CN107092653A - A kind of landslide Critical Rainfall Threshold based on method of fuzzy cluster analysis - Google Patents

A kind of landslide Critical Rainfall Threshold based on method of fuzzy cluster analysis Download PDF

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CN107092653A
CN107092653A CN201710153276.7A CN201710153276A CN107092653A CN 107092653 A CN107092653 A CN 107092653A CN 201710153276 A CN201710153276 A CN 201710153276A CN 107092653 A CN107092653 A CN 107092653A
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class
landslide
rainfall threshold
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温宗周
李璐
张阳阳
董勋凯
王真
李志文
王妍
李帅
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Xian Polytechnic University
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Abstract

The invention discloses a kind of landslide Critical Rainfall Threshold based on method of fuzzy cluster analysis, developing algorithm Investment Models are determined to landslide critical excitation approaches threshold value, the selection of the fuzzy clustering factor are carried out by Delphi method;Based on the fuzzy cluster analysis of this progress landslide Critical Rainfall threshold value, create data matrix, standardized data matrix and set up fuzzy similarity matrix, finally carry out fuzzy clustering and determine Critical Rainfall threshold value.Landslide Critical Rainfall Threshold of the invention based on method of fuzzy cluster analysis, strict mathematical algorithm is derived and statistical technique and physical means, each factor of influence in region is taken into full account, so that it is determined that rainfall threshold value.This method degree of accuracy is high, can meet the requirement of current landslide precaution alarm, greatly improves threshold accuracy, the reasonable determination of Critical Rainfall threshold value is to ensureing that landslide precaution alarm accuracy plays an important role.

Description

A kind of landslide Critical Rainfall Threshold based on method of fuzzy cluster analysis
Technical field
The invention belongs to landslide disaster forecasting technique field, and in particular to a kind of landslide based on method of fuzzy cluster analysis is faced Boundary's rainfall Threshold.
Background technology
With Global climate change, the extreme catchment frequency is constantly raised, and causes global mountain flood event to rise, times It is concerned;China's mountain area area is vast, the features such as landslide disaster has occurrence frequency height, has a very wide distribution, loses serious, in advance Survey, forecast, early warning difficulty are big, and the main risk factor that landslide occurs is rainfall.Nationwide internal cause extra torrential rain in 1998 And it is 1157 people to induce substantial amounts of landslide, the death toll that causes of avalanche and mud-stone flow disaster, the wounded is more than 10,000.Face Using more universal in the mountain flood prevention work at home and abroad of this index of boundary's rainfall, determine that method is also varied, respectively have An eternal lasting.Rational rainfall threshold value index is the key point that Regional Heavy Rain mud-rock flow is prevented and reduced natural disasters.
Conventional rainfall threshold value research method mainly has 2 kinds at present, and the first is the statistical analysis side based on disaster data Method, by carrying out statistical analysis to actual rainfall and landslide disaster data, draws corresponding early stage effective precipitation and triggering Relation between rainfall, so as to draw rainfall threshold curve, this method often have ignored underlying surface vegetation state, geological conditions Deng some other factorses of influence landslide disaster, and the landslide Critical Rainfall of gained is to represent a regional extent rather than one Individual specific landslide point;Second is similar analogy method, the area for lacking rainfall and disaster data, when these local ground Reason, geology, ecology etc. cause the area of calamity threshold limit value more similar to having determined that, can approximately think to cause calamity Critical Rainfall also phase Seemingly, can suitably it be adjusted according to actual conditions.No matter but each region topography and geomorphology or factor of influence are not identical , accuracy rate is greatly reduced.
The content of the invention
It is an object of the invention to provide a kind of landslide Critical Rainfall Threshold based on method of fuzzy cluster analysis, solution Statistical analysis technique and the similar analogy method of having determined are when calculating threshold value, the problem of accuracy is too low.
The technical solution adopted in the present invention is that a kind of landslide Critical Rainfall threshold value based on method of fuzzy cluster analysis is determined Method, specifically implements according to following steps:
Step 1, the fuzzy clustering factor are determined;
The fuzzy cluster analysis of step 2, the Critical Rainfall threshold value that comes down;
Step 3, carry out fuzzy clustering and determine Critical Rainfall threshold value.
The beneficial effects of the invention are as follows,
(1) during the fuzzy clustering factor is determined, carried out using De Feier methods special for the purpose of determining landslide formative element Family's investigation, the fuzzy clustering factor finally chosen.
