Abstract
Monsoon Inversion (MI) plays a key role and is one of the semi-permanent features of Asian Summer Monsoon. MI is defined as a sustained temperature inversion (TI) that is observed in the lower troposphere, during summer monsoon (June to September) over the Western AS (WAS) with its peak between July and August. A comprehensive analysis of formation, evolution, and dissipation of MI is made using long-term observations from satellites and ERA-5 reanalysis of 15 years (2008–2022). The climatological day-to-day and monthly variations of MI over the Arabian Sea are studied. The occurrence of inversion (TI) during pre-monsoon, i.e., during April and May, is at a lower altitude and is strengthened by subsidence. The MI is found to occur strongly over the WAS, while it is seen occasionally with lesser strength over the Eastern Arabian Sea (EAS) during July–August. The advection is nearly five times stronger than subsidence. The reasons for the existence and strength of MI are investigated using the data of dust from the CALIPSO. There is a ~ 15% difference in the occurrence of dust over WAS compared to EAS. Also, MI occurrence has shown significant differences in temperature profiles during dust and non-dust cases. The analysis of MI reveals that strong MI is due to more advection of warm dry and dust laden air from desert regions (west, north and northwest directions). The present study has significance to the understanding of interannual monsoon variability.
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Abbreviations
- AGL:
-
Above ground level
- ARL:
-
Air Resources Laboratory
- AS:
-
Arabian Sea
- ASM:
-
Asian Summer Monsoon
- ARMEX:
-
Arabian Sea Monsoon Experiment
- CALIPSO:
-
Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observation
- CC:
-
Clear Continental
- CM:
-
Continental Marine
- C3S:
-
Copernicus Climate Change Service
- DT:
-
Dust
- DAOD:
-
Dust aerosol optical depth
- DM:
-
Dusty Marine
- EAS:
-
Eastern Arabian Sea
- ECMWF:
-
European Centre for Medium-Range Weather Forecasts
- ESA:
-
European Space Agency’s
- FGGE:
-
First GARP Global Experiment
- HYSPLIT:
-
Hybrid SingleParticle Lagrangian Integrated Trajectory
- IASI:
-
Infrared Atmospheric Sounding Interferometer
- ISM:
-
Indian Summer Monsoon
- IIOE:
-
International Indian Ocean Expedition
- ITCZ:
-
Inter-Tropical Convergence Zone
- MONEX:
-
Monsoon Experiment
- MI:
-
Monsoon Inversion
- NCMWRF:
-
National Centre for Medium Range Weather Forecasting
- PC:
-
Polluted Continental
- PD:
-
Polluted Dust
- SBDART:
-
Santa Barbara Discrete Ordinate Atmospheric Radiative Transfer
- SM:
-
Smoke
- SST:
-
Sea surface temperature
- TI:
-
Temperature inversion
- VFM:
-
Vertical Feature Mask
- WAS:
-
Western Arabian Sea
References
Abish B, Mohanakumar K (2011) Role of fine mode aerosols in modulating cloud properties over industrial locations in north India. Ann Geophys 29:1605–1612
Ackerman AS, Toon OB, Stevens DE et al (2000) Reduction of tropical cloudiness by soot. Science (80- ) 288:1042–1047. https://doi.org/10.1126/science.288.5468.1042
Badarinath KVS, Kharol SK, Kaskaoutis DG et al (2010) Long-range transport of dust aerosols over the Arabian Sea and Indian region - a case study using satellite data and ground-based measurements. Glob Planet Change 72:164–181. https://doi.org/10.1016/j.gloplacha.2010.02.003
Byrne MP, Pendergrass AG, Rapp AD, Wodzicki KR (2018) Response of the intertropical convergence zone to climate change : location, width, and strength. Curr Clim Chang Reports 4:355–370. https://doi.org/10.1007/s40641-018-0110-5
Clerbaux C, Boynard A, Clarisse L et al (2009) Monitoring of atmospheric composition using the thermal infrared IASI/MetOp sounder. Atmos Chem Phys 9:6041–6054
Colon JA (1964) On interactions between the southwest monsoon current and the sea surface over the Arabian Sea. Indian J Meteorol Hydrol Geophys 15:183–200
Das PK (1962) Mean vertical motion and non-adiabatic heat sources over India during the monsoon. Tellus 14:212–220
Das PK (1988) The Monsoons. National Book Trust, India
Desai BN (1968) Causes of aridity and inversion over the desert areas of West Pakistan and neighbourhood during the south-west monsoon season. In: Proceedings of the Indian Academy of Sciences - Section A. Springer, pp 103–107
Dey S, Tripathi SN (2008) Aerosol direct radiative effects over Kanpur in the Indo-Gangetic basin, northern India: long-term (2001–2005) observations and implications to regional climate. J Geophys Res Atmos 113:1–20. https://doi.org/10.1029/2007JD009029
Dey S, Tripathi SN, Mishra SK (2008) Probable mixing state of aerosols in the Indo-Gangetic Basin, northern India. Geophys Res Lett 35:1–5. https://doi.org/10.1029/2007GL032622
Draxler RR (1996) Boundary layer isentropic and kinematic trajectories during the August 1993 North Atlantic Regional Experiment Intensive. J Geophys Res Ser 101:29,229–255,268
Dwivedi S (2016) Investigations on low level Indian summer monsoon inversion. SRM University, Chennai
Dwivedi S, Narayanan MS, VenkatRatnam M, Narayana Rao D (2016) Characteristics of monsoon inversions over the Arabian Sea observed by satellite sounder and reanalysis data sets. Atmos Chem Phys 16:4497–4509. https://doi.org/10.5194/acp-16-4497-2016
Dwivedi S, Sathiyamoorthy V, Narayanan MS, Narayana Rao D (2016) A study on the lower tropospheric thermal inversion over the Arabian Sea using radiosonde and IASI data. IEEE J Sel Top Appl Earth Obs Remote Sens 9:490–495. https://doi.org/10.1109/JSTARS.2015.2506759
Dwivedi S, Yesubabu V, Ratnam MV et al (2021) Variability of monsoon inversion over the Arabian Sea and its impact on rainfall. Int J Climatol 41:E2979–E2999. https://doi.org/10.1002/joc.6896
Gadgil S (2018) The monsoon system : Land – sea breeze or the ITCZ ? J Earth Syst Sci 127:1–29. https://doi.org/10.1007/s12040-017-0916-x
Gadgil S, Joseph PV (2003) On breaks of the Indian monsoon. J Earth Syst Sci 112:529–558
Gastineau G, Li L, Le Treut H (2009) The Hadley and Walker circulation changes in global warming conditions described by idealized atmospheric simulations. J Clim 22:3993–4013. https://doi.org/10.1175/2009JCLI2794.1
Ghosh SK, Pant MC, Dewan BN (1978) Influence of the Arabian Sea on the Indian summer monsoon. Tellus 30:117–125. https://doi.org/10.1111/j.2153-3490.1978.tb00825.x
Hersbach H, Bell B, Berrisford P et al (2020) The ERA5 global reanalysis. 1999–2049. https://doi.org/10.1002/qj.3803
Hoffmann L, Günther G, Li D et al (2019) From ERA-Interim to ERA5: The considerable impact of ECMWF’s next-generation reanalysis on Lagrangian transport simulations. Atmos Chem Phys 19:3097–3214. https://doi.org/10.5194/acp-19-3097-2019
Holton JR, Hakim GJ (2012) An introduction to dynamic meteorology. Academic press
Hu Z, Huang J, Zhao C et al (2019) Modeling dust sources, transport, and radiative effects at different altitudes over the Tibetan Plateau. Atmos Chem Phys Discuss 1–47. https://doi.org/10.5194/acp-2019-431
Jin Q, Wei J, Yang Z (2014) Positive response of Indian summer rainfall to Middle East dust. Geophys Res Lett 41:4068–4074
Jish Prakash P, Stenchikov G, Kalenderski S et al (2015) The impact of dust storms on the Arabian Peninsula and the Red Sea. Atmos Chem Phys 15:199–222. https://doi.org/10.5194/acp-15-199-2015
