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284<br />

The models generally show a warm bias in summer for this<br />

region but lower bias in winter. By contrast, precipitation<br />

amounts simulated for winter are higher than observations,<br />

and the annual maximum generally occurs about one month<br />

earlier than is observed. The spring-to-summer decrease in<br />

precipitation is more abrupt in the models than in<br />

observations.<br />

The delayed peak in seasonal precipitation in the models<br />

leads to a delayed seasonal peak in streamflow as well, as<br />

shown in Fig. 1c. The range of results for streamflow is<br />

larger than the range in either temperature or precipitation.<br />

For instance if a model is both too warm and too dry it has<br />

two factors leading to a low simulations of streamflow.<br />

All regional models capture two major features of the<br />

interannual variability that occurred during the period of<br />

1980-2004. The major flood of 1993 was the dominant<br />

hydrological feature of this region over the period simulated.<br />

Individual models have systematic biases over the entire<br />

simulated record, but all capture the flood of 1993, albeit<br />

with reduced or amplified (depending on bias) difference<br />

from the long term mean. All models also capture the<br />

weaker extreme dry period of 2000, although with less<br />

distinctiveness than the flood year. Small interannual<br />

variations are simulated differently by individual models,<br />

with some showing much less variability, particularly in the<br />

first half of the record.<br />

5. Future Results<br />

SWAT simulations with results of additional NARCCAP<br />

models are in progress and will be reported at the workshop.<br />

6. Acknowledgement<br />

We acknowledge the North American Regional Climate<br />

Change Assessment Program (NARCCAP) including the<br />

climate modeling groups and the NCAR/LLNL archiving<br />

teams (http://www.narccap.ucar.edu/about/participants.html)<br />

for providing the data used in this publication. NARCCAP is<br />

funded by the US National Science Foundation, US<br />

Department of Energy, the National Oceanic and<br />

Atmospheric Administration (NOAA) and the U. S.<br />

Environmental Protection Agency Office of Research and<br />

Development. Partial support for this work was provided by<br />

USDA National Research Initiative Grant<br />

#20063561516724.<br />

References<br />

NARCCAP, 2009: North American Regional Climate<br />

Change Assessment Program. [Available online at<br />

http://www.narccap.ucar.edu ]<br />

Neitsch, S.L., J.G. Arnold, J.R. Kiniry, R. Srinivasan, and<br />

J.R. Williams (2002), Soil and Water Assessment<br />

Tool: User Manual, Version 2000, Texas Water<br />

Resour. Inst. TR-192, GSWRL 02-02, BRC 02-06.<br />

455 pp.

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