CN115688588A - Sea surface temperature daily change amplitude prediction method based on improved XGB method - Google Patents
Sea surface temperature daily change amplitude prediction method based on improved XGB method Download PDFInfo
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Abstract
The invention relates to the technical field of ocean surface temperature prediction, and provides a sea surface temperature daily variation amplitude prediction method based on an improved XGB method, which comprises the following steps: s1: acquiring a data set and preprocessing the data set, wherein the data set comprises wind speed data and short wave radiation value data; s2: establishing an XGboost model; s3: modifying the algorithm weight of the XGboost model by applying an LDS algorithm, and establishing an LDS-XGB model; s4: selecting a training set from the data set, and training the LDS-XGB model by using the training set; s5: and predicting the daily change amplitude of the sea surface temperature by using the trained LDS-XGB model. The XGB algorithm is innovatively used in SST daily variation amplitude prediction, and machine learning is applied to SST daily variation amplitude prediction; and smoothing the data label value by using an LDS method, so that the traditional unbalanced classification method can be applied to the regression problem.
Description
Technical Field
The invention relates to the technical field of ocean surface temperature prediction, in particular to a sea surface temperature daily change amplitude prediction method based on an improved XGB method.
Background
SST stands for sea surface temperature, and the current main methods for SST daily change research include observation research, empirical models and numerical simulation.
The development of marine observation greatly promotes the development of research on the daily change process of the SST, but is limited by observation means and data, and the understanding of the daily change process of the SST still has great defects.
Since the United kingdom 'challenger' started the science investigation of ocean environment in 1872, ship observation, offshore station or buoy observation become mainstream ocean observation means in nearly 150 years, and then the ocean observation capability is greatly improved through multiple ocean observation technology changes such as satellite remote sensing, TAO/TRITON ocean buoy array, argo, glider and the like.
In early marine SST data, sverdrupeteal, (1942) and Roll (1965) mentioned the daily warming phenomenon of SST. During the tropical marine global climate response experiment (TOGA/COARE), websteret et al (1992) observed a complete diurnal variation process over time in the warm pool region of the western pacific, and observed a maximum diurnal variation amplitude greater than 3 ℃. The large-area observation of the satellite provides a brand-new means for SST daily variation research, stuart-Mentethital, (2003) and the like provide a large-scale space-time characteristic diagram of SST daily variation close to the global range, find that large SST daily variation amplitude is easy to appear in tropical and mid-latitude areas, and emphasize the importance of the SST daily variation on SST measurement and marine environment. Yanetal, (2021) revealed variability of SST over the time scale of the season with SST daily changes using global tropical mooring buoy arrays, indicating that SST daily changes have a significant nonlinear effect on variability over longer time scales. The Lietal (2021) discovers that the daily change of the SST of the China sea is in a sine form through research, establishes an inversion mode of the daily average sea temperature product of the polar orbit satellite based on the daily change condition of the SST, and applies the inversion mode to 7716 visible infrared imaging radiometers in the China sea area.
However, since ship survey, buoy and the like can only perform observation on a single point, argo is mainly used for marine internal observation, and the description capability on the upper layer of the sea is insufficient. The large-area observation of the satellite provides a brand-new means for SST daily change research, but the time resolution of polar orbit satellites for the observation of the same place is up to twice a day, the daily change process of the resolution cannot be effectively realized, the synchronous satellite is limited by the influence of cloud and rain and the like, and the SST is difficult to continuously and effectively observe at present. Although marine scientists have conducted a great deal of research on the daily change process of the SST based on the above observation data, especially on the observation data of the SST, short-wave radiation, wind speed, wind direction and the like distributed in the range of 140 ° E-180 ° W,10 ° S-10 ° N at the hour level of time resolution in 1985 provided by the tropical marine global climate response experiment (TOGA/coarse). However, the SST daily change process is a complex process, on one hand, the ocean surface is the underlying surface of the atmosphere, and the SST directly affects the weather and climate, and on the other hand, the SST is also affected and controlled by various atmospheric and marine internal processes, so that people still have great defects in understanding the SST daily change.
A series of empirical models are developed, which can grasp the basic characteristics of SST daily variation, but the SST daily variation has limited application range and low precision.
