Spatiotemporal Change of Vegetation Coverage and its Relationship with Climate Change in Freshwater Marshes of Northeast China
Abstract Based on the normalized difference vegetation index and climate data, this study investigated the spatiotemporal change of fractional vegetation cover (FVC) and its relationship with climate change in freshwater marshes of Northeast China from 2000 to 2016. Although freshwater marshes in No...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Shen, Xiangjin [verfasserIn] |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2018 |
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| Schlagwörter: |
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| Anmerkung: |
© Society of Wetland Scientists 2018 |
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| Übergeordnetes Werk: |
Enthalten in: Wetlands - [S.l.] : Springer, 1981, 39(2018), 3 vom: 03. Sept., Seite 429-439 |
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| Übergeordnetes Werk: |
volume:39 ; year:2018 ; number:3 ; day:03 ; month:09 ; pages:429-439 |
| Links: |
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| DOI / URN: |
10.1007/s13157-018-1072-z |
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| Katalog-ID: |
SPR030699681 |
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| 100 | 1 | |a Shen, Xiangjin |e verfasserin |4 aut | |
| 245 | 1 | 0 | |a Spatiotemporal Change of Vegetation Coverage and its Relationship with Climate Change in Freshwater Marshes of Northeast China |
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| 520 | |a Abstract Based on the normalized difference vegetation index and climate data, this study investigated the spatiotemporal change of fractional vegetation cover (FVC) and its relationship with climate change in freshwater marshes of Northeast China from 2000 to 2016. Although freshwater marshes in Northeast China have undergone loss during the past nearly 20 years, the FVC of unchanged marshes has increased by 0.34% per year over the study area, with the largest increases in Songnen Plain. Correlation analysis results showed that warm growing season temperatures could enhance the FVC of marshes in the Greater and Lesser Khingan Mountains, but reduce the FVC in arid and semi-arid grassland regions of Songnen Plain and Eastern Inner Mongolia. By contrast, the increased growing season precipitation could significantly enhance the FVC of marshes in semi-arid grassland regions of Northeast China, but reduce the FVC of marshes in the Lesser Khingan Mountains and Sanjiang Plain. Under the background of future climate change, we can predict lower FVC of marshes in Songnen Plain and Eastern Inner Mongolia, but higher FVC of marshes in the Changbai Mountains in the future. This research is expected to provide valuable implications for the protection and restoration of wetland vegetation in Northeast China. | ||
| 650 | 4 | |a Fractional vegetation cover |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Freshwater marshes |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Wetland |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Climate change |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Northeast China |7 (dpeaa)DE-He213 | |
| 700 | 1 | |a Xue, Zhenshan |4 aut | |
| 700 | 1 | |a Jiang, Ming |4 aut | |
| 700 | 1 | |a Lu, Xianguo |4 aut | |
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10.1007/s13157-018-1072-z doi (DE-627)SPR030699681 (SPR)s13157-018-1072-z-e DE-627 ger DE-627 rakwb eng Shen, Xiangjin verfasserin aut Spatiotemporal Change of Vegetation Coverage and its Relationship with Climate Change in Freshwater Marshes of Northeast China 2018 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Society of Wetland Scientists 2018 Abstract Based on the normalized difference vegetation index and climate data, this study investigated the spatiotemporal change of fractional vegetation cover (FVC) and its relationship with climate change in freshwater marshes of Northeast China from 2000 to 2016. Although freshwater marshes in Northeast China have undergone loss during the past nearly 20 years, the FVC of unchanged marshes has increased by 0.34% per year over the study area, with the largest increases in Songnen Plain. Correlation analysis results showed that warm growing season temperatures could enhance the FVC of marshes in the Greater and Lesser Khingan Mountains, but reduce the FVC in arid and semi-arid grassland regions of Songnen Plain and Eastern Inner Mongolia. By contrast, the increased growing season precipitation could significantly enhance the FVC of marshes in semi-arid grassland