CN111833202A - A short-term forecasting method of farmland evapotranspiration considering dynamic changes of crop coefficients and rainfall - Google Patents

A short-term forecasting method of farmland evapotranspiration considering dynamic changes of crop coefficients and rainfall Download PDF

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CN111833202A
CN111833202A CN202010674470.1A CN202010674470A CN111833202A CN 111833202 A CN111833202 A CN 111833202A CN 202010674470 A CN202010674470 A CN 202010674470A CN 111833202 A CN111833202 A CN 111833202A
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张宝忠
韩信
魏征
李益农
杜太生
陈鹤
韩聪颖
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Abstract

本发明公开了一种考虑作物系数动态变化与降雨的农田蒸散量短期预测方法,该方法包括获取农田作物生长环境的气象数据;根据预测基准日的参考作物蒸散量和农田实测蒸散量计算预测基准日的作物系数;分别构建训练集和测试集,并进行预处理;建立考虑作物系数动态变化和降雨影响的前馈神经网络模型,并进行训练优化;利用优化后的前馈神经网络模型根据测试集数据短期预测农田作物蒸散量。本发明考虑了作物系数变化与降雨对农田作物蒸散量的影响,有效构建了农田参考作物蒸散量与其驱动因素之间的非线性关系,据此可以得到更符合作物实际生长状况的作物蒸散量,为农田下垫面的未来水分管理提供科学依据。

Figure 202010674470

The invention discloses a short-term forecasting method for farmland evapotranspiration considering dynamic changes of crop coefficients and rainfall. The method includes obtaining meteorological data of the growing environment of farmland crops; calculating a forecasting benchmark according to the reference crop evapotranspiration on the forecasting base day and the measured farmland evapotranspiration. daily crop coefficients; build training sets and test sets respectively, and perform preprocessing; establish a feedforward neural network model considering the dynamic changes of crop coefficients and the influence of rainfall, and perform training optimization; use the optimized feedforward neural network model to test Set data for short-term prediction of crop evapotranspiration. The present invention takes into account the influence of crop coefficient changes and rainfall on crop evapotranspiration, and effectively constructs a nonlinear relationship between the reference crop evapotranspiration and its driving factors, and accordingly, the crop evapotranspiration that is more in line with the actual growth conditions of crops can be obtained. Provide scientific basis for future water management of farmland underlying surface.

Figure 202010674470

Description

考虑作物系数动态变化与降雨的农田蒸散量短期预测方法A short-term forecasting method of farmland evapotranspiration considering dynamic changes of crop coefficients and rainfall

技术领域technical field

本发明属于作物蒸腾预测技术领域,具体涉及一种考虑作物系数动态变化与降雨的农田蒸散量短期预测方法。The invention belongs to the technical field of crop transpiration prediction, and in particular relates to a short-term prediction method for farmland evapotranspiration considering the dynamic change of crop coefficients and rainfall.

背景技术Background technique

蒸散过程是陆地水文循环的重要组成部分,蒸散量(Evapotranspiration,ETc)对于灌溉计划以及区域水资源分配具有重要的指导意义。蒸散量的准确预测可在一定程度上节约灌溉用水量,因此为了更好地管理作物灌溉用水量以及提高作物水分利用效率,亟待对作物蒸散量进行准确预测。Evapotranspiration is an important part of the terrestrial hydrological cycle, and evapotranspiration (ET c ) has important guiding significance for irrigation planning and regional water resources allocation. Accurate prediction of evapotranspiration can save irrigation water to a certain extent. Therefore, in order to better manage crop irrigation water consumption and improve crop water use efficiency, it is urgent to accurately predict crop evapotranspiration.

目前,蒸散量的预测方法主要分为4类:时间序列法、灰色模型法、经验公式法和神经网络模型法等。时间序列法由于其所用数据单一(只采用蒸散量的历史数据),而未能充分考虑其他因素影响下的超历史变化,所以预测精度存在不确定性。灰色预测方法实质是一个指数模型,当目标函数发生零增长时,系统误差严重,而且预测周期越多,误差越严重。经验公式法需要针对不同研究区进行参数修正,并且需要的气象资料多,计算较为复杂。人工神经网络是近几年发展起来的非线性理论,不需要了解非线性系统内部具体结构条件,具有自组织、自适应及自学习的功能,非常适合用来模拟、处理影响因素多、关系复杂的系统,为高度非线性动态关系的时间序列预测和评判提供了一条有效途径。蒸散量与其驱动因素之间存在复杂的非线性关系,针对常规耗水预测模型在预测中存在的盲目性大,拟合精度不高且预测容易失真的不足,引入神经网络的计算方法,建立非线性人工神经网络的预测模型,能够考虑众多因素对蒸散量的影响,所建立的预测模型预测精度高,简便易行,具有良好的应用推广价值。At present, the prediction methods of evapotranspiration are mainly divided into four categories: time series method, grey model method, empirical formula method and neural network model method. Due to the single data used by the time series method (only the historical data of evapotranspiration is used), the ultra-historical changes under the influence of other factors cannot be fully considered, so there is uncertainty in the prediction accuracy. The grey forecasting method is essentially an exponential model. When the objective function has zero growth, the systematic error is serious, and the more the forecast period is, the more serious the error is. The empirical formula method requires parameter correction for different study areas, and requires a lot of meteorological data, making the calculation more complicated. Artificial neural network is a nonlinear theory developed in recent years. It does not need to understand the specific structural conditions of the nonlinear system. It has the functions of self-organization, self-adaptation and self-learning. It is very suitable for simulating and processing many influencing factors and complex relationships. The system provides an effective way for the prediction and evaluation of time series with highly nonlinear dynamic relationship. There is a complex nonlinear relationship between evapotranspiration and its driving factors. In view of the large blindness in the prediction of the conventional water consumption prediction model, the low fitting accuracy and the easy distortion of the prediction, the neural network calculation method is introduced to establish a non-linear model. The prediction model of linear artificial neural network can consider the influence of many factors on evapotranspiration. The established prediction model has high prediction accuracy, is simple and easy to implement, and has good application and promotion value.