Early Pricetotal (1987) proposed a representative empirical model that used wind stress and ocean heat flux to estimate the magnitude of the change in SST day. Since then, websteret al (1996) proposed a widely used diagnostic model for the daily variation range of SST skin temperature based on the analysis of a large amount of observed data. KawaiandandKawamura (2002) uses buoy data of tropical and mid-latitude areas, finds that precipitation has no obvious influence on SST daily change, removes daily average precipitation terms, and rewrites the daily average precipitation terms on the basis of a formula proposed by Websteret. Zenital (1999) and Gentemann et al (2003) propose empirical models estimating hourly changes in SST from a minimum value within a day, respectively. At present, people still have great defects in understanding the change of the SST day, and the traditional empirical models still have the problems of low precision, complex calculation and the like, so that the reasonable simulation and prediction of the change process of the SST day still remain a challenge at present.
Numerical simulation is an effective means of simulating and predicting the SST diurnal variation process, but is limited by the level of numerical pattern development, and accurate simulation and prediction remains a challenge.
With the rapid development of computer technology in the middle of the last century, the numerical model has been used in various fields rapidly and widely, and many researches for simulating the daily change of the SST by using the numerical dynamic model have been carried out by scientists. The ocean mixing layer mode, the ocean circulation mode and the ocean air coupling mode are all applied to the simulation of SST daily change. The marine mixed layer mode can be basically divided into three types: a multilayer threshold mode, a bulk-mix layer mode, and a multilayer turbulent flow mode. The one-dimensional mixed layer mode has the advantages of clear physical process, small calculation amount, easy operation and the like, but the one-dimensional mixed layer mode can only simulate the vertical change characteristics of temperature, salt and flow and cannot depict the horizontal change of the temperature, the salt and the flow. The ocean circulation mode and the ocean air coupling mode mainly simulate the daily change of the SST in two modes of direct simulation of the ocean circulation mode and nested mixed layer mode simulation of the ocean circulation mode, but the ocean mode in the mode needs higher vertical resolution (the upper 50 m layer needs to reach 1 m layer), so that on one hand, the calculated amount is greatly increased, and meanwhile, mode integral is unstable due to the fact that the vertical layer is too thin. The vertical subgrid parameterization scheme proposed by Schiller and Godfrey (2005) is applied to a three-dimensional ocean circulation mode NEMO for the first time by Yantal, and the daily change process of SST is accurately simulated in a global range. Because the vertical subgrid parameterization scheme has low requirements on mode calculation amount, long-time integration can be performed. In addition, because the SST daily change process itself is not known and the model itself has uncertainty factors such as parameterization, the simulation precision is difficult to guarantee.
The machine learning is more and more emphasized in the aspects of marine environment research, simulation, prediction and the like, and is expected to play an important role in the aspect of SST daily change process research under physical constraint.
With the rapid development of deep learning technology, the data-driven method based on the deep learning model is more and more emphasized in marine environment element prediction. In 2007, elisa et al used an Artificial Neural Network (ANN) to analyze the sea surface temperature in the western part of the Mediterranean sea, and the model better predicted the seasonal and annual changes in the sea temperature in that area. In 2017, qin and the like adopt an LSTM model to predict the sea surface temperature, the network architecture of the method consists of an LSTM layer and a fully-connected dense layer, and the effectiveness of the method is verified by taking the coastal sea area of China as an example. In the same year, jiang et al analyze the influence of temperature, salinity and geographical location on the thermocline, and propose an improved thermocline selection model based on an entropy method, which can effectively predict the change of temperature. In 2019, xiao et al established an LSTM model by using 36-year satellite-borne sea surface temperature data in the east and the middle of China, and the model has a good daily prediction effect on short-term and medium-term sea surface temperature fields. In 2020, xu et al proposed an M-LCNN prediction model that decomposed and reconstructed time series using wavelet transform to predict the sequence variation of sea surface temperature over multiple time scales. In the same year, he and the like construct an SSTP model adopting a local search strategy, and the SSTP model is suitable for sea temperature data prediction of a long-time sequence. Currently, there is a gap in the field of predicting SST daily changes using machine learning.
In summary, (1) although the conventional empirical model can grasp the basic characteristics of the SST daily change, the conventional empirical model has a limited application range and is not high in precision. At present, people still have great defects in understanding the daily change of the SST, and the traditional empirical model still has the problems of low precision, complex calculation and the like, so that the reasonable simulation and prediction of the daily change process of the SST still remain a challenge at present.
