The contribution of advective fluxes to net ecosystem exchange in a high-elevation, subalpine forest

Chuixiang Yi, Dean E. Anderson, Andrew A. Turnipseed, Sean P. Burns, Jed P. Sparks, David I. Stannard, Russell Monson

Research output: Contribution to journalArticle

63 Citations (Scopus)

Abstract

The eddy covariance technique, which is used in the determination of net ecosystem CO2 exchange (NEE), is subject to significant errors when advection that carries CO2 in the mean flow is ignored. We measured horizontal and vertical advective CO2 fluxes at the Niwot Ridge AmeriFlux site (Colorado, USA) using a measurement approach consisting of multiple towers. We observed relatively high rates of both horizontal (F hadv) and vertical (Fhadv) advective fluxes at low surface friction velocities (u*) which were associated with downslope katabatic flows. We observed that F hadv was confined to a relatively thin layer (0-6 m thick) of subcanopy air that flowed beneath the eddy covariance sensors principally at night, carrying with it respired CO2 from the soil and lower parts of the canopy. The observed Fvadv came from above the canopy and was presumably due to the convergence of drainage flows at the tower site. The magnitudes of both Fhadv and Fvaadv were similar, of opposite sign, and increased with decreasing u*, meaning that they most affected estimates of the total CO2 flux on calm nights with low wind speeds. The mathematical sign, temporal variation and dependence on u* of both Fhadv and Fvadv were determined by the unique terrain of the Niwot Ridge site. Therefore, the patterns we observed may not be broadly applicable to other sites. We evaluated the influence of advection on the cumulative annual and monthly estimates of the total CO2 flux (Fc), which is often used as an estimate of NEE, over six years using the dependence of Fhadv and F vadv on u*. When the sum of Fhaadv and F vaadv was used to correct monthly Fe, we observed values that were different from the monthly Fc calculated using the traditional u*-filter correction by -16 to 20 g C m-2 mo -1; the mean percentage difference in monthly Fc for these two methods over the six-year period was 10%. When the sum of Fhadv and Fvadv was used to correct annual Fc, we observed a 65% difference compared to the traditional u*-filter approach. Thus, the errors to the local CO2 budget, when Fhadv and F vadv are ignored, can become large when compounded in cumulative fashion over long time intervals. We conclude that the " micrometeorological" (using observations of Fhadv and F vadv) and "biological" (using the u* filter and temperature vs. Fc relationship) corrections differ on the basis of fundamental mechanistic grounds. The micrometeorological correction is based on aerodynamic mechanisms and shows no correlation to drivers of biological activity. Conversely, the biological correction is based on climatic responses of organisms and has no physical connection to aerodynamic processes. In those cases where they impose corrections of similar magnitude on the cumulative Fc sum, the result is due to a serendipitous similarity in scale but has no clear mechanistic explanation.

Original languageEnglish (US)
Pages (from-to)1379-1390
Number of pages12
JournalEcological Applications
Volume18
Issue number6
DOIs
StatePublished - Sep 2008
Externally publishedYes

Fingerprint

net ecosystem exchange
eddy covariance
filter
aerodynamics
advection
katabatic flow
canopy
ecosystem
temporal variation
friction
wind velocity
drainage
sensor
air
soil
temperature

Keywords

  • AmeriFlux
  • Annual cumulative NEE
  • Colorado
  • Complex topography
  • Drainage flows
  • Eddy flux tower
  • Friction velocity
  • Horizontal advection
  • Niwot ridge
  • USA
  • Vertical advection

ASJC Scopus subject areas

  • Ecology

Cite this

Yi, C., Anderson, D. E., Turnipseed, A. A., Burns, S. P., Sparks, J. P., Stannard, D. I., & Monson, R. (2008). The contribution of advective fluxes to net ecosystem exchange in a high-elevation, subalpine forest. Ecological Applications, 18(6), 1379-1390. https://doi.org/10.1890/06-0908.1

The contribution of advective fluxes to net ecosystem exchange in a high-elevation, subalpine forest. / Yi, Chuixiang; Anderson, Dean E.; Turnipseed, Andrew A.; Burns, Sean P.; Sparks, Jed P.; Stannard, David I.; Monson, Russell.

In: Ecological Applications, Vol. 18, No. 6, 09.2008, p. 1379-1390.

