Variations of the glacier mass balance and lake water storage in the Tarim Basin, northwest China, over the period of 2003–2009 estimated by the ICESat-GLAS data
Abstract Accurately estimating the changes in glacier mass balance and water storage in lakes and reservoirs is critical to studying the water cycle in the inland river basin in northwest China. We used high-resolution satellite images to analyze the changes in water surface area of lakes and reserv...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Wang, Ninglian [verfasserIn] |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2015 |
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| Schlagwörter: |
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| Anmerkung: |
© Springer-Verlag Berlin Heidelberg 2015 |
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| Übergeordnetes Werk: |
Enthalten in: Environmental earth sciences - Berlin : Springer, 2009, 74(2015), 3 vom: 26. Juni, Seite 1997-2008 |
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| Übergeordnetes Werk: |
volume:74 ; year:2015 ; number:3 ; day:26 ; month:06 ; pages:1997-2008 |
| Links: |
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| DOI / URN: |
10.1007/s12665-015-4662-6 |
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SPR026711664 |
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| 245 | 1 | 0 | |a Variations of the glacier mass balance and lake water storage in the Tarim Basin, northwest China, over the period of 2003–2009 estimated by the ICESat-GLAS data |
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| 520 | |a Abstract Accurately estimating the changes in glacier mass balance and water storage in lakes and reservoirs is critical to studying the water cycle in the inland river basin in northwest China. We used high-resolution satellite images to analyze the changes in water surface area of lakes and reservoirs in Tarim Basin, and used the ICESat-GLAS altimeter data to estimate their water level changes and the glacier mass balance change, over the period 2003–2009. The results showed the average glacier thinning in the entire basin was at a rate of 0.34 ± 0.25 m w.e./year equivalent height of water, which means that the glacier mass balance occurred −6.8 ± 1.2 $ km^{3} $ water equivalent over the study period. However, the mean water level of nearby lakes decreased by 0.41 ± 0.2 m even with the influx of glacial melt water, indicating that the lake level declines were caused by the withdrawal of lake water for human activities. | ||
| 650 | 4 | |a ICESat-GLAS |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Glacier mass balance |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Elevation change |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Tarim Basin |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Lakes water storage |7 (dpeaa)DE-He213 | |
| 700 | 1 | |a Wu, Hongbo |4 aut | |
| 700 | 1 | |a Wu, Yuwei |4 aut | |
| 700 | 1 | |a Chen, Anan |4 aut | |
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10.1007/s12665-015-4662-6 doi (DE-627)SPR026711664 (SPR)s12665-015-4662-6-e DE-627 ger DE-627 rakwb eng Wang, Ninglian verfasserin aut Variations of the glacier mass balance and lake water storage in the Tarim Basin, northwest China, over the period of 2003–2009 estimated by the ICESat-GLAS data 2015 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Springer-Verlag Berlin Heidelberg 2015 Abstract Accurately estimating the changes in glacier mass balance and water storage in lakes and reservoirs is critical to studying the water cycle in the inland river basin in northwest China. We used high-resolution satellite images to analyze the changes in water surface area of lakes and reservoirs in Tarim Basin, and used the ICESat-GLAS altimeter data to estimate their water level changes and the glacier mass balance change, over the period 2003–2009. The results showed the average glacier thinning in the entire basin was at a rate of 0.34 ± 0.25 m w.e./year equivalent height of water, which means that the glacier mass balance occurred −6.8 ± 1.2 $ km^{3} $ water equivalent over the study period. However, the mean water level of nearby lakes decreased by 0.41 ± 0.2 m even with the influx of glacial melt water, indicating that the lake level declines were caused by the withdrawal of lake water for human activities. ICESat-GLAS (dpeaa)DE-He213 Glacier mass balance (dpeaa)DE-He213 Elevation change (dpeaa)DE-He213 Tarim Basin (dpeaa)DE-He213 Lakes water storage (dpeaa)DE-He213 Wu, Hongbo aut Wu, Yuwei aut Chen, Anan aut Enthalten in Environmental earth sciences Berlin : Springer, 2009 74(2015), 3 vom: 26. Juni, Seite 1997-2008 (DE-627)599673451 (DE-600)2493699-6 1866-6299 nnns volume:74 year:2015 number:3 day:26 month:06 pages:1997-2008 https://dx.doi.org/10.1007/s12665-015-4662-6 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER 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_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 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_2360 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 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_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 74 2015 3 26 06 1997-2008 |