(2) Numerical simulation is an effective means of simulating and predicting the SST daily variation process, but is limited by the level of numerical pattern development, and accurate simulation and prediction remains a challenge. In addition, because the SST daily change process itself is not known and the model itself has parameterization and other uncertainty factors, the simulation precision is also difficult to guarantee.
(3) The machine learning is more and more emphasized in the aspects of marine environment research, simulation, prediction and the like, and is expected to play an important role in the aspect of SST daily change process research under physical constraint. The machine learning method achieves great results in the aspect of sea temperature prediction and the like, but the field of predicting SST daily change by utilizing machine learning is vacant at present.
Disclosure of Invention
In order to solve the problems in the background art, the invention provides a sea surface temperature daily variation amplitude prediction method based on an improved XGB method, which comprises the following steps:
s1: acquiring a data set and preprocessing the data set, wherein the data set comprises wind speed data and short wave radiation value data;
s2: establishing an XGboost model;
s3: modifying the algorithm weight of the XGboost model by applying an LDS algorithm, and establishing an LDS-XGB model;
s4: selecting a training set from the data set, and training the LDS-XGB model by using the training set;
s5: and predicting the daily change amplitude of the sea surface temperature by using the trained LDS-XGB model.
In a preferred scheme, the data set comprises average wind speed data every three hours within a plurality of days and average short wave radiation value data every three hours.
Further, the specific process of step S2 includes:
the XGboost model is a machine learning algorithm model which is added into another model based on the current model, so that the effect of the combined model is better than that of the current model, and the building process is as follows:
in the formula (I), the compound is shown in the specification,representing the predicted value of the model, K representing the number of decision trees, f k Representing the kth tree model, x i Which represents the (i) th training sample,representing all decision tree modelsA set of (a);
constructing an objective function, and then optimizing the objective function:
in the formula, n is the number of training samples; the objective function is composed of two parts, one part is a loss function l which is generally mean square error, and the other part is a regularization term omega which is the sum of the complexity of each tree, and the objective is to control the complexity of the model and prevent overfitting;
the tree set model of the formula (2) takes a function as a parameter, so that the traditional optimization method cannot be directly used for optimization, and an additive learning mode (additive learning) is adopted for training; each time the original model is kept unchanged, a new function f is added to the model as follows:
in the formula:iterating the ith sample for t times to obtain a predicted value;is the initial value of the ith sample;
constructing an optimal model by minimizing a loss function to obtain an objective function of the t-th round:
in the formula, cons is a constant term and is the complexity of the first t-1 trees;
and performing second-order Taylor expansion on the target function of the t-th round:
in the formula: g i ,h i Respectively representing the objective function pairFirst and second derivatives of;
due to loss functionIs a fixed value and is therefore incorporated into the constant term cons; the constant term has no influence on the optimization solution, so that the constant term can be removed; the target function depends only on the first and second derivatives at each sample point on the loss function, resulting in a new target function:
next consider the complexity term Ω of the decision tree; firstly, defining each tree, and converting a tree structure expression into a leaf structure expression; dividing the decision tree into a structure part q and a leaf weight part omega;
f t (x)=ω q(x) ,ω∈R T ,q:R d →{1,2,…,T} (8)
in the formula: t is the total number of leaf nodes of the regression tree, ω is a T-dimensional vector consisting of values of the leaf nodes, q (x) denotes that the sample x is on a certain leaf node, ω is q (x) Is the score of the node, i.e. the model prediction value of the sample;
the complexity term of the tree in the XGboost algorithm comprises two parts, one part is the total number of leaf nodes, the other part is the score of the leaf node, and an L2 smoothing term is added aiming at the score of each leaf node to avoid overfitting;
in the formula:modulo a leaf node vector; gamma represents the difficulty of node segmentation, lambda represents an L2 regularization coefficient, and the values of gamma and lambda represent the punishment to the tree with more leaf nodes;
rewriting the objective function according to the leaf structure:
in the formula: i is j ={i|q(x i ) = j } is the set of samples on leaf node j;
the target function comprises T independent univariate quadratic functions; we can define:
the final objective function is simplified as:
for unknown variable omega j Calculating a partial derivative, making the derivative be 0, obtaining an input loss function after an extreme point, and obtaining an extreme valueWill be provided withSubstituting formula (12) to obtain an optimal objective function:
the objective function is used for measuring the quality of the t tree structure, a greedy algorithm is utilized to traverse all the segmentation points in the splitting process, loss values are respectively calculated, then the segmentation point with the maximum gain value is selected, and the smaller the maximum value of the gain loss is, the better the model prediction is represented; the final gain expression is as follows:
in the formula:the score of the left sub-tree is represented,the score of the right sub-tree is represented,denotes the score without segmentation and λ denotes the complexity cost introduced by adding a new node. If the judgment value is larger than 0, the segmentation can be carried out, otherwise, the segmentation is not carried out.
