Table 2.

Reach-scale morphology, subsurface flow capacity, and likelihood of streamflow presence within Falling Rock. Flow-state sensors were placed in four reaches, as recorded in the last column and shown in Fig. 1. Reach ID 3802 is the most downstream reach.

Reach no.	Strahler Order	Slope (m m−1)	Upstream Area (m2)	Qsub,c (m3 hr−1)	Likelihood Streamflow Present	Flow-state sensor designation
1	4	0.03	954,609	0.0287	100
2	4	0.02	916,783	0.0255	100
3	4	0.02	898,584	0.026	100	FC1
4	4	0.03	785,984	0.0276	100
5	3	0.04	482,728	0.0394	100
6	3	0.05	300,299	0.0547	100
7	3	0.04	263,696	0.0416	100
8	3	0.03	219,253	0.0362	100	FC2
9	3	0.05	220,585	0.0518	100
10	3	0.06	117,539	0.0647	100
11	2	0.06	174,347	0.0614	100
12	2	0.14	52,007	0.1444	86.5
13	2	0.16	69,432	0.1727	98.1
14	2	0.14	57,838	0.152	85.8	FC3
15	2	0.08	92,160	0.0884	100
16	2	0.16	90,109	0.1708	98.5
17	1	0.32	15,737	0.3434	31.1
18	1	0.36	9,921	0.3851	1.9
19	1	0.36	21,300	0.3784	21.6
20	1	0.45	25,755	0.475	65.7
21	1	0.2	71,803	0.2084	43.9
22	1	0.18	54,620	0.1883	56.6
23	1	0.35	21,383	0.3697	2.1
24	1	0.4	10,251	0.4228	26
25	1	0.43	15,732	0.4508	22.8	FC4
26	1	0.46	21,102	0.4862	0
27	1	0.42	20,006	0.4448	37.2
28	1	0.23	18,446	0.2439	46.8
29	1	0.36	10,148	0.3782	32.4
30	1	0.42	22,004	0.4422	31.6
31	1	0.4	20,894	0.4223	71.4
32	1	0.22	77,674	0.2297	52.4
33	1	0.23	59,307	0.2434	10.2