Abstract. Wise management of water resources requires data. Nevertheless, the amount of
streamflow data being collected globally continues to decline. Generating
hydrologic data together with citizen scientists can help fill this growing
hydrological data gap. Our aim herein was to (1) perform an initial
evaluation of three simple streamflow measurement methods (i.e., float, salt
dilution, and Bernoulli run-up), (2) evaluate the same three methods with
citizen scientists, and (3) apply the preferred method at more sites with
more people. For computing errors, we used midsection measurements from an
acoustic Doppler velocimeter as reference flows. First, we (authors) performed 20 evaluation
measurements in headwater catchments of the Kathmandu Valley, Nepal.
Reference flows ranged from 6.4 to 240 L s−1. Absolute errors averaged
23 %, 15 %, and 37 % with average biases of 8 %, 6 %, and
26 % for float, salt dilution, and Bernoulli methods, respectively.
Second, we evaluated the same three methods at 15 sites in two watersheds
within the Kathmandu Valley with 10 groups of citizen
scientists (three to four members
each) and one “expert” group (authors). At each site, each group performed three simple
methods; experts also performed SonTek FlowTracker midsection reference
measurements (ranging from 4.2 to 896 L s−1). For float, salt
dilution, and Bernoulli methods, absolute errors averaged 41 %, 21 %,
and 43 % for experts and 63 %, 28 %, and 131 % for citizen
scientists, while biases averaged 41 %, 19 %, and 40 % for
experts and 52 %, 7 %, and 127 % for citizen scientists,
respectively. Based on these results, we selected salt dilution as the
preferred method. Finally, we performed larger-scale pilot testing in
week-long pre- and post-monsoon Citizen Science Flow campaigns involving 25
and 37 citizen scientists, respectively. Observed flows (n=131
pre-monsoon; n=133 post-monsoon) were distributed among the 10 headwater
catchments of the Kathmandu Valley and ranged from 0.4 to 425 L s−1
and from 1.1 to 1804 L s−1 in pre- and post-monsoon, respectively.
Future work should further evaluate uncertainties of citizen science salt
dilution measurements, the feasibility of their application to larger
regions, and the information content of additional streamflow data.