2015 Valley Branch Watershed District Watershed Management Plan Goose Lake Watershed Management Plan
Barr Engineering Company Page 5.29-7
P:\Mpls\23 MN\82\2382174\WorkFiles\2015 VBWD Plan\Final\Section 5.29 - Goose Lake.doc
Purple loosestrife was found along the south basin’s shore on all sides of the lake during the 2003 ,
2009, and 2012 surveys. Once a waterbody becomes infested with purple loosestrife, the plant
typically replaces native vegetation and rapidly becomes the sole emergent species.
Purple loosestrife can be effectively managed through the use of leaf-eating beetles, which reduce
plant growth and seed production by feeding on the leaves and new shoots. The VBWD may consider
partnering with the MDNR to introduce leaf-eating beetles to the purple loosestrife areas along the
lake’s shore to control purple loosestrife.
Curlyleaf pondweed (CLP) was found throughout the south basin’s periphery during June 2003, in
two locations, east and southwest sides of the lake, during August 2003, and at many points around
the south basin in June 2012. Plant densities were light to moderate during all surveys. Once a lake
becomes infested with curlyleaf pondweed, this plant typically displaces native vegetation, thereby
increasing its coverage and density. Curlyleaf pondweed begins growing in late August, grows
throughout the winter at a slow rate, grows rapidly in the spring, and dies in early summer. Native
plants that grow from seed in the spring are unable to grow in areas already occupied by CLP, and
are replaced by this plant. Elodea (Elodea Canadensis) and coontail (Ceratophyllum demersum),
species that overwinter, may limit curlyleaf pondweed increases in coverage and density in the south
basin of Goose Lake. Because CLP densities are light and overwintering native species may control
the spread of this plant, the proposed strategy for dealing with CLP in Goose Lake is monitoring its
population and instituting active management techniques only if its density or dominance of native
species becomes problematic.
5.29.3 Water Quantity
Goose Lake has a high overflow at Elevation 931.7 (1992 VBWD survey, NGVD29 datum). The
MDNR’s Ordinary High Water level (OHW) for Goose Lake is at Elevation 924.4 (NGVD29 datum).
At water levels above Elevation 931.7, water from Goose Lake will flow north in a ravine which
leads to Eagle Point Lake. Before Goose Lake reaches its overflow elevation, 10th Street North
(CSAH 10) would be inundated. The VBWD monitored Goose Lake water levels from 1972 to 1986,
and resumed monitoring in 2008. Figure 5.29-5shows the recorded water levels. Under normal
conditions, the culvert connecting the north and south lobes of Goose Lake maintains equal water
levels between the two lobes. The highest recorded water level of Goose Lake was 925.1 in July,
1978. Since resuming water level measurements in 2008, the highest observed water level was
Elevation 923.2, which occurred in the summer of 2014. Records from early 1975 indicate the lake
was dry. The VBWD 100-year flood elevation of Goose Lake is 932, just above its overflow
elevation of 931.7. The 100-year flood level was computed using the VBWD 100-year annual runoff
method. All homes surrounding the lake within subdivisions permitted by the VBWD were required
to have minimum floor elevations at least two feet higher than the 100-year flood level.
In 2013, the National Oceanographic and Atmospheric Administration’s (NOAA) published Atlas 14,
Volume 8 (see Section 4.7.6). Atlas 14 contains updated precipitation data for Minnesota. The
VBWD’s calculation of the Goose Lake 100-year flood level predates Atlas 14. Over the next several
years The VBWD plans to update the 100-year flood level for lakes, including Goose Lake, to reflect