CN111582557A - Wind power climbing event multi-stage early warning method based on variation function - Google Patents

Wind power climbing event multi-stage early warning method based on variation function Download PDF

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CN111582557A
CN111582557A CN202010313374.4A CN202010313374A CN111582557A CN 111582557 A CN111582557 A CN 111582557A CN 202010313374 A CN202010313374 A CN 202010313374A CN 111582557 A CN111582557 A CN 111582557A
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汪岩佳
任国瑞
万杰
刘浩
张庭赫
刘雅茜
文人庆
谭代敏
鄂鹏
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Abstract

The invention relates to a method for depicting a wind power climbing event, in particular to a wind power climbing event multi-stage early warning method based on a variation function, which specifically comprises the following steps: firstly, a corresponding relative wind power time sequence is obtained by using the definition of relative wind power. And describing the relative wind power time sequence by using the square root of the variation function, and performing autocorrelation analysis on the obtained wind power real-time change rate time sequence. And according to the analysis result, establishing a prediction model by using a BP neural network, and predicting the sequence. And selecting a multi-level threshold value of the wind power climbing event in a variation depicting mode, and identifying a prediction result of the BP neural network by using the threshold value to realize multi-level early warning of the wind power climbing event. The method makes up the defect that only the first and last points of power are considered in the traditional wind power climbing event definition; the change conditions of all time points in a period of time are comprehensively considered, and the climbing event is more accurately defined and identified.

Description

Wind power climbing event multi-stage early warning method based on variation function
Technical Field
The invention relates to a method for depicting a wind power climbing event, in particular to a wind power climbing event multi-stage early warning method based on a variation function depicting mode, and the predictability of the prediction of the wind power climbing event is improved.
Background
The uncertain understanding and mastering of wind power is a key basic problem for promoting safe and efficient consumption of large-scale renewable energy and structure transformation of clean energy in China. The power climbing event caused by long-time limit weather is an important expression of wind power uncertainty; although the occurrence probability is small, the prediction and control are difficult, and the method can cause great influence and harm to the safe and stable operation, scheduling planning and real-time control of the power grid. Therefore, it is necessary to perform the prediction work of the wind power climbing event.
At present, the early warning research results of wind power climbing events are more, and Zhangying and the like review and prospect are carried out on the wind power climbing event research; it is a common form to characterize a hill climbing event by the absolute value of the power difference between the first and last time of the time period being greater than a threshold. Ruan Rui et al propose a wind power generation power prediction based on equivalent average wind speed, which carries out mean value processing on the change values at the first and last moments; the combined prediction method based on atom sparse decomposition and back propagation neural network is provided by the tomimen and the like, and the prediction accuracy is improved. However, in the above research, only the first and last time values of a certain period of time are considered for defining and describing the climbing event, the change conditions of all time points within a certain period of time are not considered, and the predictability of the time series obtained by only considering the first and last time change values is poor.
In practice, a wind power climbing event is a random occurrence event, and even a serious wind power climbing event can occur in a short time, so that only a difference value at the first moment and the last moment is selected to define after a fixed time period is set, and all wind power climbing events cannot be considered, so that how to describe the wind power climbing event is more accurate and how to improve the predictability of the climbing event is a problem worthy of deep research.
Disclosure of Invention
In order to improve the predictability of the wind power climbing event and increase the predictable length of the wind power climbing event, the invention provides a wind power climbing event multi-stage early warning method based on a variation function. The method comprises the following steps:
the method comprises the following steps: acquiring a relative wind power curve by utilizing the output power curve of the wind power plant and the corresponding load curve of the power grid;
step two: on the basis of using the definition of an absolute value of the relative wind power variation, quantitatively depicting a wind power climbing event by using a square root of a variation function, and acquiring a time series curve of the real-time variation rate of the wind power after variation;
step three; after the time sequence of the real-time change rate of the wind power is obtained, the self-correlation analysis is carried out on the time sequence, and the predictability of the time sequence is observed;
step four: establishing a predictive model of the wind power climbing event based on the wind power real-time change rate time sequence by utilizing a BP neural network algorithm;
step five: and defining a threshold selecting method of the wind power climbing event according to the absolute value of the relative wind power variation to obtain a multi-level threshold in a variation depicting mode, and effectively identifying a prediction result of the BP neural network by using the threshold to realize multi-level early warning of the wind power climbing event.
The invention has the advantages that:
1) the wind power climbing event is described by using the variation, the predictable length for describing the wind power state sequence is increased, and the predictability of the wind power climbing event is improved.