目前采用BP神经网络模型预测蒸散量主要是将常规变量进行训练和测试,且多采用FAO推荐的作物系数,或者采用历史实测作物系数进行蒸散量预测。但是随着作物本身与外界条件的不同,作物系数也在不断变化,且具有明显的地域和时序差别。研究表明,基于FAO推荐的作物系数值,适用于时间步长较大的过程计算,但不能反映作物逐日动态变化情况,在进行蒸散量预测时,预测值与实测值存在稍大偏差。因此,对于作物系数的获取需要考虑作物生长阶段对其动态变化的影响。此外,降雨作为蒸散量预测精度的重要影响因素,目前还没有学者直接将降雨考虑到蒸散量的预测中。At present, the BP neural network model is used to predict evapotranspiration mainly by training and testing conventional variables, and most of the crop coefficients recommended by FAO are used, or the historical measured crop coefficients are used to predict evapotranspiration. However, with the difference between the crop itself and the external conditions, the crop coefficient is also constantly changing, and there are obvious regional and time series differences. Studies have shown that the crop coefficient values recommended by FAO are suitable for process calculations with large time steps, but cannot reflect the daily dynamic changes of crops. When predicting evapotranspiration, there is a slight deviation between the predicted value and the measured value. Therefore, for the acquisition of crop coefficients, it is necessary to consider the influence of crop growth stages on its dynamic changes. In addition, rainfall is an important factor affecting the prediction accuracy of evapotranspiration. At present, no scholars have directly considered rainfall into the prediction of evapotranspiration.

综上所述,进行蒸散量预测的研究已经开展不少,但是目前主要存在两大问题:(1)FAO-56推荐的固定或者简单差值作物系数,适合较长周期蒸散量的预测,而对于短期蒸散量的预测适用价值较低,并且作物系数法中的基础作物系数曲线只由确定的3个节点进行线性差值,对作物生长过程处理有所简化,从而会造成较大偏差;(2)由于降雨的不确定性,考虑降雨的蒸散量预测模型的研究较少,仅考虑确定性气象因子必然会造成典型天气下蒸散量预测的偏差,适用性较弱。To sum up, a lot of research on evapotranspiration prediction has been carried out, but there are two main problems: (1) The fixed or simple difference crop coefficient recommended by FAO-56 is suitable for long-term evapotranspiration prediction, while The prediction of short-term evapotranspiration has a low applicable value, and the basic crop coefficient curve in the crop coefficient method is only linearly differentiated by the determined three nodes, which simplifies the processing of the crop growth process, which will cause a large deviation; ( 2) Due to the uncertainty of rainfall, there are few studies on evapotranspiration prediction models considering rainfall. Only considering deterministic meteorological factors will inevitably lead to deviations in evapotranspiration prediction under typical weather, and the applicability is weak.

发明内容SUMMARY OF THE INVENTION

针对现有技术中的上述不足,本发明提供了一种考虑作物系数动态变化与降雨的农田蒸散量短期预测方法。In view of the above deficiencies in the prior art, the present invention provides a short-term forecasting method for farmland evapotranspiration considering the dynamic change of crop coefficients and rainfall.

为了达到上述发明目的,本发明采用的技术方案为:In order to achieve the above-mentioned purpose of the invention, the technical scheme adopted in the present invention is:

一种考虑作物系数动态变化与降雨的农田蒸散量短期预测方法,包括以下步骤:A short-term prediction method of farmland evapotranspiration considering the dynamic changes of crop coefficients and rainfall, including the following steps:

S1、获取农田作物生长环境的气象数据,所述气象数据包括最高气温、最低气温、日照时数和降雨量;S1, obtain the meteorological data of the growing environment of farmland crops, the meteorological data includes the highest temperature, the lowest temperature, the number of sunshine hours and the rainfall;

S2、根据预测基准日的参考作物蒸散量和农田实测蒸散量计算预测基准日的作物系数;S2. Calculate the crop coefficient on the forecast base day according to the reference crop evapotranspiration on the forecast base day and the farmland measured evapotranspiration;

S3、根据步骤S1获取的气象数据和步骤S2中农田实测蒸散量及计算的作物系数,分别构建训练集和测试集,并对训练集和测试集数据进行预处理;S3, according to the meteorological data obtained in step S1 and the measured evapotranspiration of the farmland and the calculated crop coefficient in step S2, respectively construct a training set and a test set, and preprocess the data of the training set and the test set;

S4、建立考虑作物系数动态变化和降雨影响的前馈神经网络模型,并利用训练集数据对模型进行训练优化;S4. Establish a feedforward neural network model considering the dynamic changes of crop coefficients and the influence of rainfall, and use the training set data to train and optimize the model;

S5、利用步骤S4优化后的前馈神经网络模型根据测试集数据预测农田作物蒸散量。S5, using the feedforward neural network model optimized in step S4 to predict the evapotranspiration of farmland crops according to the test set data.

