The large Aral Sea water balance: a future prospective of the large Aral Sea depending on water volume alteration
Abstract The Aral Sea is the biggest saline lake in Central Asia. The Amu Darya and Syr Darya rivers flow into the Aral Sea. These rivers were heavily used for irrigation fields after 1960 because of Soviet Union plans. Consequently, the Aral Sea separated into two parts: Large Aral Sea to the south...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Gaybullaev, Behzod [verfasserIn] |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2013 |
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| Schlagwörter: |
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| Anmerkung: |
© Springer-Verlag Berlin Heidelberg 2013 |
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| Übergeordnetes Werk: |
Enthalten in: Carbonates and evaporites - [Dordrecht [u.a.]] : Springer Netherlands, 1986, 29(2013), 2 vom: 06. Okt., Seite 211-219 |
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| Übergeordnetes Werk: |
volume:29 ; year:2013 ; number:2 ; day:06 ; month:10 ; pages:211-219 |
| Links: |
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| DOI / URN: |
10.1007/s13146-013-0174-1 |
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| Katalog-ID: |
SPR030658683 |
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| 100 | 1 | |a Gaybullaev, Behzod |e verfasserin |4 aut | |
| 245 | 1 | 4 | |a The large Aral Sea water balance: a future prospective of the large Aral Sea depending on water volume alteration |
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| 520 | |a Abstract The Aral Sea is the biggest saline lake in Central Asia. The Amu Darya and Syr Darya rivers flow into the Aral Sea. These rivers were heavily used for irrigation fields after 1960 because of Soviet Union plans. Consequently, the Aral Sea separated into two parts: Large Aral Sea to the south and a small Aral Sea in the north in 1987. The current study estimated the evaporation and precipitation rates of the Large Aral Sea by examining Aral Sea observed records from 1987 to 2011. As a result, the precipitation decreased exponentially from 5.8 $ km^{3} $ in 1987 to 2 $ km^{3} $ in 2011. Evaporation exponentially reduced from 34.2 $ km^{3} $ in 1987 to 5 $ km^{3} $ in 2011. The Nash–Sutcliffe model was used to predict the water volume by using previously observed and estimated data of the large Aral Sea precipitation, runoff, and evaporation from 2001 to 2025. The estimations indicate the large Aral Sea water volume will decrease to approximately 21.1 $ km^{3} $ in 2025 (R2 = 0.9654). The forecasted value of the water volume in the Large Aral Sea after 2025 will slowly decrease and eventually diminish to zero by 2057 if all variables remain unchanged. | ||
| 650 | 4 | |a Large Aral Sea |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Water volume |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Evaporation |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Precipitation |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Salinity |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Irrigation |7 (dpeaa)DE-He213 | |
| 700 | 1 | |a Chen, Su-Chin |4 aut | |
| 700 | 1 | |a Gaybullaev, Gulomjon |4 aut | |
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10.1007/s13146-013-0174-1 doi (DE-627)SPR030658683 (SPR)s13146-013-0174-1-e DE-627 ger DE-627 rakwb eng Gaybullaev, Behzod verfasserin aut The large Aral Sea water balance: a future prospective of the large Aral Sea depending on water volume alteration 2013 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Springer-Verlag Berlin Heidelberg 2013 Abstract The Aral Sea is the biggest saline lake in Central Asia. The Amu Darya and Syr Darya rivers flow into the Aral Sea. These rivers were heavily used for irrigation fields after 1960 because of Soviet Union plans. Consequently, the Aral Sea separated into two parts: Large Aral Sea to the south and a small Aral Sea in the north in 1987. The current study estimated the evaporation and precipitation rates of the Large Aral Sea by examining Aral Sea observed records from 1987 to 2011. As a result, the precipitation decreased exponentially from 5.8 $ km^{3} $ in 1987 to 2 $ km^{3} $ in 2011. Evaporation exponentially reduced from 34.2 $ km^{3} $ in 1987 to 5 $ km^{3} $ in 2011. The Nash–Sutcliffe model was used to predict the water volume by using previously observed and estimated data of the large Aral Sea precipitation, runoff, and evaporation from 2001 to 2025. The estimations indicate the large Aral Sea water volume will decrease to approximately 21.1 $ km^{3} $ in 2025 (R2 = 0.9654). The forecasted value of the water volume in the Large Aral Sea after 2025 will slowly