% IMPORTANT: The following is UTF-8 encoded. This means that in the presence
% of non-ASCII characters, it will not work with BibTeX 0.99 or older.
% Instead, you should use an up-to-date BibTeX implementation like “bibtex8” or
% “biber”.
@ARTICLE{Heinrich:4862,
author = {Heinrich, I. and Weidner, K. and Helle, G. and Vos, H. and
Lindesay, J. and Banks, J.C.C.},
title = {{I}nterdecadal modulation of the relationship between
{ENSO}, {IPO} and precipitation: insights from tree rings in
{A}ustralia},
journal = {Climate dynamics},
volume = {33},
issn = {0930-7575},
address = {Berlin},
publisher = {Springer},
reportid = {PreJuSER-4862},
pages = {63 - 73},
year = {2009},
note = {Ingo Heinrich would like to thank the late Dr. John Banks,
School of Resources, Environment and Society (SRES),
Australian National University (ANU), for his excellent
guidance and advice as PhD supervisor and friend. IH also
thanks all other members of the SRES-ANU staff, in
particular Peter Kanowski, Sue Holzknecht, Ann Gibson and
Jurrgen Bauhus, for their important support during his PhD.
IH is grateful to the rangers of the Lamington National Park
for their advice and logistic support during the field work.
IH received PhD scholarships from the Australian National
University, the Cooperative Research Centre for Greenhouse
Accounting, and the German Academic Exchange Service
(DAAD).},
abstract = {Australian climate-proxy reconstructions based on tree
rings from tropical and subtropical forests have not been
achieved so far due to the rarity of species producing
anatomically distinct annual growth rings. Our study
identifies the Australian Red Cedar (Toona ciliata) as one
of the most promising tree species for tree-ring research in
Australasia because this species exhibits distinct annual
tree rings, a prerequisite for high quality tropical
dendroclimatology. Based on these preliminary studies, we
were able, for the first time in subtropical and tropical
Australia, to develop a statistically robust, precisely
dated and annually resolved chronology back to AD1854. We
show that the variability in ring widths of T. ciliata is
mainly dependent on annual precipitation. The developed
proxy data series contains both high- and low-frequency
climate signals which can be associated with the El NiA +/-
o Southern Oscillation (ENSO) and the Interdecadal Pacific
Oscillation (IPO). A comparison of different data sets
(Brisbane precipitation, tree rings, coral luminescence
record from the Great Barrier Reef, ENSO and IPO) revealed
non-stationary correlation patterns throughout the twentieth
century but little instability between the new tree-ring
chronology and Brisbane precipitation.},
keywords = {J (WoSType)},
cin = {ICG-3},
ddc = {550},
cid = {I:(DE-Juel1)ICG-3-20090406},
pnm = {Terrestrische Umwelt},
pid = {G:(DE-Juel1)FUEK407},
shelfmark = {Meteorology $\&$ Atmospheric Sciences},
typ = {PUB:(DE-HGF)16},
UT = {WOS:000266266500005},
doi = {10.1007/s00382-009-0544-5},
url = {https://juser.fz-juelich.de/record/4862},
}