Open AccessInsights from simulations with high‐resolution transport and process models on sampling of the atmosphere for constraining midlatitude land carbon sinks
Author(s) -
Karstens U.,
Gloor M.,
Heimann M.,
Rödenbeck C.
Publication year - 2006
Publication title -
journal of geophysical research: atmospheres
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.67
H-Index - 298
eISSN - 2156-2202
pISSN - 0148-0227
DOI - 10.1029/2005jd006278
Subject(s) - troposphere , middle latitudes , atmospheric sciences , environmental science , planetary boundary layer , sink (geography) , atmosphere (unit) , sampling (signal processing) , climatology , latitude , atmospheric model , meteorology , geology , geodesy , physics , geography , cartography , optics , detector , turbulence
We analyze the requirements for detecting changes in midlatitude land carbon sources or sinks from sampling the atmospheric CO 2 concentration. Programs to sample the continental lower troposphere have only recently started, and it is not yet clear which atmospheric sampling strategy is most adequate. To shed some light on this question, we use simulations of atmospheric CO 2 over Eurasia with two regional‐scale atmospheric transport models. Our analysis focuses on the detection of the monthly mean CO 2 signal caused by a perturbation of Eurasian summer biospheric fluxes by 20% (0.06 PgC/month). The main results are (1) that several measurements per day, preferably during the afternoon, are necessary to permit the detection of the additional land sink and (2) that the ratio between signal and background variation, corrected for autocorrelation in time, suggests no preferred level in the vertical for sampling. However, (3) the signals in the free troposphere are very small (0.2 ppm per 0.06 PgC/month) given the precision of atmospheric measurements. In contrast, signals in the planetary boundary layer (PBL) are on the order of 1 ppm per 0.06 PgC/month. This suggests that optimal sampling on continents should concentrate on the mixed portion of the PBL during afternoon. (4) Finally, the spatial correlation structure of the atmospheric CO 2 concentrations suggests that a horizontal sampling density on the order of a few 100 km is needed.