Further, the specific process of step S3 includes:
is provided withRepresenting a training set of sample size n, whereinThe input is represented by a representation of the input,represents a label, y is of continuous type;
i.e. [ y ] 0 ,y 1 ),[y 1 ,y 2 ),…,[yB -1 ,y B ) (ii) a We useTo represent a group index of the target value byRepresenting an index space;
Calculating density distribution of SST daily variation amplitude of the label value in the training set according to delta y, and calling the density distribution as empirical density distribution; previous research shows that the empirical density distribution of the labels cannot reflect the real label density distribution under the condition that the label values are continuous because of the dependency between the data samples on the adjacent labels; LDS uses kernel density estimation to improve imbalance in continuous data sets;
A Gaussian kernel is a symmetric kernel satisfying k (y, y ') = k (y', y) and it characterizes the similarity between the target values y' and y; then convolution is carried out on the empirical density distribution to obtain a new distribution which is called as effective density distribution; the calculation formula is as follows:
wherein p (y) represents an empirical density distribution,represents the effective density distribution of the label value y';
in a general XGBoost algorithm, the regression tree loss function is generally chosen as the squared loss; after the effective density distribution is obtained through calculation, the weight is improved by using a weight weighting method for prediction;
in particular, we weight each training sample by multiplying it by the inverse of its effective density distribution; the resulting loss function is:
The invention has the following beneficial effects:
in the SST daily variation amplitude prediction, machine learning algorithms such as Bagging and RF can be used for predicting the SST daily variation amplitude, but the prediction error is larger than that of the XGB method, and the predicted SST daily variation amplitude is lower. The XGB algorithm is innovatively used in SST daily variation amplitude prediction, and machine learning is applied to SST daily variation amplitude prediction; and smoothing the data label value by using an LDS method, so that the traditional unbalanced classification method can be applied to the regression problem.
Drawings
FIG. 1 is a schematic overall flow diagram of the present invention;
FIG. 2 is a graph of empirical label density versus error;
FIG. 3 is a graph of effective label density versus error distribution;
FIG. 4 is a graphical representation of the predicted results of the XGB model;
FIG. 5 is a diagram showing the predicted result of the LDS-XGB model.
Detailed Description
The technical solutions of the present invention will be clearly and completely described below with reference to the drawings of the present invention, and the forms of the respective structures described in the following embodiments are merely examples, and the present invention is not limited to the respective structures described in the following embodiments, and all other embodiments obtained by a person of ordinary skill in the art without creative efforts belong to the scope of the present invention.
Referring to fig. 1-5, a sea surface temperature daily variation amplitude prediction method based on an improved XGB method includes the steps of: s1: acquiring a data set and preprocessing the data set, wherein the data set comprises wind speed data and short wave radiation value data; s2: establishing an XGboost model; s3: modifying the algorithm weight of the XGboost model by applying an LDS algorithm, and establishing an LDS-XGB model; s4: selecting a training set from the data set, and training the LDS-XGB model by using the training set; s5: and predicting the daily change amplitude of the sea surface temperature by using the trained LDS-XGB model.
