2013
DOI: 10.1016/j.agrformet.2013.04.024
|View full text |Cite
|
Sign up to set email alerts
|

Random errors in carbon and water vapor fluxes assessed with Gaussian Processes

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
1
1
1
1

Citation Types

1
13
0

Year Published

2015
2015
2022
2022

Publication Types

Select...
5
1

Relationship

2
4

Authors

Journals

citations
Cited by 20 publications
(14 citation statements)
references
References 39 publications
1
13
0
Order By: Relevance
“…This was only slightly higher than the range reported in the literature for forest sites (Hollinger and Richardson, 2005;Liu et al, 2009;Menzer et al, 2013), which increases our confidence in eddy covariance CO 2 sums from urban sites. We also found the half-hourly uncertainties inferred from our models to increase with the flux magnitude (i.e., error variances were heteroscedastic) and approximately Laplacian distributed, which are typical statistical properties of eddy covariance measurement error (Hollinger and Richardson, 2005;Richardson et al, 2006).…”
Section: Annual Urban Co 2 Flux Sums and Uncertaintiessupporting
confidence: 45%
See 1 more Smart Citation
“…This was only slightly higher than the range reported in the literature for forest sites (Hollinger and Richardson, 2005;Liu et al, 2009;Menzer et al, 2013), which increases our confidence in eddy covariance CO 2 sums from urban sites. We also found the half-hourly uncertainties inferred from our models to increase with the flux magnitude (i.e., error variances were heteroscedastic) and approximately Laplacian distributed, which are typical statistical properties of eddy covariance measurement error (Hollinger and Richardson, 2005;Richardson et al, 2006).…”
Section: Annual Urban Co 2 Flux Sums and Uncertaintiessupporting
confidence: 45%
“…They directly relate to ANNs as they can be considered an ANN (or RBF) with infinitely many hidden units (MacKay, 1998). GPs are widely implemented as Kriging in geostatistics, following Matheron (1963), and have more recently been applied for random uncertainty estimation in EC flux time series (Menzer et al, 2013). A GP is a stochastic process that can be defined by a mean function and a covariance function.…”
Section: Gap-filling Techniquesmentioning
confidence: 99%
“…In relative terms, the accumulated uncertainty varied between ±0.38 and ±2.39% of the seasonal CO 2 efflux across sites. These values of uncertainty could vary depending of the length of the data [ Liu et al ., ; Loescher et al ., ], the frequency of the measurements, the magnitude of fluxes [ Richardson et al ., ], and the method to calculate random errors [ Menzer et al ., ; Richardson and Hollinger , ]. For example, the Stu site had not only the highest uncertainty due to random errors but also the highest magnitude of F (Figure ), the highest total annual sum (Table ), and the highest daily variability (Table ) that is translated into a large standard deviation in the annual sum (Table ).…”
Section: Discussionmentioning
confidence: 99%
“…There are different methods to calculate random errors in flux measurements, mainly explained in the eddy covariance literature. The “model residuals” approach [ Lasslop et al ., ; Menzer et al ., ; Richardson et al ., ] infers the errors from the difference between model predictions and measurements from instruments [ Richardson et al ., ; Vargas et al ., ]. The “paired instruments” [ Schmidt et al ., ] or “two towers” [ Hollinger et al ., ] approach uses the difference of two similar instruments/towers that measure at the “same” time and place to estimate the random errors [see Kessomkiat et al ., ].…”
Section: Methodsmentioning
confidence: 98%
“…C5 is a low estimate, because it assumed no correlation between half-hourly errors. An improved quantification of correlations requires the full variance-covariance matrix of the LRC parameter fits (Lasslop et al, 2010;Menzer et al, 2013), which were not available for 15 the BGC online tool.…”
mentioning
confidence: 99%