Influence of Local Climate and ENSO on the Growth of Cedrela odorata L. in Suriname

被引:3
|
作者
Koehl, Michael [1 ,2 ]
Lotfiomran, Neda [1 ,2 ]
Gauli, Archana [1 ,2 ]
机构
[1] Univ Hamburg, Inst Wood Sci World Forestry, Leuschner Str 91, D-21031 Hamburg, Germany
[2] Univ Hamburg, Ctr Earth Syst Res & Sustainabil CEN, Leuschner Str 91, D-21031 Hamburg, Germany
关键词
dendroclimatology; neotropic; Cedera odorata L; climate-growth relationship; global climate change; ENSO; TREE GROWTH; INCREMENT PATTERNS; TROPICAL TREES; CHANGE IMPACTS; FOREST; VARIABILITY; SENSITIVITY; MANAGEMENT; DYNAMICS; RAINFALL;
D O I
10.3390/atmos13071119
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
In this study, we used retrospective dendroclimatological analyses to explore whether El Nino Southern Oscillation (ENSO) and local precipitation patterns have an influence on tree growth in Suriname, a country located on the Guiana Shield, as annual precipitation patterns on the Guiana Shield are related to ENSO. Discs were taken from 20 trees of Cedrela odorata, whose stem forms very distinct annual growth rings, for tree ring analyses. The trees grew in unmanaged tropical wet forests of Suriname. The tree-ring series of individual trees started between 1836 and 1931 and extended over a period of 84-180 years. The 20 dated series were utilized for constructing a tree-ring chronology. Unlike many other studies that used local anomalies such as flood pulse, precipitation, and drought events to describe the influence of El Nino on tree growth, we used monthly precipitation and ENSO indices as predictors of tree growth to calculate response and correlation functions. The study observed that tree ring growth of Cedrela odorata is influenced by precipitation in August and June of the current year and in August of the previous year, as well as by the ENSO indices SSTA, TSA, TNA, and NAO. Systematic increases in the strength of the El Nino southern oscillation (ENSO) teleconnection due to climate change could affect the growth of trees on the Guiana Shield.
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页数:13
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