Abstract
Solar radiation consists of a wide range of electromagnetic waves emitted as visible light (40 %), as well as invisible radiations, viz., ultraviolet (10 %) and infrared (50 %). The fraction of ultraviolet radiation of sun’s rays comprises three wavebands, viz., UV-A (315–390 nm), UV-B (280–315 nm), and UVC (100–280 nm), each with energy of impact corresponding to the respective wavelengths. Entry of these UV wavebands into the earth’s atmosphere is differentially restricted by an “ozone layer” that spans the lower region of the stratosphere. Due to such restricted penetration of UV radiation into earth’s atmosphere, UV exhibits limited presence (only 0.5 % of total solar UV) in earth’s surface. Of the UV radiation penetrating in earth’s atmosphere, UV-A comprises 90 % and UV-B comprises 5–10 %; UV-C is totally absent in earth’s atmosphere. Of these, UV-B presents the most deleterious fraction with UV-A (of lower energy) following suit. Five layers of atmosphere, each with specific composition, temperature, and function, envelop the earth. Of these, the two biologically most important layers are troposphere and stratosphere: the troposphere representing the closest overlay on earth’s surface constitutes the weather determining region, while the stratosphere, lying just above, houses the UV screening ozone layer. UV restraining ozone layer developed through evolution of oxygenic life forms on earth pioneered by appearance of Cyanobacteria about 3 billion years ago. In that age, molecular oxygen resulting from oxygenic photosynthesis of Cyanobacteria as well as other later evolved photosynthetic organisms led to the formation of ozone layer through reaction between molecular oxygen and atomic oxygen under influence of UV that, being a fraction of sunshine, is highest at the equator. Ozone thus formed accumulates as a layer in the stratosphere being thicker at the poles with gradually decreasing thickness toward the equator, UV penetration varying as a function of wavelength, through the ozone layer. The penetration of UV radiation is affected by various factors such as latitude (as a factor of ozone thickness), altitude (as a factor of air rarification), variation in sun’s zenith angle relating to solar movement, diurnal, seasonal variation, and aerosol/cloud cover variation.
The temperature requirement for life support, early in earth’s evolutionary history, was provided by IR radiation that caused warming of earth’s supercool condition. This aided in origin and perpetuation of life on earth. Ironically in recent times, the same (IR) radiation, being trapped by enhanced “greenhouse gases,” accumulating due to adverse anthropogenic activities, is contributing to destruction of life through the process of global warming. Global warming on the earth’s surface has a two-pronged destructive effect; this warming of earth simultaneously causes cooling in the stratosphere, a condition that enhances ozone destruction, thereby augmenting depletion of the ozone layer.
As a result of gradual ozone thinning, during the later part of the last century, an “ozone hole” was detected, first in the coldest Antarctic (polar) region and subsequently in the Arctic region. Appreciable ozone thinning has also been recorded at the mid-latitudes. During the later part of the past century, reports on ozone thinning/ozone hole associated with concomitant increase in UV fluence on earth’s surface raised an alarm, and reports rapidly (particularly in the post-ozone hole era) started coming up on the harmful effects of UV radiation on living organisms. Realization that a gradual thinning of the protective ozone layer is occurring due to anthropogenic effect related release of damaging gases like CFC and related compounds as well as the greenhouse effect in the atmosphere prompted the UN to take urgent regulatory measures for reducing/reversing this state of global (UV related) predicament. Several regulations have been made mandatory through regulations of Kyoto Protocol and Montreal Protocol to control ozone thinning and atmospheric degradation worldwide. Since the universal acceptance of the Montreal Protocol, in 1987 there has been growing evidence for the recovery of the stratospheric ozone layer, albeit with apprehension of continuing low level destruction of the ozone layer.
