Great Lakes hydroclimate extremes variability

Started in 2024

This project focuses on understanding the response of the Great Lakes’ ice cover and thermal structure to past and future climate variability using a physics-based modeling approach. A three-dimensional hydrodynamic-ice model was developed using the Finite Volume Community Ocean Model (FVCOM), configured specifically for the Great Lakes system. The model is forced with the ERA5 reanalysis dataset and is used to simulate lake dynamics at high spatial and temporal resolution. By reconstructing historical conditions, the model enables detailed analysis of extreme events such as lake heatwaves and cold-spells, and the factors that impacts them like air temperature, ice cover anomalies, and lakes characteristics (missing reference). This work provides a physically grounded framework for examining how climate change has shaped, and is likely to continue shaping, the thermal and cryospheric behavior of large lake systems.

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Modeled surface temperature for all Great Lakes from 1941 to 2021

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Lake surface temperature detrending and extremes calculation framework. (a) Schematic showing the effect of data detrending. b, c, d, and e show the steps used to obtain the distribution of the detrended lake surface temperature (DLST). (b) modeled lake surface temperature (LST) for all lakes. (c) Example lake-wide average surface temperature for Lake Michigan with the detected nonlinear trend. (d) The resulting DLST. (e) The change in the DLST distribution with time.

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