Forest Evapotranspiration and Energy Flux Partitioning Based on Eddy Covariance Methods in an Arid Desert Region of Northwest China

Table 1

Daily means of the energy balance components and major biometeorological factors.

	(a) DOY; 323–64	(b) DOY; 65–130	(c) DOY; 131–169	(d) DOY; 170–253	(e) DOY; 254–288	(f) DOY; 289–322	Whole year
(°C)	−6.52	11.21	21.99	25.14	15.31	6.06	10.28
(°C)	−4.61	12.34	23.58	27.13	18.54	8.65	12.23
(%)	1.37	0.64	2.90	2.43	1.15	1.21	1.69
(%)	3.20	1.66	2.39	3.22	2.36	2.65	2.63
RH (%)	31.85	17.48	18.69	27.32	25.31	33.13	26.29
Precipitation (mm) (sum.)	0	1.2	6	7.1	0	2.1	16.4
(W·m^−2)	63.71	148.48	181.97	185.44	128.66	74.85	126.96
(W·m^−2)	17.80	74.91	59.33	21.91	38.90	21.34	35.81
LE (W·m^−2)	4.52	37.38	96.53	150.78	55.47	15.95	60.05
(W·m^−2)	−6.24	6.24	9.46	5.48	−4.16	−6.24	0.63
	0.28	0.50	0.33	0.12	0.30	0.29	0.28
LE/	0.07	0.25	0.53	0.81	0.43	0.21	0.47
	−0.10	0.04	0.05	0.03	−0.03	−0.08	0.01
EF	0.14	0.25	0.49	0.75	0.44	0.24	0.38
ET (mm)	0.17	1.20	3.40	5.09	1.96	0.56	1.79
ET0 (mm)	1.42	4.61	7.13	6.81	4.75	2.80	4.30
	0.12	0.26	0.48	0.75	0.41	0.2	0.42