Main Characteristics of Mexico City Local Wind Events during the MILAGRO 2006 Campaign within a Meso-β Scale Lattice Wind Modeling Approach

Table 2

The first ten discrete wind states with the highest frequencies.

State number	[U : θ : γ : ω]	Frequency (%)	WSP (m/s)	WDR	WDIV	WVOR
110	[1 : 4 : 0 : 2]	6.45	0.25 ≤ v < 1.5	S	Convergent	Cyclonic
117	[1 : 5 : 0 : 0]	6.45	0.25 ≤ v < 1.5	SW	Convergent	Anticyclonic
146	[2 : 0 : 0 : 2]	5.91	1.5 ≤ v < 3.5	N	Convergent	Cyclonic
137	[1 : 7 : 0 : 2]	5.65	0.25 ≤ v < 1.5	NW	Convergent	Cyclonic
126	[1 : 6 : 0 : 0]	5.38	0.25 ≤ v < 1.5	W	Convergent	Anticyclonic
87	[1 : 1 : 2 : 0]	4.84	0.25 ≤ v < 1.5	NE	Divergent	Anticyclonic
96	[1 : 2 : 2 : 0]	3.90	0.25 ≤ v < 1.5	E	Divergent	Anticyclonic
182	[2 : 4 : 0 : 2]	3.90	1.5 ≤ v < 3.5	S	Convergent	Cyclonic
119	[1 : 5 : 0 : 2]	3.76	0.25 ≤ v < 1.5	SW	Convergent	Cyclonic
128	[1 : 6 : 0 : 2]	3.09	0.25 ≤ v < 1.5	W	Convergent	Cyclonic

WSP: wind speed, WDR: wind direction, WDIV: wind divergence, and WVOR: wind vorticity.