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Author name code: edmonds
ADS astronomy entries on 2022-09-14
author:"Edmonds, Frank N." 

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Title: A Statistical Analysis of NAID1 Profile Fluctuations at the
    Center of the Solar Disk - Part One - Data Reduction and Resolvable
    Velocities
Authors: Edmonds, F. N., Jr.; Hsu, J. -C.
1983SoPh...83..217E    Altcode:
  Three radial-velocity fluctuation arrays V(Δλ, Y) and line-formation
  fluctuation arrays L(Δλ, Y),where Δλ is wavelength displacement
  from the center of NaI D<SUB>1</SUB> and Y is displacement on the Sun's
  surface along the spectrograph slit, were obtained from Sacramento
  Peak Observatory spectrograms. The variations of these line profile
  fluctuations are qualitatively described. The RMS<SUB>υ</SUB>'s,
  coherences, and power spectra shapes for V(Δλ, Y) fluctuations are
  examined at different Δλ with the corresponding effective heights
  of formation calculated with Mein weighting functions.

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Title: A statistical analysis of resolvable velocities obtained from
    solar Na I D<SUB>1</SUB> profile fluctuations.
Authors: Edmonds, F. N., Jr.; Hsu, J. -C.
1983BAAS...15..615E    Altcode:
  No abstract at ADS

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Title: A feasibility study of calibrating stellar photographic
    equivalent widths against solar photoelectric equivalent widths.
Authors: Edmonds, F. N., Jr.
1978PASP...90..322E    Altcode:
  The feasibility of reducing average systematic-plus-random errors in
  stellar photographic equivalent widths to S 5% by a direct calibration
  method is examined. Solar and stellar 2.5 A mm ' spectrograms covering
  the same wavelength range are exposed, developed, and reduced as
  similarly as possible, and the calibration of the solar equivalent
  widths against those obtained from A High-Resolution Spectral
  Atlas of the Solar Irradiance from 380 to 770 Nanometers is used
  to correct the stellar equivalent widths for systematic errors. The
  effects on overall accuracy of the procedure due to collimator (slit)
  illumination, development uniformity, density-to-intensity calibration,
  fixing continuum, width of profile measured, and filtering of noise are
  investigated. Overall procedure accuracy is estimated by comparison
  of calibrated (i.e., corrected) equivalent widths for Arcturus with
  those obtained from A Photometric Atlas of the Spectrum of Arcturus,
  and from reticon spectra taken at McDonald Observatory. The 5% average
  accuracy upper limit is feasible. The study also produces several
  cautions and recommended improvements for the procedure. Its potential
  for standardizing stellar equivalent widths is briefly discussed. Key
  words: equivalent widths-photographic spectra

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Title: A Feasibility Study of Calibrating Stellar Photographic
    Equivalent Widths against solar Photoelectric Equivalent Widths.
Authors: Edmonds, F. N., Jr.
1977BAAS....9..635E    Altcode:
  No abstract at ADS

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Title: Spectral analyses of solar photospheric fluctuations. V:
    A two-dimensional analysis of granulation at the center of the disk.
Authors: Edmonds, F. N., Jr.; Hinkle, K. H.
1977SoPh...51..273E    Altcode:
  Successful subtraction of instrumental background variations has
  permitted spectral analyses of two-dimensional measurement arrays of
  granulation brightness fluctuations at the center of the disk, arrays
  obtained from Stratoscope I, 1959B-flight, high-resolution frames B1551
  and B3241. RMS's, uncorrected for instrumental blurring, are 0.0850 of
  mean intensity for B1551 and 0.0736 for B3241, somewhat higher than
  other determinations. These between-frame and between-investigation
  differences probably result from a combination of calibration errors,
  frame resolution differences, and, most likely, granulation pattern
  differences.

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Title: A Two-Dimensional Spectral Analysis of Solar Granulation at
    the Center of the Disk
Authors: Edmonds, F. N., Jr.; Hinkle, K. H.
1976BAAS....8..311E    Altcode:
  No abstract at ADS

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Title: Spectral Analyses of Solar Photospheric Eluctuations. IV:
    The Low-Wavenumber Power of Granulation Brightness Eluctuations
Authors: Edmonds, F. N., Jr.
1975SoPh...44..293E    Altcode:
  Synthetic one-dimensional scans of brightness fluctuations are generated
  from intergranulegranule profiles (IGP), which approximate observed
  scans of granulation fluctuations except that the local (i.e. IGP)
  mean intensity is kept constant. Comparing the power spectrum of such
  scans with the power spectrum of observed scans shows that nearly
  two thirds of the low-wavenumber (k &lt; 0.0025 km<SUP>-1</SUP>)
  granulation power is due to this variable mean effect. This result
  favors the interpretation of granulation as turbulent thermal convection
  but cannot rule out the laminar convection interpretation.

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Title: Convective Flux in the Solar Photosphere as Determined from
    Fluctuations
Authors: Edmonds, F. N., Jr.
1975BAAS....7..362E    Altcode:
  No abstract at ADS

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Title: Convective Flux in the Solar Photosphere as Determined from
    Fluctuations
Authors: Edmonds, F. N., Jr.
1974SoPh...38...33E    Altcode:
  The fractional convective flux πF<SUB>c</SUB>(x<SUB>c</SUB>/πF)
  is computed for the effective level x<SUB>c</SUB>= logτ<SUB>c</SUB> =
  0.125, using bi-dimensional co-spectra for relative continuum-brightness
  fluctuations ΔI and radial velocity fluctuations ΔV measured for
  the C<SUB>I</SUB> 5052.16 spectral line. A more uncertain flux for
  x<SUB>Fe</SUB> ≈ - 0.9 is obtained for the Fe<SUB>I</SUB> 5049.83
  line. Since the results (Figure 1) incorporate current uncertainties
  in RMS<SUB>ΔI</SUB>, RMS<SUB>ΔV</SUB> and RMS<SUB>ΔT</SUB>(x),
  where ΔT are photospheric temperature fluctuations, they must be
  considered qualitative until these uncertainties are appreciably
  reduced. The requirement that the fractional convective flux &lt; 1,
  places restrictions on these uncertainties which suggest that current
  RMS<SUB>ΔT</SUB>(x)'s are too large.

