Advances and Perspectives in Precipitation Research for Himalayan Mountains

  • OUYANG Lin ,
  • YANG Kun ,
  • QIN Jun ,
  • WANG Yan ,
  • LU Hui
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  • Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing 100101, China;Chinese Academy of Sciences Center for Excellence in Tibetan Plateau Earth Sciences, Beijing 100101, China;University of Chinese Academy of Sciences, Beijing 100049, China;Center for Earth System Science, Tsinghua University, Beijing 100084, China

Received date: 2016-07-05

  Online published: 2017-10-28

Abstract

Exploring the spatiotemporal variability of precipitation is very important to the understanding of climate, hydrology and glacier processes in Himalaya.With the emergence of the "Third Pole Environment (TPE)" international program that is initiated by Chinese scientists, it is urgent to understand the processes and drivers of precipitation around the region.This study reviews the research progresses of precipitation in Himalayan region, based on which we put forward frontier issues of hydro-meteorological studies for this region.Previous progresses are summarized as follows:(1) Precipitation in Himalaya has distinct diurnal variation, with a nocturnal peak at night in low-elevation zone, which is related to Plateau-scale wind convergence/divergence and mountain-valley scale asymmetric diurnal variation of wind field during South Asian monsoon.(2) Precipitation in summer usually dominates the annual precipitation amount, but in northwest high elevation regions spring and winter precipitation may account for 50% of annual precipitation.(3) In south slope of Himalaya, precipitation amount increases with the increase of elevation up to 2500 m (above sea level), and then decreases toward higher elevations.(4) Regional climate modeling shows reasonable applicability in Less Himalaya, but there is, lack of valid precipitation assessments for ultra-high-elevation regions.So we propose research priorities in future to enhance observing network for high-elevation regions, evaluate satellite-based global precipitation measurements, analyze the difference of climate between south and north slopes, and to improve the skill of regional climate models in the complex mountain region.

Cite this article

OUYANG Lin , YANG Kun , QIN Jun , WANG Yan , LU Hui . Advances and Perspectives in Precipitation Research for Himalayan Mountains[J]. Plateau Meteorology, 2017 , 36(5) : 1165 -1175 . DOI: 10.7522/j.issn.1000-0534.2016.00111

