Lake Inventory and Evolution of Glacial Lakes in the Nubra-Shyok Basin of Karakoram Range

Abstract The trends of glacier lake evolution during the past few decades and their future development are still not well understood. The aim of the present study is to investigate the growth and changes in moraine and bed rock dammed glacier lakes of the Nubra and Shyok basin, Karakoram Range using...
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Autor*in:	Kumar, Rajesh [verfasserIn] Bahuguna, I. M. [verfasserIn] Ali, S. Nawaz [verfasserIn] Singh, Rupendra [verfasserIn]

Format:	E-Artikel
Sprache:	Englisch

Erschienen:	2019

Schlagwörter:	Lake inventory Moraine-dammed lake GLOF Sentinel 2

Übergeordnetes Werk:	Enthalten in: Earth systems and environment - [Cham] : Springer International Publishing, 2017, 4(2019), 1 vom: 22. Okt., Seite 57-70
Übergeordnetes Werk:	volume:4 ; year:2019 ; number:1 ; day:22 ; month:10 ; pages:57-70

Links:	Volltext

DOI / URN:	10.1007/s41748-019-00129-6

Katalog-ID:	SPR039179303

Internformat


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520			\|a Abstract The trends of glacier lake evolution during the past few decades and their future development are still not well understood. The aim of the present study is to investigate the growth and changes in moraine and bed rock dammed glacier lakes of the Nubra and Shyok basin, Karakoram Range using multi-temporal satellite images. The glacier lake inventory is based on Landsat 7 and 8 (15 m spatial resolution), and Sentinels 2A (10 m spatial resolution) satellite imageries. The data revealed that during the years 2002–2017, the number of glacial lakes increased from 215 to 255. The glacial lake area also increased from ~ 9.0 $ km^{2} $ in 2003 to ~ 9.36 $ km^{2} $ in 2013 and ~ 11.27 $ km^{2} $ in 2017. During 2002–2017, the lake area increased by ~ 2.27 $ km^{2} $, out of which ~ 1.9 $ km^{2} $ increase is recorded between 2013 and 2017 accounts for almost 84% of the total increase. The lakes with an area of ≥ 0.2 $ km^{2} $ have been considered for glacial lake outburst flood (GLOF) susceptibility studies and volume estimation. Analyses of the data show a progressive increase in number of glacial lakes and their areal extent. This study would help planners to minimize the adverse effects of GLOF in the Nubra-Shyok basin.
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700	1		\|a Bahuguna, I. M. \|e verfasserin \|4 aut
700	1		\|a Ali, S. Nawaz \|e verfasserin \|4 aut
700	1		\|a Singh, Rupendra \|e verfasserin \|4 aut
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912			\|a GBV_ILN_110
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912			\|a GBV_ILN_138
912			\|a GBV_ILN_150
912			\|a GBV_ILN_151
912			\|a GBV_ILN_161
912			\|a GBV_ILN_170
912			\|a GBV_ILN_171
912			\|a GBV_ILN_187
912			\|a GBV_ILN_213
912			\|a GBV_ILN_224
912			\|a GBV_ILN_230
912			\|a GBV_ILN_250
912			\|a GBV_ILN_266
912			\|a GBV_ILN_281
912			\|a GBV_ILN_285
912			\|a GBV_ILN_293
912			\|a GBV_ILN_370
912			\|a GBV_ILN_602
912			\|a GBV_ILN_636
912			\|a GBV_ILN_702
912			\|a GBV_ILN_2001
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912			\|a GBV_ILN_2044
912			\|a GBV_ILN_2048
912			\|a GBV_ILN_2049
912			\|a GBV_ILN_2050
912			\|a GBV_ILN_2055
912			\|a GBV_ILN_2057
912			\|a GBV_ILN_2059
912			\|a GBV_ILN_2061
912			\|a GBV_ILN_2064
912			\|a GBV_ILN_2065
912			\|a GBV_ILN_2068
912			\|a GBV_ILN_2070
912			\|a GBV_ILN_2086
912			\|a GBV_ILN_2088
912			\|a GBV_ILN_2093
912			\|a GBV_ILN_2106
912			\|a GBV_ILN_2107
912			\|a GBV_ILN_2108
912			\|a GBV_ILN_2110
912			\|a GBV_ILN_2111
912			\|a GBV_ILN_2112
912			\|a GBV_ILN_2113
912			\|a GBV_ILN_2116
912			\|a GBV_ILN_2118
912			\|a GBV_ILN_2119
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author_variant	r k rk i m b im imb s n a sn sna r s rs
matchkey_str	article:25099434:2019----::aenetradvltoogailaeiteursyk
