20th century seasonal moisture balance in Southeast Asian montane forests from tree cellulose $ δ^{18} $O
Abstract The seasonally varying moisture balance in a montane forest of Southeast Asia is reconstructed for the 20th century from the oxygen isotopic composition ($ δ^{18} $O) of subannual tree cellulose samples of Pinus kesiya growing at 1,500 m elevation on Doi Chiang Dao in northern Thailand. The...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Zhu, Mengfan [verfasserIn] Stott, Lowell [verfasserIn] Buckley, Brendan [verfasserIn] Yoshimura, Kei [verfasserIn] |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2012 |
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| Schlagwörter: |
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| Übergeordnetes Werk: |
Enthalten in: Climatic change - Dordrecht [u.a.] : Springer Science + Business Media B.V, 1977, 115(2012), 3-4 vom: 28. März, Seite 505-517 |
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| Übergeordnetes Werk: |
volume:115 ; year:2012 ; number:3-4 ; day:28 ; month:03 ; pages:505-517 |
| Links: |
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| DOI / URN: |
10.1007/s10584-012-0439-z |
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| Katalog-ID: |
SPR011464534 |
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| 245 | 1 | 0 | |a 20th century seasonal moisture balance in Southeast Asian montane forests from tree cellulose $ δ^{18} $O |
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| 520 | |a Abstract The seasonally varying moisture balance in a montane forest of Southeast Asia is reconstructed for the 20th century from the oxygen isotopic composition ($ δ^{18} $O) of subannual tree cellulose samples of Pinus kesiya growing at 1,500 m elevation on Doi Chiang Dao in northern Thailand. The cellulose $ δ^{18} $O values exhibit a distinctive annual cycle with amplitude of up to 12 ‰, which we interpret to represent primarily the seasonal cycle of precipitation $ δ^{18} $O. The annual mean $ δ^{18} $O values correlate significantly with the amount of summer monsoon precipitation, and suggest a temporal weakening relationship between the South Asian monsoon and El Niño-Southern Oscillation over the late 20th century. The cellulose $ δ^{18} $O annual maxima values, which reflect the dry season moisture status, have declined progressively over the 20th century by about 3.5 ‰. We interpret this to indicate a change in the contribution of the isotopically distinct fog water to the dry season soil moisture in response to rising temperature as well as deforestation. | ||
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| 650 | 4 | |a Tropical Montane Forest |7 (dpeaa)DE-He213 | |
| 700 | 1 | |a Stott, Lowell |e verfasserin |4 aut | |
| 700 | 1 | |a Buckley, Brendan |e verfasserin |4 aut | |
| 700 | 1 | |a Yoshimura, Kei |e verfasserin |4 aut | |
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10.1007/s10584-012-0439-z doi (DE-627)SPR011464534 (SPR)s10584-012-0439-z-e DE-627 ger DE-627 rakwb eng 550 ASE 38.82 bkl 43.47 bkl Zhu, Mengfan verfasserin aut 20th century seasonal moisture balance in Southeast Asian montane forests from tree cellulose $ δ^{18} $O 2012 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract The seasonally varying moisture balance in a montane forest of Southeast Asia is reconstructed for the 20th century from the oxygen isotopic composition ($ δ^{18} $O) of subannual tree cellulose samples of Pinus kesiya growing at 1,500 m elevation on Doi Chiang Dao in northern Thailand. The cellulose $ δ^{18} $O values exhibit a distinctive annual cycle with amplitude of up to 12 ‰, which we interpret to represent primarily the seasonal cycle of precipitation $ δ^{18} $O. The annual mean $ δ^{18} $O values correlate significantly with the amount of summer monsoon precipitation, and suggest a temporal weakening relationship between the South Asian monsoon and El Niño-Southern Oscillation over the late 20th century. The cellulose $ δ^{18} $O annual maxima values, which reflect the dry season moisture status, have declined progressively over the 20th century by about 3.5 ‰. We interpret this to indicate a change in the contribution of the isotopically distinct fog water to the dry season soil moisture in response to rising temperature as well as deforestation. Tree Ring (dpeaa)DE-He213 Montane Forest (dpeaa)DE-He213 Empirical Orthogonal Function Mode (dpeaa)DE-He213 South Asian Summer Monsoon (dpeaa)DE-He213 Tropical Montane Forest (dpeaa)DE-He213 Stott, Lowell verfasserin aut Buckley, Brendan verfasserin aut Yoshimura, Kei verfasserin aut Enthalten in Climatic change Dordrecht [u.a.] : Springer Science + Business Media B.V, 1977 115(2012), 3-4 vom: 28. März, Seite 505-517 (DE-627)270429514 (DE-600)1477652-2 1573-1480 nnns volume:115 year:2012 number:3-4 day:28 month:03 pages:505-517 https://dx.doi.org/10.1007/s10584-012-0439-z 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_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_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_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 38.82 ASE 43.47 ASE AR 115 2012 3-4 28 03 505-517 |