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Title: Statistical Line Blanketing in
    Arcturus. I. Blanketing-Coefficient Description of Observations
Authors: Edmonds, Frank N., Jr.
1973PASP...85...24E    Altcode:
  A statistical description of line blanketing is presented for Arcturus
  (a Boo, K2 IlIp, V = +0.06) which is based on equivalent widths and
  identifications of roughly 10,000 spectral lines within the wavelength
  region AA3600-25,000 A. Equivalent-width contributions or blanketing
  coefficients for lines grouped as to equivalent width and identification
  are given for 100 A wavelength intervals for A &lt; 9000 A and 500 A
  intervals for A&gt; 9000 A (Tables I and II). Strong lines are listed
  individually (Table III), and the variation or scatter of blanketing
  within intervals is described. Corrections to this description for
  limitations in the observations and their analysis are discussed. Key
  words: line blanketing - statistics of spectral lines - spectroscopy

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Title: Spectral Analyses of Solar Photospheric
    Fluctuations. III. Bi-Dimensional Power, Coherence and Phase Spectra
    of Deep-Seated Radial Velocity and Photometric Fluctuations
Authors: Edmonds, Frank N., Jr.; Webb, Carol J.
1972SoPh...25...44E    Altcode:
  Fluctuations measured from a time sequence of high-resolution,
  high-dispersion Sacramento Peak Observatory spectrograms and
  previously analyzed by computing one-dimensional temporal and spatial
  spectra (Edmonds et al., 1965), are re-analyzed using bi-dimensional
  (temporal and spatial) power, coherence and phase spectra computed by
  fast-Fourier-transform techniques. The fluctuations measured are radial
  velocity for the FeI 5049.83, CrI 5051.91 and CI 5052.16 spectral lines,
  continuum brightness, and equivalent width and central intensity of the
  CI line. The bidimensional spectra, particularly those of coherence
  and phase, allow isolating different components of the fluctuations
  to a degree not possible in the one-dimensional analyses.

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Title: Line Blanketing in Arcturus - Statistical Descriptions of
    Observations.
Authors: Edmonds, F. N., Jr.; Morgan, T. E.
1972BAAS....4..236E    Altcode:
  No abstract at ADS

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Title: Spectral Analyses of Solar Photospheric
    Fluctuations. II. Profile Fluctuations in the Wings of the λ 5183. 6
    MgI b<SUB>1</SUB> Line
Authors: Edmonds, Frank N., Jr.
1972SoPh...23...47E    Altcode:
  Residual intensity fluctuation measurements within the wings of the
  λ5183.6 MgI b<SUB>1</SUB> line, obtained from two, high-resolution,
  high-dispersion, Sacramento Peak Observatory spectrograms, have been
  subtracted from intensity fluctuations in the adjacent continuum
  in order to isolate fluctuations associated exclusively with line
  formation. The useable spectral range for studying these lineformation
  fluctuations is restricted to wavelengths between 1040 and 7170 km
  because the subtraction increases the relative importance of noise
  and large-scale photographic variations across the spectrograms
  could not be completely removed. Power and cross-power (coherence and
  phase) spectra proved to be valuable diagnostic tools in isolating
  line-formation fluctuations.

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Title: Spectral Analyses of Solar Photospheric Fluctuations. I: Power,
    Coherence and Phase Spectra Calculated by Fast-Fourier-Transform
    Techniques
Authors: Edmonds, Frank N., Jr.; Webb, Carol J.
1972SoPh...22..276E    Altcode:
  The application of the fast-Fourier-transform (FFT) algorithm to
  calculating one-dimensional and bi-dimensional (temporal and spatial),
  power and cross-power (coherence and phase) spectra is examined for
  solar photospheric fluctuations. Alternative methods for smoothing raw
  spectra, direct averaging (employing various weights) and indirect
  truncation of the correlation function, are compared, and indirect
  smoothing is compared with spectra calculated by mean-lagged-product
  (MLP) methods. Besides providing the raw spectrum, FFT techniques
  easily allow computing a series of spectra with varying amounts of
  smoothing. From these spectra a range of satisfactory compromise
  between resolution and stability can be determined which helps in the
  interpretation of spectral trends, and in identifying more clearly the
  existence and significance of spectral features. For bi-dimensional
  spectra presented as contour plots, this range of satisfactory smoothing
  can be restricted, particularly when spectral trends must be represented
  by small-scale contours. Equivalent spectra (i.e. comparable equivalent
  degrees of freedom) computed or smoothed by different methods have
  minor, but not negligible, differences. Examination of these differences
  favors computing of FFT spectra smoothed by averaging for photospheric
  fluctuations.

