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@ARTICLE{Anhuf:834459,
author = {Anhuf, Dieter and Schleser, Gerhard, Hans},
title = {{T}ree ring studies in the tropics and subtropics},
journal = {Erdkunde},
volume = {71},
number = {1},
issn = {0014-0015},
address = {Bonn},
publisher = {Geographisches Inst., Univ. Bonn},
reportid = {FZJ-2017-04410},
pages = {1 - 4},
year = {2017},
abstract = {According to the Intergovernmental Panel on Climate Change
the global surface temperature has continuously risen since
1861. Increasing temperatures combined with changing
precipitation patterns are strong indications for a more
active and more intense hydrological cycle in the coming
decades. In this respect, it is undisputed that the tropical
regions are important for the global climate system. The
reaction of tropical forests to enhanced atmospheric CO2
concentrations plays a pivotal role for the land carbon and
the land water cycle. Currently our understanding of the
physiological reactions such as growth response of tropical
trees to rising atmospheric CO2 concentration, partly
related to water-use-efficiency (WUE) and climate change is
still rather poor and controversially discussed (Frank et
al. 2015). Modifications in their carbon uptake and
transpiration rate have inevitably global consequences. It
is still unclear if tropical trees assimilate more CO2 with
constant or slightly reduced water losses in a CO2 richer
world or if the carbon gain remains almost unchanged with
reduced transpiration.Tree-rings are well suited for
environmental investigations with much potential for
verifications of their well-being. Tree rings are mostly
annually resolved, contain environmental information, are
easily sampled and as such valuable archives. Growth
limiting factors control the development of trees allowing
the derivation of transfer functions that relate tree growth
to tree physiological quantities as well as climatic
parameters (Cook and Kairiukstis 1992; Fritts 1976).Up to
now hemispheric investigations using tree rings are mainly
based on data sets of mid and high latitude sites or Nordic
tree-line sites. Investigations based on trees of tropical
or subtropical regions are comparatively rare. This has
several causes. One reason is the difficulty to identify
tree-rings or growth increments of annual resolution.
Consequently, it is often demanding to construct reliable
data sets, i.e. chronologies of annual time resolution, for
extracting climatic signals and/or tree physiological
parameters. Therefore, tropical or subtropical trees have
only just recently come into focus of environmentalists and
climatologists. Subsequently tree-ring widths chronologies
of tropical tree ensembles are anything but numerous and
chronologies, e.g. regarding stable isotopes are almost
non-existent.},
cin = {IBG-3},
ddc = {910},
cid = {I:(DE-Juel1)IBG-3-20101118},
pnm = {255 - Terrestrial Systems: From Observation to Prediction
(POF3-255)},
pid = {G:(DE-HGF)POF3-255},
typ = {PUB:(DE-HGF)16},
UT = {WOS:000402315800001},
doi = {10.3112/erdkunde.2017.01.06},
url = {https://juser.fz-juelich.de/record/834459},
}