New Delhi, (Samajweekly) The coastal communities that are vulnerable to sea level rise due to climate change also have to worry about wave activity now. The extreme wind-wave pattern directly correlates with the location of extreme wind activity, scientists have said.
The regions over the Bay of Bengal, South China Sea and South Indian Ocean can experience higher wave activity in the future, posing a serious threat to coastal communities in the region, a recent study by Indian scientists has indicated.
These communities are already most vulnerable to the impact of climate change and other environmental drivers due to their exposure to severe inundation and its frequency associated with extreme water levels in the near shore regions apart from facing increasing instances of cyclones.
The impact resulting from coastal inundation can significantly affect the shoreline configuration, damage infrastructure, saltwater intrusion into groundwater, destruction of crops, and affect the human population with a range of socio-economic consequences. Scientists around the world are trying to estimate the magnitude of this impact, a release from the Ministry of Science & Technology said.
The present study performed a detailed investigation on future extreme wind-wave projections and its relationship with wind speed, sea level pressure, and sea surface temperature for the mid-and end-century under two different greenhouse gas emission scenarios projected by the Intergovernmental Panel on Climate Change (IPCC) called RCP4.5 and RCP8.5 (possible climatic conditions depending on different levels of global temperatures rise at that point in time)
An analysis of the projections have indicated maximum extreme wind and wave activity over the South Indian Ocean region during June-July-August and September-October-November. Regions over the central Bay of Bengal show extreme wind activity from the end-century projections, signifying the likelihood of more extreme events. Extreme wave heights are seen to intensify by about 1 m over the South Indian Ocean during the June-July-August months. An increase of 0.4 m in maximum significant wave heights are projected over regions in the North Indian Ocean, northwest Arabian Sea, northeast Bay of Bengal, and South China Sea.
A team of scientists, Athira Krishnan and Prasad K Bhaskaran from the Department of Ocean Engineering & Naval Architecture, IIT Kharagpur, jointly with Prashant Kumar, Department of Applied Sciences, National Institute of Technology, Delhi with support from the Department of Science & Technology, Government of India under the Climate Change Programme (CCP), carried out this study, which was published in the journal ‘Climate Dynamics’, Springer recently.
Findings from the study show that the projected change in wave heights are maximum for the South China Sea in RCP4.5, whereas the maximum rise is about 23 per cent in RCP8.5 by the end of the end-century. Also, the projected change in winds and waves over the western tropical Indian Ocean is consistent with changes in sea-level pressure variations and warm ocean temperatures. A significant increment in sea surface temperature is projected over the Arabian Sea during December-January-February and June-July-August months ranging between 1.5 and 2.0 degrees Celsius that is 0.5 degrees Celsius greater than the Bay of Bengal. Projections show that regions over the Gulf of Oman and Persian Gulf can experience higher warming rates exceeding 2 degrees Celsius under RCP8.5 by the end-century.
The team elaborates that the seasonal signatures in the extreme wind-wave patterns over the Indian Ocean directly correlate with the location of extreme wind activity. The end-century projections identified the hotspot locations of extreme wind activity over the central Bay of Bengal with magnitudes reaching 13-15 m/s, demarcating the likelihood of more extreme events in this region.
Projected changes during the mid-and end-century showed a dipole behaviour or seesaw effect having two distinct dipoles over the western and eastern regions in the tropical Indian Ocean belt. Regions in the northern, central, and eastern sectors of the Bay of Bengal, the southern part of the South China Sea, northern and western regions of the Arabian Sea, and eastern tropical Indian Ocean can witness changes ranging from 1-1.25 m by the end-century under the extreme RCP forcing scenario.
The new findings from this study are expected to augment more advanced research on extreme wind-wave activity for the North Indian Ocean region and also provide the scope for a detailed investigation on the possible linkages and teleconnection with climate indices in a changing climate.