进一步地,所述步骤S2具体采用彭曼算法计算预测基准日的参考作物蒸散量,计算公式为:Further, the step S2 specifically adopts the Penman algorithm to calculate the reference crop evapotranspiration on the forecast base day, and the calculation formula is:

Figure BDA0002583554930000031
Figure BDA0002583554930000031

其中,ET0为参考作物蒸散量,Δ为饱和水汽压曲线斜率,Rn为地表净辐射,G为土壤热通量,γ为干湿常数,Tmean为日平均温度,u2为设定高度位置风速,es为饱和水汽压,ea为实际水汽压。Among them, ET 0 is the reference crop evapotranspiration, Δ is the slope of the saturated water vapor pressure curve, Rn is the surface net radiation, G is the soil heat flux, γ is the dry and wet constant, T mean is the daily average temperature, and u 2 is the set height position wind speed, es is the saturated water vapor pressure, and ea is the actual water vapor pressure.

进一步地,所述步骤S2具体采用涡度相关法计算预测基准日的农田实测蒸散量,计算公式为:Further, the step S2 specifically adopts the vorticity correlation method to calculate the measured evapotranspiration of the farmland on the prediction base day, and the calculation formula is:

Figure BDA0002583554930000032
Figure BDA0002583554930000032

其中,w′为垂直风速脉动量,q′为水汽密度脉动值。Among them, w' is the vertical wind speed fluctuation, and q' is the water vapor density fluctuation value.

进一步地,所述步骤S2中预测基准日的作物系数的计算公式为:Further, the calculation formula of the crop coefficient of the prediction base day in the step S2 is:

Figure BDA0002583554930000041
Figure BDA0002583554930000041

其中,Kc为预测基准日的作物系数,ETc-EC为涡度相关系统实测值;Among them, K c is the crop coefficient on the forecast base day, and ET c-EC is the measured value of the eddy correlation system;

并设定农田作物在未来设定时间内的作物系数与预测基准日的作物系数相同。And set the crop coefficient of the field crops in the future set time to be the same as the crop coefficient of the forecast base day.

进一步地,所述步骤S3中对训练集和测试集数据进行预处理具体为:Further, the preprocessing of the training set and the test set data in the step S3 is specifically:

采用双曲正切变换函数,根据训练集和测试集中样本数据测量值的最大值和最小值的权重对样本数据测量值进行标准化处理,表示为:Using the hyperbolic tangent transformation function, the sample data measurement values are standardized according to the weights of the maximum and minimum values of the sample data measurement values in the training set and the test set, which are expressed as:

Figure BDA0002583554930000042
Figure BDA0002583554930000042

其中,X'为标准化处理后的样本数据测量值,X为样本数据测量值,Xmax、Xmin分别为样本数据测量值的最大值和最小值。Wherein, X' is the measured value of the sample data after standardization, X is the measured value of the sample data, and X max and X min are the maximum and minimum values of the measured value of the sample data, respectively.

进一步地,所述步骤S4具体为:Further, the step S4 is specifically:

构建包含输入层、隐藏层和输出层三层拓扑结构的前馈神经网络模型,并设定BP神经网络中输入层包含4个神经元、隐藏层包含10个神经元、输出层包含1个神经元。Construct a feedforward neural network model with three-layer topology including input layer, hidden layer and output layer, and set the input layer to contain 4 neurons, the hidden layer to contain 10 neurons, and the output layer to contain 1 neuron in the BP neural network. Yuan.

本发明具有以下有益效果:The present invention has the following beneficial effects:

本发明考虑作物系数动态变化和降雨因素对农田作物蒸散量短期预测的影响,建立考虑作物系数动态变化和降雨影响的前馈神经网络模型,并利用涡度相关法实测的蒸散量作为实测值对模型进行训练优化,有效构建了农田参考作物蒸散量与其驱动因素之间的非线性关系,据此可以得到更符合作物实际生长状况的作物蒸散量,为农田下垫面的未来水分管理提供科学依据。。The present invention considers the influence of the dynamic changes of crop coefficients and rainfall factors on the short-term prediction of crop evapotranspiration, establishes a feedforward neural network model considering the dynamic changes of crop coefficients and the influence of rainfall, and uses the evapotranspiration measured by the vorticity correlation method as the measured value pair. The model is trained and optimized to effectively construct the nonlinear relationship between the reference crop evapotranspiration and its driving factors. Based on this, the crop evapotranspiration that is more in line with the actual growth conditions of the crop can be obtained, providing a scientific basis for the future water management of the underlying surface of the farmland. . .

