================================================================================ Data format for the UARS97.PLT. COL FMT DESCRIPTION -------------------------------------------------------------------------------- 1- 4 I4 Year 5- 6 I2 Month 7- 8 I2 Day 9 1X Blank 10-17 F8.3 Total Solar Irradiance (TSI) is reported on 'ACRIM II native scale' defined by operation of sensor 'B', the full-time monitoring sensor. Results are reconciled to a heliocentric rest frame at 1 A.U. and are fully corrected for sensor degradation. 18 1X Blank 19-23 F5.3 Standard error of the daily means (W/M*2) 24 1X Blank 25-32 F8.3 Acrim II data normalized to Acrim I UARS/ACRIMII results reported on scale defined by operation of SMM/ACRIMI instrumentation. NOTE: The 1991 - 1997 UARS/ACRIM II database has been updated to make a small correction in the time base for 1996. It includes TSI reported on both the 'native scale' of the ACRIM II sensor and in terms of the SMM/ACRIM I scale, as rekonned by mutual intercomparisons using the Nimbus7/ERB results. The ratio of ACRIM I/ACRIM II (native scale) is 1.001689. -------------------------------------------------------------------------------- Total Solar Irradiance Results (TSI) from the Upper Atmosphere Research Satellite (UARS) Active Cavity Radiometer Irradiance Monitor II Experiment (ACRIM II) The second Active Cavity Radiometer Irradiance Monitor experiment (ACRIM II) was launched in September 1991 as part of the science payload of the Upper Atmosphere Research Satellite (UARS). The variations on solar rotational and active region time scales are clearly seen. The large, short-term decreases are caused by the TSI blocking effect of sunspots in magnetically active regions as they rotate through our view from Earth. The peaks of TSI preceding and following these sunspot 'dips' are caused by the faculae of solar active regions whose larger areal extent causes them to be seen first as the region rotates onto our side of the sun and last as they rotate over the opposite solar limb. The downward trend through the 1991-1997 period is similar in slope and amplitude to that observed by ACRIM I during the declining activity phase of solar cycle 21. From the peak of solar cycle 21 to its minimum the TSI decreased by about 0.08 %. It appears likely from the ACRIM II results thus far that the cycle 22-23 minimum in TSI will occur during 1997, near the average solar cycle period of about 11 years after the cycle 21-22 minimum, and with a similar decrease relative to the maximum of cycle 22 in the 1990-1991 period.