2) The defect that only the first and last points of power are considered in the traditional wind power climbing event definition is made up; the change conditions of all time points in a period of time are comprehensively considered, and the climbing event is more accurately defined and identified.
3) By utilizing a method of dividing a plurality of thresholds, the multi-stage early warning suitable for climbing of different degrees is realized.
Drawings
FIG. 1 is a schematic flow diagram of the process of the present invention;
FIG. 2 is a relative wind power curve;
FIG. 3 is a real-time variation rate curve of wind power;
FIG. 4 is a diagram of the results of the autocorrelation analysis of the time series of the real-time variation rate of the wind power;
FIG. 5 is a partial enlarged view of the autocorrelation analysis result of the time series of the real-time variation rate of the wind power;
FIG. 6 is a diagram of the result of the time-series autocorrelation analysis of the absolute value of the relative wind power variation;
FIG. 7 is a partial enlarged view of the result of the autocorrelation analysis of the absolute time series of the relative wind power variation;
FIG. 8 is a prediction result of the BP neural network model;
fig. 9 shows a wind power climbing event prediction situation after threshold division.
Detailed Description
The first embodiment is as follows:
the wind power climbing event multilevel early warning idea based on the variation function in the embodiment is as follows:
firstly, a corresponding relative wind power time sequence is obtained by using the definition of relative wind power. And describing the relative wind power time sequence by using the square root of the variation function, and performing autocorrelation analysis on the obtained wind power real-time change rate time sequence. And according to the analysis result, establishing a prediction model by using a BP neural network, and predicting the sequence. And selecting a multi-level threshold value of the wind power climbing event in a variation depicting mode, and identifying a prediction result of the BP neural network by using the threshold value to realize multi-level early warning of the wind power climbing event.
The method comprises the following steps: acquiring a relative wind power curve by utilizing the output power curve of the wind power plant and the corresponding load curve of the power grid;
step two: on the basis of using the definition of the absolute value of the variation relative to the wind power, quantitatively depicting the wind power climbing event by using the square root of the variation function, and acquiring a time series curve of the real-time variation rate of the wind power after variation;
step three; after the time sequence of the real-time change rate of the wind power is obtained, the self-correlation analysis is carried out on the time sequence, and the predictability of the time sequence is observed;
step four: establishing a predictive model of the wind power climbing event based on the wind power real-time change rate time sequence by utilizing a BP neural network algorithm;
step five: and defining a threshold selecting method of the climbing event according to the absolute value of the relative wind power variation to obtain a multi-level threshold in a variation depicting mode, and effectively identifying a prediction result of the BP neural network by using the threshold to realize multi-level early warning of the wind power climbing event.
The second embodiment is as follows:
the embodiment further defines the wind power climbing event multi-stage early warning method based on the variation function in the first specific embodiment.
The prediction of the wind power climbing event mainly prevents the wind power climbing event from threatening the stable operation of a power grid. Therefore, a relative wind power curve is selected to predict the wind power climbing event.
The method comprises the following steps: setting the time sequence of the output power curve of the wind power plant as P (t), the time sequence of the load curve of the power grid as Q (t), and setting the time sequence P' (t) relative to the wind power curve as:
P'(t)=P(t)-Q(t) (1)
the positive and negative peak regulation characteristics of wind power are fully considered relative to the wind power. When the wind power change trend is consistent with the load demand of the power grid, even larger wind power output power change is beneficial to the power grid; when the wind power change trend is opposite to the load demand of the power grid, even smaller wind power output power is harmful to the power grid, so the wind power climbing event using the relative wind power is more accurate.
The invention uses the wind power data of one month of a power plant in Changchun to calculate the relative wind power. The sampling interval of the data points is 1min, and fig. 2 is a relative wind power curve obtained after calculation.
The third concrete implementation mode:
the embodiment further defines the wind power climbing event multi-stage early warning method based on the variation function in the first specific embodiment.
Step two, firstly: the wind power climbing event is defined by using the absolute value of the relative wind power variation, as shown in a formula (2):
|P'(t+Δt)-P'(t)|>Pval(2)
the change value of the relative wind power represents the difference value of the relative wind power at the first moment and the last moment in the time period from t to t + delta t. When the absolute value of the difference is larger than the set threshold value PvalWhen the wind power climbing event occurs, the wind power climbing event is considered to occur; and when the absolute value of the difference value at the first moment and the last moment is smaller than the set threshold value, the wind power climbing event is not considered to occur.
