Harmonic Mean

It is sometimes appropriate for situations when the average rate is desired.

The harmonic mean can be expressed as the reciprocal of the arithmetic mean of the reciprocals of the given set of observations. As a simple example, the harmonic mean of 1, 4, and 4 is

${\displaystyle \left({\frac {1^{-1}+4^{-1}+4^{-1}}{3}}\right)^{-1}={\frac {3}{{\frac {1}{1}}+{\frac {1}{4}}+{\frac {1}{4}}}}={\frac {3}{1.5}}=2\,.}$

The harmonic mean H of the positive real numbers ${\displaystyle x_{1},x_{2},\ldots ,x_{n}}$  is defined to be

${\displaystyle H(x_{1},x_{2},\ldots ,x_{n})={\frac {n}{\displaystyle {\frac {1}{x_{1}}}+{\frac {1}{x_{2}}}+\cdots +{\frac {1}{x_{n}}}}}={\frac {n}{\displaystyle \sum _{i=1}^{n}{\frac {1}{x_{i}}}}}.}$ 

It is the reciprocal of the arithmetic mean of the reciprocals, and vice versa:

${\displaystyle {\begin{aligned}H(x_{1},x_{2},\ldots ,x_{n})&={\frac {1}{\displaystyle A\left({\frac {1}{x_{1}}},{\frac {1}{x_{2}}},\ldots {\frac {1}{x_{n}}}\right)}},\\[10mu]A(x_{1},x_{2},\ldots ,x_{n})&={\frac {1}{\displaystyle H\left({\frac {1}{x_{1}}},{\frac {1}{x_{2}}},\ldots {\frac {1}{x_{n}}}\right)}},\end{aligned}}}$ 

where the arithmetic mean is defined as ${\textstyle A(x_{1},x_{2},\ldots ,x_{n})={\tfrac {1}{n}}\sum _{i=1}^{n}x_{i}.}$ 

The harmonic mean is a Schur-concave function, and dominated by the minimum of its arguments, in the sense that for any positive set of arguments, ${\displaystyle \min(x_{1}\ldots x_{n})\leq H(x_{1}\ldots x_{n})\leq n\min(x_{1}\ldots x_{n})}$ . Thus, the harmonic mean cannot be made arbitrarily large by changing some values to bigger ones (while having at least one value unchanged). ^{[citation needed]}

The harmonic mean is also concave, which is an even stronger property than Schur-concavity. One has to take care to only use positive numbers though, since the mean fails to be concave if negative values are used.^{[citation needed]}

 

The harmonic mean is one of the three Pythagorean means. For all positive data sets containing at least one pair of nonequal values, the harmonic mean is always the least of the three means, while the arithmetic mean is always the greatest of the three and the geometric mean is always in between. (If all values in a nonempty dataset are equal, the three means are always equal to one another; e.g., the harmonic, geometric, and arithmetic means of {2, 2, 2} are all 2.)

It is the special case M₋₁ of the power mean:

$${\displaystyle H\left(x_{1},x_{2},\ldots ,x_{n}\right)=M_{-1}\left(x_{1},x_{2},\ldots ,x_{n}\right)={\frac {n}{x_{1}^{-1}+x_{2}^{-1}+\cdots +x_{n}^{-1}}}}$$

 

Since the harmonic mean of a list of numbers tends strongly toward the least elements of the list, it tends (compared to the arithmetic mean) to mitigate the impact of large outliers and aggravate the impact of small ones.

The arithmetic mean is often mistakenly used in places calling for the harmonic mean. In the speed example below for instance, the arithmetic mean of 40 is incorrect, and too big.

The harmonic mean is related to the other Pythagorean means, as seen in the equation below. This can be seen by interpreting the denominator to be the arithmetic mean of the product of numbers n times but each time omitting the j-th term. That is, for the first term, we multiply all n numbers except the first; for the second, we multiply all n numbers except the second; and so on. The numerator, excluding the n, which goes with the arithmetic mean, is the geometric mean to the power n. Thus the n-th harmonic mean is related to the n-th geometric and arithmetic means. The general formula is

$${\displaystyle H\left(x_{1},\ldots ,x_{n}\right)={\frac {\left(G\left(x_{1},\ldots ,x_{n}\right)\right)^{n}}{A\left(x_{2}x_{3}\cdots x_{n},x_{1}x_{3}\cdots x_{n},\ldots ,x_{1}x_{2}\cdots x_{n-1}\right)}}={\frac {\left(G\left(x_{1},\ldots ,x_{n}\right)\right)^{n}}{A\left({\frac {1}{x_{1}}}{\prod \limits _{i=1}^{n}x_{i}},{\frac {1}{x_{2}}}{\prod \limits _{i=1}^{n}x_{i}},\ldots ,{\frac {1}{x_{n}}}{\prod \limits _{i=1}^{n}x_{i}}\right)}}.}$$

 

If a set of non-identical numbers is subjected to a mean-preserving spread — that is, two or more elements of the set are "spread apart" from each other while leaving the arithmetic mean unchanged — then the harmonic mean always decreases.