(2) landslide Critical Rainfall Threshold is carried out from method of fuzzy cluster analysis, strengthens threshold accuracy, it is to avoid Because misleading rate caused by threshold value is inaccurate, so as to effectively remind people's disaster prevention to occur in landslide disaster.
In summary, compared with the existing methods:The problem of Critical Rainfall threshold value that comes down determination is a complexity, to make really Process is determined more comprehensively from Systems Theory, based on method of fuzzy cluster analysis, passes through developing algorithm Investment Models, strict mathematics Algorithmic derivation and statistical technique and physical means, take into full account each factor of influence in region, so that it is determined that rainfall threshold value, the determination Method is more comprehensive, as a result relatively reliable, mutually presses close to actual.
Brief description of the drawings
Fig. 1 is that heavy rain landslide is excited in the landslide Critical Rainfall Threshold based on method of fuzzy cluster analysis of the invention Rainfall pattern generally changes figure;
Fig. 2 is that landslide causes calamity critical in the landslide Critical Rainfall Threshold based on method of fuzzy cluster analysis of the invention Rainfall threshold value assessment technology flow chart;
Fig. 3 be in the landslide Critical Rainfall Threshold based on method of fuzzy cluster analysis of the invention Liu family's ditch come down it is close Degree and critical excitation approaches strength relationship figure.
Embodiment
The present invention is described in detail with reference to the accompanying drawings and detailed description.
Landslide Critical Rainfall Threshold of the invention based on method of fuzzy cluster analysis, it is specifically real according to following steps Apply:
The Critical Rainfall threshold value that comes down is affected by many factors, and these factors are with including but is not limited to the landform in landslide basin Looks, material resource deposit, physical geography position, condition of raining etc..Data are observed in part landslide basin without accurate rainfall, if Other landslide basins can be found, it is essentially identical with the landslide basin surface condition, while Critical Rainfall threshold values is, it is known that can join The Critical Rainfall value is examined, so as to obtain the value that the Critical Rainfall threshold values is close.
Step 1, the fuzzy clustering factor are determined
The factor for characterizing landslide surface condition feature is numerous, and interdependence between each factor, mutually restriction.In order to select Take out the most representational fuzzy clustering factor, main following several principles:1) simplicity and operability principle;2) Comprehensive and representativeness principle;3) leading factor principle;4) principle of combination of qualitative and quantitative analysis.
Take a broad survey in the wild, indoor synthetic analysis and with reference on the basis of existing research, enter using De Feier methods Expert investigation of the row for the purpose of determining landslide formative element, the fuzzy clustering factor finally chosen.
The illegal specific implementation step of Dare is as follows:
(1) panel of expert is constituted.Expert's number number, can according to prediction problem size and be related to face width and It is fixed, it is usually no more than 20 people.
(2) the problem of proposing to be predicted to all experts and relevant requirement, and enclose all back ofs the body about this problem Scape material, while asking expert proposes what material also needed to.Then, written reply is done by expert.
(3) material that each expert is received according to them, proposes the prediction opinion of oneself, and illustrates it how sharp oneself is With these materials and propose predicted value.
(4) every expert is judged that opinion collects for the first time, arranges into chart, contrasted, then be distributed to every expert, allowed Expert compares oneself different opinions with other people, changes opinion and the judgement of oneself.Every expertise can also be subject to Arrange, or other experts for asking identity higher are commented on, and these opinions are then distributed to every expert again, so that they join The opinion of oneself is changed after examination.
The fuzzy cluster analysis of step 2, the Critical Rainfall threshold value that comes down
Existing disaster data shows that heavy rain landslide excites rainfall pattern main based on fast peak type, as shown in Figure 1.It is above-mentioned , there is number of peaks when rainy in the rainfall of type;The time that rainfall occurs is also different, and early stage, mid-term, later stage are all present Possibility;The generally only heavy showers of short period, but some heavy showers can be with last longer.
Every landslide basin geologic setting environment is different, and its Critical Rainfall threshold value is incomplete same, but notices simultaneously The similar landslide basin difference of surface condition is little.Based on this understanding, the essentially identical landslide of two geological conditions represents three The similitude of a variety of physical quantitys in dimension space, it is above-mentioned similar based on what is occurred under fuzzy concept, the phase of fuzzy mathematics can be relied on Theory is closed to be solved.The Critical Rainfall threshold value estimating techniques flow that comes down is as shown in Figure 2.