The specific process of the step S2 includes:
the XGboost model is a machine learning algorithm model which is added into another model based on the current model, so that the effect of the combined model is better than that of the current model, and the building process is as follows:
in the formula (I), the compound is shown in the specification,representing the predicted value of the model, K representing the number of decision trees, f k Representing the kth tree model, x i Which represents the (i) th training sample,representing a set of all decision tree models;
an objective function is constructed and then optimized:
in the formula, n is the number of training samples; the objective function is composed of two parts, one part is a loss function l, generally a mean square error, and the other part is a regularization term omega, namely the sum of the complexity of each tree, so as to control the complexity of the model and prevent overfitting;
the tree set model of the formula (2) takes a function as a parameter, so that the traditional optimization method cannot be directly used for optimization, and an additive learning mode (additive learning) is adopted for training; each time the original model is kept unchanged, a new function f is added to the model as follows:
in the formula:iterating the ith sample for t times to obtain a predicted value;is the initial value of the ith sample;
constructing an optimal model by minimizing a loss function to obtain an objective function of the t-th round:
in the formula, cons is a constant term and is the complexity of the first t-1 trees;
and performing second-order Taylor expansion on the target function of the t-th round:
in the formula: g i ,h i Respectively representing the objective function pairFirst and second derivatives of;
due to loss functionIs a fixed value and is therefore incorporated into the constant term cons; the constant term has no influence on the optimization solution, so that the constant term can be removed; the target function depends only on the first and second derivatives of each sample point on the loss function, resulting in a new target function:
next consider the complexity term Ω of the decision tree; firstly, defining each tree, and converting a tree structure expression into a leaf structure expression; dividing the decision tree into a structure part q and a leaf weight part omega;
f t (x)=ω q(x) ,ω∈R T ,q:R d →{1,2,…,T} (8)
in the formula: t is the total number of leaf nodes of the regression tree, ω is a T-dimensional vector composed of values of the leaf nodes, q (x) represents that a sample x is on a certain leaf node, and ω is q (x) Is the score of the node, i.e. the model prediction value of the sample;
the complexity term of the tree in the XGboost algorithm comprises two parts, one part is the total number of leaf nodes, the other part is the score of the leaf node, and an L2 smoothing term is added aiming at the score of each leaf node to avoid overfitting;
in the formula:modulo a leaf node vector; gamma represents the difficulty of node segmentation, lambda represents an L2 regularization coefficient, and the values of gamma and lambda represent the punishment to the tree with more leaf nodes;
rewriting the objective function according to the leaf structure:
in the formula: i is j ={i|q(x i ) = j } is the set of samples on leaf node j;
the target function comprises T independent univariate quadratic functions; we can define:
the final objective function is simplified as:
for unknown variable omega j Calculating a partial derivative, making the derivative be 0, obtaining an input loss function after an extreme point, and obtaining an extreme valueWill be provided withSubstituting formula (12) to obtain an optimal objective function:
the objective function is used for measuring the quality of the t tree structure, all the division points are traversed by using a greedy algorithm in the splitting process, loss values are respectively calculated, then the division point with the maximum gain value is selected, and the smaller the maximum value of the gain loss is, the better the model prediction is represented; the final gain expression is as follows:
in the formula:the score of the left sub-tree is represented,the score of the right sub-tree is represented,denotes the score without segmentation and λ denotes the complexity cost introduced by adding a new node. If the judgment value is larger than 0, the segmentation can be carried out, otherwise, the segmentation is not carried out.
Further, the specific process of step S3 includes:
is provided withRepresenting a training set of sample size n, whereinThe input is represented by a representation of the input,represents a label, y is of continuous type;
i.e. [ y ] 0 ,y 1 ),[y 1 ,y 2 ),…,[y B-1 ,y B ) (ii) a We useTo represent a group index of the target value byRepresenting an index space;
Calculating density distribution of SST daily variation amplitude of the label value in the training set according to delta y, and calling the density distribution as empirical density distribution; previous research shows that the empirical density distribution of the labels cannot reflect the real label density distribution under the condition that the label values are continuous because of the dependency between the data samples on the adjacent labels; LDS uses kernel density estimation to improve imbalance in continuous data sets;
The Gaussian kernel is a symmetric kernel satisfying k (y, y ') = k (y', y) and it characterizes the similarity between the target values y' and y; then convolution is carried out on the empirical density distribution to obtain a new distribution which is called as effective density distribution; the calculation formula is as follows:
wherein p (y) represents an empirical density distribution,represents the effective density distribution of the label value y';
in a general XGBoost algorithm, the regression tree loss function is generally chosen as the squared loss; after the effective density distribution is obtained through calculation, the weight is improved by using a weight weighting method for prediction;
in particular, we weight the loss function by multiplying it by the inverse of the effective density distribution of each training sample; the resulting loss function is:
Example 1:
the embodiment is applied to the sea surface temperature daily change amplitude prediction, and develops the LDS-XGB model suitable for predicting the sea surface temperature daily change amplitude. The observation data of tropical sea and global atmospheric-ocean coupling response experiment (TOGACOARE) during observation period are adopted, and the observation data comprises parameters such as heat sensitivity, latent heat, short-wave radiation, wind stress, sea surface temperature and the like. Buoy data of 133 sites are selected, the distribution range is 25 degrees S-21 degrees N in the global range, the time resolution is 1 hour or 10 minutes, and the time span is 10 months-2021 months-8 months in 1992.