Two numbers

 

For the special case of just two numbers, ${\displaystyle x_{1}}$  and ${\displaystyle x_{2}}$ , the harmonic mean can be written

${\displaystyle H={\frac {2x_{1}x_{2}}{x_{1}+x_{2}}}\qquad }$  or ${\displaystyle \qquad {\frac {1}{H}}={\frac {(1/x_{1})+(1/x_{2})}{2}}.}$ 

In this special case, the harmonic mean is related to the arithmetic mean ${\displaystyle A={\frac {x_{1}+x_{2}}{2}}}$  and the geometric mean ${\displaystyle G={\sqrt {x_{1}x_{2}}},}$  by

${\displaystyle H={\frac {G^{2}}{A}}=G\left({\frac {G}{A}}\right).}$ 

Since ${\displaystyle {\tfrac {G}{A}}\leq 1}$  by the inequality of arithmetic and geometric means, this shows for the n = 2 case that H ≤ G (a property that in fact holds for all n). It also follows that ${\displaystyle G={\sqrt {AH}}}$ , meaning the two numbers' geometric mean equals the geometric mean of their arithmetic and harmonic means.

Three numbers

For the special case of three numbers, ${\displaystyle x_{1}}$ , ${\displaystyle x_{2}}$  and ${\displaystyle x_{3}}$ , the harmonic mean can be written

${\displaystyle H={\frac {3x_{1}x_{2}x_{3}}{x_{1}x_{2}+x_{1}x_{3}+x_{2}x_{3}}}.}$ 

Three positive numbers H, G, and A are respectively the harmonic, geometric, and arithmetic means of three positive numbers if and only if^{: p.74, #1834} the following inequality holds

${\displaystyle {\frac {A^{3}}{G^{3}}}+{\frac {G^{3}}{H^{3}}}+1\leq {\frac {3}{4}}\left(1+{\frac {A}{H}}\right)^{2}.}$ 

If a set of weights ${\displaystyle w_{1}}$ , ..., ${\displaystyle w_{n}}$  is associated to the dataset ${\displaystyle x_{1}}$ , ..., ${\displaystyle x_{n}}$ , the weighted harmonic mean is defined by

${\displaystyle H={\frac {\sum \limits _{i=1}^{n}w_{i}}{\sum \limits _{i=1}^{n}{\frac {w_{i}}{x_{i}}}}}=\left({\frac {\sum \limits _{i=1}^{n}w_{i}x_{i}^{-1}}{\sum \limits _{i=1}^{n}w_{i}}}\right)^{-1}.}$ 

The unweighted harmonic mean can be regarded as the special case where all of the weights are equal.

In physics

Average speed

In many situations involving rates and ratios, the harmonic mean provides the correct average. For instance, if a vehicle travels a certain distance d outbound at a speed x (e.g. 60 km/h) and returns the same distance at a speed y (e.g. 20 km/h), then its average speed is the harmonic mean of x and y (30 km/h), not the arithmetic mean (40 km/h). The total travel time is the same as if it had traveled the whole distance at that average speed. This can be proven as follows:

Average speed for the entire journey = Total distance traveled/Sum of time for each segment = 2d/d/x + d/y = 2/1/x+1/y

However, if the vehicle travels for a certain amount of time at a speed x and then the same amount of time at a speed y, then its average speed is the arithmetic mean of x and y, which in the above example is 40 km/h.

Average speed for the entire journey = Total distance traveled/Sum of time for each segment = xt+yt/2t = x+y/2

The same principle applies to more than two segments: given a series of sub-trips at different speeds, if each sub-trip covers the same distance, then the average speed is the harmonic mean of all the sub-trip speeds; and if each sub-trip takes the same amount of time, then the average speed is the arithmetic mean of all the sub-trip speeds. (If neither is the case, then a weighted harmonic mean or weighted arithmetic mean is needed. For the arithmetic mean, the speed of each portion of the trip is weighted by the duration of that portion, while for the harmonic mean, the corresponding weight is the distance. In both cases, the resulting formula reduces to dividing the total distance by the total time.)

