Precipitation characteristics over the steep slope of the Himalayas in rainy season observed by TRMM PR and VIRS

  • Yunfei Fu
  • Xiao Pan
  • Tao Xian
  • Guosheng Liu
  • Lei Zhong
  • Qi Liu
  • Rui Li
  • Yu Wang
  • Ming Ma
Article

Abstract

Characteristics of the precipitation in rainy season over the steep Himalayas and adjacent regions, including four selected sectors of the flat Gangetic Plains (FGP), foothills of the Himalayas (FHH), the steep slope of the southern Himalayas (SSSH), and the Himalayan–Tibetan Plateau tableland (HTPT), are investigated using collocated satellite datasets from the TRMM PR and VIRS at pixel level during May–August of 1998–2012. Results indicate that the rain frequency increases significantly from the FGP via FHH to the lower elevations of the SSSH (~ 2.5 km), then decreases as the elevation further increases up to the HTPT, and reaches the minimum over the HTPT. Along with such spatial variation of the rain frequency, mean rain rates (RRs) are the heaviest over the FGP (4 mm h−1) and the FHH (5.5 mm h−1), medium over the SSSH (2–4 mm h−1), and the weakest over the HTPT (less than 2 mm h−1). More than 60% of precipitation over the FGP, FHH, and HTPT is produced by ice-phase topped clouds, while more than 70% over the SSSH is from mixed-phase topped clouds.

Analysis suggests that the highest rain frequency over the SSSH in rainy season may be caused by a strong upward motion over the SSSH as warm moist air monsoon flow interacting with the terrain of the Himalayas, while the heaviest RR over the FHH may result from low-level convergence where the air flow is blocked by the SSSH. The elevation and relief effects have linear relationships with precipitation over the south sub-region of the SSSH, which indicates that both effects play important roles on precipitation over complex plateau topography.