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Title: Line Blanketing in Arcturus - Statistical Descriptions of
    Observations.
Authors: Edmonds, F. N.; Morgan, T. E.
1971BAAS....3..454E    Altcode:
  No abstract at ADS

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Title: Profile Fluctuations in the Wings of the λ5183.6 Mg b Line
    Due to Solar Photospheric Inhomogeneities
Authors: Edmonds, Frank N., Jr.
1971BAAS....3....6E    Altcode:
  No abstract at ADS

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Title: Bidimensional (Spatial and Temporal) Power, Coherence, and
    Phase Spectra for Solar Photospheric Spectral Lines
Authors: Edmonds, Frank N., Jr.; Webb, Carol Jean
1970BAAS....2..311E    Altcode:
  No abstract at ADS

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Title: A Comparison of the Statistical Stability and Spectral
    Resolution of Power Coherence and Phase Spectra of Solar Photospheric
    Fluctuations as Evaluated by Fast-Fourier-Transform Techniques and
    by the Mean-Lagged-Product Method
Authors: Edmonds, Frank N., Jr.; Webb, Carol Jean
1970BAAS....2Q.312E    Altcode:
  No abstract at ADS

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Title: The Radial Velocity of Arcturus Determined from Interferometric
    Spectra
Authors: Bopp, Bernard W.; Edmonds, Frank N., Jr.
1970PASP...82..299B    Altcode:
  From high-resolution, infrared, interferometric spectra, the radial
  velocity of Arcturus is deterrnined by simple measurements between
  superposed spectral tracings of the star and the sun. A velocity
  of -5.47 1 0.07 km/sec obtained from metal lines is comparable to a
  highly accurate result obtained by Petrie and Fletcher (1967) using
  standard methods. A velocity of -5.82 1 0.18 obtained from CO lines
  is interpreted in terms of a differentially expanding atmosphere.

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Title: The Infrared Spectrum of Arcturus
Authors: Montgomery, Earl F.; Connes, Pierre; Connes, Janine; Edmonds,
   Frank N., Jr.
1969ApJS...19....1M    Altcode:
  Equivalent widths of 1036 stellar lines have been measured from
  high-resolution interferometric spectra of Arcturus covering the
  spectral range 876&amp;3978 (1 129 A). Approximately 60 percent of
  these lines have been identified.

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Title: The Infrared Spectrum of Arcturus
Authors: Montgomery, Earl F.; Connes, Pierre; Connes, Janine; Edmonds,
   Frank N., Jr.
1969BAAS....1R.201M    Altcode:
  No abstract at ADS

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Title: The McDonald Coudé Sensitometer
Authors: Edmonds, Frank N., Jr.
1969BAAS....1..150E    Altcode:
  No abstract at ADS

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Title: Radiative transfer within a stellar absorption line. The
    contribution curves of fine-analysis methods.
Authors: Edmonds, F. N., Jr.
1969JQSRT...9.1427E    Altcode:
  No abstract at ADS

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Title: Contribution Curves in the Fine Analysis of Stellar Spectral
    Lines.
Authors: Edmonds, Frank N., Jr.
1967AJ.....72R.793E    Altcode:
  Three methods for the fine analysis of spectral lines are: (1)
  a straightforward combination of formulas arising from pertinent
  formal solutions to the equation of radiative transfer; (2) the
  Planckian-gradient method developed by Mugglestone; (3) the weight-
  saturation method developed by Pecker and others. These three methods
  are equivalent in that the formulas for one method can be obtained
  from those of another by simple integration by parts. In each of the
  three cases the formulas allow the computing of contribution curves
  which presumably show the relative contribution to line formation
  of the different layers of the model atmosphere used in the fine
  analysis. Computer programs have been developed for the three methods
  which compute the equivalent width and profiles of spectral lines under
  the assumption of formation by pure absorption. These programs have
  been designed to give contribution curves as well. The contribution
  curves for the same line abundance-model atmosphere situation are
  quite different for the three methods, and many of the properties of
  contribution curves which have been determined previously, using the
  weight saturation method, are not found in those for the formal solution
  or Planckian-gradient methods. These results lead to the conclusion that
  contribution curves are critically method dependent and do not provide
  information about the depth dependence of line formation. Previous
  determinations of effective depths of line formation based on or
  related to contribution curves are therefore suspect. The differences
  in the contribution curves of the three methods are such that the
  weight-saturation method weights more heavily the contribution from the
  upper layers of the atmosphere, while the Planckian-gradient method
  gives the least weight to these layers. One might expect, therefore,
  differences in equivalent widths and profiles computed by the different
  methods because of this difference in weighting. In particular, a
  method which weighted the most reliably determined layers of a model
  atmosphere would be preferable. Calculations testing these possibilities
  are under way, but results obtained so far indicate that differences
  between the methods are small, except when layer-dependent factors,
  such as the damping constant, critically affect equivalent widths.

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Title: Amplitude Distributions of Solar Photospheric Fluctuations
Authors: Edmonds, Frank N., Jr.
1967SoPh....1....5E    Altcode:
  Amplitude distributions, which are nearly Gaussian, have been calculated
  for radial velocity, continuum brightness, spectral line equivalent
  width and spectral line central residual intensity fluctuations measured
  from high-dispersion high-resolution spectrograms taken at the center
  of the solar disk. The RMS and skewness S for each distribution have
  been calculated in a manner which allows testing of the homogeneity
  of the granulation pattern (i.e. variations in its statistics across
  the solar disk and with time). Pattern inhomogeneity across the disk
  is strongly indicated, and further evidence suggesting appreciable
  pattern persistence over time intervals ≳ 15 minutes is presented. The
  possibilities for investigations of S and its associated bi-spectrum
  are discussed. The qualitative values of S obtained are shown not
  to be due to unusually bright, rising granules (though a statistical
  tendency towards such granules is possible). An attempt to explain S for
  continuum brightness fluctuations in terms of the nonlinear effects of
  Planckian emission and opacity fluctuations in a stratified photosphere,
  leads to contradiction with the measured amplitude distributions,
  a contradiction which is probably due to an oversimplified treatment
  of radiative transfer in an inhomogeneous photosphere.