References

[1]Ageta Y, Ohata T, Tanaka Y, et al. 1980. Mass balance of glacier AX010 in Shorong Himal, east Nepal during the summer monsoon season[J]. Journal of the Japanese Society of Snow and Ice, 41(Special), 34-41.
[2]Aizen V B, Aizen E M, Melack J M, et al. 1997. Climatic and hydrologic changes in the Tien Shan, central Asia[J]. J Climate, 10(6):1393-1404.
[3]Barros A P, Joshi M, Putkonen J, et al. 2000. A study of the 1999 monsoon rainfall in a mountainous region in central Nepal using TRMM products and rain gauge observations[J]. Geophys Res Lett, 27(22):3683-3686.
[4]Bhatt B C, Nakamura K. 2005. Characteristics of monsoon rainfall around the Himalayas revealed by TRMM precipitationradar[J]. Mon Wea Rev, 133(1):149-165.
[5]Bhatt B C, Sobolowski S, King M P. 2014. Assessment of downscaled current and future projections of diurnal rainfall patterns for the Himalaya[J]. J Geophys Res, 119(22):12533-12545.
[6]Bhutiyani M R, Kale V S, Pawar N J. 2010. Climate change and the precipitation variations in the northwestern Himalaya:1866-2006[J]. Int J Climatol, 30(4):535-548.
[7]Bollasina M, Bertolani L, Tartari G. 2002. Meteorological observations at high altitude in the Khumbu Valley, Nepal Himalayas, 1994-1999[J]. Bulletin of Glaciological Research, 19:1-11.
[8]Bookhagen B, Burbank D W. 2006. Topography, relief, and TRMM-derived rainfall variations along the Himalaya[J]. Geophys Res Lett, 33(8):153-172.
[9]Bookhagen B, Burbank D W. 2010. Toward a complete Himalayan hydrological budget:Spatiotemporal distribution of snowmelt and rainfall and their impact on river discharge[J]. J Geophys Res:Earth Surface, 115(F3):F03019. DOI:10. 1029/2009JF001426.
[10]Cannon F, Carvalho L M V, Jones C, et al. 2015. Winter westerly disturbance dynamics and precipitation in the western Himalaya and Karakoram:a wave-tracking approach[J]. Theor Appl Climatol, 125(1/2):27-44.
[11]Craddock W H, Burbank D W, Bookhagen B, et al. 2007. Bedrock channel geometry along an orographic rainfall gradient in the upper Marsyandi River valley in central Nepal[J]. J Geophys Res:Earth Surface, 112(F3):F03007. DOI:10. 1029/2006JF000589.
[12]Das S. 2005. Mountain weather forecasting using MM5 modellingsystem[J]. Current Science, 88(6):899-905.
[13]Gao Y, Xu J, Chen D. 2015. Evaluation of WRF mesoscale climate simulations over the tibetan plateau during 1979-2011[J]. J Climate, 28(7):2823-2841.
[14]Higuchi K, Ageta Y, Yasunari T, et al. 1982. Characteristics of precipitation during the monsoon season in high-mountain areas of the Nepal Himalaya[J]. Hydrological Aspects of Alpine and High-Mountain Areas, 138:21-30.
[15]Higuchi K. 1977. Effect of nocturnal precipitation on the mass balance of theRikha Samba Glacier, Hidden Valley, Nepal[J]. Journal of the Japanese Society of Snow and Ice, 39(Special):43-49.
[16]Houze R A. 2012. Orographic effects on precipitating clouds[J]. Rev Geophys, 50(1). DOI:10. 1029/2011RG000365.
[17]Johansson B, Chen D. 2003. The influence of wind and topography on precipitation distribution in Sweden:Statistical analysis andmodelling[J]. Int J Climatol, 23(12):1523-1535.
[18]Kang E, Cheng G, Lan Y, et al. 1999. A model for simulating the response of runoff from the mountainous watersheds of inland river basins in the arid area of northwest China to climatic changes[J]. Sci China:Earth Sci, 42(1):52-63.
[19]Kummerow C, Barnes W, Kozu T, et al. 1998. The tropical rainfall measuring mission (TRMM) sensor package[J]. J Atmos Ocean Technol, 15(3):809-817.
[20]Lei Y, Yang K, Wang B, et al. 2014. Response of inland lake dynamics over the Tibetan Plateau to climatechange[J]. Climatic Change, 125(2):281-290.
[21]Liu X, Bai A, Liu C. 2009. Diurnal variations of summertime precipitation over the Tibetan Plateau in relation toorographically-induced regional circulations[J]. Environ Res Lett, 4(4):045203.
[22]Ma J, Wang H, Fan K. 2015. Dynamic downscaling of summer precipitation prediction over China in 1998 using WRF andCCSM4[J]. Adv Atmos Sci, 32(5):577-584.
[23]Mani A. 1981. The climate of theHimalaya[M]. The Himalaya:Aspects of Change. Oxford University Press, Delhi, 115.
[24]Maussion F, Scherer D, M lg T, et al. 2014. precipitation seasonality and variability over the Tibetan Plateau as resolved by the High Asia Reanalysis[J]. J Climate, 27(5):1910-1927.
