a b s t r a c tClimate change is expected to alter coastal ecosystems in ways which may have predictable consequences for the seasonality and geographical distribution of human pathogens and harmful algae. Here we demonstrate relatively simple approaches for evaluating the risk of occurrence of pathogenic bacteria in the genus Vibrio and outbreaks of toxin-producing harmful algae in the genus Alexandrium, with estimates of uncertainty, in U.S. coastal waters under future climate change scenarios through the end of the 21st century. One approach forces empirical models of growth, abundance and the probability of occurrence of the pathogens and algae at specific locations in the Chesapeake Bay and Puget Sound with ensembles of statistically downscaled climate model projections to produce first order assessments of changes in seasonality. In all of the case studies examined, the seasonal window of occurrence for Vibrio and Alexandrium broadened, indicating longer annual periods of time when there is increased risk for outbreaks. A second approach uses climate model projections coupled with GIS to identify the potential for geographic range shifts for Vibrio spp. in the coastal waters of Alaska. These two approaches could be applied to other coastal pathogens that have climate sensitive drivers to investigate potential changes to the risk of outbreaks in both time (seasonality) and space (geographical distribution) under future climate change scenarios. Ó 2015 Published by Elsevier B.V. This is an open access article under the CC BY-NC-ND license (http://creativecommons.org/licenses/by-nc-nd/4.0/).
IntroductionThe most recent assessment by the Intergovernmental Panel on Climate Change provided unequivocal evidence for warming of the climate system. Emissions of greenhouse gases from human activities are the highest in history, and have caused unprecedented warming (IPCC, 2014). During the period from 1880 to 2012, mean global land surface air temperatures have increased by 0.85°C with a greater rate of change in the period from 1970 to present (IPCC, 2014). Similarly, over the last four decades, surface waters of our oceans have warmed at a rate of 0.11°C per decade, and alterations in precipitation patterns have increased salinity in the Atlantic Ocean and decreased salinity in the Pacific and Southern Oceans (IPCC, 2014). From 1901 to 2010, mean global sea level has risen 0.19 m and the rate of ice loss from glaciers around the http://dx.