Keywords

Precipitation Steep Himalayas Elevation Relief TRMM merged data 

References

  1. Alcala CM, Dessler AE (2002) Observations of deep convection in the tropics using the tropical rainfall measuring mission (TRMM) precipitation radar. J Geophys Res Atmos 107:4792. https://doi.org/10.1029/2002JD002457 CrossRefGoogle Scholar
  2. Amante C, Eakins BW (2009) ETOPO1 1 arc-minute global relief model: procedures, data sources and analysis. US Department of Commerce, National Oceanic and Atmospheric Administration, National Environmental Satellite, Data, and Information Service, National Geophysical Data Center, Marine Geology and Geophysics Division, Colorado, p 19Google Scholar
  3. Anders AM, Roe GH, Hallet B, Montgomery DR, Finnegan NJ, Putkonen J (2006) Spatial patterns of precipitation and topography in the Himalaya. Geol Soc Am Spec Pap 398:39–53. https://doi.org/10.1130/2006.2398(03) Google Scholar
  4. Arkin PA, Xie PP (1994) The global precipitation climatology project: first algorithm intercomparison project. BAMS 75(3):401–419CrossRefGoogle Scholar
  5. Barros AP, Lang TJ (2003) Monitoring the monsoon in the Himalayas: observations in central Nepal, June 2001. Mon Weather Rev 131(7):1408–1427CrossRefGoogle Scholar
  6. Barros AP, Joshi M, Putkonen J, Burbank DW (2000) A study of the 1999 monsoon rainfall in a mountainous region in central Nepal using TRMM products and rain gauge observations. Geophys Res Lett 27(22):3683–3686. https://doi.org/10.1029/2000gl011827 CrossRefGoogle Scholar
  7. Barros AP, Kim G, Williams E, Nesbitt SW (2004) Probing orographic controls in the Himalayas during the monsoon using satellite imagery. Nat Hazards Earth Syst Sci 4(1):29–51CrossRefGoogle Scholar
  8. Bhatt BC, Nakamura K (2005) Characteristics of monsoon rainfall around the Himalayas revealed by TRMM precipitation radar. Mon Weather Rev 133(1):149–165CrossRefGoogle Scholar
  9. Bhatt BC, Nakamura K (2006) A climatological-dynamical analysis associated with precipitation around the southern part of the Himalayas. J Geophys Res Atmos 111:D02115CrossRefGoogle Scholar
  10. Bookhagen B, Burbank DW (2010) Toward a complete Himalayan hydrological budget: spatiotemporal distribution of snowmelt and rainfall and their impact on river discharge. J Geophys Res Earth Surf. https://doi.org/10.1029/2009jf001426 Google Scholar
  11. Boos WR, Kuang Z (2010) Dominant control of the South Asian monsoon by orographic insulation versus plateau heating. Nature 463(7278):218–222CrossRefGoogle Scholar
  12. Braga R. Vila DA (2014) Investigating the ice water path in convective cloud life cycles to improve passive microwave rainfall retrievals. J Hydrometeorol 15(4):1486–1497CrossRefGoogle Scholar
  13. Chen G, Sha W, Iwasaki T, Ueno K (2012) Diurnal variation of rainfall in the Yangtze River Valley during the spring-summer transition from TRMM measurements. J Geophys Res Atmos. https://doi.org/10.1016/j.atmosres.2015.09.017 Google Scholar
  14. Chen F, Fu Y, Liu P, Yang Y (2016) Seasonal variability of storm top altitudes in the tropics and subtropics observed by TRMM PR. Atmos Res 169:113–126CrossRefGoogle Scholar
  15. Chow KC, Chan JCL (2009) Diurnal variations of circulation and precipitation in the vicinity of the Tibetan Plateau in early summer. Clim Dyn 32(1):55–73CrossRefGoogle Scholar
  16. Duan AM, Wu GX (2005) Role of the Tibetan Plateau thermal forcing in the summer climate patterns over subtropical Asia. Clim Dyn 24(7–8):793–807CrossRefGoogle Scholar
  17. Feng S, Fu Y, Xiao Q (2011) Is the tropopause higher over the Tibetan Plateau? Observational evidence from constellation observing system for meteorology, ionosphere, and climate (COSMIC) data. J Geophys Res Atmos. https://doi.org/10.1029/2011jd016140 Google Scholar
  18. Flohn H (1968) Contributions to a meteorology of the Tibetan highlands. atmospheric science paper; no. 130. Colorado State University, Fort Collins, p. 120Google Scholar
  19. Fu YF, Liu G (2003) Precipitation characteristics in mid-latitude East Asia as observed by TRMM PR and TMI. J METEOROL SOC JPN Ser II 81(6):1353–1369CrossRefGoogle Scholar