decrease and eventually diminish to zero by 2057 if all variables remain unchanged. Large Aral Sea (dpeaa)DE-He213 Water volume (dpeaa)DE-He213 Evaporation (dpeaa)DE-He213 Precipitation (dpeaa)DE-He213 Salinity (dpeaa)DE-He213 Irrigation (dpeaa)DE-He213 Chen, Su-Chin aut Gaybullaev, Gulomjon aut Enthalten in Carbonates and evaporites [Dordrecht [u.a.]] : Springer Netherlands, 1986 29(2013), 2 vom: 06. Okt., Seite 211-219 (DE-627)617505799 (DE-600)2533885-7 1878-5212 nnns volume:29 year:2013 number:2 day:06 month:10 pages:211-219 https://dx.doi.org/10.1007/s13146-013-0174-1 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_206 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_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_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 29 2013 2 06 10 211-219 |
| spelling |
10.1007/s13146-013-0174-1 doi (DE-627)SPR030658683 (SPR)s13146-013-0174-1-e DE-627 ger DE-627 rakwb eng Gaybullaev, Behzod verfasserin aut The large Aral Sea water balance: a future prospective of the large Aral Sea depending on water volume alteration 2013 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Springer-Verlag Berlin Heidelberg 2013 Abstract The Aral Sea is the biggest saline lake in Central Asia. The Amu Darya and Syr Darya rivers flow into the Aral Sea. These rivers were heavily used for irrigation fields after 1960 because of Soviet Union plans. Consequently, the Aral Sea separated into two parts: Large Aral Sea to the south and a small Aral Sea in the north in 1987. The current study estimated the evaporation and precipitation rates of the Large Aral Sea by examining Aral Sea observed records from 1987 to 2011. As a result, the precipitation decreased exponentially from 5.8 $ km^{3} $ in 1987 to 2 $ km^{3} $ in 2011. Evaporation exponentially reduced from 34.2 $ km^{3} $ in 1987 to 5 $ km^{3} $ in 2011. The Nash–Sutcliffe model was used to predict the water volume by using previously observed and estimated data of the large Aral Sea precipitation, runoff, and evaporation from 2001 to 2025. The estimations indicate the large Aral Sea water volume will decrease to approximately 21.1 $ km^{3} $ in 2025 (R2 = 0.9654). The forecasted value of the water volume in the Large Aral Sea after 2025 will slowly decrease and eventually diminish to zero by 2057 if all variables remain unchanged. Large Aral Sea (dpeaa)DE-He213 Water volume (dpeaa)DE-He213 Evaporation (dpeaa)DE-He213 Precipitation (dpeaa)DE-He213 Salinity (dpeaa)DE-He213 Irrigation (dpeaa)DE-He213 Chen, Su-Chin aut Gaybullaev, Gulomjon aut Enthalten in Carbonates and evaporites [Dordrecht [u.a.]] : Springer Netherlands, 1986 29(2013), 2 vom: 06. Okt., Seite 211-219 (DE-627)617505799 (DE-600)2533885-7 1878-5212 nnns volume:29 year:2013 number:2 day:06 month:10 pages:211-219 https://dx.doi.org/10.1007/s13146-013-0174-1 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_206 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_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_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 29 2013 2 06 10 211-219 |
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10.1007/s13146-013-0174-1 doi (DE-627)SPR030658683 (SPR)s13146-013-0174-1-e DE-627 ger DE-627 rakwb eng Gaybullaev, Behzod verfasserin aut The large Aral Sea water balance: a future prospective of the large Aral Sea depending on water volume alteration 2013 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Springer-Verlag Berlin Heidelberg 2013 Abstract The Aral Sea is the biggest saline lake in Central Asia. The Amu Darya and Syr Darya rivers flow into the Aral Sea. These rivers were heavily used for irrigation fields after 1960 because of Soviet Union plans. Consequently, the Aral Sea separated into two parts: Large Aral Sea to the south and a small Aral Sea in the north in 1987. The current study estimated the evaporation and precipitation rates of the Large Aral Sea by examining Aral Sea observed records from 1987 to 2011. As a result, the precipitation decreased exponentially from 5.8 $ km^{3} $ in 1987 to 2 $ km^{3} $ in 2011. Evaporation exponentially reduced from 34.2 $ km^{3} $ in 1987 to 5 $ km^{3} $ in 2011. The Nash–Sutcliffe model was used to predict the water volume by using previously observed and estimated data of the large Aral Sea precipitation, runoff, and evaporation from 2001 to 2025. The estimations indicate the large Aral Sea water volume will decrease to approximately 21.1 $ km^{3} $ in 2025 (R2 = 0.9654). The forecasted value of the water volume in the Large Aral Sea after 2025 will slowly decrease and eventually diminish to zero by 2057 if all variables remain unchanged. Large Aral Sea (dpeaa)DE-He213 Water volume (dpeaa)DE-He213 Evaporation (dpeaa)DE-He213 Precipitation (dpeaa)DE-He213 Salinity (dpeaa)DE-He213 Irrigation (dpeaa)DE-He213 Chen, Su-Chin aut Gaybullaev, Gulomjon aut Enthalten in Carbonates and evaporites [Dordrecht [u.a.]] : Springer Netherlands, 1986 29(2013), 2 vom: 06. Okt., Seite 211-219 (DE-627)617505799 (DE-600)2533885-7 1878-5212 nnns volume:29 year:2013 number:2 day:06 month:10 pages:211-219 https://dx.doi.org/10.1007/s13146-013-0174-1 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_206 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_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_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 29 2013 2 06 10 211-219 |