| spelling |
10.1007/s10584-012-0439-z doi (DE-627)SPR011464534 (SPR)s10584-012-0439-z-e DE-627 ger DE-627 rakwb eng 550 ASE 38.82 bkl 43.47 bkl Zhu, Mengfan verfasserin aut 20th century seasonal moisture balance in Southeast Asian montane forests from tree cellulose $ δ^{18} $O 2012 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract The seasonally varying moisture balance in a montane forest of Southeast Asia is reconstructed for the 20th century from the oxygen isotopic composition ($ δ^{18} $O) of subannual tree cellulose samples of Pinus kesiya growing at 1,500 m elevation on Doi Chiang Dao in northern Thailand. The cellulose $ δ^{18} $O values exhibit a distinctive annual cycle with amplitude of up to 12 ‰, which we interpret to represent primarily the seasonal cycle of precipitation $ δ^{18} $O. The annual mean $ δ^{18} $O values correlate significantly with the amount of summer monsoon precipitation, and suggest a temporal weakening relationship between the South Asian monsoon and El Niño-Southern Oscillation over the late 20th century. The cellulose $ δ^{18} $O annual maxima values, which reflect the dry season moisture status, have declined progressively over the 20th century by about 3.5 ‰. We interpret this to indicate a change in the contribution of the isotopically distinct fog water to the dry season soil moisture in response to rising temperature as well as deforestation. Tree Ring (dpeaa)DE-He213 Montane Forest (dpeaa)DE-He213 Empirical Orthogonal Function Mode (dpeaa)DE-He213 South Asian Summer Monsoon (dpeaa)DE-He213 Tropical Montane Forest (dpeaa)DE-He213 Stott, Lowell verfasserin aut Buckley, Brendan verfasserin aut Yoshimura, Kei verfasserin aut Enthalten in Climatic change Dordrecht [u.a.] : Springer Science + Business Media B.V, 1977 115(2012), 3-4 vom: 28. März, Seite 505-517 (DE-627)270429514 (DE-600)1477652-2 1573-1480 nnns volume:115 year:2012 number:3-4 day:28 month:03 pages:505-517 https://dx.doi.org/10.1007/s10584-012-0439-z 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_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_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_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 38.82 ASE 43.47 ASE AR 115 2012 3-4 28 03 505-517 |
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10.1007/s10584-012-0439-z doi (DE-627)SPR011464534 (SPR)s10584-012-0439-z-e DE-627 ger DE-627 rakwb eng 550 ASE 38.82 bkl 43.47 bkl Zhu, Mengfan verfasserin aut 20th century seasonal moisture balance in Southeast Asian montane forests from tree cellulose $ δ^{18} $O 2012 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract The seasonally varying moisture balance in a montane forest of Southeast Asia is reconstructed for the 20th century from the oxygen isotopic composition ($ δ^{18} $O) of subannual tree cellulose samples of Pinus kesiya growing at 1,500 m elevation on Doi Chiang Dao in northern Thailand. The cellulose $ δ^{18} $O values exhibit a distinctive annual cycle with amplitude of up to 12 ‰, which we interpret to represent primarily the seasonal cycle of precipitation $ δ^{18} $O. The annual mean $ δ^{18} $O values correlate significantly with the amount of summer monsoon precipitation, and suggest a temporal weakening relationship between the South Asian monsoon and El Niño-Southern Oscillation over the late 20th century. The cellulose $ δ^{18} $O annual maxima values, which reflect the dry season moisture status, have declined progressively over the 20th century by about 3.5 ‰. We interpret this to indicate a change in the contribution of the isotopically distinct fog water to the dry season soil moisture in response to rising temperature as well as deforestation. Tree Ring (dpeaa)DE-He213 Montane Forest (dpeaa)DE-He213 Empirical Orthogonal Function Mode (dpeaa)DE-He213 South Asian Summer Monsoon (dpeaa)DE-He213 Tropical Montane Forest (dpeaa)DE-He213 Stott, Lowell verfasserin aut Buckley, Brendan verfasserin aut Yoshimura, Kei verfasserin aut Enthalten in Climatic change Dordrecht [u.a.] : Springer Science + Business Media B.V, 1977 115(2012), 3-4 vom: 28. März, Seite 505-517 (DE-627)270429514 (DE-600)1477652-2 1573-1480 nnns volume:115 year:2012 number:3-4 day:28 month:03 pages:505-517 https://dx.doi.org/10.1007/s10584-012-0439-z 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_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_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_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 38.82 ASE 43.47 ASE AR 115 2012 3-4 28 03 505-517 |
