From SCHUEHLE@sumop1.nascom.nasa.gov Tue Nov 18 16:43:38 2003 Date: Wed, 10 Mar 1999 16:55:14 GMT From: SCHUEHLE@sumop1.nascom.nasa.gov Reply-To: sumer-soft@esa.nascom.nasa.gov To: sumer-soft@esa.nascom.nasa.gov Cc: SCHUEHLE@sumop1.nascom.nasa.gov Subject: SUMER-SOFT: SUMER sensitivity change The intercalibration_1 data of 1998 have been analysed by Joerg Hollandt (PTB), and the results give us for the first time some quantitative information about a sensitivity change of SUMER as a result of the SOHO loss period in 1998. The SUMER part of the Intercal_1 JOP monitors the intensity of the lines of He I (584A), Mg X (609A, 624A), Ne VIII (770A), and N V (1238A) at quiet Sun locations since the beginning of the SOHO mission. These data are well suitable to track the sensitivity of the instrument. Up to June 1998 the data prove that there was no sensitivity loss of the SUMER instrument during the entire time period starting in March 1996. The first intercal_1 measurement campaign after the SOHO accident, however, performed on 6 November 1998 indicates for the first time a loss of sensitivity of the SUMER instrument. This average sensitvity change at the wavelengths mentioned above is about 20%. Two intercal_1 measurements have been done, one with the A-Detector, one with the B-Detector with consistent results. Thus it is most likely that the instrument suffered from the SOHO accident with the temperature excursions that happened during the 3 months period in such a way that contaminants, that have accumulated at cold surfaces during three years of nominal operations, have been released and distributed inside the instrument. These contaminants have obviously not disappeared when the door was re-opend after the recovery of SOHO. For the radiometric calibration of the SUMER data after the recovery we will have to correct our calibration curves by this 20% factor until we might have more detailed results on the sensitivity change over full the spectral range. Further Intercal_1 measurements will be made to confirm these results which are always subject to large variations due to the solar variability. Udo Schuehle, GSFC, 10 March 199