Investigation of lake shrinkage attributed to climate change over the past 33 years in Inner Mongolia, China
Abstract Inner Mongolia, located in northern China and bordered by Mongolia and Russia, has numerous lakes. Constrained by water scarcity, precious lakes play key roles in degraded grassland ecosystems and the social and economic development of Inner Mongolia. This study combines 1815 Landsat image...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Zhang, Yanfei [verfasserIn] |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2023 |
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| Schlagwörter: |
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| Anmerkung: |
© The Author(s), under exclusive licence to Springer Nature B.V. 2023. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. |
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| Übergeordnetes Werk: |
Enthalten in: Climatic change - Dordrecht [u.a.] : Springer Science + Business Media B.V, 1977, 176(2023), 2 vom: 23. Jan. |
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| Übergeordnetes Werk: |
volume:176 ; year:2023 ; number:2 ; day:23 ; month:01 |
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| DOI / URN: |
10.1007/s10584-023-03487-3 |
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SPR049122231 |
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| 520 | |a Abstract Inner Mongolia, located in northern China and bordered by Mongolia and Russia, has numerous lakes. Constrained by water scarcity, precious lakes play key roles in degraded grassland ecosystems and the social and economic development of Inner Mongolia. This study combines 1815 Landsat image interpretations and ground-based surveys to track the area changes in 573 lakes in Inner Mongolia during the period 1987–2019. Our results demonstrate that the number of dried-up lakes increased by 0.87 per year, the number of lakes with water areas below 0.1 $ km^{2} $ increased by 1.02 per year, and the number of lakes with water areas between 0.1 and 1 $ km^{2} $ increased by 0.39 per year. The number of lakes with areas larger than 1 $ km^{2} $ shows a decreased or fluctuating trend. The lake area in Inner Mongolia increased at a rate of 7.04 $ km^{2} $/year from 1987 to 1998 but then shows an overall decreasing trend at a rate of 0.71 $ km^{2} $/year over the next 20 years. The period from 1999 to 2010 was the most serious period of lake shrinkage in Inner Mongolia in the past 30 years, with a shrinkage rate of 33.99 $ km^{2} $/year. The climate changes from wet to dry and from dry to wet are the main reasons for the breakpoint occurrence of the lake area time series in the 2000s and 2010s, respectively. The response of lake area changes to climate-related factors has significant regional differences. In addition, intensification of human activities, such as the rapid development of livestock and coal mining, is also the main driver of lake change. The multiple regression model shows that the contribution of climate-related variables and human activity–related variables to the change in lake area over the 1987–2019 time period was about 40% and 60%, respectively. | ||
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10.1007/s10584-023-03487-3 doi (DE-627)SPR049122231 (SPR)s10584-023-03487-3-e DE-627 ger DE-627 rakwb eng Zhang, Yanfei verfasserin (orcid)0000-0002-7211-7238 aut Investigation of lake shrinkage attributed to climate change over the past 33 years in Inner Mongolia, China 2023 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Author(s), under exclusive licence to Springer Nature B.V. 2023. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. Abstract Inner Mongolia, located in northern China and bordered by Mongolia and Russia, has numerous lakes. Constrained by water scarcity, precious lakes play key roles in degraded grassland ecosystems and the social and economic development of Inner Mongolia. This study combines 1815 Landsat image interpretations and ground-based surveys to track the area changes in 573 lakes in Inner Mongolia during the period 1987–2019. Our results demonstrate that the number of dried-up lakes increased by 0.87 per year, the number of lakes with water areas below 0.1 $ km^{2} $ increased by 1.02 per year, and the number of lakes with water areas between 0.1 and 1 $ km^{2} $ increased by 0.39 per year. The number of lakes with areas larger than 1 $ km^{2} $ shows a decreased or fluctuating trend. The lake area in Inner Mongolia increased at a rate of 7.04 $ km^{2} $/year from 1987 to 1998 but then shows an overall decreasing trend at a rate of 0.71 $ km^{2} $/year over the next 20 years. The period from 1999 to 2010 was the most serious period of lake shrinkage in Inner Mongolia in the past 30 years, with a shrinkage rate of 33.99 $ km^{2} $/year. The climate changes from wet to dry and from dry to wet are the main reasons for the breakpoint occurrence of the lake area time series in the 2000s and 2010s, respectively. The response of lake area changes to climate-related factors has significant regional differences. In addition, intensification of human activities, such as the rapid development of livestock and coal mining, is also the main driver of lake change. The multiple regression model shows that the contribution of climate-related variables and human activity–related variables to the change in lake area over the 1987–2019 time period was about 40% and 60%, respectively. Lake shrinkage (dpeaa)DE-He213 Climate change (dpeaa)DE-He213 Inner Mongolia (dpeaa)DE-He213 Landsat (dpeaa)DE-He213 Time series (dpeaa)DE-He213 Liao, Zilong aut Xu, Xiaomin aut Liang, Wentao aut Han, Zhenhua aut Ji, Gang aut Jiao, Rui aut Enthalten in Climatic change Dordrecht [u.a.] : Springer Science + Business Media B.V, 1977 176(2023), 2 vom: 23. Jan. (DE-627)270429514 (DE-600)1477652-2 1573-1480 nnns volume:176 year:2023 number:2 day:23 month:01 https://dx.doi.org/10.1007/s10584-023-03487-3 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_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_381 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_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_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 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_2118 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_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_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 176 2023 2 23 01 |
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10.1007/s10584-023-03487-3 doi (DE-627)SPR049122231 (SPR)s10584-023-03487-3-e DE-627 ger DE-627 rakwb eng Zhang, Yanfei verfasserin (orcid)0000-0002-7211-7238 aut Investigation of lake shrinkage attributed to climate change over the past 33 years in Inner Mongolia, China 2023 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Author(s), under exclusive licence to Springer Nature B.V. 2023. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. Abstract Inner Mongolia, located in northern China and bordered by Mongolia and Russia, has numerous lakes. Constrained by water scarcity, precious lakes play key roles in degraded grassland ecosystems and the social and economic development of Inner Mongolia. This study combines 1815 Landsat image interpretations and ground-based surveys to track the area changes in 573 lakes in Inner Mongolia during the period 1987–2019. Our results demonstrate that the number of dried-up lakes increased by 0.87 per year, the number of lakes with water areas below 0.1 $ km^{2} $ increased by 1.02 per year, and the number of lakes with water areas between 0.1 and 1 $ km^{2} $ increased by 0.39 per year. The number of lakes with areas larger than 1 $ km^{2} $ shows a decreased or fluctuating trend. The lake area in Inner Mongolia increased at a rate of 7.04 $ km^{2} $/year from 1987 to 1998 but then shows an overall decreasing trend at a rate of 0.71 $ km^{2} $/year over the next 20 years. The period from 1999 to 2010 was the most serious period of lake shrinkage in Inner Mongolia in the past 30 years, with a shrinkage rate of 33.99 $ km^{2} $/year. The climate changes from wet to dry and from dry to wet are the main reasons for the breakpoint occurrence of the lake area time series in the 2000s and 2010s, respectively. The response of lake area changes to climate-related factors has significant regional differences. In addition, intensification of human activities, such as the rapid development of livestock and coal mining, is also the main driver of lake change. The multiple regression model shows that the contribution of climate-related variables and human activity–related variables to the change in lake area over the 1987–2019 time period was about 40% and 60%, respectively. Lake shrinkage (dpeaa)DE-He213 Climate change (dpeaa)DE-He213 Inner Mongolia (dpeaa)DE-He213 Landsat (dpeaa)DE-He213 Time series (dpeaa)DE-He213 Liao, Zilong aut Xu, Xiaomin aut Liang, Wentao aut Han, Zhenhua aut Ji, Gang aut Jiao, Rui aut Enthalten in Climatic change Dordrecht [u.a.] : Springer Science + Business Media B.V, 1977 176(2023), 2 vom: 23. Jan. (DE-627)270429514 (DE-600)1477652-2 1573-1480 nnns volume:176 year:2023 number:2 day:23 month:01 https://dx.doi.org/10.1007/s10584-023-03487-3 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_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_381 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_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_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 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_2118 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_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_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 176 2023 2 23 01 |
