Abstract
The Asian Summer Monsoon (ASM) exhibit different modes of variability in which the active and break phases is one of the most prominent intraseasonal scale variability of the ASM. The shift in convective centres to more polluted regions coupled with the associated circulation features during these phases results in a redistribution of trace species in the upper troposphere and lower stratosphere (UTLS) region. Apropos to this, this study presents a quantitative assessment of the variability in the spatial distribution of ozone, carbon monoxide (CO) and water vapour (H2O) in the UTLS during the active and break phase of ASM with respect to the seasonal mean background using fifteen years (2005–2019) of Aura-MLS observations in conjunction with reanalysis data sets, cloud-top brightness temperatures and trajectory analysis. These 15-years of data is used to make composite maps of tracer anomalies to investigate the varying influence of monsoon convection, transport and ASMA dynamics in the UTLS region during the active/break phase. This study shows that, while the distribution of trace species during both phases is determined by the combined role of convection and transport in the upper troposphere, changes in ASMA modes, transport and tropopause dynamics during the active/break phases controls the spatial pattern of both tropospheric and stratospheric species near the tropopause level.
Similar content being viewed by others
Data availability
The datasets analysed during the current study are freely available in their respective public domains. MLS: https://mls.jpl.nasa.gov/eos-aura-mls; NCEP/NCAR reanalysis: https://psl.noaa.gov/data/gridded/data.ncep.reanalysis.pressure.html; NOAA OLR: https://data.nodc.noaa.gov/cgi-bin/iso?id=gov.noaa.ncdc:C00875; NOAA GridSat-B1 TIRBT: https://www.ncei.noaa.gov/products/gridded-geostationary-brightness-temperature.
References
Adcock KE et al (2021) Aircraft-based observations of ozone-depleting substances in the upper troposphere and lower stratosphere in and above the asian summer monsoon. J Geophys Res Atmospheres 126(1):e2020JD033137. https://doi.org/10.1029/2020JD033137
Amemiya A, Sato K (2020) Characterizing quasi-biweekly variability of the Asian monsoon anticyclone using potential vorticity and large-scale geopotential height field. Atmos Chem Phys 20(22):13857–13876. https://doi.org/10.5194/acp-20-13857-2020
Annamalai H, Slingo JM (2001) Active/break cycles: diagnosis of the intraseasonal variability of the Asian summer monsoon. Clim Dyn 18(1):85–102. https://doi.org/10.1007/s003820100161
Apel EC et al (2015) Upper tropospheric ozone production from lightning NOx-impacted convection: smoke ingestion case study from the DC3 campaign. J Geophys Res Atmospheres 120(6):2505–2523. https://doi.org/10.1002/2014JD022121
Appel O et al (2022) Chemical analysis of the Asian tropopause aerosol layer (ATAL) with emphasis on secondary aerosol particles using aircraft-based in situ aerosol mass spectrometry. Atmos Chem Phys 22(20):13607–13630. https://doi.org/10.5194/acp-22-13607-2022
Basha G, Ratnam MV, Jiang JH, Kishore P, RavindraBabu S (2021) Influence of Indian summer monsoon on tropopause, trace gases and aerosols in Asian summer monsoon anticyclone observed by COSMIC. MLS CALIPSO Remote Sensing 13(17):3486
Bhat G, Chakraborty A, Nanjundiah R ,Srinivasan J (2002) Vertical thermal structure of the atmosphere during active and weak phases of convection over the north Bay of Bengal: observation and model results. Curr Sci 83296–302
Bhatla R, Mohanty UC, Raju PVS, Madan OP (2004) A study on dynamic and thermodynamic aspects of breaks in the summer monsoon over India. Int J Climatol 24(3):341–360. https://doi.org/10.1002/joc.1005
Bian J, Pan LL, Paulik L, Vömel H, Chen H, Lu D (2012) In situ water vapor and ozone measurements in Lhasa and Kunming during the Asian summer monsoon. Geophys Res Lett. https://doi.org/10.1029/2012GL052996
Bluestein H (1993) Synoptic-dynamic meteorology in midlatitudes: Vol II observations and theory of weather systems. Oxford University Press, New York, p 594
