Figures & data
Table 1. Number and wavelength range of the interference filters in the sun photometer types SP2H, SP1A and PFR
Fig. 2 Cluster allocation of ensemble trajectories at all heights (850, 700 and 500 hPa) for Ny-Ålesund 1995–2008.
![Fig. 2 Cluster allocation of ensemble trajectories at all heights (850, 700 and 500 hPa) for Ny-Ålesund 1995–2008.](/cms/asset/85b1d0c1-a0c1-48c6-a9e6-b2aee667df3d/zelb_a_11817285_f0002_ob.jpg)
Fig. 3 (a) Mean values and standard deviation of τ 500nm and α and (b) number of hourly mean AOD in different trajectory groups from Ny-Ålesund 1995–2008. Seasonal separation: spring – red; summer – green; autumn – blue.
![Fig. 3 (a) Mean values and standard deviation of τ 500nm and α and (b) number of hourly mean AOD in different trajectory groups from Ny-Ålesund 1995–2008. Seasonal separation: spring – red; summer – green; autumn – blue.](/cms/asset/18fe33fc-0315-4888-b2fb-810e0bb658d0/zelb_a_11817285_f0003_ob.jpg)
Fig. 4 Cluster allocation of ensemble trajectories at all heights (850, 700 and 500 hPa) for Sodankylä 2004–2007.
![Fig. 4 Cluster allocation of ensemble trajectories at all heights (850, 700 and 500 hPa) for Sodankylä 2004–2007.](/cms/asset/70172aef-b52a-4d83-afad-f5559e6a63f7/zelb_a_11817285_f0004_ob.jpg)
Fig. 5 (a) Mean values and standard deviation of τ 500nm and α and (b) number of hourly mean AOD in different trajectory groups from Sodankylä 2004–2007. Seasonal separation: spring – red; summer – green; autumn – blue.
![Fig. 5 (a) Mean values and standard deviation of τ 500nm and α and (b) number of hourly mean AOD in different trajectory groups from Sodankylä 2004–2007. Seasonal separation: spring – red; summer – green; autumn – blue.](/cms/asset/c6dadb04-137a-48e1-93a8-3bf2656b7a70/zelb_a_11817285_f0005_ob.jpg)
Fig. 6 (a) Clustering of the ensemble trajectories at all heights (850, 700, 500 hPa) from NP-35 between 14 March and 7 April, 2008, and (b) hourly mean of τ 500nm and α in the different trajectory groups and the group mean of τ 500nm and α.
![Fig. 6 (a) Clustering of the ensemble trajectories at all heights (850, 700, 500 hPa) from NP-35 between 14 March and 7 April, 2008, and (b) hourly mean of τ 500nm and α in the different trajectory groups and the group mean of τ 500nm and α.](/cms/asset/612f968c-fc91-4969-930b-6eec99061f8c/zelb_a_11817285_f0006_ob.jpg)
Fig. 9 Correlation between NAO-Index and monthly mean AOD in March (blue) and April (red) for Ny-Ålesund 1995–2008. Drawn are the monthly mean standard deviation and the linear regression of a) τ 500nm and b) α. The parameters of the regression, including the correlation coefficient and their confidence range, are shown in the legend.
![Fig. 9 Correlation between NAO-Index and monthly mean AOD in March (blue) and April (red) for Ny-Ålesund 1995–2008. Drawn are the monthly mean standard deviation and the linear regression of a) τ 500nm and b) α. The parameters of the regression, including the correlation coefficient and their confidence range, are shown in the legend.](/cms/asset/3a905c70-a2b2-4d57-b01c-3b896bbc191e/zelb_a_11817285_f0009_ob.jpg)
Fig. 10 First five EOF of mean sea-level pressure of three periods: left – December, January and February (1995–2008); middle – March (1995–2008); right – April (1995–2008) and their variance in %. The white star marks the position of Ny-Ålesund, respectively Spitsbergen.
![Fig. 10 First five EOF of mean sea-level pressure of three periods: left – December, January and February (1995–2008); middle – March (1995–2008); right – April (1995–2008) and their variance in %. The white star marks the position of Ny-Ålesund, respectively Spitsbergen.](/cms/asset/ce9bd49b-3040-4794-91cd-bd1721effb8c/zelb_a_11817285_f0010_ob.jpg)
Table 2. Correlation coefficients and confidence range for the correlation between the principle components (PC) of the first five EOF MSLP DJF and the monthly mean τ 500nm of March and April in Ny-Ålesund (1995–2008)
Table 3. Correlation coefficients and confidence range for the correlation between the principle components (PC) of the first five EOF MSLP March and April and the daily mean τ 500nm of March and April in Ny-Ålesund (1995–2008)
Table 4. Correlation coefficients and confidence range between the measured τ 500nm/α in Ny-Ålesund, which were assigned a trajectory cluster, and the measured concentration of different atmospheric chemical components at Zeppelin
Table 5. Correlation coefficients and confidence range between the measured τ 500nm in Ny-Ålesund, which were assigned to a unique trajectory cluster, and the measured concentration of different atmospheric chemical components at Zeppelin