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10.1007/s13146-013-0174-1 doi (DE-627)SPR030658683 (SPR)s13146-013-0174-1-e DE-627 ger DE-627 rakwb eng Gaybullaev, Behzod verfasserin aut The large Aral Sea water balance: a future prospective of the large Aral Sea depending on water volume alteration 2013 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Springer-Verlag Berlin Heidelberg 2013 Abstract The Aral Sea is the biggest saline lake in Central Asia. The Amu Darya and Syr Darya rivers flow into the Aral Sea. These rivers were heavily used for irrigation fields after 1960 because of Soviet Union plans. Consequently, the Aral Sea separated into two parts: Large Aral Sea to the south and a small Aral Sea in the north in 1987. The current study estimated the evaporation and precipitation rates of the Large Aral Sea by examining Aral Sea observed records from 1987 to 2011. As a result, the precipitation decreased exponentially from 5.8 $ km^{3} $ in 1987 to 2 $ km^{3} $ in 2011. Evaporation exponentially reduced from 34.2 $ km^{3} $ in 1987 to 5 $ km^{3} $ in 2011. The Nash–Sutcliffe model was used to predict the water volume by using previously observed and estimated data of the large Aral Sea precipitation, runoff, and evaporation from 2001 to 2025. The estimations indicate the large Aral Sea water volume will decrease to approximately 21.1 $ km^{3} $ in 2025 (R2 = 0.9654). The forecasted value of the water volume in the Large Aral Sea after 2025 will slowly decrease and eventually diminish to zero by 2057 if all variables remain unchanged. Large Aral Sea (dpeaa)DE-He213 Water volume (dpeaa)DE-He213 Evaporation (dpeaa)DE-He213 Precipitation (dpeaa)DE-He213 Salinity (dpeaa)DE-He213 Irrigation (dpeaa)DE-He213 Chen, Su-Chin aut Gaybullaev, Gulomjon aut Enthalten in Carbonates and evaporites [Dordrecht [u.a.]] : Springer Netherlands, 1986 29(2013), 2 vom: 06. Okt., Seite 211-219 (DE-627)617505799 (DE-600)2533885-7 1878-5212 nnns volume:29 year:2013 number:2 day:06 month:10 pages:211-219 https://dx.doi.org/10.1007/s13146-013-0174-1 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_206 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_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_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 29 2013 2 06 10 211-219 |
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10.1007/s13146-013-0174-1 doi (DE-627)SPR030658683 (SPR)s13146-013-0174-1-e DE-627 ger DE-627 rakwb eng Gaybullaev, Behzod verfasserin aut The large Aral Sea water balance: a future prospective of the large Aral Sea depending on water volume alteration 2013 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Springer-Verlag Berlin Heidelberg 2013 Abstract The Aral Sea is the biggest saline lake in Central Asia. The Amu Darya and Syr Darya rivers flow into the Aral Sea. These rivers were heavily used for irrigation fields after 1960 because of Soviet Union plans. Consequently, the Aral Sea separated into two parts: Large Aral Sea to the south and a small Aral Sea in the north in 1987. The current study estimated the evaporation and precipitation rates of the Large Aral Sea by examining Aral Sea observed records from 1987 to 2011. As a result, the precipitation decreased exponentially from 5.8 $ km^{3} $ in 1987 to 2 $ km^{3} $ in 2011. Evaporation exponentially reduced from 34.2 $ km^{3} $ in 1987 to 5 $ km^{3} $ in 2011. The Nash–Sutcliffe model was used to predict the water volume by using previously observed and estimated data of the large Aral Sea precipitation, runoff, and evaporation from 2001 to 2025. The estimations indicate the large Aral Sea water volume will decrease to approximately 21.1 $ km^{3} $ in 2025 (R2 = 0.9654). The forecasted value of the water volume in the Large Aral Sea after 2025 will slowly decrease and eventually diminish to zero by 2057 if all variables remain unchanged. Large Aral Sea (dpeaa)DE-He213 Water volume (dpeaa)DE-He213 Evaporation (dpeaa)DE-He213 Precipitation (dpeaa)DE-He213 Salinity (dpeaa)DE-He213 Irrigation (dpeaa)DE-He213 Chen, Su-Chin aut Gaybullaev, Gulomjon aut Enthalten in Carbonates and evaporites [Dordrecht [u.a.]] : Springer Netherlands, 1986 29(2013), 2 vom: 06. Okt., Seite 211-219 (DE-627)617505799 (DE-600)2533885-7 1878-5212 nnns volume:29 year:2013 number:2 day:06 month:10 pages:211-219 https://dx.doi.org/10.1007/s13146-013-0174-1 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_206 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_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_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 29 2013 2 06 10 211-219 |
