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

<div>The daily evapotranspiration (ET) and daily reference evapotranspiration (ET<sub>0</sub>) in the following periods: (a) the soil-frozen period; (b) the soil ablation period; (c) the germination, flowering, and leaf expansion period; (d) the vibrant growing season; (e) the leaf senescence period; and (f) the early soil-frozen period.</div>

Advances in Meteorology

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Figure 6

Figure 6: Forest Evapotranspiration and Energy Flux Partitioning Based on Eddy Covariance Methods in an Arid Desert Region of Northwest China 