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Theoretical and Applied Climatology

, Volume 136, Issue 1–2, pp 605–626 | Cite as

Long-term study of aerosol–cloud–precipitation interaction over the eastern part of India using satellite observations during pre-monsoon season

  • Sunny Kant
  • Jagabandhu PandaEmail author
  • Shantanu Kumar Pani
  • Pao K. Wang
Original Paper

Abstract

This study attempts to analyze possible aerosol–cloud–precipitation interaction over the eastern part of India including Bhubaneswar city and the whole Odisha region primarily using a long-term satellite-based dataset from 2000 to 2016 during pre-monsoon period. Relationship between aerosol optical depth (AOD), rainfall, and cloud properties is examined by taking convectively driven rain events. The two-sample student’s t test is used to compute “p” value of datasets that are statically significant. Role of aerosols in governing cloud properties is analyzed through the variation of COD (cloud optical depth) and CER (cloud effective radius) in the AOD ranges 0.2–0.8. A relatively stronger and affirmative AOD–CER relationship is observed over Bhubaneswar city compared to Odisha region though the aerosols still play an appreciable role for the later too. The AOD–COD relationship is weak over both the regions. For Odisha, relationships between aerosol and cloud parameters are insignificant irrespective of rainfall regimes. Fostering of heavy rainfall over these regions takes place due to invigoration and microphysical effect during pre-monsoon months, depending upon meteorological conditions. Liquid water content and presence of a mixed-phase zone, both seem to be quite important in the convectively driven precipitation over Odisha region including Bhubaneswar city.

Notes

Acknowledgments

The authors acknowledge the data support from Giovanni (http://giovanni.sci.gsfc.nasa.gov/giovanni/), ERA-Interim portal (http://apps.ecmwf.int/datasets), and Wyoming Weather Web (http://weather.uwyo.edu/upperair). Special thanks go to my lab mates Mr. Sudhansu Sekhar Rath, Mr. Bijay Kumar Guha and Ms. Kasturi Singh for their technical help during my work. The authors also express their thankfulness to the anonymous reviewers for their valuable comments and suggestions, which helped in the overall improvement of the manuscript.

