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European CO budget and links with synoptic circulation based on GEOS-CHEM model simulations Cover

European CO budget and links with synoptic circulation based on GEOS-CHEM model simulations

Open Access
|Jan 2013

Figures & Tables

Table 1. Longitude and latitude of source regions shown in Fig. 1 and corresponding CO fossil fuel-biofuel/biomass burning emissions (Tg(CO)/yr) on seasonal basis in GEOS-CHEM as considered in this study

ContinentLatitudeLongitudeDJFMAMJJASON1. Europe32°N–88°N17.5°W–42.5°E28.7/0.128.7/0.227.9/2.228.3/0.32. North America24°N–88°N172.5°W–17.5°W28.0/0.128.0/0.927.3/3.527.6/3.53. Asia32°N–88°N 8°N–32°N42.5°E–177.5°E
70°E–177.5°E64.8/10.764.8/39.563.3/10.264.1/2.64. Africa36°S–32°N17.5°W–70°E14.6/68.315.0/14.215.0/75.814.8/52.25. South America56°S–24°N122.5°W–32.5°W14.6/20.115.0/32.115.0/51.414.8/77.56. Oceania52°S–8°N70°E–177.5°E5.7/7.15.8/8.95.8/15.45.8/18.1Total156.4/106.4157.3/95.8154.3/158.5155.4/154.2

Table 2. CO tagged tracers considered in GEOS-CHEM according to emission sources, geographical regions and chemical production

NameTracerCOtotalCO total concentrationCOFFEUCO from fossil fuel/biofuel burning in EuropeCOFFNA>> >> in North AmericaCOFFAS>> >> in AsiaCOFFRW>> >> in rest of the worldCOBBEUCO from biomass burning in EuropeCOBBNA>> >> in North AmericaCOBBAS>> >> in AsiaCOBBAF>> >> in AfricaCOBBSA>> >> in South AmericaCOBBOC>> >> in OceaniaCOCH4CO by CH4 oxidationCOISOPCO by isoprene >>COACETCO by acetone >>COMONOCO by monoterpenes >>COMEOHCO by methanol >>

Table 3. The main characteristics of the seasonal circulation patterns at SLP

Circulation typeSeason of occurrencePrevailing pressure systems in NHPrevailing circulation over EuropeLocation of main pressure centre over EuropeW_CTi i=+1,7WinterIcelandic Low, Azores High, Siberian HighAnticyclonic (+)1. Fennoscandia, 2. United Kingdom, 3. Central Europe–Western Mediterranean, 4. Iberian Peninsula, 5. Central–Eastern Europe, 6. Benelux, 7. Eastern Mediterranean–Eastern EuropeW_CTi i=−1,7WinterIcelandic Low, Azores High, Siberian HighCyclonic (−)1. Scandinavia, 2. Iceland, 3. Central Mediterranean, 4. Western Ireland–United Kingdom, 5. Central–Eastern Europe, 6. North Sea, 7. Eastern MediterraneanSP_CTi i=+1,8SpringIcelandic Low, Azores High, Siberian HighAnticyclonic (+)1. Fennoscandia–North-eastern Europe, 2. Central Europe–Central Mediterranean, 3. Ireland–United Kingdom, 4. Iceland, 5. Central–Eastern Europe, 6. Iberian Peninsula, 7. Eastern Europe–Eastern Mediterranean, 8. BeneluxSP_CTi i=−1,8SpringIcelandic Low, Azores High, Siberian HighCyclonic (−)1. Scandinavia, 2. Central Europe–Central Mediterranean, 3. Ireland–United Kingdom, 4. Iceland, 5. Eastern Europe, 6. Iberian Peninsula, 7. Eastern Mediterranean, 8.North Sea-Western ScandinaviaSU_CTi i=+1,8SummerAzores High, Asian Thermal LowAnticyclonic (+)1. Fennoscandia, 2. Central–Western Europe, 3. Ireland–United Kingdom, 4. Iceland, 5. South-eastern Europe, 6. North Atlantic–Iberian Peninsula, 7. Central–Eastern Europe, 8. North Sea–BeneluxSU_CTi i=−1,8SummerAzores High, Asian Thermal LowCyclonic (−)1. Scandinavia, 2. Central Europe, 3. United Kingdom, 4. Iceland, 5. South-eastern Europe, 6. South-eastern Europe–Iberian Peninsula, 7. Eastern Europe, 8. Western ScandinaviaA_CTi i=+1,8AutumnIcelandic Low, Azores High Siberian HighAnticyclonic (+)1. Scandinavia, 2. Central Europe, 3. United Kingdom, 4. Iceland, 5. Eastern Europe, 6. Iberian Peninsula, 7. Eastern Mediterranean–Eastern Europe, 8. BeneluxA_CTi i=−1,8AutumnIcelandic Low, Azores High Siberian HighCyclonic (−)1. Scandinavia, 2. Central Mediterranean–Central Europe, 3. United Kingdom, 4. Iceland, 5. Eastern Europe, 6. Iberian Peninsula, 7. Eastern Mediterranean, 8. Western Scandinavia

