Extended Data Fig. 7. Rooting zone water storage capacity along topographic gradients in central Asia.

(a) Rooting zone water storage capacity in central Asia, estimated by the magnitude of cumulative water deficit extreme events with a return period of 80 years S_CWDX80). (b) Compound Topography Index⁶⁰, shown as 90% quantiles of underlying pixels, given at 15 arcsec, within matching 0.05^∘ gridcells. (c) Elevation from ETOPO1⁴³. Red and blue rectangles indicate the domains for which S_CWDX80 distributions along a CTI and an elevation gradient are shown in (d), (e), (f) and (g). The Compound Topography Index (CTI) is a measure for subsurface flow convergence and the water table depth based on the topographical setting⁶¹. Boxes represent the interquartile ranges of binned values (Q₂₅, Q₇₅), and whiskers cover Q₂₅ − 1.5(Q₇₅ − Q₂₅) to Q₇₅ + 1.5(Q₇₅ − Q₂₅). Numbers of data points per bin are given above boxes.