Climate Change Impacts on Local Flood Risks in the U.S. Northeast: A Case Study on the Connecticut and Merrimack River Basins

摘要

This study investigates the potential impacts of climate change on future flows in the main stem of the Connecticut and Merrimack rivers within Massachusetts. The study applies two common climate projections based on (Representative Concentration Pathways), RCP 4.5 and RCP 8.5 and downscaled gridded climate projections from 14 global climate models (GCMs) to estimate the 100-year, 24-h extreme precipitation events for two future time-periods: near-term (2021-2060) and far-term (2060-2099). 100-year 24-h precipitation events at near- and far-term are compared to GCM-driven historical extreme precipitation events during a base period (1960-1999) and results for RCP 8.5 scenario show average increases between 25%-50% during the near-term compared to the base period and increases of over 50% during the far-term. Streamflow conditions are generated with a distributed hydrological model where downscaled climate projections are used as inputs. For the near-term, the medians of the GCMs using the RCP 4.5 and RCP 8.5 suggest 2.9%-8.1% increases in the 100-year, 24-h flow event in the Connecticut and an increase of 9.9%-13.7% in the Merrimack River. For the far-term, the medians of the GCMs using the RCP 4.5 and RCP 8.5 suggest a 9.0%-14.1% increase in the Connecticut and 15.8%-20.6% for the Merrimack River. Ultimately, the results presented here can be used as a guidance for the long-term management of infrastructures on the Connecticut and Merrimack River floodplains.