Chen P (1995) Isentropic cross-tropopause mass exchange in the extratropics. J Geophys Rese Atmospheres 100(D8):16661–16673. https://doi.org/10.1029/95JD01264
Clemens J, Ploeger F, Konopka P, Portmann R, Sprenger M, Wernli H (2022) Characterization of transport from the Asian summer monsoon anticyclone into the UTLS via shedding of low potential vorticity cutoffs. Atmos Chem Phys 22(6):3841–3860. https://doi.org/10.5194/acp-22-3841-2022
Dethof A, O’Neill A, Slingo JM, Smit HGJ (1999) A mechanism for moistening the lower stratosphere involving the Asian summer monsoon. Q J R Meteorol Soc 125(556):1079–1106. https://doi.org/10.1002/qj.1999.49712555602
Dethof A, O’Neill A, Slingo J (2000) Quantification of the isentropic mass transport across the dynamical tropopause. J Geophys Res Atmospheres 105(D10):12279–12293. https://doi.org/10.1029/2000JD900127
Devasthale A, Fueglistaler S (2010) A climatological perspective of deep convection penetrating the TTL during the Indian summer monsoon from the AVHRR and MODIS instruments. Atmos Chem Phys 10(10):4573–4582. https://doi.org/10.5194/acp-10-4573-2010
Devasthale A, Grassl H (2009) A daytime climatological distribution of high opaque ice cloud classes over the Indian summer monsoon region observed from 25-year AVHRR data. Atmos Chem Phys 9(12):4185–4196. https://doi.org/10.5194/acp-9-4185-2009
Draxler R, Hess G (1998) An overview of the HYSPLIT_4 modeling system for trajectories, dispersion, and deposition. Australian Meteorol Magazine 47:295–308
Dwivedi S, Mittal AK (2007) Forecasting the duration of active and break spells in intrinsic mode functions of Indian monsoon intraseasonal oscillations. Geophys Res Lett. https://doi.org/10.1029/2007GL030540
Emmanuel M, Sunilkumar SV, Muhsin M, SatheeshChandran PR, Parameswaran K, Kumar BS, Maitra A, Satyanarayana ANV, Nagendra N (2021) Effect of monsoon dynamics and deep convection on the upper troposphere lower stratosphere water vapour over Indian monsoon region. Atmospheric Res. https://doi.org/10.1016/j.atmosres.2020.105336
Fadnavis S, Roy C, Chattopadhyay R, Sioris CE, Rap A, Müller R, Kumar KR, Krishnan R (2018) Transport of trace gases via eddy shedding from the Asian summer monsoon anticyclone and associated impacts on ozone heating rates. Atmos Chem Phys 18(15):11493–11506. https://doi.org/10.5194/acp-18-11493-2018
Gadgil S (2003) The Indian monsoon and its variability. Annu Rev Earth Planet Sci 31(1):429–467. https://doi.org/10.1146/annurev.earth.31.100901.141251
Gadgil S, Joseph PV (2003) On breaks of the Indian monsoon. J Earth Syst Sci 112(4):529–558. https://doi.org/10.1007/BF02709778
Garny H, Randel WJ (2013) Dynamic variability of the Asian monsoon anticyclone observed in potential vorticity and correlations with tracer distributions. J Geophys Res Atmospheres 118(24):13,421-413,433. https://doi.org/10.1002/2013JD020908
Gill AE (1980) Some simple solutions for heat-induced tropical circulation. Q J R Meteorol Soc 106(449):447–462. https://doi.org/10.1002/qj.49710644905
Goswami BN (2005) South Asian monsoon. In: Intraseasonal variability in the atmosphere-ocean climate system. Springer Praxis Books. Springer, Berlin, Heidelberg. https://doi.org/10.1007/3-540-27250-X_2
Gottschaldt KD et al (2018) Dynamics and composition of the Asian summer monsoon anticyclone. Atmos Chem Phys 18(8):5655–5675. https://doi.org/10.5194/acp-18-5655-2018
Holton JR, Haynes PH, McIntyre ME, Douglass AR, Rood RB, Pfister L (1995) Stratosphere-troposphere exchange. Rev Geophys 33(4):403–439. https://doi.org/10.1029/95RG02097
Honomichl SB, Pan LL (2020) Transport from the Asian summer monsoon anticyclone over the western pacific. J Geophys Res Atmospheres 125(13):e2019JD032094. https://doi.org/10.1029/2019JD032094
Hoor P, Fischer H, Lange L, Lelieveld J, Brunner D (2002) Seasonal variations of a mixing layer in the lowermost stratosphere as identified by the CO-O3 correlation from in situ measurements. J Geophys Res. https://doi.org/10.1029/2000JD000289