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10.1007/s10584-023-03487-3 doi (DE-627)SPR049122231 (SPR)s10584-023-03487-3-e DE-627 ger DE-627 rakwb eng Zhang, Yanfei verfasserin (orcid)0000-0002-7211-7238 aut Investigation of lake shrinkage attributed to climate change over the past 33 years in Inner Mongolia, China 2023 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Author(s), under exclusive licence to Springer Nature B.V. 2023. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. Abstract Inner Mongolia, located in northern China and bordered by Mongolia and Russia, has numerous lakes. Constrained by water scarcity, precious lakes play key roles in degraded grassland ecosystems and the social and economic development of Inner Mongolia. This study combines 1815 Landsat image interpretations and ground-based surveys to track the area changes in 573 lakes in Inner Mongolia during the period 1987–2019. Our results demonstrate that the number of dried-up lakes increased by 0.87 per year, the number of lakes with water areas below 0.1 $ km^{2} $ increased by 1.02 per year, and the number of lakes with water areas between 0.1 and 1 $ km^{2} $ increased by 0.39 per year. The number of lakes with areas larger than 1 $ km^{2} $ shows a decreased or fluctuating trend. The lake area in Inner Mongolia increased at a rate of 7.04 $ km^{2} $/year from 1987 to 1998 but then shows an overall decreasing trend at a rate of 0.71 $ km^{2} $/year over the next 20 years. The period from 1999 to 2010 was the most serious period of lake shrinkage in Inner Mongolia in the past 30 years, with a shrinkage rate of 33.99 $ km^{2} $/year. The climate changes from wet to dry and from dry to wet are the main reasons for the breakpoint occurrence of the lake area time series in the 2000s and 2010s, respectively. The response of lake area changes to climate-related factors has significant regional differences. In addition, intensification of human activities, such as the rapid development of livestock and coal mining, is also the main driver of lake change. The multiple regression model shows that the contribution of climate-related variables and human activity–related variables to the change in lake area over the 1987–2019 time period was about 40% and 60%, respectively. Lake shrinkage (dpeaa)DE-He213 Climate change (dpeaa)DE-He213 Inner Mongolia (dpeaa)DE-He213 Landsat (dpeaa)DE-He213 Time series (dpeaa)DE-He213 Liao, Zilong aut Xu, Xiaomin aut Liang, Wentao aut Han, Zhenhua aut Ji, Gang aut Jiao, Rui aut Enthalten in Climatic change Dordrecht [u.a.] : Springer Science + Business Media B.V, 1977 176(2023), 2 vom: 23. Jan. (DE-627)270429514 (DE-600)1477652-2 1573-1480 nnns volume:176 year:2023 number:2 day:23 month:01 https://dx.doi.org/10.1007/s10584-023-03487-3 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_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_381 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_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_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 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_2118 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_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_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 176 2023 2 23 01 |
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10.1007/s10584-023-03487-3 doi (DE-627)SPR049122231 (SPR)s10584-023-03487-3-e DE-627 ger DE-627 rakwb eng Zhang, Yanfei verfasserin (orcid)0000-0002-7211-7238 aut Investigation of lake shrinkage attributed to climate change over the past 33 years in Inner Mongolia, China 2023 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Author(s), under exclusive licence to Springer Nature B.V. 2023. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. Abstract Inner Mongolia, located in northern China and bordered by Mongolia and Russia, has numerous lakes. Constrained by water scarcity, precious lakes play key roles in degraded grassland ecosystems and the social and economic development of Inner Mongolia. This study combines 1815 Landsat image interpretations and ground-based surveys to track the area changes in 573 lakes in Inner Mongolia during the period 1987–2019. Our results demonstrate that the number of dried-up lakes increased by 0.87 per year, the number of lakes with water areas below 0.1 $ km^{2} $ increased by 1.02 per year, and the number of lakes with water areas between 0.1 and 1 $ km^{2} $ increased by 0.39 per year. The number of lakes with areas larger than 1 $ km^{2} $ shows a decreased or fluctuating trend. The lake area in Inner Mongolia increased