However, one may avoid the use of the harmonic mean for the case of "weighting by distance". Pose the problem as finding "slowness" of the trip where "slowness" (in hours per kilometre) is the inverse of speed. When trip slowness is found, invert it so as to find the "true" average trip speed. For each trip segment i, the slowness s_i = 1/speed_i. Then take the weighted arithmetic mean of the s_i's weighted by their respective distances (optionally with the weights normalized so they sum to 1 by dividing them by trip length). This gives the true average slowness (in time per kilometre). It turns out that this procedure, which can be done with no knowledge of the harmonic mean, amounts to the same mathematical operations as one would use in solving this problem by using the harmonic mean. Thus it illustrates why the harmonic mean works in this case.

Density

Similarly, if one wishes to estimate the density of an alloy given the densities of its constituent elements and their mass fractions (or, equivalently, percentages by mass), then the predicted density of the alloy (exclusive of typically minor volume changes due to atom packing effects) is the weighted harmonic mean of the individual densities, weighted by mass, rather than the weighted arithmetic mean as one might at first expect. To use the weighted arithmetic mean, the densities would have to be weighted by volume. Applying dimensional analysis to the problem while labeling the mass units by element and making sure that only like element-masses cancel makes this clear.

Electricity

If one connects two electrical resistors in parallel, one having resistance x (e.g., 60 Ω) and one having resistance y (e.g., 40 Ω), then the effect is the same as if one had used two resistors with the same resistance, both equal to the harmonic mean of x and y (48 Ω): the equivalent resistance, in either case, is 24 Ω (one-half of the harmonic mean). This same principle applies to capacitors in series or to inductors in parallel.

However, if one connects the resistors in series, then the average resistance is the arithmetic mean of x and y (50 Ω), with total resistance equal to twice this, the sum of x and y (100 Ω). This principle applies to capacitors in parallel or to inductors in series.

As with the previous example, the same principle applies when more than two resistors, capacitors or inductors are connected, provided that all are in parallel or all are in series.

The "conductivity effective mass" of a semiconductor is also defined as the harmonic mean of the effective masses along the three crystallographic directions.

Optics

As for other optic equations, the thin lens equation 1/f = 1/u + 1/v can be rewritten such that the focal length f is one-half of the harmonic mean of the distances of the subject u and object v from the lens.

Two thin lenses of focal length f₁ and f₂ in series is equivalent to two thin lenses of focal length f_hm, their harmonic mean, in series. Expressed as optical power, two thin lenses of optical powers P₁ and P₂ in series is equivalent to two thin lenses of optical power P_am, their arithmetic mean, in series.

In finance

The weighted harmonic mean is the preferable method for averaging multiples, such as the price–earnings ratio (P/E). If these ratios are averaged using a weighted arithmetic mean, high data points are given greater weights than low data points. The weighted harmonic mean, on the other hand, correctly weights each data point. The simple weighted arithmetic mean when applied to non-price normalized ratios such as the P/E is biased upwards and cannot be numerically justified, since it is based on equalized earnings; just as vehicles speeds cannot be averaged for a roundtrip journey (see above).

For example, consider two firms, one with a market capitalization of $150 billion and earnings of $5 billion (P/E of 30) and one with a market capitalization of $1 billion and earnings of $1 million (P/E of 1000). Consider an index made of the two stocks, with 30% invested in the first and 70% invested in the second. We want to calculate the P/E ratio of this index.

Using the weighted arithmetic mean (incorrect):

${\displaystyle P/E=0.3\times 30+0.7\times 1000=709}$ 

Using the weighted harmonic mean (correct):

${\displaystyle P/E={\frac {0.3+0.7}{0.3/30+0.7/1000}}\approx 93.46}$ 

Thus, the correct P/E of 93.46 of this index can only be found using the weighted harmonic mean, while the weighted arithmetic mean will significantly overestimate it.

In geometry

In any triangle, the radius of the incircle is one-third of the harmonic mean of the altitudes.

For any point P on the minor arc BC of the circumcircle of an equilateral triangle ABC, with distances q and t from B and C respectively, and with the intersection of PA and BC being at a distance y from point P, we have that y is half the harmonic mean of q and t.

In a right triangle with legs a and b and altitude h from the hypotenuse to the right angle, h² is half the harmonic mean of a² and b².

