Northland College, Wisconsin
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Affiliated Works
sorted by decreasing year, and then by display-name
- Methane Emissions and Warming Potentials of Wetlands of the Great Lakes Region
- Title: Interannual variability in the temperature-responsiveness of CO2 flux from forest and peatland soils
- ENSO & NAO Impacts on Intra-Seasonal Temperature Variability in United States Winters
- Interactions between Langmuir turbulence and submesoscale eddies
- Place-based research project design for 10-week REU and two-week "mini-REU" internships using lake sediment cores
- Predicting Species-environment Relationships with Functional Traits for the Understory Flora of Wisconsin
- A new estimate of climate sensitivity using Last Glacial Maximum model-data constraints that includes parametric, feedback, and proxy uncertainties
- Determining Deglacial Climate from δ<SUP>18</SUP>O - The GISS-E2-rosetta
- Did the Laurentide ice sheet survive through Marine Isotope Stage 9?
- Eastward routing of glacial Lake Agassiz runoff caused the Younger Dryas cold event
- Advancing Graduate Limnology Education through Active Learning and Community Partnerships: A Pilot Program at the Large Lakes Observatory
- Climate influence on Susquehanna River streamflow dynamics
- Exploring the Mass Balance and Sea Level Contribution of Global Glaciers During the Last Interglaciation and Mid-Holocene
- Laurentide Ice-Sheet Meltwater Sources to the Gulf of Mexico During the Last Deglaciation: Assessing Data Reconstructions Using Water Isotope Enabled Simulations
- Lichen biogeochemical and spatial dynamics in canopies of Eastern white pine (Pinus strobus)
- The Forest Canopy as a Temporally and Spatially Dynamic Ecosystem: Preliminary Results of Biomass Scaling and Habitat Use from a Case Study in Large Eastern White Pines (Pinus Strobus)
- Water Source and Isotope changes through the Deglaciation and Holocene
- Deglaciation of the Huron Mountains in Northern Michigan and the Implications for Continental Meltwater Routing
- Establishing a New Chronology of Glacial Lake Duluth and its Implications for Ice Sheet Retreat in the Lake Superior Basin
- Using Last Glacial Maximum proxy data and a large ensemble of climate simulations to constrain an estimate of equilibrium climate sensitivity