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10.1007/s12665-015-4662-6 doi (DE-627)SPR026711664 (SPR)s12665-015-4662-6-e DE-627 ger DE-627 rakwb eng Wang, Ninglian verfasserin aut Variations of the glacier mass balance and lake water storage in the Tarim Basin, northwest China, over the period of 2003–2009 estimated by the ICESat-GLAS data 2015 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Springer-Verlag Berlin Heidelberg 2015 Abstract Accurately estimating the changes in glacier mass balance and water storage in lakes and reservoirs is critical to studying the water cycle in the inland river basin in northwest China. We used high-resolution satellite images to analyze the changes in water surface area of lakes and reservoirs in Tarim Basin, and used the ICESat-GLAS altimeter data to estimate their water level changes and the glacier mass balance change, over the period 2003–2009. The results showed the average glacier thinning in the entire basin was at a rate of 0.34 ± 0.25 m w.e./year equivalent height of water, which means that the glacier mass balance occurred −6.8 ± 1.2 $ km^{3} $ water equivalent over the study period. However, the mean water level of nearby lakes decreased by 0.41 ± 0.2 m even with the influx of glacial melt water, indicating that the lake level declines were caused by the withdrawal of lake water for human activities. ICESat-GLAS (dpeaa)DE-He213 Glacier mass balance (dpeaa)DE-He213 Elevation change (dpeaa)DE-He213 Tarim Basin (dpeaa)DE-He213 Lakes water storage (dpeaa)DE-He213 Wu, Hongbo aut Wu, Yuwei aut Chen, Anan aut Enthalten in Environmental earth sciences Berlin : Springer, 2009 74(2015), 3 vom: 26. Juni, Seite 1997-2008 (DE-627)599673451 (DE-600)2493699-6 1866-6299 nnns volume:74 year:2015 number:3 day:26 month:06 pages:1997-2008 https://dx.doi.org/10.1007/s12665-015-4662-6 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER 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_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 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_2360 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 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_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 74 2015 3 26 06 1997-2008 |
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10.1007/s12665-015-4662-6 doi (DE-627)SPR026711664 (SPR)s12665-015-4662-6-e DE-627 ger DE-627 rakwb eng Wang, Ninglian verfasserin aut Variations of the glacier mass balance and lake water storage in the Tarim Basin, northwest China, over the period of 2003–2009 estimated by the ICESat-GLAS data 2015 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Springer-Verlag Berlin Heidelberg 2015 Abstract Accurately estimating the changes in glacier mass balance and water storage in lakes and reservoirs is critical to studying the water cycle in the inland river basin in northwest China. We used high-resolution satellite images to analyze the changes in water surface area of lakes and reservoirs in Tarim Basin, and used the ICESat-GLAS altimeter data to estimate their water level changes and the glacier mass balance change, over the period 2003–2009. The results showed the average glacier thinning in the entire basin was at a rate of 0.34 ± 0.25 m w.e./year equivalent height of water, which means that the glacier mass balance occurred −6.8 ± 1.2 $ km^{3} $ water equivalent over the study period. However, the mean water level of nearby lakes decreased by 0.41 ± 0.2 m even with the influx of glacial melt water, indicating that the lake level declines were caused by the withdrawal of lake water for human activities. ICESat-GLAS (dpeaa)DE-He213 Glacier mass balance (dpeaa)DE-He213 Elevation change (dpeaa)DE-He213 Tarim Basin (dpeaa)DE-He213 Lakes water storage (dpeaa)DE-He213 Wu, Hongbo aut Wu, Yuwei aut Chen, Anan aut Enthalten in Environmental earth sciences Berlin : Springer, 2009 74(2015), 3 vom: 26. Juni, Seite 1997-2008 (DE-627)599673451 (DE-600)2493699-6 1866-6299 nnns volume:74 year:2015 number:3 day:26 month:06 pages:1997-2008 https://dx.doi.org/10.1007/s12665-015-4662-6 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER 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_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 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_2360 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 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_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 74 2015 3 26 06 1997-2008 |