hierarchy_sort_str	2019
publishDate	2019
allfields	10.1007/s41748-019-00129-6 doi (DE-627)SPR039179303 (SPR)s41748-019-00129-6-e DE-627 ger DE-627 rakwb eng 550 ASE 550 ASE Kumar, Rajesh verfasserin aut Lake Inventory and Evolution of Glacial Lakes in the Nubra-Shyok Basin of Karakoram Range 2019 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract The trends of glacier lake evolution during the past few decades and their future development are still not well understood. The aim of the present study is to investigate the growth and changes in moraine and bed rock dammed glacier lakes of the Nubra and Shyok basin, Karakoram Range using multi-temporal satellite images. The glacier lake inventory is based on Landsat 7 and 8 (15 m spatial resolution), and Sentinels 2A (10 m spatial resolution) satellite imageries. The data revealed that during the years 2002–2017, the number of glacial lakes increased from 215 to 255. The glacial lake area also increased from ~ 9.0 $ km^{2} $ in 2003 to ~ 9.36 $ km^{2} $ in 2013 and ~ 11.27 $ km^{2} $ in 2017. During 2002–2017, the lake area increased by ~ 2.27 $ km^{2} $, out of which ~ 1.9 $ km^{2} $ increase is recorded between 2013 and 2017 accounts for almost 84% of the total increase. The lakes with an area of ≥ 0.2 $ km^{2} $ have been considered for glacial lake outburst flood (GLOF) susceptibility studies and volume estimation. Analyses of the data show a progressive increase in number of glacial lakes and their areal extent. This study would help planners to minimize the adverse effects of GLOF in the Nubra-Shyok basin. Lake inventory (dpeaa)DE-He213 Moraine-dammed lake (dpeaa)DE-He213 GLOF (dpeaa)DE-He213 Sentinel 2 (dpeaa)DE-He213 Bahuguna, I. M. verfasserin aut Ali, S. Nawaz verfasserin aut Singh, Rupendra verfasserin aut Enthalten in Earth systems and environment [Cham] : Springer International Publishing, 2017 4(2019), 1 vom: 22. Okt., Seite 57-70 (DE-627)884895904 (DE-600)2892530-0 2509-9434 nnns volume:4 year:2019 number:1 day:22 month:10 pages:57-70 https://dx.doi.org/10.1007/s41748-019-00129-6 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-ASE 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_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_266 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 4 2019 1 22 10 57-70
spelling	10.1007/s41748-019-00129-6 doi (DE-627)SPR039179303 (SPR)s41748-019-00129-6-e DE-627 ger DE-627 rakwb eng 550 ASE 550 ASE Kumar, Rajesh verfasserin aut Lake Inventory and Evolution of Glacial Lakes in the Nubra-Shyok Basin of Karakoram Range 2019 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract The trends of glacier lake evolution during the past few decades and their future development are still not well understood. The aim of the present study is to investigate the growth and changes in moraine and bed rock dammed glacier lakes of the Nubra and Shyok basin, Karakoram Range using multi-temporal satellite images. The glacier lake inventory is based on Landsat 7 and 8 (15 m spatial resolution), and Sentinels 2A (10 m spatial resolution) satellite imageries. The data revealed that during the years 2002–2017, the number of glacial lakes increased from 215 to 255. The glacial lake area also increased from ~ 9.0 $ km^{2} $ in 2003 to ~ 9.36 $ km^{2} $ in 2013 and ~ 11.27 $ km^{2} $ in 2017. During 2002–2017, the lake area increased by ~ 2.27 $ km^{2} $, out of which ~ 1.9 $ km^{2} $ increase is recorded between 2013 and 2017 accounts for almost 84% of the total increase. The lakes with an area of ≥ 0.2 $ km^{2} $ have been considered for glacial lake outburst flood (GLOF) susceptibility studies and volume estimation. Analyses of the data show a progressive increase in number of glacial lakes and their areal extent. This study would help planners to minimize the adverse effects of GLOF in the Nubra-Shyok basin. Lake inventory (dpeaa)DE-He213 Moraine-dammed