Solar Flux Measurements from the Pioneer Venus Sounder Probe The LSFR instrument and the reduction and analysis of the LSFR data are described in some detail in Measurements of the Flux of Sunlight in the Atmosphere of Venus by M. G. Tomasko, L. R. Doose, Peter H. Smith, and A. P. Odell, J.G.R., volume 85, 1980. The upward, downward, and net fluxes measured by the LSFR are presented in UADS file LSFRDAT. The table in that file contains 12 columns, as follows: TIME - The ground receipt time corresponding to when the data sample was taken. PRESS - The atmospheric pressure in earth atmospheres when the data sample was taken. The pressure and altitude are derived from interpolation in the LAS experiment results distributed on April 11, 1979. CAUTION - this may not be the most recent time - pressure - altitude table. ALT - The altitude of the sample in kilometers, again obtained by interpolation in the LAS table of April 11, 1979. The remaining nine columns are fluxes in watts per square meter. Some data are missing at 19:53:57.49 because of a gap in the telemetry. VIS UP, DOWN, and NET - The upward going, downward going, and net (downward going minus upward going) flux in the LSFR visible channel. This channel extends from approximately 0.40 to 0.96 microns. Note that the width of the spectral profile of this channel changes somewhat during the descent due to temperature effects ( see Tomasko et al., 1980). COMBINED UP, DOWN, and NET - The upward going, downward going, and net fluxes for the LSFR combined channel. The combined channel is a synthesis of both the visible and infrared channels into a single broad band. Its bandpass extends from approximately 0.41 to 1.78 microns, but it too changes slightly during the descent (see Tomasko et al., 1980). After 19:10:46 the signals in the infrared portion of the combined channel were too small to measure. Below about 50 kilometers altitude the combined channel fluxes must be viewed with caution. NB UP, DOWN, and NET - The upward going, downward going, and net fluxes for the LSFR narrow-band channel. This channel extends from approximately 0.59 to 0.67 microns. The upward (and therefore also the net) fluxes are not given in the lowest kilometer due to an instrumental problem associated with the presence of water vapor within the probe )see Tomasko et al., 1980). Note: An empty data field means that value was blank in the original source file.