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10.1007/s10584-012-0439-z doi (DE-627)SPR011464534 (SPR)s10584-012-0439-z-e DE-627 ger DE-627 rakwb eng 550 ASE 38.82 bkl 43.47 bkl Zhu, Mengfan verfasserin aut 20th century seasonal moisture balance in Southeast Asian montane forests from tree cellulose $ δ^{18} $O 2012 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract The seasonally varying moisture balance in a montane forest of Southeast Asia is reconstructed for the 20th century from the oxygen isotopic composition ($ δ^{18} $O) of subannual tree cellulose samples of Pinus kesiya growing at 1,500 m elevation on Doi Chiang Dao in northern Thailand. The cellulose $ δ^{18} $O values exhibit a distinctive annual cycle with amplitude of up to 12 ‰, which we interpret to represent primarily the seasonal cycle of precipitation $ δ^{18} $O. The annual mean $ δ^{18} $O values correlate significantly with the amount of summer monsoon precipitation, and suggest a temporal weakening relationship between the South Asian monsoon and El Niño-Southern Oscillation over the late 20th century. The cellulose $ δ^{18} $O annual maxima values, which reflect the dry season moisture status, have declined progressively over the 20th century by about 3.5 ‰. We interpret this to indicate a change in the contribution of the isotopically distinct fog water to the dry season soil moisture in response to rising temperature as well as deforestation. Tree Ring (dpeaa)DE-He213 Montane Forest (dpeaa)DE-He213 Empirical Orthogonal Function Mode (dpeaa)DE-He213 South Asian Summer Monsoon (dpeaa)DE-He213 Tropical Montane Forest (dpeaa)DE-He213 Stott, Lowell verfasserin aut Buckley, Brendan verfasserin aut Yoshimura, Kei verfasserin aut Enthalten in Climatic change Dordrecht [u.a.] : Springer Science + Business Media B.V, 1977 115(2012), 3-4 vom: 28. März, Seite 505-517 (DE-627)270429514 (DE-600)1477652-2 1573-1480 nnns volume:115 year:2012 number:3-4 day:28 month:03 pages:505-517 https://dx.doi.org/10.1007/s10584-012-0439-z 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_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_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_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 38.82 ASE 43.47 ASE AR 115 2012 3-4 28 03 505-517 |
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10.1007/s10584-012-0439-z doi (DE-627)SPR011464534 (SPR)s10584-012-0439-z-e DE-627 ger DE-627 rakwb eng 550 ASE 38.82 bkl 43.47 bkl Zhu, Mengfan verfasserin aut 20th century seasonal moisture balance in Southeast Asian montane forests from tree cellulose $ δ^{18} $O 2012 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract The seasonally varying moisture balance in a montane forest of Southeast Asia is reconstructed for the 20th century from the oxygen isotopic composition ($ δ^{18} $O) of subannual tree cellulose samples of Pinus kesiya growing at 1,500 m elevation on Doi Chiang Dao in northern Thailand. The cellulose $ δ^{18} $O values exhibit a distinctive annual cycle with amplitude of up to 12 ‰, which we interpret to represent primarily the seasonal cycle of precipitation $ δ^{18} $O. The annual mean $ δ^{18} $O values correlate significantly with the amount of summer monsoon precipitation, and suggest a temporal weakening relationship between the South Asian monsoon and El Niño-Southern Oscillation over the late 20th century. The cellulose $ δ^{18} $O annual maxima values, which reflect the dry season moisture status, have declined progressively over the 20th century by about 3.5 ‰. We interpret this to indicate a change in the contribution of the isotopically distinct fog water to the dry season soil moisture in response to rising temperature as well as deforestation. Tree Ring (dpeaa)DE-He213 Montane Forest (dpeaa)DE-He213 Empirical Orthogonal Function Mode (dpeaa)DE-He213 South Asian Summer Monsoon (dpeaa)DE-He213 Tropical Montane Forest (dpeaa)DE-He213 Stott, Lowell verfasserin aut Buckley, Brendan verfasserin aut Yoshimura, Kei verfasserin aut Enthalten in Climatic change Dordrecht [u.a.] : Springer Science + Business Media B.V, 1977 115(2012), 3-4 vom: 28. März, Seite 505-517 (DE-627)270429514 (DE-600)1477652-2 1573-1480 nnns volume:115 year:2012 number:3-4 day:28 month:03 pages:505-517 https://dx.doi.org/10.1007/s10584-012-0439-z 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_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_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_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 38.82 ASE 43.47 ASE AR 115 2012 3-4 28 03 505-517 |
