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Analyzing the major drivers of NEE in a Mediterranean alpine shrubland

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Figure

Table 1. Empirically determined linear relations used to estimate random errors (σ) in fluxes as a function of the flux magnitude for theLaguna Seca field site (see Richardson et al., 2006)
Figure 2. Average daily environmental conditions in the Mediterranean alpine shrubland located in the Sierra Nevada mountain range (southeast Spain): (a) soil water content, (b) Fig
Figure 3. Annual and daily evolution of NEE (alpine Mediterranean shrubland located in the Sierra Nevada moun-tain range during (a) 2007 and (b)) by the alpine Mediterranean shrubland 2 -2-11µmol m slocated in the Sierra Nevada mountain range during (a) 20
Fig. 5a. Mean hourly NEE flux vs. PPFD during May, June, Julyand August 2007. Hysteresis was found for every month, with thetemporal trend proceeding counterclockwise.
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