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@INPROCEEDINGS{Klosterhalfen:808763,
author = {Klosterhalfen, Anne and Graf, Alexander and Schmidt, Marius
and Ney, Patrizia and Vereecken, Harry},
title = {{S}ource {P}artitioning {B}ased on {H}igh {F}requency
{E}ddy {C}ovariance {D}ata},
reportid = {FZJ-2016-02381},
year = {2016},
abstract = {Source partitioning of eddy covariance measurements is
routinely used for a better understanding of the exchange of
greenhouse gases, especially between terrestrial ecosystems
and the atmosphere. Quantifications of CO2 and H2O fluxes,
their dynamics, variabilities and feedbacks with
environmental drivers give a better insight of the
biosphere’s sensitivity towards global change.The
BMBF-funded project “Instrumental and Data-driven
Approaches to Source-Partitioning of Greenhouse Gas Fluxes:
Comparison, Combination, Advancement” (IDAS-GHG) aims at
comparing and improving existing methods for partitioning of
CO2 and H2O fluxes into their respective raw components.
Data-driven approaches use existing (raw or processed) data
of typical eddy covariance stations. Instrumental approaches
of source partitioning require additional measurements at
different parts of ecosystems and different methods, e.g.
soil-flux chamber measurements, profile measurements or
tracer measurements (isotopes).This present study is part of
the data-driven approaches, using some results from
additional profile measurements to gain further insights.
SCANLON and SAHU (2008), and SCANLON and KUSTAS (2010)
proposed an interesting method to estimate the contributions
of photosynthesis, soil respiration (autotrophic and
heterotrophic sources), transpiration and evaporation using
measured high-frequency time series of CO2 and H2O fluxes -
no extra instrumentation necessary. This method (SK10 in the
following) is based on the dissimilarities of sources and
sinks of CO2 and water vapor among the sub-canopy, canopy
and atmosphere, which lead to unique “signals” in the
eddy covariance measurements for air transported from
differing locations. Thus, the flux-variance similarity
theory is separately applied to the stomatal and
non-stomatal components of the regarded fluxes.In this study
we apply the SK10 analysis to observations of several
agroecosystems, and compare the results to outcomes of other
well-known source partitioning methods as well as to chamber
and profile measurements. For example, state variables
measured in the canopy air are used to test the profile
assumption required by SK10 analysis.Scanlon, T.M., Kustas,
W.P., 2010. Partitioning carbon dioxide and water vapor
fluxes using correlation analysis. Agricultural and Forest
Meteorology 150 (1), 89-99.Scanlon, T.M., Sahu, P., 2008. On
the correlation structure of water vapor and carbon dioxide
in the atmospheric surface layer: A basis for flux
partitioning. Water Resources Research 44 (10), W10418, 15
pp.},
month = {Jun},
date = {2016-06-20},
organization = {32nd Conference on Agricultural and
Forest Meteorology, American
Meteorology Society, Salt Lake City
(USA), 20 Jun 2016 - 24 Jun 2016},
subtyp = {Other},
cin = {IBG-3},
cid = {I:(DE-Juel1)IBG-3-20101118},
pnm = {255 - Terrestrial Systems: From Observation to Prediction
(POF3-255) / IDAS-GHG - Instrumental and Data-driven
Approaches to Source-Partitioning of Greenhouse Gas Fluxes:
Comparison, Combination, Advancement (BMBF-01LN1313A)},
pid = {G:(DE-HGF)POF3-255 / G:(DE-Juel1)BMBF-01LN1313A},
typ = {PUB:(DE-HGF)24},
url = {https://juser.fz-juelich.de/record/808763},
}