Hoskins BJ, McIntyre ME, Robertson AW (1985) On the use and significance of isentropic potential vorticity maps. Q J R Meteorol Soc 111(470):877–946. https://doi.org/10.1002/qj.49711147002
Jiang X, Li T, Wang B (2004) Structures and mechanisms of the northward propagating boreal summer intraseasonal oscillation. J Clim 17(5):1022–1039. https://doi.org/10.1175/1520-0442(2004)017%3c1022:Samotn%3e2.0.Co;2
Joseph PV, Sabin TP (2008) An ocean–atmosphere interaction mechanism for the active break cycle of the Asian summer monsoon. Clim Dyn 30(6):553–566. https://doi.org/10.1007/s00382-007-0305-2
Kalnay E et al (1996) The NCEP/NCAR 40-year reanalysis project. Bull Am Meteor Soc 77(3):437–472. https://doi.org/10.1175/1520-0477(1996)077%3c0437:Tnyrp%3e2.0.Co;2
Karmakar N, Chakraborty A, Nanjundiah RS (2017) Space-time evolution of the low- and high-frequency intraseasonal modes of the Indian summer monsoon. Mon Weather Rev 145(2):413–435. https://doi.org/10.1175/mwr-d-16-0075.1
Karmakar N, Joseph S, Sahai AK, Kaur M, Phani R, Mandal R, Dey A (2022) Northward propagation of convection over the Indian region in multiphysics multimodel ensemble. Quart J Royal Meteorol Soc. https://doi.org/10.1002/qj.4404
Khaykin SM et al (2022) Persistence of moist plumes from overshooting convection in the Asian monsoon anticyclone. Atmos Chem Phys 22(5):3169–3189. https://doi.org/10.5194/acp-22-3169-2022
Knapp KR et al (2011) Globally gridded satellite observations for climate studies. Bull Am Meteor Soc 92(7):893–907. https://doi.org/10.1175/2011bams3039.1
Krishnamurthy V, Shukla J (2008) Seasonal persistence and propagation of intraseasonal patterns over the Indian monsoon region. Clim Dyn 30(4):353–369. https://doi.org/10.1007/s00382-007-0300-7
Kumar AH, Ratnam MV (2021) Variability in the UTLS chemical composition during different modes of the Asian summer monsoon anti-cyclone. Atmospheric Res. https://doi.org/10.1016/j.atmosres.2021.105700
Kumari A, Kumar P (2022) Contrasting changes in precipitation events during active and break spells of Indian summer monsoon in recent decades. Clim Dyn 59(3):887–902. https://doi.org/10.1007/s00382-022-06162-y
Lal S, Venkataramani S, Chandra N, Cooper OR, Brioude J, Naja M (2014) Transport effects on the vertical distribution of tropospheric ozone over western India. J Geophys Res Atmospheres 119(16):10012–10026. https://doi.org/10.1002/2014JD021854
Lelieveld J et al (2002) Global air pollution crossroads over the mediterranean. Science 298(5594):794–799. https://doi.org/10.1126/science.1075457
Lelieveld J et al (2018) The South Asian monsoon—pollution pump and purifier. Science 361(6399):270–273. https://doi.org/10.1126/science.aar2501
Livesey NJ, Snyder WV, Read WG, Wagner PA (2006) Retrieval algorithms for the EOS Microwave limb sounder (MLS). IEEE Trans Geosci Remote Sens 44(5):1144–1155. https://doi.org/10.1109/TGRS.2006.872327
Livesey. NJ, Read WG ,Wagner PA, Froidevaux L, Lambert A, Manney GL, Valle LFM, Pumphrey HC, Santee ML, Schwartz MJ, Wang S, Fuller RA, Jarnot RF, Knosp BW, Martinez E, Lay RR (2018) Earth observing system (EOS) Aura microwave limb sounder (MLS) Version 4.2x Level 2 data quality and description document. JPL D-33509 Rev. D
Ortega S, Webster PJ, Toma V, Chang H-R (2017) Quasi-biweekly oscillations of the South Asian monsoon and its co-evolution in the upper and lower troposphere. Clim Dyn 49(9):3159–3174. https://doi.org/10.1007/s00382-016-3503-y
Ortega S, Webster PJ, Toma V, Chang H-R (2018) The effect of potential vorticity fluxes on the circulation of the tropical upper troposphere. Q J R Meteorol Soc 144(712):848–860. https://doi.org/10.1002/qj.3261
Pai DS, Sridhar L, Ramesh Kumar MR (2016) Active and break events of Indian summer monsoon during 1901–2014. Clim Dyn 46(11):3921–3939. https://doi.org/10.1007/s00382-015-2813-9
Pan LL, Honomichl SB, Kinnison DE, Abalos M, Randel WJ, Bergman JW, Bian J (2016) Transport of chemical tracers from the boundary layer to stratosphere associated with the dynamics of the Asian summer monsoon. J Geophys Res Atmospheres 121(23):14,159-114,174. https://doi.org/10.1002/2016JD025616
