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Assessment of Erythemal UV Level in Nepal Based on Solar UV Estimates from Total Ozone Mapping Spectrometer


doi: 10.1007/s00376-010-9222-0

  • Nepal lies on the southern slope of Himalaya in Asia. In a width ranging between 150 and 250 km, the altitude varies greatly from about 100 m at its southern border to a maximum of 8848 min the northern part. Like the variation in altitude, climatic condition varies quite a lot. Long-term monthly mean erythemal UV daily dose values for Nepal are evaluated using Total Ozone Mapping Spectrometer (TOMS) estimation from the time of its overpass between 1996 and 2003. The results are presented as summer and winter maps of mean UV levels in each satellite grid. The mean winter erythemal UV daily dose ranges between 2.1 and 3.6 kJ m-2 whereas summer values are found to lie between 4.6 and 9.7 kJ m-2. The altitude variation increases the UV levels by about 0.2 kJ km-1 in winter months, and 0.9 kJ km-1 in summer. A multiyear monthly average erythemal daily dose in most of the areas shows that the summer value is about three times higher than that in winter. Although year-to-year variation is not pronounced in high- and mid-elevation regions, UV levels seemed to decrease from 1997 to 2002 in the southern part of the country in the low elevation region by about 5.35%. Due to the combined effects of the altitude, low ozone concentration in the troposphere, and thin air, surface UV radiation at higher altitudes is found to be higher than in the surrounding regions.
  • [1] Sang Seo PARK, Yun Gon LEE, Jung Hyun KIM, 2015: Impact of UV-A Radiation on Erythemal UV and UV-index Estimation over Korea, ADVANCES IN ATMOSPHERIC SCIENCES, 32, 1639-1646.  doi: 10.1007/s00376-015-4231-7
    [2] Wang Pucai, Jacqueline Lenoble, 1996: Influence of Clouds on UV Irradiance at Ground Level and Backscattered Exittance, ADVANCES IN ATMOSPHERIC SCIENCES, 13, 217-228.  doi: 10.1007/BF02656864
    [3] Sang Seo PARK, Yeonjin JUNG, Yun Gon LEE, 2016: Spectral Dependence on the Correction Factor of Erythemal UV for Cloud, Aerosol, Total Ozone, and Surface Properties: A Modeling Study, ADVANCES IN ATMOSPHERIC SCIENCES, 33, 865-874.  doi: 10.1007/s00376-016-5201-4
    [4] Fei XIE, Yan XIA, Wuhu FENG, Yingli NIU, 2023: Increasing Surface UV Radiation in the Tropics and Northern Mid-Latitudes due to Ozone Depletion after 2010, ADVANCES IN ATMOSPHERIC SCIENCES, 40, 1833-1843.  doi: 10.1007/s00376-023-2354-9
    [5] HU Bo, WANG Yuesi, LIU Guangren, 2008: Influences of the Clearness Index on UV Solar Radiation for Two Locations in the Tibetan Plateau---Lhasa and Haibei, ADVANCES IN ATMOSPHERIC SCIENCES, 25, 885-896.  doi: 10.1007/s00376-008-0885-8
    [6] Bian Jianchun, Chen Hongbin, Zhao Yanliang, Lü Daren, 2002: Variation Features of Total Atmospheric Ozone in Beijing and Kunming Based on Dobson and TOMS Data, ADVANCES IN ATMOSPHERIC SCIENCES, 19, 279-286.  doi: 10.1007/s00376-002-0022-z
    [7] Dongxu YANG, Yi LIU, Zhaonan CAI, Xi CHEN, Lu YAO, Daren LU, 2018: First Global Carbon Dioxide Maps Produced from TanSat Measurements, ADVANCES IN ATMOSPHERIC SCIENCES, 35, 621-623.  doi: 10.1007/s00376-018-7312-6
    [8] You Ronggao, Hong Zhongxiang, Lu Weixiu, Zhao Deshan, Kong Qinxin, Zhu Wenqin, 1985: VARIATIONS OF ATMOSPHERIC AEROSOL CONCENTRATION AND SIZE DISTRIBUTION WITH TIME AND ALTITUDE IN THE BOUNDARY LAYER, ADVANCES IN ATMOSPHERIC SCIENCES, 2, 243-250.  doi: 10.1007/BF03179756
    [9] Sandeep D. WAGH, Baban NAGARE, Sanjay D. MORE, P. Pradeep KUMAR, 2017: Multiyear Observations of Deposition-Mode Ice Nucleating Particles at Two High-Altitude Stations in India, ADVANCES IN ATMOSPHERIC SCIENCES, 34, 1437-1446.  doi: 10.1007/s00376-017-7048-8
    [10] Xuefen ZHANG, Liangxu LI, Rongkang YANG, Ran GUO, Xia SUN, Jianping LUO, Hongbin CHEN, Daxin LIU, Kebing TANG, Wenwu PENG, Xiaodong HAN, Qiyun GUO, Xiaoxia LI, Xikun FEI, 2021: Comprehensive Marine Observing Experiment Based on High-Altitude Large Unmanned Aerial Vehicle (South China Sea Experiment 2020 of the “Petrel Project”), ADVANCES IN ATMOSPHERIC SCIENCES, 38, 531-537.  doi: 10.1007/s00376-020-0314-1
    [11] Fang Juan, Wu Rongsheng, 2001: Topographic Effect on Geostrophic Adjustment and Frontogenesis, ADVANCES IN ATMOSPHERIC SCIENCES, 18, 524-538.  doi: 10.1007/s00376-001-0042-0
    [12] CHEN Lianshou, LUO Zhexian, 2004: A Study of the Effect of Topography on the Merging of Vortices, ADVANCES IN ATMOSPHERIC SCIENCES, 21, 13-22.  doi: 10.1007/BF02915676
    [13] DUAN Yihong, WU Rongsheng, YU Hui, LIANG Xudong, Johnny C L CHAN, 2004: The Role of -effect and a Uniform Current on Tropical Cyclone Intensity, ADVANCES IN ATMOSPHERIC SCIENCES, 21, 75-86.  doi: 10.1007/BF02915681
    [14] LING Jian, LI Chongyin, ZHOU Wen, JIA Xiaolong, Chidong ZHANG, 2013: Effect of Boundary Layer Latent Heating on MJO Simulations, ADVANCES IN ATMOSPHERIC SCIENCES, 30, 101-115.  doi: 10.1007/s00376-012-2031-x
    [15] MIAO Shiguang, LI Pingyang, WANG Xiaoyun, 2009: Building Morphological Characteristics and Their Effect on the Wind in Beijing, ADVANCES IN ATMOSPHERIC SCIENCES, 26, 1115-1124.  doi: 10.1007/s00376-009-7223-7
    [16] FANG Juan, TANG Jianping, WU Rongsheng, 2009: The Effect of Surface Friction on the Development of Tropical Cyclones, ADVANCES IN ATMOSPHERIC SCIENCES, 26, 1146-1156.  doi: 10.1007/s00376-009-8020-z
    [17] Zhao Ming, 1991: The Effect of Topography on Quasi-Geostrophic Frontogenesis, ADVANCES IN ATMOSPHERIC SCIENCES, 8, 23-40.  doi: 10.1007/BF02657362
    [18] Zhang Pei, Ni Yunqi, 1991: Effect of Nonlinear Dynamic Process on Formation and Breakdown of Blocking, ADVANCES IN ATMOSPHERIC SCIENCES, 8, 41-50.  doi: 10.1007/BF02657363
    [19] BI Yun, CHEN Yuejuan, ZHOU Renjun, YI Mingjian, DENG Shumei, 2011: Simulation of the Effect of an Increase in Methane on Air Temperature, ADVANCES IN ATMOSPHERIC SCIENCES, 28, 129-138.  doi: 10.1007/s00376-010-9197-x
    [20] Zhang Pei, Ni Yunqi, 1991: The Effect of Topographic Forcing on the Formation and Maintenance of Blocking, ADVANCES IN ATMOSPHERIC SCIENCES, 8, 317-326.  doi: 10.1007/BF02919614

