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On the basis of the measurements at two monitoring sites located close to each other (220 km) in plain regions in Hungary, the representativeness of low‐elevation continental CO 2 measurements is estimated. It is shown that under such conditions only the measurements carried out in the early afternoon hours can be considered as regionally representative for the CO 2 content of the planetary boundary layer (PBL). Filtering the data in this way, it is calculated that the characteristic CO 2 mixing ratio in the PBL may be about 2.5 ppm higher over this part of Europe than at the Mauna Loa Observatory (National Oceanic and Atmospheric Administration), Hawaii.
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László Haszpra (1999) studied this question.
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