R. Sutherland, TEACHING THE HYDROLOGIC AND GEOMORPHIC SIGNIFICANCE OF DRAINAGE BASINS AND DISCHARGE IN PHYSICAL-GEOGRAPHY, Journal of geography, 93(2), 1994, pp. 80-95
Drainage basins, stream discharge, and sediment discharge are fundamen
tal concepts in physical geography, and they play an integral part in
other cognate disciplines. To enhance student understanding of water a
nd sediment discharge there needs to be an integration of field-based
monitoring exercises with classroom exercises using readily available
(published) discharge data from water resource agencies. This paper ou
tlines two groups of exercises. The first set of exercises involves a
combination of field-based monitoring and associated laboratory analys
is, and they include the following worked examples for Manoa Stream, O
ahu, Hawai'i: 1) discharge measurement using the velocity-area techniq
ue, 2) measurement of suspended sediment concentration, and computatio
n of suspended sediment load, yield and erosion rates for a drainage b
asin, and 3) determination of channel hydraulic parameters. The second
set of exercises was developed for students who are not able to condu
ct field monitoring. These may also be used by students who have compl
eted field discharge monitoring. These exercises focus on readily avai
lable daily discharge data for several drainage basins in Hawai'i, and
worked examples include: 1) developing annual stream discharge hydrog
raphs for drainage basins of different size, 2) comparing river regime
s of local systems to global models, and 3) developing flow-duration c
urves for different drainage basins. Utilization of real-world dischar
ge data allows students the opportunity to explore relationships and t
o grasp the underlying controls on discharge variation from drainage b
asins. These are important aspects in developing an understanding of w
ater and sediment linkages within environmental systems.