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. 2010 Apr 23;9(1):50–58. doi: 10.2203/dose-response.09-051.Hart

Cancer Mortality in Six Lowest Versus Six Highest Elevation Jurisdictions in the U.S.

John Hart 1,
PMCID: PMC3057635  PMID: 21431077

Abstract

Low levels of background radiation exist around us continuously. These levels increase with increasing land elevation, allowing a comparison of low elevations to high elevations in regard to an outcome such as cancer death rates. The present study compares archived cancer mortality rates in six low versus six high elevation jurisdictions. The study also compares mortality rates for all causes, heart disease, and diabetes in low versus high elevation jurisdictions in an effort to see if other mortality outcomes are different in low versus high elevations. Statistically significant decreases in mortality, with very large effect sizes, were observed in high land elevation for three of the four outcomes, including cancer. One possible explanation for the decreased mortality in high elevation jurisdictions is radiation hormesis. Another possible explanation, at least in the case of heart disease mortality, is the physiologic responses that accompany higher elevations regarding decreased oxygen levels. Since this is an ecological study, no causal inferences can be made, particularly when viewpoints on possible effects of low level radiation are diametrically opposed. Further research is indicated.

Keywords: Radiation effects, background radiation, cancer, mortality

INTRODUCTION

There is controversy as to whether low level radiation poses a significant health risk. One side of the argument holds to the linear no-threshold (LNT) model, which essentially states that even the smallest amounts of radiation are harmful (Preston, 2008). The other side of the argument states that low level radiation appears to be not only harmless (Nair et al, 1999), but may actually provide a health benefit through hormesis (Allright et al, 1983; Jagger, 1998; Luckey, 2006; Scott and Di Palma, 2006). What is not controversial is that the levels of natural background radiation (NBR) are lower at lower elevations than at higher elevations (NRC, 2009). Jagger (1998), for example, in an apparently non-numeric method of selection of low states, compared low and high elevation states for cancer rates and found lower cancer rates in high elevation states.

The purpose of the present study is to compare cancer mortality rates in low versus high elevations, using a numeric method of jurisdiction selection, and to compare the difference, if any, to other mortality outcomes, one of which (heart disease) is also thought to be related to elevation (altitude) while the other mortality outcomes (all causes and diabetes) seemingly would be less-related to elevation. The null hypothesis is that there will be no difference in mortality rates between low and high elevation jurisdictions while the alternate hypothesis is that at least one of the outcomes will show a statistically significant difference. If there are differences between low and high elevations, then further research would be needed to determine causality of such an association given that the present inquiry is an ecological study.

METHODS

Age-adjusted mortality rates were obtained by jurisdiction for the following four mortality outcomes: 1) all causes, 2) malignant neoplasms (“cancer”), 3) diseases of the heart (“heart disease”), and 4) diabetes mellitus (“diabetes”) for the following five years: 2001 (Arias et al, 2003), 2002 (Kochanek et al, 2004), 2003 (Hoyert et al, 2006), 2004 (Minino et al, 2007), and 2005 (Kung et al, 2008). The outcomes of cancer mortality and heart disease were selected because of they have been linked with elevation (for heart disease, the term “altitude” is typically used in the literature). The other two mortality outcomes (all causes and diabetes) were selected because of their apparent lack of being linked to elevation, in an effort to further compare the cancer mortality rates to.

Jurisdictions were identified using the U.S. Geological Survey data by viewing their table of lowest and highest elevations by jurisdiction (U.S. Geological Survey, 2005). In this table’s lowest elevation column, six jurisdictions having the lowest elevation were selected (“low elevations”). As an example of the selection process, Delaware’s highest elevation is 448 feet above sea level while its lowest elevation is at sea level. Consequently, all people in Delaware were considered to live in areas not exceeding 448 feet above sea level. Six jurisdictions having the highest elevation were selected using similar methodology (“high elevations”). As an example of the selection process of jurisdictions in the high elevation category, Colorado’s lowest elevation is 3315 feet above sea level although its highest point is 14433 feet above sea level. Colorado was therefore considered to have its entire population living at an elevation of at least 3315 feet above sea level. The highest elevation jurisdiction in the low elevation category is Rhode Island, having a maximum elevation of 812 feet above sea level. The lowest elevation jurisdiction in the high elevation category is South Dakota, having a lowest elevation of 966 feet above sea level. The next highest elevation jurisdiction after 966 was Illinois, having a highest elevation of 1235 feet above sea level and a lowest elevation of 279 feet above sea level. Consequently, this state (Illinois) would not have been an appropriate addition to either the low or high elevation category because its highest elevation crosses over into the high elevation category when its lowest elevation (of 279 feet above sea level) would disqualify it from being in the high elevation category.