  20. Fu YF, Liu G (2007) Possible misidentification of rain type by TRMM PR over Tibetan Plateau. J Appl Meteorol Clim 46(5):667–672CrossRefGoogle Scholar
  21. Fu YF, Qin F (2014) Summer daytime precipitation in ice, mixed and water phase as viewed by PR and VIRS in tropics and subtropics. Remote sensing of the atmosphere, clouds, and Precipitation V. In: Eastwood IM, Song Y, Peng Z (eds) Proc. of SPIE, vol. 9259, 925906 © 2014 SPIE CCC code: 0277-786X/14/$18. https://doi.org/10.1117/12.2069128 (Proc. of SPIE Vol. 9259 925906-1 ~ 11)
  22. Fu YF, Liu G, Wu G, Yu R, Xu Y, Wang Y, Li R, Liu Q (2006) Tower mast of precipitation over the central Tibetan Plateau summer. Geophys Res Lett. https://doi.org/10.1029/2005gl024713 Google Scholar
  23. Fu YF, Zhang AM, Liu Y, Zheng YY, Hu YF, Feng S, Cao AQ (2008) Characteristics of seasonal scale convective and stratiform precipitation in Asia based on measurements by TRMM Precipitation Radar. Acta Meteorol Sin 66(5):730–746 (Chinese)Google Scholar
  24. Fu YF, Liu P, Liu Q, Ma M, Sun L, Wang Y (2011) Climatological characteristics of VIRS channels for precipitating cloud in summer over the tropics and subtropics. J Atmos Environ Opt 6(2):129–140 (Chinese) Google Scholar
  25. Fu YF, Cao AQ, Li TY, Feng S, Zheng YY, Liu Y, Zhang AM (2012) Climate characteristics of the storm top altitude for the convective and stratiform precipitation in summer Asia based on measurements of the TRMM precipitation on radar. Acta Meteorol Sin 70(3):436–451 (Chinese) Google Scholar
  26. Fujinami H, Nomura S, Yasunari T (2005) Characteristics of diurnal variations in convection and precipitation over the southern Tibetan Plateau during summer. SOLA 1:49–52CrossRefGoogle Scholar
  27. Geerts B, Dejene T (2005) Regional and diurnal variability of the vertical structure of precipitation systems in Africa based on spaceborne radar data. J Clim 18:893–916CrossRefGoogle Scholar
  28. Hirose M, Nakamura K (2002) Spatial and seasonal variation of rain profiles over asia observed by spaceborne precipitation radar. J Clim 15:3443–3458CrossRefGoogle Scholar
  29. Hirose M, Nakamura K (2004) Spatiotemporal variation of the vertical gradient of rainfall rate observed by the TRMM precipitation radar. J Clim 17:3378–3397CrossRefGoogle Scholar
  30. Hirose M, Nakamura K (2005). Spatial and diurnal variation of precipitation systems over Asia observed by the TRMM precipitation radar. J Geophys Res Atmos. https://doi.org/10.1029/2004JD004815 Google Scholar
  31. Houze RA (2014) Cloud dynamics. Academic press, WalthamGoogle Scholar
  32. Houze RA, Wilton DC, Smull BF (2007) Monsoon convection in the Himalayan region as seen by the TRMM precipitation radar. Q J Roy Meteor Soc 33(627):1389–1411Google Scholar
  33. Houze AR, Rasmussen KL, Medina S, Brodzik SR, Romatschke U (2011) Anomalous atmospheric events leading to the summer 2010 floods in Pakistan. Bull Am Meteorol Soc 92(3):291–298CrossRefGoogle Scholar
  34. Hsu HH, Liu X (2003) Relationship between the Tibetan Plateau heating and east Asian summer monsoon rainfall. Geophys Res Lett 30(20):2066. https://doi.org/10.1029/2003GL017909 CrossRefGoogle Scholar
  35. Jiang J, Xiang X (1996) Spatial and temporal distributions of severe mesoscale convective systems on Tibetan Plateau in summer (in Chinese). J Appl Meteorol Sci 7:474–478Google Scholar
  36. Kelley OA, Stout J, Summers M, Zipser EJ (2010) Do the tallest convective cells over the tropical ocean have slow updrafts. Mon Weather Rev 138(5):1651–1672CrossRefGoogle Scholar
  37. Kikuchi K, Wang B (2008) Diurnal precipitation regimes in the global tropics. J Clim 21(11):2680–2696CrossRefGoogle Scholar
  38. King MD, Kaufman YJ, Menzel WP, Tanre D (1992) Remote sensing of cloud, aerosol, and water vapor properties from the moderate resolution imaging spectrometers (MODIS). IEEE Trans Geos Remote Sens 30:2–27CrossRefGoogle Scholar
  39. Liu GS, Fu YF (2001) The characteristics of tropical precipitation profiles as inferred from satellite radar measurements. J METEOROL SOC JPN Ser. II 79(1):131–143CrossRefGoogle Scholar
