scholarly journals Inference about complex relationships using peak height data from DNA mixtures

2021 ◽  
Author(s):  
Peter J. Green ◽  
Julia Mortera
Keyword(s):  
Peak Height ◽  
Dna Mixtures ◽  
Complex Relationships ◽  
Height Data

The information gain from peak height data in DNA mixtures

2018 ◽  
Vol 36 ◽  
pp. 119-123 ◽  
Author(s):  
K. Slooten
Keyword(s):  
Information Gain ◽  
Peak Height ◽  
Dna Mixtures ◽  
Height Data

scholarly journals Proposed Framework for Comparison of Continuous Probabilistic Genotyping Systems amongst Different Laboratories

2021 ◽  
Vol 1 (1) ◽  
pp. 33-45
Author(s):  
Dennis McNevin ◽  
Kirsty Wright ◽  
Mark Barash ◽  
Sara Gomes ◽  
Allan Jamieson ◽  
...  
Keyword(s):  
Numerical Methods ◽  
Analytical Solutions ◽  
Peak Height ◽  
Dna Profiling ◽  
Likelihood Ratios ◽  
Dna Mixtures ◽  
Individual Laboratory ◽  
Multiple Variables

Continuous probabilistic genotyping (PG) systems are becoming the default method for calculating likelihood ratios (LRs) for competing propositions about DNA mixtures. Calculation of the LR relies on numerical methods and simultaneous probabilistic simulations of multiple variables rather than on analytical solutions alone. Some also require modelling of individual laboratory processes that give rise to electropherogram artefacts and peak height variance. For these reasons, it has been argued that any LR produced by continuous PG is unique and cannot be compared with another. We challenge this assumption and demonstrate that there are a set of conditions defining specific DNA mixtures which can produce an aspirational LR and thereby provide a measure of reproducibility for DNA profiling systems incorporating PG. Such DNA mixtures could serve as the basis for inter-laboratory comparisons, even when different STR amplification kits are employed. We propose a procedure for an inter-laboratory comparison consistent with these conditions.

scholarly journals Is peak height important for the statistical evaluation of the weight of evidence in DNA mixtures?

2015 ◽  
Vol 5 ◽  
pp. e395-e397
Author(s):  
A. Caglià ◽  
L. Baldassarri ◽  
I. Boschi ◽  
F. Scarnicci ◽  
V.L. Pascali
Keyword(s):  
Statistical Evaluation ◽  
Peak Height ◽  
Weight Of Evidence ◽  
Dna Mixtures

An objective, rapid and reproducible method for scoring AFLP peak-height data that minimizes genotyping error

2008 ◽  
Vol 0 (0) ◽  
pp. 080310190901533-??? ◽  
Author(s):  
R. WHITLOCK ◽  
H. HIPPERSON ◽  
M. MANNARELLI ◽  
R. K. BUTLIN ◽  
T. BURKE
Keyword(s):  
Peak Height ◽  
Genotyping Error ◽  
Reproducible Method ◽  
Height Data

An objective, rapid and reproducible method for scoring AFLP peak-height data that minimizes genotyping error

2008 ◽  
Vol 8 (4) ◽  
pp. 725-735 ◽  
Author(s):  
R. WHITLOCK ◽  
H. HIPPERSON ◽  
M. MANNARELLI ◽  
R. K. BUTLIN ◽  
T. BURKE
Keyword(s):  
Peak Height ◽  
Genotyping Error ◽  
Reproducible Method ◽  
Height Data

Specific rotation measurements from peak height data, with a Gaussian peak model

Talanta ◽  
1989 ◽  
Vol 36 (4) ◽  
pp. 473-478 ◽  
Author(s):  
P RICE ◽  
Y SHAO ◽  
S ERSKINE ◽  
T TEAGUE ◽  
D BOBBITT
Keyword(s):  
Specific Rotation ◽  
Peak Height ◽  
Gaussian Peak ◽  
Peak Model ◽  
Height Data

scholarly journals Dynamic Channel Selection of Microwave Temperature Sounding Channels under Cloudy Conditions

2020 ◽  
Vol 12 (3) ◽  
pp. 403 ◽  
Author(s):  
Luyao Qin ◽  
Yaodeng Chen ◽  
Tianlei Yu ◽  
Gang Ma ◽  
Yang Guo ◽  
...  
Keyword(s):  
Data Assimilation ◽  
Weighting Function ◽  
Channel Selection ◽  
Peak Height ◽  
Utilization Rate ◽  
Time Dynamic ◽  
Dynamic Channel ◽  
The Impact ◽  
Height Data ◽  
Function Peak

