RESEARCH PROJECT · 2025 ENVIRONMENTAL DATA

A Cross-Sectional Analysis of Environmental Radiation Levels Across Four U.S. Locations and Relevance to Radiation Exposure During Long-Duration Spaceflight

An exploratory epidemiological-style analysis examining geographic variation in environmental radiation measurements and what these patterns can — and cannot — tell us about radiation-related cancer risk during future space missions.

Elizabeth Khimey
NYC Lab High School for Collaborative Studies

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Research Approach

From a Broad Question to an Exploratory Epidemiological Analysis

This project began with a broader question about the relationship between radiation exposure and cancer risk during long-duration spaceflight.

My original goal was to explore this question using evidence from astronauts and other exposed populations. However, I encountered an important limitation: the number of astronauts with long-duration deep-space radiation exposure is very small.

This creates a challenge for epidemiological research. When a sample is very small, it becomes difficult to identify reliable patterns, estimate risk with confidence, or determine whether an observed relationship is meaningful.

Research pivot:

Because the astronaut population was too small for the type of epidemiological analysis I wanted to explore, I changed the scope of the project. I conducted an exploratory epidemiological-style analysis using environmental radiation-monitoring data from four U.S. locations.

What the Analysis Allowed Me to Investigate

The environmental dataset provided thousands of radiation measurements, giving me a larger dataset in which to examine geographic differences, distributions, temporal patterns, and statistical relationships.

This approach does not directly measure cancer risk in astronauts. Instead, it allowed me to investigate radiation measurements using statistical and epidemiological concepts while recognizing the limitations of the available evidence.

Broad Research Question
Small Astronaut Sample
Research Limitation
Environmental Dataset
Exploratory Analysis
01 · Overview

The Research Question

As scientists develop plans for longer missions to the Moon and Mars, radiation exposure remains one of the major health concerns of deep-space exploration.

Central question:

How does radiation exposure relate to cancer risk, and what can environmental radiation measurements tell us about radiation exposure relevant to long-duration spaceflight?

Ionizing radiation can damage DNA, and accumulated or incorrectly repaired DNA damage can contribute to cancer. However, directly studying cancer risk in astronauts is difficult because relatively few people have experienced long-duration deep-space missions.

This project therefore combines background research on radiation and cancer with an exploratory analysis of 2025 environmental radiation-monitoring data from four U.S. locations. The environmental analysis was chosen as an alternative approach after recognizing that the small number of astronauts with long-duration deep-space exposure makes direct epidemiological analysis of astronaut cancer outcomes difficult.

02 · Radiation Biology

Why Does Radiation Matter?

Ionizing radiation has enough energy to remove electrons from atoms and can damage biological molecules, including DNA. Cells have repair systems, but repair is not always perfect.

Radiation Exposure
DNA Damage
Cellular Repair
Mutation
Potential Cancer

DNA damage does not automatically cause cancer. Cells can repair damage, and heavily damaged cells may die. However, mutations affecting genes that control cell growth and division can sometimes contribute to cancer.

03 · Space Radiation

Where Does Space Radiation Come From?

Galactic Cosmic Rays

Extremely energetic particles originating outside our solar system. They are continuously present and can be difficult to shield against.

Solar Particle Events

Bursts of energetic particles released by the Sun that can temporarily increase radiation levels around a spacecraft.

Trapped Radiation

Charged particles trapped by Earth's magnetic field in regions known as the Van Allen radiation belts.

Earth's Protection

Earth's atmosphere and magnetic field provide important protection from parts of the space radiation environment.

04 · Cancer Risk

Does More Radiation Mean More Cancer?

Scientists have strong evidence that sufficiently high doses of ionizing radiation can increase cancer risk. Evidence comes from populations including atomic-bomb survivors, radiation-exposed workers, patients receiving certain radiation treatments, and other exposed groups.

Understanding the risks associated with relatively low doses is more difficult. Cancer is influenced by many factors, including age, genetics, smoking, diet, ultraviolet radiation, occupation, lifestyle, and other environmental exposures.

The Linear No-Threshold Model

The Linear No-Threshold model is one approach used to estimate radiation-related cancer risk. Under this model, risk is assumed to increase approximately linearly with radiation dose, with no dose considered completely risk-free. However, the LNT model is a risk-estimation model rather than a direct prediction of what will happen to every individual.

