Hydrologic variability in black ash wetlands: Implications for vulnerability to emerald ash borer

被引:10
作者
Cianciolo, Thomas R. [1 ]
Diamond, Jacob S. [2 ,3 ]
McLaughlin, Daniel L. [4 ]
Slesak, Robert A. [5 ]
D'Amato, Anthony W. [6 ]
Palik, Brian J. [7 ]
机构
[1] Univ Minnesota, Dept Forest Resources, St Paul, MN 55455 USA
[2] Irstea, Quantitat Ecohydrol Lab, RiverLy, Lyon, France
[3] Univ Tours, Continental Geohydrosyst Lab, Tours, France
[4] Virginia Tech, Dept Forest Resources & Environm Conservat, Blacksburg, VA USA
[5] US Forest Serv, USDA, Pacific Northwest Res Stn, Olympia, WA USA
[6] Univ Vermont, Rubenstein Sch Environm & Nat Resources, Burlington, VT USA
[7] US Forest Serv, USDA, Northern Res Stn, Grand Rapids, MN USA
关键词
evapotranspiration; groundwater exchange; invasive pest; microtopography; specific yield; terrain analysis; WATER-TABLE; MICROTOPOGRAPHY; MINNESOTA; VEGETATION; LIDAR; EVAPOTRANSPIRATION; MORTALITY; IMPACTS; FORESTS; DEM;
D O I
10.1002/hyp.14014
中图分类号
TV21 [水资源调查与水利规划];
学科分类号
081501 ;
摘要
Black ash (Fraxinus nigra) wetlands are widespread, forested landscape features in the western Great Lakes region. However, the future of these ecosystems is threatened due to impending spread of the invasive emerald ash borer (EAB), which results in tree mortality, decreased transpiration, and potential shifts to wetter, non-forested conditions. The vulnerability to such ecohydrologic shifts likely varies according to local hydrologic regimes controlled by landscape settings, but this site-dependent vulnerability and our ability to predict it is unknown. Here, we assessed vulnerability potential as a function of site hydrology in 15 undisturbed black ash wetlands from their three most common hydrogeomorphic settings in northern Minnesota: lowland, depression, and transition. Further, we used high-resolution (1-cm) surface elevation models to assess spatial variability of water levels at a subset of 10 sites. Although we observed similar ET and groundwater exchange rates among settings, lowland sites were generally drier because of elevated landscape position and greater water level drawdowns (via lower specific yield). We predict that such drier sites will exhibit greater water level increases following EAB-induced ash mortality, compared to wetter sites where open water evaporation and shallow-rooted understory transpiration will offset losses in tree transpiration. Moreover, compared to wetter sites, drier sites exhibited minimal microtopographic variation, limiting the number of elevated microsites for tree establishment and eventual canopy recovery after ash loss. These results suggest that site wetness is a simple and effective predictor of black ash wetland vulnerability to hydrologic regime change. To that end, we assessed the ability of common terrain metrics to predict site wetness, providing a potential tool to target vulnerable areas for active management efforts.
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页数:13
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