CN102662172A - Stormy cloud cluster extrapolation method based on Doppler radar reflectivity image - Google Patents

Stormy cloud cluster extrapolation method based on Doppler radar reflectivity image Download PDF

Info

Publication number
CN102662172A
CN102662172A CN2012100882563A CN201210088256A CN102662172A CN 102662172 A CN102662172 A CN 102662172A CN 2012100882563 A CN2012100882563 A CN 2012100882563A CN 201210088256 A CN201210088256 A CN 201210088256A CN 102662172 A CN102662172 A CN 102662172A
Authority
CN
China
Prior art keywords
extrapolation
barycenter
cloud cluster
pocket
image
Prior art date
Legal status (The legal status is an assumption and is not a legal conclusion. Google has not performed a legal analysis and makes no representation as to the accuracy of the status listed.)
Pending
Application number
CN2012100882563A
Other languages
Chinese (zh)
Inventor
王萍
王龙
刘畅
刘恒
Current Assignee (The listed assignees may be inaccurate. Google has not performed a legal analysis and makes no representation or warranty as to the accuracy of the list.)
Tianjin University
Original Assignee
Tianjin University
Priority date (The priority date is an assumption and is not a legal conclusion. Google has not performed a legal analysis and makes no representation as to the accuracy of the date listed.)
Filing date
Publication date
Application filed by Tianjin University filed Critical Tianjin University
Priority to CN2012100882563A priority Critical patent/CN102662172A/en
Publication of CN102662172A publication Critical patent/CN102662172A/en
Pending legal-status Critical Current

Links

Images

Classifications

    • YGENERAL TAGGING OF NEW TECHNOLOGICAL DEVELOPMENTS; GENERAL TAGGING OF CROSS-SECTIONAL TECHNOLOGIES SPANNING OVER SEVERAL SECTIONS OF THE IPC; TECHNICAL SUBJECTS COVERED BY FORMER USPC CROSS-REFERENCE ART COLLECTIONS [XRACs] AND DIGESTS
    • Y02TECHNOLOGIES OR APPLICATIONS FOR MITIGATION OR ADAPTATION AGAINST CLIMATE CHANGE
    • Y02ATECHNOLOGIES FOR ADAPTATION TO CLIMATE CHANGE
    • Y02A90/00Technologies having an indirect contribution to adaptation to climate change
    • Y02A90/10Information and communication technologies [ICT] supporting adaptation to climate change, e.g. for weather forecasting or climate simulation

Landscapes

  • Radar Systems Or Details Thereof (AREA)

Abstract

The invention discloses a stormy cloud cluster extrapolation method based on a Doppler radar reflectivity image. Doppler radar reflectivity images at current time and at previous time are divided into seven layers respectively according to different reflectivity thresholds to form seven monochrome images; blocking processing is carried out on each of the monochrome images and thus the complex cloud cluster is decomposed into small block regions and large block regions; extrapolation results of all the regions at future time are respectively obtained; combination is carried out on the extrapolation results of all the regions in terms of layers so as to obtain a complete extrapolation imaged based on layers; by taking an extrapolation result of layer with a threshold of 25dBz as a base, extrapolation images of layers with higher thresholds are successively utilized to cover extrapolation images of layers with lower thresholds and at last, a region that has extremely high reflectivity and has an area less than 50 units is used for final coverage, so that an extrapolation image of the stormy cloud cluster is obtained. The experiments proves that the stormy cloud cluster that is extrapolated by the method is capable of embodying important information about the structure and the form, so that an extrapolation coincidence rate of a typical stormy cloud cluster is obviously higher than those in other existing methods.