附图说明Description of drawings

图1为本发明考虑作物系数动态变化与降雨的农田蒸散量短期预测方法流程示意图;Fig. 1 is the schematic flow chart of the short-term prediction method of farmland evapotranspiration considering the dynamic change of crop coefficient and rainfall in the present invention;

图2为本发明实施例中本发明与多元线性回归模型的预测值与实测值对比图;Fig. 2 is the comparison chart of the predicted value and the measured value of the present invention and the multiple linear regression model in the embodiment of the present invention;

图3为本发明实施例中本发明与多元线性回归模型的预测值与实测值验证结果图。FIG. 3 is a graph showing the verification result of the predicted value and the measured value of the present invention and the multiple linear regression model in the embodiment of the present invention.

具体实施方式Detailed ways

下面对本发明的具体实施方式进行描述,以便于本技术领域的技术人员理解本发明,但应该清楚,本发明不限于具体实施方式的范围,对本技术领域的普通技术人员来讲,只要各种变化在所附的权利要求限定和确定的本发明的精神和范围内,这些变化是显而易见的,一切利用本发明构思的发明创造均在保护之列。The specific embodiments of the present invention are described below to facilitate those skilled in the art to understand the present invention, but it should be clear that the present invention is not limited to the scope of the specific embodiments. For those of ordinary skill in the art, as long as various changes Such changes are obvious within the spirit and scope of the present invention as defined and determined by the appended claims, and all inventions and creations utilizing the inventive concept are within the scope of protection.

如图1所示,本发明实施例提供了一种考虑作物系数动态变化与降雨的农田蒸散量短期预测方法,包括以下步骤S1至S5:As shown in FIG. 1 , an embodiment of the present invention provides a short-term prediction method for farmland evapotranspiration considering dynamic changes of crop coefficients and rainfall, including the following steps S1 to S5:

S1、获取农田作物生长环境的气象数据,所述气象数据包括最高气温、最低气温、日照时数和降雨量;S1, obtain the meteorological data of the growing environment of farmland crops, the meteorological data includes the highest temperature, the lowest temperature, the number of sunshine hours and the rainfall;

在本实施例中,本发明以北京市大兴区为研究区对相关数据进行说明。北京市大兴区(39°26′-39°51′N,116°13′-116°43′E)位于华北平原北部永定河冲击平原,总面积为1031km2,属于温带半湿润季风气候,多年平均气温为12.1℃。多年年平均降雨量为540mm,7月和9月降雨较多,降雨量占全年降雨总量的80%以上。北京市大兴试验站下垫面主要为农田,包括玉米/小麦、大豆,其中以玉米和小麦轮作为主,冬小麦整个生育期为260天左右(10月1日-次年6月30日),在正常年份冬小麦需补充灌溉,以保证作物对水分的需求。夏玉米生长期约90天左右(7月1日-9月30日),夏玉米全生育期不灌水。研究区作物生长阶段不存在水分胁迫。从试验站的气候及下垫面条件与大兴地区对比分析,试验站具有较好的典型性。In this embodiment, the present invention takes Daxing District of Beijing as a research area to describe the relevant data. Daxing District, Beijing (39°26′-39°51′N, 116°13′-116°43′E) is located in the Yongding River Shock Plain in the northern part of the North China Plain, with a total area of 1031km2. It belongs to a temperate semi-humid monsoon climate with an annual average temperature is 12.1°C. The average annual rainfall for many years is 540mm, with more rainfall in July and September, accounting for more than 80% of the total annual rainfall. The underlying surface of Beijing Daxing Experiment Station is mainly farmland, including corn/wheat and soybean, among which corn and wheat are the main ones. The whole growth period of winter wheat is about 260 days (October 1st to June 30th of the following year). In normal years, winter wheat needs supplemental irrigation to ensure the water demand of crops. The growth period of summer corn is about 90 days (July 1st to September 30th), and no irrigation is required during the whole growth period of summer corn. There was no water stress in the growing stage of crops in the study area. From the comparative analysis of the climate and underlying surface conditions of the experimental station and the Daxing area, the experimental station has a good typicality.

本发明在中国气象科学共享服务网收集了2015-2017年的历史气象数据,在天气网收集了2018年-2019年的1d~7d预见期逐日天气预报数据。历史气象资料数据包括:气压Pa、风速U、最高气温Tmax、最低气温Tmin、平均相对湿度RH、日照时数n、降雨量P等。天气预报数据及信息包括:最高气温Tmax、最低气温Tmin、天气情况等。The present invention collects historical meteorological data from 2015 to 2017 on the China Meteorological Science Shared Service Network, and collects daily weather forecast data for the forecast period from 1d to 7d from 2018 to 2019 on the Weather Network. Historical meteorological data include: air pressure P a , wind speed U, maximum temperature T max , minimum temperature T min , average relative humidity RH, sunshine hours n, rainfall P and so on. Weather forecast data and information include: maximum temperature T max , minimum temperature T min , weather conditions, and the like.

本发明根据降雨对地面的影响而引起的各种现象,按照降雨量等级表估计降雨共分11等级。再根据天气预报的降雨预报信息确定降雨量值。降雨量等级表如表1所示。According to the various phenomena caused by the influence of rainfall on the ground, the present invention estimates the rainfall to be divided into 11 grades according to the rainfall grade table. The rainfall value is then determined according to the rainfall forecast information of the weather forecast. The rainfall grade table is shown in Table 1.

