Characterizing Microclimate and Plant Community Variation in Wetlands
Abstract Groundwater-fed calcareous wetlands (fens) support diverse plant assemblages including rare species and boreal disjuncts, yet factors structuring related microclimatic and plant community variation have not been thoroughly examined. We investigated factors influencing microclimate variation...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Raney, Patrick A. [verfasserIn] |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2013 |
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| Schlagwörter: |
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| Anmerkung: |
© Society of Wetland Scientists 2013 |
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| Übergeordnetes Werk: |
Enthalten in: Wetlands - [S.l.] : Springer, 1981, 34(2013), 1 vom: 20. Sept., Seite 43-53 |
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| Übergeordnetes Werk: |
volume:34 ; year:2013 ; number:1 ; day:20 ; month:09 ; pages:43-53 |
| Links: |
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| DOI / URN: |
10.1007/s13157-013-0481-2 |
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| Katalog-ID: |
SPR030692806 |
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| 245 | 1 | 0 | |a Characterizing Microclimate and Plant Community Variation in Wetlands |
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| 520 | |a Abstract Groundwater-fed calcareous wetlands (fens) support diverse plant assemblages including rare species and boreal disjuncts, yet factors structuring related microclimatic and plant community variation have not been thoroughly examined. We investigated factors influencing microclimate variation in temperate fens relative to uplands and examined associated plant compositional gradients within fens. Large differences in average soil temperatures were observed between monitoring locations during a 161 day period in 2010 (range: 14.5 to 20.0 °C). Using a regression approach, we developed accurate daily resolution soil temperature models (min and max) from a 29-sensor network by integrating atmospheric and hydrologic terms. Models accurately predicted validation observations from an independent 17-sensor network ($ R^{2} $ values 0.92 minimums; 0.95 maximums) with low error compared to null models. Environmental variation in seasonal average soil temperature, snow depth, specific conductance, canopy closure, and non-vascular plant cover were correlated with spatial patterns in vascular plant community composition. Results of plant community analyses provided insufficient support to suggest boreal and non-boreal species occupied distinct microsites. Given the significant soil temperature variation observed, we suggest further investigation of climatic factors structuring wetland plant communities are warranted to inform the placement of conservation reserves that may be less vulnerable to climate change. | ||
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| 700 | 1 | |a Fridley, Jason D. |4 aut | |
| 700 | 1 | |a Leopold, Donald J. |4 aut | |
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10.1007/s13157-013-0481-2 doi (DE-627)SPR030692806 (SPR)s13157-013-0481-2-e DE-627 ger DE-627 rakwb eng Raney, Patrick A. verfasserin aut Characterizing Microclimate and Plant Community Variation in Wetlands 2013 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Society of Wetland Scientists 2013 Abstract Groundwater-fed calcareous wetlands (fens) support diverse plant assemblages including rare species and boreal disjuncts, yet factors structuring related microclimatic and plant community variation have not been thoroughly examined. We investigated factors influencing microclimate variation in temperate fens relative to uplands and examined associated plant compositional gradients within fens. Large differences in average soil temperatures were observed between monitoring locations during a 161 day period in 2010 (range: 14.5 to 20.0 °C). Using a regression approach, we developed accurate daily resolution soil temperature models (min and max) from a 29-sensor network by integrating atmospheric and hydrologic terms. Models accurately predicted validation observations from an independent 17-sensor network ($ R^{2} $ values 0.92 minimums; 0.95 maximums) with low error compared to null models. Environmental variation in seasonal average soil temperature, snow depth, specific conductance, canopy closure, and non-vascular plant cover were correlated with spatial patterns in vascular plant community composition. Results of plant community analyses provided insufficient support to suggest boreal and non-boreal species occupied distinct microsites. Given the significant soil temperature variation observed, we suggest further investigation of climatic factors structuring wetland plant communities are warranted to inform the placement of conservation reserves that may be less vulnerable to climate change. Climate (dpeaa)DE-He213 Wetlands (dpeaa)DE-He213 Soil (dpeaa)DE-He213 Temperature (dpeaa)DE-He213 Modeling (dpeaa)DE-He213 Boreal (dpeaa)DE-He213 Fridley, Jason D. aut Leopold, Donald J. aut Enthalten in Wetlands [S.l.] : Springer, 1981 34(2013), 1 vom: 20. Sept., Seite 43-53 (DE-627)478509081 (DE-600)2175922-4 1943-6246 nnns volume:34 year:2013 number:1 day:20 month:09 pages:43-53 https://dx.doi.org/10.1007/s13157-013-0481-2 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OLC-PHA GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_101 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_165 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 34 2013 1 20 09 43-53 |
