This securely fenced 1.6 acre microenvironmental study plot was established in 1978 with a grant from the University of Wisconsin System. There are two towers for deployment of climate instrumentation, one of 10 m in the "open"" and one of 16 m that ascends into but does not transcend a forest canopy of mixed conifer-hardwoods. Until 2002 neither instruments nor personnel were available to make systematic records, but at the end of the summer of, an array of environmental sensors were deployed.
Schmeeckle Reserve is natural area slightly greater than 100 ha situated just north of the campus of the University of Wisconsin at Stevens Point. Its substrate ranges from well-drained shallow soils over bedrock to the north to wetlands in the south over increasingly deep strata of outwash sands. Its upland vegetation is second-growth, dating back primarily to logging in the early part of the 20th century, with much subsequently historically farmed, though the soils are paradoxically droughty and subject to flooding. The soils tend to be sandy, bit no part of the reserve sits far above the water table. During the last century its hydrology has been influenced by the widest variety of road construction and urban development. As one would expect in Wisconsin, ecological succession is likely to proceed rapidly towards forest cover. As one would expect in this part of Wisconsin, the forest is likely to be a mix of hardwoods and conifers.
The intent behind the establishment of the plot was to provide a textbook setting for studying the strong microenvironmental differences that may be expected over the short distance between open and forested sites. A variety of subtle elements compromise that ideal. One can rationalize that the plot does well in illustrating "real world" conditions as opposed to textbook climatic variation. A secondary objective was to document the relatively great variation in temperature and small variation in moisture characteristic of our geographical area.
Compromises:
Towers: