No synthesized global gridded runoff product,
derived from multiple sources, is available, despite such a
product being useful for meeting the needs of many global
water initiatives. We apply an optimal weighting approach
to merge runoff estimates from hydrological models con-
strained with observational streamflow records. The weight-
ing method is based on the ability of the models to match
observed streamflow data while accounting for error co-
variance between the participating products. To address the
lack of observed streamflow for many regions, a dissimilar-
ity method was applied to transfer the weights of the par-
ticipating products to the ungauged basins from the closest
gauged basins using dissimilarity between basins in physio-
graphic and climatic characteristics as a proxy for distance.
We perform out-of-sample tests to examine the success of
the dissimilarity approach, and we confirm that the weighted
product performs better than its 11 constituent products in
a range of metrics. Our resulting synthesized global grid-
ded runoff product is available at monthly timescales, and
includes time-variant uncertainty, for the period 1980–2012
on a 0.5◦ grid. The synthesized global gridded runoff prod-
uct broadly agrees with published runoff estimates at many
river basins, and represents the seasonal runoff cycle for
most of the globe well. The new product, called Linear Op-
timal Runoff Aggregate (LORA), is a valuable synthesis
of existing runoff products and will be freely available for
download on https://geonetwork.nci.org.au/geonetwork/srv/eng/catalog.search#/metadata/f9617_9854_8096_5291
Key Figure
Figure 10. Mean seasonal runoff calculated for the period 1980–2012.
This page is maintained by Jason Evans |
Last updated 23 January 2018