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Title: Hydrogen-line Stark broadening functions
Authors: Edmonds, Frank N., Jr.; Schluter, Hans; Wells, Donald C.
1967MmRAS..71..271E    Altcode: 1967MmRAS..70..271E
  No abstract at ADS

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Title: A Spectrophotometric Analysis of Procyon. II. The Continuous
    Spectrum and Line Blanketing
Authors: Talbert, Freddie D.; Edmonds, Frank N., Jr.
1966ApJ...146..177T    Altcode:
  Photoelectric spectral scans of Procyon (F5 IV-V), obtained at McDonald
  Observatory, are combined with monochromatic magnitudes obtained by
  other observers to determine a measured continuous spectrum extending
  over the wavelength range X 3390-7460 and corrected for line blanketing
  measured from high-dispersion spectrograms. Line-blanketing measurements
  over the wavelength range X 3025- 4100 are also given. An attempt
  is made, with partial success, to correct further the continuum in
  the ultraviolet for blanketing by Balmer lines and unresolved lines,
  using primarily a straight-line extrapolation method which assumes that
  variations of color temperature with wavelength are small. Comparisons
  made between the measured continuous spectrum and the emergent flux
  predicted by a set of model atmospheres lead to the selection of a
  model atmosphere for the star.

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Title: The Evidence for an Oscillatory Component in Solar Granulation
    Brightness Fluctuations
Authors: Edmonds, Frank N., Jr.; McCullough, James R.
1966ApJ...144..754E    Altcode:
  The evidence for an oscillatory component of continuum brightness
  fluctuations, secondary maxima in temporal autocorrelation functions
  and power spectra, is examined critically with the provisional
  conclusion that such a component is theoretically possible and
  probably does exist. This component, with periods distributed about 5
  min, constitutes between 0.5 and 2 per cent of the total fluctuation
  power. The results from one analysis (725) suggest the coexistence of
  a second oscillatory component with periods distributed about 10 min,
  but the evidence is quite uncertain. There are also indications that
  the effects of spectral windows may be masking a stronger concentration
  of power of continuum brightness fluctuations to lower frequencies

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Title: A Coherence Analysis of Fraunhofer-Line Fine Structure and
    Continuum Brightness Fluctutations Near the Center of the Solar
    Disk. II
Authors: Edmonds, Frank N., Jr.
1966ApJ...144..733E    Altcode:
  Spatial cross-correlation analyses between fluctuations in radial
  velocity, V, and continuum brightness, I, have been carried out for four
  high-resolution spectrograms of the center of the solar disk obtained
  by Michard at the Pic-du-Midi Observatory. These analyses employed a
  coherence technique, and the results are quite similar to those recently
  obtained from an analysis of Sacramento Peak Observatory spectrograms
  by Edmonds, Michard, and Servajean. These results suggest that the
  V fluctuations contain a large-scale oscillatory component poorly
  correlated with the I fluctuations, and a smaller-scale convective
  component sigiiificantly correlated with the I fluctuations. An improved
  method for determining confidence limits for the results of a coherence
  analysis is presented in the Appendix, and these limits are applied
  to the results of four spatial coherence analyses. It is shown that
  these and other estimates of random errors of the statistical analysis
  cannot explain the differences between the different analyses. Whereas
  instrumental and atmospheric blurring may be important causes of these
  differences, it appears that for the most part they are real differences
  between different samples of photospheric inhomogeneities. The effects
  of the possible inclination of inhomogeneities found by Evans are
  also discussed. Confidence limits estimates further show that small
  variations with wavenumber k1 of power spectra and coherences cannot
  be considered significant.

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Title: The Determination of the Ultraviolet Continuum of Procyon
    from Balmer Line Profiles
Authors: Edmonds, F. N., Jr.
1966IAUS...26..159E    Altcode:
  No abstract at ADS

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Title: Observational studies of macroscopic inhomogeneities in the
    solar atmosphere. VII. A statistical analysis of photometric and
    kinematic inhomogeneities in the deep atmosphere
Authors: Edmonds, F. N.; Michard, R., Jr.; Servajean, R.
1965AnAp...28..534E    Altcode:
  No abstract at ADS

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Title: Asymmetry in the Brightness Fluctuations of Solar Granulation.
Authors: Edmonds, Frank N., Jr.
1965AJ.....70Q.674E    Altcode:
  Recent determination of the amplitude of solar photospheric temperature
  fluctuations as a function of optical depth (Edmonds, F. N., Jr.,
  Astrophys. J. 139, 1358) has been combined with the empirical model
  atmosphere of Pierce and Waddell (Mem. Roy. Astron. Soc. 68, 89) to
  calculate the skewness of source-function fluctuations and of emergent
  intensity fluctuations for assumed Gaussian and skew Gaussian-like
  distributions of the temperature fluctuations. These calculations
  show the skewness introduced into the emergent intensity fluctuations
  by the Planckian nature of the source function emission and by the
  stratification of the continuum contributing layers. This skewness
  is calculated as a function of position on the solar disk and is
  compared with that determined from a statistical analysis of solar
  granulation (Edmonds, F. N., Jr., Astrophys. J. Suppl. 6, 357). This
  photometric asymmetry of the granulation pattern is distinguished
  from the topological asymmetry (bright blobs surrounded by dark lanes)
  which is a manifestation of the upper boundary of the solar hydrogen
  convection zone.

