Arid
DOI10.1002/agj2.20325
Spatio-temporal calibration of Hargreaves-Samani model to estimate reference evapotranspiration across US High Plains
Kukal, M. S.; Irmak, S.; Walia, H.; Odhiambo, L.
通讯作者Irmak, S (corresponding author), Univ Nebraska, 239 LW Chase Hall, Lincoln, NE 68583 USA.
来源期刊AGRONOMY JOURNAL
ISSN0002-1962
EISSN1435-0645
出版年2020
卷号112期号:5页码:4232-4248
英文摘要Temperature-based grass-reference evapotranspiration (ETo) estimation methods (e.g., Hargreaves-Samani [HS] model) present advantages over combination-based methods that require full-suite weather data. The U.S. High Plains region has scarce and short-term full-suite weather sites. This data scarcity presents challenges for combination-based ETo estimation. The performance of HS model against the American Society of Civil Engineers (ASCE) standardized Penman-Monteith (PM) model was assessed using long-term data at 124 full-suite weather sites across nine states in the U.S. High Plains. The HS model underestimated ETo at arid (mean bias error [MBE] = -1.68 mm d(-1)), semi-arid (MBE = -0.34 mm d(-1)), and dry subhumid sites (MBE = -0.16 mm d(-1)) and overestimated ETo at humid sites (MBE = 0.14 mm d(-1)). There was a significant relationship (p < .01) between HS model performance and aridity index. The HS model performed better (27% lower root mean squared difference [RMSD]) in summer months than the rest of the year at semi-arid and dry subhumid sites. The model performance was non-ideal during the summer months in subhumid climates. Spatio-temporal annual zonal (climate division), monthly zonal, annual site-specific, and monthly site-specific calibration resulted in 12, 16, 20, and 26% reduction in RMSD and 11, 16, 17, and 23% reduction in relative error, respectively. Monthly site-specific calibration performed the best and was used to quantify annual and growing season ETo across the region. The research characterized performance patterns of the HS model over an important agroecosystem-dominated region. Practical data-driven strategies were proposed to better estimate PM ETo using limited weather data at any given site (with similar aridity) and time of the year.
类型Article
语种英语
收录类别SCI-E
WOS记录号WOS:000600983000082
WOS关键词GRASS-REFERENCE EVAPOTRANSPIRATION ; DAILY TEMPERATURE-RANGE ; LIMITED WEATHER DATA ; LONG-TERM PATTERNS ; GREAT-PLAINS ; POTENTIAL EVAPOTRANSPIRATION ; AIR TEMPERATURES ; ARIDITY INDEX ; EQUATION ; PRECIPITATION
WOS类目Agronomy
WOS研究方向Agriculture
资源类型期刊论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/369155
作者单位[Kukal, M. S.; Irmak, S.; Walia, H.; Odhiambo, L.] Univ Nebraska, 239 LW Chase Hall, Lincoln, NE 68583 USA
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Kukal, M. S.,Irmak, S.,Walia, H.,et al. Spatio-temporal calibration of Hargreaves-Samani model to estimate reference evapotranspiration across US High Plains[J],2020,112(5):4232-4248.
APA Kukal, M. S.,Irmak, S.,Walia, H.,&Odhiambo, L..(2020).Spatio-temporal calibration of Hargreaves-Samani model to estimate reference evapotranspiration across US High Plains.AGRONOMY JOURNAL,112(5),4232-4248.
MLA Kukal, M. S.,et al."Spatio-temporal calibration of Hargreaves-Samani model to estimate reference evapotranspiration across US High Plains".AGRONOMY JOURNAL 112.5(2020):4232-4248.
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