  40. Liu Q, Fu Y (2007) An examination of summer precipitation over Asia based on TRMM/TMI. Sci China Ser D Earth Sci 50(3):430–441CrossRefGoogle Scholar
  41. Liu C, Zipser EJ (2005) Global distribution of convection penetrating the tropical tropopause. J Geophys Res 110:D23104. https://doi.org/10.1029/2005JD006063 CrossRefGoogle Scholar
  42. Liu C, Zipser E, Nesbitt SW (2007) Global distribution of tropical deep convection: different perspectives using infrared and radar as the primary data source. J Clima 20(3):489–503CrossRefGoogle Scholar
  43. Liu X, Bai A, Liu C (2009) Diurnal variations of summertime precipitation over the Tibetan Plateau in relation to orographically-induced regional circulations. Environ Res Lett 4(4):045203CrossRefGoogle Scholar
  44. Liu L, Zheng J, Ruan Z, Cui Z, Hu Z, Wu S, Dai G, Wu Y (2015) Comprehensive radar observations of clouds and precipitation over the Tibetan Plateau and preliminary analysis of cloud properties. J Meteorol Res 29:546–561CrossRefGoogle Scholar
  45. Nakajima T, King MD (1990) Determination of the optical thickness and effective particle radius of clouds from reflected solar radiation measurements. Part I: theory. J Atmos Sci 47:1878–1893CrossRefGoogle Scholar
  46. Pan X, Fu YF (2015) Analysis on climatological characteristics of deep and shallow precipitation cloud in summer over the Tibetan Plateau. Plateau Meteorol 34(5):1182–1189 (Chinese) Google Scholar
  47. Park M, Randel WJ, Gettelman A, Massie ST, Jiang JH (2007) Transport above the Asian summer monsoon anticyclone inferred from aura microwave limb sounder tracers. J Geophys Res 112:D16309. https://doi.org/10.1029/2006JD008294 CrossRefGoogle Scholar
  48. Platnick S, Twomey S (1994) Determining the susceptibility of cloud albedo to changes in droplet concentration with the advanced very high resolution radiometer. J Appl Meteorol 33:334–347CrossRefGoogle Scholar
  49. Qian Z, Zhang S, Shan F (1984) Analysis on convective activities over the Tibet Plateau in summer of 1979 (in Chinese), in the collectives of the Qinghai-Xizang Plateau meteorological experiment in 1979, vol 1. Sci. Press, Beijing, pp 243–257Google Scholar
  50. Qie XS, Wu X, Yuan T, Bian J, Lu D (2014) Comprehensive pattern of deep convective systems over the Tibetan Plateau–South asian monsoon region based on TRMM Data. J Clim 27(17):6612–6626CrossRefGoogle Scholar
  51. Romatschke U, Houze RA (2011) Characteristics of precipitating convective systems in the South Asian monsoon. J Hydrometeoro 12(1):3–26CrossRefGoogle Scholar
  52. Romatschke U, Medina S, Houze RA (2010) Regional, seasonal, and diurnal variations of extreme convection in the South Asian region. J Clim 23(2):419–439CrossRefGoogle Scholar
  53. Schumacher C, Houze RA (2003) Stratiform rain in the tropics as seen by the TRMM precipitation radar. J Clim 16(11):1739–1756CrossRefGoogle Scholar
  54. Shi Y, Tang M, Ma Y (1999) Linkage between the second uplifting of the Qinghai-Xizang (Tibetan) Plateau and the initiation of the Asian monsoon system. Sci China Ser D Earth Sci 42(3):303–312CrossRefGoogle Scholar
  55. Shimizu S, Ueno K, Fujii H, Yamada H, Shirooka R, Liu L (2001) Mesoscale characteristics and structures of stratiform precipitation on the Tibetan Plateau. J Meteorol Soc Jpn 79:435–461CrossRefGoogle Scholar
  56. Shrestha D, Singh P, Nakamura K (2012) Spatiotemporal variation of rainfall over the central Himalayan region revealed by TRMM Precipitation Radar. J Geophys Res 117:D22106. https://doi.org/10.1029/2012JD018140 CrossRefGoogle Scholar
  57. Tao SY, Ding YH (1981) Observational evidence of the influence of the Qinghai-Xizang (Tibet) Plateau on the occurrence of heavy rain and severe convective storms in China. Bull Am Meteorol Soc 62(1):23–30CrossRefGoogle Scholar
  58. Uyeda H, Yamada H, Horikomi J, Shirooka R, Shimizu S, Liu L, Ueno K, Fujii H, Koike T (2001) Characteristics of convective clouds observed by a Doppler radar at Naqu on Tibetan Plateau during the GAME-Tibet IOP. J Meteorol Soc Jpn 79:463–474CrossRefGoogle Scholar