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Title: The Continuous Spectrum and Line Blanketing for Procyon.
Authors: Talbert, F. D.; Edmonds, F. N., Jr.
1965AJ.....70Q.332T    Altcode:
  Low-dispersion photoelectric spectrum scans coupled with high-dispersion
  coude' plates have been used to construct an empirical continuum
  of Procyon corrected for line blanketing. Blanketing factors for
  25 A intervals in the range XA30254100 have been determined. The
  straight-line extrapolation method of Canavaggia and Chalonge has been
  used to determine the continuum in the near ultraviolet, ~x3650#000,
  and concordant results have been obtained from a determination based
  on matching observed and computed profiles of the Balmer lines in
  this wavelength range. Comparison of the empirical continuum with that
  predicted by several model atmospheres calculated for Procyon indicate
  moderate discrepancies in the ultraviolet. Possible causes for these
  discrepancies are discussed.

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Title: A Set of Non-Gray Model Atmospheres for Procyon.
Authors: Edmonds, Frank N., Jr.
1964ApJ...140..902E    Altcode:
  A set of eight non-gray model atmospheres has been calculated for
  the subgiant Procyon (F5 IV) using the Str6mgren-Swihart method for
  determining a temperature-optical depth relation which maintains
  constant flux. The eight models correspond to two values each of the
  parameters Te (effective temperature), A (hydrogen-to-metal ratio),
  and p (helium-to-hydrogen ratio). These models are compared with respect
  to the variation with optical depth and/or wavelength of the following
  properties: 0 = 5040/T, log Fe, log Pg, hydrogen convection zone, limb
  darkening, and emergent flux with associated continuum contribution
  functions. The problem of model selection (and parameter determination)
  is discussed in general terms. The parameter Te can be obtained from
  the observed continuous spectrum, but the parameters A and p cannot,
  as would be expected for the spectral class F5 IV. The parameters A
  and p cannot be determined effectively from the observed strengths of
  weak spectral lines or from the Stark of the Balmer lines. Conversely,
  the determination of these two parameters does not seem to be necessary
  for a spectrophotometric analysis of weak lines.

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Title: Source-Function and Temperature Fluctuations in the Solar
    Photosphere. I. The Isotropic Approximation.
Authors: Edmonds, Frank N., Jr.
1964ApJ...139.1358E    Altcode:
  Measurements of power spectra and RMS's for granulation brightness
  fluctuations across the solar disk, as obtained from 1957 Stratoscope
  photographs by Edmonds (1962), are used to determine source- function
  and temperature fluctuations as a function of optical depth in the
  solar photosphere. This involves the solving, by the Laplace-transform
  method employing polynomials, of integral equations which are based
  on an approximation of isotropy and which are quite similar to the
  formal solution of the equation of radiative transfer. Limitations
  imposed on the results by the measurements and the method employed are
  discussed. Source-function and temperature fluctuations are presented
  in Tables 2,3, and 4 and in Figures 3 and 4. These fluctuations
  increase with optical depth r, this increase becoming more gradual or
  leveling off around optical depth 1.5 as the result of the maximum
  in the granulation brightness fluctuations which occurs at 0 500 on
  the disk. The best determined RMS of temperature fluctuations at the
  same opticat depth is approximately 880 K at r = 0.32, 2720 K at r =
  0.80, 4540 K at r = 1.28, and 5140 K at r = 2.08. For the first three
  of these optical depths, the RMS's at the same geometricat tevet are
  880 K, 3600 K, and 7400 K.

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Title: On the Calculation of Equivalent Widths from Spectral-Line
    Profiles. II.
Authors: Edmonds, Frank N., Jr.
1964ApJ...139.1017E    Altcode:
  No abstract at ADS

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Title: Cross Correlation between Continuum Brightness and Radial
    Velocity Fluctuations in the Solar Photosphere.
Authors: Edmonds, Frank N., Jr.
1964AJ.....69Q.540E    Altcode:
  Spatial coherence and phase analyses of the cross correlation
  between continuum brightness and radial velocity fluctuations in
  the solar photosphere have been completed for four bigh-resolution
  spectrograms obtained by R. Michard at the Pic-du-Midi Observatory,
  and from a time sequence of 60 spectrograms taken by J. W. Evans at
  Sacramento Peak Observatory. The latter set includes the low-lying CI
  line N5052.16, and its analysis is a joint effort with Dr. R. Michard
  and Dr. R. Servajean at the Observatoire de Paris Meudon. The results
  give mean cross-correlation coefficients for each set of 0.35 and
  mean, nearly anti- phase coherences which are significant (&gt;0.5)
  in wavenumber ranges that lie between 10- and 2.5 X 1O-i km-'. These
  results, together with earlier analyses (Edmonds, Astrophys. J. 136,
  507,1962), indicate first that, in general, significant cross
  correlation does exist between continuum brightness and radial
  velocities fluctuations with scales less than 8000 km. Therefore,
  thermal- driven convection is an appreciable physical cause of the
  fluctuations. Secondly, there is considerable variation in behavior
  between different samples of solar photospheric inhomogeneities,
  these differences appearing in other statistical properties and in
  the tracings of the fluctuations. That stronger cross correlation
  is not found is possibly understandable in terms of the recent
  discovery by Evans (to be published in A strophysica Norvegica;
  also see abstract by J. W. Evans) that photospheric inhomogeneities
  may be strongly inclined to the radial direction. There are problems
  with this interpretation which arise from the small separation ($ 200
  km) between layers of continuum formation and of line formation. An
  analysis of the effects of random shifts in position on the solar disk
  between radial velocity and continuum brightness fluctuations predicts
  that orientation could reduce the cross-correlation coefficient only
  to about 0.75 and reduce coherence correspondingly in a manner which
  increases with wavenumber. Also, temporal coherence and phase analysis
  (Evans Michard, and Servajean, Ann. d'Astrophys. 26, 368,1963), provides
  a clearer picture as to the role played by oscillations (with periods
  around 300 sec) which are an important component of the radial velocity
  fluctuations but not of the contiuum brightness fluctuations. These
  results, together with more recent power spectra computed by Michard and
  Servajean suggest that whereas the oscillatory component is dominant
  for optical depths &amp;0.01, it is still appreciable in continuum-
  forming depths &gt;1.0.

