Green Lake is the deepest natural inland lake in Wisconsin. Through time its water quality has degraded, with relatively high phosphorus concentrations and zones of hypoxia. This project is quantifying the water quality of the lake and its tributaries, and it will provide information to help guide efforts to improve the lake.
Green Lake is the deepest natural inland lake in Wisconsin. The lake’s watershed includes the cities of Ripon and Green Lake and is dominated by agriculture. The lake was oligotrophic with very good water quality in the early 1900s. But several factors have led to degradation in its water quality, including changes in land use and climate. These changes resulted in increased nutrient loading, which may have caused increased phosphorus concentrations and hypoxic conditions in both the metalimnion and hypolimnion of the lake.
Objectives
The goals of this study are to: 1) describe water quality in Green Lake, especially metalimnetic and hypolimnetic hypoxia; 2) describe what factors have caused the degradation in water quality using eutrophication models; 3) quantify how reductions in nutrient loading should improve the water quality of the lake (reductions in phosphorus, algae, and reduction in metalimnetic and hypolimnetic hypoxia) using the eutrophication models; and 4) provide information to help guide actions to reduce the nutrient loading, improve the water quality, and remove the lake from the State's impaired waters list.
Approach
Automated stream monitoring techniques are being used to collect streamflow, and phosphorus, nitrogen concentrations in four main tributaries to the lake. Phosphorus loading is being estimated with GCLAS. Standard limnological procedures are being used to monitor water quality in the lake. The Canfield Bachman eutrophication model is being used to determine load reductions needed to reduce the phosphorus concentrations in the lake. The hydrodynamic/water quality GLM/AED model is being used to describe the hydrodynamic, chemical, and biological processes that lead to the hypoxia, and what type of nutrient reductions are needed to reduce it.
Below are data associated with this project.
Eutrophication models to simulate changes in the water quality of Green Lake, Wisconsin in response to changes in phosphorus loading, with supporting water-quality data for the lake, its tributaries, and atmospheric deposition
Response of Green Lake, Wisconsin, to changes in phosphorus loading, with special emphasis on near-surface total phosphorus concentrations and metalimnetic dissolved oxygen minima
Appendix E. Water quality and hydrology of Green Lake, Wisconsin, and the response in its near-surface water-quality and metalimnetic dissolved oxygen minima to changes in phosphorus loading
Below are web tools associated with this project.
Below are partners associated with this project.
- Overview
Green Lake is the deepest natural inland lake in Wisconsin. Through time its water quality has degraded, with relatively high phosphorus concentrations and zones of hypoxia. This project is quantifying the water quality of the lake and its tributaries, and it will provide information to help guide efforts to improve the lake.
Map of Green Lake, Wisconsin, and its watershed, with sampling data. Green Lake is the deepest natural inland lake in Wisconsin. The lake’s watershed includes the cities of Ripon and Green Lake and is dominated by agriculture. The lake was oligotrophic with very good water quality in the early 1900s. But several factors have led to degradation in its water quality, including changes in land use and climate. These changes resulted in increased nutrient loading, which may have caused increased phosphorus concentrations and hypoxic conditions in both the metalimnion and hypolimnion of the lake.
Objectives
The goals of this study are to: 1) describe water quality in Green Lake, especially metalimnetic and hypolimnetic hypoxia; 2) describe what factors have caused the degradation in water quality using eutrophication models; 3) quantify how reductions in nutrient loading should improve the water quality of the lake (reductions in phosphorus, algae, and reduction in metalimnetic and hypolimnetic hypoxia) using the eutrophication models; and 4) provide information to help guide actions to reduce the nutrient loading, improve the water quality, and remove the lake from the State's impaired waters list.
Dissolved oxygen profiles in Green Lake, WI, demonstrating metalimnetic and hypolimnetic hypoxia in 2017. Approach
Automated stream monitoring techniques are being used to collect streamflow, and phosphorus, nitrogen concentrations in four main tributaries to the lake. Phosphorus loading is being estimated with GCLAS. Standard limnological procedures are being used to monitor water quality in the lake. The Canfield Bachman eutrophication model is being used to determine load reductions needed to reduce the phosphorus concentrations in the lake. The hydrodynamic/water quality GLM/AED model is being used to describe the hydrodynamic, chemical, and biological processes that lead to the hypoxia, and what type of nutrient reductions are needed to reduce it.
- Data
Below are data associated with this project.
Eutrophication models to simulate changes in the water quality of Green Lake, Wisconsin in response to changes in phosphorus loading, with supporting water-quality data for the lake, its tributaries, and atmospheric deposition
In this data release, we provide data to describe the water quality in Green Lake, Wisconsin, from 1905 to 2020, primarily the constituents for which it is impaired, including near-surface total phosphorus concentrations and metalimnetic dissolved oxygen concentrations, and quantify the water and phosphorus inputs to the lake. We also provide inputs to and outputs from the General Lake Model coupl - Publications
Response of Green Lake, Wisconsin, to changes in phosphorus loading, with special emphasis on near-surface total phosphorus concentrations and metalimnetic dissolved oxygen minima
Green Lake is the deepest natural inland lake in Wisconsin, with a maximum depth of about 72 meters. In the early 1900s, the lake was believed to have very good water quality (low nutrient concentrations and good water clarity) with low dissolved oxygen (DO) concentrations occurring in only the deepest part of the lake. Because of increased phosphorus (P) inputs from anthropogenic activities in itAppendix E. Water quality and hydrology of Green Lake, Wisconsin, and the response in its near-surface water-quality and metalimnetic dissolved oxygen minima to changes in phosphorus loading
Green Lake is the deepest natural inland lake in Wisconsin, USA, with a maximum depth of about 72 meters (m). In the early 1900’s, the lake was believed to have very good water quality (low nutrient concentrations and good water clarity), with low dissolved oxygen (DO) concentrations only in the deepest part of the lake. Because of increased phosphorus (P) inputs from anthropogenic activities in i - Web Tools
Below are web tools associated with this project.
- Partners
Below are partners associated with this project.