OCEANIC LIDAR - RADIATIVE-TRANSFER IN THE ATMOSPHERE AT OPERATING ALTITUDES FROM 100 M TO 100 KM

The feasibility of measuring water-column parameters of the sea with a fluorescence lidar under daylight conditions and at flight altitudes between 100 m and 100 km is studied by modeling the atmospheric radiat ive transfer. Parameters to be measured are fluorescence of gelbstoff and chlorophyll and Raman scattering of water molecules. A cloudless a nd stratified atmosphere with various conditions of near-surface visib ility and ozone concentration is taken into consideration. Solar zenit h angles are varied between 0 degrees and 60 degrees. Lidar specificat ions are set to 1 J output energy, 10 ns pulse duration, 0.1 mrad beam divergence, 0.1 mrad detection angle, and 400 cm(-1) detection bandwi dth. Signal recovery is carried out over the effective purse length of the returned signal, which is roughly 20-30 ns. Sensor zenith angles are set between 0 degrees and 60 degrees. As a result of the study the recommended range of excitation wavelengths for high altitudes should be chosen between 350 and 400 nm. Under these circumstances, and with the given laser and sensor specifications, oceanic lidar measurements should also be possible at flight altitudes of up to 100 km under cle ar visibility conditions, even at noon.