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 Atmospheres. https://doi.org/10.1029/2006JD008294
Ploeger F, Konopka P, Walker K, Riese M (2017) Quantifying pollution transport from the Asian monsoon anticyclone into the lower stratosphere. Atmos Chem Phys 17(11):7055–7066. https://doi.org/10.5194/acp-17-7055-2017
Rajeevan M, Gadgil S, Bhate J (2010) Active and break spells of the Indian summer monsoon. J Earth Syst Sci 119(3):229–247. https://doi.org/10.1007/s12040-010-0019-4
Rajeevan M, Rohini P, Niranjan Kumar K, Srinivasan J, Unnikrishnan CK (2013) A study of vertical cloud structure of the Indian summer monsoon using CloudSat data. Clim Dyn 40(3):637–650. https://doi.org/10.1007/s00382-012-1374-4
Randel WJ, Park M, Emmons L, Kinnison D, Bernath P, Walker KA, Boone C, Pumphrey H (2010) Asian monsoon transport of pollution to the stratosphere. Science 328(5978):611–613. https://doi.org/10.1126/science.1182274
Ravi Kiran V, Rajeevan M, VijayaBhaskara Rao S, Prabhakara Rao N (2009) Analysis of variations of cloud and aerosol properties associated with active and break spells of Indian summer monsoon using MODIS data. Geophys Res Lett. https://doi.org/10.1029/2008GL037135
Revadekar JV, Ravi Kumar K, Tiwari YK, Valsala V (2016) Variability in AIRS CO2 during active and break phases of Indian summer monsoon. Sci Total Environ. https://doi.org/10.1016/j.scitotenv.2015.09.078
Rodwell MJ, Hoskins BJ (1996) Monsoons and the dynamics of deserts. Q J R Meteorol Soc 122(534):1385–1404. https://doi.org/10.1002/qj.49712253408
Roja Raman M, Jagannadha Rao VVM, VenkatRatnam M, Kishore Kumar G, Narendra Babu A, VijayaBhaskara Rao S, Prabhakara Rao N, Narayana Rao D (2008) Atmospheric circulation during active and break phases of Indian summer monsoon: a study using MST radar at Gadanki (13.5°N, 79.2°E). J Geophys Res Atmospheres. https://doi.org/10.1029/2008JD010341
Sahu DK, Krishnamurti TN, Kumar V (2019) Elucidating intra-seasonal characteristics of Indian summer monsoon Part-I: Viewed from remote sensing observations, reanalysis and model datasets. J Earth Syst Sci 129(1):29. https://doi.org/10.1007/s12040-019-1276-5
SatheeshChandran PR, Sunilkumar SV, Muhsin M, Emmanuel M, Ramkumar G, Nair PR (2021) Effect of meteorology on the variability of ozone in the troposphere and lower stratosphere over a tropical station Thumba (8.5°N, 76.9°E). J Atmospheric Solar-Terrestrial Phys 215:105567. https://doi.org/10.1016/j.jastp.2021.105567
Siu LW, Bowman KP (2020) Unsteady vortex behavior in the Asian monsoon anticyclone. J Atmos Sci 77(12):4067–4088. https://doi.org/10.1175/jas-d-19-0349.1
Sivan C, Kottayil A, Legras B, Bucci S, Mohanakumar K, Satheesan K (2022) Tracing the convective sources of air at tropical tropopause during the active and break phases of Indian summer monsoon. Clim Dyn 59(9):2717–2734. https://doi.org/10.1007/s00382-022-06238-9
Slingo JM, Annamalai H (2000) 1997: The El Niño of the century and the response of the Indian summer monsoon. Mon Weather Rev 128(6):1778–1797. https://doi.org/10.1175/1520-0493(2000)128%3c1778:Tenoot%3e2.0.Co;2
Sperber KR, Slingo JM, Annamalai H (2000) Predictability and the relationship between subseasonal and interannual variability during the Asian summer monsoon. Q J R Meteorol Soc 126(568):2545–2574. https://doi.org/10.1002/qj.49712656810
Straus DM (2022) Preferred intra-seasonal circulation patterns of the Indian summer monsoon and active-break cycles. Clim Dyn 59(5):1415–1434. https://doi.org/10.1007/s00382-021-06047-6
Sudeepkumar BL, Babu CA, Varikoden H (2018) Future projections of active-break spells of Indian summer monsoon in a climate change perspective. Global Planetary Change 161:222–230. https://doi.org/10.1016/j.gloplacha.2017.12.020
Swathi MS, Izumo T, Lengaigne M, Vialard J, Kumar MRR (2020) Remote influences on the Indian monsoon low-level jet intraseasonal variations. Clim Dyn 54(3):2221–2236. https://doi.org/10.1007/s00382-019-05108-1