[25]Ménégoz M, Gallée H, Jacobi H W. 2013. Precipitation and snow cover in the Himalaya:from reanalysis to regional climate simulations[J]. Hydrology and Earth System Sciences, 17(10):3921-3936.
[26]Norris J, Carvalho L M V, Jones C, et al. 2015a. High resolution WRF simulation of the spatiotemporal variability of precipitation over the Himalaya[C] AGU Fall Meeting Abstracts.
[27]Norris J, Carvalho L M V, Jones C, et al. 2015b. WRF simulations of two extreme snowfall events associated with contrasting extratropical cyclones over the western and central Himalaya[J]. J Geophys Res, 120(8):3114-3138.
[28]Ohata T, Higuchi K, Ikegami K. 1981. Mountain-valley wind system in the Khumbu Himal, East Nepal[J]. J Meteor Soc Japan, 59(5):753-762.
[29]Palazzi E, von Hardenberg J, Terzago S, et al. 2015. Precipitation in the Karakoram-Himalaya:a CMIP5 view[J]. Climate Dyn, 45(1-2):21-45.
[30]Salerno F, Guyennon N, Thakuri S, et al. 2015. Weak precipitation, warm winters and springs impact glaciers of south slopes of Mt. Everest (central Himalaya) in the last 2 decades (1994-2013)[J]. The Cryosphere, 9(3):1229-1247.
[31]Shea J M, Wagnon P, Immerzeel W W, et al. 2015. A comparative high-altitude meteorological analysis from three catchments in the Nepalese Himalaya[J]. International Journal of Water Resources Development, 31(2):174-200.
[32]Shekhar M S, Kumar M S, Joshi P, et al. 2014. Mountain weather research and forecasting over western and central Himalaya by using mesoscale models[J]. International Journal of Earth and Atmospheric Science, 1(2):71-84.
[33]Shen M, Piao S, Cong N, et al. 2015. Precipitation impacts on vegetation spring phenology on the Tibetan Plateau[J]. Global Change Biology, 21(10):3647-3656.
[34]Shrestha A B, Wake C P, Dibb J E, et al. 2000. Precipitation fluctuations in the Nepal Himalaya and its vicinity and relationship with some large scale climatological parameters[J]. Int J Climatol, 20(3):317-327.
[35]Shrestha D, Singh P, Nakamura K. 2012. Spatiotemporal variation of rainfall over the central Himalayan region revealed by TRMM PrecipitationRadar[J]. J Geophys Res, 117(D22):D22106. DOI:10. 1029/2012JD018140.
[36]Singh D, Bhutiyani M R, Ram T. 2014. Station-based verification of qualitative and quantitative MM5 precipitation forecasts over Northwest Himalaya (NWH)[J]. Meteor Atmos Phys, 125(3/4):107-118.
[37]Sun F, Ma Y, Li M, et al. 2007. Boundary layer effects above a Himalayan valley near MountEverest[J]. Geophys Res Lett, 34(8):L08808. DOI:10. 1029/2007GL029484.
[38]Ueno K, Toyotsu K, Bertolani L, et al. 2008. Stepwise onset of monsoon weather observed in the Nepal Himalaya[J]. Mon Wea Rev, 136(7):2507-2522.
[39]Wagnon P, Vincent C, Arnaud Y, et al. 2013. Seasonal and annual mass balances of Mera and Pokalde glaciers (Nepal Himalaya) since 2007[J]. Cryosphere, 7(6):1769-1786.
[40]Wang Z, Duan A, Wu G, et al. 2016. Mechanism for occurrence of precipitation over the southern slope of the Tibetan Plateau without local surface heating[J]. Int J Climatol, 36(12):4164-4171.
[41]Wen R, Tian L D, Weng Y B, et al. 2012. The altitude effect of δ<sup>1</sup>8O in precipitation and river water in the Southern Himalayas[J]. Chinese Sci Bull, 57(14):1693-1698.
[42]Wu G, Liu Y, He B, et al. 2012. Thermal controls on the Asian summermonsoon[J]. Scientific Reports, 2(5):404.
[43]Wulf H, Bookhagen B, Scherler D. 2010. Seasonal precipitation gradients and their impact on fluvial sediment flux in the Northwest Himalaya[J]. Geomorphology, 118(1):13-21.
[44]Xiao C, Qin D, Yao T, et al. 2008. Progress on observation ofcryospheric components and climate-related studies in China[J]. Adv Atmos Sci, 25:164-180.
[45]Yang K, Wu H, Qin J, et al. 2014. Recent climate changes over the Tibetan Plateau and their impacts on energy and water cycle:Areview[J]. Global and Planetary Change, 112:79-91.
[46]Yang K, Ye B, Zhou D, et al. 2011. Response of hydrological cycle to recent climate changes in the Tibetan Plateau[J]. Climatic Change, 109(3/4):517-534.
[47]Yang M, Yao T, Gou X, et al. 2007. Comparison analysis of the summer monsoon precipitation between northern and southern slopes ofTanggula Mountains, Qinghai-Xizang (Tibetan) Plateau:a case study in summer 1998[J]. Hydrological Processes, 21(14):1841-1847.