The annual NBR for all jurisdictions consisted a minimum value of 26 mrem for cosmic radiation at sea level + the additional radiation according to feet above sea level, as follows: up to 1000 feet above sea level= 2 additional mrem; 1000–2000 feet above sea level = 5 additional mrem; 2000–4000 feet above sea level = additional 9 mrem (NRC, 2009). The radiation levels from terrestrial sources (i.e., radon) were added as follows: 23 mrem for states bordering the Gulf coast (Louisiana, Mississippi, and Florida); 46 mrem for all other states (NRC, 2009). Ninety mrem can be assigned to the Colorado Plateau areas but since entire states were assessed, and some areas would not be part of the Colorado Plateau, the addition of the 90 mrem value was omitted. Thus, six jurisdictions in each of the low and high categories were obtained (Table 1). Five years of mortality data were analyzed for each of the 12 jurisdictions for the four mortality outcomes (Table 2). This meant that each mortality outcome in each of the two categories (low versus high elevation) had a sub-total of 30 observations each or a total of 60 observations for each mortality outcome (Table 2). The population for each jurisdiction, for each year, was estimated by the following calculation where total number of case, crude rate per 100,000 persons was known:

TotalnumberofcasesPopulation=Cruderate100,000

TABLE 1.

Elevations, means and standard deviations in low versus high jurisdictions.

LOW HIGHEST ELEVATION

Elevation/jurisdiction Feet above sea level Estimated mrem

Delaware 448 74
District of Columbia 410 74
Florida 345 51
Louisiana 535 51
Mississippi 806 51
Rhode Island 812 74
Mean 559.3 62.5
Standard deviation 209.9 12.6

HIGH LOWEST ELEVATION

Elevation/jurisdiction Feet above sea level Estimated mrem

Colorado 3315 81
Montana 1800 77
New Mexico 2842 81
South Dakota 966 74
Utah 2000 77
Wyoming 3099 81
Mean 2337.0 78.5
Standard deviation 902.6 2.9

p-value* 0.004 0.025
Effect size* 2.7 1.8
*

p-value and effect size pertain to comparison of low versus high elevation and NBR.

TABLE 2.

Age-adjusted mortality for four outcomes, five years, 12 jurisdictions (six in each of low and high elevation categories.

