Status of the XIS Orbital Calibration and Softwares K. Hayashida, N. Tawa, M. Nagai, H. Nakajima, M. Uchino, N. Anabuki, S. Katsuda, H. Uchida, H. Tsunemi.

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Status of the XIS Orbital Calibration and Softwares K. Hayashida, N. Tawa, M. Nagai, H. Nakajima, M. Uchino, N. Anabuki, S. Katsuda, H. Uchida, H. Tsunemi (Osaka Univ.), H. Matsumoto, H. Mori, H. Uchiyama, M. Ozawa, T. G. Tsuru, Y. Hyodo, M. Nobukawa, K. Koyama (Kyoto Univ.), T. Dotani, H. Murakami, A. Bamba, M. Ozaki, T.Anada (JAXA), D. Takei, S. Kitamoto (Rikkyo Univ.), T. Kato, S. Maeno, K. Mori (Miyazaki Univ), Y. Ishisaki (TMU), T. Kohmura (Kohgakuinn Univ.), E. Miller, B. LaMarr, S. E. Kissel, M. W. Bautz (MIT), and the Suzaku Team

Current Status of the XIS No significant change in the XIS hardware since the last Users’ Meeting 2007May SCI-ON for all the observations Peak ch of Mn K  from 55 Fe calibration sources / that at the lauch SCI-ON 0.98 FWHM of Mn K  from 55 Fe calibration sources 200eV 300eV 100eV SCI-ON SCI-OFF 2%/yr %/yr

Ver. 2 Processing & HEASOFT6.4 Ver. 2 processing started. –Full processing of the SCI-ON data HEASOFT v6.4 –Updates + New software xisnxbgen is introudced CALDB updated (as always) Processing FTOOLSCALDB for Processing CALDB for Users’ AnalysisAnalysis FTOOLS Updating Parameters Accuracy Check Data Products for Users Raw Data Science Results Quality of the CCD Data (accuracy of the energy scale etc) is significantly affected by the processing

Contamination on the XIS OBF until 2007Apr evaluated from E0102 obs. (ver.1.x products) Shown in the 2007May Users Meeting & Displayed on the Web in the Technical Description Page

Previous trend model used in CALDB2006 Current trend model used in CALDB2007Oct Contamination of XIS0 increases rapidly Ver.2 CALDB will be updated at the end of this Dec.

green = XIS black = XIS blue = XIS red = XIS XIS0,XIS3 spectra of E0102 Almost Similar

RXJ1856 observed on 2007Oct XIS0 XIS3 Current contami-model under-estimate Current contami-model over-estimate Observed Spectra of XIS0 and XIS3 agree well. No apparent difference in the absorber properties, except for the time evolution.

XIS1(BI) 2005Oct 2006Mar 2006Oct 2007Oct Factor of 2 Underestimate Below 0.3keV RJX1856

Contamination N_O vs N_C O/C=1/10; offset_N_C=0 O/C=1/6; offset_N_C=1.27 *)Error bars are 90% error for 2parameters confidence,i.e., delta  2=4.61 XIS0(2005) XIS1(2005) XIS2 ( 2006) XIS3(2005) XIS2 ( 2005) XIS1(2006) XIS0(2006) XIS3(2006)

Factor of 2 underestimate below 0.3keV Unable to improve the fit only with C & O Absorption by Heavier Element Absorption by H (or He) but too much ~10 21 cm^2 Constant Factor (Grading Problem at low energy?) Tune C and O absorption only Include absorption by H No apparent edge found

PKS Apr XIS1 XIS0 XIS3 Power * Abs Index  and N H free & common Normalization free &vary independently Users may encounter this level of inconsistency among sensors

Atmospheric Fluorescence Line When the telescope is looking at the shining Earth or its atmosphere, fluorescence lines of the Earth atmosphere (N-K, O-K) by Solar X-rays are contaminated in the observed spectra. Intensity and line ratio depends on the elevation angle from the Earth rim and the Solar activity. DAY EARTH 0 < DYE_ELV < 5 5 < DYE_ELV < < DYE_ELV < < DYE_ELV < 30 N-K (0.39keV) O-K (0.52keV)

Detected Intensity of N-K line can be used to measure the contamination thickness N-K line Day Earth 0 < DYE_ELV < 5 5 < DYE_ELV < < DYE_ELV < < DYE_ELV < < DYE_ELV <

Radius (mm) 12mm 0 5 N_C(10 18 cm -2 ) Radial Profile of Contamination from Atmospheric N-K, O-K 2005/11/ /5/ /2/ /8/1 XIS1 Model Profile impemented in the current CALDB for xissimarfgen N-K O-K

Radial Profile of Contamination from Atmospheric O-K for FI-CCD 2007/8/6 2007/1/ /11/2 2006/4/7XIS0 Under investigation

Cut-Off-Rigidity Dependence of the XIS NXB keV keV Count rate COR XIS0 XIS1 XIS2 XIS3 The COR dependence of the NXB can be used to model the XIS NXB. 1) Sort the NXB spectra from the Night Earth Database into each COR bin. 2) Calculate the appropriate weights of each COR bin for a given source observation. 3) Make the NXB spectrum for the given source observation by summing the sorted spectra with appropriate weights. Other parameters, such as PINUD of the HXD, can be used instead of the COR.

5-12keV NXB (integrated for 5ks) Raw Residual from COR2-Model XIS0XIS2 with “Orbit filter” -2005/9 Frequency Residual from PINUD-Model Tawa et al., 2008 PASJ in press

Reproducibility 5-12keV XIS NXB 2005Oct-2006Jun (Cut 2005Sep) Applying “Orbit Filter” 5ks integration –Duration>>5ks ParameterCORCOR2PINUD XIS04.4±0.5%3.5±0.7%2.8±0.9% XIS16.6±0.1%6.9±0.1%4.4±0.1% XIS25.7±0.4% 4.0±0.6% XIS33.3±0.9%2.4±1.2%3.8±0.8% We introduced a new COR database Tawa et al., 2008 % of the NXB

Case Study Target is (excess) diffuse emission over XIS FOV with comparable surface density as the average CXB Exposure 100ks For 5-12keV band integrated counts for the whole area of an FI-CCD –CXB: 9.7x10 -3 c/s –Target Diffuse Emission: 9.7x10 -3 c/s (assumed) –NXB: 52 x10 -3 c/s Statistical Error ΔI stat = 0.84x10 -3 c/s Fluctuation of the CXB (estimated) ΔI CXB = 1.5x10 -3 c/s NXB reproducibility (PINUD) ΔI NXB = 1.8 x c/s Tawa et al., 2008 PASJ in press Comparable *) CXB fluctuation dominates when we take 1-7keV band.

xisnxbgen is introduced HEASOFT6.4 to make an appropriate NXB spectra for a given source observation 1. Create an estimated NXB file 'xis1_nxb.pi' in the DET coordinates region 'ds9.reg‘ % xisnxbgen xis1_nxb.pi xis1_src.pi DETREG ds9.reg suzaku.orb none 2.Create an estimated NXB file 'xis1_nxb.pi‘ in the SKY coordinates region 'ds9.reg' including the calibration source area, and an image in the energy range of 274 <= PI <= 548 (1-2 keV). % xisnxbgen xis1_nxb.pi xis1_src.pi SKYREG ds9.reg suzaku.orb suzaku.att pixq_and=0 pi_min=274 pi_max=548 We (XIS team) had been providing perl scripts and the NXB database independent to the HEASOFT/CALDB. The new ftool xisnxbgen is simper to use, and the NXB data base is now included in the CALDB. See Detail by fhelp We have to update every half a year at least