Table 4. Contribution (%) of the CO sources to the European CO concentrations at surface, 500 hPa and 200 hPa in winter and summer of 2001

Contribution (%)Surface500 hPa200 hPaCO sourcesWinterSummerWinterSummerWinterSummerCOFFEU16–7913–687–186–225–104–22COFFNA4–184–1210–189–136–113–14COFFAS6–205–1519–2512–1715–2213–30COFFRW<5<2<5<5<5<5COBBEU–0–34–<3%–<3%COBBNA<2<2––––COBBAS<2<5––––COBBAF, COBBSA, COBBOC<3–<6–––COCH45–2210–3222–3025–3528–3222–35COISOP<64–186–89–128–109–13COACET, COMONO, COMEOH<2%2–19<2%2–10<2%2–10
Fig. 1

Global CO anthropogenic surface emissions (in molec/cm2/s). Black boxes depict the geographical regions considered in GEOS-CHEM tagged CO analysis; 1: Europe, 2: North America, 3: Asia, 4: Africa, 5: South America, 6: Oceania.

Fig. 2

a) European domain (http://www.ngdc.noaa.gov/mgg/topo/globegal.html#continents) where the 31 rural background stations are located. b) PC1, PC2 and PC3 station regions in Europe.

Table 5. Annual contribution (%) of COFFEU, COFFNA, COFFAS, COFFRW and LRT (sum of COFFNA, COFFAS and COFFRW) to CO budget at the three station regions (PCs) in 2001

RegionMO
(ppbv) MES
(ppbv) MB
(ppbv)ME
(ppbv)R2
COFFEU
% COFFNA
% COFFAS
% COFFRW
% LRT
%PC1217.8221.9−4.132.90.8360.17.49.00.917.3PC2208.4236.4−28.049.10.5754.78.09.71.218.9PC3265.7255.310.435.40.6855.77.69.81.218.6

[i] Statistical parameters of the observed (O) and the estimated (ES) by the nested-grid simulation of GEOS-CHEM mean monthly CO concentrations in Europe are also presented. Statistical parameters equations can be found in Appendix S5.

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Table 6. Percentage contribution (%) of COFFNA, COFFAS and their sum (COFFLRT) in winter at each PC sub-region in relation to the frequency of occurrence (FO) of the circulation patterns in percentage (%)

PC1PC2PC3


CTFOCOFFNACOFFASCOFFLRTCOFFNACOFFASCOFFLRTCOFFNACOFFASCOFFLRTW_CT1+22.25.27.112.36.07.513.56.19.615.7W_CT2+8.97.510.017.56.07.713.68.210.418.5W_CT3+0.00.00.00.00.00.00.00.00.00.0W_CT4+2.210.915.626.57.09.816.811.416.728.1W_CT5+6.73.96.210.25.88.013.86.19.115.2W_CT6+5.67.110.217.45.57.312.87.19.616.7W_CT7+12.24.86.711.45.97.913.86.69.315.9W_CT1−5.610.613.023.58.110.518.59.712.822.5W_CT2−8.910.912.623.512.814.927.78.09.817.8W_CT3−2.27.111.919.06.311.718.06.412.518.9W_CT4−7.89.913.022.910.813.824.510.614.224.8W_CT5−5.611.317.328.68.912.521.411.618.129.6W_CT6−11.19.611.521.110.011.821.88.39.818.1W_CT7−1.14.66.711.38.713.221.96.38.614.9
Fig. 3

Frequency of occurrence of CTs in winter and summer of 2001 at a) SLP, b) 500 hPa, c) 200 hPa.

