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Connections between the hydrological cycle and crop yield in the rainfed U.S. Corn Belt

机译:美国雨养玉米带水文循环与作物产量之间的联系

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Water stress is one of the major abiotic stresses and directly affects crop growth and influences crop yields. To better quantify the responses of crop yield to hydrological variability in the rainfed Corn Belt of the United States (U.S.), we analyzed the relationships between corn/soybean yield and hydrological cycle metrics, as well as their spatio-temporal dynamic at the agricultural district and interannual scale between 2003 and 2014. We used Partial Least Square Regression (PLSR) to optimally integrate different hydrological metrics and drought indices to define a crop-specific new drought index that uses crop yield as the target, and investigated the contributions of those hydrological cycle components to the new drought index. We used both observed and modeled hydrological cycle metrics, as well as several drought indices in this study, including evapotranspiration (ET) and potential ET (PET), terrestrial water storage change (ΔS), surface soil moisture (SSM), river discharge (Q),Standardized Precipitation-Evapotranspiration Index (SPEI), Palmer Drought Severity Index (PDSI), fET (the ratio of ET to PET), and vapor pressure deficit (VPD). Our results revealed that: (1) VPD, SSM, and fET showed the strongest correlations with crop yield, among the observation-based hydrological cycle metrics and drought indices considered here. Most of the hydrological cycle metrics and drought indices showed similar seasonal correlation patterns with crop yield, and this pattern revealed that the sensitivity of crop growth to water stress peaked in July for corn and in August for soybean in the rainfed U.S. Corn Belt. (2) The drought in 2012 started with higher water demand (reflected in abnormally high ET, PET, and VPD) and lower water supply (reflected in abnormally low P), followed by soil water depletion (as revealed in SSM and ΔS), leading to massive crop yield losses due to increased constraints on both water supply and demand. (3) The R~2 of the PLSR-based crop yiel
机译:水分胁迫是主要的非生物胁迫之一,直接影响作物生长并影响作物产量。为了更好地量化美国雨养玉米带作物产量对水文变化的响应,我们分析了2003—2014年玉米/大豆产量与水文循环指标之间的关系,以及它们在农业区和年际尺度上的时空动态。我们采用偏最小二乘回归(PLSR)对不同的水文指标和干旱指数进行优化整合,以定义以作物产量为目标的作物特异性新干旱指数,并研究了这些水文循环成分对新干旱指数的贡献。本研究使用了观测和模拟的水文循环指标,以及几个干旱指数,包括蒸散量(ET)和潜在ET(PET)、陆地储水量变化(ΔS)、表层土壤湿度(SSM)、河流流量(Q)、标准化降水-蒸散指数(SPEI)、帕尔默干旱严重程度指数(PDSI)、fET(ET与PET的比值)和蒸气压赤字(VPD)。结果表明:(1)在基于观测的水文循环指标和干旱指数中,VPD、SSM和fET与作物产量的相关性最强。大多数水文循环指标和干旱指数与作物产量显示出相似的季节性相关性模式,这种模式表明,作物生长对水分胁迫的敏感性在7月达到顶峰,在8月达到顶峰,在雨养的美国玉米带中,大豆在8月达到顶峰。(2)2012年的干旱始于较高的需水量(反映在异常高的ET、PET和VPD)和较低的供水量(反映在异常低的磷)上,随后是土壤水分枯竭(如SSM和ΔS所示),由于水资源供应和需求的制约增加,导致大量作物产量损失。(3)基于PLSR的作物的R~2

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