lake (dpeaa)DE-He213 GLOF (dpeaa)DE-He213 Sentinel 2 (dpeaa)DE-He213 Bahuguna, I. M. verfasserin aut Ali, S. Nawaz verfasserin aut Singh, Rupendra verfasserin aut Enthalten in Earth systems and environment [Cham] : Springer International Publishing, 2017 4(2019), 1 vom: 22. Okt., Seite 57-70 (DE-627)884895904 (DE-600)2892530-0 2509-9434 nnns volume:4 year:2019 number:1 day:22 month:10 pages:57-70 https://dx.doi.org/10.1007/s41748-019-00129-6 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-ASE 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_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_266 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 4 2019 1 22 10 57-70
allfields_unstemmed	10.1007/s41748-019-00129-6 doi (DE-627)SPR039179303 (SPR)s41748-019-00129-6-e DE-627 ger DE-627 rakwb eng 550 ASE 550 ASE Kumar, Rajesh verfasserin aut Lake Inventory and Evolution of Glacial Lakes in the Nubra-Shyok Basin of Karakoram Range 2019 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract The trends of glacier lake evolution during the past few decades and their future development are still not well understood. The aim of the present study is to investigate the growth and changes in moraine and bed rock dammed glacier lakes of the Nubra and Shyok basin, Karakoram Range using multi-temporal satellite images. The glacier lake inventory is based on Landsat 7 and 8 (15 m spatial resolution), and Sentinels 2A (10 m spatial resolution) satellite imageries. The data revealed that during the years 2002–2017, the number of glacial lakes increased from 215 to 255. The glacial lake area also increased from ~ 9.0 $ km^{2} $ in 2003 to ~ 9.36 $ km^{2} $ in 2013 and ~ 11.27 $ km^{2} $ in 2017. During 2002–2017, the lake area increased by ~ 2.27 $ km^{2} $, out of which ~ 1.9 $ km^{2} $ increase is recorded between 2013 and 2017 accounts for almost 84% of the total increase. The lakes with an area of ≥ 0.2 $ km^{2} $ have been considered for glacial lake outburst flood (GLOF) susceptibility studies and volume estimation. Analyses of the data show a progressive increase in number of glacial lakes and their areal extent. This study would help planners to minimize the adverse effects of GLOF in the Nubra-Shyok basin. Lake inventory (dpeaa)DE-He213 Moraine-dammed lake (dpeaa)DE-He213 GLOF (dpeaa)DE-He213 Sentinel 2 (dpeaa)DE-He213 Bahuguna, I. M. verfasserin aut Ali, S. Nawaz verfasserin aut Singh, Rupendra verfasserin aut Enthalten in Earth systems and environment [Cham] : Springer International Publishing, 2017 4(2019), 1 vom: 22. Okt., Seite 57-70 (DE-627)884895904 (DE-600)2892530-0 2509-9434 nnns volume:4 year:2019 number:1 day:22 month:10 pages:57-70 https://dx.doi.org/10.1007/s41748-019-00129-6 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-ASE 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_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_266 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 4 2019 1 22 10 57-70
allfieldsGer	10.1007/s41748-019-00129-6 doi (DE-627)SPR039179303 (SPR)s41748-019-00129-6-e DE-627 ger DE-627 rakwb eng 550 ASE 550 ASE Kumar, Rajesh verfasserin aut Lake Inventory and Evolution of Glacial Lakes in the Nubra-Shyok Basin of Karakoram Range 2019 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract The trends of glacier lake evolution during the past few decades and their future development are still not well understood. The aim of the present study is to investigate the growth and changes in moraine and bed rock dammed glacier lakes of the Nubra and Shyok basin, Karakoram Range using multi-temporal satellite images. The glacier lake inventory is based on Landsat 7 and 8 (15 m spatial resolution), and Sentinels 2A (10 m spatial resolution) satellite imageries. The data revealed that during the years 2002–2017, the number of glacial lakes increased from 215 to 255. The glacial lake area also