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Enthalten in Climatic change 115(2012), 3-4 vom: 28. März, Seite 505-517 volume:115 year:2012 number:3-4 day:28 month:03 pages:505-517 |
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Tree Ring Montane Forest Empirical Orthogonal Function Mode South Asian Summer Monsoon Tropical Montane Forest |
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Zhu, Mengfan @@aut@@ Stott, Lowell @@aut@@ Buckley, Brendan @@aut@@ Yoshimura, Kei @@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">SPR011464534</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20220110225032.0</controlfield><controlfield tag="007">cr uuu---uuuuu</controlfield><controlfield tag="008">201005s2012 xx |||||o 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1007/s10584-012-0439-z</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)SPR011464534</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(SPR)s10584-012-0439-z-e</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rakwb</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">550</subfield><subfield code="q">ASE</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">38.82</subfield><subfield code="2">bkl</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">43.47</subfield><subfield code="2">bkl</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Zhu, Mengfan</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">20th century seasonal moisture balance in Southeast Asian montane forests from tree cellulose $ δ^{18} $O</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2012</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">Text</subfield><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">Computermedien</subfield><subfield code="b">c</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Online-Ressource</subfield><subfield code="b">cr</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Abstract The seasonally varying moisture balance in a montane forest of Southeast Asia is reconstructed for the 20th century from the oxygen isotopic composition ($ δ^{18} $O) of subannual tree cellulose samples of Pinus kesiya growing at 1,500 m elevation on Doi Chiang Dao in northern Thailand. The cellulose $ δ^{18} $O values exhibit a distinctive annual cycle with amplitude of up to 12 ‰, which we interpret to represent primarily the seasonal cycle of precipitation $ δ^{18} $O. The annual mean $ δ^{18} $O values correlate significantly with the amount of summer monsoon precipitation, and suggest a temporal weakening relationship between the South Asian monsoon and El Niño-Southern Oscillation over the late 20th century. The cellulose $ δ^{18} $O annual maxima values, which reflect the dry season moisture status, have declined progressively over the 20th century by about 3.5 ‰. 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Zhu, Mengfan |
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Zhu, Mengfan ddc 550 bkl 38.82 bkl 43.47 misc Tree Ring misc Montane Forest misc Empirical Orthogonal Function Mode misc South Asian Summer Monsoon misc Tropical Montane Forest 20th century seasonal moisture balance in Southeast Asian montane forests from tree cellulose $ δ^{18} $O |
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550 ASE 38.82 bkl 43.47 bkl 20th century seasonal moisture balance in Southeast Asian montane forests from tree cellulose $ δ^{18} $O Tree Ring (dpeaa)DE-He213 Montane Forest (dpeaa)DE-He213 Empirical Orthogonal Function Mode (dpeaa)DE-He213 South Asian Summer Monsoon (dpeaa)DE-He213 Tropical Montane Forest (dpeaa)DE-He213 |
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ddc 550 bkl 38.82 bkl 43.47 misc Tree Ring misc Montane Forest misc Empirical Orthogonal Function Mode misc South Asian Summer Monsoon misc Tropical Montane Forest |
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20th century seasonal moisture balance in Southeast Asian montane forests from tree cellulose $ δ^{18} $O |