Step two: the variation function is a tool for measuring the variation of the attribute parameters of the spatial variation along with the distance variation, and can reflect the spatial characteristics of the regionalized variables.
Assuming that P' (t) represents a wind power time series, the variation function of the wind power can be expressed as:
Figure BDA0002458527660000041
wherein, P' (t)i) Represents the value of the ith point in the time series of the relative wind power curve, P' (t)i+ Δ t) represents the value of the i + Δ t point in the time series of the relative wind power curve, Δ t represents the time interval, and N (Δ t) represents the total amount of data points in the Δ t time.
The variation function refers to the degree of variation of a spatial variable over a distance in a particular direction. Due to this feature of degradation, it can be applied to the time domain. According to the definition in the first step, when a climbing event occurs, the change value of the relative wind power is increased, and the change value of the relative wind power is increased accordingly. The variation alpha (Δ t) can thus be expressed as a hill climbing situation of the power system over a period of time. This value continues to increase when a hill climbing event occurs. The load climbing event can be quantitatively characterized by the parameter of the relative wind power variation alpha (delta t).
However, considering that the square operation in the variation function makes the curve change more steeply, and the predictability is reduced, the method performs the evolution processing on the basis of the variation function, and defines the obtained final variation square root as the real-time variation rate γ (Δ t) of the wind power, as shown in formula (4). The hill climbing event can be effectively identified by setting a reasonable threshold value.
Figure BDA0002458527660000042
The final description mode based on the variation function carries out square root operation and accumulation operation on the basis of the variation value operation, so that the description sequence is more gentle, and the predictability of the description sequence is improved. And the defect that only the first time point and the last time point can be selected in the change value operation is made up, so that the wind power climbing event is more accurately described.
The time interval delta t selected by the method is 15min, and the wind power climbing condition in the delta t period 15min in the future is predicted. And (3) obtaining a wind power real-time change rate time series curve based on the real relative wind power curve obtained in the step one, wherein the real relative wind power curve is shown in figure 3.
The fourth concrete implementation mode:
the embodiment further defines the wind power climbing event multi-stage early warning method based on the variation function in the first specific embodiment.
Before the actual forecasting is performed, the predictability of the time series needs to be studied first. Let { xt}t=1:nIs a random time sequence, xtDelayed by k steps of sample xt+kThe autocorrelation coefficient between them indicates the degree of correlation of the two signals. The larger the autocorrelation coefficient is, the stronger dependence relationship exists between the two signals, and the rules hidden in the data can be mined by using a statistical method to realize the prediction of future data. The k steps at this time represent the autocorrelation length, i.e., the best modeling prediction length of the time series.
There are many methods for time series autocorrelation analysis, among which Pearson autocorrelation analysis is a more classical method whose basic principle is as follows:
let { xt}t=1:nIs a random time sequence, then measure xtDelayed by k steps of sample xt+kThe autocorrelation coefficient ρ (k) of (a) is calculated as follows:
Figure BDA0002458527660000051
Figure BDA0002458527660000052
in practice, the random time sequence in the formula (6) is replaced by the actual time sequence in different depicting ways during the specific calculation, k is the delay step length, n is the length of the wind power time sequence in different depicting ways,
Figure BDA0002458527660000054
is the mean value, x, of the wind power time series under different depicting modest+kIs to time-sequence the original power xtAnd (3) analyzing the predictability of the wind power time sequence under different depicting modes according to the calculation result, wherein gamma (k) is the covariance after delaying k steps, gamma (0) is the covariance when the delay step k is equal to 0, and rho (k) is the autocorrelation coefficient obtained after delaying k steps. In general, the correlation coefficients and their corresponding degrees of correlation are shown in table 1 below:
TABLE 1 correlation coefficient and degree of correlation
Figure BDA0002458527660000053
In general, the autocorrelation coefficient tends to decrease as the autocorrelation length increases. Moreover, the autocorrelation coefficient is between 0.5 and 0.8, which indicates that strong correlation exists between data, so the threshold value of the autocorrelation coefficient is 0.6 in the invention. Strong dependence exists between signals with autocorrelation coefficients within an autocorrelation time range of more than 0.6, and the time scale is the optimal prediction length. Therefore, in the correlation analysis of the present invention, the calculated predictable length is based on the length of the correlation coefficient 0.6, which is defined as the predictable time series step size.
