8. Analysis of impacts of lake-level management on wetland resources of Sebago Lake.


Based on available literature of wetland, FOSL believes the present lake level management plan may adversely affect Sebago Lake's wetlands. This contention is supported by a report titled, "Living with the Lakes: Challenges and Opportunities. A Progress Report to the International Joint Commission. July 1989" which states in part:

pp. 27-28 "There are many types of wetland configurations on the Great Lakes (Figure 16), but they share an immediate dependency on the actions of the lake levels for their cyclical transformations. Fluctuating water levels increase wildlife diversity. During high water periods, waterfowl, muskrats, terns and herons and many reptiles and amphibians flourish. Fish populations increase through their access to the lake from the spawning grounds provided in the wetlands. Low water levels allow for different populations, such as redwinged blackbirds, marsh wrens, rails, deer, rabbits and smaller mammals, to be nurtured. The important thing to note here is that neither flooded wetlands nor dry wetlands are most suitable to wildlife, but rather the changes themselves seem to be most effective in sustaining and balancing populations (Annex B Section 3.3)."

p.28 "The role of wetlands in water purification is also of critical importance in attempting to gain an overview of the interconnectedness of the elements of the natural ecosystem and the implications for human beings in the Basin. Recent studies have indicated that the role of the wetlands in water purification needs to be given serious consideration. Not only do the wetlands slow down the movement of sediments and thereby trap pollutants, but the plant life absorbs many of the more persistant pollutants, such as heavy metals. All these functions are, of course, in addition to the uses which humans make of the wetlands for sport, recreation, commercial activities and aesthetic enjoyment."

p. 28: "The relationship of water levels, wildlife and vegetation is the basis for the support of life in the Great Lakes Basin. Although not all aspects of this relationship are known and understood, it is clear that changes in any part of it will have very wide implications for the others. For some wildlife, such as migratory waterfowl, the wetlands of the Great Lakes are critical to their survival."

We do know that other lake wetlands in Maine have been altered by lake regulation. China Lake is one example. In the early 1970s China Lake regulation changed from a more naturally fluctuating regime to an increased lake level management with reduced annual water level fluctuation. Dramatic changes in wetland vegetation occurred, as evidenced in aerial photographs. Constant inundation of the wetlands adjacent to China Lake has eliminated the ability of the lake wetlands to dry out, preventing nutrients from being oxidized and safely reduced. The story of China Lake is available on the web site http://www.depu.org/

FOSL believes the present water level management has reduced the habitat values of Sebago Lake wetland. Sebago Lake wetlands need periods of drying out to allow organic nutrient oxidation and reduction. Natural, seasonal drying of the wetland bottom also serves to create more biodiversity and a more healthy wetland (Wilcox 1991,1992,1993, 1995). Many of the Sebago Lake wetlands under the present water level management will never be dry during the growing season. This is a great change for the Sebago Lake wetlands. FOSL requests the Commission review pertinent wetland literature and conduct an analysis of the impacts of lake level regulation on the ability of Sebago Lake wetlands to oxidize and filter out nutrients and prevent them from reaching the lake.

Normandeau Associates (1994) provided additional support for the importance of of natural water level fluctuations to the health and maintenance of Sebago Lake's wetlands:

p. 23: "Research on the Great Lakes and elsewhere has shown that fluctuating water levels play critical roles in developing and maintaining wetlands. Periodic flooding and drying maximizes the areal extent of the wetland development, increases diversity of wetland species and generally improves overall wetland value as habitat for fish and wildllife. Of course, the range, duration and periodicity of water level fluctuations are all important in influencing wetland development -- not all water level fluctuations are beneficial. However, it has been generally concluded that fluctuations that more or less duplicate natural fluctuations usually provide the greatest benefits and create wetlands of the greatest overall ecological value"

p.23-24: "On the Great Lakes, most of which are largely unregulated, it has been concluded that periodic water level fluctuation by as much as 2 meters (6 plus feet) are not only acceptable, but necessary to maintain riparian wetlands in their current state. Reductions in fluctuations, of either extreme highs or lows would be expected to result in negative impacts to the wetlands. As discussed previously, water level fluctuations on Sebago are similar to those on the Great Lakes when evaluated over 20 years or more. Therefore, it seems reasonable to assume that water level fluctuations on Sebago would be desirable and necessary to maximize wetland values. Although detailed wetland evaluations have not been made on Sebago, it is known that there are several hundred acres of wetlands associated with the lake (Pierce and Eldridge, 1992). Using the Great Lakes example, it seems logical to conclude that these wetlands have developed because of, not in spite of, historic water level fluctuations and that those fluctuations play an integral role in maintaining the wetlands in their current conditions. One might also conclude that a permanent reduction in the range of fluctuations could be expected to have negative impacts to the wetlands."

P.24: "Although the optimal range of fluctuations can only be determined by detailed study, we can apply the Great Lakes model to hypothesize a desirable range. On the Great Lakes, it was concluded that the minimum range of fluctuation should encompass the "exceeded 10% and 90% range." Figure 4-1 presents this model as applied to Sebago Lake. In evaluating this figure, it becomes immediately apparent that the hypothesized optimal range of water level fluctuations far exceeds the current operational strategy mediated by the Maine DEP, although maximum target ranges fairly closely approximate the 10% exceeded curve. This is particularly true in the spring, summer and fall when minimum target levels are consistently 2-3 feet higher than assumed desirable levels. From a wetlands perspective, one must tentatively conclude that continued management of Sebago Lake water levels within the MeDEP target ranges may result in long-term negative impacts to associated wetlands."

Normandeau Associates (1994) offered the following recommendations:

"3. At a minimum, Sebago Lake water level fluctuations should be within the historic 'exceeded 10% and 90% range to maximize wetland values.'
4. Both the 10% and 90% levels should be achieved at least once every 10-15 years, and probably in all seasons."

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