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Austin J, Butchart N, Shine KP (1992) Possibility of an Arctic ozone hole in a doubled-CO2 climate. Nature 360:221–225
Blumethaler M, Ambach W, Silbernagl R, Staehelin J (1994) Erythemal UV-B irradiance under ozone deficiencies in winter/spring 1993. Photochem Photobiol 59:657–659
Blumthaler M, Ambach W (1990) Indication of increasing solar ultraviolet-B radiation flux in alpine regions. Science 248(4952):206–208
Blumthaler M, Ambach W, Rehwald W (1992) Solar UV-A and UV-B radiation fluxes at two alpine stations at different altitudes. Theor Appl Climatol 46:39–44
Blumthaler M, Ambach W, Ellinger R (1997) Increase in solar UV radiation with altitude. J Photochem Photobiol 39:130–134
Bornman JF, Barnes PW, Robinson SA, Ballaré CL, Flint SD, Caldwell MM (2015) Solar ultraviolet radiation and ozone depletion-driven climate change: effects on terrestrial ecosystems. Photochem Photobiol Sci 14:88–107
Brune WH, Anderson JG, Toohey DW, Fahey DW et al (1991) The potential for ozone depletion in the Arctic polar stratosphere. Science 252:1260–1266
Caldwell MM, Ballare CL, Bornman JF, Flint SD, Bj€orn LO, Teramura AH, Kulandaivelu G, Tevini M (2003) Terrestrial ecosystems increased solar ultraviolet radiation and interactions with other climatic change factors. Photochem Photobiol Sci 2:29–38
Chaplin G (2004) Geographic distribution of environmental factors influencing human skin coloration. Am J Phys Anthropol 125:292–304
Crutzen PJ (1970) The influence of nitrogen oxides on the atmospheric ozone content. Q J R Meteorol Soc 96:320–325
Crutzen PJ (1992) Ultraviolet on the increase. Nature 356:104–105
Day TA, Neale PJ (2002) Effects of UV-B radiation on terrestrial and aquatic primary producers. Ann Rev Ecol Syst 33:371–396
Diffey BL (1991) Solar ultraviolet radiation effects on biological systems. Rev Phys Med Biol 36(3):299–328
Diffey BL (2002) Sources and measurement of ultraviolet radiation. Methods 28:4–13
Engelsen O (2010) The relationship between ultraviolet radiation exposure and vitamin D status. Nutrient 2:482–495
Farman JC, Gardiner BG, Shanklin JD (1985) Large losses of total ozone in Antarctica reveal seasonal ClOx/NOx interaction. Nature 315:207–210
Foster KL, Plastridge RA, Bottenheim JW, Shepson PB, Finlayson-Pitts BJ, Spicer CW (2001) The role of Br2 and BrCl in surface ozone destruction at polar sunrise. Science 291:471–474
Frederick JE, Snell HE (1990) Tropospheric influence on solar ultraviolet radiation: the role of clouds. J Clim 3:373–381
Gleason JF, Bhartia PK, Herman JR, McPeters R (1993) Record low global ozone in 1992. Science 260:523–526
Hader DP, Kumar HD, Smith RC (2003) Aquatic ecosystems: effects of solar ultraviolet radiation and interactions with other climatic change factors. Photochem Photobiol Sci 2:39–50
Herman JR (2010a) Use of an improved radiation amplification factor to estimate the effect of total ozone changes on action spectrum weighted irradiances and an instrument response function. J Geophys Res 115, D23119
Herman JR (2010b) Global increase in UV irradiance during the past 30 years (1978–2008) estimated from satellite data. J Geophys Res 115
Herman JR, Lrko D (1994) Low ozone amounts during 1992–93 from nimbus 7 and meteor 3 total ozone mapping spectrometers. J Geophys Res 98:12783–12793
http://www.uio.no/studier/emner/matnat/fys/FYS3610/h04/undervisningsmateriale/Moan7.pdf
https://www.skepticalscience.com/water-vapor-greenhouse-gas.htm
Kerr RA (1988) Stratospheric ozone is decreasing. Science 239:1489–1491
Kerr JB, McElory (1993) Evidence for large upward trends of ultraviolet –B radiation linked to ozone depletion. Science 262:1032–1034
Liew SC (2006) Electromagnetic waves. Centre for Remote Imaging, Sensing and Processing. Retrieved, pp 10–27
Lucas R, McMichael T, Smith W, Armstrong B (2006). Solar ultraviolet radiation. Global burden of disease from solar ultraviolet radiation World Health Organization, Environmental Burden of Disease Series, 13
