Abstract
Todays, Climate change can be effect on the intensity of ultraviolet (UV) radiation and cause of many human diseases. In this cross-sectional study, changes of the intensity of UV ray were associated with the changes in latitude and longitude, height, climatic conditions, natural and human-made artifacts. Given that the highest radiation intensity was at the beginning of the summer, the radiation rate of UV ray in Mashhad was measured in the summer using a Hagner radiometer, the UV-A model. The radiation rate of the UV ray was determined in 2000 stations, which were 5 km far from each other. Data were analyzed using SPSSv16 software, T-test, and ANOVA tests. The results of this study showed that the radiation rate of UV ray in Mashhad was 0.49±0.143 mSv per year. The findings showed that latitudinal and longitudinal changes did not have a significant effect on the intensity of UV radiation (P > 0.001). The changes in the height above the sea level influenced the irradiance rate of UV and increasing the height above the sea level raised UV radiation (P < 0.001). Human artifacts significantly changed the rate of UV radiation (P < 0.001). Cloudy, semi-cloudy and sunny conditions had the most effects on UV radiation (P < 0.001). The results revealed that the average rate of UV ray in Mashhad was below the global standard (10 W/m2 for UV ray), and traffic in open air could not be risky.
Keywords: Radiation, Ultraviolet, Ionizing radiation, Mashhad
Specifications Table
| Subject area | Environmental sciences |
| More specific subject area | Description of hazardous natural rays |
| Type of data | Tables and figures |
| How data was acquired | The data were collected by 2000 sampling stations in different parts of the city. The UV radiation was measured using Hagner radiometer (model UV-A in watt/m2). |
| Data format | Raw, analyzed |
| Experimental factors | The sampling points were approximately 5000 meters far from each other |
| Experimental features | In this study, all conditions for the selection of sampling points, as well as the method for measuring ultraviolet radiation, were in accordance with the conditions set out in the valid references. |
| Data source location | Mashhad, Khorasan Razavi province, Iran |
| Data accessibility | Data are included in this article |
Value of the data
-
•
UV is the most important cosmic rays. UV radiation with medium and short wavelengths endangers human and living organisms in the open air. Therefore, continuous and periodic monitoring of this radiations is necessary. The data of this study is aimed at achieving the mentioned goal.
-
•
Due to, no study has been done on this topic in the region so far. The data of this study can help to better understand the rate of hazardous Ultraviolet ray in the area and provide further studies.
-
•
According to The data of this study, the average of UV ray in the Mashhad city was safe and below the global standard (10 W/m2 for UV ray)
1. Data
1.1. Relationship between longitudinal changes and the intensity of UV radiation in Mashhad
Fig. 1 show the relationship between changes in longitude and UV in Mashhad. These figures show that longitudinal changes have no effect on the intensity of UV radiation (P-value > 0.001).
Fig. 1.
Comparison of the relationship between longitude and UV.
1.2. Relationship between latitudinal changes and the intensity of UV radiation in Mashhad
Fig. 2 shows that there is a meaningful relationship between latitudinal changes and UV radiation. In other words, as the latitude increases, the intensity of UV radiation decreases (P-value < 0.001).
Fig. 2.
Comparison of the relationship between latitude and UV ray.
1.3. Relationship between the height above free sea level and the intensity of UV radiation in Mashhad
Fig. 3 show the relationship between the height above sea level and the intensity of UV radiation in Mashhad. As it is shown in Fig. 3 by increasing heights above free sea level, the intensity of UV irradiation significantly increases (P-value <0.001).
Fig. 3.
The relationship between the altitude of the open sea with the intensity of UV ray of the Gonabad city.
1.4. The effect of human-made artifacts on the intensity of UV radiation
Table 1 shows the effect of human on the intensity of UV radiation in Mashhad. Table 1 shows that in the village, the average UV was higher than other human-made artifacts, and the lowest level of UV radiation was related to urban artifacts. Table 1 shows that there is a significant relationship between human-made artifacts and UV radiation (P-value < 0.001).
Table 1.
Effect of manmade effects on ultraviolet radiation intensity in Mashhad.
| Radiation type | Average of UV (W m-2) | |||
|---|---|---|---|---|
| Location | City | Village | Avenue | Other |
| Manmade effects | 0.39 | 0.63 | 0.56 | 0.41 |
1.5. The effect of weather conditions on the intensity of UV radiation in Mashhad
Table 2 shows the effect of climatic conditions on the intensity of UV radiation in Mashhad. Table 2 shows that there is a significant correlation between weather conditions and UV (P-value < 0.001) and the cloudy, semi-cloudy and sunny conditions have the most effect on the intensity of UV radiation, respectively. Also in Table 3, Table 4 meteorological parameters and amount of particulate matter (PM 2.5) in Mashhad (2016–2017) are reported.