表1 降雨量等级表Table 1 Rainfall grade table

Figure BDA0002583554930000061
Figure BDA0002583554930000061

本发明中日照时数是指太阳每天垂直于其光线的平面上的辐射强度超过或者等于120w/m2的时间长度。根据地区地理位置参数,一年中每天的辐射Ra可以由太阳常数、太阳倾斜角等计算出,计算公式为:In the present invention, sunshine hours refer to the length of time during which the radiation intensity of the sun on a plane perpendicular to its rays exceeds or equals to 120w/m2 every day. According to the geographical location parameters of the region, the daily radiation Ra in a year can be calculated from the solar constant, the solar inclination angle, etc. The calculation formula is:

Figure BDA0002583554930000071
Figure BDA0002583554930000071

其中,Ra为辐射,c为光速,Gsc为太阳常数、dr为太阳与地球相对距离,W为太阳倾角,h为当地纬度,采用弧度单位;ks为日落时角。Among them, Ra is the radiation, c is the speed of light, G sc is the solar constant, d r is the relative distance between the sun and the earth, W is the inclination of the sun, h is the local latitude, in radians; k s is the sunset time angle.

S2、根据预测基准日的参考作物蒸散量和农田实测蒸散量计算预测基准日的作物系数;S2. Calculate the crop coefficient on the forecast base day according to the reference crop evapotranspiration on the forecast base day and the farmland measured evapotranspiration;

在本实施例中,为了得到预测基准日较为精确的参考作物蒸散量,本发明基于气象数据利用(Penman-Monteith)PM法计算预测基准日的参考作物蒸散量,计算公式为:In the present embodiment, in order to obtain a more accurate reference crop evapotranspiration on the forecast base day, the present invention uses the (Penman-Monteith) PM method to calculate the reference crop evapotranspiration on the forecast base day based on meteorological data, and the calculation formula is:

Figure BDA0002583554930000072
Figure BDA0002583554930000072

其中,ET0为参考作物蒸散量,Δ为饱和水汽压曲线斜率,Rn为地表净辐射,G为土壤热通量,γ为干湿常数,Tmean为日平均温度,u2为设定高度位置风速,具体为2米高处的风速,es为饱和水汽压,ea为实际水汽压。Among them, ET 0 is the reference crop evapotranspiration, Δ is the slope of the saturated water vapor pressure curve, Rn is the surface net radiation, G is the soil heat flux, γ is the dry and wet constant, T mean is the daily average temperature, and u 2 is the set height Location wind speed, specifically the wind speed at a height of 2 meters, es is the saturated water vapor pressure, and ea is the actual water vapor pressure.

本发明采用涡度相关系统(Campbell Scientific Inc.,USA)测定预测基准日的农田实测蒸散量,计算公式为:The present invention adopts the eddy correlation system (Campbell Scientific Inc., USA) to measure the measured evapotranspiration of the farmland on the forecast base day, and the calculation formula is:

Figure BDA0002583554930000073
Figure BDA0002583554930000073

其中,w′为垂直风速脉动量,q′为水汽密度脉动值。Among them, w' is the vertical wind speed fluctuation, and q' is the water vapor density fluctuation value.

上述涡度相关系统由CSAT3型三维超声风速仪、LI7500 CO2/H2O开路气体分析仪、HMP45C空气温湿度传感器和CR5000型数据采集器等组成。净辐射Rn由CNR4净辐射传感器测定,土壤热通量G由两块位于地表以下2cm处的HFP01土壤热通量板测定,全部测定项均取30min的平均值作为每次记录值,日蒸散量由24h数据累计得到。在涡度相关实际数据处理过程中,依据以下原则对异常数据进行剔除:①降水时段以及前后各1h的数据;②明显超出物理含义的数据;③传感器状态出现异常的数据。此外,通过计算日内波文比修正潜热通量来消除能量不闭合引起的误差。The above eddy correlation system consists of CSAT3 three-dimensional ultrasonic anemometer, LI7500 CO2/H2O open-circuit gas analyzer, HMP45C air temperature and humidity sensor and CR5000 data collector. The net radiation Rn is measured by the CNR4 net radiation sensor, and the soil heat flux G is measured by two HFP01 soil heat flux panels located 2cm below the surface. Accumulated from 24h data. In the actual data processing process of vorticity correlation, the abnormal data is eliminated according to the following principles: (1) the data of the precipitation period and 1 hour before and after; (2) the data that obviously exceeds the physical meaning; (3) the abnormal data of the sensor state. In addition, the latent heat flux is corrected by calculating the intraday Bowen ratio to eliminate errors caused by energy non-closure.

