Abstract
A zonal dipole in the observed trends of wind speed and significant wave height over the Head Bay of Bengal region was recently reported in the literature attributed due to the variations in sea level pressure (SLP). The SLP in turn is governed by prevailing atmospheric conditions such as local temperature, humidity, rainfall, atmospheric pressure, wind field distribution, formation of tropical cyclones, etc. The present study attempts to investigate the inter-annual variability of atmospheric parameters and its role on the observed zonal dipole trend in sea level pressure, surface wind speed and significant wave height. It reports on the aspects related to linear trend as well as its spatial variability for several atmospheric parameters: air temperature, geopotential height, omega (vertical velocity), and zonal wind, over the head Bay of Bengal, by analyzing National Centers for Environmental Prediction (NCEP) Reanalysis 2 dataset covering a period of 38 years (1979–2016). Significant warming from sea level to 200 mb pressure level and thereafter cooling above has been noticed during all the seasons. Warming within the troposphere exhibits spatial difference between eastern and western side of the domain. This led to fall in lower tropospheric geopotential height and its east–west variability, exhibiting a zonal dipole pattern across the Head Bay. In the upper troposphere, uplift in geopotential height was found as a result of cooling in higher levels (10–100 mb). Variability in omega also substantiated the observed variations in geopotential height. The study also finds weakening in the upper level westerlies and easterlies. Interestingly, a linear trend in lower tropospheric u-wind component also reveals an east–west dipole pattern over the study region. Further, the study corroborates the reported dipole in trends of sea level pressure, wind speed and significant wave height by evaluating the influence of atmospheric variability on these parameters.
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References
Bhaskaran PK, Gupta N, Dash MK (2014) Wind-wave climate projections for the Indian Ocean from satellite observations. J Mar Sci Res Dev S11:1
Cagnazzo C, Claud C, Hare S (2006) Aspects of stratospheric long-term changes induced by ozone depletion. Clim Dyn 27:101–111. doi:10.1007/s00382-006-0120-1
Carnell R, Senior C (1998) Changes in mid-latitude variability due to increasing greenhouse gases and sulphate aerosols. Clim Dyn 14:369–383. doi:10.1007/s003820050229
D’Mello JR, Prasanna Kumar S (2016) Why is the Bay of Bengal experiencing a reduced rate of sea surface warming? Int J Climatol 36(3):1539–1548
Ding Y (1994), Monsoons over China. Kluwer Academy, Dordrecht
Fontaine B, Janicot S, Monerie P-A (2013) Recent changes in air temperature, heat waves occurrences, and atmospheric circulation in Northern Africa. J Geophys Res Atmos 118:8536–8552. doi:10.1002/jgrd.50667
Gupta N, Bhaskaran PK, Dash MK (2015) Recent trends in wind-wave climate for the Indian Ocean. Curr Sci 108(12):2191–2201
Hartmann DL, Wallace JM, Limpasuvan V, Thompson DW, Holton JR (2000) Can ozone depletion and global warming interact to produce rapid climate change. Proc Natl Acad Sci 97(4):1412–1417
Hu Y, Tung KK, Liu J (2005) A closer comparison of early and late-winter atmospheric trends in the Northern Hemisphere. J Clim 18:3204–3216
Kanamitsu M, Ebisuzaki W, Woollen J, Yang S-K, Hnilo JJ, Fiorino M, Potter GL (2002) NCEP-DOE AMIP-II Reanalysis (R-2). Bull Am Meteorol Soc 83:1631–1643
Kumar VS, Anoop TR (2015) Spatial and temporal variations of wave height in shelf seas around India. Nat Hazards 78(3):1693–1706
Kumar ED, Sannasiraj SA, Sundar V, Polnikov VG (2013) Wind-wave characteristics and climate variability in the Indian Ocean region using altimeter data. Mar Geodesy 36(3):303–318
