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Atmospheric Measurement Techniques An interactive open-access journal of the European Geosciences Union
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Volume 8, issue 4
Atmos. Meas. Tech., 8, 1657–1671, 2015
https://doi.org/10.5194/amt-8-1657-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
Atmos. Meas. Tech., 8, 1657–1671, 2015
https://doi.org/10.5194/amt-8-1657-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 07 Apr 2015

Research article | 07 Apr 2015

How well do tall-tower measurements characterize the CO2 mole fraction distribution in the planetary boundary layer?

L. Haszpra1,2, Z. Barcza3,4, T. Haszpra5, Zs. Pátkai1, and K. J. Davis6 L. Haszpra et al.
  • 1Hungarian Meteorological Service, Budapest, Hungary
  • 2Geodetic and Geophysical Institute, MTA Research Centre for Astronomy and Earth Sciences, Sopron, Hungary
  • 3Dept. of Meteorology, Eötvös Loránd University, Budapest, Hungary
  • 4Institute of Ecology and Botany, MTA Centre for Ecological Research, Vácrátót, Hungary
  • 5MTA-ELTE Theoretical Physics Research Group, Budapest, Hungary
  • 6Dept. of Meteorology, Pennsylvania State University, University Park, Pennsylvania, USA

Abstract. Planetary boundary layer (PBL) CO2 mole fraction data are needed by transport models and carbon budget models as both input and reference for validation. The height of in situ CO2 mole fraction measurements is usually different from that of the model levels where the data are needed; data from short towers, in particular, are difficult to utilize in atmospheric models that do not simulate the surface layer well. Tall-tower CO2 mole fraction measurements observed at heights ranging from 10 to 115 m above ground level at a rural site in Hungary and regular airborne vertical mole fraction profile measurements (136 vertical profiles) above the tower allowed us to estimate how well a tower of a given height could estimate the CO2 mole fraction above the tower in the PBL. The statistical evaluation of the height-dependent bias between the real PBL CO2 mole fraction profile (measured by the aircraft) and the measurement at a given elevation above the ground was performed separately for the summer and winter half years to take into account the different dynamics of the lower troposphere and the different surface CO2 flux in the different seasons. The paper presents (1) how accurately the vertical distribution of CO2 in the PBL can be estimated from the measurements on the top of a tower of height H; (2) how tall of a tower would be needed for the satisfaction of different requirements on the accuracy of the estimation of the CO2 vertical distribution; (3) how accurate of a CO2 vertical distribution estimation can be expected from the existing towers; and (4) how much improvement can be achieved in the accuracy of the estimation of CO2 vertical distribution by applying the virtual tall-tower concept.

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