To make better use of microwave radiance observations for data assimilation, removal of radiances contaminated by hydrometeor particles is one of the most important steps. Generally, all observations below the middle troposphere are eliminated before the analysis when precipitation is present. However, the altitude of the cloud top varies; when the weighting function peak height of a channel is higher than the altitude of the cloud top, observations are not affected by the absorption or scattering of cloud particles. Thus, the radiative transfer calculation can be performed under a clear sky scenario. In this paper, a dynamic channel selection (DCS) method was developed to determine the radiance observations unaffected by clouds under cloudy conditions in assimilation. First, the sensitivity of cloud liquid water (CLW) profiles to radiance from the microwave temperature sounding frequencies was analyzed. It was found that the impact of CLW on transmittance can be neglected where the cloud top height is below the weighting function peak height. Second, three lookup tables were devised through analysis of the impact of cloud fraction and cloud top height on radiance, which is the basis of the DCS method. The unified cloud top height of the Microwave Temperature Sounder (MWTS)-2 fields of view (FOVs) can be calculated by remapping the cloud mask and cloud top height data from the Medium Resolution Spectral Imager-2 (MERSI-2). Observations from various channels may be removed or retained based on real-time dynamic unified cloud top height data. Twelve-hour and long-term time-series brightness temperature simulation experiments both showed that an increase in the amount of observations used for data assimilation of more than 300% can be achieved by application of DCS, but this had no effect on the amount of error. Through DCS, areas of strong precipitation can be accurately identified and removed, and more observations above cloud top height can be included in the data assimilation. The application of DCS to data assimilation will greatly improve the data utilization rate, and therefore allow for more accurate characterization of upper atmospheric circulation.

Trophoblast Cell Membrane Interactions at Implantation

1970 ◽  
Vol 28 ◽  
pp. 310-311
Author(s):  
A. C. Enders
Keyword(s):  
Epithelial Cells ◽  
Cell Membrane ◽  
Membrane Fusion ◽  
Trophoblast Cell ◽  
Membrane Interactions ◽  
Uterine Epithelial Cells ◽  
Functional Complex ◽  
Cytotrophoblast Cells ◽  
Complex Relationships ◽  
Syncytial Trophoblast

The alteration in membrane relationships seen at implantation include 1) interaction between cytotrophoblast cells to form syncytial trophoblast and addition to the syncytium by subsequent fusion of cytotrophoblast cells, 2) formation of a wide variety of functional complex relationships by trophoblast with uterine epithelial cells in the process of invasion of the endometrium, and 3) in the case of the rabbit, fusion of some uterine epithelial cells with the trophoblast.Formation of syncytium is apparently a membrane fusion phenomenon in which rapid confluence of cytoplasm often results in isolation of residual membrane within masses of syncytial trophoblast. Often the last areas of membrane to disappear are those including a desmosome where the cell membranes are apparently held apart from fusion.

Valence electron spectroscopy of inhomogeneous media

1992 ◽  
Vol 50 (2) ◽  
pp. 1150-1151
Author(s):  
A. Howie ◽  
D.W. McComb
Keyword(s):  
Specific Gravity ◽  
Loss Function ◽  
Electron Spectroscopy ◽  
Valence Electron ◽  
Peak Height ◽  
Loss Functions ◽  
Loss Peak ◽  
High Energies ◽  
Valence Electron Density ◽  
Electron Microscopist

The bulk loss function Im(-l/ε (ω)), a well established tool for the interpretation of valence loss spectra, is being progressively adapted to the wide variety of inhomogeneous samples of interest to the electron microscopist. Proportionality between n, the local valence electron density, and ε-1 (Sellmeyer's equation) has sometimes been assumed but may not be valid even in homogeneous samples. Figs. 1 and 2 show the experimentally measured bulk loss functions for three pure silicates of different specific gravity ρ - quartz (ρ = 2.66), coesite (ρ = 2.93) and a zeolite (ρ = 1.79). Clearly, despite the substantial differences in density, the shift of the prominent loss peak is very small and far less than that predicted by scaling e for quartz with Sellmeyer's equation or even the somewhat smaller shift given by the Clausius-Mossotti (CM) relation which assumes proportionality between n (or ρ in this case) and (ε - 1)/(ε + 2). Both theories overestimate the rise in the peak height for coesite and underestimate the increase at high energies.

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