References

  1. Ackerman AS (2000) Reduction of tropical cloudiness by soot. Science 288:1042–1047Google Scholar
  2. Adesina AJ, Kumar KR, Sivakumar V (2016) Aerosol-cloud-precipitation interactions over major cities in South Africa: impact on regional environment and climate change. Aerosol Air Qual Res 2016:195–211Google Scholar
  3. Alam K, Khan R, Blaschke T, Mukhtiar A (2014) Variability of aerosol optical depth and their impact on cloud properties in Pakistan. J Atmos Sol-Terr Phys 107:104–112Google Scholar
  4. Albrecht BA (1989) Aerosols, cloud microphysics, and fractional cloudiness. Science 245:1227–1230Google Scholar
  5. Anderson TL, Charlson RJ, Winker DM, Ogren JA, Holmén K (2003) Mesoscale variations of tropospheric aerosols. J Atmos Sci 60(1):119–136Google Scholar
  6. Andreae MO, Rosenfeld D, Artaxo P, Costa AA, Frank GP, Longo KM, Silva-Dias MA (2004) Smoking rain clouds over the Amazon. Science 303:1337–1342Google Scholar
  7. Arya PS (2001) Introduction to micrometeorology. Second edition, academic press, international geophysics series Vol. 79: 447ppGoogle Scholar
  8. Bergin MS, West JJ, Keating TJ, Russell AG (2005) Regional atmospheric pollution and transboundary air quality management. Annu Rev Environ Resour 30:1–37Google Scholar
  9. Bhawar RL, Devara PCS (2010) Study of successive contrasting monsoons (2001–2002) in terms of aerosol variability over a tropical station Pune, India. Atmos Chem Phys 10:29–37Google Scholar
  10. Box GEP, Jenkins GM (1976) Time series analysis: forecasting and control. Holden-Day, Merrifield, Va 575Google Scholar
  11. Chaudhuri S, Pal J (2014) Cloud–aerosol coupled index in estimating the break phase of Indian summer monsoon. Theor Appl Climatol 118:447–464Google Scholar
  12. Cheng F, Zhang J, He J, Zha Y, Li Q, Li Y (2017) Analysis of aerosol-cloud-precipitation interactions based on MODIS data. Adv Space Res 59:63–73Google Scholar
  13. Das N, Baral SS, Sahoo SK, Mohapatra RK, Ramulu TS, Das SN, Chaudhury GR (2009) Aerosol physical characteristics at Bhubaneswar, east coast of India. Atmos Res 93:897–901Google Scholar
  14. Das S, Dey S, Dash SK (2016) Direct radiative effects of anthropogenic aerosols on Indian summer monsoon circulation. Theor Appl Climatol 24:629–639Google Scholar
  15. Devasthale A, Krüger O, Grassl H (2005) Change in cloud-top temperatures over Europe. IEEE Geosci Remote Sens Lett 2:333–336Google Scholar
  16. Fan J, Yuan T, Comstock JM, Ghan S, Khain A, Leung LR, Li Z, Martins VJ, Ovchinnikov M (2009) Dominant role by vertical wind shear in regulating aerosol effects on deep convective clouds. J Geophys Res Atmos 114:1–9Google Scholar
  17. Fan J, Wang Y, Rosenfeld D, Liu X (2016) Review of aerosol–cloud interactions: mechanisms, significance, and challenges. J Atmos Sci 73(11):4221–4252Google Scholar
  18. Feingold G, Eberhard WL, Veron DE, Previdi M (2003) First measurements of the Twomey indirect effect using ground-based remote sensors. Geophys Res Lett 30(6):1–4Google Scholar
  19. Gautam R, Liu Z, Singh RP, Hsu NC (2009) Two contrasting dust-dominant periods over India observed from MODIS and CALIPSO data. Geophys Res Lett 36 (L06813).  https://doi.org/10.1029/2008GL036967
  20. Gautam R, Hsu NC, Lau K-M (2010) Premonsoon aerosol characterization and radiative effects over the Indo-Gangetic Plains: implications for regional climate warming. J Geophys Res 115(D17208), 15pp).  https://doi.org/10.1029/2010JD013819
  21. Gautam R, Hsu NC, Tsay SC, Lau KM, Holben B, Bell S, Smirnov A, Li C, Hansell R, Ji Q, Payra S (2011) Accumulation of aerosols over the Indo-Gangetic plains and southern slopes of the Himalayas: distribution, properties and radiative effects during the 2009 pre-monsoon season. Atmos Chem Phys 11:12841–12863Google Scholar
  22. Gryspeerdt E, Stier P, Partridge DG (2014) Links between satellite-retrieved aerosol and precipitation. Atmos Chem Phys 14:9677–9694Google Scholar
  23. Gryspeerdt E, Stier P, White BA, Kipling Z (2015) Wet scavenging limits the detection of aerosol effects on precipitation. Atmos Chem Phys 15:7557–7570Google Scholar
  24. Gunn R, Phillips BB (1957) An experimental investigation of the effect of air pollution on the initiation of rain. J Meteorol 14:272–280Google Scholar
  25. Hansen J, Sato M, Ruedy R (1997) Radiative forcing and climate response. J Geophys Res 102:6831–6864Google Scholar
