atmosphere_optical_thickness_due_to_water_in_ambient_aerosol_particles

The specification of a physical process by the phrase due_to_process means that the quantity named is a single term in a sum of terms which together compose the general quantity named by omitting the phrase. The optical thickness is the integral along the path of radiation of a volume scattering/absorption/attenuation coefficient. The radiative flux is reduced by a factor exp(-optical_thickness) on traversing the path. The atmosphere optical thickness applies to radiation passing through the entire atmosphere. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). "atmosphere_optical_thickness_due_to_water_in_ambient_aerosol" refers to the optical thickness due to the water that is associated with aerosol particles due to hygroscopic growth in ambient air, affecting the particle's radius and refractive index. It corresponds to the difference between the total dry aerosol optical thickness and the total ambient aerosol optical thickness.
  • List containing this term version:
  • Proposls with this term version:
  • Proposal: Alison Pamment [HTAP2 Final proposal = 102 CF Standard N]

  • Aliases for this term

    atmosphere_optical_thickness_due_to_water_in_ambient_aerosol

    The specification of a physical process by the phrase due_to_process means that the quantity named is a single term in a sum of terms which together compose the general quantity named by omitting the phrase. The optical thickness is the integral along the path of radiation of a volume scattering/absorption/attenuation coefficient. The radiative flux is reduced by a factor exp(-optical_thickness) on traversing the path. The atmosphere optical thickness applies to radiation passing through the entire atmosphere. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). "atmosphere_optical_thickness_due_to_water_in_ambient_aerosol" refers to the optical thickness due to the water that is associated with aerosol particles due to hygroscopic growth in ambient air, affecting the particle's radius and refractive index. It corresponds to the difference between the total dry aerosol optical thickness and the total ambient aerosol optical thickness.
  • List containing this term version: CF (7) CF (8) CF (9) CF (10) CF (11) CF (12) CF (13) CF (14) CF (15) CF (16) CF (17) CF (18) CF (19) CF (20) CF (21) CF (25) CF (22) CF (27) CF (23) CF (24) CF (26)
  • Proposls with this term version:
  • Proposal: Alison Pamment [HTAP2 Final proposal = 102 CF Standard N]

  • This term is not aliased.