Comparisons of continuous atmospheric CH₄, CO₂ and N₂O measurements – results from a travelling instrument campaign at Mace Head

Even though some HCHO and HCDO is lost to reactions through the course of the experiment the model shows that this a ff ects both formalde- hyde isotopologues almost equally (i.e.

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

In our previous studies (Benson et al., 2008; Young et al., 2008), we reported the residual [H 2 SO 4 ] (measured at the end of the nucleation reactor) and further used the

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

First, the longitudinal distributions of these species in January 2008 highlight strong variations of OClO and NO 2 (relative to the longitude) in the lower stratosphere: in the

The similar rate of increase of CO 2 emissions in function of increasing soil water content observed in the burned and unburned plots (field data), despite the very di ff

Weekly aggregated values of environmental parameters (upper panel: precipitation (black bars), temperature (red line: soil temperature, red dashed line: air temperature), soil

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