05 · Previous Evidence

Astronauts and Radiation Workers

Astronaut Studies

Researchers have studied early NASA astronauts to investigate whether estimated space-radiation exposure was associated with cancer mortality. These studies are valuable but limited by the small number of astronauts and relatively few cancer deaths.

INWORKS

The International Nuclear Workers Study included approximately 309,932 workers from France, the United Kingdom, and the United States. Researchers found that mortality from solid cancer increased as cumulative radiation dose increased, although uncertainty was greater at relatively low doses.

Important distinction:

Occupational radiation exposure is not identical to deep-space radiation. Space radiation includes galactic cosmic rays and solar particle events with different physical characteristics.

06 · Environmental Study

2025 Environmental Radiation Analysis

Why This Is an Epidemiological-Style Analysis

Epidemiology investigates patterns of health-related exposures and outcomes across populations. In this project, environmental radiation measurements represent the exposure-related variable being investigated, while location serves as the population-level comparison.

Because this dataset does not contain individual cancer diagnoses, mortality, medical histories, or individual radiation exposure, this study cannot estimate cancer risk directly. Instead, it represents a small exploratory analysis of environmental radiation exposure patterns.

Data Quality and Observation Periods

Before comparing radiation levels between locations, I evaluated the size, completeness, and observation periods of each dataset. I examined the number of observations, missing radiation measurements, missing timestamps, negative measurements, and the dates and times covered by each monitoring station.

Dataset sizes for the four study locations
Figure 1. Number of radiation observations included in each location's 2025 dataset. The datasets contain different numbers of observations, which should be considered when comparing locations.
Missing radiation measurements across the four locations
Figure 2. Assessment of missing dose-equivalent rate measurements across the four study locations. The datasets contained no missing radiation measurements.
Missing timestamps across the four locations
Figure 3. Assessment of missing timestamps across the four study locations. No missing timestamps were identified in the datasets used for analysis.
Negative radiation measurements across the four locations
Figure 4. Assessment of negative radiation measurements across the four study locations. No negative dose-equivalent rate measurements were identified.
Start and end dates and times for each radiation monitoring location
Figure 5. Observation periods for the four monitoring locations, showing the beginning and ending dates and times of the available measurements. Edison began monitoring in March 2025, while Phoenix, Miami, and Seattle began in January 2025.

The monitoring periods were not identical across all four locations. Phoenix, Miami, and Seattle had observations beginning in January 2025, while Edison began in March 2025. All four datasets extended through December 31, 2025. This difference is an important limitation because Edison contains fewer months of observations.

Descriptive Results

After evaluating the datasets, I examined the distribution of environmental radiation measurements at each location. The primary descriptive measure was the mean dose-equivalent rate, measured in nanosieverts per hour (nSv/h).

Mean environmental radiation dose-equivalent rate by location
Figure 6. Mean environmental dose-equivalent rate by location. Phoenix had the highest mean measurement at 85.21 nSv/h, followed by Miami at 47.84 nSv/h, Edison at 40.81 nSv/h, and Seattle at 27.07 nSv/h.
Descriptive statistics for environmental radiation measurements by location
Figure 7. Descriptive statistics for environmental radiation measurements by location, including mean, standard deviation, median, interquartile range, minimum, maximum, and upper percentiles. The statistics show differences in the typical values and ranges of radiation measurements among the four locations.
Box plot showing distribution of environmental radiation measurements by location
Figure 8. Distribution of environmental radiation measurements across the four locations. The box plot shows differences in the central values, spread, and ranges of the measurements, with Phoenix generally showing higher measurements than the other locations.

Phoenix had the highest mean dose-equivalent rate at 85.21 nSv/h, followed by Miami at 47.84 nSv/h, Edison at 40.81 nSv/h, and Seattle at 27.07 nSv/h. The distributions also differed in their ranges and overall spread.

Why might radiation levels differ?

Background radiation is not exactly the same everywhere. Possible factors include altitude, geology, naturally radioactive materials in soil and rocks, atmospheric conditions, and geography. However, the dataset alone cannot determine exactly why one location had higher measurements than another.

Phoenix
85.21 nSv/h
Miami
47.84 nSv/h
Edison
40.81 nSv/h
Seattle
27.07 nSv/h
85.21
nSv/h · Phoenix, Arizona
47.84
nSv/h · Miami, Florida
40.81
nSv/h · Edison, New Jersey
27.07
nSv/h · Seattle, Washington
Location Mean Dose-Equivalent Rate
Phoenix, Arizona 85.21 nSv/h
Miami, Florida 47.84 nSv/h
Edison, New Jersey 40.81 nSv/h
Seattle, Washington 27.07 nSv/h

Methods

The study was designed as a cross-sectional, exploratory comparison of environmental radiation measurements across four U.S. locations. The primary exposure-related variable was dose-equivalent rate, while geographic location was the primary comparison variable.