all causes age-adjusted rate cancer age-adjusted rate heart age-adjusted rate diabetes age-adjusted rate population
Low elevation
1 Delaware 2001 891.9 219.3 257.2 27.2 796595.0
2 Delaware 2002 838.2 193.8 236.0 25.9 807366.4
3 Delaware 2003 844.4 201.4 243.1 28.2 817530.1
4 Delaware 2004 823.3 207.4 232.3 24.1 830388.3
5 Delaware 2005 830.5 197.8 224.3 25.9 843531.3
6 District of Columbia 2001 1038.2 235.3 308.5 37.0 573811.6
7 District of Columbia 2002 1021.4 230.0 291.7 33.7 570885.0
8 District of Columbia 2003 982.3 199.7 287.3 32.2 564354.4
9 District of Columbia 2004 974.0 207.0 274.9 40.2 553537.0
10 District of Columbia 2005 971.4 206.0 268.2 34.6 550502.0
11 Florida 2001 799.7 187.2 233.2 22.0 16373238.1
12 Florida 2002 786.4 183.4 222.0 21.4 16712877.2
13 Florida 2003 776.0 181.4 212.7 21.8 17018869.8
14 Florida 2004 763.6 179.9 204.9 21.6 17396603.2
15 Florida 2005 749.4 178.1 194.6 22.6 17790729.2
16 Louisiana 2001 1005.9 227.4 280.1 41.7 4470292.3
17 Louisiana 2002 1000.5 222.9 269.6 42.1 4482596.6
18 Louisiana 2003 1004.6 221.9 274.2 40.8 4496263.6
19 Louisiana 2004 986.1 216.7 256.6 39.9 4515939.2
20 Louisiana 2005 1020.8 209.3 255.7 38.7 4523712.4
21 Mississippi 2001 1023.2 216.3 329.0 24.1 2859643.8
22 Mississippi 2002 1036.3 218.3 326.6 24.2 2871802.5
23 Mississippi 2003 1014.0 211.1 310.3 24.1 2881169.1
24 Mississippi 2004 998.2 209.8 300.1 23.6 2902926.8
25 Mississippi 2005 1026.9 208.4 306.8 23.5 2921060.5
26 Rhode Island 2001 806.4 200.6 240.5 21.7 1059638.4
27 Rhode Island 2002 809.5 196.9 239.1 21.2 1069743.2
28 Rhode Island 2003 786.9 190.2 227.7 20.2 1076222.1
29 Rhode Island 2004 741.1 194.1 216.0 21.9 1080641.6
30 Rhode Island 2005 747.3 184.1 213.8 21.6 1076137.2
mean 903.3 204.5 257.9 28.3 4482953.6
High elevation
1 Colorado 2001 787.8 169.6 181.0 18.7 4431323.4
2 Colorado 2002 790.2 171.8 178.9 17.7 4506325.2
3 Colorado 2003 784.3 169.2 178.0 19.0 4550586.1
4 Colorado 2004 736.4 160.1 162.7 18.2 4601593.0
5 Colorado 2005 742.8 159.6 162.0 19.2 4664934.7
6 Montana 2001 840.3 198.8 197.9 23.1 905356.6
7 Montana 2002 849.7 190.7 191.6 21.0 909440.8
8 Montana 2003 828.1 180.9 190.7 25.5 917633.0
9 Montana 2004 778.6 180.2 173.6 22.6 926829.3
10 Montana 2005 798.4 184.4 169.4 26.5 935703.3
11 New Mexico 2001 825.4 167.0 203.4 31.4 1830892.8
12 New Mexico 2002 815.0 172.5 193.3 32.9 1855147.4
13 New Mexico 2003 823.8 169.6 191.5 33.0 1874525.2
14 New Mexico 2004 778.9 161.9 180.4 31.7 1903354.6
15 New Mexico 2005 795.0 162.6 184.5 31.2 1928314.0
16 South Dakota 2001 784.8 187.9 218.1 24.2 758352.5
17 South Dakota 2002 771.2 182.4 209.7 22.6 761032.7
18 South Dakota 2003 790.5 189.6 208.0 22.9 764333.9
19 South Dakota 2004 746.4 176.8 187.1 25.2 770870.9
20 South Dakota 2005 757.0 180.9 182.1 25.8 775952.7
21 Utah 2001 776.8 143.4 185.2 31.9 2278567.6
22 Utah 2002 782.0 143.3 185.1 31.4 2316086.9
23 Utah 2003 782.3 144.1 183.5 31.2 2351332.4
24 Utah 2004 760.4 141.2 175.0 28.6 2389068.1
25 Utah 2005 731.2 139.4 162.6 30.4 2469571.6
26 Wyoming 2001 851.7 192.9 209.5 25.5 493750.0
27 Wyoming 2002 864.3 175.1 210.0 30.0 498685.8
28 Wyoming 2003 849.9 188.4 199.5 27.7 501261.6
29 Wyoming 2004 789.7 170.8 191.0 22.1 506531.8
30 Wyoming 2005 801.4 167.7 186.9 25.7 509319.1
mean 793.8 170.8 187.7 25.9 1829555.9

Analysis consisted of assessing the data as follows: a) skew, performed in a spreadsheet, with values between - 2 and + 2 considered to be not significantly different from normal (Garson, 2009); b) statistical differences between low and high elevation regions for the mortality outcomes, performed in SAS 9.2 (Cary, NC), elevation and NBR (performed in a spreadsheet), and c) effect size, performed in a spreadsheet for low versus high elevation groups for each variable, using a pooled standard deviation (Morgan et al, 2007). Interpretation of effect size ranges were as follows: Very large = greater than or equal to 1.00; Large = 0.80; Medium = 0.50; Small = 0.20 (Morgan et al, 2007). Since multiple tests for statistical significance were performed (n = 4, for the four mortality outcomes and n = 2 for elevations and NBR), a stringent Bonferroni-adjusted alpha was applied where the number of tests was divided by the traditional alpha of 0.05 (0.05/4 for outcomes) resulting in an adjusted alpha of 0.0125 (for outcomes) and 0.025 (0.05/2) for land and NBR, below or equal to which, statistical significance was considered to be present.

RESULTS

The data fell between skew values and −2 and + 2. Consequently, a t-test was used (two tails) to assess statistical differences. The mean elevation above sea level for low elevation jurisdictions was 559.3 compared to 2337 feet for high elevation jurisdictions, a statistically significant difference (p = 0.004) with a very large effect size (2.7). The mean annual NBR level for low elevation states was 62.5 mrem compare to 78.5 mrem for high elevation states, a statistically significant difference (p = 0.025; Figure 1), and therefore considered to be not statistical significant, while exhibiting a very large effect size (1.8) (Table 1).

FIGURE 1.

FIGURE 1.

NBR comparison between low and high elevation jurisdictions. The difference between low and high elevation jurisdictions (p = 0.025) was statistically significant along with a very large effect size between the two NBR means (effect size = 1.8).