[48]Yao T, Thompson L G, Mosbrugger V, et al. 2012. Third pole environment (TPE)[J]. Environmental Development, 3:52-64.
[49]Yao T, Thompson L, Yang W, et al. 2012. Different glacier status with atmospheric circulations in Tibetan Plateau andsurroundings[J]. Nature Climate Change, 2(9):663-667.
[50]Zhou L, Zou H, Ma S, et al. 2008. Study on impact of the South Asian summer monsoon on the down-valley wind on the northern slope of Mt. Everest[J]. Geophys Res Lett, 35(14):L14811. DOI:10. 1029/2008GL034151.
[51]Bai Aijuan, Liu Changhai, Liu Xiaodong. 2008. Diurnal variation of summer rainfall over the Tibetan Plateau and its neighboring regions revealed by TRMM multi-satellite precipitation analysis[J]. Chinese J Geophys, 51(3):704-714.<br/>白爱娟, 刘长海, 刘晓东. 2008. TRMM多卫星降水分析资料揭示的青藏高原及其周边地区夏季降水日变化[J].地球物理学报, 51(3):704-714.
[52]Fu Yunfei, Liu Qi, Zi Yong, et al. 2008. Summer precipitation and latent heating over the Tibetan Plateau based on TRMM measurements[J]. Plateau Mountain Meteor Res, 28(1):8-18.<br/>傅云飞, 刘奇, 自勇, 等. 2008.基于TRMM卫星探测的夏季青藏高原降水和潜热分析[J].高原山地气象研究, 28(1):8-18.
[53]He You, Yang Kun, Yao Tandong, et al. 2012. Numerical simulation of a heavy precipitation in Qinghai-Xizang Plateau based on WRF model[J]. Plateau Meteor, 31(5):1183-1191.<br/>何由, 阳坤, 姚檀栋, 等. 2012.基于WRF模式对青藏高原一次强降水的模拟[J].高原气象, 31(5):1183-1191.
[54]Li Fei, Li Jianping, Li Yanjie, et al. 2012. Climatological characteristics of flow around and flow over the Tibetan Plateau[J]. Chinese J Atmosc Sci, 36(6):1236-1252.<br/>李斐, 李建平, 李艳杰, 等. 2012.青藏高原绕流和爬流的气候学特征[J].大气科学, 36(6):1236-1252.
[55]Lin Houbo, You Qinglong, Jiao Yang, et al. 2015. Spatial and temporal characteristics of the precipitation over the Tibetan Plateau from 1961 to 2010 based on high resolution grid-observation dataset[J]. J Natural Resour, 30(2):272-281.<br/>林厚博, 游庆龙, 焦洋, 等. 2015.基于高分辨率格点观测数据的青藏高原降水时空变化特征[J].自然资源学报, 30(2):272-281.
[56]Lin Houbo, You Qinglong, Jiao Yang. 2016. Water vapor transportation and its influences on precipitation in summer over Qinghai-Xizang Plateau and Its Surroundings[J]. Plateau Meteor, 35(2):309-317. DOI:10. 7522/j. issn. 1000-0534. 2014. 00146.<br/>林厚博, 游庆龙, 焦洋. 2016.青藏高原及附近水汽输送对其夏季降水影响的分析[J].高原气象, 35(2):309-317.
[57]Lu Chunxia, Wang Ling, Xie Gaodi, et al. 2007. Altitude effect of precipitation and spatial distribution of Qinghai-Tibetan Plateau[J]. J Mountain Sci, 25(6):655-663.<br/>鲁春霞, 王菱, 谢高地, 等. 2007.青藏高原降水的梯度效应及其空间分布模拟[J].山地学报, 25(6):655-663.
[58]Lu Hongya, Du Jun, Yuan Lei, et al. 2014. Variation characteristics of extreme precipitation events over Mt. Qomolangma region in China from 1971 to 2012[J]. Journal of Glaciology and Geocryology, 36(3):563-572.<br/>路红亚, 杜军, 袁雷, 等. 2014. 1971-2012年珠穆朗玛峰地区极端降水事件变化研究[J].冰川冻土, 36(3):563-572.
[59]Tian Hongying, Tian Wenshou, Luo Jiali, et al. 2014. Characteristics of water vapor distribution and variation in upper troposphere and lower stratosphere over Qinghai-Xizang Plateau[J]. Plateau Meteor, 33(1):1-13. DOI:10. 7522/j. issn. 1000-0534. 2013. 00074.<br/>田红瑛, 田文寿, 雒佳丽, 等. 2014.青藏高原地区上对流层-下平流层区域水汽分布和变化特征[J].高原气象, 33(1):1-13.
[60]Tian Shanru, Duan Anmin, Wang Ziqian, et al. 2015. Interaction among the surface heating, Tibetan Plateau vortex, and convective system:A case study[J]. Chinese J Atmos Sci, 39(1):125-136.<br/>田珊儒, 段安民, 王子谦, 等. 2015.地面加热与高原低涡和对流系统相互作用的一次个例研究[J].大气科学, 39(1):125-136.
[61]Xie Chengying, Li Minjiao, Zhang Xueqin, et al. 2015. Moisture transport features in summer and its rainfall effects over key region in southern margin of Qinghai-Xizang Plateau[J]. Plateau Meteor, (2):327-337. DOI:10. 7522/j. issn. 1000-0534. 2014. 00034.<br/>解承莹, 李敏姣, 张雪芹, 等. 2015.青藏高原南缘关键区夏季水汽输送特征及其与高原降水的关系[J].高原气象, (2):327-337.
[62]Zhang Jinshan, Zhong Zhong, Huang Jin. 2005. An introduction to meso-scale model MM5[J]. Marine Forecasts, 22(1):31-40.<br/>张金善, 钟中, 黄瑾. 2005.中尺度大气模式MM5简介[J].海洋预报, 22(1):31-40.
[63]Zhou Libo, Zou Han, Ma Shupo, et al. 2007. Impacts of the South Asian summer monsoon on variations of surface wind on the northern slope of Mt. Qomolangma[J]. Plateau Meteor, 26(6):1173-1186.<br/>周立波, 邹捍, 马舒坡, 等. 2007.南亚夏季风对珠穆朗玛峰北坡地面风场的影响[J].高原气象, 26(6):1173-1186.
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