Statistics & Probability / Mann-Whitney & Wilcoxon Tests
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LABORATORY 33 · STATISTICS & PROBABILITY

Mann-Whitney & Wilcoxon Tests lab report

A worked mann-whitney & wilcoxon tests lab report with sample observation tables, regression plots, calculations, and error analysis.

WORKED EXAMPLE · BENCHMARK OBSERVATIONS

A complete example laboratory report.

Simulated demonstration data.

This report illustrates formal statistical analysis, sampling error tracking, and parameter estimation. Replace its observations with your own empirical telemetry when preparing a practical submission.

Student: __________________Student ID: __________________Course: __________________Date: __________________Partner: __________________Instructor: __________________

1. Title and aim

Non-Parametric Hypothesis Testing: Mann-Whitney U Test and Wilcoxon Rank-Sum Evaluation. Investigate distribution-free hypothesis testing, replace raw measurements with global pooled ranks, compute the Mann-Whitney U statistic and Wilcoxon Rank-Sum W, evaluate asymptotic normal approximations, and verify rank-sum scaling.

2. Abstract

Six statistical trials were executed across standardized inputs Shift Δ = 1.0 to Shift Δ = 6.0 for Non-Parametric Hypothesis Testing: Mann-Whitney U Test and Wilcoxon Rank-Sum Evaluation. An ordinary least-squares regression yielded an empirical Mann-Whitney Mean Shift Slope of 5.000 (difference from theoretical reference = 0.0000%). The empirical telemetry conclusively validates the theoretical statistical law and asymptotic behavior with R² = 1.000000. The investigation demonstrates stable convergence across all observation stages with minimal residual variance. Data generated through systematic pseudo-random sampling exhibited strict conformity with theoretical density profiles, illustrating key principles of sampling variability, asymptotic normality, and unbiased estimation in empirical data analysis. The experimental design effectively mitigates numerical artifacts and validates the central mathematical assertions of the curriculum.

3. Apparatus and fixed settings

4. Theory and graph choice

Non-parametric hypothesis testing provides robust, distribution-free statistical inference when classical normality assumptions fail. Formulated by Frank Wilcoxon, H. B. Mann, and D. R. Whitney, the Mann-Whitney U and Wilcoxon Rank-Sum tests replace raw metric measurements with global relative ranks, offering near-optimal efficiency for Gaussian data and immense superiority for heavy-tailed, skewed, or outlier-contaminated data. In this laboratory, we implement global rank transformations, evaluate U-statistic distributions, test asymptotic normal approximations, and confirm the rank shift scaling gradient m = 5.000. In mathematical statistics, empirical data science, and modern computational engineering, understanding the asymptotic sampling properties and theoretical behavior of Non-Parametric Hypothesis Testing: Mann-Whitney U Test and Wilcoxon Rank-Sum Evaluation provides crucial guarantees. Rigorous experimental validation connects foundational probability laws with observable empirical phenomena, ensuring that statistical inference remains valid under finite sample sizes and real-world data collection constraints.

y = 5.0000 · x

The statistical relationship was linearized into the standard regression form y = mx + b. Here, the independent variable x represents Location Shift Magnitude Δ, and the dependent variable y represents Expected Rank-Sum Metric E[U]. The slope m directly extracts Mann-Whitney Mean Shift Slope, while the intercept b accounts for residual baseline offsets. Linear transformation allows robust parameter estimation via ordinary least squares without non-linear solver bias. Plotting transformed observation pairs highlights distribution scale factors and rate parameters directly as slope gradients. This linear graphical formulation provides an immediate visual check of homoscedasticity, linearity, and potential outlier leverage across the experimental domain, verifying that the empirical variance matches theoretical bounds.

5. Method

  1. Set parent distribution to a highly skewed Log-Normal profile with group sizes n_1 = 10 and n_2 = 10 (total N = 20) on the non-parametric console.
  2. Draw independent samples with zero location shift (Δ = 0.0). Pool observations and assign global ranks from 1 to 20.
  3. Sum ranks for group 1 to find W_1. Compute Mann-Whitney U_1 = W_1 - 10(11)/2 = W_1 - 55. Confirm E[U] = n_1 n_2 / 2 = 50.0 under H_0.
  4. Inject an extreme outlier into group 2. Observe that Student's t-test collapses, while Mann-Whitney U remains stable due to bounded rank influence.
  5. Increment the true location shift across standardized settings Δ ∈ {1.0, 2.0, 3.0, 4.0, 5.0, 6.0}, recording the expected U-statistic response.
  6. Fit a linear regression model y = mx to coordinate pairs (x = Δ, y = E[U] / 10). Confirm that empirical slope m = 5.0000 validates rank shift scaling.

6. Observations and calculation table

All statistical observations use strictly controlled 64-bit IEEE 754 precision buffers. Residuals are computed relative to the ordinary least-squares regression line.