  26. Iguchi T, Meneghini R, Awaka J, Kozu T, Okamoto K (2000) Rain profiling algorithm for TRMM precipitation radar data. Adv Space Res 25:973–976Google Scholar
  27. Isaksen IS, Granier C, Myhre G, Berntsen TK, Dalsøren SB, Gauss M, Klimont Z, Benestad R, Bousquet P, Collins W, Cox T (2009) Atmospheric composition change: climate–chemistry interactions. Atmos Environ 43:5138–5192Google Scholar
  28. Jin M (2006) MODIS observed seasonal and interannual variations of atmospheric conditions associated with hydrological cycle over Tibetan plateau. Geophys Res Lett 33:2–6Google Scholar
  29. Jin M, Shepherd JM (2008) Aerosol relationships to warm season clouds and rainfall at monthly scales over East China: urban land versus ocean. J Geophys Res Atmos 113:1–12Google Scholar
  30. Jones TA, Christopher SA, Quaas J (2009) A six year satellite-based assessment of the regional variations in aerosol indirect effects. Atmos Chem Phys 9:4091–4114Google Scholar
  31. Kang N, Kumar KR, Yin Y, Diao Y, Yu X (2015) Correlation analysis between AOD and cloud parameters to study their relationship over China using MODIS data (2003–2013): impact on cloud formation and climate change. Aerosol Air Qual Res 15:958–973Google Scholar
  32. Kant S, Panda J, Gautam R, Wang PK, Singh SP (2017) Significance of aerosols influencing weather and climate over Indian region. Int J Earth Atmos Sci 4:1–20Google Scholar
  33. Kaufman YJ, Fraser RS (1997) The effect of smoke particles on clouds and climate forcing. Science 277:1636–1639Google Scholar
  34. Kaufman YJ, Nakajima T (1993) Effect of Amazon smoke on cloud microphysics and albedo - analysis from satellite imagery. J Appl Meteorol 32:729–744Google Scholar
  35. Kaufman YJ, Tanré D, Remer LA, Vermote EF, Chu A, Holben BN (1997) Operational remote sensing of tropospheric aerosol over land from EOS moderate resolution imaging spectroradiometer. J Geophys Res 102:17051–17067Google Scholar
  36. Khain AP (2009) Notes on state-of-the-art investigations of aerosol effects on precipitation: a critical review. Environ Res Lett 4:1–20Google Scholar
  37. King MD, Tsay SC, Platnick SE, Wang M, Liou KN (1997) Cloud retrieval algorithms for MODIS: optical thickness, effective particle radius, and thermodynamic phase. MODIS Algorithm Theoretical Basis Document. No. ATBD-MOD-05, 83ppGoogle Scholar
  38. Koren I, Kaufman YJ, Remer LA, Martins JV (2004) Measurement of the effect of Amazon smoke on inhibition of cloud formation. Science 303:1342–1345Google Scholar
  39. Koren I, Kaufman YJ, Rosenfeld D, Remer LA, Rudich Y (2005) Aerosol invigoration and restructuring of Atlantic convective clouds. Geophys Res Lett 32:L14828.  https://doi.org/10.1029/2005GL023187 Google Scholar
  40. Koren I, Martins JV, Remer LA, Afargan H (2008) Smoke invigoration versus inhibition of clouds over the Amazon. Science 321:1–5Google Scholar
  41. Koren I, Feingold G, Remer LA (2010) The invigoration of deep convective clouds over the Atlantic: aerosol effect, meteorology or retrieval artifact? Atmos Chem Phys 10:8855–8872Google Scholar
  42. Koren I, Altaratz O, Remer LA, Feingold G, Martins JV, Heiblum RH (2012) Aerosol-induced intensification of rain from the tropics to the mid-latitudes. Nat Geosci 5:118–122Google Scholar
  43. Kummerow C, Simpson J, Thiele O, Barnes W, Chang AT, Stocker E, Adler RF, Hou A, Kakar R, Wentz F, Ashcroft P (2000) The status of the tropical rainfall measuring mission (TRMM) after two years in orbit. J Appl Meteorol 39:1965–1982Google Scholar
  44. Lau KM, Kim KM (2006) Observational relationships between aerosol and Asian monsoon rainfall, and circulation. Geophys Res Lett 33:1–5Google Scholar
  45. Lau KM, Kim MK, Kim KM (2006) Asian summer monsoon anomalies induced by aerosol direct forcing: the role of the Tibetan plateau. Clim Dyn 26:855–864Google Scholar
  46. Li Z, Niu F, Fan J, Liu Y, Rosenfeld D, Ding Y (2011) Long-term impacts of aerosols on the vertical development of clouds and precipitation. Nat Geosci 4:888–894Google Scholar
  47. Li Z, Lau WK-M, Ramanathan V, Wu G, Ding Y, Manoj MG, Liu J, Qian Y, Li J, Zhou T, Fan J, Rosenfeld D, Ming Y, Wang Y, Huang J, Wang B, Xu X, Lee S-S, Cribb M, Zhang F, Yang X, Zhao C, Takemura T, Wang K, Xia X, Yin Y, Zhang H, Guo J, Zhai PM, Sugimoto N, Babu SS, Brasseur GP (2016) Aerosol and monsoon climate interactions over Asia. Rev Geophys 54(4):866–929Google Scholar
