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Fig. 2 Field photo showing basalt flow layers Fig. 3 Spatial distribution of elevation in and around Koyna region (100 Km radius).
SRTM data having three arc-second (~90 m) ground resolutions is used to produce the spatial distribution of elevation and slope.
These ecoregions, and the geographic distribution of elevation and vegetation are illustrated in Figure 1.
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To study straylight testing as a screening method for ocular fitness after refractive surgery in demanding professions and to determine the distribution of elevations in straylight as a result of refractive surgery in a non-research setting in contrast with earlier reports in research settings.
In case of bimodal distribution of elevated micronuclei, the second elevation occurred at about 60% cytotoxicity (example shown in Table 1, experiments 1 and 2).
The hypsometry of the region indicate two peaks in the distribution frequency of elevation (3600 4100 m and 4400 4800 m asl).
The spatial distribution of the elevation map was prepared after reclassifying the elevation layer into seven (7) classes (< 100, 100 200, 200 300, 300 400, 400 500, 500 1000 and > 1000 m) where brown colour indicates maximum altitude found in north, north-west, and blue indicated < 100 m altitude zone in the east and south-east part in the study area (Fig. 2b).
Evidence suggests that some high elevation species, which are strongly climatically restricted, may limit the upslope distribution of lower elevation species, but there is no evidence of the reverse.
To simulate the distribution of Ca2+ elevations, a random number uniformly distributed between 0 and 1 was chosen for each synapse at every fifth time step (every 180 msec).
Upper treeline ecotones within alpine and arctic ecosystems are mainly controlled by climate (e.g. Lavoie and Payette, 1994; Kullman, 1999; Grace et al., 2002), and are considered as sensitive proxy biomonitors for revealing the impact of climate variability on the distribution of high-elevation mountain forests (e.g. Camarero and Gutiérrez, 2004; Danby and Hik, 2007; Elliott, 2011).
According to Harlin (1978), the HC can be considered as a cumulative probability distribution function of elevations and, in this approach, the HC is represented by a continuous polynomial function with the form: f(x) = a_{0} + a_{1} x + a_{2} x^{2} + ldots + a_{n} x^{n}, (1 where f(x) is a polynomial function fitted to the HC by regression and a 0, a 1, a 2, … a n are the coefficients.
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Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com