Abstract
Titli was the cataclysmic storm to afflict Indian coast during 2018. Tropical cyclones may inflate nutrients on the surface layer of the ocean by entrainment and mixing, as a result, the upper oligotrophic and euphotic layers may be recharged with rich nutrients resulting in triggering phytoplankton blooms and significant increase in primary production. The biological response using the chlorophyll concentration from Oceansat-2 OCM and the Net Primary Productivity from MODIS-A to this cyclone and its relation with the cyclone intensity has been studied. Role of physical oceanography parameters has been studied using multiple satellite-derived parameters like SST, TCHP, SLA, Ekman pumping velocity, wind stress and wind vectors and eddies during the passage of cyclone Titli. The results showed an increase in the surface chlorophyll concentration from 0.08 (before) to 0.32 mg m−3 (after), whereas NPP enhanced from 457 to 1313 mgC m−2 day−1 with an SST drop of ~2.58°C (30.25°–27.67°C). The study confirms that the physical parameters are the key components that influence the biological response in addition to the cyclone intensity.
Similar content being viewed by others
References
Banzon V, Thomas M S, Toshio M C, Liu C Y and William H 2016 A long-term record of blended satellite and in-situ sea-surface temperature for climate monitoring, modeling and environmental studies; Earth Syst. Sci. Data 8 165–176.
Behrenfeld M J and Paul G F 1997 Photosynthetic rates derived from satellite-based chlorophyll concentration; Limnol. Oceanogr. 42(1) 1–20.
Behrenfeld M J, Robert T O, David A S, Charles R M, Jorge L S, Gene C F, Allen J M, Paul G F, Ricardo M L and Emmanuel S B 2006 Climate-driven trends in contemporary ocean productivity; Nature 444(7120) 752–755.
Chaudhuri D, Debasis S, Eric D, Venkatesan R and Ravichandran M 2019 Response of the salinity-stratified Bay of Bengal to cyclone Phailin; J. Phys. Oceanogr. 49(5) 1121–1140.
Gierach M M and Subrahmanyam B 2008 Biophysical responses of the upper ocean to major Gulf of Mexico hurricanes in 2005; J. Geophys. Res. Oceans 113 (C4).
Hong X, Simon W C, Sethu R, Lynn K S and Richard H 2000 The interaction between Hurricane Opal (1995) and a warm core ring in the Gulf of Mexico; Mon. Weather Rev. 128(5) 1347–1365.
Huang S M and Lie-Yauw O 2015 Right-side cooling and phytoplankton bloom in the wake of a tropical cyclone; J. Geophys. Res. Oceans 120(8) 5735–5748.
IMD Report (2018) 2019 Report on cyclonic disturbances over north Indian Ocean during 2018; Indian Meteorological Department, Technical Report, pp. 178–204.
Kahru M, Paul C F, Gille S T, Manzano M and Mitchell B G 2007 Sea level anomalies control phytoplankton biomass in the Costa Rica Dome area; Geophys. Res. Lett. 34(22) L22601.
Large W G and Pond S 1981 Open ocean momentum flux measurements in moderate to strong winds; J. Phys. Oceanogr. 11 324–336.
Latha T P, Rao K H, Nagamani P V, Amminedu E, Choudhury S B, Dutt C B S and Dadhwal V K 2015 Impact of cyclone Phailin on chlorophyll-a concentration and productivity in the Bay of Bengal; Int. J. Geosci. 6(5) 473–480.
Lin I, Timothy L W, Chun‐Chieh W, George T F W, Chuanmin H, Zhiqiang C, Wen‐Der L, Yih Y and Kon‐Kee L 2003 New evidence for enhanced ocean primary production triggered by tropical cyclone; Geophys. Res. Lett. 30(13) 1718.
Ma Z, Fei J, Liu L, Huang X and Cheng X 2013 Effects of the cold core eddy on tropical cyclone intensity and structure under idealized air–sea interaction conditions; Mon. Weather Rev. 141(4) 1285–1303.
Mainelli M, Mark D, Lynn K S and Gustavo G 2008 Application of oceanic heat content estimation to operational forecasting of recent Atlantic category 5 hurricanes; Wea. Forecast. 23(1) 3–16.
Maneesha S and Behera M R 2015 Impact of SST on tropical cyclones in North Indian Ocean; Procedia Eng. 116 1072–1077.
Nagamani P V, Prakash C and Dwivedi R M 2008 Development of chlorophyll-a algorithm for ocean colour monitor onboard OCEANSAT-2 satellite; IEEE Geosci. Remote Sens. 5(3) 527–531.
