The Scientific World Journal / 2012 / Article / Tab 6 / Research Article
The Influence of Wildfires on Aerosol Size Distributions in Rural Areas Table 6 Weather types and radiative and subsidence thermal inversions during the days with an average number of particles exceeding 2000 particles cm−3 (—) means the data are not available.
Day No. of particles cm−3 Circulation weather type Madrid 0000 UTC A Coruña 0000 UTC Santander 0000 UTC Inversions Inversions Inversions Radiative (m AGL) Subsidence (m AGL) Radiative (m AGL) Subsidence (m AGL) Radiative (m AGL) Subsidence (m AGL) 21/07/00 2084 ± 748 C 208 662 252 01/08/00 2501 ± 1041 NE 94 494 837 767 07/08/00 2775 ± 3243 E 664 894 09/08/00 4723 ± 3233 NE 235 462 277 10/08/00 2376 ± 1671 N 361 602 441 634 11/08/00 2380 ± 505 NW 113 — — 77 798 12/08/00 3755 ± 2562 A 720 13/08/00 2431 ± 1092 A 102 14/08/00 3032 ± 1991 A 177 — — 111 15/08/00 3014 ± 2090 ANE — — 16/08/00 3101 ± 2911 NE 190 794 17/08/00 3000 ± 2766 N 132 960 18/08/00 2240 ± 2304 CNW 161 733 85 20/08/00 2330 ± 1155 N 65 69 25/08/00 2157 ± 4291 C 46 324 26/08/00 2760 ± 3202 AN — — 09/09/00 2028 ± 886 E 664 68 606 103 436 16/09/00 2896 ± 2179 C 186 945 22/09/00 2931 ± 2227 ASW 292 111 23/09/00 4912 ± 4005 W 192 295 267 897 24/09/00 5201 ± 3079 A 184 278 25/09/00 2654 ± 3305 A 268 341 16 26/09/00 5405 ± 4341 AN 92 968 372 27/09/00 6972 ± 7035 A 109 28/09/00 6259 ± 4654 W — — — — — 29/09/00 3625 ± 6597 NW — — — — — 30/09/00 2736 ± 2870 NW