NABOS Project
Nansen and Amundsen Basins Observational System
Nansen and Amundsen Basins Observational System
The Arctic is undergoing significant changes, and the extensive modification of stratification that is associated with freshwater distribution is among the most prominent shifts that are taking place in the Arctic. To better understand these changes, our study investigates the impacts of a strong freshening event on oceanic stratification, heat fluxes, and currents in the eastern Eurasian Basin of the Arctic Ocean in 2015–2017. Our analysis of mooring observations revealed an excess of freshwater content by about 0.5m in the upper ~170m ocean. Tracer analysis showed that the main cause of this extraordinary freshening was the influx of riverine water from the Kara Sea through the Vilkitsky Straight (and, to a lesser extent, the Laptev Sea shelf) and reduced advection of saltier waters from St. Anna Trough. This freshening resulted in increased upper ocean stratification and weakened ventilation of the halocline. Furthermore, there was a three-to four-fold suppression of oceanic heat fluxes, which resulted in slower winter sea ice formation rates and lower summer sea ice melting rates in 2016 and 2017. One of the important ramifications of these changes was the weakening of total and near-inertial currents and shear in the upper ocean. My findings highlight the important role that extreme events may play in the Arctic's shift to a new climate state.
• Conducted a study of mortality data across eight stations in Ahmedabad during the summer of 2018.
• Investigating heat island effects using maximum temperature and PM2.5 correlations during the summer of 2018.
• Studied the variation of atmospheric total gaseous mercury (TGM) in Pune over three years (2015–2017) and its relationship with meteorological parameters.
• Performed air mass trajectory analysis using HYSPLIT back trajectory to identify potential sources of mercury emissions.