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Enthalten in Carbonates and evaporites 29(2013), 2 vom: 06. Okt., Seite 211-219 volume:29 year:2013 number:2 day:06 month:10 pages:211-219 |
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Enthalten in Carbonates and evaporites 29(2013), 2 vom: 06. Okt., Seite 211-219 volume:29 year:2013 number:2 day:06 month:10 pages:211-219 |
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Large Aral Sea Water volume Evaporation Precipitation Salinity Irrigation |
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Carbonates and evaporites |
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Gaybullaev, Behzod @@aut@@ Chen, Su-Chin @@aut@@ Gaybullaev, Gulomjon @@aut@@ |
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<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">SPR030658683</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230331100952.0</controlfield><controlfield tag="007">cr uuu---uuuuu</controlfield><controlfield tag="008">201007s2013 xx |||||o 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1007/s13146-013-0174-1</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)SPR030658683</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(SPR)s13146-013-0174-1-e</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rakwb</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Gaybullaev, Behzod</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="4"><subfield code="a">The large Aral Sea water balance: a future prospective of the large Aral Sea depending on water volume alteration</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2013</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">Text</subfield><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">Computermedien</subfield><subfield code="b">c</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Online-Ressource</subfield><subfield code="b">cr</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="500" ind1=" " ind2=" "><subfield code="a">© Springer-Verlag Berlin Heidelberg 2013</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Abstract The Aral Sea is the biggest saline lake in Central Asia. The Amu Darya and Syr Darya rivers flow into the Aral Sea. These rivers were heavily used for irrigation fields after 1960 because of Soviet Union plans. Consequently, the Aral Sea separated into two parts: Large Aral Sea to the south and a small Aral Sea in the north in 1987. The current study estimated the evaporation and precipitation rates of the Large Aral Sea by examining Aral Sea observed records from 1987 to 2011. As a result, the precipitation decreased exponentially from 5.8 $ km^{3} $ in 1987 to 2 $ km^{3} $ in 2011. Evaporation exponentially reduced from 34.2 $ km^{3} $ in 1987 to 5 $ km^{3} $ in 2011. The Nash–Sutcliffe model was used to predict the water volume by using previously observed and estimated data of the large Aral Sea precipitation, runoff, and evaporation from 2001 to 2025. The estimations indicate the large Aral Sea water volume will decrease to approximately 21.1 $ km^{3} $ in 2025 (R2 = 0.9654). The forecasted value of the water volume in the Large Aral Sea after 2025 will slowly decrease and eventually diminish to zero by 2057 if all variables remain unchanged.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Large Aral Sea</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Water volume</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Evaporation</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Precipitation</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Salinity</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Irrigation</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Chen, Su-Chin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Gaybullaev, Gulomjon</subfield><subfield code="4">aut</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="t">Carbonates and evaporites</subfield><subfield code="d">[Dordrecht [u.a.]] : Springer Netherlands, 1986</subfield><subfield code="g">29(2013), 2 vom: 06. 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Gaybullaev, Behzod |
