It might be surprising to know that the smoke has even made its way as far as Europe.
Fig. 1: A view of the smoke from the California fires as seen from the Copernicus Sentinel-3 satellite, taken on 10 September 2020
Federico Fierli, Atmospheric Composition expert at EUMETSAT said:
Each year, we observe extensive and prolonged wildfires in many regions and California is known to be one of the most affected. However, this year appears to be exceptional, as preliminary data has shown it is estimated to be a record in terms of extent and fire emissions.
Last week was characterised by an even higher intensity of fires as documented by NASA satellite observations, who reported a rare Pyrocumulonibus cloud developing in southern California from 6 September (see Fig.2).
These types of clouds are comparable to convective towers and are generated by fire at high temperatures. They are usually more likely to appear at northern latitudes (e.g. Canada or Siberia) where the atmosphere is colder.
The clouds release the fire’s emissions (such as gas and particles) at a higher altitude, thanks to the intense uplift amplifying the impact the fire has on the composition of the atmosphere.
Fig. 2: This infrared image shows a white corona-like structure – the high cloud and plume extending out of it clearly depicts the particle outflow. Image taken by EUMETSAT’s Metop-C satellite.
Vertical uplift plays a role in spreading fire emissions over longer distances, due to the fact that horizontal transport is more efficient at a higher altitude in the atmosphere because of stronger winds and therefore, removal of these products is less efficient.
Monitoring the smoke’s reach
The long-range transport of emissions can be observed by satellites and the carbon monoxide (CO) that is produced by combustion stays in the atmosphere for weeks, making it easier for us to track. In this next example, a burst of CO is visible over southern California from 7 September during the most intense phase of the fires, generating a vast plume of smoke that has been spread by atmospheric winds across the Atlantic Ocean.
Cathy Clerbaux, Senior Scientist at LATMOS/CNRS said:
CO is a very good tracer of combustion. Since the launch of the IASI instrument in 2006, it is the first time that we’ve seen such a clear, massive CO plume travelling across the ocean and reaching Europe.
Fig. 3: An animation showing data from the CNES-developed infrared atmospheric sounding interferometer (IASI) instrument on board Metop-A, -B and -C, showing the evolution of CO over one month from 19 August, mostly produced as a result of the fires in California
The transport of plumes over Europe is also due to the exceptional amount of CO released into the atmosphere, much larger than other regions where active wildfires are also intense emitters. Federico added:
Wildfires contribute substantially to the global budget of atmospheric carbon, which also includes CO2. Satellite data tells us that the carbon monoxide observed over the west of California has tropospheric concentrations that are four times higher than those recorded in Amazonia and Central Africa, known to be the highest emissive regions. These appear as red plumes over the Western Pacific.
Fig 4: This image shows the concentration of CO from the TROPOspheric Monitoring Instrument (TROPOMI) on board Sentinel-5P, accumulated from 9 – 11 September
Fig. 5: The intensity of the emissions being transported is also visible as atmospheric particles, observed by the aerosol index from the Global Ozone Monitoring Experiment–2 (GOME-2) instrument onboard both the Metop-B and -C satellites on 15 September, with a similar plume extending from California to the Northern Atlantic