Role of boundary layer processes on the mixed layer CO2-budget

Research output: Chapter in Book/Report/Conference proceedingConference paperAcademic

Abstract

The diurnal and vertical variability of temperature, humidity and specially CO2 in the atmospheric boundary layer is studied by combining detailed observations taken at Cabauw (The Netherlands), Large-Eddy simulations (LES) and mixed layer theory. The research focus on the role played by the entrainment and other boundary layer driven processes on the distribution and diurnal evolution of CO2 in the boundary layer. The relative importance of this entrained air to ventilate CO2 will be analyzed. During the morning the exchange of CO2 between the residual free tropospheric air masses with the growing boundary layer is a more important contribution than the CO2 uptake by the vegetation, whereas during the afternoon the assimilation by grass at the ground could become the dominant process. This work is completed by quantifying the terms of the budget conservation equation of CO2 using observations and the LES numerical experiments. It will be shown that under non-advective conditions, the flux divergence measurements can correctly reproduce the diurnal variability of temperature, moisture and CO2. The role of boundary layer dynamics on the CO2-budget has direct implications in inferring the CO2-uptake flux from CO2 observations. Our findings show how dynamic factors, as the morning temperature inversion or the lapse rate, are relevant in the retrieval of the CO2 flux. By analyzing the sensitivity of the inferred CO2 flux to the dynamics of the boundary layer and to the CO2 variables, we are able to estimate the uncertainties of the inferred CO2 flux to mean CO2 concentrations
Original languageEnglish
Title of host publication19th Symposium on Boundary Layers and Turbulence and the 29th Conference on Agricultural and Forest Meteorology; Keystone, Colorado, USA
Place of PublicationBoston
PublisherAMS
PagesJ9.1
Publication statusPublished - 2010
Event19th Symposium on Boundary Layers and Turbulence - Keystone, United States
Duration: 1 Aug 20106 Aug 2010

Conference

Conference19th Symposium on Boundary Layers and Turbulence
CountryUnited States
CityKeystone
Period1/08/106/08/10

Fingerprint

mixed layer
boundary layer
large eddy simulation
temperature inversion
entrainment
air mass
budget
humidity
temperature
divergence
moisture
grass
vegetation
air
experiment

Cite this

Pino, D., & Vilà-Guerau de Arellano, J. (2010). Role of boundary layer processes on the mixed layer CO2-budget. In 19th Symposium on Boundary Layers and Turbulence and the 29th Conference on Agricultural and Forest Meteorology; Keystone, Colorado, USA (pp. J9.1). Boston: AMS.
Pino, D. ; Vilà-Guerau de Arellano, J. / Role of boundary layer processes on the mixed layer CO2-budget. 19th Symposium on Boundary Layers and Turbulence and the 29th Conference on Agricultural and Forest Meteorology; Keystone, Colorado, USA. Boston : AMS, 2010. pp. J9.1
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abstract = "The diurnal and vertical variability of temperature, humidity and specially CO2 in the atmospheric boundary layer is studied by combining detailed observations taken at Cabauw (The Netherlands), Large-Eddy simulations (LES) and mixed layer theory. The research focus on the role played by the entrainment and other boundary layer driven processes on the distribution and diurnal evolution of CO2 in the boundary layer. The relative importance of this entrained air to ventilate CO2 will be analyzed. During the morning the exchange of CO2 between the residual free tropospheric air masses with the growing boundary layer is a more important contribution than the CO2 uptake by the vegetation, whereas during the afternoon the assimilation by grass at the ground could become the dominant process. This work is completed by quantifying the terms of the budget conservation equation of CO2 using observations and the LES numerical experiments. It will be shown that under non-advective conditions, the flux divergence measurements can correctly reproduce the diurnal variability of temperature, moisture and CO2. The role of boundary layer dynamics on the CO2-budget has direct implications in inferring the CO2-uptake flux from CO2 observations. Our findings show how dynamic factors, as the morning temperature inversion or the lapse rate, are relevant in the retrieval of the CO2 flux. By analyzing the sensitivity of the inferred CO2 flux to the dynamics of the boundary layer and to the CO2 variables, we are able to estimate the uncertainties of the inferred CO2 flux to mean CO2 concentrations",
author = "D. Pino and {Vil{\`a}-Guerau de Arellano}, J.",
note = "Joint Session 9 Exchange of Trace Gases (CO2, BVOC, Nitrogen) between the Surface and the PBL for Forest Ecosystems II (Joint between the 19th Symposium on Boundary Layers and Turbulence and the 29th Conference on Agricultural and Forest Meteorology)",
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Pino, D & Vilà-Guerau de Arellano, J 2010, Role of boundary layer processes on the mixed layer CO2-budget. in 19th Symposium on Boundary Layers and Turbulence and the 29th Conference on Agricultural and Forest Meteorology; Keystone, Colorado, USA. AMS, Boston, pp. J9.1, 19th Symposium on Boundary Layers and Turbulence, Keystone, United States, 1/08/10.