increased from ~ 9.0 $ km^{2} $ in 2003 to ~ 9.36 $ km^{2} $ in 2013 and ~ 11.27 $ km^{2} $ in 2017. During 2002–2017, the lake area increased by ~ 2.27 $ km^{2} $, out of which ~ 1.9 $ km^{2} $ increase is recorded between 2013 and 2017 accounts for almost 84% of the total increase. The lakes with an area of ≥ 0.2 $ km^{2} $ have been considered for glacial lake outburst flood (GLOF) susceptibility studies and volume estimation. Analyses of the data show a progressive increase in number of glacial lakes and their areal extent. This study would help planners to minimize the adverse effects of GLOF in the Nubra-Shyok basin. Lake inventory (dpeaa)DE-He213 Moraine-dammed lake (dpeaa)DE-He213 GLOF (dpeaa)DE-He213 Sentinel 2 (dpeaa)DE-He213 Bahuguna, I. M. verfasserin aut Ali, S. Nawaz verfasserin aut Singh, Rupendra verfasserin aut Enthalten in Earth systems and environment [Cham] : Springer International Publishing, 2017 4(2019), 1 vom: 22. Okt., Seite 57-70 (DE-627)884895904 (DE-600)2892530-0 2509-9434 nnns volume:4 year:2019 number:1 day:22 month:10 pages:57-70 https://dx.doi.org/10.1007/s41748-019-00129-6 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-ASE 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_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_266 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 4 2019 1 22 10 57-70
allfieldsSound	10.1007/s41748-019-00129-6 doi (DE-627)SPR039179303 (SPR)s41748-019-00129-6-e DE-627 ger DE-627 rakwb eng 550 ASE 550 ASE Kumar, Rajesh verfasserin aut Lake Inventory and Evolution of Glacial Lakes in the Nubra-Shyok Basin of Karakoram Range 2019 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract The trends of glacier lake evolution during the past few decades and their future development are still not well understood. The aim of the present study is to investigate the growth and changes in moraine and bed rock dammed glacier lakes of the Nubra and Shyok basin, Karakoram Range using multi-temporal satellite images. The glacier lake inventory is based on Landsat 7 and 8 (15 m spatial resolution), and Sentinels 2A (10 m spatial resolution) satellite imageries. The data revealed that during the years 2002–2017, the number of glacial lakes increased from 215 to 255. The glacial lake area also increased from ~ 9.0 $ km^{2} $ in 2003 to ~ 9.36 $ km^{2} $ in 2013 and ~ 11.27 $ km^{2} $ in 2017. During 2002–2017, the lake area increased by ~ 2.27 $ km^{2} $, out of which ~ 1.9 $ km^{2} $ increase is recorded between 2013 and 2017 accounts for almost 84% of the total increase. The lakes with an area of ≥ 0.2 $ km^{2} $ have been considered for glacial lake outburst flood (GLOF) susceptibility studies and volume estimation. Analyses of the data show a progressive increase in number of glacial lakes and their areal extent. This study would help planners to minimize the adverse effects of GLOF in the Nubra-Shyok basin. Lake inventory (dpeaa)DE-He213 Moraine-dammed lake (dpeaa)DE-He213 GLOF (dpeaa)DE-He213 Sentinel 2 (dpeaa)DE-He213 Bahuguna, I. M. verfasserin aut Ali, S. Nawaz verfasserin aut Singh, Rupendra verfasserin aut Enthalten in Earth systems and environment [Cham] : Springer International Publishing, 2017 4(2019), 1 vom: 22. Okt., Seite 57-70 (DE-627)884895904 (DE-600)2892530-0 2509-9434 nnns volume:4 year:2019 number:1 day:22 month:10 pages:57-70 https://dx.doi.org/10.1007/s41748-019-00129-6 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-ASE 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_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_266 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 4 2019 1 22 10 57-70
language	English
source	Enthalten in Earth systems and environment 4(2019), 1 vom: 22. Okt., Seite 57-70 volume:4 year:2019 number:1 day:22 month:10 pages:57-70
sourceStr	Enthalten in Earth systems and environment 4(2019), 1 vom: 22. Okt., Seite 57-70 volume:4 year:2019 number:1 day:22 month:10 pages:57-70
