|
Ecoregion Description
|
The Northern Appalachian Plateau and Uplands ecoregion is located in south-central New York and north-central Pennsylvania and covers approximately 29,900 km2 (11,550 mi2) (fig. 1). The ecoregion is defined as a “transitional ecoregion between the less irregular, more agricultural and urbanized ecoregions to the north and west and the more mountainous and forested, less populated ecoregions to the south and east” (U. S. Environmental Protection Agency, 2002). The landscape is rural with rolling hills and fertile stream valleys. Forest and agriculture are the dominant land covers in the ecoregion. The forest consists of northern hardwoods that include sugar maple (Acer saccharum), red maple (Acer rubrum), white ash (Fraxinus americana), American beech (Fagus grandifolia), northern red oak (Quercus rubra), black cherry (Prunus avium), and eastern hemlock (Tsuga canadensis) (Smallidge, 1997). Dairy and cattle farming, along with the production of corn, wheat, and hay, are the major agricultural activities in this ecoregion (Fick and Cox, 1995). The climate is temperate with an average January temperature of –6.1oC (21oF) and an average July temperature of 20.7oC (69oF), with more than 940 mm (37 in) of precipitation annually (National Oceanic and Atmospheric Administration, 2002).
|

Figure 1: Northern Appalachian Plateau and Uplands Ecoregion showing the location of the sample blocks used in the study. Click on image to enlarge
|
Contemporary Land Cover Change from 1973 to 2000
|
Compared to other ecoregions of the Eastern United States (fig. 2), the overall estimated change between 1973 and 2000 for the Northern Appalachian Plateau and Uplands was quite low, just 2.4 percent (718 km2 or 227 mi2). An estimated 1.8 percent (538 km2 or 207 mi2) of total land area changed land cover once, and the area undergoing multiple changes was estimated at just 0.6 percent (209 km2 or 80 mi2) (table 1).
The estimated change per time period varied modestly during the study period. The first two time intervals, 1972 to 1980 and 1980 to 1986, experienced a change of 0.7 percent. The third time interval, 1986 to 1992, had the only increase in change from 0.7 percent to 1.0 percent. Finally, in the last interval, 1992 to 2000, the total change was 0.8 percent. The margin of error at the 85-percent confidence level was very low during all time periods. The average annual rate of change for all time intervals was 0.1 percent, with the exception of the 1986 to 1992 time interval, which had a rate of change of 0.2 percent (table 2).
|
Table 1: Estimated overall spatial land cover change between 1973 and 2000 is 2.4%

Table 2: Estimated change and average annual change (normalized to account for varying time intervals) for each time interval

|
|

Figure 2: The overall spatial change in all Eastern U.S. ecoregions. Each bar chart shows the proportion of the ecoregion that experienced change on 1, 2, 3, or 4 dates. Click on image to enlarge
|
Figure 3: Estimates of land cover change per time interval normalized to annual rates of change. Click on image to enlarge
|
Land cover in the Northern Appalachian Plateau and Uplands ecoregion was extremely stable throughout the 1973 to 2000 study period. The dominant land covers were forest with 60.1 percent of the land area in 2000, agriculture with 33.9 percent, and developed lands with 3.3 percent of the ecoregion (table 3).
Table 3: Summary table showing the estimated percent of land area of individual land cover classes between 1973 and 2000 and calculated estimated net change per time interval.

Net change for all land covers, with the exception of agriculture, was modest during the 1973 to 2000 study period. Agriculture saw the largest net change with a –0.9 percent change during the study period. Land covers that gained at the expense of agriculture included developed lands with an increase of 0.5 percent and grassland/shrubland with 0.3 percent (fig. 4).
The top two land cover conversions indicate that the ecoregion experienced a decline in agricultural lands during the study period. An estimated 161 km2 (62 mi2) of agricultural lands converted to forest, and 160 km2 (62 mi2) were converted to grassland/shrubland. The third leading conversion was 136 km2 (53 mi2) from grassland/shrubland to forest. The second and third leading conversions were the result of the natural progression of abandoned agricultural lands reverting back to forest. Leading factors that contribute to the abandonment of agricultural lands are topography, road access, poor drainage, and poor soil (Flinn, Vellend, and Marks, 2005). The fourth and fifth leading conversions consisted of 124 km2 (48 mi2) of forest being cleared for farmland and 85 km2 (33 mi2) of forest becoming mechanically disturbed because of timber harvesting (table 4).
The Northern Appalachian Plateau and Uplands ecoregion remained stable throughout the 1973 to 2000 study period. The loss of agricultural lands was the most significant land cover change. Farmlands declined in each time interval. The 1986 to 1992 time interval experienced the greatest amount of agricultural land being abandoned, with an estimated 148 km2 (57 mi2) being converted to forest, grassland/shrubland, or developed land (table 4).
|
Table 4: Leading land cover conversions are listed for each of the four time intervals and for the entire study period

|

Figure 4: Net Change of Land Cover Categories per Time Period Click on image to enlarge
|
1 Mark S. Brooks - U.S. Geological Survey, Eastern Geographic Science Center, Reston, VA 20192
References
Fick, Gary W., and Cox, William J., 1995, The agronomy of dairy farming in New York state: Ithaca, N.Y., Cornell University, Department of Soil, Crop and Atmospheric Sciences, SCAS Teaching Series No. T95-1, 8 p.
Flinn, Kathryn M., Vellend, Mark, and Marks, P.L., 2005, Environmental causes and consequences of forest clearance and agricultural abandonment in central New York, USA: Journal of Biogeography, v. 32, p. 439–452.
National Oceanic and Atmospheric Administration, 2002, Monthly station normals of temperature, precipitation, and heating and cooling degree days 1971–2000 for New York [revised]: NOAA, available online at
http://hurricane.ncdc.noaa.gov/climatenormals/clim81/NYnorm.pdf.
Smallidge, Peter, 1997, New York’s forest—then and now: Ithaca, N.Y., Cornell University, New York State College of Agriculture and Life Sciences, Department of Natural Resources.
U.S. Environmental Protection Agency, 2002, Primary distinguishing characteristics of Level III ecoregions of the continental United States [draft]: EPA, available online at ftp://ftp.epa.gov/wed/ecoregions/us/useco_desc.doc.
|