Kedia S, Ramachandran S, Kumar A, Sarin MM (2010) Spatiotemporal gradients in aerosol radiative forcing and heating rate over Bay of Bengal and Arabian Sea derived on the basis of optical, physical, and chemical properties. J Geophys Res Atmos 115:1–17. https://doi.org/10.1029/2009JD013136
Kumar S, Devara PCS (2012) A long-term study of aerosol modulation of atmospheric and surface solar heating over Pune, India. Tellus, Ser B Chem Phys Meteorol 64:1–13. https://doi.org/10.3402/tellusb.v64i0.18420
Kwon EH, Sohn BJ, Smith WL, Li J (2012) Validating IASI temperature and moisture sounding retrievals over East Asia using radiosonde observations. J Atmos Ocean Technol 29:1250–1262. https://doi.org/10.1175/JTECH-D-11-00078.1
Lockwood JG (1988) Climate and climatic variability in semi-arid regions at low latitudes. In: Parry ML, Carter TR, Konijn NT (eds) The impact of climatic variations on agriculture, vol 2. Assessments in semi-arid regions. Springer, Netherlands, Dordrecht, pp 85–120
Menon S, Hansen J, Nazarenko L, Luo Y (2002) Climate effects of black carbon aerosols in China and India. Science (80- ) 297:2250–2253. https://doi.org/10.1126/science.1075159
Narayanan MS, Rao BM (1981) Detection of monsoon inversion by TIROS-N satellite. Nature 294:546–548. https://doi.org/10.1038/294546a0
Narayanan MS, Rao BM, Shah S et al (2004) Role of atmospheric stability over the Arabian Sea and the unprecedented failure of monsoon 2002. Curr Sci 86:938–947
Nguyen HD, Riley M, Leys J, Salter D (2019) Dust storm event of February 2019 in Central and East Coast of Australia and evidence of long-range transport to New Zealand and Antarctica. Atmosphere (Basel) 10:1–34. https://doi.org/10.3390/atmos10110653
Pandey SK, Vinoj V, Landu K, Babu SS (2017) Declining pre-monsoon dust loading over South Asia: signature of a changing regional climate. Sci Rep 7:1–10. https://doi.org/10.1038/s41598-017-16338-w
Pougatchev N, August T, Calbet X et al (2008) Validation of the IASI temperature and water vapor profile retrievals by correlative radiosondes. Earth Obs Syst XIII 7081:70810J. https://doi.org/10.1117/12.795382
Preethi B, Revadekar JV, Kripalani RH (2011) Anomalous behaviour of the Indian summer monsoon 2009. J Earth Syst Sci 120:783–794. https://doi.org/10.1007/s12040-011-0112-3
Rémy S, Benedetti A, Bozzo A et al (2015) Feedbacks of dust and boundary layer meteorology during a dust storm in the eastern Mediterranean. Atmos Chem Phys 15:12909–12933. https://doi.org/10.5194/acp-15-12909-2015
Ricchiazzi P, Yang S, Gautier C, Sowle D (1998) SBDART: a research and teaching software tool for plane-parallel radiative transfer in the earth’s atmosphere. Bull Am Meteorol Soc 79:2101–2114. https://doi.org/10.1175/1520-0477(1998)079%3c2101:SARATS%3e2.0.CO;2
Rotstayn LD, Keywood MD, Forgan BW et al (2009) Possible impacts of anthropogenic and natural aerosols on Australian climate: a review. Int J Climatol 29:461–479. https://doi.org/10.1002/joc.1729
Sathiyamoorthy V, Mahesh C, Gopalan K et al (2013) Characteristics of low clouds over the Arabian Sea. J Geophys Res Atmos 118:13489–13503. https://doi.org/10.1002/2013JD020553
Schlüssel P, Hultberg TH, Phillips PL et al (2005) The operational IASI Level 2 processor. Adv Sp Res 36:982–988
Seetha CJ, Mehta SK, Kakkanattu SP et al (2023) Characteristics of the atmospheric boundary layer during transient conditions of the Indian summer monsoon. Theor Appl Climatol. https://doi.org/10.1007/s00704-023-04578-y
Stull RB (1988) An introduction to boundary layer meteorology. Springer Science & Business Media
Swathi MS, Muraleedharan PM, Ramaswamy V et al (2018) Upper air thermal inversion and their impact on the summer monsoon rainfall over Goa – a case study. J Atmos Solar-Terrestrial Phys 169:37–44. https://doi.org/10.1016/j.jastp.2018.01.002
