High levels of air pollution in South-Eastern England

High air pollution in parts of western Europe

01 April 02:56 UTC–02 April 2014 02:58

High levels of air pollution in South-Eastern England
High levels of air pollution in South-Eastern England

On 1 April, the Global Ozone Monitoring Experiment (GOME-2) instruments on Metop-A and B observed elevated levels of NO2 total column concentration over parts of Germany, Belgium, the Netherlands and England.

Last Updated

10 March 2021

Published on

01 April 2014

by Ruediger Lang (EUMETSAT)

In late March a large amount of Saharan dust was transported to Europe , this was still being carried to South-East England on 1 April.

Also, as shown in this RGB dust video , 1 April 08:00 UTC–2 April 08:00 UTC (Credit: Met Office/YouTube), further dust was lifted into the atmosphere on 1 April. The dust can clearly be seen being carried north towards Europe.

At the same time elevated aerosol thickness was observed over the North Sea and over the Channel area. Note: GOME-2 can currently only observe aerosol concentration over water surfaces.

RGB Dust animation, 28 March 12:00 UTC–31 March 12:00 UTC

 
Tropospheric NO
Figure 1: Tropospheric NO2 columns, 1 April. Full Resolution
 
Tropospheric NO
Figure 2: Tropospheric NO2 columns, 20 March–4 April. Credit: O3MSAF (DLR/EUMETSAT)
Aerosol optical depth (AOD), 30 March
Figure 3: Aerosol optical depth (AOD), 30 March. Full Resolution
 
Aerosol optical depth (AOD), 22 March–6 April
Figure 4: Aerosol optical depth (AOD), 22 March–6 April. The animated gif is derived from data from Metop, GOME-2, AVHRR and IASI.
 

 

High levels of air pollution in parts of western Europe
Figure 5: Convection RGB, 3 April 12:00 UTC

On the daytime convection RGB (Credit: EUMeTrain) the dust-polluted clouds can be seen as the large yellow area.

Dust aerosols have a large impact on cloud microphysics such as cloud phase and cloud particle size.

In general, clouds that have ingested dust glaciate more quickly, forming a large number of very small ice particles. These have a higher reflectance than large ice particles in the 'microphysical' channels (near-IR 1.6 and IR 3.9 micrometer), so they appear as bright yellow in the convection RGB.

Download full resolution Convection RGB, 3 April 12:00 UTC
Download full resolution Convection RGB, 4 April 07:00 UTC

 
Figure 6: Daily Air Quality Index

Met Office air pollution forecast, 2/3 April

 

The formation of aerosols, or Particulate Matter (PM), may originate from natural or anthropogenic sources. In industrial areas aerosols may be formed through the emission of gases like NOx, SOx or formaldehyde (HCHO), from combustion processes which form larger particles through chemical reactions in a process called secondary aerosol formation.

Belgium, the Netherlands, the German region of Ruhrgebiet and southern Britain are known to have elevated NO2 concentrations throughout the year, due to industrial emissions and emissions from traffic.

The formation of particulate matter or aerosols from these precursor gases depends largely on the weather conditions, including wind speed, humidity and temperature. A lack of rain over western Europe significantly contributed to the situation. 

But also the inflow of natural aerosols, like long-range transport from Saharan dust, may contribute to the overall levels of abundant levels of PM, leading to a mixed-case scenario.


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