The present note uses the setup outlined in a previous note about a 2016 paper in Physical Review Letters on the large deviation analysis of rapid-onset rain showers. This paper will be referred to as MW2016 herein. In order to apply large deviation theory to a collector-drop framework for rapid-onset rain formation, equation [14] in MW2016 presents the cumulant generating function for the random variable , which I will write here as
The Laplace transform of the required probability density is , so equation [15] in MW2016 sets up a relevant Bromwich integral equation, which I will write here as
At first sight, this seems intractable directly, and a saddle-point approximation for the density in (1) is presented in equation [17] in MW2016. This saddle-point approximation involves the large deviation entropy function for the random variable , and an intricate asymptotic analysis is then embarked upon to obtain an explicit expression for this entropy function. The result is the expression given in equation [24] in MW2016.
However, instead of approximating (1), it is possible to work out the Bromwich integral exactly. The result is the exact version of the probability density which is approximated in equation [17] in MW2016. This is a known distribution called the generalised Erlang distribution, but I have not been able to find any derivations of it using the Bromwich integral approach. Typically, derivations are carried out using characteristic functions (see, e.g., Bibinger, M., 2013, Notes on the sum and maximum of independent exponentially distributed random variables with different scale parameters, arXiv:1307.3945 [math.PR]), or phase-type distribution methods (see, e.g., O’Cinneide, C., 1999, Phase-type distribution: open problems and a few properties, Communication in Statistic-Stochastic Models, 15(4), pp. 731-757).
To derive this distribution directly from the Bromwich integral in (1), begin by replacing the term by the product it gives rise to:
Then, starting from an elementary bivariate partial fraction expansion, and extending this to variables by induction, we can obtain the following expression for the product term in (2):
The detailed derivation of (3) is set out in an Appendix below. Putting (3) back into (2), and moving the integral sign `through’ the summation and product in (3), we obtain the following form for the Bromwich integral:
Each integrand in (4) has a simple pole at , so the residue at each such singularity is given by
We can construct a contour in the complex plane which is appropriate for each by creating a semicircle with the straight vertical part located at a point
to the right of
, and with the arc of the semicircle large enough to enclose the point
on the real axis (diagram below). Since
is the smallest collision rate, and
is the largest, this ensures that the contour will enclose each
point.

It then follows by Cauchy’s residue theorem, and the fact that the integral along the circular arc component of the contour vanishes as the radius of the semicircle goes to infinity, that
Putting (6) in (4), we then get the exact form of the required density:
This is the density function of the generalised Erlang distribution, and is given in an alternative (but equivalent) form in equation [SB1.1] on page 241 of a paper by Kostinski and Shaw (Kostinski, A., Shaw, R., 2005, Fluctuations and Luck in Droplet Growth by Coalescence, Bull. Am. Meteorol. Soc. 86, 235). Integrating (7) with respect to , we obtain the cumulative distribution function
Again this is given in an alternative (but equivalent) form on page 241 of Kostinski and Shaw’s paper, as equation [SB1.2].
Although we now have the exact pdf and cdf corresponding to the Bromwich integral in MW2016, these are not practical for calculations in the context of runaway raindrop growth. This runaway process can involve large numbers of water particle collisions , e.g.,
, so the expressions in (7) and (8) would involve sums of thousands of product terms, each of these products in turn involving thousands of terms. Therefore, we are still interested in obtaining a formula for the entropy function
to enable large deviation approximations for (7) and (8) for practical calculations. It may be possible to obtain an approximation for the entropy function directly from the cdf in (8), but this would require further investigation.
An initial problem that might need to be overcome is that the forms for the cdf in (8) above and also in Kostinski and Shaw (which is similar) are inconvenient. However, they can be manipulated as follows. First, expand (8) to obtain
A recent paper by Yanev (Yanev, G., 2020, Exponential and Hypoexponential Distributions: Some Characterizations, Mathematics, 8(12), 2207) pointed out that the product terms appearing in (9) are related to the terms appearing in the Lagrange polynomial interpolation formula. This formula and its properties are well known in the field of approximation theory (see, e.g., pages 33-35 in Powell, M., 1981, Approximation Theory and Methods, Cambridge University Press). This fact was used in a paper by Sen and Balakrishnan (Sen, A., Balakrishnan, N., 1999, Convolution of geometrics and a reliability problem, Statistics & Probability Letters, 43, pp. 421-426) to give a simple proof that the sum/product which appears as the first term on the right-hand side of (9) is identically equal to 1:
(See my previous note about this). Using (10) in (9), we then obtain the cdf in a potentially more convenient form:
Appendix: Proof of the partial fraction expansion in (3)
The following arguments use the Lagrange polynomial interpolation formula to prove the partial fraction expansion in (3) above. We will need formula (6) in my previous note about this, which is repeated here for convenience:
To prove (3) above, we begin by using Lagrange’s polynomial interpolation formula to prove the following auxiliary result:
Taking apart (12) above (which equals 1) and using (10) above, we obtain
Therefore we conclude
We will need this result shortly. Next, we expand the bracketed terms on the left-hand side of (13) by partial fractions. We write
where and
are to be determined. Therefore
Upon setting , (17) yields
Putting (18) in (16), we see that the left-hand side of (13) becomes
Now, the term in curly brackets in (19) is
Therefore (19) becomes
The last equality follows because the first term in the penultimate step is zero by (15) above, and the sum in the square brackets in the second term in the penultimate step is equal to 1 by (10) above. Therefore the auxiliary result in (13) is now proved.
Now we use this result to prove (3) by mathematical induction. As the basis for the induction, we can use the case which is easy to prove by repeated bivariate partial fraction expansions, and clearly exhibits the pattern represented by (3):
Next, suppose (3) is true. Then adding another factor to the product on the left-hand side of (3) would produce
where the expressions in square brackets in the two steps before the last are equal by the auxiliary result (13) proved earlier. Therefore, by the principle of mathematical induction, (3) must hold for all , so (3) is proved.
