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HYDRO-CLIMATIC VARIABILITY IN SOUTHERN ECUADOR REFLECTED BY TREE-RING OXYGEN ISOTOPES
被引:22
|作者:
Volland, Franziska
[1
]
Pucha, Darwin
[2
]
Braeuning, Achim
[1
]
机构:
[1] Univ Erlangen Nurnberg, Dept Geog, Wetterkreuz 15, D-91058 Erlangen, Germany
[2] Univ Nacl Loja, Carrera Ingn Forestal, Ciudadela Univ Guillermo, Falconi Espinosa Argelia, Loja, Ecuador
来源:
关键词:
Climate variability;
oxygen isotopes;
tropical mountain rain forest;
Ecuador;
Cedrela montana;
ANDEAN ICE CORES;
RAIN-FOREST;
STABLE-ISOTOPES;
PRECIPITATION;
DELTA-O-18;
GROWTH;
CELLULOSE;
RECORDS;
CHRONOLOGIES;
SIMULATION;
D O I:
10.3112/erdkunde.2016.01.05
中图分类号:
P9 [自然地理学];
K9 [地理];
学科分类号:
0705 ;
070501 ;
摘要:
Variations of stable oxygen isotopes in tree-ring cellulose are a widely used proxy to reconstruct hydro-climate variability in tropical and subtropical regions. We present the first delta O-18 chronology from annual tree rings in tropical Cedrela montana trees growing in the mountain rain forest of the Podocarpus National Park (PNP) in southern Ecuador. The more than a century long data record (1885- 2011) comes from up to 15 individual trees (1980- 2005) and represents the best-replicated isotope tree-ring chronology from the tropics. In comparison with tree-ring width, stable isotope variations show considerably higher correlations between individuals and thus represent a more reliable climate proxy in this very humid environment. High teleconnections to other stable isotope chronologies from the Amazon lowland indicate a high degree of consistency of regional hydro-climate variations. The PNP delta O-18 record is correlated with seasonal precipitation (January to April, CRU TS 3.21), frequency of wet days, and cloud cover over the Andean Cordillera Real. Spatial correlations indicate that the El Nino-Southern Oscillation (ENSO) has strong impact on tree-ring delta O-18 variations. Sea Surface Temperatures (SSTs) of the Nino 3.4 region and Nino 4 region, and the Oceanic Nino Index (ONI) show strong positive correlations with Cedrela oxygen isotope ratios, whereas the ENSO precipitation index correlates negatively. The Nino 3.4 and 4 SST influence is stronger after 1960 than before, indicating a shift in the influence of the Pacific Ocean on moisture variations in the Ecuadorian Andes. In the same period, the positive correlation with oxygen isotope signals from Andean glacier ice cores (r=0.2; p<0.05, 1894-1993) increased strongly (r=0.51; p<0.01, 1960-1993). In conclusion, stable oxygen isotope series from tropical tree species can help reconstruct variations in the hydroclimate of the Andean mountains and their surrounding areas.
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页码:69 / 82
页数:14
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