Let t and s (t > s) be the sides of the two inscribed squares in a right triangle with hypotenuse c. Then s² equals half the harmonic mean of c² and t².

Let a trapezoid have vertices A, B, C, and D in sequence and have parallel sides AB and CD. Let E be the intersection of the diagonals, and let F be on side DA and G be on side BC such that FEG is parallel to AB and CD. Then FG is the harmonic mean of AB and DC. (This is provable using similar triangles.)

 

One application of this trapezoid result is in the crossed ladders problem, where two ladders lie oppositely across an alley, each with feet at the base of one sidewall, with one leaning against a wall at height A and the other leaning against the opposite wall at height B, as shown. The ladders cross at a height of h above the alley floor. Then h is half the harmonic mean of A and B. This result still holds if the walls are slanted but still parallel and the "heights" A, B, and h are measured as distances from the floor along lines parallel to the walls. This can be proved easily using the area formula of a trapezoid and area addition formula.

In an ellipse, the semi-latus rectum (the distance from a focus to the ellipse along a line parallel to the minor axis) is the harmonic mean of the maximum and minimum distances of the ellipse from a focus.

In other sciences

In computer science, specifically information retrieval and machine learning, the harmonic mean of the precision (true positives per predicted positive) and the recall (true positives per real positive) is often used as an aggregated performance score for the evaluation of algorithms and systems: the F-score (or F-measure). This is used in information retrieval because only the positive class is of relevance, while number of negatives, in general, is large and unknown. It is thus a trade-off as to whether the correct positive predictions should be measured in relation to the number of predicted positives or the number of real positives, so it is measured versus a putative number of positives that is an arithmetic mean of the two possible denominators.

A consequence arises from basic algebra in problems where people or systems work together. As an example, if a gas-powered pump can drain a pool in 4 hours and a battery-powered pump can drain the same pool in 6 hours, then it will take both pumps 6·4/6 + 4, which is equal to 2.4 hours, to drain the pool together. This is one-half of the harmonic mean of 6 and 4: 2·6·4/6 + 4 = 4.8. That is, the appropriate average for the two types of pump is the harmonic mean, and with one pair of pumps (two pumps), it takes half this harmonic mean time, while with two pairs of pumps (four pumps) it would take a quarter of this harmonic mean time.

In hydrology, the harmonic mean is similarly used to average hydraulic conductivity values for a flow that is perpendicular to layers (e.g., geologic or soil) - flow parallel to layers uses the arithmetic mean. This apparent difference in averaging is explained by the fact that hydrology uses conductivity, which is the inverse of resistivity.

In sabermetrics, a baseball player's Power–speed number is the harmonic mean of their home run and stolen base totals.

In population genetics, the harmonic mean is used when calculating the effects of fluctuations in the census population size on the effective population size. The harmonic mean takes into account the fact that events such as population bottleneck increase the rate genetic drift and reduce the amount of genetic variation in the population. This is a result of the fact that following a bottleneck very few individuals contribute to the gene pool limiting the genetic variation present in the population for many generations to come.

When considering fuel economy in automobiles two measures are commonly used – miles per gallon (mpg), and litres per 100 km. As the dimensions of these quantities are the inverse of each other (one is distance per volume, the other volume per distance) when taking the mean value of the fuel economy of a range of cars one measure will produce the harmonic mean of the other – i.e., converting the mean value of fuel economy expressed in litres per 100 km to miles per gallon will produce the harmonic mean of the fuel economy expressed in miles per gallon. For calculating the average fuel consumption of a fleet of vehicles from the individual fuel consumptions, the harmonic mean should be used if the fleet uses miles per gallon, whereas the arithmetic mean should be used if the fleet uses litres per 100 km. In the USA the CAFE standards (the federal automobile fuel consumption standards) make use of the harmonic mean.

In chemistry and nuclear physics the average mass per particle of a mixture consisting of different species (e.g., molecules or isotopes) is given by the harmonic mean of the individual species' masses weighted by their respective mass fraction.

 

 

 

 

The harmonic mean of a beta distribution with shape parameters α and β is:

${\displaystyle H={\frac {\alpha -1}{\alpha +\beta -1}}{\text{ conditional on }}\alpha >1\,\,\&\,\,\beta >0}$ 

The harmonic mean with α < 1 is undefined because its defining expression is not bounded in [0, 1].

