Decadal variability of soil CO₂ NO, N₂O, and CH₄ fluxes at the Höglwald Forest, Germany

Model estimated CO 2 time series at two surface stations in the southern extra-tropics, compared to CO 2 measurements taken at those stations.. The “GOSAT” line is from an

Seven of the reservoirs (Lake Wohlen, Lake Gruy `ere, Lake Sihl, Lake Luzzone, Lake Santa Maria, Lake Oberaar and Lake Lungern) were sampled several times during the campaign

at continental sites, which are attributed to model transport errors within the planetary boundary layer or in the stratosphere or model errors in the seasonal amplitude of

The framework is based on a mass balance ap- proach and given that for Europe most of the components have been independently estimated, di ff erent accounting schemes may be used

To test the impact of changing the vertical resolution of the transport model on the optimized fluxes, we assimilated the same data sets (surface layer and GOSAT) in inversions

incubating intact soil cores from four sites (three savanna, one pasture) under controlled soil temperatures (ST) and soil moisture (SM) we investigated the release of the trace

Another impact of non-acyl peroxy nitrates is that they are a possible positive inter- ference to in-situ NO 2 measurements in the upper troposphere because the non-acyl peroxy

In this manuscript, we describe observations of atmospheric reactive nitrogen com- pounds including NO, NO 2 , total peroxy nitrates ( Σ PNs), total alkyl nitrates ( Σ ANs), and HNO