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Manuscript History

Manuscript received: 10 July 2011
Manuscript revised: 10 July 2011
通讯作者: 陈斌, bchen63@163.com
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    沈阳化工大学材料科学与工程学院 沈阳 110142

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Assessment of Erythemal UV Level in Nepal Based on Solar UV Estimates from Total Ozone Mapping Spectrometer

  • 1. Department of Engineering Science and Humanities, Pulchowk Campus, Institute of Engineering, Tribhuvan University, Kathmandu, Nepal,Norwegian University of Science and Technology, N~$7491$ Trondheim, Norway,Sor Trondelag University College, N7004 Trondheim, Norway

Abstract: Nepal lies on the southern slope of Himalaya in Asia. In a width ranging between 150 and 250 km, the altitude varies greatly from about 100 m at its southern border to a maximum of 8848 min the northern part. Like the variation in altitude, climatic condition varies quite a lot. Long-term monthly mean erythemal UV daily dose values for Nepal are evaluated using Total Ozone Mapping Spectrometer (TOMS) estimation from the time of its overpass between 1996 and 2003. The results are presented as summer and winter maps of mean UV levels in each satellite grid. The mean winter erythemal UV daily dose ranges between 2.1 and 3.6 kJ m-2 whereas summer values are found to lie between 4.6 and 9.7 kJ m-2. The altitude variation increases the UV levels by about 0.2 kJ km-1 in winter months, and 0.9 kJ km-1 in summer. A multiyear monthly average erythemal daily dose in most of the areas shows that the summer value is about three times higher than that in winter. Although year-to-year variation is not pronounced in high- and mid-elevation regions, UV levels seemed to decrease from 1997 to 2002 in the southern part of the country in the low elevation region by about 5.35%. Due to the combined effects of the altitude, low ozone concentration in the troposphere, and thin air, surface UV radiation at higher altitudes is found to be higher than in the surrounding regions.

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