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