| spelling |
10.1007/s13157-013-0481-2 doi (DE-627)SPR030692806 (SPR)s13157-013-0481-2-e DE-627 ger DE-627 rakwb eng Raney, Patrick A. verfasserin aut Characterizing Microclimate and Plant Community Variation in Wetlands 2013 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Society of Wetland Scientists 2013 Abstract Groundwater-fed calcareous wetlands (fens) support diverse plant assemblages including rare species and boreal disjuncts, yet factors structuring related microclimatic and plant community variation have not been thoroughly examined. We investigated factors influencing microclimate variation in temperate fens relative to uplands and examined associated plant compositional gradients within fens. Large differences in average soil temperatures were observed between monitoring locations during a 161 day period in 2010 (range: 14.5 to 20.0 °C). Using a regression approach, we developed accurate daily resolution soil temperature models (min and max) from a 29-sensor network by integrating atmospheric and hydrologic terms. Models accurately predicted validation observations from an independent 17-sensor network ($ R^{2} $ values 0.92 minimums; 0.95 maximums) with low error compared to null models. Environmental variation in seasonal average soil temperature, snow depth, specific conductance, canopy closure, and non-vascular plant cover were correlated with spatial patterns in vascular plant community composition. Results of plant community analyses provided insufficient support to suggest boreal and non-boreal species occupied distinct microsites. Given the significant soil temperature variation observed, we suggest further investigation of climatic factors structuring wetland plant communities are warranted to inform the placement of conservation reserves that may be less vulnerable to climate change. Climate (dpeaa)DE-He213 Wetlands (dpeaa)DE-He213 Soil (dpeaa)DE-He213 Temperature (dpeaa)DE-He213 Modeling (dpeaa)DE-He213 Boreal (dpeaa)DE-He213 Fridley, Jason D. aut Leopold, Donald J. aut Enthalten in Wetlands [S.l.] : Springer, 1981 34(2013), 1 vom: 20. Sept., Seite 43-53 (DE-627)478509081 (DE-600)2175922-4 1943-6246 nnns volume:34 year:2013 number:1 day:20 month:09 pages:43-53 https://dx.doi.org/10.1007/s13157-013-0481-2 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OLC-PHA GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_101 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_165 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 34 2013 1 20 09 43-53 |
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10.1007/s13157-013-0481-2 doi (DE-627)SPR030692806 (SPR)s13157-013-0481-2-e DE-627 ger DE-627 rakwb eng Raney, Patrick A. verfasserin aut Characterizing Microclimate and Plant Community Variation in Wetlands 2013 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Society of Wetland Scientists 2013 Abstract Groundwater-fed calcareous wetlands (fens) support diverse plant assemblages including rare species and boreal disjuncts, yet factors structuring related microclimatic and plant community variation have not been thoroughly examined. We investigated factors influencing microclimate variation in temperate fens relative to uplands and examined associated plant compositional gradients within fens. Large differences in average soil temperatures were observed between monitoring locations during a 161 day period in 2010 (range: 14.5 to 20.0 °C). Using a regression approach, we developed accurate daily resolution soil temperature models (min and max) from a 29-sensor network by integrating atmospheric and hydrologic terms. Models accurately predicted validation observations from an independent 17-sensor network ($ R^{2} $ values 0.92 minimums; 0.95 maximums) with low error compared to null models. Environmental variation in seasonal average soil temperature, snow depth, specific conductance, canopy closure, and non-vascular plant cover were correlated with spatial patterns in vascular plant community composition. Results of plant community analyses provided insufficient support to suggest boreal and non-boreal species occupied distinct microsites. Given the significant soil temperature variation observed, we suggest further investigation of climatic factors structuring wetland plant communities are warranted to inform the placement of conservation reserves that may be less vulnerable to climate change. Climate (dpeaa)DE-He213 Wetlands (dpeaa)DE-He213 Soil (dpeaa)DE-He213 Temperature (dpeaa)DE-He213 Modeling (dpeaa)DE-He213 Boreal (dpeaa)DE-He213 Fridley, Jason D. aut Leopold, Donald J. aut Enthalten in Wetlands [S.l.] : Springer, 1981 34(2013), 1 vom: 20. Sept., Seite 43-53 (DE-627)478509081 (DE-600)2175922-4 1943-6246 nnns volume:34 year:2013 number:1 day:20 month:09 pages:43-53 https://dx.doi.org/10.1007/s13157-013-0481-2 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OLC-PHA GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_101 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_165 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 34 2013 1 20 09 43-53 |