Because the study used environmental monitoring data rather than individual-level health records, the analysis focuses on differences in measured radiation rather than individual cancer outcomes.

The primary variable was dose-equivalent rate, measured in nanosieverts per hour (nSv/h). Descriptive statistics included the mean, standard deviation, median, interquartile range, minimum, maximum, and upper percentiles.

A Kruskal-Wallis test was used to compare radiation measurements among the four locations, followed by pairwise Mann-Whitney U tests with Bonferroni correction.

07 · Results

Statistical Results

Statistical tests were used to determine whether the observed radiation measurements differed significantly among the four study locations.

Kruskal-Wallis test results with Miami zero measurements included
Figure 9. Kruskal-Wallis test comparing dose-equivalent rate distributions among Phoenix, Miami, Edison, and Seattle, with the Miami zero measurements included. The test produced a large H statistic and p < 0.001, providing strong statistical evidence that the four distributions were not all the same.
Pairwise Mann-Whitney U test results
Figure 10. Pairwise Mann-Whitney U tests comparing dose-equivalent rate distributions between each pair of locations. The extremely small p-values provide strong evidence of differences between the location pairs.
Pairwise Mann-Whitney U test results with adjusted p-values
Figure 11. Pairwise Mann-Whitney U comparisons with Bonferroni-adjusted p-values. All six location comparisons remained statistically significant after correction for multiple comparisons.
Kruskal-Wallis H statistic and epsilon-squared effect size
Figure 12. Summary of the Kruskal-Wallis analysis, including the H statistic, total sample size, number of groups, and epsilon-squared effect size. The epsilon-squared value of approximately 0.928 indicates a very large difference among the distributions in this environmental dataset.
28,315.01 Kruskal-Wallis H statistic
p < 0.001 Kruskal-Wallis significance
≈ 0.928 Epsilon-squared effect size

Kruskal-Wallis Test

The Kruskal-Wallis test provided strong statistical evidence that the distributions of radiation measurements were not the same across all four locations.

The test provides evidence that at least one location had a different pattern of radiation measurements from the others.

Pairwise Mann-Whitney U Tests

Pairwise Mann-Whitney U tests were then performed between all six pairs of locations. These tests compare locations two at a time and are useful when the data may not follow a normal distribution.

All pairwise comparisons produced extremely small p-values, and all remained statistically significant after Bonferroni correction.

How should the p-value be interpreted?

An extremely small p-value does not mean that the true p-value is literally zero. It indicates that the observed differences would be very unlikely under the assumption that the groups had the same distributions.

Statistical Significance vs. Practical Significance

The extremely small p-values are partly related to the very large number of observations. With thousands of measurements per location, even relatively small differences can produce very small p-values.

These findings support an association between geographic location and the distribution of measured environmental radiation in this dataset. They should not be interpreted as evidence that geographic location itself causes differences in radiation levels, or that the differences directly translate into differences in cancer risk.

Bonferroni Correction

Because six pairwise statistical tests were performed, there was a greater chance of obtaining a statistically significant result simply by chance. The Bonferroni correction makes the significance requirement stricter to account for these multiple comparisons.

Epsilon-Squared Effect Size

Because statistical significance does not explain the magnitude of the difference, I calculated epsilon-squared as an effect-size measure for the Kruskal-Wallis test.

The estimated epsilon-squared effect size was approximately 0.928, indicating a very large difference in the distributions of measurements among the locations.

This suggests that the location groups were very different within this environmental radiation dataset.

Important interpretation:

The value of 0.928 does not mean that 92.8% of cancer risk is caused by location or radiation. The effect size describes the differences observed in this environmental dataset.

08 · Data Investigation

The Miami Data Mystery

Descriptive statistics for Miami radiation measurements
Figure 13. Descriptive statistics for the Miami radiation measurements. The minimum value of 0 nSv/h was substantially lower than the other measurements and prompted further investigation of the Miami dataset.
Miami zero measurements and percentage of observations
Figure 14. Number and percentage of zero radiation measurements identified in the Miami dataset. Sixteen zero measurements were identified among 7,349 observations, representing approximately 0.218% of the Miami dataset.
Miami mean radiation measurement with and without zero measurements
Figure 15. Comparison of the Miami mean dose-equivalent rate with zero measurements included and excluded. Removing the 16 zero measurements changed the mean by approximately 0.10 nSv/h, indicating little effect on the overall Miami average.