Lee E, Sacks WJ, Chase TN, Foley JA (2011) Simulated impacts of irrigation on the atmospheric circulation over Asia. J Geophys Res 116:D08114. doi:10.1029/2010JD014740
McGregor GR, Nieuwolt S (1998) Tropical climatology: an introduction to the climate of the low latitudes, 2nd edn. Wiley, New York, p 352
Mitas CM, Clement A (2005) Has the Hadley cell been strengthening in recent decades? GeophysRes Lett 32:L03809. doi:10.1029/2004GL021765
Patra A, Bhaskaran PK (2016a) Temporal variability in wind–wave climate and its validation with ESSO-NIOT wave atlas for the head Bay of Bengal. Clim Dyn. doi:10.1007/s00382-016-3385-z
Patra A, Bhaskaran PK (2016b) Trends in wind-wave climate over the head Bay of Bengal region. Int J Climatol 36:4222–4240
Qian W, Wu K, Leung JC-H, Shi J (2016) Long-term trends of the Polar and Arctic cells influencing the Arctic climate since 1989. J Geophys Res Atmos. doi:10.1002/2015JD024252
Schwendike J, Berry GJ, Reeder MJ, Jakob C, Govekar P, Wardle R (2015) Trends in the local Hadley and local Walker circulations. J Geophys Res D Atmos 120:7599–7618
Shanas PR, Kumar VS (2015) Trends in surface wind speed and significant wave height as revealed by ERA-Interim wind wave hindcast in the Central Bay of Bengal. Int J Climatol 35(9):2654–2663
Sreekala PP, Rao SVB, Arunachalam MS, Harikiran C (2014) A study on the decreasing trend in tropical easterly jet stream (TEJ) and its impact on Indian summer monsoon rainfall. Theor Appl Climatol 118:107–114
Steenburgh WJ, Holton JR (1993) On the interpretation of geopotential height tendency equations. Mon Weather Rev 121(9):2642–2645
Ulbrich U, Christoph M (1999) A shift of the NAO and increasing storm track activity over Europe due to anthropogenic greenhouse gas forcing. Clim Dyn 15:551–559. doi:10.1007/s003820050299
Wallace JM, Thompson DW (2002) Annular modes and climate prediction. Phys Today 55(2):28
Wang H, Murtugudde R, Kumar A (2016) Evolution of Indian Ocean dipole and its forcing mechanisms in the absence of ENSO. Clim Dyn 47(7–8):2481–2500
Watson RT, Zinyowera MC, Moss RH (1997) The regional impacts of climate change: an assessment of vulnerability. Cambridge University Press, Cambridge, p 517
Zhang L, Li T (2016) Relative roles of differential SST warming, uniform SST warming and land surface warming in determining the Walker circulation changes under global warming. Clim Dyn. doi:10.1007/s00382-016-3123-6
Acknowledgements
The authors sincerely thank the Ministry of Human Resources Development (MHRD), Government of India for the financial support. This study is conducted as a part of the Mega Project “Future of Cities” under the module ‘Effect of Climate change on local sea level rise and its impact on coastal areas: Kolkata region as a pilot study’ supported by MHRD at IIT Kharagpur. The authors also thank the anonymous reviewers for their critical comments and suggestion that improved the overall scientific quality of this article.
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382_2017_3892_MOESM1_ESM.jpeg
Figure-S1: Linear trend (shaded) and climatology (black lines) of u wind (m) at 100 mb for monsoon season during 1992-2012. Significant trends at 95% level are indicated by dots. (JPEG 5438 KB)
382_2017_3892_MOESM2_ESM.jpeg
Figure-S2: Longitude-height cross sections of streamlines (u; -omega*200) at 20°N during monsoon: (a) 1992, (b) 1997, and (c) 2012. (JPEG 3089 KB)
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Patra, A., Bhaskaran, P.K. & Jose, F. Time evolution of atmospheric parameters and their influence on sea level pressure over the head Bay of Bengal. Clim Dyn 50, 4583–4598 (2018). https://doi.org/10.1007/s00382-017-3892-6
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DOI: https://doi.org/10.1007/s00382-017-3892-6