Satellite- and ground-based CO total column observations over 2010 Russian fires: Accuracy of top-down estimates based on thermal IR satellite data

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Abstract

CO total column data are presented from three space sounders and two ground-based spectrometers in Moscow and its suburbs during the forest and peat fires that occurred in Central Russia in July-August 2010. Also presented are ground-based in situ CO measurements. The Moscow area was strongly impacted by the CO plume from these fires. Concurrent satellite- and ground-based observations were used to quantify the errors of CO top-down emission estimates. On certain days, CO total columns retrieved from the data of the space-based sounders were 2-3 times less than those obtained from the ground-based sun-tracking spectrometers. The depth of the polluted layer over Moscow was estimated using total column measurements compared with CO volume mixing ratios in the surface layer and on the TV tower and found to be around 360 m. The missing CO that is the average difference between the CO total column accurately determined by the ground spectrometers and that retrieved by AIRS, MOPITT, and IASI was determined for the Moscow area between 1.6 and 3.3 Ã- 1018 molec cm-2. These values were extrapolated onto the entire plume; subsequently, the CO burden (total mass) over Russia during the fire event was corrected. A top-down estimate of the total emitted CO, obtained by a simple mass balance model increased by 40-100 % for different sensors due to this correction. Final assessments of total CO emitted by Russian wildfires obtained from different sounders are between 34 and 40 Tg CO during July-August 2010. © 2011 Author(s).

Figures

  • Fig. 1. Moscow, Russia, locations of ground-based instruments.
  • Fig. 2. Normalized averaging kernels for CO TC retrieved from data of space- and ground-based instruments, various days of 2010 (e.g. 0809 corresponds to 9 August 2010). A priori profiles: AP 5.4 corresponds to CO TC equal to 5.4× 1018 molec cm−2, etc. SCIAMACHY AK is adopted from Liu et al. (2011).
  • Fig. 3. Daily mean CO TC retrieved from spectra recorded by 3 sounders over grid cell centered at 55.5◦ N and 36.5◦ E. Data of Zvenigorod spectrometer play a role of ground truth. Vertical bars are standard deviations of individual measurements.
  • Table 1. CO TC (in units × 1018 molec cm−2) calculated according to Eq. (1) with a “true” CO profile for Moscow around 11:30 Moscow local time (7 ppm of CO VMR from the surface to 300 m above the surface; 0.22 ppm between 300 m and 5000 m above the surface; then gradual decline down to 0.026 ppm near the tropopause). A priori profiles correspond to those used normally for each data set. AK correspond to Fig. 2. Bottom row is a relation of convolved value to the truth.
  • Fig. 4. Scattergrams of CO TC for 3 sounders compared to ground data over Zvenigorod for matching days between January 2009 and September 2010: (a) AIRS; (b) MOPITT; (c) IASI-OE; (d) IASISFA.
  • Table 2. Averages, STD of daily means, and numbers of days for CO TC (× 1018 molec cm−2) for the 1◦× 1◦ degrees grid cell centered at 55.5◦ N, 36.5◦ E for different data sets for 2009, months May through September, and 2010, months May and June, inclusive. MOPITT data for August and September 2009 are lacking due to a calibration of the instrument. The bottom row is for the period that is common for all 5 data sets.
  • Fig. 6. Averaged over the area 40◦–75◦ N, 30◦–150◦ E CO TC values (right scale) and corresponding burdens (left scale) according to operational data of MOPITT V4 and AIRS V5, as well as IASI retrieved using 3 different algorithms, in 2010. AIRS background line is shown as an example. The background line represents TC that is expected without wildfires and is plotted through the lowest points of data in 10-days intervals.
  • Fig. 5. (a) Map of OMI aerosol index for 9 August 2010. (b) Distribution of CO VMR-500 for 9 August, 2010, according to AIRS. Black square is the area of CO averaging. Location of Moscow is marked by a white cross.

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CITATION STYLE

APA

Yurganov, L. N., Rakitin, V., Dzhola, A., August, T., Fokeeva, E., George, M., … Strow, L. (2011). Satellite- and ground-based CO total column observations over 2010 Russian fires: Accuracy of top-down estimates based on thermal IR satellite data. Atmospheric Chemistry and Physics, 11(15), 7925–7942. https://doi.org/10.5194/acp-11-7925-2011

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