regions of Northeast China, but reduce the FVC of marshes in the Lesser Khingan Mountains and Sanjiang Plain. Under the background of future climate change, we can predict lower FVC of marshes in Songnen Plain and Eastern Inner Mongolia, but higher FVC of marshes in the Changbai Mountains in the future. This research is expected to provide valuable implications for the protection and restoration of wetland vegetation in Northeast China. Fractional vegetation cover (dpeaa)DE-He213 Freshwater marshes (dpeaa)DE-He213 Wetland (dpeaa)DE-He213 Climate change (dpeaa)DE-He213 Northeast China (dpeaa)DE-He213 Xue, Zhenshan aut Jiang, Ming aut Lu, Xianguo aut Enthalten in Wetlands [S.l.] : Springer, 1981 39(2018), 3 vom: 03. Sept., Seite 429-439 (DE-627)478509081 (DE-600)2175922-4 1943-6246 nnns volume:39 year:2018 number:3 day:03 month:09 pages:429-439 https://dx.doi.org/10.1007/s13157-018-1072-z 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 39 2018 3 03 09 429-439 |
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10.1007/s13157-018-1072-z doi (DE-627)SPR030699681 (SPR)s13157-018-1072-z-e DE-627 ger DE-627 rakwb eng Shen, Xiangjin verfasserin aut Spatiotemporal Change of Vegetation Coverage and its Relationship with Climate Change in Freshwater Marshes of Northeast China 2018 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Society of Wetland Scientists 2018 Abstract Based on the normalized difference vegetation index and climate data, this study investigated the spatiotemporal change of fractional vegetation cover (FVC) and its relationship with climate change in freshwater marshes of Northeast China from 2000 to 2016. Although freshwater marshes in Northeast China have undergone loss during the past nearly 20 years, the FVC of unchanged marshes has increased by 0.34% per year over the study area, with the largest increases in Songnen Plain. Correlation analysis results showed that warm growing season temperatures could enhance the FVC of marshes in the Greater and Lesser Khingan Mountains, but reduce the FVC in arid and semi-arid grassland regions of Songnen Plain and Eastern Inner Mongolia. By contrast, the increased growing season precipitation could significantly enhance the FVC of marshes in semi-arid grassland regions of Northeast China, but reduce the FVC of marshes in the Lesser Khingan Mountains and Sanjiang Plain. Under the background of future climate change, we can predict lower FVC of marshes in Songnen Plain and Eastern Inner Mongolia, but higher FVC of marshes in the Changbai Mountains in the future. This research is expected to provide valuable implications for the protection and restoration of wetland vegetation in Northeast China. Fractional vegetation cover (dpeaa)DE-He213 Freshwater marshes (dpeaa)DE-He213 Wetland (dpeaa)DE-He213 Climate change (dpeaa)DE-He213 Northeast China (dpeaa)DE-He213 Xue, Zhenshan aut Jiang, Ming aut Lu, Xianguo aut Enthalten in Wetlands [S.l.] : Springer, 1981 39(2018), 3 vom: 03. Sept., Seite 429-439 (DE-627)478509081 (DE-600)2175922-4 1943-6246 nnns volume:39 year:2018 number:3 day:03 month:09 pages:429-439 https://dx.doi.org/10.1007/s13157-018-1072-z 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 39 2018 3 03 09 429-439 |
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10.1007/s13157-018-1072-z doi (DE-627)SPR030699681 (SPR)s13157-018-1072-z-e DE-627 ger DE-627 rakwb eng Shen, Xiangjin verfasserin aut Spatiotemporal Change of Vegetation Coverage and its Relationship with Climate Change in Freshwater Marshes of Northeast China 2018 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Society of Wetland Scientists 2018 Abstract Based on the normalized difference vegetation index and climate data, this study investigated the spatiotemporal change of fractional vegetation cover (FVC) and its relationship with climate change in freshwater marshes of Northeast China from 2000 to 2016. Although freshwater marshes in Northeast China have undergone loss during the past nearly 20 years, the FVC of unchanged marshes has increased by 0.34% per year over the study area, with the largest increases in Songnen Plain. Correlation analysis results showed that warm growing season temperatures could enhance the FVC of marshes in the Greater and Lesser Khingan Mountains, but reduce the FVC in arid and semi-arid grassland regions of Songnen Plain and Eastern Inner Mongolia. By contrast, the increased growing season precipitation could significantly enhance the FVC of marshes in semi-arid grassland regions of Northeast China, but reduce the FVC of marshes in the Lesser Khingan Mountains and Sanjiang Plain. Under