Madronich S, de Gruijl FR (1994) Stratospheric ozone depletion between 1978 and 1992: implications for biologically active ultraviolet-B radiation and non-melanoma skin cancer incidence. Photochem Photobiol 59(5):541–546
McKenzie RL, Kotkamp M, Seckmeyer G, Erb R, Gies R, Toomey S (1993) First southern hemisphere intercomparison of measured solar UV spectra. Geophys Res Lett 20(20):2223–2226
McKenzie RL, Bjo¨rn LO, Bais A, Ilyas M (2003) Changes in biologically active ultraviolet radiation reaching the Earth’s surface. Photochem Photobiol Sci 2:5–15
McKenzie RL, Bodeker GE, Scott G, Slusser J (2006) Geographical differences in erythemally-weighted UV measured at mid-latitude USDA sites. Photochem Photobiol Sci 5(3):343–352
McKenzie RL, Aucamp PJ, Bais AF, Bj¨orn LO, Ilyas M, Madronich S (2011) Ozone depletion and climate change: impacts on UV radiation. Photochem Photobiol Sci 10:182–198
Moan J, Grigagavicius M, Dahlback A, Baturaite Z, Juzeniene A (2013) UV-radiation and health optimal time for sun exposure. In: Reichrath J (ed) Sunlight, vitamin D and skin cancer. Landes Bioscience and Springer science + business media, pp 1–6
Molina MJ, Rowland FS (1974) Stratospheric sink for chlorofluoromethanes: chlorine atom catalyzed destruction of ozone. Nature 249:810–812
Norgaard MA, Anderson CB, Pettersson G, Caldwell MM (1998) Changes in biologically active ultraviolet radiation reaching the Earth’s surface. J Photochem Photobiol B Biol 46(1):21–31
Portmann RW, Daniel JS, Ravishankara AR (2012) Stratospheric ozone depletion due to nitrous oxide: influences of other gases. Phil Trans R Soc B 367:1256–1264
Ramanathan V, Feng Y (2009) Air pollution, greenhouse gases and climate change: global and regional perspectives. Atmos Environ 43:37–50
Ravishankara AR, Solomon S, Turnipseed AA, Waren RF (1993) Science 259:194–199
Ravishankara AR, Daniel JS, Portmann RW (2009) Nitrous oxide (N2O): the dominant ozone-depleting substance emitted in the 21st century. Science 326:123–125
Rozema J, Staaij J, Bjorn LO, Caldwell M (1997) UV-B as an environmental factor in plant life: stress and regulation. Trends Ecol Evol 12:22–28
Seckmeyer GRL, McKenzie RL (1992) Increased ultraviolet radiation in New Zealand (45øS) relative to Germany (48øN). Nature 359:135–137
Shyam Choudhury S, Sen-Mandi S (2012) Natural ultra violet irradiance related variation in antioxidant and aroma compounds in tea (Camelia sinensis L. Kuntze) plants grown into different altitudes. Int J Environ Biol 2(1):1–6
Stolarski RS, Cicerone RJ (1984) Stratospheric chlorine: a possible sink for ozone. Can J Chem 52:1610–1615
Tilmes S et al (2012) Impact of very short-lived halogens on stratospheric ozone abundance and UV radiation in a geo-engineered atmosphere. Atmos Chem Phys 12:10945–10955
Venkataramanan M, Smitha (2011) Causes and effects of global warming. Indian J Sci Technol 4:226–229
Vogelmann AM, Ackerman TP, Turco RP (1992) Enhancements in biologically effective ultraviolet radiation following volcanic eruptions. Nature 359:47–49
Wang CT, Cao GM, Wang QL, Jing ZC, Ding LM, Long RJ (2009) Changes in plant biomass and species composition of alpine Kobresia meadows along altitudinal gradient on the Qinghai-Tibetan Plateau. Sci China Life Sci 51:86–94
WHO (2002) Global solar UV index: a practical guide. A joint recommendation of the World Health Organization, World Meteorological Organization, United Nations Environmental Programme, and the International Commission on Non-Ionizing Radiation Protection. World Health Organization, Geneva. ISBN 92 4 159007 6
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Sen Mandi, S. (2016). Natural Ultraviolet Radiation. In: Natural UV Radiation in Enhancing Survival Value and Quality of Plants. Springer, New Delhi. https://doi.org/10.1007/978-81-322-2767-0_1
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