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Title: On the Calculation of Equivalent Widths from Spectral-Line
    Profiles.
Authors: Edmonds, Frank N., Jr.
1963ApJ...137..470E    Altcode:
  The determination of equivalent width from a line profile in terms
  of Hjerting functions requires knowledge of the scale factor = A /V,
  where AX is the displacement in wavelength from the line's center and V
  is the Hjerting function argument. Tables are given in Section II which
  will allow the determination of p for a profile Pk(AXk) evaluated only
  at three values of AX,. Necessary factors to compute the equivalent
  width, based on fitting a Hjerting function to these points, are also
  tabulated. More general numerical integration formulae for determining
  the equivalent width, based on Hjerting functions, are discussed in
  Section III, and the weights and divisions V, are tabulated As shown
  in Section IV, these formulae will give greater accuracy for fewer
  divisions than methods now in use. For computed profiles, this should
  effect a worthwhile reduction in computational effort.

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Title: A Coherence Analysis of Fraunhofer Line Fine Structures and
    Continuum Brightness Fluctuations Near the Center of the Solar Disk.
Authors: Edmonds, Frank N., Jr.
1962ApJ...136..507E    Altcode:
  Cross-correlation analyses between fluctuations in radial velocity
  V and continuum brightness I have been carried out for four sets of
  measurements made near the center of the solar disk: those obtained
  from a McMath-Hulbert spectrogram (w18), those of Richardson and
  Schwarzschild (1950) (RS), those of Plaskett (1954) (P), and those
  of Servajean (1961) (S). in addition, cross-correlation analyses
  between fluctuations in line equivalent width W and fluctuations
  in V and in I have been applied to the w18 measurements. These
  analyses employed a coherence technique which gives the coherence
  or cross- correlation between the Fourier components of the same
  wavelength for each set of fluctuations and the phase difference
  (across the solar disk) between these Fourier components (Figs. 4 5
  6 8 10 12). The analyses also computed power spectra (Figs. 3, 7,
  9, 11), r.m.s. `5, and filtered and unfiltered cross-correlations
  (Table 2). A significant VI coherence with 180 phase difference was
  found in the wavelength range km (on the surface of the sun) for the
  RS measurements; no VI coherence was found for the w18 measurements;
  and the S and P measurements gave inconclusive results. A significant
  1W coherence with 1800 phase difference for wavelengths &gt; 5000 km,
  and no VW coherence was obtained for the w18 measurements. These results
  cannot be explained in terms of differences in the solar atmosphere
  levels making an appreciable contribution to line formation and to
  continuum formation. The negative nature of the 1W cross-correlation
  seemingly can be explained only in terms of 4-10 per cent increases
  in the level of microturbulence for dark areas on the solar surface,
  with corresponding decreases for the bright areas The inconsistent
  picture presented by the four VI coherence analyses can be explained
  in terms of a negative VI cross-correlation existing for wavelengths
  &lt; 5000 km plus certain differences in instrumental and atmospheric
  resolution for the four sets of measurements. However, an explanation
  in terms of a heterogeneous convection pattern at the sun's surface
  seems more reasonable. The nature of the radial-velocity power spectra
  and the effects producing a low cross-correlation are also discussed.

---------------------------------------------------------
Title: A Coherence Analysis of Fraunhofer Line Radial Velocity Fine
    Structure and Continuum Brightness Fluctuations near the Center of
    the Solar Disk.
Authors: Edmonds, Frank N., Jr.
1962AJ.....67Q.271E    Altcode:
  Cross correlation analyses between fluctuations in radial velocity
  V and continuum brightness I have been carried out for four sets of
  measurements made near the center of the solar disk; those obtained
  from a McMath-Hulbert spectrogram (w18), those of R. S. Richardson
  and M. Schwarzschild (Astrophys. J. 111, 351, 1950) (RS), those
  of H. H. Plaskett (Monthly Notices Roy. Astron. Soc. 114, 251,
  1954) (P), and those of R. Servajean (Ann. Astrophys. 24, 1, 1961)
  (S). These analyses employed a coherence technique which gives the
  coherence or cross correlation between the Fourier components of the
  same wavelength for each set of fluctuations, and the phase difference
  (across the solar disk) between these Fourier components. The analyses
  also computed power spectra, RMS's and filtered and unfiltered cross
  correlations. A significant VI coherence with 180~ phase difference
  was found in the wavelength range 1200-5200 km (on the surface of
  the sun) for the RS measurements, no VI coherence was found for the
  w18 measurements, and the S and P measurements gave inconclusive
  results. These results cannot be explained in terms of differences
  in the solar atmosphere levels making an appreciable contribution to
  line formation and to continuum formation. The inconsistent picture
  presented by the four VI coherence analyses can be explained in terms
  of a negative VI cross correlation existing for wavelengths ~ 5000 km
  plus certain differences in instrumental and atmospheric resolution
  for the four sets of measurements. However, an explanation in terms
  of a heterogeneous convection pattern at the sun's surface seems
  more reasonable.