format_phy_str_mv	Article
institution	findex.gbv.de
topic_facet	Lake inventory Moraine-dammed lake GLOF Sentinel 2
dewey-raw	550
isfreeaccess_bool	false
container_title	Earth systems and environment
authorswithroles_txt_mv	Kumar, Rajesh @@aut@@ Bahuguna, I. M. @@aut@@ Ali, S. Nawaz @@aut@@ Singh, Rupendra @@aut@@
publishDateDaySort_date	2019-10-22T00:00:00Z
hierarchy_top_id	884895904
dewey-sort	3550
id	SPR039179303
language_de	englisch
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author	Kumar, Rajesh
spellingShingle	Kumar, Rajesh ddc 550 misc Lake inventory misc Moraine-dammed lake misc GLOF misc Sentinel 2 Lake Inventory and Evolution of Glacial Lakes in the Nubra-Shyok Basin of Karakoram Range
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topic_title	550 ASE Lake Inventory and Evolution of Glacial Lakes in the Nubra-Shyok Basin of Karakoram Range Lake inventory (dpeaa)DE-He213 Moraine-dammed lake (dpeaa)DE-He213 GLOF (dpeaa)DE-He213 Sentinel 2 (dpeaa)DE-He213
topic	ddc 550 misc Lake inventory misc Moraine-dammed lake misc GLOF misc Sentinel 2
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title	Lake Inventory and Evolution of Glacial Lakes in the Nubra-Shyok Basin of Karakoram Range
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title_full	Lake Inventory and Evolution of Glacial Lakes in the Nubra-Shyok Basin of Karakoram Range
author_sort	Kumar, Rajesh
journal	Earth systems and environment
journalStr	Earth systems and environment
lang_code	eng
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author_browse	Kumar, Rajesh Bahuguna, I. M. Ali, S. Nawaz Singh, Rupendra
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class	550 ASE
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author-letter	Kumar, Rajesh
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dewey-full	550
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title_sort	lake inventory and evolution of glacial lakes in the nubra-shyok basin of karakoram range
title_auth	Lake Inventory and Evolution of Glacial Lakes in the Nubra-Shyok Basin of Karakoram Range
abstract	Abstract The trends of glacier lake evolution during the past few decades and their future development are still not well understood. The aim of the present study is to investigate the growth and changes in moraine and bed rock dammed glacier lakes of the Nubra and Shyok basin, Karakoram Range using multi-temporal satellite images. The glacier lake inventory is based on Landsat 7 and 8 (15 m spatial resolution), and Sentinels 2A (10 m spatial resolution) satellite imageries. The data revealed that during the years 2002–2017, the number of glacial lakes increased from 215 to 255. The glacial lake area also increased from ~ 9.0 $ km^{2} $ in 2003 to ~ 9.36 $ km^{2} $ in 2013 and ~ 11.27 $ km^{2} $ in 2017. During 2002–2017, the lake area increased by ~ 2.27 $ km^{2} $, out of which ~ 1.9 $ km^{2} $ increase is recorded between 2013 and 2017 accounts for almost 84% of the total increase. The lakes with an area of ≥ 0.2 $ km^{2} $ have been considered for glacial lake outburst flood (GLOF) susceptibility studies and volume estimation. Analyses of the data show a progressive increase in number of glacial lakes and their areal extent. This study would help planners to minimize the adverse effects of GLOF in the Nubra-Shyok basin.
