Development of an Ensemble Gridded Hydrometeorological Forcing Dataset over the Contiguous United States

Friday, 19 December 2014: 11:20 AM
Andrew James Newman1, Martyn P Clark1, Jason Craig1, Bart Nijssen2, Andrew W Wood1, Ethan D Gutmann1, Naoki Mizukami1, Levi D Brekke3 and J R Arnold4, (1)National Center for Atmospheric Research, Boulder, CO, United States, (2)University of Washington, Department of Civil and Environmental Engineering, Seattle, WA, United States, (3)U.S. Bureau of Reclamation, Denver, CO, United States, (4)U.S. Army Engineer Institute for Water Resources, Univ. of Washington, Seattle, WA, United States
Gridded hydrometeorological forcing datasets are inherently uncertain due to myriad factors. These include interpolation from a sparse observation network, measurement representativeness, and measurement errors. Generally, uncertainty estimates are not included in gridded products; or if present, they may be included in an ad-hoc manner. A lack of quantitative uncertainty estimates for hydrometeorological forcing fields limits their utility to support land surface and hydrologic modeling techniques such as data assimilation, probabilistic forecasting and verification.

We present a first of its kind, gridded, observation-based ensemble of precipitation and temperature at a daily increment for the period 1980-2012. Statistical verification of the ensemble indicates that it provides generally good reliability and discrimination of events of various magnitudes, but has a small dry bias for high probability events. The ensemble mean is similar to another widely used hydrometeorological forcing dataset (Maurer et al. 2002) but with some important differences. The ensemble product is able to produce an improved probability-of-precipitation field, which impacts the empirical derivation of other fields used in land-surface and hydrologic modeling. Elevation lapse rates for temperature are derived directly from the observations, rather than specified a priori, resulting in different temperatures at higher elevations in the intermountain western US. Daily maximum, minimum temperature and precipitation accumulation uncertainty can be estimated through the use of the ensemble variance. These types of datasets will help improve data assimilation and probabilistic forecast components of land-surface and hydrological modeling systems and provide a quantitative estimate of observation uncertainty for use in NWP forecast verification. Finally, the software is extensible with future plans to incorporate remote sensing data (i.e. ground based precipitation radar, GPM, passive microwave) and NWP output depending on the application.