Derivation of Geodesic Flow Fields and Spectrum in Digital Topographic Basins

Figure 3

Synthetic tidal basin shown in Figure 1(c)—that consists of channelized and nonchannelized regions—after decomposing into sets. (a)–(i) sets representing channelized and nonchannelized regions of which the mean elevations increase from S₁ to S₉. The sets with even- and odd-numbered indexes, respectively, represent the zones occupied by channelized and nonchannelized regions.

(a)

(b)

(c)

(d)

(e)

(f)

(g)

(h)

(i)