本发明根据上述方法得到的预测基准日的参考作物蒸散量和农田实测蒸散量计算预测基准日的作物系数,表示为:The present invention calculates the crop coefficient of the predicted base day according to the reference crop evapotranspiration and the farmland measured evapotranspiration obtained by the above-mentioned method, and is expressed as:

Figure BDA0002583554930000081
Figure BDA0002583554930000081

其中,Kc为预测基准日的作物系数,ETc-EC为涡度相关系统实测值;Among them, K c is the crop coefficient on the forecast base day, and ET c-EC is the measured value of the eddy correlation system;

并设定农田作物在未来设定短期时间内的作物系数与预测基准日的作物系数相同,具体设定未来1~7天内的作物系数与预测基准日的动态作物系数相同,即K′c-var1=Kc=K′c-var2……=K′c-var7And set the crop coefficient of farmland crops in the short-term set in the future to be the same as the crop coefficient of the forecast base day, specifically set the crop coefficient in the next 1 to 7 days to be the same as the dynamic crop coefficient of the forecast base day, that is, K′ c- var1 = Kc =K'c -var2 ...= K'c-var7 .

由于预测基准日的作物系数既能反应气象数据对蒸散量影响,也能反映作物种类、土壤水肥条件和田间管理水平对蒸散量的影响,因此本发明通过考虑预测基准日的作物系数对农田作物蒸散量短期预测的影响,构建农田作物蒸散量短期预测能够更准确的预测农田作物蒸散量,从而实现对农田作物蒸散量的短期精准预测。Since the crop coefficient on the forecast base day can reflect the influence of meteorological data on evapotranspiration, as well as the influence of crop types, soil water and fertilizer conditions and field management level on evapotranspiration, the present invention considers the crop coefficient on the forecast base day to affect the crop in the field. The influence of short-term forecast of evapotranspiration, the construction of short-term forecast of crop evapotranspiration can more accurately predict the evapotranspiration of crops, so as to achieve short-term accurate forecast of crop evapotranspiration.

S3、根据步骤S1获取的气象数据和步骤S2中农田实测蒸散量及计算的作物系数,分别构建训练集和测试集,并对训练集和测试集数据进行预处理;S3, according to the meteorological data obtained in step S1 and the measured evapotranspiration of the farmland and the calculated crop coefficient in step S2, respectively construct a training set and a test set, and preprocess the data of the training set and the test set;

在本实施例中,由于步骤S1获取的2015年~2019年气象数据中一部分气象数据可能是因环境干扰、人为操作而不存在或不正常,因此本发明对获取的气象数据进行筛选后最终得到了900组数据集。每个训练样本从选取2015-2017年的3月-9月历史气象数据中随机选取100组数据作为训练集,从2018-2019年3月-9月历史气象预报数据中随机选取100组数据作为验证集。In this embodiment, since a part of the meteorological data from 2015 to 2019 in the meteorological data obtained in step S1 may not exist or be abnormal due to environmental interference and human operation, the present invention finally obtains the obtained meteorological data after screening the obtained meteorological data. 900 datasets. Each training sample randomly selects 100 sets of data from the historical meteorological data from March to September in 2015-2017 as the training set, and randomly selects 100 sets of data from the historical meteorological forecast data from March to September in 2018-2019 as the training set. validation set.

由于数据集中多种数据的量纲不同,量值较大,因此本发明需要对训练集和测试集数据进行预处理;具体而言,即对数据量值进行标准化,从而避免过度训练,提高某些层的神经节点数的收敛程度和计算速度,提高计算精度。Since the dimensions of various data in the data set are different and the magnitudes are relatively large, the present invention needs to preprocess the data of the training set and the test set; specifically, the data magnitudes are standardized, so as to avoid over-training and improve certain The convergence degree and calculation speed of the number of neural nodes in some layers are improved, and the calculation accuracy is improved.

本发明采用双曲正切变换函数,根据训练集和测试集中样本数据测量值的最大值和最小值的权重对样本数据测量值进行标准化处理,表示为:The present invention adopts the hyperbolic tangent transformation function to standardize the sample data measurement value according to the weight of the maximum value and the minimum value of the sample data measurement value in the training set and the test set, which is expressed as:

Figure BDA0002583554930000091
Figure BDA0002583554930000091

其中,X'为标准化处理后的样本数据测量值,X为样本数据测量值,Xmax、Xmin分别为样本数据测量值的最大值和最小值。Wherein, X' is the measured value of the sample data after standardization, X is the measured value of the sample data, and X max and X min are the maximum and minimum values of the measured value of the sample data, respectively.

通过对样本数据测量值进行标准化处理,可以将样本数据测量值标准化到[-1,1]的范围内,从而显示出最大非线性特征。By normalizing the sample data measurements, the sample data measurements can be normalized to the range [-1, 1], which shows the maximum nonlinearity.

