## What is/are Asymmetry Factor?

Asymmetry Factor - The asymmetry factor is found closely related to the transparency of struts.^{[1]}With the increase of particle agglomeration degree, the scattering coefficients and asymmetry factors of the particles increase obviously, which can be even larger than the results for independent scattering under certain circumstances.

^{[2]}In order to address this issue, this paper proposes the use of Crest Factor (CF) and Asymmetry Factor (AF) of the supply voltage to assess the impact of supply voltage harmonics on dc bus capacitor and choke inductor.

^{[3]}9, where an X/R ratio is required to obtain an asymmetry factor of 2.

^{[4]}Comparisons with this benchmark solution show that the use of gray Henyey-Greenstein functions obtained with the Planck-mean values for the asymmetry factors of the coal/char and ash particles is sufficient to model accurately the scattering phase functions.

^{[5]}Minor structures result in scattering cross-section enhancement slightly more than that of absorption cross section, and their effects on the angle-dependent phase matrix as well as asymmetry factor are negligible.

^{[6]}System suitability parameters, such as capacity factor, numbers of the theoretical plate, asymmetry factor, as well as validation parameters, including method precision, accuracy, linearity, selectivity, and robustness, were set up.

^{[7]}0, and the bands were almost perfectly symmetrical with asymmetry factors equal to 1.

^{[8]}To see the impact of neotectonic on the Htab river watershed, four morphometric indices were applied: the elongation ratio, the hypsometric curve, the hypsometric integral, and the asymmetry factor.

^{[9]}In solutions of polymeric cation/anion pairs, the screening length is shown to depend on an asymmetry factor.

^{[10]}Low values of asymmetry factor (ASY) (0.

^{[11]}6 %; and (3) asymmetry factor is −0.

^{[12]}The equivalent volume cylinder model generally gives better predictions on the extinction cross-section, absorption cross-section, and asymmetry factor of multicellular filamentous cyanobacteria.

^{[13]}This allows us to reconstruct the time-resolved 3D morphology of cardiomyocytes during a full contraction-relaxation cycle with a raw data rate of 200 μs/frame and to generate spatially resolved images of contractile parameters (maximum displacement, time delay, asymmetry factor).

^{[14]}Indeed, values for chromatographic efficiency obtained on the capillary columns meet or exceed those measured for the standard columns (20 000-40 000 vs 14 000 plates/m, respectively) with near symmetric elution bands (asymmetry factors of 1.

^{[15]}This approach considered the effects of the pigments with fractal aggregate structures on the scattering properties, including the phase functions and asymmetry factor.

^{[16]}Firstly, based on the Mie scattering theory, the parameters such as scattering, extinction coefficient and asymmetry factor of haze under different conditions are calculated.

^{[17]}Geomorphic indices such as stream order, stream length, bifurcation ratio, form factor, asymmetry factor and hypsometric integral were calculated for each drainage basin of the study regions.

^{[18]}Tests on low-cycle fatigue were carried out on the upgraded testing machine UMM-10 with repeated static stretching with an asymmetry factor of +0.

^{[19]}We present an approach for optimizing the asymmetry factor (a non-dimensional measure of Willis coupling’s effect on the specific acoustic impedance) in a metamaterial with lumped-element hidden degrees of freedom.

^{[20]}The volume of acetonitrile and flow rate showed significant effect on retention factor of both the drugs and asymmetry factor of ofloxacin.

^{[21]}An increasing relative fraction of the large size PM during the polluted periods can be deduced from the variations of the scattering Angstrom exponent, backscattering ratio, and asymmetry factor.

^{[22]}09}$ ) and asymmetry factors, advantageous for analog-style NNs with online training.

^{[23]}To quantitatively analyze the asymmetrical characteristics of these valleys identified in the southern Maxianshan, 33 parallel streams were investigated by using two drainage basin analytical techniques, namely, the transverse topographic symmetry factor (T) and asymmetry factor (AF).

^{[24]}The column-to-column reproducibility based on three columns packed with three different batches of stationary phase was found satisfactory in separation efficiency, retention factor, and asymmetry factor.

^{[25]}Fractal dimension, branching coefficients and angle, asymmetry factor and optimality ratio for both arteries and veins were computed from the processed input image and given to a support vector machine classifier which gives promising results.

^{[26]}The influence of the asymmetry factor on stiffness is analysed; the prototype designed by this method can run stably.

^{[27]}Asymmetry factor (AF) data were assessed and were found to provide only limited analytical information.

