Shale Hills, GRAD STUDENT
Shale Hills, COLLABORATOR, GRAD STUDENT
Shale Hills, INVESTIGATOR
The Susquehanna River Basin (SRB) lies in the northeastern United States and contains a mosaic of wetlands that are susceptible to future climate change. This study develops a coupled surface-subsurface modeling framework to assess the prospects for SRB wetlands under modified hydrologic processes induced by climate change. We selected seven watersheds ranging in size from 163 to 902 km2: Kettle Creek, Young Womans Creek, Little Juniata River, Shaver’s Creek, Mahantango Creek, Muddy Creek, and Lackawanna River. These watersheds represent the major landscapes of the SRB. We explored the broad spatial and temporal patterns across these watersheds between climate and wetland water levels by applying a coupled surface-subsurface model: Penn State Integrated Hydrologic Model with 7-year hourly weather records from the North-American Land Data Assimilation System. In the model calibration, we employed both streamflow and the spatial distribution of wetlands to constrain the model parameters. The possible effects of climate change on wetland hydrology were investigated by creating historical and future climate scenarios based on the output of one global climate model from phase 3 of the Coupled Model Intercomparison Project. We selected the best climate model based on historical performance to force the PIHM simulation of historical and future scenarios. The hydrologic scenarios suggested that water tables would fall, with greater declines in upland regions than in wetland areas. The key to this study is that a high-resolution spatial and temporal model can resolve the heterogeneous wetland dynamics in the context of distributed mesoscale watershed modeling.
Yu Xuan, Gopal Bhatt, Christopher Duffy, Denice Wardrop, Raymond Najjar, Andrew Ross, Matthew Rydzik (2015): A coupled surface-subsurface modeling framework to assess the impact of climate change on freshwater wetlands: a case study of seven watersheds of the Susquehanna River Basin. Climate Research, 66:211-228. DOI: 10.3354/cr01348
This Paper/Book acknowledges NSF CZO grant support.