S4、建立考虑作物系数动态变化和降雨影响的前馈神经网络模型,并利用训练集数据对模型进行训练优化;S4. Establish a feedforward neural network model considering the dynamic changes of crop coefficients and the influence of rainfall, and use the training set data to train and optimize the model;

在本实施例中,BP模型建模包括二个阶段:预处理(包括变量选择、数据分割和数据规范化)、训练(包括体系结构和网络训练过程)。BP上一层各神经元通过传递函数实现对下一层各神经元的全连接,同层神经元之间无关联。当学习样本提供给神经网络后,神经网络首先进行正向传播过程。如果输出与目标输出之间误差超出预期,该正向传播过程转入反向传播过程,将误差信号沿原来的连接通路返回,通过修改各层神经元的权值,使得误差信号减小。随着这种误差反向传播修正不断进行,网络对输入模式响应正确率不断提高,最终达到可以应用精度。In this embodiment, BP model modeling includes two stages: preprocessing (including variable selection, data segmentation and data normalization), and training (including architecture and network training process). Each neuron in the upper layer of BP realizes the full connection to each neuron in the next layer through the transfer function, and there is no relationship between the neurons in the same layer. When the learning samples are provided to the neural network, the neural network first performs a forward propagation process. If the error between the output and the target output exceeds expectations, the forward propagation process is transferred to the back propagation process, and the error signal is returned along the original connection path, and the error signal is reduced by modifying the weights of neurons in each layer. As this error back-propagation correction continues, the correct rate of the network's response to the input pattern continues to improve, and finally achieves the applicable accuracy.

本发明根据以下公式计算得到隐含层单元数设置范围为3~12,计算公式为:The present invention calculates according to the following formula that the setting range of the number of hidden layer units is 3 to 12, and the calculation formula is:

Figure BDA0002583554930000101
Figure BDA0002583554930000101

其中,J为隐含层单元数,A为输入层单元数;B为输出层单元数;K为常数,取值1~10。Among them, J is the number of hidden layer units, A is the number of input layer units; B is the number of output layer units; K is a constant, ranging from 1 to 10.

由于输入输出的神经元数量是由目标决定的,连接方式也是固定的,所以结构主要取决于隐含层神经元的数量。隐藏节点太少会影响网络的功能,而隐藏节点太多则会导致网络对数据的过度适应。因此本发明设定最佳BP神经网络架构4-10-1,即BP神经网络中输入层包含4个神经元、隐藏层包含10个神经元、输出层包含1个神经元;并设定训练的学习率和迭代分别为0.1和5000。Since the number of input and output neurons is determined by the target and the connection method is fixed, the structure mainly depends on the number of neurons in the hidden layer. Too few hidden nodes will affect the function of the network, while too many hidden nodes will cause the network to over-adapt to the data. Therefore, the present invention sets the optimal BP neural network architecture 4-10-1, that is, the input layer in the BP neural network contains 4 neurons, the hidden layer contains 10 neurons, and the output layer contains 1 neuron; and set the training The learning rate and iterations are 0.1 and 5000, respectively.

本发明利用训练集数据作为输入变量训练考虑作物系数动态变化和降雨影响的前馈神经网络模型,并以涡度相关法计算预测基准日的农田实测蒸散量为输出变量,经过多次迭代训练,最终得到优化后的前馈神经网络模型。The invention uses the training set data as input variables to train a feedforward neural network model considering the dynamic changes of crop coefficients and the influence of rainfall, and uses the eddy correlation method to calculate and predict the measured farmland evapotranspiration on the base day as an output variable, and after multiple iterations of training, Finally, the optimized feedforward neural network model is obtained.

S5、利用步骤S4优化后的前馈神经网络模型根据测试集数据预测农田作物蒸散量。S5, using the feedforward neural network model optimized in step S4 to predict the evapotranspiration of farmland crops according to the test set data.

为了验证本发明的考虑作物系数动态变化和降雨影响的前馈神经网络模型的预测效果,本发明将考虑作物系数动态变化和降雨影响的前馈神经网络模型与多元线性回归模型(MLR)进行比较,并采用平均绝对误差MAE、均方根误差RMSE、决定系数R2和预报准确率ACC来评估模型的预测精度。In order to verify the prediction effect of the feedforward neural network model considering the dynamic change of crop coefficients and the influence of rainfall, the present invention compares the feedforward neural network model considering the dynamic change of crop coefficients and the influence of rainfall with the multiple linear regression model (MLR). , and use the mean absolute error MAE, root mean square error RMSE, coefficient of determination R 2 and forecast accuracy ACC to evaluate the prediction accuracy of the model.

上述评价参数的计算公式为:The calculation formula of the above evaluation parameters is:

Figure BDA0002583554930000102
Figure BDA0002583554930000102

Figure BDA0002583554930000111
Figure BDA0002583554930000111

Figure BDA0002583554930000112
Figure BDA0002583554930000112

Figure BDA0002583554930000113
Figure BDA0002583554930000113

其中,xi为农田作物蒸散量预测值,yi为农田参考作物蒸散量期望输出值,;i为预报样本序列,i=1,2,…,n;

Figure BDA0002583554930000114
为预测值和期望输出值序列的均值;n为预报值的样本数。ACC可对单个模型的外部预测能力是否达到统计所需精度给出度量,该值越接近于1,表示预测值与实测值越吻合,一般认为ACC>0.6时模型才有实际预测价值。Among them, x i is the predicted value of crop evapotranspiration, yi is the expected output value of evapotranspiration of reference crops in the farmland, and i is the predicted sample sequence, i=1,2,...,n;
Figure BDA0002583554930000114
is the mean of the series of predicted values and expected output values; n is the number of samples of predicted values. ACC can measure whether the external prediction ability of a single model reaches the required statistical accuracy. The closer the value is to 1, the more consistent the predicted value is with the measured value. It is generally believed that the model has actual predictive value when ACC>0.6.