The obtained real-time wind power change rate sequence is subjected to autocorrelation analysis, the obtained results are shown in fig. 4 and 5, meanwhile, a corresponding time sequence (shown in formula 2) of the absolute value of the relative wind power change amount is selected for autocorrelation analysis, the obtained results are shown in fig. 6 and 7, it can be seen that the predictable length of the real-time wind power change rate sequence is 40min, and the predictable length of the time sequence (shown in formula (2)) of the absolute value of the relative wind power change amount is 6 min. By the method, the predictable length of the climbing event can be obviously improved, and the predictability of the wind power climbing event is improved.
The fifth concrete implementation mode:
the embodiment further defines the wind power climbing event multi-stage early warning method based on the variation function in the first specific embodiment.
Step four: according to the result of the autocorrelation analysis, the time series is found to satisfy a prediction condition. And selecting sequences of the first 1800 time points in one month as a training set, selecting time sequences of the last 100 time points as a prediction set, and establishing a prediction model based on the variation time sequences after evolution by using a BP (back propagation) neural network. The obtained prediction results are shown in fig. 8. The method can be seen that the prediction condition of the series is better, and the prediction requirement of the wind power climbing event is basically met.
The sixth specific implementation mode:
the embodiment further defines the wind power climbing event multi-stage early warning method based on the variation function in the first specific embodiment.
And in the wind power climbing event, the absolute value of the relative wind power variation is defined, and the threshold is selected by using the allowable value of the grid frequency. Let PForehead (forehead)The total installed capacity of the power grid is n%, the wind power station accounts for n% of the total installed capacity, and the allowable deviation of the power supply frequency of the total installed capacity of the power grid above 300 ten thousand kilowatts is 0.2Hz according to the regulation of the national power supply business rules; the allowable deviation of the power supply frequency of the total installed capacity of the power grid below 300 ten thousand kilowatts is 0.5Hz, the difference adjustment coefficient k sigma is generally 4-6%, the power grid frequency requirement in China is 50Hz, and the relative wind power climbing event threshold value can be set as follows:
Figure BDA0002458527660000071
wherein alpha is 0.2 when the total installed capacity of the power grid is more than 300 ten thousand kilowatts; when the total installed capacity of the power grid is more than 300 ten thousand watts, alpha is 0.5.
And step two, when the wind power climbing event is depicted by using the variation function after the evolution, the wind power climbing event is considered to occur in a certain period of time if the difference between any data point and the data point after the delta t time is greater than a set threshold value due to the fact that the difference represents the sum of squares of the difference between each data point and the data point after the delta t time within the certain period of time delta t. Therefore we can set the threshold γref1(Δt)、γref2(Δt)、γref3(Δ t) and γref4(Δ t) represents the occurrence of a hill climbing event for 1 data point, the occurrence of a hill climbing event for the data point of 1/3, the occurrence of a hill climbing event for the data point of 2/3, and the occurrence of a hill climbing event for all data points, respectively, during the Δ t time period. As shown in equation (8).
Figure BDA0002458527660000072
When the variation of the relative wind power is square root gamma (delta t)<γref1(delta t), no wind power climbing event occurs in the delta t period, and early warning is not needed; when the relative wind power becomes worse square rootγref1(Δt)<γ(Δt)<γref2(delta t), a small-scale wind power climbing event possibly occurs within a delta t period, and is defined as four-stage early warning; when the relative wind power is changed to gammaref2(Δt)<γ(Δt)<γref3(delta t), a medium-scale wind power climbing event possibly occurs within a delta t period, and is defined as three-level early warning; when the relative wind power is changed to gammaref3(Δt)<γ(Δt)<γref4(delta t), a large-scale wind power climbing event possibly occurs within a delta t period, and secondary early warning is defined; when the relative wind power is changed to gammaref4(Δt)<And when gamma (delta t) is obtained, a large-scale wind power climbing event is certainly generated within the delta t period, and primary early warning is defined. After the threshold value is obtained, the time series prediction result of the step four is identified, and the future wind power climbing event can be accurately predicted by using the actually measured data at the current moment.
In the invention, the actually measured power grid selects 0.2Hz as the allowable deviation of the power supply frequency, the instantaneous maximum value of the power is set as the rated power, and as the capacities of the selected wind power plants are all larger than 300 ten thousand kilowatts, α is 0.2, and the threshold value gamma can be obtainedref1(Δt)=68.283;γref2(Δt)=88.153;γref3(Δt)=176.31;γref4(Δ t) 264.46. The wind power climbing event prediction result divided by the threshold is shown in fig. 9.