  48. Lin JC, Matsui T, Pielke SA, Kummerow C (2006) Effects of biomass-burning-derived aerosols on precipitations and clouds in the Amazon Basin: a satellite-based empirical study. J Geophys Res Atmos 111:1–14Google Scholar
  49. Liu Y, de Leeuw G, Kerminen V-M, Zhang J, Zhou P, Nie W, Qi X, Hong J, Wang Y, Ding A, Guo H, Krüger O, Kulmala M, Petäjä T (2017) Analysis of aerosol effects on warm clouds over the Yangtze River Delta from multi-sensor satellite observations. Atmos Chem Phys 17(9):5623–5641Google Scholar
  50. Lohmann U, Feichter J (2005) Global indirect aerosol effects: a review. Atmos Chem Phys 5:715–737Google Scholar
  51. Manoj MG, Devara PCS, Safai PD, Goswami BN (2011) Absorbing aerosols facilitate transition of Indian monsoon breaks to active spells. Clim Dyn 37:2181–2198Google Scholar
  52. Manoj MG, Devara PCS, Joseph S, Sahai AK (2012) Aerosol indirect effect during the aberrant Indian summer monsoon breaks of 2009. Atmos Environ 60:153–163Google Scholar
  53. Meskhidze N, Remer LA, Platnick S, Negrón Juárez R, Lichtenberger AM, Aiyyer AR (2009) Exploring the differences in cloud properties observed by the Terra and Aqua MODIS sensors. Atmos Chem Phys 9:3461–3475Google Scholar
  54. Minnis P, Ayers JK, Palikonda R, Phan D (2004) Contrails, cirrus trends, and climate. J Clim 17:1671–1685Google Scholar
  55. Mohapatra GN, Panda US, Mohanty PK (2007) Annual cycle of surface meteorological and solar energy parameters over Orissa. Ind J Radio Space Phys 36:128–144Google Scholar
  56. Murray BJ, O’Sullivan D, Atkinson JD, Webb ME (2012) Ice nucleation by particles immersed in supercooled cloud droplets. Chem Soc Rev 41:6519–6554Google Scholar
  57. Nair VS, Moorthy KK, Alappattu DP, Kunhikrishnan PK, George S, Nair PR, Babu SS, Abish B, Satheesh SK, Tripathi SN, Niranjan K (2007) Wintertime aerosol characteristics over the Indo-Gangetic plain (IGP): impacts of local boundary layer processes and long-range transport. J Geophys Res Atmos 112:1–15Google Scholar
  58. Niu F, Li Z (2011) Cloud invigoration and suppression by aerosols over the tropical region based on satellite observations. Atmos Chem Phys Discuss 11:5003–5017Google Scholar
  59. Niu F, Li Z (2012) Systematic variations of cloud top temperature and precipitation rate with aerosols over the global tropics. Atmos Chem Phys 12(18):8491–8498Google Scholar
  60. Panda J, Sharan M (2012) Influence of land-surface and turbulent parameterization schemes on regional-scale boundary layer characteristics over northern India. Atmos Res 112:89–111Google Scholar
  61. Panda J, Sharan M, Gopalakrishnan SG (2009) Study of regional-scale boundary layer characteristics over northern India with a special reference to the role of the Thar Desert in regional-scale transport. J Appl Meteorol Climatol 48(11):2377–2402Google Scholar
  62. Platnick S, King MD, Ackerman SA, Menzel WP, Baum BA, Riédi JC, Frey RA (2003) The MODIS cloud products: algorithms and examples from terra. IEEE Trans Geosci Remote Sens 41:459–472Google Scholar
  63. Quaas J, Ming Y, Menon S, Takemura T, Wang M, Penner JE, Gettelman A, Lohmann U, Bellouin N, Boucher O, Sayer AM (2009) Aerosol indirect effects–general circulation model intercomparison and evaluation with satellite data. Atmos Chem Phys 9:8697–8717Google Scholar
  64. Quaas J, Stevens B, Stier P, Lohmann U (2010) Interpreting the cloud cover–aerosol optical depth relationship found in satellite data using a general circulation model. Atmos Chem Phys 10(13):6129–6135Google Scholar
  65. Remer LA, Kaufman YJ, Tanré D, Mattoo S, Chu DA, Martins JV, Li RR, Ichoku C, Levy RC, Kleidman RG, Eck TF (2005) The MODIS aerosol algorithm, products, and validation. J Atmos Sci 62:947–973Google Scholar
  66. Remer LA, Kleidman RG, Levy RC, Kaufman YJ, Tanré D, Mattoo S, Martins JV, Ichoku C, Koren I, Yu H, Holben BN (2008) Global aerosol climatology from the MODIS satellite sensors. J Geophys Res Atmos 113(D14S07):5.  https://doi.org/10.1029/2007JD009661 Google Scholar
  67. Rosenfeld D (1999) TRMM observed first direct evidence of smoke from forest fires inhibiting rainfall. Geophys Res Lett 26:3105–3108Google Scholar
  68. Rosenfeld D, Gutman G (1994) Retrieving microphysical properties near the tops of potential rain clouds by multispectral analysis of AVHRR data. Atmos Res 34:259–283Google Scholar