---------------------------------------------------------
Title: A Statistical Photometric Analysis of Granulation across the
    Solar Disk.
Authors: Edmonds, Frank N., Jr.
1962ApJS....6..357E    Altcode:
  Twenty-five microphotometer scans from Stratoscope granulation
  photographs distributed across the solar disk have been analyzed
  statistically to yield amplitude distributions, power spectra, and
  related quantities. Power spectra have been calculated for twenty
  additional scans of the center of the disk obtained by Schwarzschild
  (1959). A difference in calibration procedures in part explains
  RMS's that are nearly twice those obtained by sChwarzschild. The
  range of wave numbers k1 for which power-spectra calculations yield
  quantitative results is limited by uncertainties in low-wave-number
  filtering to k1 &gt; 0.001 km-' and by what is probably instrumental
  noise in the photographs to k1 &lt; 0.008 km-'. This upper limit
  is further reduced to k1 &lt; 0.004 km-' or less by instrumental
  corrections, using the method of Uberoi (1955b) generalized for
  foreshortening. These corrections account for the instrumental profile
  of the Stratoscope (determined from the limb of the solar disk),for
  focus of the photographs, and for the analyzing spot and focus of the
  microphotometer. The variation in the relative brightness fluctuation
  RMS across the solar disk (Figs. 4 and 9) is characterized by an
  increase from 0.14 for the central regions of the disk (out to 0 20
  , to 0.20 at 0 50 and then a sharper decrease, which levels off and
  reverses itself at 0 70 . Ezamination of limb photographs attributes
  this reversal to the emerging photometric importance of a large-scale,
  essentially unforeshortened, pattern which does not seem to be
  instrumental or telluric aild may not be part of the normal photosphere
  granulation. Scatter in the RMS of adjacent scans can be attributed to
  statistical inhomogeneities in the granulation pattern. The amplitude
  distributions are approximately Gaussian (Fig. 3) with moderate positive
  skewness. The power spectra (uncorrected, Tables 3 and 4 and Figs. 2
  and 5; corrected, Table 8 and Fig. 10) are characterized by a rapid
  decrease with increasing k,. A steepening of this falling-off toward
  the limb is probably due to the large-scale pattern. The variation in
  the brightness fluctuation RMS across the disk has been converted to
  the RMS of temperature fluctuations as a function of optical depth,
  using the Eddington-Barbier approximation (Fi . 11). The maximum of
  brightness RMS at 0 50 becomes a maximum in temperature RMS of 290
  K at r 0.65. An inhomogeneous model solar atmosphere based on these
  temperature fluctuations has been constrncted (Table 9), and, using
  the&amp;etical results of Ledoux, Schwarzschild, and Spiegel (1961),
  an associated velocity spectrum and convective transport have been
  roughly determined. Scans of two special regions have been analyzed:
  a region at the center of the disk, which is characterized by a low
  RMS and a flattened spectrum, and a facular region, which shows the
  normal spectrum and ouly a slightly higher RMS.

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Title: On Solar Granulation.
Authors: Edmonds, Frank N., Jr.
1960ApJ...131...57E    Altcode:
  From the examination of high-quality stratoscope photographs of solar
  granulation it has been determined that the fading of the granulation
  pattern occurs primarily in the region 60 &lt; 0 &lt; 78 and that
  the fading granulation is replaced by a larger, low-contrast pattern
  observable out to 0 87 . Inhomogeneities in the granulation pattern
  have also been observed. These consist of low-contrast regions which
  seem to persist for periods longer than 10 minutes and small-scale
  regions which seem to evolve with the normal pattern

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Title: Letters to the Editor CA II Emission in the Spectrum of
    Procyon.
Authors: Kraft, Robert P.; Edmonds, Frank N., Jr.
1959ApJ...129..522K    Altcode:
  No abstract at ADS

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Title: The Coefficients of Viscosity and Thermal Conductivity in
    the Hydrogen Convection Zone.
Authors: Edmonds, Frank N., Jr.
1957ApJ...125..535E    Altcode:
  The coefficient of viscosity, , the coefficient of thermal conductivity
  by conduction, X , and the coefficient of the thermal conductivity by
  radiation, X , have been calculated for stellar material (85 per cent
  hydrogen, 15 per cent helium) over temperature and pressure ranges
  which should include the hydrogen convection zones of most stars.

---------------------------------------------------------
Title: The DEBYE-HÜCKEL Effect and Statistical Theories for Collision
    Broadening.
Authors: Edmonds, Frank N., Jr.
1956ApJ...123...95E    Altcode:
  The theory of Debye and for electrolytes is shown to be valid and
  pertinent for ionized gases of astrophysical interest Corrections to
  statistical theories of collision broadening due to the effect are shown
  to be negligible in the cases of linear and quadratic Stark broadening
  of the spectral lines of ions In Appendix I, Debye- effect corrections
  are calculated for the related problem of the average distance to the
  nearest charged particle.

