Carbon stable isotope composition of berry must at harvest (δ 13 C) is an integrated assessment of plant water status during grape (Vitis vinifera L.) berry ripening. Measurement of δ 13 C of grape juice is proposed as an alternative to traditional measurements of water status to capture the spatial variability of physiological response at the vineyard scale, i.e., zoning. We performed samplings at four different locations in California, United States, with three different cultivars of table and wine grapes (Cabernet Sauvignon, Merlot, Crimson-Seedless). Leaf physiology (photosynthesis, A N , stomatal conductance, g s) and stem water potentials (stem) were routinely measured. The δ 13 C was measured at harvest and strong relationships were found between stem (R 2 = 0.71), stomatal conductance (R 2 = 0.71), net carbon assimilation (R 2 = 0.59) and WUEi (R 2 = 0.53). The role of leaf nitrogen on the signal was assessed by evaluating relationships between leaf nitrogen and WUE i (R 2 = 0.54), Ci/Ca (R 2 = 0.51), δ 13 C (R 2 = 0.44), and stem (R 2 = 0.37). Although nitrogen can be among the environmental factors able to affect the δ 13 C signal, this difference is only observable when variability in N is very large, by pooling different vineyards/varieties, but not at the within-vineyard scale. The utility of δ 13 C was further tested and measured on grape berries sampled on an equidistant grid in a 3.5 ha vineyard where stem was also measured throughout the field season and used to delineate management zones. Physiological measurements and grape composition were correlated to soil electrical resistivity and satellite-derived vegetation index. The two management zones obtained by δ 13 C or stem were spatially similar at 67% and allowed to separate the harvest in two pools having statistically different grape composition (soluble solids, organic acids, and anthocyanin profiles). Zoning by δ 13 C performed as well as zoning by stem to separate grape phenolic composition, e.g., for selective harvest. Our results provided evidence that δ 13 C of grape must is a reliable and repeatable assessor of plant water status and gas exchange in vineyard systems that are crucial for zoning vineyards, even when irrigated, and for ground-truthing sensor maps in precision viticulture.