Thirugnanasambantham D, Shukla BP, Das SK, John J, Kolanuvada SR, Gairola RM (2021) The possible linkage of satellite based cloud microphysical parameters (CMP) to the Indian summer monsoon (ISM) active and break phase. Adv Space Res 68(4):1663–1675. https://doi.org/10.1016/j.asr.2021.04.007
Thompson AM, Tao W-K, Pickering KE, Scala JR, Simpson J (1997) Tropical deep convection and ozone formation. Bull Am Meteor Soc 78(6):1043–1054. https://doi.org/10.1175/1520-0477(1997)078%3c1043:Tdcaof%3e2.0.Co;2
Traub M, Lelieveld J (2003) Cross-tropopause transport over the eastern Mediterranean. J Geophys Res Atmospheres. https://doi.org/10.1029/2003JD003754
Uma KN, Mohan TS, Das SK (2020) Role of intra-seasonal variability in the Indian summer monsoon on the hydration and dehydration of the upper troposphere. Theoret Appl Climatol 141(1):747–761. https://doi.org/10.1007/s00704-020-03243-y
von Hobe M et al (2021) Upward transport into and within the Asian monsoon anticyclone as inferred from StratoClim trace gas observations. Atmos Chem Phys 21(2):1267–1285. https://doi.org/10.5194/acp-21-1267-2021
Wang B, Webster PJ, Teng H (2005) Antecedents and self-induction of active-break south Asian monsoon unraveled by satellites. Geophys Res Lett. https://doi.org/10.1029/2004GL020996
Wang M, Wang J, Duan A, Liu Y, Zhou S (2018) Coupling of the quasi-biweekly oscillation of the Tibetan plateau summer monsoon with the arctic oscillation. Geophys Res Lett 45(15):7756–7764. https://doi.org/10.1029/2018GL077136
Waters JW et al (2006) The Earth observing system microwave limb sounder (EOS MLS) on the aura Satellite. IEEE Trans Geosci Remote Sens 44(5):1075–1092. https://doi.org/10.1109/TGRS.2006.873771
Webster PJ, Magaña VO, Palmer TN, Shukla J, Tomas RA, Yanai M, Yasunari T (1998) Monsoons: processes, predictability, and the prospects for prediction. J Geophys Res Oceans 103(C7):14451–14510. https://doi.org/10.1029/97JC02719
Wei W, Zhang R, Yang S, Li W, Wen M (2019) Quasi-biweekly oscillation of the south Asian high and its role in connecting the Indian and East Asian summer rainfalls. Geophys Res Lett 46(24):14742–14750. https://doi.org/10.1029/2019GL086180
Zhang Q, Wu G, Qian Y (2002) The bimodality of the 100 hPa South Asia high and its relationship to the climate anomaly over East Asia in summer. J Meteorol Soc Japan 80:733–744
Zhang Y, Liu C, Liu Y, Yang R (2019) Intraseasonal oscillation of tropospheric ozone over the Indian summer monsoon region. Adv Atmos Sci 36(4):417–430. https://doi.org/10.1007/s00376-018-8113-7
Acknowledgements
We thank the National Centre for Environmental Prediction/National Centre for Atmospheric Research (NCEP/NCAR) and National Oceanic and Atmospheric Administration (NOAA) for providing, NCEP-1 meteorological reanalysis, TIRBT and daily outgoing longwave radiation (OLR) data for this study. We thank the MLS team for providing Ozone, CO and H2O data.
Funding
The authors declare that no funds, grants or other support were received during the preparation of this manuscript.
Author information
Authors and Affiliations
Contributions
All authors contributed to the study conception and design. Conceptualization, Methodology, Writing-original draft preparation: PRSC; Supervision, Conceptualization and Writing-reviewing and editing: SVS.
Corresponding author
Ethics declarations
Conflict of interest
The authors declare that they have no conflict of interest.
Additional information
Publisher's Note
Springer Nature remains neutral with regard to jurisdictional claims in published maps and institutional affiliations.
Supplementary Information
Below is the link to the electronic supplementary material.
Rights and permissions
Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law.
About this article
Cite this article
Satheesh Chandran, P.R., Sunilkumar, S.V. Role of deep convection and dynamics on the tracer distribution in the upper troposphere and lower stratosphere region during active and break phases of the Asian summer monsoon. Clim Dyn 62, 1945–1963 (2024). https://doi.org/10.1007/s00382-023-07004-1
Received:
Accepted:
Published:
Issue Date:
DOI: https://doi.org/10.1007/s00382-023-07004-1