In order to make up for the shortage of the measured data of ultraviolet radiation in China, this paper calculates and analyzes ultraviolet radiation under the standard atmosphere and cloudless conditions based on the SMARTS. The temporal and spatial variation characteristics of ultraviolet radiation multi-parameters are researched, such as the global ultraviolet radiation of Eg 280 nm-400 nm, UVA of 315 nm-400 nm, UVB of 280 nm-315 nm, ultraviolet index UVI, erythema effective ultraviolet radiation CIE, global ultraviolet irradiance on the vertical plane, and the quantitative influence of atmospheric turbidity, ozone content, altitude, surface albedo and other factors on each parameter. The results show that: 1) The parameters of UV radiation decrease with the increase of latitude, and the ratio of global UV radiation to the global radiation of the whole spectrum is about 5%. 2) The parameters of UV radiation are high in summer and low in winter, high in noon and low in morning and evening, and the annual variability of high latitude is higher than that of low latitude, and the parameters of UV radiation in middle and low latitude are similar in the three months before and after the Summer Solstice Day, which may have a great impact on human health. 3) UVI may be close to 11 at noon in summer when it is completely clear, and UVA and UVB may reach 70 W/m2 and 2 W/m2 at noon, respectively. The peak value of the global ultraviolet irradiance on the south vertical plane in low latitude area can reach 70 W/m2 in the Summer Solstice Day, which is equivalent to the value on the horizontal plane; 4) When the visibility increases from 2 km to 50 km, the ultraviolet irradiance will double; On the other hand, with the increase of visibility, the increase of UV irradiance is slowed down. When the total amount of ozone is doubled from 200 DU to 400 DU, the UVI decreases by more than half, and the decreasing range slowed down with the increase of total ozone. When the altitude increases from 0 to 5 km, the UV irradiance increases by about 1/4, and the increasing range remained relatively uniform with the increase of altitude. When the surface albedo doubles from 0.2 to 0.4, the UV radiation on the south vertical plane increases by 1/5, and the global UV radiation on the south vertical plane from the reflection of the ground are larger in summer, but smaller in winter. Although the above results are only the theoretical simulation results under cloudless conditions, the basic characteristics of UV radiation and influencing factors reflected in the results can still be used for reference in the fields of meteorology and medical science.
Key words
ultraviolet radiation /
multiple parameters /
influence factor /
numerical simulation /
SMARTS
{{custom_sec.title}}
{{custom_sec.title}}
{{custom_sec.content}}
References
[1] SECKMEYER G, BAIS A, BERNHARD G, et al. Instruments to measure solar ultraviolet radiation, part 1: Spectral instruments[R]. WMO/TD-No.1066, World Meteorological Organization, Geneva, Switzerland,2001, 31 pp.
[2] SECKMEYER G, BAIS A, BERNHARD G, et al. Instruments to measure solar ultraviolet radiation, part 2: Broadband instruments measuring erythemally weighted solar irradiance[R]. WMO/TD-No.1289, World Meteorological Organization, Geneva, Switzerland, 2008:2.
[3] SECKMEYER G, BAIS A, BERNHARD G, et al. Instruments to measure solar ultraviolet radiation, part 3: Multi-channel filter instruments[R]. WMO/TD-No.1537, World Meteorological Organization, Geneva, Switzerland, 2010: 251.
[4] SECKMEYER G, BAIS A, BERNHARD G, et al. Instruments to measure solar ultraviolet radiation, part 4: Array spectroradiometers[R]. WMO/TD-No.1538, World Meteorological Organization, Geneva, Switzerland, 2010: 239.
[5] BURROWS W R.Report of the WMO-WHO meeting of experts on standardization of UV indices and their dissemination to the public[R]. WMO/TD-No.921, World Meteorological Organization, Geneva, Switzerland, 1997.
[6] World Health Organization(WHO), World Meteorological Organization(WMO), United Nations Environment Programme (UNEP), The international commision on non-ionizing radiation protection (ICNIRP).Global solar UV index: A practical guide[R]. WHO, 2002: 27pp.
