• Nenhum resultado encontrado

Quantitative bias estimates for tropospheric NO<sub>2</sub> columns retrieved from SCIAMACHY, OMI, and GOME-2 using a common standard for East Asia

N/A
N/A
Protected

Academic year: 2017

Share "Quantitative bias estimates for tropospheric NO<sub>2</sub> columns retrieved from SCIAMACHY, OMI, and GOME-2 using a common standard for East Asia"

Copied!
9
0
0

Texto

Loading

Imagem

Fig. 1. Locations of MAX-DOAS observations on a monthly mean map (0.5 ◦ grid) of GOME-2 tropospheric NO 2 VCD data in May 2010.
Fig. 3. Same as Fig. 2 but the first, second, and third rows are for SCIAMACHY, OMI, and GOME-2, respectively
Table 2. Median values of tropospheric NO 2 columns and AOD for data used in the SCIAMACHY/MAXDOAS correlation analysis with x = 0.50 ◦
Fig. 6. Dependence of satellite-retrieved tropospheric NO 2 VCDs on the coincidence criterion x over each measurement site
+2

Referências

Documentos relacionados

We present global maps of spatial and temporal trends from the application of the model to the GOME data, and discuss the influence of the local wind field on the NO 2 trace

In order to achieve these objectives, we have first compared the daily maxima of ground ozone concentrations simulated by CHIMERE for summer months of 1997 and 2001 with

Correlation coefficients between the mean columnar SO 2 measured by the Brewers in Europe and provided by the satellite products of OMI and GOME-2 during the volcanic eruptions

Similar discrepancies are found when using the HYSPLIT trajectory model at different altitudes (10–13 km) or the wind speeds and directions, actually measured on board of the

The red points correspond to the tropospheric column-averaged CH 4 mole fraction derived from N 2 O and explicitly using tropopause pressure, the blue to those derived from N 2 O

Vertical and slant tropospheric NO 2 -columns from the new satellite instrument SCIA- MACHY on ENVISAT are validated by measurements of the Airborne Multi AXis DOAS

We retrieved XCO 2 (Case 2 XCO 2 ) data by using Toon’s so- lar irradiance data instead of Kurucz’s data and by taking into account the vertical profiles of the two types of

Relative horizontal representativeness errors as a func- tion of the covered fraction of one model grid cell in the case of OMI tropospheric NO 2 columns for polluted area(s)