1. data matrix is created
Assuming that the domain for being classified object is expressed as U={ x1,x2,…,xn, the character in any object passes through m index It is described:Xi={ xi1,xi2,…,xim(i=1,2 ..., n), the domain of U presentation class objects, x represents each of set Individual element, i, j distinguish the row and column of representing matrix, xijThe element that the i-th row j is arranged in representing matrix X.
Raw data matrix is expressed as follows:X=(xij)n×m
2. standardized data matrix
In actual mechanical process, data are different, and corresponding dimension has differences.By the way of conversion data, so it is right The frequently amount in more all kinds of dimensions.Even so, the data obtained using which, do not ensure necessarily to all belong to [0,1] area In., it is necessary to which compressed data is into [0,1] interval on the basis of fuzzy matrix demand.The main side of standardized data matrix Method is as follows:
1) standard deviation is standardized
I-th of variable is standardized, the mode used is conversion xijFor xij', wherein,Jth column element average value is represented, Represent the i-th row element average value, SjRepresent variance, MjThe intermediate value of jth row is represented, max { } is represented to take maximum, and min { } is represented Take minimum value, xij' element after standardization is represented, it is as follows:
In formula:
2) standardization with extreme difference:
3) extreme difference is standardized:
4) maximum is standardized:Wherein:Mj=max (x1j, x2j..., xnj) (6)
3. fuzzy similarity matrix is set up
Set up xiWith xjSimilarity degree rij=R (xi,xj) method mainly have:
1) Similar operator
1 ° of Cosin method:
2 ° of correlation coefficient process:
Usually, r is takenij=1-c (d (xi,xj))2, wherein c, α is the parameter suitably chosen, d (xi,xj) represent xiWith xj Distance, it causes 0≤rij≤1。rijSimilarity degree is represented, R (x) represents fuzzy matrix function, xikI-th row in representing matrix Kth column element, xjkJth row kth column element in representing matrix.
The distance of use has:
1 ° of Hamming distance from:
2 ° of Euclid distances:
3 ° of hebyshev distances:d(xi,xj)=max1≤k≤n|xik-xjk| (11)
2) Study on similar degree method
1 ° of minimax method:
The minimum method of 2 ° of arithmetic averages:
The minimum method of 3 ° of geometric averages:
Step 3, carry out fuzzy clustering and determine Critical Rainfall threshold value
Obscured according to the fuzzy similarity matrix R of gained in step 2 using transitive closure computing or Direct Cluster Analysis Cluster, last Cluster merging is a class U, stops cluster, and according to γiLocate the cluster of a classes, substitute into formula IhWith IminDetermine rainfall Measure threshold value.
1) Transitive Closure Method
Under normal circumstances, R=(rij) fuzzy matrix is substantially fuzzy similarity matrix, itself not necessarily possesses equivalence, because This R is also not necessarily fuzzy equivalent matrix, and using fuzzy transmission closure, it is mainly comprised the following steps:
A) cluster sample is divided into a classes according to one, obtains fuzzy similarity matrix R transitive closure, calculateUntil meeting R2n=Rn, at this moment fuzzy matrix Rn is one fuzzy etc. Valency matrix, note will
B) clustered by the orders of parameter γ from big to small, willIt is arranged in order in sequence, γ=1 is used as initially, According to order from big to small alongTakeObtain withCorresponding γ-interceptWhen element is equal to 1, represent Two corresponding samples of division or variable belong to a class, and corresponding is classified as into equivalence class respectively.
C) γ values constantly reduce, and are analogized downwards by aforesaid way and obtain more merging, if When, whole variables (or sample) are classified as a major class U, now γ=b stops cluster, are a classes by equivalence class in cluster process γ values be defined as γi
D) γ=γiWhen, corresponding classification situation is considered as cluster result, to all classes produce critical hour and point Clock rainfall threshold trait is analyzed:
A1, a2 represent the classification I of clustering factor, II class, a respectively31, a32Respectively represent the IIIth class first factor and Second factor, a1 '=0.89, a2 '=0.82 represents the coefficient of I, II classification respectively.
2) Direct Cluster Analysis
The basic conception of Direct Cluster Analysis, is completed after fuzzy similarity matrix establishment, by similar matrix, no demand transmission Closure, so as to obtain dendrogram, here is main flow:
If a) γ1=1, to each xiMake similar class [xi]R
[xi]R={ xj|rij=1 } (15)
Represent in rijUnder conditions of 1, x is obtainediWith xjBelong to a class, as Similarity Class.Distinguish equivalence class to it is similar Common element is not present in class, equivalence class, it is as follows:
At this moment need to merge the Similarity Class in all common elements, so as to obtain γ in level1All of equal value points of=1 Class.