Pessini F, Olita A, Cotroneo Y and Perilli A 2018 Mesoscale eddies in the Algerian Basin: Do they differ as a function of their formation site?; Ocean Sci. 14 669–688.
Premkumar K, Ravichandran M, Kalsi S R, Sengupta D and Sulochana G 2000 First results from a new observational system over the Indian seas; Curr. Sci. 78(3) 323–330.
Price J F, Weller R A and Pinkel R 1986 Diurnal cycling: Observations and models of the upper ocean response to diurnal heating, cooling, and wind mixing; J. Geophys. Res. Oceans 91(C7) 8411–8427.
Qiu Y, Han W, Lin X, West B J, Li Y, Xing W, Zhang X, Arulananthan K and Guo X 2019 Upper-ocean response to the super tropical cyclone Phailin (2013) over the freshwater region of the Bay of Bengal; J. Phys. Oceanogr. 49 1201–1228.
Rao K H, Smitha A and Ali M M 2006 A study on cyclone induced productivity in south-western Bay of Bengal during November–December 2000 using MODIS (SST and chlorophyll-a); Indian J. Mar. Sci. 35(2) 153–160.
Reynolds R W, Smith T M, Liu C, Chelton D B, Casey K S and Schlax M G 2007 Daily high-resolution-blended analyses for sea surface temperature; J. Clim. 20 5473–5496.
Roxy M K, Aditi M, Raghu M, Vinu V, Swapna P, Prasanna K S, Ravichandran M, Marcello V and Marina L 2016 A reduction in marine primary productivity driven by rapid warming over the tropical Indian Ocean; Geophys. Res. Lett. 43(2) 826–833.
Soong Y S, Jian-Hwa H, Chung-Ru H and Pearn P N 1995 Cold-core eddy detected in South China Sea; Eos Trans. AGU 76(35) 345–347.
Trenberth K E, Large W G and Olson J G 1990 The mean annual cycle in global ocean wind stress; J. Phys. Oceanogr. 20 1742–1760.
Vinayachandran P N and Mathew S 2003 Phytoplankton bloom in the Bay of Bengal during the northeast monsoon and its intensification by cyclones; Geophys. Res. Lett. 30(11) 1572.
Wada A and Norihisa U 2007 Importance of tropical cyclone heat potential for tropical cyclone intensity and intensification in the western North Pacific; J. Oceanogr. 63(3) 427–447.
Walker N D, Robert R L and Shreekanth B 2005 Hurricane‐forced upwelling and chlorophyll-a enhancement within cold‐core cyclones in the Gulf of Mexico; Geophys. Res. Lett. 32(18) L18610.
Zhao H, Shao J, Han G, Yang D and Lv J 2015 Influence of typhoon Matsa on phytoplankton chlorophyll-a off East China; PLoS one 10(9) e0137863.
Zhao H, Jiayi P, Guoqi H, Adam T D, Shuwen Z and Yijun H 2017 Effect of a fast-moving tropical storm Washi on phytoplankton in the northwestern South China Sea; J. Geophys. Res. Oceans 122(4) 3404–3416.
Acknowledgements
The authors are indebted to NICES of National Remote Sensing Centre, Hyderabad (ISRO) for providing OCM-2 and TCHP data. We owe to India Meteorological Department, New Delhi, for providing the cyclone track data and report. Also, we are thankful to NASA for MODIS-A data, NOAA for AVHRR data, CMEMS for merged altimeter datasets and ECMWRF for wind vector data.
Author information
Authors and Affiliations
Contributions
KVP: Conceptualization, methodology, data collection, software, visualization, making-inferences, writing-original draft preparation. ChSGV: Conceptualization, making-inferences, writing-original draft preparation. PVN and NKB: Conceptualization, methodology, making-inferences, supervision, reviewing and editing. SM: Conceptualization, methodology, making-inferences, software, visualization, writing-original draft preparation, TPL: Conceptualization, methodology, making-inferences, writing-original draft preparation, IVGB: Software, reviewing and editing, YUR: Software. ChSNP: Conceptualization, KS: Supervision, reviewing and editing and KPK: Supervision, reviewing and editing.
Corresponding author
Additional information
Communicated by Maripi Dileep
Appendix
Appendix
Rights and permissions
About this article
Cite this article
Vijay Prakash, K., Geetha Vimala, C.S., Nagamani, P.V. et al. Role of physical oceanography parameters in ocean’s biological response with the passage of cyclone Titli in the Bay of Bengal. J Earth Syst Sci 130, 123 (2021). https://doi.org/10.1007/s12040-021-01625-y
Received:
Revised:
Accepted:
Published:
DOI: https://doi.org/10.1007/s12040-021-01625-y