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Using both methods, we estimate the contribution of an individual country, asking the question: whether, and to what extent, does the likelihood of the Argentinian heatwave occurring change when we remove the individual countries' greenhouse gas contributions from present day simulations?
Using observational estimates of W ′ (assuming a linear trend), Fmelt and τ, and combining the uncertainties arising from these data with the method uncertainty (see Methods) we estimate a change in Fcycle of 0.059 ± 0.022 Sv for En4, 0.032 ± 0.012 Sv for Ishii, and 0.068 ± 0.025 Sv for CSIRO between 1950 and 2010.
Following the procedure described in the methods, we estimate the proportion of normal cells in this sample (Figure S2) to be about 30%.
Using mitochondrial and nuclear genetic data, multiple fossil calibration points, and likelihood and Bayesian methods, we estimate phylogenetic relationships and divergence times for Barbourula.
However, as calculated in Methods, we estimate that there were on average 20 µ RNA molecules per cell in the variegated clones such as #651 and #654 that produced ∼2% as much μ RNA as #626.
From capture – recapture methods, we estimate a total of 373 cases of SLE are resident in Northern Trinidad; this includes both sexes.
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To compare the two methods, we estimated the deletion rate given by these two estimators on several samples from different species including rice (data not shown).
Using simulation methods, we estimated the power requirements for interrupted time series studies under various scenarios.
Moreover, in our previous study [26], aimed at the detection of malicious executables using ML and AL methods, we estimated the malicious executables percentage to be approximately 9 %.
With the re-sampling procedure described in Material and Methods, we estimated the total number of Prx clusters in the barley genome.
Using Equation (1) and 1 Mbp sliding window (see Materials and Methods), we estimated the genome-wide copy number of MCF-7 based on the whole cell extract (WCEseq) library.
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