National Oceanic and Atmospheric Administration (NOAA)

Also collaborating on these NE CSC projects

Climate change impacts on erosion, mass wasting, and the supply of sediment to tidal wetlands in the Northeast

Climate change is likely to impact erosion rates, the magnitude and frequency of extreme rainfall/mass wasting events, and the accumulation of sediment in coastal areas. However, long-term rates of erosion and sediment delivery to coastal systems are poorly constrained and there is limited understanding of the relative effects of climate change versus land-use change on these processes.

Predicting the fate and impact of watershed nutrient loads as Lake Michigan's hydrodynamics shift under climate change

Climate change is shifting the hydrodynamics and temperature of both the Great Lakes and their tributary rivers.  Both hydrology and temperature may play potent roles in mediating the magnitude of watershed nutrient load and their fate upon reaching the lake.  Tributary hydrology reflects the source of water (groundwater vs surface runoff) and seasonal timing of discharge, while tributary temperature determines the density difference between river and lake water.  Similarly, mixing patterns in these massive lakes strongly influence whether tributary loads remain near the shore or become dil

Determining the Skill and Value of Incorporating Streamflow Forecasts into an Early Drought Detection System

This research investigates forecast skill in predicting the onset and severity of drought.  One of the unique features of NECASC research agenda is the active engagement of major a number of water supply utilities and an evaluation of how climate informed short-term streamflow forecasts and longer-range climate change forecasts influence the water supply systems.

Development of Dynamically-Based 21st Century Projections of Snow, Lake Ice, and Winter Severity for the Great Lakes Basin to Guide Wildlife-Based Adaptation Planning, with Emphasis on Deer and Waterfowl

Our project focused on anticipated effects of 21st century climate change on winter severity, snowpack, and lake ice across the Great Lakes Basin and the response of wildlife populations, namely white-tailed deer and dabbling ducks. Winter conditions have changed substantially since the mid-20th century, with rising temperatures, declining lake ice cover, and increased lake-effect snowfall. Nonetheless, due coarse resolution, poor lake representation, and insufficient treatment of lake-effect processes in global climate models, basinwide climate change projections remain uncertain.

Impacts of sea level rise on ecosystems

A reconnaissance study distinguishes coastal areas of the northeastern U.S. (approx. Virginia to Maine) that will experience an inundation-dominated response to sea-level rise from those that will respond dynamically due to physical and bio-physical sedimentation and erosion processes. Areas that will be dominated by inundation include urban regions of intense development and/or coastal engineering, as well as bedrock coasts. Areas that will respond dynamically include beaches, unconsolidated cliffs, barrier islands, and wetlands.

Assessing climate change projections over the Northeast

Using Coupled Model Intercomparison Project Phase 5 (CMIP5) and CMIP3 data, we are developing a range of projections for the Eastern U.S.  We are also developing extreme event projections for stakeholder-relevant metrics (e.g., days over 90 °F, days below 32 °F, and days with over 1 inch of precipitation) based on CMIP5 models and North American Regional Climate Change Assessment Program (NARCCAP) dynamical downscaling.

Subscribe to National Oceanic and Atmospheric Administration (NOAA)