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10.1007/s12665-015-4662-6 doi (DE-627)SPR026711664 (SPR)s12665-015-4662-6-e DE-627 ger DE-627 rakwb eng Wang, Ninglian verfasserin aut Variations of the glacier mass balance and lake water storage in the Tarim Basin, northwest China, over the period of 2003–2009 estimated by the ICESat-GLAS data 2015 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Springer-Verlag Berlin Heidelberg 2015 Abstract Accurately estimating the changes in glacier mass balance and water storage in lakes and reservoirs is critical to studying the water cycle in the inland river basin in northwest China. We used high-resolution satellite images to analyze the changes in water surface area of lakes and reservoirs in Tarim Basin, and used the ICESat-GLAS altimeter data to estimate their water level changes and the glacier mass balance change, over the period 2003–2009. The results showed the average glacier thinning in the entire basin was at a rate of 0.34 ± 0.25 m w.e./year equivalent height of water, which means that the glacier mass balance occurred −6.8 ± 1.2 $ km^{3} $ water equivalent over the study period. However, the mean water level of nearby lakes decreased by 0.41 ± 0.2 m even with the influx of glacial melt water, indicating that the lake level declines were caused by the withdrawal of lake water for human activities. ICESat-GLAS (dpeaa)DE-He213 Glacier mass balance (dpeaa)DE-He213 Elevation change (dpeaa)DE-He213 Tarim Basin (dpeaa)DE-He213 Lakes water storage (dpeaa)DE-He213 Wu, Hongbo aut Wu, Yuwei aut Chen, Anan aut Enthalten in Environmental earth sciences Berlin : Springer, 2009 74(2015), 3 vom: 26. Juni, Seite 1997-2008 (DE-627)599673451 (DE-600)2493699-6 1866-6299 nnns volume:74 year:2015 number:3 day:26 month:06 pages:1997-2008 https://dx.doi.org/10.1007/s12665-015-4662-6 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER 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_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 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_2360 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 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_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 74 2015 3 26 06 1997-2008 |
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10.1007/s12665-015-4662-6 doi (DE-627)SPR026711664 (SPR)s12665-015-4662-6-e DE-627 ger DE-627 rakwb eng Wang, Ninglian verfasserin aut Variations of the glacier mass balance and lake water storage in the Tarim Basin, northwest China, over the period of 2003–2009 estimated by the ICESat-GLAS data 2015 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Springer-Verlag Berlin Heidelberg 2015 Abstract Accurately estimating the changes in glacier mass balance and water storage in lakes and reservoirs is critical to studying the water cycle in the inland river basin in northwest China. We used high-resolution satellite images to analyze the changes in water surface area of lakes and reservoirs in Tarim Basin, and used the ICESat-GLAS altimeter data to estimate their water level changes and the glacier mass balance change, over the period 2003–2009. The results showed the average glacier thinning in the entire basin was at a rate of 0.34 ± 0.25 m w.e./year equivalent height of water, which means that the glacier mass balance occurred −6.8 ± 1.2 $ km^{3} $ water equivalent over the study period. However, the mean water level of nearby lakes decreased by 0.41 ± 0.2 m even with the influx of glacial melt water, indicating that the lake level declines were caused by the withdrawal of lake water for human activities. ICESat-GLAS (dpeaa)DE-He213 Glacier mass balance (dpeaa)DE-He213 Elevation change (dpeaa)DE-He213 Tarim Basin (dpeaa)DE-He213 Lakes water storage (dpeaa)DE-He213 Wu, Hongbo aut Wu, Yuwei aut Chen, Anan aut Enthalten in Environmental earth sciences Berlin : Springer, 2009 74(2015), 3 vom: 26. Juni, Seite 1997-2008 (DE-627)599673451 (DE-600)2493699-6 1866-6299 nnns volume:74 year:2015 number:3 day:26 month:06 pages:1997-2008 https://dx.doi.org/10.1007/s12665-015-4662-6 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER 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_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 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_2360 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 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_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 74 2015 3 26 06 1997-2008 |
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Wang, Ninglian @@aut@@ Wu, Hongbo @@aut@@ Wu, Yuwei @@aut@@ Chen, Anan @@aut@@ |
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Wang, Ninglian |
| spellingShingle |
Wang, Ninglian misc ICESat-GLAS misc Glacier mass balance misc Elevation change misc Tarim Basin misc Lakes water storage Variations of the glacier mass balance and lake water storage in the Tarim Basin, northwest China, over the period of 2003–2009 estimated by the ICESat-GLAS data |
