From: On the use of alternative water use efficiency parameters in dryland ecosystems: a review
Scale | Definition | Methodology | Advantages/disadvantages | Patterns of WUE response to climatic variation found in references | References |
---|---|---|---|---|---|
Leaf level | \( \mathrm{WUE}=\frac{\mathrm{A}}{\mathrm{T}}=\frac{{\mathrm{C}}_{\mathrm{a}}-{\mathrm{C}}_{\mathrm{i}}}{1.6\Delta \mathrm{w}} \) Ca and Ci, ambient and inner-leaf partial pressure of CO2, respectively; ∆w, the difference of water vapor | Gas exchange | Reflects that plants control stomata to optimally satisfy the trade-off between the amount of carbon assimilated and the amount of water transpired; easy to measure; adaptable to small-scale and several species; not appropriate for all biomes | Leaf WUE decreases with precipitation increase; effect of climate warming is uncertain for leaf WUE. | |
\( {\mathrm{WUE}}_i=\frac{\mathrm{A}}{\mathrm{g}}=\frac{{\mathrm{C}}_{\mathrm{a}}-{\mathrm{C}}_{\mathrm{i}}}{\mathrm{Pa}} \) Pa, atmospheric pressure | Gas exchange; stable isotope discrimination | More appropriate than WUE for describing the biochemical functions of vascular plants; easy to measure; not applicable for all biomes | WUEi increases during dry seasons in plants with smaller and narrower leaves. | ||
Ecosystem level | \( {\mathrm{WUE}}_{\mathrm{et}}=\frac{\mathrm{GPP}}{\mathrm{ET}} \) \( \mathrm{or}=\frac{\mathrm{GEP}}{\mathrm{ET}}, \) \( =\frac{\mathrm{NPP}}{\mathrm{ET}}, \) \( =\frac{\mathrm{NEE}}{\mathrm{ET}} \) | Models with RS products; EC flux data | Could be estimated by models with RS data at large scale; but the inherent carbon–water process of plants were not clear | Precipitation increases WUE, while climate warming reduces WUE; droughts increase WUE in Northeast China and central Inner Mongolia but decrease WUE in central China; WUE response to drought in arid ecosystems (WUE increases with drought) contrasts that in semi-arid/sub-humid ecosystems (WUE decreases with drought). | |
\( {\mathrm{WUE}}_{\mathrm{t}}=\frac{\mathrm{GPP}}{\mathrm{T}} \) | Models with RS products | Other ecosystem WUE could be calculated by WUEt, but the T is not easy to measure or model at large scale | Precipitation increases WUEt, while climate warming reduces WUEt; WUEt shows lower sensitivity to precipitation than WUE. | ||
\( {\mathrm{IWUE}}_{\mathrm{et}}=\frac{\mathrm{GPP}\times \mathrm{VPD}}{\mathrm{ET}} \) | EC flux data; models with RS products | Indicates possible adaptive adjustment of ecosystem physiology in response to a changing environment; easy to estimate at large scale; | IWUEet increases during short-term moderate droughts. | ||
\( {\mathrm{IWUE}}_{\mathrm{t}}=\frac{\mathrm{GPP}\times \mathrm{VPD}}{\mathrm{T}} \) | EC flux data; models with RS products | Indicates the biophysical process at large scale; but T is not easy to measure or model | IWUEt is conservative with precipitation. |