^{[28]}

## mountain front sinuosity

In this study, we extract geomorphic indices including mountain-front sinuosity (Smf), valley floor width-to-height ratio (Vf), stream length-gradient (SL), catchment Asymmetry Factor (AF) and hypsometric integrals and curves (HI and HC) to evaluate the relative tectonic activity of the Adiyaman fault.^{[1]}A number of parameters including the mountain front sinuosity, asymmetry factor, transverse topography symmetry, hypsometry, longitudinal profile and the shape parameters have been used.

^{[2]}Seven geomorphometric parameters, namely, longitudinal profile (Lp), asymmetry factor (Af), hypsometric curve and hypsometric integral (HI), mountain front sinuosity (Smf), river sinuosity (R), stream length gradient (Sl), and shape factor (Shp) were calculated for selected drainage basins of South India.

^{[3]}Quantitative geomorphic analysis was carried out using mountain-front sinuosity (Smf), valley floor width–valley height ratio (Vf), drainage basin asymmetry factor (Af), Hypsometric integral (Hi), drainage basin shape index (Bs), mean axial slope of channel (MASC), standard deviation of topography (STD) and index of active tectonic (Iat).

^{[4]}Morphometric studies, including hypsometric curves, hypsometric integrals, asymmetry factor, mountain front sinuosity, normalised stream-length gradient, and normalised concavity indices for the Ebro River and 32 of its tributaries, show the signals of transient response to this major drainage change.

^{[5]}Active tectonics of Tehran City was evaluated by using Digital elevation model (DEM) derived drainage network and three geomorphic indices basin (asymmetry factor (AF), basin shape index (Bs) and mountain front sinuosity (Smf)).

^{[6]}

## single scattering albedo

25–4 µm) using satellite data, and the Look-up table of single scattering albedo (SSA) and asymmetry factor (ASY).^{[1]}00 µm) are calculated using this method, and it is shown that the increasing of the average diameter of primary particles and the average number of primary particles per soot particle can enhance the absorption coefficient, scattering coefficient, asymmetry factor and single-scattering albedo of soot particle ensembles 0.

^{[2]}The results of the single-scattering albedo and asymmetry factors were compared to those of conventional internally mixed spheres (i.

^{[3]}Driven by the change in physicochemical properties, the Single Scattering Albedo (SSA) and the asymmetry factor increased as the aerosol aged (with maximum increments of 0.

^{[4]}

## valley floor width

To estimate the tectonic activity in the study area, we analyzed 6 DEM derived geomorphic indices for 66 basins: the stream-gradient index (SL), asymmetry factor (Af), basin shape ratio (Bs), hypsometric integral (Hi), valley floor width-valley height ratio (Vf) and mountain-front sinuosity (Smf).^{[1]}The field investigations are supported by computation of morphometric indices, such as, low values of Valley Floor Width to Valley Height (Vf), Asymmetry Factor (Af), elongated and tilted river basin with narrow valley floor as well as higher Bifurcation Ratio (Rb) and sinuosity parameters, immature topography and landscape, elongation and tilting of drainage basin and accelerated erosion-all show that the basin is structurally controlled.

^{[2]}In this work, we present a quantitative geomorphology analysis along the Anaime River valley by using several geomorphic indexes such as the hypsometric curve, the index of drainage basin shape, the asymmetry factor, the ratio of valley floor width to valley height, normalized longitudinal stream profiles, and the relative slope-extension index.

^{[3]}

## stream length gradient

In this study, the assessment of active tectonics of study area was determined using Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER) Global Digital Elevation Model (GDEM) based on Geomorphic Indices (Stream Length Gradient index, Hypsometric integral, Asymmetry factor, Basin shape, Valley floor width to Valley height ratio, Mountain front sinuosity index) cumulatively with Linear, Areal and Relief morphometric parameters on 27 delineated basins of the study area.^{[1]}

## Basin Asymmetry Factor

Geomorphic indices of ‘Basin Asymmetry Factor (AF)’ and ‘Transverse Topography Factor (T)’ of 77 drainage basins of third-order streams developed on this tectonic block have been computed to decipher active tilt-block tectonics of a part of this vast klippe.^{[1]}The geomorphic indices of basin asymmetry factor (AF), swath topographic profiles, enhanced transverse hypsometry index (THi*) and normalized river long-profiles were used for validating a neotectonic origin for the dome-like morphologies.

^{[2]}Quantitative geomorphic analysis was carried out using mountain-front sinuosity (Smf), valley floor width–valley height ratio (Vf), drainage basin asymmetry factor (Af), Hypsometric integral (Hi), drainage basin shape index (Bs), mean axial slope of channel (MASC), standard deviation of topography (STD) and index of active tectonic (Iat).

^{[3]}