Glenn Hodgkins
Glenn Hodgkins is a Research Hydrologist with the New England Water Science Center.
Glenn's work in recent years has focused on statistical hydrology at the regional, national, and international scale, primarily on the analysis of change and variability of historical streamflow and groundwater, and also on probabilistic forecasting and model evaluation. Glenn is the lead author or co-author on 28 peer-reviewed articles in hydrology and climate journals and 31 USGS scientific reports.
Professional Experience
Research Hydrologist, U.S. Geological Survey, New England Water Science Center, 2014 to Present
Hydrologist, U.S. Geological Survey, New England Water Science Center, 1994 to 2014
Hydrologist, U.S. Geological Survey, Indiana Water Science Center, 1990 to 1994
Education and Certifications
M.S. Engineering, Purdue University, 1995
B.S. Civil Engineering, University of Maine, 1990
Science and Products
Modeled future peak streamflows in four coastal Maine rivers
Modeled future peak streamflows in four coastal Maine rivers
Historical groundwater trends in northern New England and relations with streamflow and climatic variables
Reference hydrologic networks II. Using reference hydrologic networks to assess climate-driven changes in streamflow
Reference hydrologic networks I. The status and potential future directions of national reference hydrologic networks for detecting trends
Relations between winter climatic variables and April streamflows in New England and implications for summer streamflows
Watershed scale response to climate change--Cathance Stream Basin, Maine
Historical summer base flow and stormflow trends for New England rivers
River base flow is important to aquatic ecosystems, particularly because of its influence on summer water temperatures. Summer (June through September) daily mean streamflows were separated into base flow and stormflow components by use of an automated method at 25 stations in the New England region of the United States that drain predominantly natural basins. Summer monthly mean base flows increa
Quantifying effects of climate change on the snowmelt-dominated groundwater resources of northern New England
Historical ice-out dates for 29 lakes in New England, 1807-2008
Historical changes in annual peak flows in Maine and implications for flood-frequency analyses
Historical changes in annual peak flows in Maine and implications for flood-frequency analyses
Science and Products
Modeled future peak streamflows in four coastal Maine rivers
Modeled future peak streamflows in four coastal Maine rivers
Historical groundwater trends in northern New England and relations with streamflow and climatic variables
Reference hydrologic networks II. Using reference hydrologic networks to assess climate-driven changes in streamflow
Reference hydrologic networks I. The status and potential future directions of national reference hydrologic networks for detecting trends
Relations between winter climatic variables and April streamflows in New England and implications for summer streamflows
Watershed scale response to climate change--Cathance Stream Basin, Maine
Historical summer base flow and stormflow trends for New England rivers
River base flow is important to aquatic ecosystems, particularly because of its influence on summer water temperatures. Summer (June through September) daily mean streamflows were separated into base flow and stormflow components by use of an automated method at 25 stations in the New England region of the United States that drain predominantly natural basins. Summer monthly mean base flows increa