at a rate of 7.04 $ km^{2} $/year from 1987 to 1998 but then shows an overall decreasing trend at a rate of 0.71 $ km^{2} $/year over the next 20 years. The period from 1999 to 2010 was the most serious period of lake shrinkage in Inner Mongolia in the past 30 years, with a shrinkage rate of 33.99 $ km^{2} $/year. The climate changes from wet to dry and from dry to wet are the main reasons for the breakpoint occurrence of the lake area time series in the 2000s and 2010s, respectively. The response of lake area changes to climate-related factors has significant regional differences. In addition, intensification of human activities, such as the rapid development of livestock and coal mining, is also the main driver of lake change. The multiple regression model shows that the contribution of climate-related variables and human activity–related variables to the change in lake area over the 1987–2019 time period was about 40% and 60%, respectively. Lake shrinkage (dpeaa)DE-He213 Climate change (dpeaa)DE-He213 Inner Mongolia (dpeaa)DE-He213 Landsat (dpeaa)DE-He213 Time series (dpeaa)DE-He213 Liao, Zilong aut Xu, Xiaomin aut Liang, Wentao aut Han, Zhenhua aut Ji, Gang aut Jiao, Rui aut Enthalten in Climatic change Dordrecht [u.a.] : Springer Science + Business Media B.V, 1977 176(2023), 2 vom: 23. Jan. (DE-627)270429514 (DE-600)1477652-2 1573-1480 nnns volume:176 year:2023 number:2 day:23 month:01 https://dx.doi.org/10.1007/s10584-023-03487-3 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_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_381 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_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_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 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_2118 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_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_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 176 2023 2 23 01 |
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10.1007/s10584-023-03487-3 doi (DE-627)SPR049122231 (SPR)s10584-023-03487-3-e DE-627 ger DE-627 rakwb eng Zhang, Yanfei verfasserin (orcid)0000-0002-7211-7238 aut Investigation of lake shrinkage attributed to climate change over the past 33 years in Inner Mongolia, China 2023 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Author(s), under exclusive licence to Springer Nature B.V. 2023. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. Abstract Inner Mongolia, located in northern China and bordered by Mongolia and Russia, has numerous lakes. Constrained by water scarcity, precious lakes play key roles in degraded grassland ecosystems and the social and economic development of Inner Mongolia. This study combines 1815 Landsat image interpretations and ground-based surveys to track the area changes in 573 lakes in Inner Mongolia during the period 1987–2019. Our results demonstrate that the number of dried-up lakes increased by 0.87 per year, the number of lakes with water areas below 0.1 $ km^{2} $ increased by 1.02 per year, and the number of lakes with water areas between 0.1 and 1 $ km^{2} $ increased by 0.39 per year. The number of lakes with areas larger than 1 $ km^{2} $ shows a decreased or fluctuating trend. The lake area in Inner Mongolia increased at a rate of 7.04 $ km^{2} $/year from 1987 to 1998 but then shows an overall decreasing trend at a rate of 0.71 $ km^{2} $/year over the next 20 years. The period from 1999 to 2010 was the most serious period of lake shrinkage in Inner Mongolia in the past 30 years, with a shrinkage rate of 33.99 $ km^{2} $/year. The climate changes from wet to dry and from dry to wet are the main reasons for the breakpoint occurrence of the lake area time series in the 2000s and 2010s, respectively. The response of lake area changes to climate-related factors has significant regional differences. In addition, intensification of human activities, such as the rapid development of livestock and coal mining, is also the main driver of lake change. The multiple regression model shows that the contribution of climate-related variables and human activity–related variables to the change in lake area over the 1987–2019 time period was about 40% and 60%, respectively. Lake shrinkage (dpeaa)DE-He213 Climate change (dpeaa)DE-He213 Inner Mongolia (dpeaa)DE-He213 Landsat (dpeaa)DE-He213 Time series (dpeaa)DE-He213 Liao, Zilong aut Xu, Xiaomin aut Liang, Wentao aut Han, Zhenhua aut Ji, Gang aut Jiao, Rui aut Enthalten in Climatic change Dordrecht [u.a.] : Springer Science + Business Media B.V, 1977 176(2023), 2 vom: 23. Jan. (DE-627)270429514 (DE-600)1477652-2 1573-1480 nnns volume:176 year:2023 number:2 day:23 month:01 https://dx.doi.org/10.1007/s10584-023-03487-3 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_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_381 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_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_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 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_2118 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_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_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 176 2023 2 23 01 |