Miami contained 16 measurements of 0 nSv/h out of 7,349 observations. These represented approximately 0.218% of the Miami dataset.

16 zero measurements
7,349 total Miami observations
0.218% of Miami observations

While analyzing the data, Miami had a minimum measurement of 0 nSv/h. This was unusual because nearly all of the surrounding measurements were around 48 nSv/h.

Instead of immediately removing these measurements, I tested how much they affected the results.

Removing the zero measurements changed the Miami average by approximately 0.10 nSv/h. Therefore, removing the zero measurements had very little effect on the overall Miami average.

The dataset alone cannot determine whether these zero values represent missing measurements, invalid measurements, a detector problem, or a data-recording issue.

Importantly, the Kruskal-Wallis result also remained highly significant when the Miami zero measurements were removed.

09 · Patterns

Monthly, Hourly & Gamma Measurements

Monthly variation in environmental radiation measurements
Figure 16. Monthly variation in environmental radiation measurements across the four study locations during 2025. Radiation measurements varied throughout the year, with the magnitude and pattern of variation differing among locations.
Monthly dose-equivalent rate by location
Figure 17. Monthly dose-equivalent rates by location. Phoenix showed monthly averages ranging from approximately 82.74 to 89 nSv/h, while Seattle ranged from approximately 25.97 to 28.15 nSv/h. The differences demonstrate that radiation measurements varied across both location and month.
Mean environmental radiation dose-equivalent rate by hour
Figure 18. Mean environmental dose-equivalent rate by hour of the day across the four study locations. The hourly patterns show variation in measurements throughout the day but do not establish that a specific environmental factor caused those differences.
Dose-equivalent rate and gamma count measurements across the four study locations
Figure 19. Dose-equivalent rate and gamma count-rate measurements across the four study locations. The figure shows how the measured dose-equivalent and gamma count-rate values differed among locations, providing a comparison of the radiation measurements recorded by the monitoring detectors.
Correlation between dose-equivalent rate and gamma count rates in Edison
Figure 20. Correlations between dose-equivalent rate and gamma count-rate measurements in Edison. Several gamma count rates showed strong positive relationships with dose-equivalent rate, including R05 (r = 0.789), R06 (r = 0.784), and R07 (r = 0.791). These correlations indicate that the measurements tended to vary together but do not establish causation.
Descriptive statistics for environmental radiation measurements
Figure 21. Descriptive statistics and upper-percentile measurements for the four study locations, including the 95th and 99th percentiles. Phoenix had the highest typical and upper-percentile measurements, while Phoenix and Edison also showed maximum values that were substantially higher than their typical measurements.

Monthly Variation

I also examined the average radiation measurement by month. The analysis showed that radiation levels varied over the year, but the pattern differed among locations.

Phoenix monthly averages ranged from approximately 82.74 to 89 nSv/h, while Seattle ranged from approximately 25.97 to 28.15 nSv/h.

This shows that environmental radiation is not exactly the same throughout the year. However, these monthly patterns alone cannot tell us what environmental factor caused the changes.

Hourly Variation

I also examined the average radiation measurement by hour of the day. This was done to identify possible patterns in radiation levels throughout the day.

However, since environmental conditions, monitoring stations, and sampling patterns can be different at each location, these hourly differences should only be viewed as patterns in the data. They do not prove that a specific environmental factor caused the changes.

Gamma Count Rates

The datasets also included gamma count-rate measurements from the detector variables. I examined the relationship between dose-equivalent rate and gamma count rates.

For example, Edison showed fairly strong positive relationships with several gamma count-rate measurements, including R05 (r = 0.789), R06 (r = 0.784), and R07 (r = 0.791).

Seattle also showed positive relationships with most of the gamma count-rate measurements.

These results suggest that dose-equivalent rate and gamma count rates often increased or decreased together. However, correlation does not prove that one measurement caused the other to change.

Differences in correlation between locations also suggest that detector measurements may provide additional information that could be studied in future research.

Upper-Percentile Measurements

I also examined higher-percentile measurements to identify the upper portion of each location's distribution.

