Abstract
We present atmospheric CO2 and delta(O-2/N-2) from flask samples taken on board aircraft over Fyodorovskoye (56 degrees 27'N, 32 degrees 55'E) at heights of 3000 m and 100 m between 1998 and 2008. The long-term trends for CO2 and delta(O-2/N-2) are similar for both sampling heights, and also similar to observations from marine background station Mace Head (Ireland) and coastal station Lutjewad (the Netherlands). The seasonal CO2 amplitude at 100 m was almost twice as large as at 3000 m and a phase shift in the seasonality of about two weeks between both sampling heights was observed. This indicates a dominant influence on CO2 in the boundary layer from the regional biosphere which is confirmed by analysis of the delta(O-2/N-2) to CO2 oxidative ratio (OR). Together with simulations with the TM3 model, our data suggest that the observed OR of -1.7 +/- 0.2 in the free troposphere is mainly driven by exchange processes with the ocean. Within the boundary layer an OR of -0.89 +/- 0.12 was observed which supports the results of other recent studies suggesting the commonly used value of -1.1 for biospheric OR is likely too low. (C) 2014 Elsevier Ltd. All rights reserved.
Original language | English |
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Pages (from-to) | 174-181 |
Number of pages | 8 |
Journal | Atmospheric Environment |
Volume | 97 |
DOIs | |
Publication status | Published - Nov 2014 |
Keywords
- Atmospheric CO2
- Atmospheric delta(O-2/N-2)
- Oxidative ratio
- Global carbon cycle
- APO
- SOUTHERN TAIGA
- CARBON-CYCLE
- OXYGEN
- O-2/N-2
- SIBERIA
- AIR
- CLIMATOLOGY
- VARIABILITY
- NETWORK
- TOWER