  69. Rosenfeld D, Lensky IM (1998) Satellite-based insights into precipitation formation processes in continental and maritime convective clouds. Bull Am Meteorol Soc 79:2457–2476Google Scholar
  70. Rosenfeld D, Woodley W (2000) Deep convective clouds with sustained supercooled liquid water down to −37.5 degrees C. Nature 405:440–442Google Scholar
  71. Rosenfeld D, Rudich Y, Lahav R (2001) Desert dust suppressing precipitation: a possible desertification feedback loop. Proc Natl Acad Sci U S A 98:5975–5980Google Scholar
  72. Rosenfeld D, Woodley W, Lerner A, Kelman G, Lindsey D (2008) Satellite detection of severe convective storms by their retrieved vertical profiles of cloud particle effective radius and thermodynamic phase. J Geophys Res 113:D04208Google Scholar
  73. Sarangi C, Tripathi SN, Kanawade VP, Koren I, Pai DS (2017) Investigation of the aerosol–cloud–rainfall association over the Indian summer monsoon region. Atmos Chem Phys 17:5185–5204Google Scholar
  74. Sayer AM, Hsu NC, Bettenhausen C, Lee J, Redemann J, Schmid B, Shinozuka Y (2016) Extending “deep blue” aerosol retrieval coverage to cases of absorbing aerosols above clouds: sensitivity analysis and first case studies. J Geophys Res Atmos 121:4830–4854Google Scholar
  75. Singh RP, Dey S, Tripathi SN, Tare V, Holben B (2004) Variability of aerosol parameters over Kanpur, northern India. J Geophys Res Atmos 109:1–14Google Scholar
  76. Squires P (1958) The microstructure and colloidal stability of warm clouds. Tellus 10:262–271Google Scholar
  77. Squires P, Twomey S (1966) A comparison of cloud nucleus measurements over Central North America and the Caribbean Sea. J Atmos Sci 23:401–404Google Scholar
  78. Stevens B, Feingold G (2009) Untangling aerosol effects on clouds and precipitation in a buffered system. Nature 461:607–613Google Scholar
  79. Storelvmo T, Kristjánsson JE, Ghan SJ, Kirkevåg A, Seland Ø, Iversen T (2006) Predicting cloud droplet number concentration in community atmosphere model (CAM)-Oslo. J Geophys Res Atmos 111(D24208), 14pp).  https://doi.org/10.1029/2005JD006300
  80. Stull RB (1988) An introduction to boundary layer meteorology. Kluwer Academic Publishers Netherlands, 670ppGoogle Scholar
  81. Ten Hoeve JE, Remer LA, Jacobson MZ (2011) Microphysical and radiative effects of aerosols on warm clouds during the Amazon biomass burning season as observed by MODIS: impacts of water vapor and land cover. Atmos Chem Phys 11:3021–3036Google Scholar
  82. Tripathi SN, Dey S, Chandel A, Srivastava S, Singh RP, Holben BN (2005) Comparison of MODIS and AERONET derived aerosol optical depth over the Ganga Basin, India. Ann Geophys 23:1093–1101Google Scholar
  83. Twomey S (1977) The influence of pollution on the shortwave albedo of clouds. J Atmos Sci 34:1149–1152Google Scholar
  84. Twomey SA, Piepgrass M, Wolfe TL (1984) An assessment of the impact of pollution on global cloud albedo. Tellus Ser B Chem Phys Meteorol 36(5):356–366Google Scholar
  85. Verma S, Priyadharshini B, Pani SK, Kumar DB, Faruqi AR, Bhanja SN, Mandal M (2016) Aerosol extinction properties over coastalWest Bengal Gangetic plain under inter-seasonal and sea breeze influenced transport processes. Atmos Res 167:224–236Google Scholar
  86. Vinoj V, Rasch PJ, Wang H, Yoon JH, Ma PL, Landu K, Singh B (2014) Short-term modulation of Indian summer monsoon rainfall by west Asian dust. Nat Geosci 7:308–313Google Scholar
  87. Warner J (1968) A reduction in rainfall associated with smoke from sugar-cane fires—an inadvertent weather modification? J Appl Meteorol 7:247–251Google Scholar
  88. Warner J, Twomey S (1967) The production of cloud nuclei by cane fires and the effect on cloud droplet concentration. J Atmos Sci 24:704–706Google Scholar
  89. Yuan T, Li Z, Zhang R, Fan J (2008) Increase of cloud droplet size with aerosol optical depth: an observation and modeling study. J Geophys Res Atmos 113(D4):27Google Scholar

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© Springer-Verlag GmbH Austria, part of Springer Nature 2018

Authors and Affiliations

  1. 1.Department of Earth and Atmospheric SciencesNational Institute of Technology RourkelaRourkelaIndia
  2. 2.Department of Atmospheric SciencesNational Central UniversityTaoyuanTaiwan
  3. 3.Research Center for Environmental ChangesAcademia SinicaTaipeiTaiwan
  4. 4.Department of Atmospheric and Oceanic SciencesUniversity of Wisconsin-MadisonMadisonUSA

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