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Title: Noncoherent Scattering due to Collisions. I. Zanstra's Ratio
    of Coherent to Uncorrelated Noncoherent Scattering.
Authors: Edmonds, Frank N., Jr.
1955ApJ...121..418E    Altcode:
  A quantum-theory formulation of the problem of noncoherent scattering
  due to collisions is presented in a general form and then made
  equivalent to Zanstra's classical oscillator formulation by a set
  of assumptions. These assumptions are examined critically as an
  indirect method of determining whether Zanstra's results are correct
  for statistical broadening. It would seem that Zanstra's ratio of
  coherent to uncorrelated noncoherent scattering is too large by at
  least a factor of 20, and the coherent component is not strictly
  coherent. The validity of evaluating Zanstra's results for impact
  broadening by this method is bnefly discussed.

---------------------------------------------------------
Title: Compton Scattering by Electron Atmospheres. II. Problems with
    Incident Normal Flux.
Authors: Edmonds, Frank N., Jr.
1954ApJ...119..425E    Altcode:
  The problem of the transfer of radiation in an atinosphere of free
  electrons is solved in the first approximation for two sets of boundary
  conditions involving an incident normal flux, that of the planetary
  nebula problem and that of no incident diffuse radiation field. In
  the solution, account is taken of the noncoherent character of the
  electron scattering due to the Doppler shifts arising from a Maxwellian
  distribution of thermal velocities, the red shift of the Compton
  effect, and a non-Doppler blue shift arising from thermal motions
  and first pointed out by Dirac. The latter two effects, designated as
  "Compton scattering," are shown to produce asymmetries in spectral lines
  which would be very difficult to detect for very high temperatures,
  as they are much smaller than the thermal broadening. In an appendix,
  application of the solutions obtained to multiple Compton scattering
  of low-energy gamma radiation is considered.

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Title: Compton Scattering by Electron Atmospheres. I. The Schuster
    Problem.
Authors: Edmonds, Frank N., Jr.
1954ApJ...119...58E    Altcode:
  The problem of the transfer of radiation in an atmosphere of free
  electrons is solved in the first approximation under the conditions
  of the standard Schuster problem of line formation. In the solution,
  account is taken of the noncoherent character of the electron scattering
  due to the Doppler shifts arising from a Maxwellian distribution
  of thermal velocities, the red shift of the Compton effect, and
  a non-Doppler blue shift arising from thermal motions and first
  pointed out by Dirac. The latter two effects, designated as "Compton
  scattering," are shown to produce asymmetries in spectral lines which
  would be very difficult to detect for stellar temperatures, as they
  are much smaller than the thermal broadening.

---------------------------------------------------------
Title: Compton Scattering by Electrons with a Maxwellian Distribution
    of Thermal Velocities.
Authors: Edmonds, Frank N., Jr.
1953ApJ...117..298E    Altcode:
  The theory of the Compton effect is applied to the problem of scattering
  of radiation by electrons with a Maxwellian distribution of thermal
  ; and a spectral distribution function for scattered radiation is
  obtnined in the second approximation. This function, equation (26), is
  asymmetric, and the frequency shift of scattered radiation corresponding
  to this asymmetry is given by - cos 0 - t m0 c2 (kv-3kT), where p is
  the incident frequency, p' the scattered frequency, 0 the angle of
  scattering, and the other symbols have their usual meaning. The red
  shift in this expression is due to the Compton effect, while the blue
  shift is a result of the thermal motions of the electrons, as first
  pointed out by Dirac.

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Title: Scattering by a Moving Electron Atmosphere and its Effect on
    Spectral LINES.I. the Schuster Problem.
Authors: Edmonds, Frank N., Jr.
1950ApJ...112..307E    Altcode:
  The problem of the transfer of radiation in an atmosphere of free
  electrons undergoing differential expansion is solved in the first
  approximation under the conditions of the standard Schuster problem
  of line formation. It is further assumed that electron scattering
  is in accordance with the frequency-independent Thomson scattering
  coefficient, the Rayleigh phase function, and a Maxwellian distribution
  of thermal velocities. In the solution, account is taken of the
  noncoherent character of the scattering due to velocities arising
  from the thermal and mass motions of the electrons. The solution
  for radiation emerging from the atmosphere contains terms for
  unscattered and scattered radiation. The latter contains a function
  which represents the spectral distribution of scattered radiation for
  incident monochromatic radiation. The shape of this function, which is
  due to the thermal motions of the electrons, produces broad spectral
  lines characterized by a shallow center and extended wings. Further,
  a shift of this spectral distribution function resulting from the
  differential expansion of the atmosphere produces asymmetries in
  spectral lines. Two numerical examples of these effects have been
  calculated.

---------------------------------------------------------
Title: Scattering by a Moving Electron Atmosphere and its Effect on
    Spectral Lines. II. The Planetary Nebula Problem.
Authors: Edmonds, Frank N., Jr.
1950ApJ...112..324E    Altcode:
  The problem of the transfer of radiation in a planetary nebula
  undergoing differential expansion and consisting of free electrons in
  thermal motion is solved in the first approximation for the emergent
  radiation. In the solution, account is taken of the noncoherent
  character of the scattering, which is due to the thermal and mass
  motions of the electrons. The solution for the emergent radiation
  represents radiation of the incident flux from the central star, which
  has suffered scattering by electrons in the nebula. The solution
  contains a function which describes the spectral distribution of
  scattered intensity for incident monochromatic flux. The shape of
  this function produces in the solution a broadening of spectral lines
  characterized by a shallow center and extended wings. A shift of this
  function, due to the differential expansion of the nebula, produces
  shifts in the lines. A numerical example has been worked out.