2015
DOI: 10.1007/s11207-015-0827-4
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Intensity Conserving Spectral Fitting

Abstract: The detailed shapes of spectral line profiles provide valuable information about the emitting plasma, especially when the plasma contains an unresolved mixture of velocities, temperatures, and densities. As a result of finite spectral resolution, the intensity measured by a spectrometer is the average intensity across a wavelength bin of non-zero size. It is assigned to the wavelength position at the center of the bin. However, the actual intensity at that discrete position will be different if the profile is … Show more

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Cited by 13 publications
(14 citation statements)
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“…We therefore take an additional step in order to measure the line center position as accurately as possible. We apply a procedure called Intensity Conserving Spectral Fitting (ICSF; Klimchuk et al 2016), which accounts for the finite size of the spectral bins. A spectrometer measures the average intensity over a bin, and this intensity is typically assigned to the wavelength position at bin center.…”
Section: Data Analysis and Resultsmentioning
confidence: 99%
“…We therefore take an additional step in order to measure the line center position as accurately as possible. We apply a procedure called Intensity Conserving Spectral Fitting (ICSF; Klimchuk et al 2016), which accounts for the finite size of the spectral bins. A spectrometer measures the average intensity over a bin, and this intensity is typically assigned to the wavelength position at bin center.…”
Section: Data Analysis and Resultsmentioning
confidence: 99%
“…In the bottom row of Figure 2 we present the RB asymmetries calculated following the same approach as used by De Pontieu et al (2009) which interpolates in the wavelength axis using spline. We tested the Klimchuk et al (2016) interpolation method (not shown here) and the calculated RB asymmetries do not differ from the one using spline interpolation shown in Figure 2.…”
Section: Observables and Constraintsmentioning
confidence: 99%
“…In the first and second columns of Table 1, we provide the date and µ-value of each observation, where µ is defined as the cosine of the angle between the surface normal and the LOS to the observer of the centre of the FOV (Thompson 2006) 1 We have used Level-2 IRIS raster data in which all instrumental effects such as flat-fielding, dark currents, offsets and thermal orbital variations have been accounted for, so as to make it suitable for scientific analysis 2 . Further, we apply the procedure called the Intensity Conserving Spectral Fitting (ICSF; Klimchuk et al 2016) on the original line profiles, as explained in Paper I. We use single Gaussian fitting routines 3 on the resultant spectral lines, provided in Solarsoft (Freeland & Handy 1998) for analysing the data.…”
Section: Observationsmentioning
confidence: 99%