If b) γ2Second largest value is represented, γ is searched in R2The all elements of similarity degree, are expressed as (xi,xj) element pair or Person rij2, with γ1=1 corresponding equivalence classification, merges xiAffiliated class and xjClass belonging to all, merges above-mentioned whole states Afterwards, γ2Obtained value is represented, is equivalence classification.
If c) γ3Value is the third-largest value, is searched and γ in R3Similarity identical element pair, is expressed as (xi,xj), then rij3Merge and γ2The x of corresponding all equivalence classesjAffiliated class and xiAffiliated class, merges after above-mentioned whole states, acquisition γ3For equivalence classification.
D) analogized downwards by aforesaid way, until all classes are merged into a class U, now γ=b stops cluster, will be poly- Equivalence class is defined as γ for the γ values of a classes in class processi
E) γ=γiWhen, corresponding classification situation is considered as cluster result, to all classes produce critical hour and point Clock rainfall threshold trait is analyzed:
A1, a2 represent the classification I of clustering factor, II class, a respectively31, a32Respectively represent the IIIth class first factor and Second factor, a1 '=0.89, a2 '=0.82 represents the coefficient of I, II classification respectively.
Embodiment 1
Step 1, the fuzzy clustering factor are determined
Take a broad survey in the wild, indoor synthetic analysis and the basis with reference to the research such as domestic Liu Xilin, Gong Xue, Chen Wei On, the expert investigation for the purpose of determining landslide formative element, the mould that investigation result is finally chosen are carried out using De Feier methods Paste clustering factor as shown in table 1, one has 10.And according to classifying importance, it is followed successively by the Ith important (rainfall erosivity, solid Material supply mode, slump gross area rate, regional climate type), it is the IIth important (structural property, formation lithology, dissected depth because Sub- accounting), the IIIth important (average slope of mountain slope, drainage area, the unreasonable activity of the mankind).Found in factual survey, region This two investigation value relative difficulties of the unreasonable activity of climate type, the mankind, thus it is determined that not considering during fuzzy factor, most 8 fuzzy clustering factors are chosen eventually, are rainfall erosivity, solid matter supply mode, slump gross area rate, construction spy respectively Property, formation lithology, dissected depth factor accounting, average slope of mountain slope, drainage area.
The fuzzy clustering factor of table 1
These three factors of solid matter supply mode, structural property and formation lithology are Qualitative factors, for ease of analysis meter Calculate, a kind of new method proposed based on Tan Ping Yan expert-" the quantification method of the landslide basin order of severity " can be commented according to therein Then Qualitative factor carries out Quantitative scoring to divider, and qualitative variable quantification is realized indirectly.Criteria for classification and score value are listed in table 2.
The criteria for classification of table 2 and grade form
The fuzzy cluster analysis of step 2, the Critical Rainfall threshold value that comes down
8 be have chosen with certain representativeness and oneself knows the landslide basin of Critical Rainfall, its fuzzy clustering factor parameter takes Value is shown in Table 3.
The fuzzy clustering factor value of table 3
Raw data matrix sees below formula:
In general, it is necessary to make proper transformation to raw data matrix, with reference to data characteristicses, using standardization with extreme difference method, Shown in formula is shown in.
Then, fuzzy resembling relation matrix r ij is constructed using correlation coefficient process, formula is as shown in 8.
After operation program, fuzzy similarity matrix R is obtained:
Step 3, carry out fuzzy clustering and determine Critical Rainfall threshold value
Fuzzy sample is divided into by four class a=4 according to classified adaptive factor standard, fuzzy similarity matrix R quadratic methods are transmitted Closure operation, R2->R4:R4That is t (R)=R4=R*
When taking γ=0.94, it can fall into 5 types, be respectively { A1, A3 }, { A2, A7 }, { A4 }, { A6 }, { A5, A8 }.
When taking γ=0.90,4 classes can be divided into, be respectively { A1, A3, A8 }, { A2, A7 }, { A4 }, { A6, A5 }, according to The sample clustering constituted, then γi=0.90.
The like, as γ=0.68, all landslide basins are all gathered for a class, stop cluster.
