Advances in Meteorology

Research Article

Seasonal Variation and Characterization of the Micrometeorology in Linpan Settlements in the Chengdu Plain, China: Microclimatic Effects of Linpan Size and Tree Distribution

Table 4

Seasonal differences in the micrometeorology parameters.


Parameters	ΔT (°C)		ΔSR (W/m²)		ΔRH (%)		ΔW (m/s)

Spring	ΔT₁	0.9ab	ΔSR₁	263.8cd	ΔRH₁	−2.0b	ΔW₁	0.2cd
	ΔT₂	0.0e	ΔSR₂	70.8gh	ΔRH₂	0.4c	ΔW₂	0.2d
	ΔT₃	1.0ab	ΔSR₃	334.6b	ΔRH₃	−1.7bc	ΔW₃	0.4bc

Summer	ΔT₁	0.6cd	ΔSR₁	310.6bc	ΔRH₁	−2.5ab	ΔW₁	0.3bc
	ΔT₂	0.7cd	ΔSR₂	185.4ef	ΔRH₂	−1.6bc	ΔW₂	0.2cd
	ΔT₃	1.3a	ΔSR₃	496.0a	ΔRH₃	−4.1a	ΔW₃	0.5a

Fall	ΔT₁	0.6cd	ΔSR₁	127.0fg	ΔRH₁	−1.6bc	ΔW₁	0.2cd
	ΔT₂	0.7bc	ΔSR₂	80.6gh	ΔRH₂	−0.8bc	ΔW₂	0.7d
	ΔT₃	1.3a	ΔSR₃	207.6de	ΔRH₃	−2.4ab	ΔW₃	0.4bc

Winter	ΔT₁	0.2de	ΔSR₁	64.2i	ΔRH₁	−0.6bc	ΔW₁	0.2d
	ΔT₂	0.4de	ΔSR₂	27.9j	ΔRH₂	−0.3bc	ΔW₂	0.3bc
	ΔT₃	0.6de	ΔSR₃	92.1gh	ΔRH₃	−0.9bc	ΔW₃	0.5a

All values followed by letter are significantly different at according to Duncan’s test in SPSS. The different letters indicate there is statistically significant difference between the same group of variables.