the background of future climate change, we can predict lower FVC of marshes in Songnen Plain and Eastern Inner Mongolia, but higher FVC of marshes in the Changbai Mountains in the future. This research is expected to provide valuable implications for the protection and restoration of wetland vegetation in Northeast China. Fractional vegetation cover (dpeaa)DE-He213 Freshwater marshes (dpeaa)DE-He213 Wetland (dpeaa)DE-He213 Climate change (dpeaa)DE-He213 Northeast China (dpeaa)DE-He213 Xue, Zhenshan aut Jiang, Ming aut Lu, Xianguo aut Enthalten in Wetlands [S.l.] : Springer, 1981 39(2018), 3 vom: 03. Sept., Seite 429-439 (DE-627)478509081 (DE-600)2175922-4 1943-6246 nnns volume:39 year:2018 number:3 day:03 month:09 pages:429-439 https://dx.doi.org/10.1007/s13157-018-1072-z 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 39 2018 3 03 09 429-439 |
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10.1007/s13157-018-1072-z doi (DE-627)SPR030699681 (SPR)s13157-018-1072-z-e DE-627 ger DE-627 rakwb eng Shen, Xiangjin verfasserin aut Spatiotemporal Change of Vegetation Coverage and its Relationship with Climate Change in Freshwater Marshes of Northeast China 2018 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Society of Wetland Scientists 2018 Abstract Based on the normalized difference vegetation index and climate data, this study investigated the spatiotemporal change of fractional vegetation cover (FVC) and its relationship with climate change in freshwater marshes of Northeast China from 2000 to 2016. Although freshwater marshes in Northeast China have undergone loss during the past nearly 20 years, the FVC of unchanged marshes has increased by 0.34% per year over the study area, with the largest increases in Songnen Plain. Correlation analysis results showed that warm growing season temperatures could enhance the FVC of marshes in the Greater and Lesser Khingan Mountains, but reduce the FVC in arid and semi-arid grassland regions of Songnen Plain and Eastern Inner Mongolia. By contrast, the increased growing season precipitation could significantly enhance the FVC of marshes in semi-arid grassland regions of Northeast China, but reduce the FVC of marshes in the Lesser Khingan Mountains and Sanjiang Plain. Under the background of future climate change, we can predict lower FVC of marshes in Songnen Plain and Eastern Inner Mongolia, but higher FVC of marshes in the Changbai Mountains in the future. This research is expected to provide valuable implications for the protection and restoration of wetland vegetation in Northeast China. Fractional vegetation cover (dpeaa)DE-He213 Freshwater marshes (dpeaa)DE-He213 Wetland (dpeaa)DE-He213 Climate change (dpeaa)DE-He213 Northeast China (dpeaa)DE-He213 Xue, Zhenshan aut Jiang, Ming aut Lu, Xianguo aut Enthalten in Wetlands [S.l.] : Springer, 1981 39(2018), 3 vom: 03. Sept., Seite 429-439 (DE-627)478509081 (DE-600)2175922-4 1943-6246 nnns volume:39 year:2018 number:3 day:03 month:09 pages:429-439 https://dx.doi.org/10.1007/s13157-018-1072-z 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 39 2018 3 03 09 429-439 |
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10.1007/s13157-018-1072-z doi (DE-627)SPR030699681 (SPR)s13157-018-1072-z-e DE-627 ger DE-627 rakwb eng Shen, Xiangjin verfasserin aut Spatiotemporal Change of Vegetation Coverage and its Relationship with Climate Change in Freshwater Marshes of Northeast China 2018 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Society of Wetland Scientists 2018 Abstract Based on the normalized difference vegetation index and climate data, this study investigated the spatiotemporal change of fractional vegetation cover (FVC) and its relationship with climate change in freshwater marshes of Northeast China from 2000 to 2016. Although freshwater marshes in Northeast China have undergone loss during the past nearly 20 years, the FVC of unchanged marshes has increased by 0.34% per year over the study area, with the largest increases in Songnen Plain. Correlation analysis results showed that warm growing season temperatures could enhance the FVC of marshes in the Greater and Lesser Khingan Mountains, but reduce the FVC in arid and semi-arid grassland regions of Songnen Plain and Eastern Inner Mongolia. By contrast, the increased growing season precipitation could significantly enhance the FVC of marshes in semi-arid grassland regions of Northeast China, but reduce the FVC of marshes in the Lesser Khingan Mountains and Sanjiang Plain. Under the background of future climate change, we can predict lower FVC of marshes in Songnen Plain and Eastern