A watershed is all the land area that drains to a specific water resource, such as a lake or river. Watersheds range in size from a few square miles to an entire continent. There can be smaller watersheds within larger ones, such as VLAWMO being a small subset of the larger Mississippi River watershed. VLAWMO is divided into smaller sub watersheds, as seen below. As rainwater and melting snow run downhill, they carry sediment and other materials into streams, lakes, and groundwater.
96% of the land use within VLAWMO is urban, with a small agricultural area at the northern end. Because the urban landscape heavily changes the flow, drainage, and evaporation of the water cycle, our challenge is to create harmony between the two. Understanding how watersheds and wetlands work can help us live, work, and play in ways that benefit the water cycle.
While wetlands are present across North America, they are most abundant in the glacial terrain of the north-central US, as well as eastern and southern coastal regions. As seen in the map below, the greater Twin Cities Metro is within a heavily wetland region.
Within the water cycle, wetlands act as a sponge that slows the movement of water. While urban storm systems function with speed and efficiency to keep neighborhoods dry, a slow pace allows wetlands to filter water and recharge groundwater resources. Along with clean water, wetlands provide critical wildlife habitat for fish, birds, and insects. Fishing, hunting, and a variety of recreation benefit from healthy wetlands.
The long history of this landscape greatly shapes the conditions and challenges that we face today. Visit our waterbodies tab for more links and information on VLAWMO's wetlands.
Shallow lakes fall on a spectrum between deep lakes and wetlands. Unlike the deep lakes of Northern Minnesota where aquatic plants are found in a ring around the shoreline, shallow lakes contain plants over most of the lake bed. This is largely because sunlight reaches the bottom of shallow lakes, allowing plants to grow. This also influences lake temperature and the mixing of nutrients and sediment. While deep lakes turnover in the winter and mix nutrients as the water cools in the winter, shallow lakes are continually mixing throughout the summer. This creates a fragile environment that can sway between healthy and unhealthy depending on the management of the water.
Regions with shallow lakes and wetlands also coincide with shallow groundwater, also known as the water table. In transitionary regions such as central Minnesota and the Twin Cities (see diagram below), the water table is subject to dynamic changes depending on rainfall. Soils in our region respond to this ebb and flow of water, retaining its ability to act like a sponge. When exposed to saturation for long periods, soils become hydric and change their chemical composition. Even after decades of being dry, hydric soils will retain water rather than drain it when re-exposed to a high water table. With the complex, dynamic nature of wetland areas come the complexities of living with wetlands. Because concrete boundaries are difficult in transitionary wetland regions, buffers are a natural and helpful way to separate wetland and upland areas. Plants within a buffer help uptake the excess water in the soil, as well as gives space for flexibility and adaptability to changes in the water table.
As surface runoff and storm systems direct water into our shallow lakes and wetlands, there is a continual struggle for balance. In a healthy state, shallow lakes are abundant with fish, birds, plants, and clear water. With too much sediment and nutrients, they quickly become dominated by algae. This turbid state inhibits aquatic life and raises the risk for our long-term water resources. Helping our shallow lakes can be easy and fun with a community effort – visit our water conservation at home page to learn how you can be a part of a secure water future.