TY - JOUR
T1 - A case study of field-scale maize irrigation patterns in western Nebraska
T2 - Implications for water managers and recommendations for hyper-resolution land surface modeling
AU - Gibson, Justin
AU - Franz, Trenton E.
AU - Wang, Tiejun
AU - Gates, John
AU - Grassini, Patricio
AU - Yang, Haishun
AU - Eisenhauer, Dean
N1 - Publisher Copyright:
© Author(s) 2017.
PY - 2017/2/20
Y1 - 2017/2/20
N2 - In many agricultural regions, the human use of water for irrigation is often ignored or poorly represented in land surface models (LSMs) and operational forecasts. Because irrigation increases soil moisture, feedback on the surface energy balance, rainfall recycling, and atmospheric dynamics is not represented and may lead to reduced model skill. In this work, we describe four plausible and relatively simple irrigation routines that can be coupled to the next generation of hyper-resolution LSMs operating at scales of 1 km or less. The irrigation output from the four routines (crop model, precipitation delayed, evapotranspiration replacement, and vadose zone model) is compared against a historical field-scale irrigation database (2008-2014) from a 35 km2 study area under maize production and center pivot irrigation in western Nebraska (USA). We find that the most yield-conservative irrigation routine (crop model) produces seasonal totals of irrigation that compare well against the observed irrigation amounts across a range of wet and dry years but with a low bias of 80 mm yrg-1. The most aggressive irrigation saving routine (vadose zone model) indicates a potential irrigation savings of 120 mm yrg-1 and yield losses of less than 3 % against the crop model benchmark and historical averages. The results of the various irrigation routines and associated yield penalties will be valuable for future consideration by local water managers to be informed about the potential value of irrigation saving technologies and irrigation practices. Moreover, the routines offer the hyper-resolution LSM community a range of irrigation routines to better constrain irrigation decision-making at critical temporal (daily) and spatial scales (<-1 km).
AB - In many agricultural regions, the human use of water for irrigation is often ignored or poorly represented in land surface models (LSMs) and operational forecasts. Because irrigation increases soil moisture, feedback on the surface energy balance, rainfall recycling, and atmospheric dynamics is not represented and may lead to reduced model skill. In this work, we describe four plausible and relatively simple irrigation routines that can be coupled to the next generation of hyper-resolution LSMs operating at scales of 1 km or less. The irrigation output from the four routines (crop model, precipitation delayed, evapotranspiration replacement, and vadose zone model) is compared against a historical field-scale irrigation database (2008-2014) from a 35 km2 study area under maize production and center pivot irrigation in western Nebraska (USA). We find that the most yield-conservative irrigation routine (crop model) produces seasonal totals of irrigation that compare well against the observed irrigation amounts across a range of wet and dry years but with a low bias of 80 mm yrg-1. The most aggressive irrigation saving routine (vadose zone model) indicates a potential irrigation savings of 120 mm yrg-1 and yield losses of less than 3 % against the crop model benchmark and historical averages. The results of the various irrigation routines and associated yield penalties will be valuable for future consideration by local water managers to be informed about the potential value of irrigation saving technologies and irrigation practices. Moreover, the routines offer the hyper-resolution LSM community a range of irrigation routines to better constrain irrigation decision-making at critical temporal (daily) and spatial scales (<-1 km).
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U2 - 10.5194/hess-21-1051-2017
DO - 10.5194/hess-21-1051-2017
M3 - Article
AN - SCOPUS:85013231685
SN - 1027-5606
VL - 21
SP - 1051
EP - 1062
JO - Hydrology and Earth System Sciences
JF - Hydrology and Earth System Sciences
IS - 2
ER -