The Critical Rainfall threshold trait of table 4 is obtained according to formula.
A1, a2 represent the classification I of clustering factor, II class, a respectively31, a32Respectively represent the IIIth class first factor and Second factor, a1 '=0.89, a2 '=0.82 represents the coefficient of I, II classification respectively.
Constitute new sample using basin to be asked as new cluster sample and above-mentioned 8 landslides basin sample, then according to Foregoing Fuzzy Cluster Analysis method is analyzed, in the level of γ=0.9, studies that basin to be asked and which kind of landslide basin are gathered At one group, Critical Rainfall threshold estimation value in basin to be asked is used as using the Critical Rainfall threshold value that the group comes down.
The Critical Rainfall threshold trait of table 4
It is clear to illustrate, it is assumed that great Yu Gou landslides in Gansu are basin to be asked, and detailed process is described as follows.Obtain the density that comes down Scatter diagram corresponding with rainfall intensity, the density that the comes down as seen from Figure 3 proportionate relationship approximate with the presentation of rainfall intensity, The clustering factor on Gansu great Yu Gou streams landslide is shown in Table 5.
The clustering factor value of table 5
By Gansu great Yu Gou streams A9 and above 8 landslide bands constitute new cluster sample, divide according to foregoing fuzzy clustering Analysis method is analyzed.As a result show, as γ=0.93, Dongyang Ping Gou is clustered at the Ith group, therefore, it is possible to it was initially believed that big Valley ditch is similar to the Ith group of Critical Rainfall feature.To verify the validity of Fuzzy Cluster Analysis method, result of calculation and reality are listed Survey Critical Rainfall to be contrasted, be shown in Table 6.
The Comparative result of table 6
Ith group of Critical Rainfall threshold value Survey Critical Rainfall threshold value
10min raininess >=4mm 10min raininess >=3.4mm
1h raininess >=20mm 1h raininess >=19mm
From the results shown in Table 6, the predicted value of the prediction actual Critical Rainfalls of Gansu great Yu Gou takes the Ith group of Critical Rainfall Threshold value, with certain feasibility.

Claims (8)

1. a kind of landslide Critical Rainfall Threshold based on method of fuzzy cluster analysis, it is characterised in that it is specific according to Lower step is implemented:
Step 1, the fuzzy clustering factor are determined;
The fuzzy cluster analysis of step 2, the Critical Rainfall threshold value that comes down;
Step 3, carry out fuzzy clustering and determine Critical Rainfall threshold value.
2. the landslide Critical Rainfall Threshold according to claim 1 based on method of fuzzy cluster analysis, its feature It is, the fuzzy clustering factor is illegally determined using Dare in step 1.
3. the landslide Critical Rainfall Threshold according to claim 1 based on method of fuzzy cluster analysis, its feature It is, the Critical Rainfall threshold value estimating techniques flow that come down in step 2 is:
1. data matrix is created
Assuming that the character that the domain for being classified object is expressed as in U={ x1, x2 ..., xn }, any object is entered by m index Row description:(i=1,2 ..., n), the domain of U presentation class objects, x represents each of set to xi={ xi1, xi2 ..., xim } Individual element, i, j distinguish the row and column of representing matrix, xijThe element that the i-th row j is arranged in representing matrix X.
Raw data matrix is expressed as follows:X=(xij)n×m
2. standardized data matrix
1) standard deviation is standardized
I-th of variable is standardized, the mode used is conversion xijFor xij', wherein,Jth column element average value is represented,Represent I-th row element average value, SjRepresent variance, MjThe intermediate value of jth row is represented, max { } represents to take maximum, and min { } represents to take minimum Value, xij' element after standardization is represented, it is as follows:
In formula:
2) standardization with extreme difference:
3) extreme difference is standardized:
4) maximum is standardized:Wherein:Mj=max (x1j, x2j..., xnj) (6);
3. fuzzy similarity matrix is set up
Set up xi and xj similarity degrees rij=R (xi, xj), wherein main method has Similar operator and Study on similar degree method.
4. the landslide Critical Rainfall Threshold according to claim 3 based on method of fuzzy cluster analysis, its feature It is, Similar operator is specially:
1 ° of Cosin method:
2 ° of correlation coefficient process:
Usually, r is takenij=1-c (d (xi,xj))2, wherein c, α is the parameter suitably chosen, d (xi,xj) represent xiWith xjAway from From it causes 0≤rij≤1。rijSimilarity degree is represented, R (x) represents fuzzy matrix function, xikThe i-th row kth is arranged in representing matrix Element, xjkJth row kth column element in representing matrix.