如图2和图3所示,为本发明考虑作物系数动态变化和降雨影响的前馈神经网络模型与多元线性回归模型的预测值与实测值变化趋势对比图。从图中可以看出,这两种方法预测值与实测值的变化趋势基本一致,但是本发明考虑作物系数动态变化和降雨影响的前馈神经网络模型的预准确率较高,各项误差均较小,也证明了本发明在反映复杂非线性关系的优越性。As shown in Figure 2 and Figure 3, it is a comparison chart of the change trend of the predicted value and the measured value of the feedforward neural network model and the multiple linear regression model considering the dynamic change of the crop coefficient and the influence of rainfall in the present invention. It can be seen from the figure that the change trends of the predicted values and the measured values of these two methods are basically the same, but the pre-accuracy rate of the feedforward neural network model considering the dynamic changes of crop coefficients and the influence of rainfall is high, and the errors are all Smaller, it also proves the superiority of the present invention in reflecting complex nonlinear relationships.

本领域的普通技术人员将会意识到,这里所述的实施例是为了帮助读者理解本发明的原理,应被理解为本发明的保护范围并不局限于这样的特别陈述和实施例。本领域的普通技术人员可以根据本发明公开的这些技术启示做出各种不脱离本发明实质的其它各种具体变形和组合,这些变形和组合仍然在本发明的保护范围内。Those of ordinary skill in the art will appreciate that the embodiments described herein are intended to assist readers in understanding the principles of the present invention, and it should be understood that the scope of protection of the present invention is not limited to such specific statements and embodiments. Those skilled in the art can make various other specific modifications and combinations without departing from the essence of the present invention according to the technical teaching disclosed in the present invention, and these modifications and combinations still fall within the protection scope of the present invention.

Claims (6)

1. A farmland evapotranspiration short-term prediction method considering crop coefficient dynamic change and rainfall is characterized by comprising the following steps:
s1, acquiring meteorological data of the growth environment of the farmland crops according to meteorological forecast data, wherein the meteorological data comprise the highest air temperature, the lowest air temperature, sunshine hours and rainfall;
s2, calculating a crop coefficient of the prediction reference day according to the reference crop evapotranspiration of the prediction reference day and the actual field measurement evapotranspiration;
s3, respectively constructing a training set and a testing set according to the meteorological data obtained in the step S1, the actual field measurement evapotranspiration in the step S2 and the calculated crop coefficient, and preprocessing the data of the training set and the testing set;
s4, establishing a feedforward neural network model considering crop coefficient dynamic change and rainfall influence, and training and optimizing the model by using training set data;
and S5, predicting the evapotranspiration of the farmland crops according to the test set data by using the feedforward neural network model optimized in the step S4.
2. The method for short-term prediction of farmland evapotranspiration considering crop coefficient dynamic changes and rainfall as claimed in claim 1, wherein the step S2 specifically adopts a penman algorithm to calculate the reference crop evapotranspiration of the predicted reference day, and the calculation formula is as follows:
Figure FDA0002583554920000011
wherein, ET0For reference to crop evapotranspiration, delta is the slope of the saturated water-vapor pressure curve, Rn is the net surface radiation, G is the soilHeat flux, gamma is the dry-wet constant, TmeanIs the average daily temperature u2To set the altitude position wind speed, esSaturated water vapor pressure, eaThe actual water vapor pressure.
3. The method for short-term prediction of farmland evapotranspiration considering crop coefficient dynamic changes and rainfall as claimed in claim 2, wherein the step S2 specifically uses vorticity correlation method to calculate the actual farmland evapotranspiration predicted on the reference day by the following formula:
Figure FDA0002583554920000021
wherein w 'is the pulsating quantity of the vertical wind speed, and q' is the pulsating value of the water vapor density.
4. The method for short-term prediction of agricultural evapotranspiration considering crop coefficient dynamics and rainfall according to claim 3, wherein the calculation formula for predicting the crop coefficient on the reference day in step S2 is:
Figure FDA0002583554920000022
wherein, KcTo predict the crop coefficient of the reference day, ETc-ECIs the measured value of the vorticity correlation system;
and setting the crop coefficient of the farmland crop in the future set time to be the same as the crop coefficient of the prediction reference day.
5. The method for short-term prediction of farmland evapotranspiration considering crop coefficient dynamic changes and rainfall as claimed in claim 1, wherein the preprocessing of the training set and test set data in step S3 is specifically:
and adopting a hyperbolic tangent transformation function to carry out standardization processing on the sample data measurement value according to the weights of the maximum value and the minimum value of the sample data measurement value in the training set and the test set, wherein the weights are expressed as follows:
Figure FDA0002583554920000023
wherein, X' is the measured value of the sample data after standardization, X is the measured value of the sample data, Xmax、XminRespectively the maximum and minimum values of the sample data measurement.
6. The method for short-term prediction of farmland evapotranspiration considering crop coefficient dynamic changes and rainfall as claimed in claim 1, wherein said step S4 is specifically:
a feedforward neural network model of a three-layer topological structure comprising an input layer, a hidden layer and an output layer is constructed, and the input layer comprises 4 neurons, the hidden layer comprises 10 neurons and the output layer comprises 1 neuron in the BP neural network.
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