1. Multimodel Ensemble Reconstruction of Drought over the Continental U.S
Aihui Wang1, Dennis P. Lettenmaier1,
Sarith Mahanama2, and Randal D. Koster2
for presentation at
Climate Diagnostics and Prediction Workshop
Tallahassee, FL
October
1Department of Civil and Environmental Engineering,
University of Washington, Seattle, WA 98195
2NASA Goddard Space Flight Center, Greenbelt MD 20771

2. Outline
Motivation
Models
Methodology
Results
Summary

3. Motivation
Widely used, but link to direct observations (e.g., of soil moisture) is weak – hence reliance on indirect methods, such as PDSI.
Need for reproducible basis for identifying drought-affected regions.
Land surface model representations of soil moisture (and runoff) offer an alternative means for estimating severity, frequency, duration, and variability of current droughts, and linking them to the climatology of observed droughts.

4. Models VIC: Variable Infiltration Capacity Model
(Liang et al. 1994)
CLM3.5: Community Land Model version 3.5
(Oleson et al. 2007)
NOAH LSM: NCEP, OSU, Air Force, Hydrol. research lab
(Mitchell et al. 1994, Chen and Mitchell 1996)
Catchment LSM: NASA Seasonal-to-Interannual Prediction Project (NSIPP) LSM
(Koster et al. 2000; Ducharne et al. 2000)

5. Model Schematic

6. Data
Daily precipitation and temperature max-min, other land surface variables (downward solar and longwave radiation, near-surface humidity, and wind) derived via index methods. Methods as described in Maurer et al. (2002). Data duration is from , and period of analysis is Spatial resolution 0.5  (3322 land grid cells), domain conterminous United States.
Soil and vegetation parameters are from different sources for different models (generally NLDAS), as provided by model developers. Other parameters are model standard setup.

7. The challenge: Different land schemes have different soil moisture dynamics
Model simulated
soil moisture at cell
(40.25N, W)

8. Solution: Normalized total column soil moisture
For each model, total column soil moisture was expressed as percentiles (hence by construct, uniformly distributed from zero to one).
Percentiles were estimated for each model by month, using simulated total column soil moisture for the period
Percentiles were computed using the Weibull plotting position formula.

9. Ensemble methods Two ensemble methods were used:
Ensemble-1: averaged 4 modeled soil moisture percentiles of each grid cell on monthly scale.
Ensemble –2: first, normalized column total soil moisture
modeled by 4 models individually; second, averaged those normalized soil moisture of each grid cell in 4 models; third, calculated percentiles of those averaged values .

10. Areas for spatially averaged soil moisture percentilesNW NE SW SE
Box sizes are 5 x 5 degrees

11. NW

12. NE

13. SW

14. SE

15. Multimodel comparison –soil moisture as percentiles
July 1934
VIC
CLM3.5
NOAH
Catchment
Ensemble-2
Ensemble-1

16. November 1952
VIC
CLM3.5
NOAH
Catchment
Ensemble-1
Ensemble-2

17. October 1963
CLM3.5
VIC
NOAH
Catchment
Ensemble-1
Ensemble-2

18. February 1977
CLM3.5
VIC
NOAH
Catchment
Ensemble-1
Ensemble-2

19. June 1988
CLM3.5
VIC
NOAH
Catchment
Ensemble-2
Ensemble-1

20. June 2002
CLM3.5
VIC
NOAH
Catchment
Ensemble-2
Ensemble-1

21. Severity-area-duration for the 1930s drought(s)

22. Conclusions
Current drought products suffer from the absence of reproducible, objective methods for identifying drought extent and severity.
Although widely used, PDSI has well-known shortcomings, especially the absence of a strong link to physical processes
Land surface parameterizations, such as the family of NLDAS models, avoid these shortcomings. However, soil moisture, a key drought-related variable, is model-dependent
Multi-model estimates of soil moisture, appropriately normalized, address all of the above shortcomings. When forced with common observations, major drought events appear to be plausibly reproduced by the individual models, and two methods of combining results into a multi-model ensemble.