Table 2.
Effect of climatic conditions on the intensity of ultraviolet radiation in Mashhad.
| Radiation type | Average of UV (W m-2) | ||
|---|---|---|---|
| Conditions | Cloudy | partly cloudy | Sunny |
| Climatic effects | 0.45 | 0.66 | 0.46 |
Table 3.
Meteorological parameters, including the number of rainy days and sunny days in Mashhad.
| Parameter | Data |
|---|---|
| Sunny hours | 2857 |
| Rainy days | 21 |
| Relative humidity (%) | 53 |
| Minimum temperature (°C) | -21 |
| Minimum temperature (°C) | 43.8 |
| Average annual temperature (°C) | 14.5 |
| Annual average precipitation (mm/year) | 233.8 |
| Average annual evaporation (mm/year) | 1824 |
| The highest wind speed (m/s) | 25 |
Table 4.
The amount of particulate matter (PM 2.5) in Mashhad.
| Month | Concentration (µg/L) |
|---|---|
| January | 32.3 |
| February | 41.5 |
| March | 36.2 |
| April | 27.6 |
| May | 19.4 |
| June | 14.2 |
| July | 33.5 |
| August | 40.8 |
| September | 60.3 |
| October | 31.5 |
| November | 48.9 |
| December | 33.7 |
2. Experimental design, materials and methods
2.1. Geographical location of studied are
Mashhad city with population over three billion person and an area of about 351 km2 is located in 59°,36 E longitude and 36°,18 N latitude (Fig. 4). The neighboring cities are Torbat-e Heydarieh and Ghoochan in the south and north, Sabzevar and Sarakhs in the west. The average height of the city from the open sea level is 1050 m. Its center of Khorasan Razavi province and according to the last divisions of the country.
Fig. 4.
Geographic location of Gonabad city in Iran.
2.2. Method and material
This cross-sectional study was carried out in July of 2017 to determine how the variations of UV radiation were associated with changes in latitude, longitude and, height above the sea level and artificial or human-made and natural artifacts in Mashhad, Khorasan Razavi province in Iran. To this end, the data were collected 2000 sampling stations in different parts of the city (urban, rural, road, etc.). The sampling points were approximately 5000 m far from each other [1]. UV radiation was measured using Hagner radiometer, model UV-A in watt/m2 in milliseconds [2]. In this study, all conditions for the selection of sampling points were in accordance with the conditions set out in the valid references [1], [2], [3], [4], [5]. Data were analyzed by SPSS16 software using t-test and ANOVA.
Acknowledgements
We would like to thank and appreciate Mashhad University of Medical Sciences for scientific (94329) supporting and all colleagues who have collaborated on writing this paper.
Footnotes
Transparency data associated with this article can be found in the online version at doi:10.1016/j.dib.2018.05.116.
Transparency document. Supplementary material
Supplementary material
References
- 1.Hokmabadi R.A., Shoja E. Measurement of cosmic ultraviolet ray intensity (type A) in Bojnurd. J North Khorasan Univ. Med Sci. 2013;5:733–739. [Google Scholar]
- 2.Samadi M.T., Golzar Khojasteh B., Rostampour N., Mirazizi L.Shokery. Evaluation of the natural gamma radiation level in residential zones and determination of annual effective exposure dose in the residents of Hamadan province, Iran, 2012. J Kurd. Univ. Med Sci. 2014;19:30–44. [Google Scholar]
- 3.Pirsaheb M., Najafi F., Haghparast A., Hemati L., Sharafi K., Kurd N. The influence of internal wall and floor covering materials and ventilation type on indoor radon and thoron levels in hospitals of Kermanshah, Iran. Iran. Red. Crescent Med. J. 2016;18:e25292. doi: 10.5812/ircmj.25292. [DOI] [PMC free article] [PubMed] [Google Scholar]
- 4.Diffey B.L. Sources and measurement of ultraviolet radiation. Methods. 2002;28:4–13. doi: 10.1016/s1046-2023(02)00204-9. [DOI] [PubMed] [Google Scholar]
- 5.Pirsaheb M., Sharafi K., Hemati L., Fazlzadehdavil M. Radon measurement in drinking water and assessment of average annual effective dose in the west region of Iran. Fresenius Environ. Bull. 2015;24:3515–3519. [Google Scholar]
Associated Data
This section collects any data citations, data availability statements, or supplementary materials included in this article.
Supplementary Materials
Supplementary material




