How well do tall-tower measurements characterize the CO&amp;lt;sub&amp;gt;2&amp;lt;/sub&amp;gt; mole fraction distribution in the planetary boundary layer?

L Haszpra,Z Barcza,K J Davis,T Haszpra,Zs Pátkai

doi:10.5194/amt-8-1657-2015

Abstract

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.

Highlights

Anthropogenic activity can influence the global climate in the long term through the emission of greenhouse gases, most notably carbon dioxide (CO2) (Skeie et al, 2011; IPCC, 2013)
We present the trade-off between the height of the tower and the accuracy of the CO2 mole fraction estimation at higher elevation above the tower
In summer the shorter the tower, the higher the underestimation of the mole fraction above the tower, especially close to the top of the Planetary boundary layer (PBL). It is caused by two facts: (1) in summer daytime the surface is usually a net CO2 sink due to the intense photosynthetic CO2 uptake that exceeds the sum of total ecosystem respiration and anthropogenic sources in this rural region (Barcza, 2001); (2) the upper part of the PBL may be strongly influenced by the entrainment of free-tropospheric air usually having a higher CO2 mole fraction at this time of the year than the layers below (Haszpra et al, 2012)

Summary

Introduction

Anthropogenic activity can influence the global climate in the long term through the emission of greenhouse gases, most notably carbon dioxide (CO2) (Skeie et al, 2011; IPCC, 2013). Mathematical models (inverse models of atmospheric transport of varying complexity) have been developed to describe the atmospheric carbon budget (e.g., Tans et al, 1989; Gurney et al, 2003; Baker et al, 2006; Butler et al, 2010; Ciais et al, 2010; Trusilova et al, 2010; Saeki et al, 2013; Broquet et al, 2013; Jiang et al, 2013; Peylin et al, 2013; and references therein) estimating surface sources and sinks of carbon dioxide.

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