LONG–TERM PRECIPITATION ANALYSES FOR THE CENTRAL TEXAS BLACKLAND PRAIRIE

Continuous records of intensively monitored precipitation data are rare, but where available they provide valuable regional information on hydrologic structure design and on other water supply and water quality management and modeling issues. One such long–term precipitation record exists for the Texas Blackland Prairie region. Beginning in 1937 and continuing to the present, hydrologic data have been collected at the USDA–ARS Grassland Soil and Water Research Laboratory watershed facility near Riesel, Texas. The objectives of this article are to present long–term analyses and to publicize the availability of that precipitation database. Long–term analyses included examination of general precipitation properties, depth–duration–frequency relationships, and trends in rainfall amount and occurrence. Annual rainfall for the region averages about 890 mm, with relatively wet springs and falls and drier summer and winter months. Depth–duration–frequency results emphasize the need for engineers to use the most current and extensive data sets and/or proven relationships in the design of hydrologic structures. Several significant temporal trends that can affect water resource management were also determined. These trends include increases in October rainfall, non–spring rainfall, and the number of summer, fall, and annual rainy days. These increases, however, are offset to some degree by decreases in April rainfall, in the number of extreme events in the spring, and in the magnitude of extreme fall rain events.

[1]  C. W. Richardson,et al.  Effects of Conservation Practices on Storm Runoff in the Texas Blackland Prairie , 1969 .

[2]  David M. Hershfield,et al.  Rainfall frequency atlas of the United States for durations from 30 minutes to 24 hours and return periods from 1 to 100 years , 1961 .

[3]  E. A. Hiler,et al.  Prediction of Sediment Yields from Small Watersheds , 1971 .

[4]  Leo R Beard,et al.  Statistical Methods in Hydrology , 1962 .

[5]  C. W. Richardson,et al.  Simulation of Sediment and Nitrate Loss on a Vertisol with Conservation Tillage Practices , 1996 .

[6]  Thomas R. Karl,et al.  Secular Trends of Precipitation Amount, Frequency, and Intensity in the United States , 1998 .

[7]  V. Yevjevich Probability and statistics in hydrology , 1972 .

[8]  Indrajeet Chaubey,et al.  QUANTIFYING MODEL OUTPUT UNCERTAINTY DUE TO SPATIAL VARIABILITY OF RAINFALL 1 , 1999 .

[9]  C. W. Richardson,et al.  Losses of Nitrogen in Surface Runoff in the Blackland Prairie of Texas , 1976 .

[10]  Jeffrey G. Arnold,et al.  Validation of SWRRB—Simulator for Water Resources in Rural Basins , 1987 .

[11]  W. Asquith Depth-duration frequency of precipitation for Texas , 1998 .

[12]  C. W. Richardson,et al.  Erosion and Nutrient Losses From Zero Tillage on a Clay Soil , 1995 .

[13]  Kenneth G. Renard,et al.  PRECIPITATION CHANGES FROM 1956 TO 1996 ON THE WALNUT GULCH EXPERIMENTAL WATERSHED 1 , 2002 .

[14]  David C. Robertson,et al.  Long‐Term Snow Database, Reynolds Creek Experimental Watershed, Idaho, United States , 2001 .

[15]  D. Favis-Mortlock,et al.  The use of synthetic weather for soil erosion modelling. , 1995 .

[16]  D. Wilks Interannual variability and extreme-value characteristics of several stochastic daily precipitation models , 1999 .

[17]  Thomas R. Karl,et al.  Heavy Precipitation and High Streamflow in the Contiguous United States: Trends in the Twentieth Century. , 2001 .

[18]  C. W. Richardson,et al.  HYDROLOGIC RESPONSE OF A SMALL WATERSHED MODEL TO GENERATED PRECIPITATION , 2000 .