Letting α = β

${\displaystyle H={\frac {\alpha -1}{2\alpha -1}}}$ 

showing that for α = β the harmonic mean ranges from 0 for α = β = 1, to 1/2 for α = β → ∞.

The following are the limits with one parameter finite (non-zero) and the other parameter approaching these limits:

${\displaystyle {\begin{aligned}\lim _{\alpha \to 0}H&={\text{ undefined }}\\\lim _{\alpha \to 1}H&=\lim _{\beta \to \infty }H=0\\\lim _{\beta \to 0}H&=\lim _{\alpha \to \infty }H=1\end{aligned}}}$ 

With the geometric mean the harmonic mean may be useful in maximum likelihood estimation in the four parameter case.

A second harmonic mean (H_{1 − X}) also exists for this distribution

${\displaystyle H_{1-X}={\frac {\beta -1}{\alpha +\beta -1}}{\text{ conditional on }}\beta >1\,\,\&\,\,\alpha >0}$ 

This harmonic mean with β < 1 is undefined because its defining expression is not bounded in [ 0, 1 ].

Letting α = β in the above expression

${\displaystyle H_{1-X}={\frac {\beta -1}{2\beta -1}}}$ 

showing that for α = β the harmonic mean ranges from 0, for α = β = 1, to 1/2, for α = β → ∞.

The following are the limits with one parameter finite (non zero) and the other approaching these limits:

${\displaystyle {\begin{aligned}\lim _{\beta \to 0}H_{1-X}&={\text{ undefined }}\\\lim _{\beta \to 1}H_{1-X}&=\lim _{\alpha \to \infty }H_{1-X}=0\\\lim _{\alpha \to 0}H_{1-X}&=\lim _{\beta \to \infty }H_{1-X}=1\end{aligned}}}$ 

Although both harmonic means are asymmetric, when α = β the two means are equal.

The harmonic mean ( H ) of the lognormal distribution of a random variable X is

${\displaystyle H=\exp \left(\mu -{\frac {1}{2}}\sigma ^{2}\right),}$ 

where μ and σ² are the parameters of the distribution, i.e. the mean and variance of the distribution of the natural logarithm of X.

The harmonic and arithmetic means of the distribution are related by

${\displaystyle {\frac {\mu ^{*}}{H}}=1+C_{v}^{2}\,,}$ 

where C_v and μ^* are the coefficient of variation and the mean of the distribution respectively..

The geometric (G), arithmetic and harmonic means of the distribution are related by

${\displaystyle H\mu ^{*}=G^{2}.}$ 

The harmonic mean of type 1 Pareto distribution is

${\displaystyle H=k\left(1+{\frac {1}{\alpha }}\right)}$ 

where k is the scale parameter and α is the shape parameter.

For a random sample, the harmonic mean is calculated as above. Both the mean and the variance may be infinite (if it includes at least one term of the form 1/0).

Sample distributions of mean and variance

The mean of the sample m is asymptotically distributed normally with variance s².

${\displaystyle s^{2}={\frac {m\left[\operatorname {E} \left({\frac {1}{x}}-1\right)\right]}{m^{2}n}}}$ 

The variance of the mean itself is

${\displaystyle \operatorname {Var} \left({\frac {1}{x}}\right)={\frac {m\left[\operatorname {E} \left({\frac {1}{x}}-1\right)\right]}{nm^{2}}}}$ 

where m is the arithmetic mean of the reciprocals, x are the variates, n is the population size and E is the expectation operator.

Delta method

Assuming that the variance is not infinite and that the central limit theorem applies to the sample then using the delta method, the variance is

${\displaystyle \operatorname {Var} (H)={\frac {1}{n}}{\frac {s^{2}}{m^{4}}}}$ 

where H is the harmonic mean, m is the arithmetic mean of the reciprocals

${\displaystyle m={\frac {1}{n}}\sum {\frac {1}{x}}.}$ 

s² is the variance of the reciprocals of the data

${\displaystyle s^{2}=\operatorname {Var} \left({\frac {1}{x}}\right)}$ 

and n is the number of data points in the sample.

Jackknife method

A jackknife method of estimating the variance is possible if the mean is known. This method is the usual 'delete 1' rather than the 'delete m' version.

This method first requires the computation of the mean of the sample (m)

${\displaystyle m={\frac {n}{\sum {\frac {1}{x}}}}}$ 

where x are the sample values.