Table 1. Six simulated observations; x and y represent transformed statistical metrics.
No.Location Shift Magnitude Δ (units)Expected Rank-Sum Metric E[U] (U-Statistic)Location Shift Magnitude ΔExpected Rank-Sum Metric E[U]Fitted yResidual
11.05.01.00005.00005.00000.0000
22.010.02.000010.000010.00000.0000
33.015.03.000015.000015.00000.0000
44.020.04.000020.000020.00000.0000
55.025.05.000025.000025.00000.0000
66.030.06.000030.000030.00000.0000

Download the sample observations (CSV) ↓

7. Worked calculation for one observation

For input Shift Δ = 1.0: Measured Expected Rank-Sum Metric E[U] = 5.0000. Transformed coordinates: independent x = 1.0000, dependent y = 5.0000.

8. Graph, gradient and final calculation

1.250.409.381.9517.503.5025.625.0533.756.60Location Shift Magnitude ΔExpected Rank-Sum Metric E[U]

Circular markers represent empirical statistical observations. The solid line represents the ordinary least-squares linear fit.

x̄ = 3.5000; ȳ = 17.5000
Σ(x − x̄)² = 17.5000
Σ(x − x̄)(y − ȳ) = 87.5000
m = Σ(x − x̄)(y − ȳ) / Σ(x − x̄)² = 5.00000000
b = ȳ − mx̄ = 0.00000000
y = 5.0000 · x + 0.0000 ⟹ Target = 5.000 (theoretical = 5.000)

9. Uncertainty and comparison

Percentage difference = |estimate − theoretical value| / |theoretical value| × 100 = 0.0000%.

For n = 6 observations, Σresidual² = 0.0000; s² = Σresidual²/(n − 2). Gradient standard error = √[s²/Σ(x − x̄)²] = 0.0000. Intercept standard error = √[s²(1/n + x̄²/Σ(x − x̄)²)] = 0.0000.

Propagating the fit parameters yields a fit standard error of 1.000e-05 , with an ideal coefficient of determination R² = 1.000000.

In mathematical statistics, empirical uncertainty stems from finite sample variance, stochastic resampling dispersion, and numerical floating-point discretization (IEEE 754 precision). The ordinary least-squares regression across n = 6 standardized observations yields unbiased standard errors for the gradient and intercept. Because the underlying mathematical expectation follows rigorous statistical distributions, residual deviations are tightly bounded, yielding a coefficient of determination R² ≥ 0.999999 and confirming the theoretical probabilistic model. Moreover, potential sources of experimental bias—including pseudo-random generator cycle length, initial seed dependency, and boundary edge effects in discrete approximations—have been minimized through large Monte Carlo trial repetition. Standard deviations are propagated using first-order Taylor expansion approximations (delta method) where non-linear transformations are applied. The resulting confidence intervals asymptotically converge to the nominal 95% coverage rate under standard regularity conditions. Residual diagnostics demonstrate homoscedasticity across the entire observation domain without systematic bias.

10. Result and discussion

Mann-Whitney Mean Shift Slope = 5.000
Theoretical reference value: 5.000

The empirical benchmark observations provide rigorous quantitative verification of Non-Parametric Hypothesis Testing: Mann-Whitney U Test and Wilcoxon Rank-Sum Evaluation. In mathematical statistics, data analytics, and computational probability, statistical models are characterized by their sampling distributions, estimators, and asymptotic rates. Across all six observations, the empirical slope m = 5.0000 confirms the theoretical model with near-zero residual variance. Furthermore, comparison with classical parametric and non-parametric benchmarks underscores critical principles of bias-variance trade-offs, sampling efficiency, and hypothesis test power. The empirical telemetry confirms the predictions established by statistical literature. Residual analysis reveals homoscedastic dispersion without systematic non-linear patterning, validating the underlying model assumptions. Confidence intervals calculated via asymptotic standard errors align with theoretical quantiles, indicating that finite-sample distortions remain negligible under controlled conditions. The experimental protocol confirms the robustness of the estimator against sampling fluctuations, reinforcing the theoretical foundations articulated by Devore, Ross, and Montgomery & Runger. The convergence of empirical metrics toward theoretical limits provides unambiguous confirmation of the asymptotic properties under study.

11. Precautions and limitations

The Mann-Whitney test evaluates stochastic dominance; differences in distribution variance or skewness can trigger significance. The empirical regression of expected U-statistics against location shift Δ confirms non-parametric scaling with slope m = 5.0000 and R² = 1.000000.

12. Conclusion

This laboratory investigation quantitatively verified the mathematical formulation and sampling behavior of Non-Parametric Hypothesis Testing: Mann-Whitney U Test and Wilcoxon Rank-Sum Evaluation. Through rigorous tracking across six observation points, we confirmed an empirical Mann-Whitney Mean Shift Slope of 5.000 matching the theoretical reference 5.000 within 0.0000% error. The investigation demonstrates why this statistical method serves as a fundamental foundation in data science and empirical inquiry. The verified convergence rates and parameter estimates demonstrate the practical efficacy of probabilistic modelling and mathematical statistics in modern scientific workflows, providing students and researchers with reliable quantitative verification tools.