Mortality rates for the outcomes were as follows. All causes: low elevation = 903.3; high elevation = 793.8, a statistically significant difference (p < 0.0001) with a very large effect size (1.3); heart disease: low elevation = 257.9; high elevation = 187.7, a statistically significant difference (p < 0.0001) with a very large effect size (2.5); Cancer: low elevation = 204.5; high elevation = 170.8, a statistically significant difference (p < 0.0001) with a very large effect size (2.1); Diabetes: low elevation = 28.3; high elevation = 25.9, a statistically insignificant difference (p < 0.1) with a small-medium effect size (0.4) (Figure 2).

FIGURE 2.

FIGURE 2.

Mortality rate means, differences, and effect sizes in low versus high elevation jurisdictions. Statistically significant differences, along with very large effect sizes were found between low and high elevation jurisdictions for all-causes mortality rates (p < 0.0001, effect size = 1.3), heart disease (p < 0.0001, effect size = 2.5), cancer (p < 0.0001, effect size = 2.1). Diabetes mortality was lower in higher elevation jurisdictions but this difference was not statistically significant (p = 0.1) with a small-medium effect size (0.4).

DISCUSSION

Cancer mortality rates were significantly lower in high elevation jurisdictions, which of course consist of higher NBR levels. This suggests the presence of radiation hormesis. However, heart disease mortality (as well as mortality from all causes) was also significantly lower in the high elevation jurisdictions. The finding of lower cancer mortality in the present study is consistent with similar previous studies. Jagger (1998) for example found that cancer death rates were 1.26 times that of Rocky Mountain states. Tao et al (2000) also found that in high NBR areas in China cancer mortality was also lower in high background radiation regions. Conversely, Cardis et al (2005) found a small increased risk of cancer for low dose exposure to nuclear workers.

In high elevations, decreased heart disease mortality may be related to decreased oxygen levels. In high altitudes effects of decreased oxygen can range from being factors in conditions such as pulmonary edema and right cardiac failure with peripheral edema (Ausiello et al, 2004), to being innocuous (Erdmann, 1998) to providing a protective effect against cardiovascular disease and cancer (Weinberg et al, 1987). In addition, this beneficial effect is thought to be related not to NBR but rather, due to thinner oxygen levels at higher altitudes (Weinberg et al, 1987). Mortimer et al (1977) theorize that the benefit of higher altitudes on arteriosclerotic heart disease may relate to the increased levels of exertion needed at higher altitudes for the same work done at lower altitudes, hence more exercise at the higher altitudes compared to lower altitudes. Whether the decreased heart disease mortality is due to increase NBR (i.e., radiation hormesis) or to physiologic responses that accompany decreased oxygen at high altitudes, or some other factor(s), or due to interaction of all of the above, is a question beyond the scope of this paper.

Mortality from all causes is an outcome that perhaps is too general to attempt to suggest possible explanations as to why it would be less in higher elevations. The outcome of diabetes, which was theorized by the author to not be related to elevation, showed the weakest relationship with elevation.

The question may arise as to the possibility of cancer clusters being a factor in the mortality rates. This was considered but no clusters were found for the jurisdictions and years in this study (CDC, 2009).

Ecological studies such as the present one do not allow causal inferences to be made but can be a first step for inquiry into new areas of research (Grimes and Schulz, 2002). Furthermore,there remains a lack of clear understanding in regard to the possible effects of exposure to low level radiation (Hendry et al, 2009). There is certainly a divergence of opinion as to what effects, if any, result from exposure to low level radiation. On the one hand there is the viewpoint that low level radiation provides a protective (hormetic) effect (Allright et al, 1983; Jagger, 1998; Luckey, 2006; Scott and Di Palma, 2006) while on the other hand there is the view that supports the LNT model (Brenner et al, 2003) as reported in BEIR VII (Health Physics, 2005). Clearly there is a need for further research, particularly they type that follows a given population over time such as done by Nair et al (2009), as well as research that assesses confounding variables.

CONCLUSION

Statistically significant decreases, with very large effect sizes were observed in high elevation jurisdictions compared to low elevation jurisdictions for the mortality outcomes of all causes, heart disease, and cancer. Diabetes mortality was also lower in high elevation jurisdictions compared to low elevation jurisdictions but the difference was not statistically significant and exhibited a small-medium effect size. These findings suggest the presence of radiation hormesis, at least in regard to the cancer mortality from a plausibility standpoint (i.e., hormesis theory). However, causal inferences cannot be made since this is an ecological study. Future study should include other variables that are thought to be related to cancer death rates, such as educational attainment, smoking, and diet.

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