And (3) preprocessing an experimental data set, dividing a training set and a testing set according to a ratio of 8. And simultaneously calculating the average wind speed every three hours and the average short wave radiation every three hours. The SST daily variation amplitude is predicted by taking the average wind speed every three hours and the average short wave radiation every three hours as input.
First, the pearson correlation coefficient between the empirical label density and the error distribution is calculated to be-0.38, and the correlation between the empirical label density and the error distribution is weak. The results are shown in FIG. 2:
the Pearson correlation coefficient between the effective label density and the error distribution is-0.56, and the result shows that the effective label density obtained by LDS calculation has good correlation with the error distribution. The results are shown in FIG. 3:
and respectively training the training set by using the XGboost and the LDS-XGB, and predicting the test set after training. The prediction result shows that the model LDS-XGB after the re-weighting has good performance in both a training set and a verification set. The prediction results of the XGboost and the LDS-XGB are shown in FIGS. 4 and 5:
the evaluation results of the fitness and prediction error of the XGB model and the LDS-XGB model with unmodified weights are shown in tables 1 to 2.
TABLE 1 SST daily variation amplitude prediction model evaluation results
TABLE 2 SST daily variation amplitude model prediction statistics
As can be seen from tables 1-2: both the training set and the test set obtain higher fitting degree and smaller error value, and the model is proved to have good performance in the prediction of SST day change amplitude. And the fitting degree of the XGB model and the LDS-XGB model reaches more than 70 percent from the aspect of the fitting degree. In terms of errors, the RMSE of the model is taken as an evaluation index and reaches 17.773 percent and 17.771 percent respectively. When the weight is not modified, the predicted SST daily variation amplitude value is more than 99% and less than 2 ℃, and after the weight is modified, the model can predict the value more than 2 ℃, which shows that the model has certain effect on improving the data imbalance. The LDS _ XGB model improves the prediction of high values to a certain extent.
The above description is only for the purpose of illustrating the preferred embodiments of the present invention and is not to be construed as limiting the invention, and any modifications, equivalents, improvements and the like that are within the spirit and principle of the present invention are intended to be included in the scope of the present invention.
Claims (4)
1. A sea surface temperature day change amplitude prediction method based on an improved XGB method is characterized by comprising the following steps:
s1: acquiring a data set and preprocessing the data set, wherein the data set comprises wind speed data and short wave radiation value data;
s2: establishing an XGboost model;
s3: modifying the algorithm weight of the XGboost model by applying an LDS algorithm, and establishing an LDS-XGB model;
s4: selecting a training set from the data set, and training the LDS-XGB model by using the training set;
s5: and predicting the daily change amplitude of the sea surface temperature by using the trained LDS-XGB model.
2. The sea surface temperature daily variation amplitude prediction method based on the improved XGB method as claimed in claim 1, wherein the method comprises the following steps: the data set includes average wind speed data at three hour intervals over several days, and average short wave radiance data at three hour intervals.
