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Title: Mechanistic links between underestimated CO 2 fluxes and non-closure of the surface energy balance in a semi-arid sagebrush ecosystem

Abstract

The surface energy balance non-closure problem in eddy covariance (EC) studies has been largely attributed to the influence of large-scale turbulent eddies (hereafter large eddies) on latent and sensible heat fluxes. However, how such large eddies concurrently affect CO2 fluxes remains less studied and mechanistic links between the energy balance non-closure and CO2 fluxes are not well understood. Here, using turbulence data collected from an EC tower over a sagebrush ecosystem during two growing seasons, we decomposed the turbulence data into small and large eddies at a cutoff frequency and analyzed their contributions to the fluxes. We found that the magnitude of CO2 fluxes decreased concurrently with decreased sensible and latent heat fluxes (and thus increased energy balance non-closure), primarily caused by large turbulent eddies. The contributions of such large eddies to fluxes are dependent not only upon their magnitudes of vertical velocity (w) and scalars (i.e. temperature, water vapor density, and CO2 concentration), but also upon the phase differences between the large eddies of w and scalars via their covariances. Enlarged phase differences between large eddies of w and these scalars simultaneously led to reductions in the magnitudes of both CO2 and heat fluxes, linking the lower CO2 fluxesmore » to energy balance non-closure. Such increased phase differences of large eddies were caused by changes in the structures of large eddies from unstable to near neutral conditions. Given widespread observations in non-closure in the flux community, the processes identified here may bias CO2 fluxes at many sites and cause upscaled regional and global budgets to be underestimated. More studies are needed to investigate how landscape heterogeneity influences CO2 fluxes through the influence of associated large eddies on flux exchange.« less

Authors:
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Publication Date:
Research Org.:
Pacific Northwest National Laboratory (PNNL), Richland, WA (United States)
Sponsoring Org.:
USDOE
OSTI Identifier:
1506141
Alternate Identifier(s):
OSTI ID: 1525293
Report Number(s):
PNNL-SA-142139
Journal ID: ISSN 1748-9326
Grant/Contract Number:  
AC05-76RL01830
Resource Type:
Published Article
Journal Name:
Environmental Research Letters
Additional Journal Information:
Journal Name: Environmental Research Letters Journal Volume: 14 Journal Issue: 4; Journal ID: ISSN 1748-9326
Publisher:
IOP Publishing
Country of Publication:
United Kingdom
Language:
English
Subject:
54 ENVIRONMENTAL SCIENCES; CO2 flux; eddy covariance method; ensemble empirical mode decomposition; sensible and latent heat fluxes; surface energy balance closure

Citation Formats

Gao, Zhongming, Liu, Heping, Missik, Justine E. C., Yao, Jingyu, Huang, Maoyi, Chen, Xingyuan, Arntzen, Evan, and Mcfarland, Douglas P. Mechanistic links between underestimated CO 2 fluxes and non-closure of the surface energy balance in a semi-arid sagebrush ecosystem. United Kingdom: N. p., 2019. Web. doi:10.1088/1748-9326/ab082d.
Gao, Zhongming, Liu, Heping, Missik, Justine E. C., Yao, Jingyu, Huang, Maoyi, Chen, Xingyuan, Arntzen, Evan, & Mcfarland, Douglas P. Mechanistic links between underestimated CO 2 fluxes and non-closure of the surface energy balance in a semi-arid sagebrush ecosystem. United Kingdom. https://doi.org/10.1088/1748-9326/ab082d
Gao, Zhongming, Liu, Heping, Missik, Justine E. C., Yao, Jingyu, Huang, Maoyi, Chen, Xingyuan, Arntzen, Evan, and Mcfarland, Douglas P. Mon . "Mechanistic links between underestimated CO 2 fluxes and non-closure of the surface energy balance in a semi-arid sagebrush ecosystem". United Kingdom. https://doi.org/10.1088/1748-9326/ab082d.
@article{osti_1506141,
title = {Mechanistic links between underestimated CO 2 fluxes and non-closure of the surface energy balance in a semi-arid sagebrush ecosystem},
author = {Gao, Zhongming and Liu, Heping and Missik, Justine E. C. and Yao, Jingyu and Huang, Maoyi and Chen, Xingyuan and Arntzen, Evan and Mcfarland, Douglas P.},
abstractNote = {The surface energy balance non-closure problem in eddy covariance (EC) studies has been largely attributed to the influence of large-scale turbulent eddies (hereafter large eddies) on latent and sensible heat fluxes. However, how such large eddies concurrently affect CO2 fluxes remains less studied and mechanistic links between the energy balance non-closure and CO2 fluxes are not well understood. Here, using turbulence data collected from an EC tower over a sagebrush ecosystem during two growing seasons, we decomposed the turbulence data into small and large eddies at a cutoff frequency and analyzed their contributions to the fluxes. We found that the magnitude of CO2 fluxes decreased concurrently with decreased sensible and latent heat fluxes (and thus increased energy balance non-closure), primarily caused by large turbulent eddies. The contributions of such large eddies to fluxes are dependent not only upon their magnitudes of vertical velocity (w) and scalars (i.e. temperature, water vapor density, and CO2 concentration), but also upon the phase differences between the large eddies of w and scalars via their covariances. Enlarged phase differences between large eddies of w and these scalars simultaneously led to reductions in the magnitudes of both CO2 and heat fluxes, linking the lower CO2 fluxes to energy balance non-closure. Such increased phase differences of large eddies were caused by changes in the structures of large eddies from unstable to near neutral conditions. Given widespread observations in non-closure in the flux community, the processes identified here may bias CO2 fluxes at many sites and cause upscaled regional and global budgets to be underestimated. More studies are needed to investigate how landscape heterogeneity influences CO2 fluxes through the influence of associated large eddies on flux exchange.},
doi = {10.1088/1748-9326/ab082d},
journal = {Environmental Research Letters},
number = 4,
volume = 14,
place = {United Kingdom},
year = {Mon Apr 01 00:00:00 EDT 2019},
month = {Mon Apr 01 00:00:00 EDT 2019}
}

Journal Article:
Free Publicly Available Full Text
Publisher's Version of Record
https://doi.org/10.1088/1748-9326/ab082d

Citation Metrics:
Cited by: 13 works
Citation information provided by
Web of Science

Figures / Tables:

Figure 1 Figure 1: Scatter plots of the total CO2 fluxes ($Fc$) against (a) the net radiation ($R$$n$), (b) the sum of turbulent heat fluxes ($H$+$LE$), (c) air temperature, (d) vapor pressure deficit, and (e) the surface energy balance closure ratio (CR), and (f) of CO2 fluxes contributed by large eddies ($Fc$$l$)more » against CR. The black dash lines are second-order polynomial fits. In figures 1(e) and (f), the gray squares and bars refer to the bin averages and the corresponding standard deviations, respectively. Red circles in figure 1(e) are highlighted to illustrate the variations in $Fc$ with CR within a small range of air temperature (283–285 K).« less

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Figures/Tables have been extracted from DOE-funded journal article accepted manuscripts.