  59. Wang JXL, Gaffen D (2001) Late-twentieth-century climatology and trends of surface humidity and temperature in China. J Clim 14(13):2833–2845CrossRefGoogle Scholar
  60. Wang B, LinHo (2002) Rainy Season of the Asian–Pacific summer monsoon. J Clim 15(4):386–398CrossRefGoogle Scholar
  61. Wang B, Bao Q, Hoskins B, Wu G, Liu Y (2008) Tibetan Plateau warming and precipitation changes in East Asia. Geophys Res Lett. https://doi.org/10.1029/2008gl034330 Google Scholar
  62. Wang Z, Duan A, Wu G, Yang S (2015) Mechanism for occurrence of precipitation over the southern slope of the Tibetan Plateau without local surface heating. Int J Climatol. https://doi.org/10.1002/joc.4609 Google Scholar
  63. Wu G, Zhang Y (1998) Tibetan Plateau forcing and the timing of the monsoon onset over South Asia and the South China Sea. Mon Weather Rev 126(4):913–927CrossRefGoogle Scholar
  64. Wu G, Li W, Guo H, Liu H (1997) Sensible heating-driving air pump of the Tibetan Plateau and the Asian summer monsoon (in Chinese). In: Duzheng Y (ed) Memorial volume of Professor Zhao Jiuzheng. Sci. Press, Beijing, pp 116–126Google Scholar
  65. Wu GX, Liu Y, Wang T, Wan R, Liu X, Li W, Wang Z, Zhang Q, Duan A, Liang X (2007) The influence of mechanical and thermal forcing by the Tibetan Plateau on Asian climate. J Hydrometeor 8(4):770–789CrossRefGoogle Scholar
  66. Wu GX, Liu Y, He B, Bao Q, Duan A, Jin FF (2012) Thermal controls on the Asian summer monsoon. Sci Rep 2. https://doi.org/10.1038/srep00404 Google Scholar
  67. Xian T, Fu YF (2015) Characteristics of tropopause-penetrating convection determined by TRMM and COSMIC GPS radio occultation measurements. J Geophys Res Atmos 120(14):7006–7024CrossRefGoogle Scholar
  68. Xie SP, Xu HM, Saji NH, Wang YQ, Liu WT (2006) Role of narrow mountains in large-scale organization of Asian monsoon convection. J Clim 19(14):3420–3429CrossRefGoogle Scholar
  69. Xu W, Zipser EJ (2011) Diurnal variations of precipitation, deep convection, and lightning over and east of the eastern Tibetan Plateau. J Clim 24(2):448–465CrossRefGoogle Scholar
  70. Xu XD, Zhou MY, Chen JY et al (2001) A comprehensive physical pattern of land-air dynamic and thermal structure on the Qinghai-Xizang Plateau. Sci in China (Ser D) 31(5):428–440 (Chinese) Google Scholar
  71. Xu XD, Tao SY, Wang JZ, Chen LS, Zhou L, Wang XR (2002) The relationship between water vapor transport features of Tibetan Plateau-monsoon “large triangle” affecting region and drought-flood abnormality of China. Acta meteorol sin 60(3):257–266 (Chinese) Google Scholar
  72. Xu XD, Wang YJ, Zhao TL, Yao WQ (2014a) Relationship between turbulent energy in the near-surface layer and atmospheric boundary layer thermodynamic structure over the southeastern side of Tibetan Plateau. Meteorol Mon 40(10):1165–1173 (Chinese) Google Scholar
  73. Xu XD, Zhao TL, Lu CG, Shi XH (2014b) Characteristics of the water cycle in the atmosphere over the Tibetan Plateau. Acta Meteorol Sin 72(6):1079–1095 (Chinese) Google Scholar
  74. Yang YJ, Lu DR, Fu YF, Chen FJ, Wang Y (2015) Spectral characteristics of tropical anvils obtained by combining TRMM precipitation radar with visible and infrared scanner data. Pure Appl Geophys 172(6):1717–1733CrossRefGoogle Scholar
  75. Zipser EJ, Cecil DJ, Liu C, Nesbitt SW, Yorty DP (2006) Where are the most intense thunderstorms on earth? Bull Am Meteorol Soc 87(8):1057–1071CrossRefGoogle Scholar

Copyright information

© Springer-Verlag GmbH Germany 2017

Authors and Affiliations

  • Yunfei Fu
    • 1
  • Xiao Pan
    • 2
  • Tao Xian
    • 1
  • Guosheng Liu
    • 3
  • Lei Zhong
    • 1
  • Qi Liu
    • 1
  • Rui Li
    • 1
  • Yu Wang
    • 1
  • Ming Ma
    • 1
  1. 1.School of Earth and Space SciencesUniversity of Science and Technology of ChinaHefeiChina
  2. 2.Institute of Atmospheric EnvironmentCMAShenyangChina
  3. 3.Department of Earth, Ocean and Atmospheric ScienceFlorida State UniversityTallahasseeUSA

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