Inner Mongolia, but higher FVC of marshes in the Changbai Mountains in the future. This research is expected to provide valuable implications for the protection and restoration of wetland vegetation in Northeast China. Fractional vegetation cover (dpeaa)DE-He213 Freshwater marshes (dpeaa)DE-He213 Wetland (dpeaa)DE-He213 Climate change (dpeaa)DE-He213 Northeast China (dpeaa)DE-He213 Xue, Zhenshan aut Jiang, Ming aut Lu, Xianguo aut Enthalten in Wetlands [S.l.] : Springer, 1981 39(2018), 3 vom: 03. Sept., Seite 429-439 (DE-627)478509081 (DE-600)2175922-4 1943-6246 nnns volume:39 year:2018 number:3 day:03 month:09 pages:429-439 https://dx.doi.org/10.1007/s13157-018-1072-z 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 39 2018 3 03 09 429-439 |
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Shen, Xiangjin @@aut@@ Xue, Zhenshan @@aut@@ Jiang, Ming @@aut@@ Lu, Xianguo @@aut@@ |
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<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">SPR030699681</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230519095449.0</controlfield><controlfield tag="007">cr uuu---uuuuu</controlfield><controlfield tag="008">201007s2018 xx |||||o 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1007/s13157-018-1072-z</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)SPR030699681</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(SPR)s13157-018-1072-z-e</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rakwb</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Shen, Xiangjin</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Spatiotemporal Change of Vegetation Coverage and its Relationship with Climate Change in Freshwater Marshes of Northeast China</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2018</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">Text</subfield><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">Computermedien</subfield><subfield code="b">c</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Online-Ressource</subfield><subfield code="b">cr</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="500" ind1=" " ind2=" "><subfield code="a">© Society of Wetland Scientists 2018</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Abstract Based on the normalized difference vegetation index and climate data, this study investigated the spatiotemporal change of fractional vegetation cover (FVC) and its relationship with climate change in freshwater marshes of Northeast China from 2000 to 2016. Although freshwater marshes in Northeast China have undergone loss during the past nearly 20 years, the FVC of unchanged marshes has increased by 0.34% per year over the study area, with the largest increases in Songnen Plain. Correlation analysis results showed that warm growing season temperatures could enhance the FVC of marshes in the Greater and Lesser Khingan Mountains, but reduce the FVC in arid and semi-arid grassland regions of Songnen Plain and Eastern Inner Mongolia. By contrast, the increased growing season precipitation could significantly enhance the FVC of marshes in semi-arid grassland regions of Northeast China, but reduce the FVC of marshes in the Lesser Khingan Mountains and Sanjiang Plain. Under the background of future climate change, we can predict lower FVC of marshes in Songnen Plain and Eastern Inner Mongolia, but higher FVC of marshes in the Changbai Mountains in the future. 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Shen, Xiangjin |
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Shen, Xiangjin misc Fractional vegetation cover misc Freshwater marshes misc Wetland misc Climate change misc Northeast China Spatiotemporal Change of Vegetation Coverage and its Relationship with Climate Change in Freshwater Marshes of Northeast China |
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Spatiotemporal Change of Vegetation Coverage and its Relationship with Climate Change in Freshwater Marshes of Northeast China Fractional vegetation cover (dpeaa)DE-He213 Freshwater marshes (dpeaa)DE-He213 Wetland (dpeaa)DE-He213 Climate change (dpeaa)DE-He213 Northeast China (dpeaa)DE-He213 |
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Shen, Xiangjin Xue, Zhenshan Jiang, Ming Lu, Xianguo |
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spatiotemporal change of vegetation coverage and its relationship with climate change in freshwater marshes of northeast china |
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Spatiotemporal Change of Vegetation Coverage and its Relationship with Climate Change in Freshwater Marshes of Northeast China |
| abstract |
