A very severe cyclonic storm, Hudhud, made landfall at Visakhapatnam city, the central east coast of India, on 12 October 2014 and it is the most destructive cyclone to ever hit the Indian subcontinent since the past two decades. In order to examine its impact on the flux of trace gases into the atmosphere, a study was made in the coastal Bay of Bengal, off Visakhapatnam, after the cyclone and compared with the pre-cyclone conditions. Hudhud suppressed the vertical mixing of the water column due to the occurrence of strong salinity stratification associated with torrential rainfall. The land run-off and precipitation brought significant amount of ammonium to the coastal waters, resulting in increased pH. The increased pH shifted the inorganic carbon equilibrium towards the formation of bicarbonate, resulting in decreased partial pressure of carbon dioxide (pCO$_{2}$) after the cyclone Hudhud. The undersaturation of carbon dioxide (CO$_{2}$) and nitrous oxide (N$_{2}$O) with respect to atmospheric equilibrium was observed during the post-cyclone period compared to the pre-cyclone period. About 80% of the post-cyclone decrease in N$_{2}$O (>2 nM)) and pCO$_{2}$ (150–200 $\mu$ atm) was contributed by the dilution of coastal waters with the precipitated waters. In contrast, methane (CH$_{4}$) concentrations were increased by 0.5–2.8 nM during the post-cyclone period than in the pre-cyclone period, and were attributed to the input of domestic sewage through land run-off. Dimethyl sulphide (DMS) and the total dimethyl sulphonio-propionate (DMSP$_{t}$) concentrations decreased by 0.4–3.9 and 0.2–6.0 nM, respectively, during the post-cyclone period in comparison with the pre-cyclone period and it was consistent with lower phytoplankton biomass during the former than the latter. The sea-to-air flux of CO$_{2}$, N$_{2}$O and DMS were 1.3 $\pm$ 0.5 mmol C m$^{-2}$d$^{-1}$, 0.9 $\pm$ 0.3 $\mu$ mol m$^{-2}$ d$^{-1}$ and 5.8 $\pm$ 3 $\mu$ mol m$^{-2}$ d$^{-1}$ during the pre-cyclone period, respectively. The corresponding values during the post-cyclone period were lower at $-$2.0 $\pm$ 1 mmol C m$^{-2}$ d$^{-1}$, $-$0.4 $\pm$ 0.1 $\mu$ mol m$^{-2}$ d$^{-1}$ and 2.8 $\pm$ 2 $\mu$ mol m$^{-2}$ d$^{-1}$, respectively. In contrast, the sea-to-air flux of CH$_{4}$ increased from 0.6 to 1.5 $\mu$ mol C m$^{-2}$ d$^{-1}$ from the pre- to the post-cyclone period. This study suggested that the cyclone Hudhud modified the magnitude of the biogenic gas flux to the atmosphere from the coastal Bay of Bengal than hitherto hypothesised.

Tropical cyclones generally enhance biological production due to the increase in nutrients input due to vertical mixing. In contrast, the very severe cyclonic storm (VSCS)Hudhud decreased primary production due to the strong stratification associated with torrential rainfall and high suspended load from the major city where the cyclone made landfall. The study region received nutrients from the cold core eddy and coastal upwelling in the offshore and inshore regions, respectively, during pre-cyclone period and the same was suppressed under the influence of cyclonic winds led to convergence by shoreward Ekman transport. The land run-off brought nutrients to the coast during cyclone Hudhud; however, their concentrations were less than that during other cyclones (Orissa supercyclone, Sidr and Phailin). Such low nutrient levels resulted from the VSCS Hudhud crossing the urban region (Visakhapatnam city) whereas other cyclones crossed the coast over fertile agricultural lands which led to high nutrients input associated with phytoplankton blooms. Therefore, the biological response to a cyclone not only depends on the intensity of the cyclone but also on the region of the land it crosses.