Tackett JL, Winker DM, Getzewich BJ et al (2018) CALIPSO lidar level 3 aerosol profile product: Version 3 algorithm design. Atmos Meas Tech 11:4129–4152. https://doi.org/10.5194/amt-11-4129-2018
Vinoj V, Satheesh SK, Moorthy KK (2010) Optical, radiative, and source characteristics of aerosols at Minicoy, a remote island in the southern Arabian Sea. J Geophys Res Atmos 115:1–19. https://doi.org/10.1029/2009JD011810
Vinoj V, Rasch PJ, Wang H et al (2014) Short-term modulation of Indian summer monsoon rainfall by West Asian dust. Nat Geosci 7:308–313
Wallace JM, Hobbs PV (2006) Atmospheric science: an introductory survey. Academic press, California, USA
Wenegrat JO, Thomas LN (2017) Ekman transport in balanced currents with curvature. J Phys Oceanogr 47:1189–1203. https://doi.org/10.1175/JPO-D-16-0239.1
Winker DM, Hunt WH, McGill MJ (2007) Initial performance assessment of CALIOP. Geophys Res Lett 34:1–5. https://doi.org/10.1029/2007GL030135
Winker DM, Vaughan MA, Omar A et al (2009) Overview of the CALIPSO Mission and CALIOP Data Processing Algorithms. J Atmos Ocean Technol 26:2310–2323. https://doi.org/10.1175/2009JTECHA1281.1
Wu CH, Wang SYS, Hsu HH (2018) Large-scale control of the Arabian Sea monsoon inversion in August. Clim Dyn 51:2581–2592. https://doi.org/10.1007/s00382-017-4029-7
Yang L, Shi Z, Sun H et al (2021) Distinct effects of winter monsoon and westerly circulation on dust aerosol transport over East Asia. Theor Appl Climatol 144:1031–1042. https://doi.org/10.1007/s00704-021-03579-z
Yu Y, Notaro M, Kalashnikova OV, Garay MJ (2016) Climatology of summer Shamal wind in the Middle East. J Geophys Res 121:289–305. https://doi.org/10.1002/2015JD024063
Acknowledgements
The first author (Sanjeev Dwivedi) is thankful to Science and Engineering Research Board (SERB), Department of Science & Technology (DST), Government of India, for providing a National Post-Doctoral Fellowship (PDF/2016/003854) at National Atmospheric Research Laboratory (NARL), Gadanki, IIT Bhubaneswar, for providing the facility and a Post-Doctoral Fellowship to carry out this work. The author is also thankful to Meteorological Centre, Bhubaneswar, for providing necessary support. The authors gratefully acknowledge the ARL for HYSPLIT, NOAA, and ECMWF and NCEP for providing model, satellite (IASI), and CALIPSO and reanalyzed data sets used in this study. We wish to thank T.V. Lakshmi Kumar, Kiranamayi Landu, Harish Gadhvi, K. Venkatesh, S. T. Akhil Raj, A. Aravindhavel, and K. Aruna for active discussions in the data analysis.
Funding
The first author is thankful to Science and Engineering Research Board (SERB), Department of Science & Technology (DST), Government of India, for providing a National Post-Doctoral Fellowship via grant number PDF/2016/003854.
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M. S. Narayanan conceived the idea and supervision. S. Dwivedi carried out analysis, methodology and conceptualization, and writing the original manuscript with subsequent input from all co-authors. A. Pandit compiled the dust analysis. Buddhi Prakash Jangid carried out SBDART analysis. D. Narayana Rao, V. Sathiyamoorthy, M. V. Ratnam, V. Yesubabu, and V. Vinoj are responsible for the discussion and supervision.
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Dwivedi, S., Pandit, A.K., Jangid, B.P. et al. Formation and maintenance of monsoon inversion over the Arabian Sea. Theor Appl Climatol 155, 2841–2856 (2024). https://doi.org/10.1007/s00704-023-04785-7
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DOI: https://doi.org/10.1007/s00704-023-04785-7