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Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law.</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Abstract Inner Mongolia, located in northern China and bordered by Mongolia and Russia, has numerous lakes. Constrained by water scarcity, precious lakes play key roles in degraded grassland ecosystems and the social and economic development of Inner Mongolia. This study combines 1815 Landsat image interpretations and ground-based surveys to track the area changes in 573 lakes in Inner Mongolia during the period 1987–2019. Our results demonstrate that the number of dried-up lakes increased by 0.87 per year, the number of lakes with water areas below 0.1 $ km^{2} $ increased by 1.02 per year, and the number of lakes with water areas between 0.1 and 1 $ km^{2} $ increased by 0.39 per year. The number of lakes with areas larger than 1 $ km^{2} $ shows a decreased or fluctuating trend. The lake area in Inner Mongolia increased at a rate of 7.04 $ km^{2} $/year from 1987 to 1998 but then shows an overall decreasing trend at a rate of 0.71 $ km^{2} $/year over the next 20 years. The period from 1999 to 2010 was the most serious period of lake shrinkage in Inner Mongolia in the past 30 years, with a shrinkage rate of 33.99 $ km^{2} $/year. The climate changes from wet to dry and from dry to wet are the main reasons for the breakpoint occurrence of the lake area time series in the 2000s and 2010s, respectively. The response of lake area changes to climate-related factors has significant regional differences. In addition, intensification of human activities, such as the rapid development of livestock and coal mining, is also the main driver of lake change. 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Zhang, Yanfei |
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Zhang, Yanfei misc Lake shrinkage misc Climate change misc Inner Mongolia misc Landsat misc Time series Investigation of lake shrinkage attributed to climate change over the past 33 years in Inner Mongolia, China |
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Investigation of lake shrinkage attributed to climate change over the past 33 years in Inner Mongolia, China Lake shrinkage (dpeaa)DE-He213 Climate change (dpeaa)DE-He213 Inner Mongolia (dpeaa)DE-He213 Landsat (dpeaa)DE-He213 Time series (dpeaa)DE-He213 |
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Zhang, Yanfei Liao, Zilong Xu, Xiaomin Liang, Wentao Han, Zhenhua Ji, Gang Jiao, Rui |
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investigation of lake shrinkage attributed to climate change over the past 33 years in inner mongolia, china |
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Investigation of lake shrinkage attributed to climate change over the past 33 years in Inner Mongolia, China |
| abstract |
Abstract Inner Mongolia, located in northern China and bordered by Mongolia and Russia, has numerous lakes. Constrained by water scarcity, precious lakes play key roles in degraded grassland ecosystems and the social and economic development of Inner Mongolia. This study combines 1815 Landsat image interpretations and ground-based surveys to track the area changes in 573 lakes in Inner Mongolia during the period 1987–2019. Our results demonstrate that the number of dried-up lakes increased by 0.87 per year, the number of lakes with water areas below 0.1 $ km^{2} $ increased by 1.02 per year, and the number of lakes with water areas between 0.1 and 1 $ km^{2} $ increased by 0.39 per year. The number of lakes with areas larger than 1 $ km^{2} $ shows a decreased or fluctuating trend. The lake area in Inner Mongolia increased at a rate of 7.04 $ km^{2} $/year from 1987 to 1998 but then shows an overall decreasing trend at a rate of 0.71 $ km^{2} $/year over the next 20 years. The period from 1999 to 2010 was the most serious period of lake shrinkage in Inner Mongolia in the past 30 years, with a shrinkage rate of 33.99 $ km^{2} $/year. The climate changes from wet to dry and from dry to wet are the main reasons for the breakpoint occurrence of the lake area time series in the 2000s and 2010s, respectively. The response of lake area changes to climate-related factors has significant regional differences. In addition, intensification of human activities, such as the rapid development of livestock and coal mining, is also the main driver of lake change. The multiple regression model shows that the contribution of climate-related variables and human activity–related variables to the change in lake area over the 1987–2019 time period was about 40% and 60%, respectively. © The Author(s), under exclusive licence to Springer Nature B.V. 2023. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. |
