Abstract
Spectral transmissions through haze are computed using meteorological observations to specify aerosol scattering and water vapor, carbon dioxide, and ozone absorption. The computed spectral transmissions are compared with the appropriate experimental transmissions to evaluate the degree to which a natural spectral transmission can be simulated by a computed spectral transmission. The comparison indicates that the dominant atmospheric attenuating parameter is the absolute distribution of aerosols.
© 1967 Optical Society of America
Full Article |
PDF Article
More Like This
Cited By
You do not have subscription access to this journal. Cited by links are available to subscribers only. You may subscribe either as an Optica member, or as an authorized user of your institution.
Contact your librarian or system administrator
or
Login to access Optica Member Subscription
Figures (7)
You do not have subscription access to this journal. Figure files are available to subscribers only. You may subscribe either as an Optica member, or as an authorized user of your institution.
Contact your librarian or system administrator
or
Login to access Optica Member Subscription
Tables (1)
You do not have subscription access to this journal. Article tables are available to subscribers only. You may subscribe either as an Optica member, or as an authorized user of your institution.
Contact your librarian or system administrator
or
Login to access Optica Member Subscription
Equations (6)
You do not have subscription access to this journal. Equations are available to subscribers only. You may subscribe either as an Optica member, or as an authorized user of your institution.
Contact your librarian or system administrator
or
Login to access Optica Member Subscription