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20th century seasonal moisture balance in Southeast Asian montane forests from tree cellulose $ δ^{18} $O |
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Zhu, Mengfan Stott, Lowell Buckley, Brendan Yoshimura, Kei |
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20th century seasonal moisture balance in southeast asian montane forests from tree cellulose $ δ^{18} $o |
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20th century seasonal moisture balance in Southeast Asian montane forests from tree cellulose $ δ^{18} $O |
| abstract |
Abstract The seasonally varying moisture balance in a montane forest of Southeast Asia is reconstructed for the 20th century from the oxygen isotopic composition ($ δ^{18} $O) of subannual tree cellulose samples of Pinus kesiya growing at 1,500 m elevation on Doi Chiang Dao in northern Thailand. The cellulose $ δ^{18} $O values exhibit a distinctive annual cycle with amplitude of up to 12 ‰, which we interpret to represent primarily the seasonal cycle of precipitation $ δ^{18} $O. The annual mean $ δ^{18} $O values correlate significantly with the amount of summer monsoon precipitation, and suggest a temporal weakening relationship between the South Asian monsoon and El Niño-Southern Oscillation over the late 20th century. The cellulose $ δ^{18} $O annual maxima values, which reflect the dry season moisture status, have declined progressively over the 20th century by about 3.5 ‰. We interpret this to indicate a change in the contribution of the isotopically distinct fog water to the dry season soil moisture in response to rising temperature as well as deforestation. |
| abstractGer |
Abstract The seasonally varying moisture balance in a montane forest of Southeast Asia is reconstructed for the 20th century from the oxygen isotopic composition ($ δ^{18} $O) of subannual tree cellulose samples of Pinus kesiya growing at 1,500 m elevation on Doi Chiang Dao in northern Thailand. The cellulose $ δ^{18} $O values exhibit a distinctive annual cycle with amplitude of up to 12 ‰, which we interpret to represent primarily the seasonal cycle of precipitation $ δ^{18} $O. The annual mean $ δ^{18} $O values correlate significantly with the amount of summer monsoon precipitation, and suggest a temporal weakening relationship between the South Asian monsoon and El Niño-Southern Oscillation over the late 20th century. The cellulose $ δ^{18} $O annual maxima values, which reflect the dry season moisture status, have declined progressively over the 20th century by about 3.5 ‰. We interpret this to indicate a change in the contribution of the isotopically distinct fog water to the dry season soil moisture in response to rising temperature as well as deforestation. |
| abstract_unstemmed |
Abstract The seasonally varying moisture balance in a montane forest of Southeast Asia is reconstructed for the 20th century from the oxygen isotopic composition ($ δ^{18} $O) of subannual tree cellulose samples of Pinus kesiya growing at 1,500 m elevation on Doi Chiang Dao in northern Thailand. The cellulose $ δ^{18} $O values exhibit a distinctive annual cycle with amplitude of up to 12 ‰, which we interpret to represent primarily the seasonal cycle of precipitation $ δ^{18} $O. The annual mean $ δ^{18} $O values correlate significantly with the amount of summer monsoon precipitation, and suggest a temporal weakening relationship between the South Asian monsoon and El Niño-Southern Oscillation over the late 20th century. The cellulose $ δ^{18} $O annual maxima values, which reflect the dry season moisture status, have declined progressively over the 20th century by about 3.5 ‰. We interpret this to indicate a change in the contribution of the isotopically distinct fog water to the dry season soil moisture in response to rising temperature as well as deforestation. |
| collection_details |
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| container_issue |
3-4 |
| title_short |
20th century seasonal moisture balance in Southeast Asian montane forests from tree cellulose $ δ^{18} $O |
| url |
https://dx.doi.org/10.1007/s10584-012-0439-z |
| remote_bool |
true |
| author2 |
Stott, Lowell Buckley, Brendan Yoshimura, Kei |
| author2Str |
Stott, Lowell Buckley, Brendan Yoshimura, Kei |
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false |
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| doi_str |
10.1007/s10584-012-0439-z |
| up_date |
2024-07-03T22:48:16.348Z |
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1803599894391291904 |
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| score |
7.4005327 |