. |
|
|
Cloud Amount/Frequency |
The fraction of the skycover (reported in tenths of sky
covered) that is attributed to a particular cloud type, or cloud
layer; often used synonymously with cloud cover. |
Glossary of Weather and Climate, American Meteorological Society, 1996. |
|
LW Cloud Radiative Forcing |
The change induced by clouds on the long wave energy budget at
the top of the atmosphere. |
|
|
SW Cloud Radiative Forcing |
The impact of clouds on the short wave energy budget at the top
of the atmosphere. |
|
|
Precipitable Water |
The vertically integrated content of water in the atmospheric
column and in its three phases. |
|
|
Precipitation Rate |
The amount of precipitation that is collected over a specific
time period; usually measured in kg per squared meter and seconds.
This unit is equivalent to millimeters per seconds. |
|
|
Snow |
A type of frozen precipitation composed of white or translucent
ice crystals, chiefly in complex branch hexagonal form and often
agglomerated into snow-flakes, especially at temperatures warmer
than -5 C (23 F). |
Glossary of Weather and Climate, American Meteorological Society, 1996. |
|
Temporal Precipitation Variance |
The day to day variance of precipitation. Typically computed
over a month. |
|
|
Interception Loss |
The evaporation of the water intercepted by the canopy. |
|
|
Leaf Area Index |
The area of all leafs divided by the surface on the ground
covered by the plant. |
|
|
Transpiration |
Evaporation by the plants of water in the soil moisture
reservoir. |
|
|
Snow Water Equivalent |
The mass of water in the snow cover. |
|
|
Runoff |
The excess water which can no infiltrate into the soils or
which is lost because the soil moisture exceeds the holding
capacity. |
|
|
Moisture Avaibility Function |
The ratio of actual over potential evaporation as simulated by
the land-surface model. |
|
|
Land Surface Temperature |
The surface temperature resulting from the energy balance
simulated at the surface. The exact definition of this variable is
model specific as it depends on the assumptions made. |
|
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Soil Evaporation |
Evaporation from the bare soil fraction. |
|
|
Soil Heat Flux |
The thermal flux from the surface into the soil. |
|
|
Soil Moisture/Water Content |
The amount of water in the soil as assumed by the land-surface
model. This variable is also strongly dependent on the assumption
made by the model on the soil characteristics. |
|
|
Albedo |
Albedo is the ratio of the radiation (radiant energy or
luminous energy) reflected by a surface to that incident on it.
Snow and cloud surfaces have a high albedo, because most of the
energy of the visible solar spectrum is reflected. Vegetation and
ocean surfaces have low albedo, because they absorb a large
fraction of the energy. Clouds are the chief cause of variations
in the Earth's albedo. |
Maunder, W.J. 1994. Dictionary of Global Climate Change, 2nd ed. Chapman and Hall, NY. WMO, 1966. International Meteorological Vocabulary, WMO/OMM/BMO - No. 182 TP. 91, Switzerland. |
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List Creation Date: |
2002-07-10 |
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Last List Revision Date: |
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