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The chance-constrained version of the above-mentioned model can be described using the following simple denotations, assuming one ship and one cargo.
In this model, the 3-dB bandwidth of the channel impulse response is calculated from the channel temporal dispersion D using the following simple analytical relation f 3 dB = 1 4 π D. (3.1).
Yang (2010) simplifies the general implementation of the CS algorithm by using the following simple representation: each cuckoo egg in a host nest represents a solution and each cuckoo can only lay one egg which represents one solution.
It may also be calculated using the following simple formula: P = N × d n / d o (10 where P is pore pressure in ppg, N is normal pore pressure in ppg, dn is normal d-exponent, do is observed d-exponent.
The linked earthquakes were then grouped into clusters using the following simple rule: if earthquakes A and B are linked and if B and C are also linked, then A, B, and C are included in the same cluster irrespective of the waveform similarity between A and C. The CCmax thresholds were determined for a given p value in the manner described above.
We explore this hypothesis using the following simple mathematical model.
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In particular, we will use the following simple result.
These methods use the following simple reasoning for the estimation of time delay.
Our further reasoning related to problem (1.3), (1.4) uses the following simple observation.
To simplify our sufficient condition, we use the following simple lemma.
We will use the following simple lemma for obtaining our results.
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Since I tried Ludwig back in 2017, I have been constantly using it in both editing and translation. Ever since, I suggest it to my translators at ProSciEditing.

Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com