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10.1007/s13157-013-0481-2 doi (DE-627)SPR030692806 (SPR)s13157-013-0481-2-e DE-627 ger DE-627 rakwb eng Raney, Patrick A. verfasserin aut Characterizing Microclimate and Plant Community Variation in Wetlands 2013 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Society of Wetland Scientists 2013 Abstract Groundwater-fed calcareous wetlands (fens) support diverse plant assemblages including rare species and boreal disjuncts, yet factors structuring related microclimatic and plant community variation have not been thoroughly examined. We investigated factors influencing microclimate variation in temperate fens relative to uplands and examined associated plant compositional gradients within fens. Large differences in average soil temperatures were observed between monitoring locations during a 161 day period in 2010 (range: 14.5 to 20.0 °C). Using a regression approach, we developed accurate daily resolution soil temperature models (min and max) from a 29-sensor network by integrating atmospheric and hydrologic terms. Models accurately predicted validation observations from an independent 17-sensor network ($ R^{2} $ values 0.92 minimums; 0.95 maximums) with low error compared to null models. Environmental variation in seasonal average soil temperature, snow depth, specific conductance, canopy closure, and non-vascular plant cover were correlated with spatial patterns in vascular plant community composition. Results of plant community analyses provided insufficient support to suggest boreal and non-boreal species occupied distinct microsites. Given the significant soil temperature variation observed, we suggest further investigation of climatic factors structuring wetland plant communities are warranted to inform the placement of conservation reserves that may be less vulnerable to climate change. Climate (dpeaa)DE-He213 Wetlands (dpeaa)DE-He213 Soil (dpeaa)DE-He213 Temperature (dpeaa)DE-He213 Modeling (dpeaa)DE-He213 Boreal (dpeaa)DE-He213 Fridley, Jason D. aut Leopold, Donald J. aut Enthalten in Wetlands [S.l.] : Springer, 1981 34(2013), 1 vom: 20. Sept., Seite 43-53 (DE-627)478509081 (DE-600)2175922-4 1943-6246 nnns volume:34 year:2013 number:1 day:20 month:09 pages:43-53 https://dx.doi.org/10.1007/s13157-013-0481-2 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OLC-PHA GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_101 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_165 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 34 2013 1 20 09 43-53 |
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10.1007/s13157-013-0481-2 doi (DE-627)SPR030692806 (SPR)s13157-013-0481-2-e DE-627 ger DE-627 rakwb eng Raney, Patrick A. verfasserin aut Characterizing Microclimate and Plant Community Variation in Wetlands 2013 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Society of Wetland Scientists 2013 Abstract Groundwater-fed calcareous wetlands (fens) support diverse plant assemblages including rare species and boreal disjuncts, yet factors structuring related microclimatic and plant community variation have not been thoroughly examined. We investigated factors influencing microclimate variation in temperate fens relative to uplands and examined associated plant compositional gradients within fens. Large differences in average soil temperatures were observed between monitoring locations during a 161 day period in 2010 (range: 14.5 to 20.0 °C). Using a regression approach, we developed accurate daily resolution soil temperature models (min and max) from a 29-sensor network by integrating atmospheric and hydrologic terms. Models accurately predicted validation observations from an independent 17-sensor network ($ R^{2} $ values 0.92 minimums; 0.95 maximums) with low error compared to null models. Environmental variation in seasonal average soil temperature, snow depth, specific conductance, canopy closure, and non-vascular plant cover were correlated with spatial patterns in vascular plant community composition. Results of plant community analyses provided insufficient support to suggest boreal and non-boreal species occupied distinct microsites. Given the significant soil temperature variation observed, we suggest further investigation of climatic factors structuring wetland plant communities are warranted to inform the placement of conservation reserves that may be less vulnerable to climate change. Climate (dpeaa)DE-He213 Wetlands (dpeaa)DE-He213 Soil (dpeaa)DE-He213 Temperature (dpeaa)DE-He213 Modeling (dpeaa)DE-He213 Boreal (dpeaa)DE-He213 Fridley, Jason D. aut Leopold, Donald J. aut Enthalten in Wetlands [S.l.] : Springer, 1981 34(2013), 1 vom: 20. Sept., Seite 43-53 (DE-627)478509081 (DE-600)2175922-4 1943-6246 nnns volume:34 year:2013 number:1 day:20 month:09 pages:43-53 https://dx.doi.org/10.1007/s13157-013-0481-2 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OLC-PHA GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_101 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_165 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 34 2013 1 20 09 43-53 |
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Raney, Patrick A. @@aut@@ Fridley, Jason D. @@aut@@ Leopold, Donald J. @@aut@@ |
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Raney, Patrick A. |
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Raney, Patrick A. misc Climate misc Wetlands misc Soil misc Temperature misc Modeling misc Boreal Characterizing Microclimate and Plant Community Variation in Wetlands |
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Characterizing Microclimate and Plant Community Variation in Wetlands Climate (dpeaa)DE-He213 Wetlands (dpeaa)DE-He213 Soil (dpeaa)DE-He213 Temperature (dpeaa)DE-He213 Modeling (dpeaa)DE-He213 Boreal (dpeaa)DE-He213 |
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Characterizing Microclimate and Plant Community Variation in Wetlands |