Hamming distance from:
Euclid distances:
Chebyshev distances:d(xi,xj)=max1≤k≤n|xik-xjk| (11)。
5. the landslide Critical Rainfall Threshold according to claim 3 based on method of fuzzy cluster analysis, its feature It is, Study on similar degree method is specially:
1 ° of minimax method:
The minimum method of 2 ° of arithmetic averages:
The minimum method of 3 ° of geometric averages:
6. according to any described landslide Critical Rainfall Thresholds based on method of fuzzy cluster analysis of claim 3-5, Characterized in that, using Transitive Closure Method or Direct Cluster Analysis according to the fuzzy similarity matrix R of gained in step 2 in step 3 Fuzzy clustering is carried out, and is a class U by last Cluster merging, stops cluster, and according to γiLocate the cluster of a classes, substitute into formula Ih With IminDetermine rainfall threshold value.
7. the landslide Critical Rainfall Threshold according to claim 6 based on method of fuzzy cluster analysis, its feature It is, Transitive Closure Method is specially:
A) cluster sample is divided into a classes according to one, obtains fuzzy similarity matrix R transitive closure, calculateUntil meeting R2n=Rn, at this moment fuzzy matrix Rn is one fuzzy etc. Valency matrix, note will
B) clustered by the orders of parameter γ from big to small, willIt is arranged in order in sequence, γ=1 conduct is initial, according to Order from big to small alongTakeObtain withCorresponding γ-interceptWhen element is equal to 1, represent to divide Two corresponding samples or variable belong to a class, and corresponding is classified as into equivalence class respectively;
C) γ values constantly reduce, and are analogized downwards by aforesaid way and obtain more merging, if When, whole variables (or sample) are classified as a major class U, now γ=b stops cluster, are a classes by equivalence class in cluster process γ values be defined as γi
D) γ=γiWhen, corresponding classification situation is considered as cluster result, the critical hour produced to all classes and minute rain Amount threshold trait is analyzed:
A1, a2 represent the classification I of clustering factor, II class, a respectively31, a32Respectively represent the IIIth class first factor and second The factor, a1 '=0.89, a2 '=0.82 represents the coefficient of I, II classification respectively.
8. the landslide Critical Rainfall Threshold according to claim 6 based on method of fuzzy cluster analysis, its feature It is, Direct Cluster Analysis is specially:
If a) γ1=1, to each xiMake similar class [xi]R
[xi]R={ xj|rij=1 } (15)
Represent in rijUnder conditions of 1, x is obtainediWith xjBelong to a class, as Similarity Class.Equivalence class and Similarity Class are distinguished, etc. Common element is not present in valency class, it is as follows:
At this moment need to merge the Similarity Class in all common elements, so as to obtain γ in level1=1 all equivalence classifications;
If b) γ2Second largest value is represented, γ is searched in R2The all elements of similarity degree, are expressed as (xi,xj) element pair or rij2, with γ1=1 corresponding equivalence classification, merges xiAffiliated class and xjClass belonging to all, merges after above-mentioned whole states, γ2 Obtained value is represented, is equivalence classification;
If c) γ3Value is the third-largest value, is searched and γ in R3Similarity identical element pair, is expressed as (xi,xj), then rij= γ3Merge and γ2The x of corresponding all equivalence classesjAffiliated class and xiAffiliated class, merges after above-mentioned whole states, the γ of acquisition3For Equivalence classification;
D) analogized downwards by aforesaid way, until all classes are merged into a class U, now γ=b stops cluster, by cluster process Middle equivalence class is defined as γ for the γ values of a classesi
E) γ=γiWhen, corresponding classification situation is considered as cluster result, the critical hour produced to all classes and minute rain Amount threshold trait is analyzed:
A1, a2 represent the classification I of clustering factor, II class, a respectively31, a32Respectively represent the IIIth class first factor and second The factor, a1 '=0.89, a2 '=0.82 represents the coefficient of I, II classification respectively.
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CN115170820A (en) * 2022-05-13 2022-10-11 中铁西北科学研究院有限公司 Feature extraction and boundary identification method applied to data curve transition stage
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CN111581793A (en) * 2020-04-26 2020-08-25 中国人民解放军海军航空大学青岛校区 Airplane structure partitioning method based on actually measured environmental data
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