The electric power system can make a more reasonable and economic dispatching plan according to the forecasting result of the wind power climbing event, more rotary standby is provided in the time period of forecasting the occurrence of the large power load climbing event, and the safe, efficient and stable operation of the regional electric power system is ensured.

Claims (6)

1. Wind power climbing event multi-stage early warning method based on variation function is characterized in that: the method comprises the following steps:
the method comprises the following steps: acquiring a relative wind power curve by utilizing the output power curve of the wind power plant and the corresponding load curve of the power grid;
step two: on the basis of using the definition of an absolute value of the relative wind power variation, quantitatively depicting a wind power climbing event by using a square root of a variation function, and acquiring a time series curve of the real-time variation rate of the wind power after variation;
step three: after the time sequence of the real-time change rate of the wind power is obtained, the self-correlation analysis is carried out on the time sequence, and the predictability of the time sequence is observed;
step four: establishing a predictive model of the wind power climbing event based on the wind power real-time change rate time sequence by utilizing a BP neural network algorithm;
step five: and defining a threshold selecting method of the wind power climbing event according to the absolute value of the relative wind power variation to obtain a multi-level threshold in a variation depicting mode, and effectively identifying a prediction result of the BP neural network by using the threshold to realize multi-level early warning of the wind power climbing event.
2. The wind power climbing event multi-stage early warning method based on the variation function as claimed in claim 1, wherein: in the first step, the time sequence P' (t) relative to the wind power curve is:
P'(t)=P(t)-Q(t) (1)
the time sequence of the output power curve of the wind power plant is P (t), and the time sequence of the load curve of the power grid is Q (t).
3. The wind power climbing event multi-stage early warning method based on the variation function as claimed in claim 1, wherein: and the wind power climbing event in the second step meets the following requirements:
|P'(t+Δt)-P'(t)|>Pval(2)
wherein P '(t) and P' (t + Deltat) are relative wind power values of t and t + Deltat, respectively, PvalThe set wind power climbing event threshold value is set.
4. The wind power climbing event multi-stage early warning method based on the variation function as claimed in claim 1, wherein: in step two, the variation function is expressed as:
Figure FDA0002458527650000011
wherein P '(t) represents the time series of the relative wind power curve, P' (t)i) Represents the value of the ith point in the time series of the relative wind power curve, P' (t)i+ Δ t) represents the value of the i + Δ t point in the time sequence of the relative wind power curve, Δ t represents the time interval, and N (Δ t) represents the total amount of data points in the Δ t time;
the real-time change rate gamma (Δ t) of the wind power is expressed as:
Figure FDA0002458527650000021
5. the wind power climbing event multi-stage early warning method based on the variation function as claimed in claim 1 or 3, wherein: in the fifth step, the threshold value of the wind power climbing event is represented as
Figure FDA0002458527650000022
Wherein, PForehead (forehead)The total installed capacity of the power grid is represented by n%, the capacity of the wind power plant in the total installed capacity is represented by α being 0.2 when the total installed capacity of the power grid is more than 300 ten thousand kilowatts, and α being 0.5 when the total installed capacity of the power grid is more than 300 ten thousand kilowatts.
6. The wind power climbing event multi-stage early warning method based on the variation function as claimed in claim 5, wherein: in the fifth step, a threshold value gamma is setref1(Δt)、γref2(Δt)、γref3(Δ t) and γref4(Δ t) indicates that a hill climbing event occurs at 1 data point, a hill climbing event occurs at 1/3 data points, a hill climbing event occurs at 2/3 data points, and a hill climbing event occurs at all data points within a Δ t period, respectively, then
Figure FDA0002458527650000023
N (delta t) represents the total amount of data points in delta t time, and when the real-time change rate gamma of the wind power is (gamma)Δt)<γref1(delta t), no wind power climbing event occurs in the delta t period, and early warning is not needed; when gamma isref1(Δt)<γ(Δt)<γref2(delta t), a small-scale wind power climbing event possibly occurs within a delta t period, and is defined as four-stage early warning; when gamma isref2(Δt)<γ(Δt)<γref3(delta t), a medium-scale wind power climbing event possibly occurs within a delta t period, and is defined as three-level early warning; when gamma isref3(Δt)<γ(Δt)<γref4(delta t), a large-scale wind power climbing event possibly occurs within a delta t period, and secondary early warning is defined; when gamma isref4(Δt)<And when gamma (delta t) is obtained, a large-scale wind power climbing event is certainly generated within the delta t period, and primary early warning is defined.
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