[7] 汤洁, 王炳忠, 姚萍.国产紫外辐射仪器性能测试(Ⅰ)——室内静态性能测试[J]. 太阳能学报, 2005: 26(2): 43-46.
TANG J, WANG B Z, YAO P.Intercomparison of China-made UV pyranometers(Ⅰ)—Performance test in laboratory[J]. Acta energiae solaris sinica, 2005, 26(2): 43-46.
[8] 汤洁, 王炳忠, 刘广仁.国产紫外总日射表性能测试(Ⅱ)——室外测试及与国外同类产品比较[J]. 太阳能学报, 2005, 26(3): 19-26.
TANG J, WANG B Z, LIU G R.Intercomparison of China-made UV pyranometers (Ⅱ)——Outdoor test and intercomparison with foreign UV pyranometers[J]. Acta energiae solaris sinica, 2005, 26(3): 19-26.
[9] GB/T 21005—2007, 紫外红斑效应参照谱、标准红斑剂量和紫外指数[S].
GB/T 21005—2007, UV erythema reference action spectrum standard erythema dose and UV index[S].
[10] GB/T 34048—2017, 紫外辐射表[S].
GB/T 34048—2017, Ultraviolet radiometer[S].
[11] GB/T 36744—2018, 紫外线指数预报方法[S].
GB/T 36744—2018, Forecasting method for ultraviolet index[S].
[12] 吴厚水.对太阳总辐射和某些植被的反射及透射辐射的分光测量[J]. 生态学报, 1987, 7(1): 18-26.
WU H S.A study of spectral radiation upon some cropland in the Zhujiang Delte, China[J]. Acta ecologica sinica, 1987, 7(1): 18-26.
[13] 刘玮, 代彩红, 田燕.紫外辐射的科学基础及应用[M]. 北京: 人民卫生出版社, 2013.
LIU W, DAI C H, TIAN Y.Scientific basis and application of ultraviolet radiation[M]. Beijing: People’s Medical Publishing House, 2013.
[14] GUEYMARD C A.Parameterized transmittance model for direct beam and circumsolar spectral irradiance[J]. Solar energy, 2001, 71(5): 325-346.
[15] 王炳忠, 申彦波.实用太阳能光谱应用模式——SMARTS模式[M]. 北京: 气象出版社, 2010.
WANG B Z, SHEN Y B.SMARTS model, a practical solar energy spectrum application model[M]. Beijing: Meteorology Press, 2010.
[16] MICHALSKY J, ANDERSON G P, BARNARD J, et al. Shortwave radiative closure studies for clear skies during the atmospheric radiation measurement2003 aerosol intensive observation period[J]. Journal of geophysical research: Atmospheres, 2006, 111(D14): D14S90.
[17] GUEYMARD C A.Prediction and validation of cloudless shortwave solar spectra incident on horizontal, tilted, or tracking surfaces[J]. Solar energy, 2008, 82(3): 260-271.
[18] 王炳忠.紫外线知识讲座——紫外辐射定义及其分类[J]. 太阳能, 2003(4): 6-9.
WANG B Z.Lecture on ultraviolet radiation-definition and classification of ultraviolet radiation[J]. Solar energy, 2003(4): 6-9.
[19] 刘扬, 赵萍, 朱旭东, 等. 我国东北地区紫外线辐射对皮肤早期损伤的流行病学研究[J]. 环境与健康杂志, 1997(5): 26-32.
LIU Y, ZHAO P, ZHU X D, et al. Epidemiological study on early dermal impairment induced by ultraviolet radiation in North East of China[J]. Journal of environment and health, 1997(5): 26-32.
[20] 王芳, 刘扬.基于人体模型模拟三亚市不同地理朝向眼部暴露紫外辐射分布的研究[J]. 环境与职业医学, 2017(3): 15-24.
WANG F, LIU Y.Simulation of ocular exposure to ultraviolet spectral irradiance in different geographic directions in Sanya based on a manikin[J]. Journal of environmental & occupational medicine, 2017(3): 15-24.