Table 7. Percentage contribution (%) of COFFNA, COFFAS and their sum (COFFLRT) in spring at each PC sub-region in relation to the frequency of occurrence (FO) of the circulation patterns in percentage (%)

PC1PC2PC3


CTFOCOFFNACOFFASCOFFLRTCOFFNACOFFASCOFFLRTCOFFNACOFFASCOFFLRTSP_CT1+0.00.00.00.00.00.00.00.00.00.0SP_CT2+0.00.00.00.00.00.00.00.00.00.0SP_CT3+12.09.711.621.37.59.817.38.511.319.8SP_CT4+15.28.613.121.78.512.320.99.714.123.9SP_CT5+2.27.911.219.19.512.522.08.311.419.7SP_CT6+2.29.615.625.111.919.231.110.014.724.8SP_CT7+3.311.513.224.713.515.428.99.512.221.7SP_CT8+0.00.00.00.00.00.00.00.00.00.0SP_CT1−6.59.713.423.011.716.528.39.612.722.3SP_CT2−7.611.416.427.812.717.330.010.614.224.8SP_CT3−15.26.510.016.510.514.024.57.812.220.0SP_CT4−6.510.012.922.913.016.829.89.913.923.8SP_CT5−8.78.613.121.67.210.417.69.013.722.7SP_CT6−12.06.610.416.910.413.924.29.314.423.7SP_CT7−1.18.314.823.110.015.625.69.815.625.4SP_CT8−8.79.314.724.010.416.326.79.114.323.4

Table 8. Percentage contribution (%) of COFFNA, COFFAS and their sum (COFFLRT) in summer at each PC sub-region in relation to the frequency of occurrence (FO) of the circulation patterns in percentage (%)

PC1PC2PC3


CTFOCOFFNACOFFASCOFFLRTCOFFNACOFFASCOFFLRTCOFFNACOFFASCOFFLRTSU_CT1+1.14.04.48.43.64.58.14.74.99.6SU_CT2+0.00.00.00.00.00.00.00.00.00.0SU_CT3+7.69.212.922.18.311.219.68.011.119.2SU_CT4+9.87.89.317.08.911.019.97.49.917.3SU_CT5+5.46.26.112.36.16.312.46.46.412.8SU_CT6+6.56.46.813.26.87.514.35.47.212.6SU_CT7+18.56.16.112.25.96.312.16.36.813.1SU_CT8+7.64.15.39.54.45.610.05.06.111.1SU_CT1−7.68.79.318.07.39.416.78.49.818.2SU_CT2−1.14.45.39.710.38.719.17.57.114.6SU_CT3−4.36.47.513.98.18.816.86.67.013.6SU_CT4−6.56.65.712.34.95.910.85.56.211.8SU_CT5−3.34.85.710.55.06.311.45.87.413.2SU_CT6−1.15.57.312.84.76.210.96.510.216.7SU_CT7−13.05.88.914.75.47.212.56.59.616.0SU_CT8−6.510.410.621.010.410.220.67.48.515.9
Fig. 4

Time series of the mean daily concentrations of CO measurements (black squares) and modelled concentrations of COtotal (red line) and COFFEU (green line) in the left axis and LRT (sum of COFFNA, COFFAS and COFFRW, purple line) concentrations in the right axis in 2001 at a) PC1, b) PC2, c) PC3.

{ label needed for table-wrap[@id='UT0009'] }

Table 9. Percentage contribution (%) of COFFNA, COFFAS and their sum (COFFLRT) in autumn at each PC sub-region in relation to the frequency of occurrence (FO) of the circulation patterns in percentage (%)

PC1PC2PC3


CTFOCOFFNACOFFASCOFFLRTCOFFNACOFFASCOFFLRTCOFFNACOFFASCOFFLRTA_CT1+0.00.00.00.00.00.00.00.00.00.0A_CT2+0.00.00.00.00.00.00.00.00.00.0A_CT3+19.89.210.419.66.97.714.69.09.718.6A_CT4+7.74.54.89.35.45.210.54.95.410.3A_CT5+7.78.35.513.810.98.018.88.26.414.6A_CT6+0.00.00.00.00.00.00.00.00.00.0A_CT7+11.09.86.716.59.88.017.87.76.814.5A_CT8+5.55.34.710.04.94.79.64.44.18.5A_CT1−8.810.98.919.98.07.315.39.48.618.0A_CT2−1.17.99.116.97.28.315.57.18.916.0A_CT3−5.54.44.38.75.24.910.15.14.69.7A_CT4−15.48.26.815.07.57.014.57.37.014.2A_CT5−0.00.00.00.00.00.00.00.00.00.0A_CT6−3.33.53.26.66.56.312.85.14.79.8A_CT7−4.45.44.810.25.35.610.85.55.611.1A_CT8−11.010.57.718.29.17.716.88.47.215.6
Language: English
Page range: 18640 - 18640
Submitted on: May 6, 2012
Accepted on: Mar 11, 2013
Published on: Jan 1, 2013
Published by: Stockholm University Press
In partnership with: Paradigm Publishing Services

© 2013 Anna P. Protonotariou, Effie Kostopoulou, Maria Tombrou, Christos Giannakopoulos, published by Stockholm University Press
This work is licensed under the Creative Commons Attribution 4.0 License.