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Variations of the glacier mass balance and lake water storage in the Tarim Basin, northwest China, over the period of 2003–2009 estimated by the ICESat-GLAS data ICESat-GLAS (dpeaa)DE-He213 Glacier mass balance (dpeaa)DE-He213 Elevation change (dpeaa)DE-He213 Tarim Basin (dpeaa)DE-He213 Lakes water storage (dpeaa)DE-He213 |
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misc ICESat-GLAS misc Glacier mass balance misc Elevation change misc Tarim Basin misc Lakes water storage |
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Variations of the glacier mass balance and lake water storage in the Tarim Basin, northwest China, over the period of 2003–2009 estimated by the ICESat-GLAS data |
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Variations of the glacier mass balance and lake water storage in the Tarim Basin, northwest China, over the period of 2003–2009 estimated by the ICESat-GLAS data |
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Wang, Ninglian Wu, Hongbo Wu, Yuwei Chen, Anan |
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variations of the glacier mass balance and lake water storage in the tarim basin, northwest china, over the period of 2003–2009 estimated by the icesat-glas data |
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Variations of the glacier mass balance and lake water storage in the Tarim Basin, northwest China, over the period of 2003–2009 estimated by the ICESat-GLAS data |
| abstract |
Abstract Accurately estimating the changes in glacier mass balance and water storage in lakes and reservoirs is critical to studying the water cycle in the inland river basin in northwest China. We used high-resolution satellite images to analyze the changes in water surface area of lakes and reservoirs in Tarim Basin, and used the ICESat-GLAS altimeter data to estimate their water level changes and the glacier mass balance change, over the period 2003–2009. The results showed the average glacier thinning in the entire basin was at a rate of 0.34 ± 0.25 m w.e./year equivalent height of water, which means that the glacier mass balance occurred −6.8 ± 1.2 $ km^{3} $ water equivalent over the study period. However, the mean water level of nearby lakes decreased by 0.41 ± 0.2 m even with the influx of glacial melt water, indicating that the lake level declines were caused by the withdrawal of lake water for human activities. © Springer-Verlag Berlin Heidelberg 2015 |
| abstractGer |
Abstract Accurately estimating the changes in glacier mass balance and water storage in lakes and reservoirs is critical to studying the water cycle in the inland river basin in northwest China. We used high-resolution satellite images to analyze the changes in water surface area of lakes and reservoirs in Tarim Basin, and used the ICESat-GLAS altimeter data to estimate their water level changes and the glacier mass balance change, over the period 2003–2009. The results showed the average glacier thinning in the entire basin was at a rate of 0.34 ± 0.25 m w.e./year equivalent height of water, which means that the glacier mass balance occurred −6.8 ± 1.2 $ km^{3} $ water equivalent over the study period. However, the mean water level of nearby lakes decreased by 0.41 ± 0.2 m even with the influx of glacial melt water, indicating that the lake level declines were caused by the withdrawal of lake water for human activities. © Springer-Verlag Berlin Heidelberg 2015 |
| abstract_unstemmed |
Abstract Accurately estimating the changes in glacier mass balance and water storage in lakes and reservoirs is critical to studying the water cycle in the inland river basin in northwest China. We used high-resolution satellite images to analyze the changes in water surface area of lakes and reservoirs in Tarim Basin, and used the ICESat-GLAS altimeter data to estimate their water level changes and the glacier mass balance change, over the period 2003–2009. The results showed the average glacier thinning in the entire basin was at a rate of 0.34 ± 0.25 m w.e./year equivalent height of water, which means that the glacier mass balance occurred −6.8 ± 1.2 $ km^{3} $ water equivalent over the study period. However, the mean water level of nearby lakes decreased by 0.41 ± 0.2 m even with the influx of glacial melt water, indicating that the lake level declines were caused by the withdrawal of lake water for human activities. © Springer-Verlag Berlin Heidelberg 2015 |
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3 |
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Variations of the glacier mass balance and lake water storage in the Tarim Basin, northwest China, over the period of 2003–2009 estimated by the ICESat-GLAS data |
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https://dx.doi.org/10.1007/s12665-015-4662-6 |
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Wu, Hongbo Wu, Yuwei Chen, Anan |
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10.1007/s12665-015-4662-6 |
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2024-07-03T22:19:02.811Z |
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| score |
7.402916 |