A series of value w_i is then computed where

${\displaystyle w_{i}={\frac {n-1}{\sum _{j\neq i}{\frac {1}{x}}}}.}$ 

The mean (h) of the w_i is then taken:

${\displaystyle h={\frac {1}{n}}\sum {w_{i}}}$ 

The variance of the mean is

${\displaystyle {\frac {n-1}{n}}\sum {(m-w_{i})}^{2}.}$ 

Significance testing and confidence intervals for the mean can then be estimated with the t test.

Size biased sampling

Assume a random variate has a distribution f( x ). Assume also that the likelihood of a variate being chosen is proportional to its value. This is known as length based or size biased sampling.

Let μ be the mean of the population. Then the probability density function f*( x ) of the size biased population is

${\displaystyle f^{*}(x)={\frac {xf(x)}{\mu }}}$ 

The expectation of this length biased distribution E^*( x ) is

${\displaystyle \operatorname {E} ^{*}(x)=\mu \left[1+{\frac {\sigma ^{2}}{\mu ^{2}}}\right]}$ 

where σ² is the variance.

The expectation of the harmonic mean is the same as the non-length biased version E( x )

${\displaystyle E^{*}(x^{-1})=E(x)^{-1}}$ 

The problem of length biased sampling arises in a number of areas including textile manufacture pedigree analysis and survival analysis

Akman et al. have developed a test for the detection of length based bias in samples.

Shifted variables

If X is a positive random variable and q > 0 then for all ε > 0

${\displaystyle \operatorname {Var} \left[{\frac {1}{(X+\epsilon )^{q}}}\right]<\operatorname {Var} \left({\frac {1}{X^{q}}}\right).}$ 

Moments

Assuming that X and E(X) are > 0 then

${\displaystyle \operatorname {E} \left[{\frac {1}{X}}\right]\geq {\frac {1}{\operatorname {E} (X)}}}$ 

This follows from Jensen's inequality.

Gurland has shown that for a distribution that takes only positive values, for any n > 0

${\displaystyle \operatorname {E} \left(X^{-1}\right)\geq {\frac {\operatorname {E} \left(X^{n-1}\right)}{\operatorname {E} \left(X^{n}\right)}}.}$ 

Under some conditions

${\displaystyle \operatorname {E} (a+X)^{-n}\sim \operatorname {E} \left(a+X^{-n}\right)}$ 

where ~ means approximately equal to.

Sampling properties

Assuming that the variates (x) are drawn from a lognormal distribution there are several possible estimators for H:

${\displaystyle {\begin{aligned}H_{1}&={\frac {n}{\sum \left({\frac {1}{x}}\right)}}\\H_{2}&={\frac {\left(\exp \left[{\frac {1}{n}}\sum \log _{e}(x)\right]\right)^{2}}{{\frac {1}{n}}\sum (x)}}\\H_{3}&=\exp \left(m-{\frac {1}{2}}s^{2}\right)\end{aligned}}}$ 

where

${\displaystyle m={\frac {1}{n}}\sum \log _{e}(x)}$ 
${\displaystyle s^{2}={\frac {1}{n}}\sum \left(\log _{e}(x)-m\right)^{2}}$ 

Of these H₃ is probably the best estimator for samples of 25 or more.

Bias and variance estimators

A first order approximation to the bias and variance of H₁ are

${\displaystyle {\begin{aligned}\operatorname {bias} \left[H_{1}\right]&={\frac {HC_{v}}{n}}\\\operatorname {Var} \left[H_{1}\right]&={\frac {H^{2}C_{v}}{n}}\end{aligned}}}$ 

where C_v is the coefficient of variation.

Similarly a first order approximation to the bias and variance of H₃ are

${\displaystyle {\begin{aligned}{\frac {H\log _{e}\left(1+C_{v}\right)}{2n}}\left[1+{\frac {1+C_{v}^{2}}{2}}\right]\\{\frac {H\log _{e}\left(1+C_{v}\right)}{n}}\left[1+{\frac {1+C_{v}^{2}}{4}}\right]\end{aligned}}}$ 

In numerical experiments H₃ is generally a superior estimator of the harmonic mean than H₁. H₂ produces estimates that are largely similar to H₁.

The Environmental Protection Agency recommends the use of the harmonic mean in setting maximum toxin levels in water.

In geophysical reservoir engineering studies, the harmonic mean is widely used.

• Contraharmonic mean
• Generalized mean
• Harmonic number
• Rate (mathematics)
• Weighted mean
• Parallel summation
• Geometric mean
• Weighted geometric mean
• HM-GM-AM-QM inequalities
• Harmonic mean p-value