Abstract

Abstract. Even in relatively wet tropical regions, seasonal fluctuations in the water cycle affect the consistent and reliable supply of water for urban, industrial, and agricultural uses. Historic streamflow monitoring datasets are crucial in assessing our ability to model and subsequently plan for future hydrologic changes. In this technical note, we evaluate a new observation-based global product of monthly runoff (GRUN; Ghiggi et al., 2019) for 55 small tropical catchments in the Philippines with at least 10 years of data, extending back to 1946 in some cases. Since GRUN did not use discharge data from the Philippines to train or calibrate their models, the data presented in this study, 11 915 monthly data points, provide an independent evaluation of this product. We demonstrate across all observations a significant but weak correlation (r2=0.372) between the GRUN-predicted values and observed river discharge, as well as somewhat skillful prediction (volumetric efficiency = 0.363 and log(Nash–Sutcliffe efficiency) = 0.453). GRUN performs best among catchments located in climate types III (no pronounced maximum rainfall with short dry season) and IV (evenly distributed rainfall, no dry season). There was a weak negative correlation between volumetric efficiency and catchment area, and there was a positive correlation between volumetric efficiency and mean observed runoff. Further, analysis for individual rivers demonstrates systematic biases (over- and underestimation) of baseflow during the dry season and underprediction of peak flow during some wet months for most catchments. To correct for underprediction during wet months, we applied a log-transform bias correction which greatly improves the nationwide root mean square error between GRUN and the observations by an order of magnitude (2.648 mm d−1 vs. 0.292 mm d−1). This technical note demonstrates the importance of performing such corrections when determining the proportional contribution of smaller catchments or tropical islands such as the Philippines to global tabulations of discharge. These results also demonstrate the potential use of GRUN and future data products of this nature after consideration and correction of systematic biases to (1) assess trends in regional-scale runoff over the past century, (2) validate hydrologic models for unmonitored catchments in the Philippines, and (3) assess the impact of hydrometeorological phenomena to seasonal water supply in this wet but drought-prone archipelago.

Highlights

  • The global water crisis affects an estimated two-thirds of the world’s population and is considered one of the three biggest global issues that we need to contend with (Kummu et al, 2016; WEF, 2018)

  • Global Runoff Reconstruction (GRUN) was not intended to be used for estimating discharge for single small catchments; we focus on the aggregated data and report the range for the result for the individual catchments

  • The results indicate a somewhat skillful prediction for monthly runoff (volumetric efficiency = 0.363 and log(Nash–Sutcliffe efficiency) = 0.453) when all data are pooled

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Summary

Introduction

The global water crisis affects an estimated two-thirds of the world’s population and is considered one of the three biggest global issues that we need to contend with (Kummu et al, 2016; WEF, 2018). The Philippines offers a unique example where manual stream-gauging programs have started in 1904 and, while spotty at times, have continued to today This island nation on the western side of the Pacific Ocean is characterized by a very dynamic hydrologic system because it is affected by tropical cyclones, seasonal monsoon rains, subdecadal cycles such as the El Niño– Southern Oscillation (ENSO) and climate change (Abon et al, 2016; David et al, 2017; Kumar et al, 2018). The impact of climate change on the hydrological cycle can be observed the most for tropical island nations, including the Philippines (Nurse et al, 2014) This technical note evaluates the accuracy of the GRUN dataset (GRUN_v1) as applied to the hydrodynamically active smaller river basins in the Philippines. It explores the possible hydrologic parameters that may need to be considered and/or optimized so that such global datasets can predict runoff in smaller, ungauged basins more accurately

Climate types
Historical streamflow data
Catchment area and pairing with GRUN grid cells
Comparison of GRUN estimates and observations
Results and discussion
Comparison of runoff distributions
Correlation and trends with watershed characteristics
Bias correction and outlook
Conclusion
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