| abstractGer |
Abstract Inner Mongolia, located in northern China and bordered by Mongolia and Russia, has numerous lakes. Constrained by water scarcity, precious lakes play key roles in degraded grassland ecosystems and the social and economic development of Inner Mongolia. This study combines 1815 Landsat image interpretations and ground-based surveys to track the area changes in 573 lakes in Inner Mongolia during the period 1987–2019. Our results demonstrate that the number of dried-up lakes increased by 0.87 per year, the number of lakes with water areas below 0.1 $ km^{2} $ increased by 1.02 per year, and the number of lakes with water areas between 0.1 and 1 $ km^{2} $ increased by 0.39 per year. The number of lakes with areas larger than 1 $ km^{2} $ shows a decreased or fluctuating trend. The lake area in Inner Mongolia increased at a rate of 7.04 $ km^{2} $/year from 1987 to 1998 but then shows an overall decreasing trend at a rate of 0.71 $ km^{2} $/year over the next 20 years. The period from 1999 to 2010 was the most serious period of lake shrinkage in Inner Mongolia in the past 30 years, with a shrinkage rate of 33.99 $ km^{2} $/year. The climate changes from wet to dry and from dry to wet are the main reasons for the breakpoint occurrence of the lake area time series in the 2000s and 2010s, respectively. The response of lake area changes to climate-related factors has significant regional differences. In addition, intensification of human activities, such as the rapid development of livestock and coal mining, is also the main driver of lake change. The multiple regression model shows that the contribution of climate-related variables and human activity–related variables to the change in lake area over the 1987–2019 time period was about 40% and 60%, respectively. © The Author(s), under exclusive licence to Springer Nature B.V. 2023. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. |
| abstract_unstemmed |
Abstract Inner Mongolia, located in northern China and bordered by Mongolia and Russia, has numerous lakes. Constrained by water scarcity, precious lakes play key roles in degraded grassland ecosystems and the social and economic development of Inner Mongolia. This study combines 1815 Landsat image interpretations and ground-based surveys to track the area changes in 573 lakes in Inner Mongolia during the period 1987–2019. Our results demonstrate that the number of dried-up lakes increased by 0.87 per year, the number of lakes with water areas below 0.1 $ km^{2} $ increased by 1.02 per year, and the number of lakes with water areas between 0.1 and 1 $ km^{2} $ increased by 0.39 per year. The number of lakes with areas larger than 1 $ km^{2} $ shows a decreased or fluctuating trend. The lake area in Inner Mongolia increased at a rate of 7.04 $ km^{2} $/year from 1987 to 1998 but then shows an overall decreasing trend at a rate of 0.71 $ km^{2} $/year over the next 20 years. The period from 1999 to 2010 was the most serious period of lake shrinkage in Inner Mongolia in the past 30 years, with a shrinkage rate of 33.99 $ km^{2} $/year. The climate changes from wet to dry and from dry to wet are the main reasons for the breakpoint occurrence of the lake area time series in the 2000s and 2010s, respectively. The response of lake area changes to climate-related factors has significant regional differences. In addition, intensification of human activities, such as the rapid development of livestock and coal mining, is also the main driver of lake change. The multiple regression model shows that the contribution of climate-related variables and human activity–related variables to the change in lake area over the 1987–2019 time period was about 40% and 60%, respectively. © The Author(s), under exclusive licence to Springer Nature B.V. 2023. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. |
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| title_short |
Investigation of lake shrinkage attributed to climate change over the past 33 years in Inner Mongolia, China |
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Liao, Zilong Xu, Xiaomin Liang, Wentao Han, Zhenhua Ji, Gang Jiao, Rui |
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Liao, Zilong Xu, Xiaomin Liang, Wentao Han, Zhenhua Ji, Gang Jiao, Rui |
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| score |
7.3985567 |