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Sassenrath, G.F., Schmidt, A.M., Schneider, J.M., Tagert, M.L., Corbitt, J.Q., van Riessen, H., Crumpton, J., Rice, B., Thornton, R., Prabhu, R., Pote, J. and Wax, C. (2013) Development of the Mississippi irrigation scheduling tool —MIST. ASABE Annual International Meeting, Kansas City, 21-23 July 2013, Paper No. 131619807

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• TITLE: Testing gridded NWS 1-day observed precipitation analysis in a daily irrigation scheduler

  AUTHORS: Gretchen F. Sassenrath, J. M. Schneider, A. M. Schmidt, J. Q. Corbitt, J. M. Halloran, R. Prabhu

  KEYWORDS: Irrigation; Daily; Precipitation; Scheduler; Gridded; Radar

  JOURNAL NAME: Agricultural Sciences, Vol.4 No.12, December 5, 2013

  ABSTRACT: One of the inputs required by daily decision support tools for scheduling irrigation is the amount of water supplied by rainfall. In-field measurements of daily precipitation are expensive or laborious, while measurements from gauges within a few kilometers are frequently not representative due to the high spatiotemporal variability of precipitation. Online radarbased precipitation analyses from NOAA’s National Weather Service (NWS) have obvious potential to provide the needed data, but are known to have varying degrees of accuracy with location and conditions. The NWS precipitation analysis is computed on a 4 km × 4 km grid, so differences should also be expected between the product and individual gauge measurements under each grid cell. In order to test the utility of the NWS precipitation analysis in a daily irrigation scheduler, daily data were gathered in July 2012 from 18 weather stations under 2 NWS precapitation analysis grid cells across instru-mented research and production fields in the Mississippi Delta. Differences between individual station measurements and the NWS precipitation analysis are examined, and root-zone daily soil water deficits computed using both station data and the NWS precipitation analysis. Sub-grid spatial variability between gauge locations, and differences in precipitation between gauges and the gridded NWS analysis, are found to be similar to those reported elsewhere. Differences between time series of soil water deficit computed using the two different precipitation data sources are noted, but prove to be of limited impact on the decision to irrigate or not to irrigate. It is also noted that profile-filling rainfalls limit the impact of accumulating error, resetting the modeled soil water to “full”. Given the Delta-local practice of irrigating to replace full evapotranspirational water used, use of the NWS daily precipitation analysis data as input for a daily irrigation scheduler is judged not only acceptable, but also preferable to other sources of daily precipitation data.