These results show that Phoenix had the highest typical radiation measurements as well as the highest measurements in the upper portion of the data. Edison and Phoenix also had maximum measurements that were much higher than their usual measurements.

These higher measurements are worth investigating, but one high measurement does not necessarily mean that the exposure was dangerous or that it increased cancer risk.

Factors such as how long the exposure lasted, the accuracy of the measurement, and the total amount of radiation exposure would need to be considered.

10 · Spaceflight

Why Does This Matter for Mars?

A future Mars mission could expose astronauts to the deep-space radiation environment for months during the journey to Mars, during time on the Martian surface, and during the return trip.

Shielding

Spacecraft materials can reduce radiation exposure, but additional shielding increases spacecraft mass.

Water

Hydrogen-rich materials such as water can potentially be positioned around crew areas as part of radiation protection.

Supplies

Food and other materials already required for a mission could also contribute to shielding around crew living areas.

Radiation Shelters

Specially protected areas could provide additional protection during intense solar particle events.

11 · Limitations

What This Study Cannot Tell Us

The environmental analysis demonstrates geographic differences in measured radiation. It does not directly measure cancer outcomes or individual radiation exposure.

01 · Astronaut Population

There are relatively few astronauts with long-duration deep-space exposure.

02 · Radiation Type

Occupational radiation exposure is not identical to deep-space radiation.

03 · Environmental Data

Monitoring stations measure environmental conditions rather than individual human exposure.

04 · Other Risk Factors

Cancer is influenced by age, genetics, smoking, UV radiation, lifestyle, occupation, and other factors.

05 · Long Latency

Cancer can develop many years after radiation exposure, requiring long-term follow-up.

06 · Unequal Observation Periods

Edison began in March 2025 while the other three locations began in January 2025.

07 · No Cancer Outcomes

The environmental dataset does not contain cancer diagnoses, mortality, or individual medical information.

References

References

  1. U.S. Environmental Protection Agency. Why Do I See Higher Levels of Radiation at Some Monitor Locations? EPA RadNet
  2. NASA. Space Radiation Is Risky Business for the Human Body. NASA
  3. Centers for Disease Control and Prevention. Health Effects of Radiation. CDC
  4. PMC Article: Radiation Exposure and Cancer Risk. PubMed Central. PubMed Central
  5. PMC Article: Radiation, Cancer Risk, and Epidemiological Evidence. PubMed Central. PubMed Central
  6. American Association for Cancer Research. Cancer Risk Estimates: What Do Those Numbers Mean? AACR
  7. NASA. Why Space Radiation Matters. NASA
12 · Conclusion

What Does the Evidence Tell Us?

The evidence provides scientific reason to be concerned about radiation exposure while also showing why the exact cancer risk from deep-space radiation remains difficult to determine.

One of the most important outcomes of this project was methodological. I began with the goal of exploring radiation and cancer risk in the context of astronauts, but the limited number of astronauts with long-duration deep-space exposure made a direct epidemiological analysis difficult. Rather than treating a small sample as sufficient evidence, I changed the approach and developed an exploratory analysis using environmental radiation data.

This environmental study found substantial differences in measured radiation levels among four U.S. locations during 2025. Phoenix had the highest average dose-equivalent rate, while Seattle had the lowest.

The statistical analysis also provided strong evidence that the distributions of measured environmental radiation differed among the four locations. Pairwise comparisons remained statistically significant after Bonferroni correction.

However, these results do not demonstrate that people living in locations with higher environmental measurements have higher cancer rates. The dataset does not contain individual radiation exposure, cancer outcomes, age, sex, smoking history, occupation, medical history, or long-term follow-up.

The bigger question:

How can scientists better estimate and reduce the long-term health risks of radiation during missions beyond Earth's protective magnetic field?

The findings of this project suggest that radiation measurements can vary substantially across environments, but environmental measurements on Earth cannot be directly substituted for measurements of deep-space radiation exposure.

Future research will require better astronaut health datasets, improved models of space-radiation exposure, and continued investigation of how different types of radiation affect human biology.

Ultimately, protecting astronauts from radiation will require both better evidence about long-term health effects and practical strategies for reducing exposure during missions to the Moon, Mars, and beyond.

Final Takeaway

This study does not show that higher environmental radiation causes higher cancer risk. Instead, it demonstrates how epidemiological and statistical methods can be used to investigate radiation patterns while carefully distinguishing statistical evidence from conclusions about human health.