the visible portion. More precise work requires the use of spectral albedos, referenced to specific wavelengths. Visible albedos of natural surfaces range from low values of 0.04 for calm, deep water and overhead Sun, to 0.8 for fresh snow or thick clouds. Many surfaces show an increase in albedo with increasing solar zenith angle. (AMS)
Atmospheric Lifetime Experiment
Atmospheric Model Intercomparison Project
Of, relating to, or being a compound (as a surfactant) consisting of molecules having a polar, water-soluble group attached to a water-insoluble hydrocarbon chain; also: being a molecule of such a compound.
Atmosphere-Ocean General Circulation Model
A global array that will eventually include approximately 3000 free-drifting profiling floats that measure the temperature and salinity of the upper 2000 m of the ocean.
Atmospheric Radiation Measurement
Atmospheric Stabilization Framework Model
A planned satellite formation consisting of two of the major EOS missions, three Earth System Science Pathfinder missions, and a French Centre National d’Etudes Spatiales (CNES) mission flying along the same orbit track and separated by only a few minutes.
Advanced Very High Resolution Radiometer
Black carbon (BC)
Light-absorbing carbonaceous aerosol, including elemental carbon and low-volatility organic compounds.
BLAG (Berner/Lasaga/Garrels) hypothesis
Variations in seafloor spreading rates lead to variations in volcanic outgassing and, thus, atmospheric CO2 concentrations.
The ratio of sensible to latent heat fluxes from the Earth’s surface up into the atmosphere. Typical values are 5 over semiarid regions, 0.5 over grasslands and forests, 0.2 over irrigated orchards or grass, 0.1 over the sea, and negative in some advective situations such as over oases where sensible heat flux can be downward while latent heat flux is upward. (AMS)
Baseline Surface Radiation Network