Recent Status and Long-Term Trends in Freshwater Discharge and Nutrient Inputs

Anthropogenic inputs of nutrients via river runoff are the primary drivers of ecosystem degradation inChesapeake Bay (CB) and the northern Adriatic Sea (NAS). The annual cycle of river flow is typically unimodalin CB (seasonal peak during spring) and bimodal in the NAS (peaks during April-June and October-December).Dissolved inorganic nitrogen accounts for most of the total nitrogen (TN) in both systems. During 1985-2015,annual loads of TN to CB tended to decrease while total phosphorus (TP) loads tended to increase. In contrast,annual loads of TN to the NAS tended to increase while TP loads tended to decrease. However, these annualinput trends were significant only for dissolved inorganic P in the NAS, whereas in the case of N they weremasked by interannual changes of the runoff. Climate-driven changes in the water cycle may bring new challengesof controlling nutrient loading in CB, where annual rainfall is expected to increase. In contrast, annualrainfall is projected to decrease in the NAS region, which would aid efforts to control nutrients. An additionalchallenge unique to CB is the filling up of Conowingo Reservoir on the Susquehanna River, which resulted inincreased P and sediment loads due to reduced trapping efficiency.