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The large Aral Sea water balance: a future prospective of the large Aral Sea depending on water volume alteration Large Aral Sea (dpeaa)DE-He213 Water volume (dpeaa)DE-He213 Evaporation (dpeaa)DE-He213 Precipitation (dpeaa)DE-He213 Salinity (dpeaa)DE-He213 Irrigation (dpeaa)DE-He213 |
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large aral sea water balance: a future prospective of the large aral sea depending on water volume alteration |
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The large Aral Sea water balance: a future prospective of the large Aral Sea depending on water volume alteration |
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Abstract The Aral Sea is the biggest saline lake in Central Asia. The Amu Darya and Syr Darya rivers flow into the Aral Sea. These rivers were heavily used for irrigation fields after 1960 because of Soviet Union plans. Consequently, the Aral Sea separated into two parts: Large Aral Sea to the south and a small Aral Sea in the north in 1987. The current study estimated the evaporation and precipitation rates of the Large Aral Sea by examining Aral Sea observed records from 1987 to 2011. As a result, the precipitation decreased exponentially from 5.8 $ km^{3} $ in 1987 to 2 $ km^{3} $ in 2011. Evaporation exponentially reduced from 34.2 $ km^{3} $ in 1987 to 5 $ km^{3} $ in 2011. The Nash–Sutcliffe model was used to predict the water volume by using previously observed and estimated data of the large Aral Sea precipitation, runoff, and evaporation from 2001 to 2025. The estimations indicate the large Aral Sea water volume will decrease to approximately 21.1 $ km^{3} $ in 2025 (R2 = 0.9654). The forecasted value of the water volume in the Large Aral Sea after 2025 will slowly decrease and eventually diminish to zero by 2057 if all variables remain unchanged. © Springer-Verlag Berlin Heidelberg 2013 |
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Abstract The Aral Sea is the biggest saline lake in Central Asia. The Amu Darya and Syr Darya rivers flow into the Aral Sea. These rivers were heavily used for irrigation fields after 1960 because of Soviet Union plans. Consequently, the Aral Sea separated into two parts: Large Aral Sea to the south and a small Aral Sea in the north in 1987. The current study estimated the evaporation and precipitation rates of the Large Aral Sea by examining Aral Sea observed records from 1987 to 2011. As a result, the precipitation decreased exponentially from 5.8 $ km^{3} $ in 1987 to 2 $ km^{3} $ in 2011. Evaporation exponentially reduced from 34.2 $ km^{3} $ in 1987 to 5 $ km^{3} $ in 2011. The Nash–Sutcliffe model was used to predict the water volume by using previously observed and estimated data of the large Aral Sea precipitation, runoff, and evaporation from 2001 to 2025. The estimations indicate the large Aral Sea water volume will decrease to approximately 21.1 $ km^{3} $ in 2025 (R2 = 0.9654). The forecasted value of the water volume in the Large Aral Sea after 2025 will slowly decrease and eventually diminish to zero by 2057 if all variables remain unchanged. © Springer-Verlag Berlin Heidelberg 2013 |
| abstract_unstemmed |
Abstract The Aral Sea is the biggest saline lake in Central Asia. The Amu Darya and Syr Darya rivers flow into the Aral Sea. These rivers were heavily used for irrigation fields after 1960 because of Soviet Union plans. Consequently, the Aral Sea separated into two parts: Large Aral Sea to the south and a small Aral Sea in the north in 1987. The current study estimated the evaporation and precipitation rates of the Large Aral Sea by examining Aral Sea observed records from 1987 to 2011. As a result, the precipitation decreased exponentially from 5.8 $ km^{3} $ in 1987 to 2 $ km^{3} $ in 2011. Evaporation exponentially reduced from 34.2 $ km^{3} $ in 1987 to 5 $ km^{3} $ in 2011. The Nash–Sutcliffe model was used to predict the water volume by using previously observed and estimated data of the large Aral Sea precipitation, runoff, and evaporation from 2001 to 2025. The estimations indicate the large Aral Sea water volume will decrease to approximately 21.1 $ km^{3} $ in 2025 (R2 = 0.9654). The forecasted value of the water volume in the Large Aral Sea after 2025 will slowly decrease and eventually diminish to zero by 2057 if all variables remain unchanged. © Springer-Verlag Berlin Heidelberg 2013 |
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The large Aral Sea water balance: a future prospective of the large Aral Sea depending on water volume alteration |
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Chen, Su-Chin Gaybullaev, Gulomjon |
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| score |
7.4010763 |