Role of boundary layer processes on the mixed layer CO2-budget. / Pino, D.; Vilà-Guerau de Arellano, J.

19th Symposium on Boundary Layers and Turbulence and the 29th Conference on Agricultural and Forest Meteorology; Keystone, Colorado, USA. Boston : AMS, 2010. p. J9.1.

Research output: Chapter in Book/Report/Conference proceedingConference paperAcademic

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N2 - The diurnal and vertical variability of temperature, humidity and specially CO2 in the atmospheric boundary layer is studied by combining detailed observations taken at Cabauw (The Netherlands), Large-Eddy simulations (LES) and mixed layer theory. The research focus on the role played by the entrainment and other boundary layer driven processes on the distribution and diurnal evolution of CO2 in the boundary layer. The relative importance of this entrained air to ventilate CO2 will be analyzed. During the morning the exchange of CO2 between the residual free tropospheric air masses with the growing boundary layer is a more important contribution than the CO2 uptake by the vegetation, whereas during the afternoon the assimilation by grass at the ground could become the dominant process. This work is completed by quantifying the terms of the budget conservation equation of CO2 using observations and the LES numerical experiments. It will be shown that under non-advective conditions, the flux divergence measurements can correctly reproduce the diurnal variability of temperature, moisture and CO2. The role of boundary layer dynamics on the CO2-budget has direct implications in inferring the CO2-uptake flux from CO2 observations. Our findings show how dynamic factors, as the morning temperature inversion or the lapse rate, are relevant in the retrieval of the CO2 flux. By analyzing the sensitivity of the inferred CO2 flux to the dynamics of the boundary layer and to the CO2 variables, we are able to estimate the uncertainties of the inferred CO2 flux to mean CO2 concentrations

AB - The diurnal and vertical variability of temperature, humidity and specially CO2 in the atmospheric boundary layer is studied by combining detailed observations taken at Cabauw (The Netherlands), Large-Eddy simulations (LES) and mixed layer theory. The research focus on the role played by the entrainment and other boundary layer driven processes on the distribution and diurnal evolution of CO2 in the boundary layer. The relative importance of this entrained air to ventilate CO2 will be analyzed. During the morning the exchange of CO2 between the residual free tropospheric air masses with the growing boundary layer is a more important contribution than the CO2 uptake by the vegetation, whereas during the afternoon the assimilation by grass at the ground could become the dominant process. This work is completed by quantifying the terms of the budget conservation equation of CO2 using observations and the LES numerical experiments. It will be shown that under non-advective conditions, the flux divergence measurements can correctly reproduce the diurnal variability of temperature, moisture and CO2. The role of boundary layer dynamics on the CO2-budget has direct implications in inferring the CO2-uptake flux from CO2 observations. Our findings show how dynamic factors, as the morning temperature inversion or the lapse rate, are relevant in the retrieval of the CO2 flux. By analyzing the sensitivity of the inferred CO2 flux to the dynamics of the boundary layer and to the CO2 variables, we are able to estimate the uncertainties of the inferred CO2 flux to mean CO2 concentrations

M3 - Conference paper

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BT - 19th Symposium on Boundary Layers and Turbulence and the 29th Conference on Agricultural and Forest Meteorology; Keystone, Colorado, USA

PB - AMS

CY - Boston

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Pino D, Vilà-Guerau de Arellano J. Role of boundary layer processes on the mixed layer CO2-budget. In 19th Symposium on Boundary Layers and Turbulence and the 29th Conference on Agricultural and Forest Meteorology; Keystone, Colorado, USA. Boston: AMS. 2010. p. J9.1