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Exact(12)
Finally, a convenient way to estimate the actual maximum width of the single-branched soot sheets is proposed, and this value is estimated to be ∼20 mm for both flames.
This value is estimated at the same location (latitude, longitude and altitude) and at the same time of Swarm measurement.
This value is estimated on the training corpus, by counting the number of frames that passed the filter, while actually being emitted by the state.
An amplification correction toward this value is estimated by applying the Vs30 from the PS logging results of K-NET and KiK-net to the empirical relationship of Midorikawa et al. (1994).
This value is estimated from a phase equilibrium relationship in a storage condition of pre-eruptive magma (at 125 MPa) and H2O analyses of melt inclusions, as discussed in Suzuki et al. (2013a).
In the present case for the C 1s XPS spectrum of graphite, this value is estimated to be 0.33 where d is 3.354 Ǻ, λ is 11.77 Ǻ [13] at 561 eV of kinetic energy which is obtained by subtracting the core level of C 1s (~284 eV) and work function of graphite (4.6 eV) [14] from the incident photon energy hv = 850 eV, and θ is 45°.
Similar(48)
This value was estimated using a MCMC method34 that searches the feasible parameter space in pursuit of a stationary distribution.
The signal-to-noise ratio of this value was estimated to be 12/1 based on repetitive measurements of several samples.
Although this value was estimated without consideration of sediment transport beyond barriers, it is assumed that a considerable amount of sediment could pass over topographic highs.
At Mt Raung, this value was estimated to be 0.269 × 106 W m−2 m−1 sr−1 using the MODTRAN radiative transfer code obtained under tropical atmospheric conditions at a height of 2900 m.
The establishment of this value was estimated based on the sample size needed to obtain a proportion of 50%% for the occurrence of a certain characteristic of the elderly population (value at which the sampling size obtained in the highest possible for p = 0.50 and q = 0.50).
More suggestions(15)
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Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com