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Characterizing Microclimate and Plant Community Variation in Wetlands |
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characterizing microclimate and plant community variation in wetlands |
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Characterizing Microclimate and Plant Community Variation in Wetlands |
| abstract |
Abstract Groundwater-fed calcareous wetlands (fens) support diverse plant assemblages including rare species and boreal disjuncts, yet factors structuring related microclimatic and plant community variation have not been thoroughly examined. We investigated factors influencing microclimate variation in temperate fens relative to uplands and examined associated plant compositional gradients within fens. Large differences in average soil temperatures were observed between monitoring locations during a 161 day period in 2010 (range: 14.5 to 20.0 °C). Using a regression approach, we developed accurate daily resolution soil temperature models (min and max) from a 29-sensor network by integrating atmospheric and hydrologic terms. Models accurately predicted validation observations from an independent 17-sensor network ($ R^{2} $ values 0.92 minimums; 0.95 maximums) with low error compared to null models. Environmental variation in seasonal average soil temperature, snow depth, specific conductance, canopy closure, and non-vascular plant cover were correlated with spatial patterns in vascular plant community composition. Results of plant community analyses provided insufficient support to suggest boreal and non-boreal species occupied distinct microsites. Given the significant soil temperature variation observed, we suggest further investigation of climatic factors structuring wetland plant communities are warranted to inform the placement of conservation reserves that may be less vulnerable to climate change. © Society of Wetland Scientists 2013 |
| abstractGer |
Abstract Groundwater-fed calcareous wetlands (fens) support diverse plant assemblages including rare species and boreal disjuncts, yet factors structuring related microclimatic and plant community variation have not been thoroughly examined. We investigated factors influencing microclimate variation in temperate fens relative to uplands and examined associated plant compositional gradients within fens. Large differences in average soil temperatures were observed between monitoring locations during a 161 day period in 2010 (range: 14.5 to 20.0 °C). Using a regression approach, we developed accurate daily resolution soil temperature models (min and max) from a 29-sensor network by integrating atmospheric and hydrologic terms. Models accurately predicted validation observations from an independent 17-sensor network ($ R^{2} $ values 0.92 minimums; 0.95 maximums) with low error compared to null models. Environmental variation in seasonal average soil temperature, snow depth, specific conductance, canopy closure, and non-vascular plant cover were correlated with spatial patterns in vascular plant community composition. Results of plant community analyses provided insufficient support to suggest boreal and non-boreal species occupied distinct microsites. Given the significant soil temperature variation observed, we suggest further investigation of climatic factors structuring wetland plant communities are warranted to inform the placement of conservation reserves that may be less vulnerable to climate change. © Society of Wetland Scientists 2013 |
| abstract_unstemmed |
Abstract Groundwater-fed calcareous wetlands (fens) support diverse plant assemblages including rare species and boreal disjuncts, yet factors structuring related microclimatic and plant community variation have not been thoroughly examined. We investigated factors influencing microclimate variation in temperate fens relative to uplands and examined associated plant compositional gradients within fens. Large differences in average soil temperatures were observed between monitoring locations during a 161 day period in 2010 (range: 14.5 to 20.0 °C). Using a regression approach, we developed accurate daily resolution soil temperature models (min and max) from a 29-sensor network by integrating atmospheric and hydrologic terms. Models accurately predicted validation observations from an independent 17-sensor network ($ R^{2} $ values 0.92 minimums; 0.95 maximums) with low error compared to null models. Environmental variation in seasonal average soil temperature, snow depth, specific conductance, canopy closure, and non-vascular plant cover were correlated with spatial patterns in vascular plant community composition. Results of plant community analyses provided insufficient support to suggest boreal and non-boreal species occupied distinct microsites. Given the significant soil temperature variation observed, we suggest further investigation of climatic factors structuring wetland plant communities are warranted to inform the placement of conservation reserves that may be less vulnerable to climate change. © Society of Wetland Scientists 2013 |
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Characterizing Microclimate and Plant Community Variation in Wetlands |
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Fridley, Jason D. Leopold, Donald J. |
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10.1007/s13157-013-0481-2 |
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| score |
7.4008408 |