3. The sea surface temperature daily variation amplitude prediction method based on the improved XGB method as claimed in claim 1, wherein the method comprises the following steps: the specific process of the step S2 includes:
the XGboost model is a machine learning algorithm model which is added into another model based on the current model, so that the effect of the combined model is better than that of the current model, and the establishing process is as follows:
in the formula (I), the compound is shown in the specification,representing the predicted value of the model, K representing the number of decision trees, f k Representing the kth tree model, x i The (i) th training sample is represented,representing a set of all decision tree models;
constructing an objective function, and then optimizing the objective function:
in the formula, n is the number of training samples; the objective function is composed of two parts, one part is a loss function l, generally a mean square error, and the other part is a regularization term omega, namely the sum of the complexity of each tree, so as to control the complexity of the model and prevent overfitting;
the tree set model of the formula (2) takes a function as a parameter, so that the traditional optimization method cannot be directly used for optimization, and an additive learning mode (additive learning) is adopted for training; each time the original model is kept unchanged, a new function f is added to the model as follows:
……
in the formula:iterating the ith sample for t times to obtain a predicted value;is the initial value of the ith sample;
constructing an optimal model by minimizing a loss function to obtain an objective function of the t-th round:
in the formula, cons is a constant term and is the complexity of the first t-1 trees;
and performing second-order Taylor expansion on the target function of the t-th round:
in the formula: g i ,h i Respectively representing the objective function pairFirst and second derivatives of;
due to loss functionIs a fixed value and is therefore incorporated into the constant term cons; the constant item has no influence on the optimization solution, so that the constant item can be removed; the target function depends only on the first and second derivatives of each sample point on the loss function, resulting in a new target function:
next consider the complexity term Ω of the decision tree; firstly, defining each tree, and converting a tree structure expression into a leaf structure expression; dividing the decision tree into a structure part q and a leaf weight part omega;
f t (x)=ω q(x) ,ω∈R T ,q:R d →{1,2,…,T} (8)
in the formula: t is the total number of leaf nodes of the regression tree, ω is a T-dimensional vector composed of values of the leaf nodes, q (x) represents that a sample x is on a certain leaf node, and ω is q (x) Is the score of the node, i.e. the model prediction value of the sample;
the complexity term of the tree in the XGboost algorithm comprises two parts, one part is the total number of leaf nodes, the other part is the score of the leaf node, and an L2 smoothing term is added aiming at the score of each leaf node to avoid overfitting;
in the formula:is the modulus of the leaf node vector; gamma represents the difficulty of node segmentation, lambda represents an L2 regularization coefficient, and the values of gamma and lambda represent the punishment to the tree with more leaf nodes;
rewriting the objective function according to the leaf structure:
in the formula: i is j ={i|q(x i ) = j } is the set of samples on leaf node j;
the target function comprises T independent univariate quadratic functions; we can define:
the final objective function is simplified as:
for unknown variable omega j Calculating a partial derivative, making the derivative be 0, obtaining an input loss function after an extreme point, and obtaining an extreme valueWill be provided withSubstituting equation (12) to obtain an optimal objective function:
the objective function is used for measuring the quality of the t tree structure, all the division points are traversed by using a greedy algorithm in the splitting process, loss values are respectively calculated, then the division point with the maximum gain value is selected, and the smaller the maximum value of the gain loss is, the better the model prediction is represented; the final gain expression is as follows:
in the formula:the score of the left sub-tree is represented,the score of the right sub-tree is represented,and the score is expressed when the node is not segmented, the lambda represents the complexity cost introduced by adding a new node, if the judgment value is greater than 0, the node can be segmented, otherwise, the node is not segmented.
4. The sea surface temperature daily variation amplitude prediction method based on the improved XGB method as claimed in claim 2, wherein the method comprises the following steps: the specific process of the step S3 includes:
is provided withRepresenting a training set of sample size n, whereinThe input is represented by a representation of the input,represents a label, y is of continuous type;
i.e. [ y ] 0 ,y 1 ],[y 1 ,y 2 ),…,[y B-1 ,y B ) (ii) a We useTo represent a group index of the target value byRepresenting an index space;
Calculating density distribution of SST daily variation amplitude of the label value in the training set according to delta y, and calling the density distribution as empirical density distribution; previous research shows that the empirical density distribution of the labels cannot reflect the real label density distribution under the condition that the label values are continuous because of the dependency between data samples on adjacent labels; LDS uses kernel density estimation to improve imbalance in continuous data sets;
The Gaussian kernel is a symmetric kernel satisfying k (y, y ') = k (y', y) and it characterizes the similarity between the target values y' and y; then convolution is carried out on the empirical density distribution to obtain a new distribution which is called as effective density distribution; the calculation formula is as follows:
wherein p (y) represents an empirical density distribution,represents the effective density distribution of the label value y';
in a general XGboost algorithm, the regression tree loss function is generally chosen as the squared loss; after the effective density distribution is obtained through calculation, the weight is improved by using a weight weighting method for prediction;
in particular, we weight the loss function by multiplying it by the inverse of the effective density distribution of each training sample; the resulting loss function is:
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