Analyze gamma density, CDF, survival, mean, and variance. Switch scale or rate inputs with ease. Export results quickly and verify examples without confusion today.
Example parameters: shape = 3 and scale = 2.
| x | CDF | |
|---|---|---|
| 1 | 0.037908 | 0.014388 |
| 2 | 0.09197 | 0.080301 |
| 3 | 0.125511 | 0.191153 |
| 4 | 0.135335 | 0.323324 |
| 5 | 0.128258 | 0.456187 |
For shape k and scale θ, the probability density function is:
f(x) = xk-1 e-x/θ / (Γ(k) θk), for x ≥ 0
The cumulative probability is:
F(x) = P(k, x/θ)
When rate β is entered, the scale becomes θ = 1/β.
Mean = kθ
Variance = kθ²
Standard Deviation = √(kθ²)
Mode = (k − 1)θ when k > 1
Gamma distribution helps model waiting times and positive skewed data. It appears in reliability, insurance, biology, queues, and risk analysis. This calculator gives fast estimates for density, cumulative probability, upper tail probability, and summary measures.
Many real processes stay above zero and vary unevenly. Repair times, rainfall totals, and claim sizes often show this pattern. Gamma distribution fits such cases well. It uses shape and scale or shape and rate parameters. That flexibility makes it useful for analysts and students.
The tool computes probability density at a chosen value. It also computes cumulative probability up to that value. The survival value shows probability above the input. It also returns mean, variance, standard deviation, and mode when valid. These outputs help compare spread, central tendency, and tail behavior.
For shape k and scale θ, the density is: f(x) = x^(k-1) e^(-x/θ) / (Γ(k) θ^k), for x ≥ 0.
The cumulative probability uses the regularized lower incomplete gamma function: F(x) = P(k, x/θ).
If you enter rate β, then scale becomes 1/β. Mean equals kθ. Variance equals kθ². Standard deviation equals √(kθ). Mode equals (k−1)θ when k is greater than one.
Choose your parameter style first. Enter shape and either scale or rate. Enter the x value where you want probability results. Submit the form to see the output above it. Use the export buttons to save the displayed results.
A larger shape value usually shifts the curve right. A larger scale stretches the distribution wider. Higher x values raise the cumulative probability. The upper tail then becomes smaller. Use the example table below to test how parameter changes affect results.
Use this calculator when data are continuous and positive. It does not fit negative values. Very small shape values create stronger right skew. Large shape values create smoother curves. Always check units before interpreting scale or rate. Match your input style to your textbook, report, or software. That simple step prevents avoidable parameter mistakes. Consistent parameter choices improve communication across teams, dashboards, audits, and statistical reports.
It models positive continuous values. It is often used for waiting times, lifetimes, rainfall totals, queue delays, and claim amounts with right skew.
They are inverse forms of the same parameter. Scale equals 1 divided by rate. The calculator automatically converts one form into the other.
The gamma distribution is defined on nonnegative values only. Negative inputs fall outside the valid support, so the calculator blocks them.
The interior mode exists only when the shape parameter is greater than 1. For smaller values, the curve does not peak inside the positive range.
It shows the probability of observing a value greater than the selected x. It is useful for exceedance and risk checks.
Yes. Gamma models are common in reliability and maintenance studies when repair or waiting times are positive and skewed.
Yes. It is useful for homework, exam review, and quick validation of hand calculations involving density, cumulative probability, and moments.
Results stay consistent only when equivalent values are entered. If scale and rate are not exact inverses, the distribution changes and so do outputs.
Important Note: All the Calculators listed in this site are for educational purpose only and we do not guarentee the accuracy of results. Please do consult with other sources as well.