Abstract Based on the normalized difference vegetation index and climate data, this study investigated the spatiotemporal change of fractional vegetation cover (FVC) and its relationship with climate change in freshwater marshes of Northeast China from 2000 to 2016. Although freshwater marshes in Northeast China have undergone loss during the past nearly 20 years, the FVC of unchanged marshes has increased by 0.34% per year over the study area, with the largest increases in Songnen Plain. Correlation analysis results showed that warm growing season temperatures could enhance the FVC of marshes in the Greater and Lesser Khingan Mountains, but reduce the FVC in arid and semi-arid grassland regions of Songnen Plain and Eastern Inner Mongolia. By contrast, the increased growing season precipitation could significantly enhance the FVC of marshes in semi-arid grassland regions of Northeast China, but reduce the FVC of marshes in the Lesser Khingan Mountains and Sanjiang Plain. Under the background of future climate change, we can predict lower FVC of marshes in Songnen Plain and Eastern Inner Mongolia, but higher FVC of marshes in the Changbai Mountains in the future. This research is expected to provide valuable implications for the protection and restoration of wetland vegetation in Northeast China. © Society of Wetland Scientists 2018 |
| abstractGer |
Abstract Based on the normalized difference vegetation index and climate data, this study investigated the spatiotemporal change of fractional vegetation cover (FVC) and its relationship with climate change in freshwater marshes of Northeast China from 2000 to 2016. Although freshwater marshes in Northeast China have undergone loss during the past nearly 20 years, the FVC of unchanged marshes has increased by 0.34% per year over the study area, with the largest increases in Songnen Plain. Correlation analysis results showed that warm growing season temperatures could enhance the FVC of marshes in the Greater and Lesser Khingan Mountains, but reduce the FVC in arid and semi-arid grassland regions of Songnen Plain and Eastern Inner Mongolia. By contrast, the increased growing season precipitation could significantly enhance the FVC of marshes in semi-arid grassland regions of Northeast China, but reduce the FVC of marshes in the Lesser Khingan Mountains and Sanjiang Plain. Under the background of future climate change, we can predict lower FVC of marshes in Songnen Plain and Eastern Inner Mongolia, but higher FVC of marshes in the Changbai Mountains in the future. This research is expected to provide valuable implications for the protection and restoration of wetland vegetation in Northeast China. © Society of Wetland Scientists 2018 |
| abstract_unstemmed |
Abstract Based on the normalized difference vegetation index and climate data, this study investigated the spatiotemporal change of fractional vegetation cover (FVC) and its relationship with climate change in freshwater marshes of Northeast China from 2000 to 2016. Although freshwater marshes in Northeast China have undergone loss during the past nearly 20 years, the FVC of unchanged marshes has increased by 0.34% per year over the study area, with the largest increases in Songnen Plain. Correlation analysis results showed that warm growing season temperatures could enhance the FVC of marshes in the Greater and Lesser Khingan Mountains, but reduce the FVC in arid and semi-arid grassland regions of Songnen Plain and Eastern Inner Mongolia. By contrast, the increased growing season precipitation could significantly enhance the FVC of marshes in semi-arid grassland regions of Northeast China, but reduce the FVC of marshes in the Lesser Khingan Mountains and Sanjiang Plain. Under the background of future climate change, we can predict lower FVC of marshes in Songnen Plain and Eastern Inner Mongolia, but higher FVC of marshes in the Changbai Mountains in the future. This research is expected to provide valuable implications for the protection and restoration of wetland vegetation in Northeast China. © Society of Wetland Scientists 2018 |
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Spatiotemporal Change of Vegetation Coverage and its Relationship with Climate Change in Freshwater Marshes of Northeast China |
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https://dx.doi.org/10.1007/s13157-018-1072-z |
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Xue, Zhenshan Jiang, Ming Lu, Xianguo |
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2024-07-03T19:37:55.351Z |
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| score |
7.4017096 |