Research output: Contribution to journalArticle

Yi, C, Anderson, DE, Turnipseed, AA, Burns, SP, Sparks, JP, Stannard, DI & Monson, R 2008, 'The contribution of advective fluxes to net ecosystem exchange in a high-elevation, subalpine forest', Ecological Applications, vol. 18, no. 6, pp. 1379-1390. https://doi.org/10.1890/06-0908.1
Yi C, Anderson DE, Turnipseed AA, Burns SP, Sparks JP, Stannard DI et al. The contribution of advective fluxes to net ecosystem exchange in a high-elevation, subalpine forest. Ecological Applications. 2008 Sep;18(6):1379-1390. https://doi.org/10.1890/06-0908.1
Yi, Chuixiang ; Anderson, Dean E. ; Turnipseed, Andrew A. ; Burns, Sean P. ; Sparks, Jed P. ; Stannard, David I. ; Monson, Russell. / The contribution of advective fluxes to net ecosystem exchange in a high-elevation, subalpine forest. In: Ecological Applications. 2008 ; Vol. 18, No. 6. pp. 1379-1390.
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N2 - The eddy covariance technique, which is used in the determination of net ecosystem CO2 exchange (NEE), is subject to significant errors when advection that carries CO2 in the mean flow is ignored. We measured horizontal and vertical advective CO2 fluxes at the Niwot Ridge AmeriFlux site (Colorado, USA) using a measurement approach consisting of multiple towers. We observed relatively high rates of both horizontal (F hadv) and vertical (Fhadv) advective fluxes at low surface friction velocities (u*) which were associated with downslope katabatic flows. We observed that F hadv was confined to a relatively thin layer (0-6 m thick) of subcanopy air that flowed beneath the eddy covariance sensors principally at night, carrying with it respired CO2 from the soil and lower parts of the canopy. The observed Fvadv came from above the canopy and was presumably due to the convergence of drainage flows at the tower site. The magnitudes of both Fhadv and Fvaadv were similar, of opposite sign, and increased with decreasing u*, meaning that they most affected estimates of the total CO2 flux on calm nights with low wind speeds. The mathematical sign, temporal variation and dependence on u* of both Fhadv and Fvadv were determined by the unique terrain of the Niwot Ridge site. Therefore, the patterns we observed may not be broadly applicable to other sites. We evaluated the influence of advection on the cumulative annual and monthly estimates of the total CO2 flux (Fc), which is often used as an estimate of NEE, over six years using the dependence of Fhadv and F vadv on u*. When the sum of Fhaadv and F vaadv was used to correct monthly Fe, we observed values that were different from the monthly Fc calculated using the traditional u*-filter correction by -16 to 20 g C m-2 mo -1; the mean percentage difference in monthly Fc for these two methods over the six-year period was 10%. When the sum of Fhadv and Fvadv was used to correct annual Fc, we observed a 65% difference compared to the traditional u*-filter approach. Thus, the errors to the local CO2 budget, when Fhadv and F vadv are ignored, can become large when compounded in cumulative fashion over long time intervals. We conclude that the " micrometeorological" (using observations of Fhadv and F vadv) and "biological" (using the u* filter and temperature vs. Fc relationship) corrections differ on the basis of fundamental mechanistic grounds. The micrometeorological correction is based on aerodynamic mechanisms and shows no correlation to drivers of biological activity. Conversely, the biological correction is based on climatic responses of organisms and has no physical connection to aerodynamic processes. In those cases where they impose corrections of similar magnitude on the cumulative Fc sum, the result is due to a serendipitous similarity in scale but has no clear mechanistic explanation.

AB - The eddy covariance technique, which is used in the determination of net ecosystem CO2 exchange (NEE), is subject to significant errors when advection that carries CO2 in the mean flow is ignored. We measured horizontal and vertical advective CO2 fluxes at the Niwot Ridge AmeriFlux site (Colorado, USA) using a measurement approach consisting of multiple towers. We observed relatively high rates of both horizontal (F hadv) and vertical (Fhadv) advective fluxes at low surface friction velocities (u*) which were associated with downslope katabatic flows. We observed that F hadv was confined to a relatively thin layer (0-6 m thick) of subcanopy air that flowed beneath the eddy covariance sensors principally at night, carrying with it respired CO2 from the soil and lower parts of the canopy. The observed Fvadv came from above the canopy and was presumably due to the convergence of drainage flows at the tower site. The magnitudes of both Fhadv and Fvaadv were similar, of opposite sign, and increased with decreasing u*, meaning that they most affected estimates of the total CO2 flux on calm nights with low wind speeds. The mathematical sign, temporal variation and dependence on u* of both Fhadv and Fvadv were determined by the unique terrain of the Niwot Ridge site. Therefore, the patterns we observed may not be broadly applicable to other sites. We evaluated the influence of advection on the cumulative annual and monthly estimates of the total CO2 flux (Fc), which is often used as an estimate of NEE, over six years using the dependence of Fhadv and F vadv on u*. When the sum of Fhaadv and F vaadv was used to correct monthly Fe, we observed values that were different from the monthly Fc calculated using the traditional u*-filter correction by -16 to 20 g C m-2 mo -1; the mean percentage difference in monthly Fc for these two methods over the six-year period was 10%. When the sum of Fhadv and Fvadv was used to correct annual Fc, we observed a 65% difference compared to the traditional u*-filter approach. Thus, the errors to the local CO2 budget, when Fhadv and F vadv are ignored, can become large when compounded in cumulative fashion over long time intervals. We conclude that the " micrometeorological" (using observations of Fhadv and F vadv) and "biological" (using the u* filter and temperature vs. Fc relationship) corrections differ on the basis of fundamental mechanistic grounds. The micrometeorological correction is based on aerodynamic mechanisms and shows no correlation to drivers of biological activity. Conversely, the biological correction is based on climatic responses of organisms and has no physical connection to aerodynamic processes. In those cases where they impose corrections of similar magnitude on the cumulative Fc sum, the result is due to a serendipitous similarity in scale but has no clear mechanistic explanation.

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