abstractGer	Abstract The trends of glacier lake evolution during the past few decades and their future development are still not well understood. The aim of the present study is to investigate the growth and changes in moraine and bed rock dammed glacier lakes of the Nubra and Shyok basin, Karakoram Range using multi-temporal satellite images. The glacier lake inventory is based on Landsat 7 and 8 (15 m spatial resolution), and Sentinels 2A (10 m spatial resolution) satellite imageries. The data revealed that during the years 2002–2017, the number of glacial lakes increased from 215 to 255. The glacial lake area also increased from ~ 9.0 $ km^{2} $ in 2003 to ~ 9.36 $ km^{2} $ in 2013 and ~ 11.27 $ km^{2} $ in 2017. During 2002–2017, the lake area increased by ~ 2.27 $ km^{2} $, out of which ~ 1.9 $ km^{2} $ increase is recorded between 2013 and 2017 accounts for almost 84% of the total increase. The lakes with an area of ≥ 0.2 $ km^{2} $ have been considered for glacial lake outburst flood (GLOF) susceptibility studies and volume estimation. Analyses of the data show a progressive increase in number of glacial lakes and their areal extent. This study would help planners to minimize the adverse effects of GLOF in the Nubra-Shyok basin.
abstract_unstemmed	Abstract The trends of glacier lake evolution during the past few decades and their future development are still not well understood. The aim of the present study is to investigate the growth and changes in moraine and bed rock dammed glacier lakes of the Nubra and Shyok basin, Karakoram Range using multi-temporal satellite images. The glacier lake inventory is based on Landsat 7 and 8 (15 m spatial resolution), and Sentinels 2A (10 m spatial resolution) satellite imageries. The data revealed that during the years 2002–2017, the number of glacial lakes increased from 215 to 255. The glacial lake area also increased from ~ 9.0 $ km^{2} $ in 2003 to ~ 9.36 $ km^{2} $ in 2013 and ~ 11.27 $ km^{2} $ in 2017. During 2002–2017, the lake area increased by ~ 2.27 $ km^{2} $, out of which ~ 1.9 $ km^{2} $ increase is recorded between 2013 and 2017 accounts for almost 84% of the total increase. The lakes with an area of ≥ 0.2 $ km^{2} $ have been considered for glacial lake outburst flood (GLOF) susceptibility studies and volume estimation. Analyses of the data show a progressive increase in number of glacial lakes and their areal extent. This study would help planners to minimize the adverse effects of GLOF in the Nubra-Shyok basin.
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title_short	Lake Inventory and Evolution of Glacial Lakes in the Nubra-Shyok Basin of Karakoram Range
url	https://dx.doi.org/10.1007/s41748-019-00129-6
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author2	Bahuguna, I. M. Ali, S. Nawaz Singh, Rupendra
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doi_str	10.1007/s41748-019-00129-6
up_date	2024-07-03T22:30:13.374Z
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fullrecord_marcxml	<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">SPR039179303</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20220112041125.0</controlfield><controlfield tag="007">cr uuu---uuuuu</controlfield><controlfield tag="008">201007s2019 xx \|\|\|\|\|o 00\| \|\|eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1007/s41748-019-00129-6</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)SPR039179303</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(SPR)s41748-019-00129-6-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="082" ind1="0" ind2="4"><subfield code="a">550</subfield><subfield code="q">ASE</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">550</subfield><subfield code="q">ASE</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Kumar, Rajesh</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Lake Inventory and Evolution of Glacial Lakes in the Nubra-Shyok Basin of Karakoram Range</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2019</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="520" ind1=" " ind2=" "><subfield code="a">Abstract The trends of glacier lake evolution during the past few decades and their future development are still not well understood. 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Lake Inventory and Evolution of Glacial Lakes in the Nubra-Shyok Basin of Karakoram Range

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