TY - JOUR
T1 - The effect of static pressure-wind covariance on vertical carbon dioxide exchange at a windy subalpine forest site
AU - Burns, Sean P.
AU - Frank, John M.
AU - Massman, William J.
AU - Patton, Edward G.
AU - Blanken, Peter D.
N1 - Publisher Copyright:
© 2021 Elsevier B.V.
PY - 2021/8/15
Y1 - 2021/8/15
N2 - Accounting for turbulent temperature and water vapor fluctuations on the vertical flux of CO2 measured by an open-path infrared gas analyzer are commonly known as the Webb–Pearman–Leuning (WPL) corrections. Static pressure fluctuations also affect air sample density, but the magnitude and effect of these changes on CO2 flux is not usually considered. In our study, the turbulent static pressure p and the vertical wind component w covariance w′p′¯ from just-above a Rocky Mountain subalpine forest are examined. The magnitude of w′p′¯ was highly correlated to the mean horizontal wind speed U with similar characteristics during the daytime and nighttime. The pressure term was calculated from w′p′¯ and compared to other terms in the equation for the vertical net ecosystem exchange of CO2 (NEE). We found the following: (1) for U≲6 m s−1, the pressure term was small, (2) as U increased beyond 6 m s−1, the pressure term became more and more important reaching a magnitude of ≈ 2 μmol m−2 s−1 at U of 12 m s−1 (for leaf area index LAI ≈ 2.6 m2 m−2), (3) for a more dense forest (LAI ≈ 4.8 m2 m−2), the magnitude of the pressure term at U of 12 m s−1 was ≈ 1 μmol m−2 s−1, or about half the open forest value, and (4) based on 14 years of measurements, the interannual mean and standard deviation of the yearly cumulative pressure and NEE terms were −32.8± 24.5 g C m−2 year−1 and −147.4± 231.7 g C m−2 year−1, respectively. Therefore, on average, including the pressure term in the NEE calculation reduces the annual carbon uptake by the GLEES forest from 147.4 g C m−2 year−1 to 114.6 g C m−2 year−1. This implies that carbon uptake by forests in windy locations that ignore the pressure term can be overestimated by as much as 20%. However, the year-to-year variability of both NEE and the pressure term was large due to changes in the forest structure and LAI from beetle attack and tree die-off. Finally, we present results from sensor-manipulation experiments examining the effect of tilting the quad-disk pressure ports on the turbulent static pressure.
AB - Accounting for turbulent temperature and water vapor fluctuations on the vertical flux of CO2 measured by an open-path infrared gas analyzer are commonly known as the Webb–Pearman–Leuning (WPL) corrections. Static pressure fluctuations also affect air sample density, but the magnitude and effect of these changes on CO2 flux is not usually considered. In our study, the turbulent static pressure p and the vertical wind component w covariance w′p′¯ from just-above a Rocky Mountain subalpine forest are examined. The magnitude of w′p′¯ was highly correlated to the mean horizontal wind speed U with similar characteristics during the daytime and nighttime. The pressure term was calculated from w′p′¯ and compared to other terms in the equation for the vertical net ecosystem exchange of CO2 (NEE). We found the following: (1) for U≲6 m s−1, the pressure term was small, (2) as U increased beyond 6 m s−1, the pressure term became more and more important reaching a magnitude of ≈ 2 μmol m−2 s−1 at U of 12 m s−1 (for leaf area index LAI ≈ 2.6 m2 m−2), (3) for a more dense forest (LAI ≈ 4.8 m2 m−2), the magnitude of the pressure term at U of 12 m s−1 was ≈ 1 μmol m−2 s−1, or about half the open forest value, and (4) based on 14 years of measurements, the interannual mean and standard deviation of the yearly cumulative pressure and NEE terms were −32.8± 24.5 g C m−2 year−1 and −147.4± 231.7 g C m−2 year−1, respectively. Therefore, on average, including the pressure term in the NEE calculation reduces the annual carbon uptake by the GLEES forest from 147.4 g C m−2 year−1 to 114.6 g C m−2 year−1. This implies that carbon uptake by forests in windy locations that ignore the pressure term can be overestimated by as much as 20%. However, the year-to-year variability of both NEE and the pressure term was large due to changes in the forest structure and LAI from beetle attack and tree die-off. Finally, we present results from sensor-manipulation experiments examining the effect of tilting the quad-disk pressure ports on the turbulent static pressure.
KW - Net ecosystem exchange of CO
KW - Subalpine forest ecosystem
KW - Turbulent pressure transport
KW - Wind profile
UR - https://www.scopus.com/pages/publications/85107064723
U2 - 10.1016/j.agrformet.2021.108402
DO - 10.1016/j.agrformet.2021.108402
M3 - Article
AN - SCOPUS:85107064723
SN - 0168-1923
VL - 306
JO - Agricultural and Forest Meteorology
JF - Agricultural and Forest Meteorology
M1 - 108402
ER -