Description

A kind of Extrapolation method of the storm cloud cluster based on the radar Doppler albedo image
Technical field
The present invention relates to meteorological field, particularly a kind of Extrapolation method of the storm cloud cluster based on radar Doppler.
Background technology
Human after getting into for 20th century, through obtaining the tracking of storm cloud cluster, the achievement in research of discerning and forecasting automatically based on the albedo image of Doppler radar.Become one type of popular and method easily based on the cloud cluster of extrapolation technique, wherein, monomer centroid method and cross-correlation technique are to use two kinds of methods the most widely.The track algorithm TREC that Rinehart proposes the earliest derives from from cross-correlation technique; Passed through the unremitting effort of some scholars such as Li, Lai and Wang Gaili etc. afterwards again; The TREC algorithm has obtained updating and is perfect; The basic way of TREC algorithm is the related coefficient of at first calculating between the radar return image zonule of adjacent moment cloud cluster, under the maximal correlation condition, obtains the mobile vector of each local cloud cluster echo, and then carries out outside forecast; Another kind of monomer centroid method is from being suggested so far; Same constantly perfect and development through numerous scholars; Present widely used TITAN and SCIT algorithm have been proposed; The basic way of these two kinds of algorithms is to identify on the storm monomer basis of (only containing a nuclear district), carries out the monomer coupling of adjacent moment, and through the adjacent matching result of carving is for a long time extrapolated.
The step that the TREC algorithm is followed the trail of the storm monomer is: go on foot the storm monomer that identifies through last one; Calculate the centroid position of two groups of cloud clusters of adjacent moment; Utilize maximal rate to control; Adopt maximum correlation coefficient to confirm the mobile vector of adjacent moment cloud cluster, predict the following centroid position constantly of corresponding monomer through the mobile vector that obtains.
The TITAN algorithm is followed the tracks of the barycenter of meteorological cloud cluster through the combinatorial optimization algorithm, describes the division and the merging of meteorological cloud cluster through geometric processing.The core concept of this algorithm is: similitude and distance based on meteorological cloud cluster current time are matched, and the similitude of cloud cluster is high more, and the distance of cloud cluster is more preferentially matched at a distance of near more.
The SCIT algorithm comprises three parts: cloud cluster identification, form coupling and position prediction.Will do matching treatment to it after having discerned cloud cluster: be the basis with the current time; Seek the corresponding with it cloud cluster of previous moment; Seek its track; On the basis of working in front, utilize the current motion vector of " historical position " match cloud cluster, this motion vector is used to do the following center of mass motion track constantly of cloud cluster.
The inventor is in realizing process of the present invention; Not enough below finding to exist at least in the prior art: the radar Doppler albedo image of strong convective weathers such as the hail in the meteorology, wind spout and heavy rain is the equal important information of carrier on inner structure and formalness, and these information can help the type of people's discrimination storm cloud cluster and storm cloud cluster.And existing extrapolation technique stresses is the extrapolation of cloud cluster position, in the knot fruit, the information of cloud cluster structure and cloud cluster form exactly can not be provided outside.
Summary of the invention
The invention provides a kind of storm cloud cluster Extrapolation method based on the radar Doppler albedo image; The present invention is on the basis of cloud cluster position extrapolation; The important form and the structural information of storm cloud cluster of extrapolation can be provided; Enriched the useful and important forecast information of extrapolation cloud cluster, filled up a blank can not releasing the storm cloud cluster that has structure and shape information outward, seen hereinafter for details and describe:
A kind of Extrapolation method of the storm cloud cluster based on the radar Doppler albedo image said method comprising the steps of:
(1) storm cloud cluster radar Doppler albedo image is carried out layering and decompose, obtain 7 monochromatic subimages of storm cloud cluster based on the different reflectivity threshold value;
(2) each Zhang Danse subimage of storm cloud cluster is carried out piecemeal and handle that to be decomposed into pocket regional with bulk; Wherein, with area in the storm cloud cluster less than 10 4Regional area be defined as said pocket; With area more than or equal to 10 4Regional area be defined as said bulk zone;
(3) adopt the linear extrapolation revised law to obtain the extrapolation result of said pocket and said bulk zone barycenter;
(4) according to the extrapolation result of said pocket barycenter, each said pocket is adopted the form extrapolation method based on scattering model, obtain the extrapolation result of said pocket local configuration;
(5) according to the extrapolation result of said bulk zone barycenter, the local fan-shaped edge to each said bulk zone adopts the form extrapolation method based on mathematical morphology, obtains the extrapolation result of said bulk Regional Bureau contouring;
(6) the extrapolation result to the extrapolation result of every layer said pocket local configuration and said bulk Regional Bureau contouring merges, and obtains the integral body extrapolation image of each monochromatic subimage;
(7) be that the integral body extrapolation result of the monochromatic subimage of 25dBz is substrate with the reflectivity threshold value; With the integral body extrapolation result of the monochromatic subimage of high reflectance threshold value the integral body extrapolation result of the monochromatic subimage of antiradar reflectivity threshold value is covered successively; Again high reflectivity regions is finally covered, obtain the extrapolation image of storm cloud cluster in the radar Doppler albedo image; Wherein, smaller or equal to 50 units, the reflectivity threshold value is defined as high reflectivity regions greater than the reflectivity regions of 55dBz with area;
(8) next one is regarded as current time constantly, repeats the step of (1) to (7), realize lasting extrapolation, obtain the extrapolation image of storm cloud cluster in the farther moment to the storm cloud cluster.
Saidly storm cloud cluster radar Doppler albedo image is carried out layering decompose and to be specially:
To current time t iWith previous moment t I-1The radar Doppler albedo image of storm cloud cluster is divided into 7 figure layers according to different reflectivity threshold values respectively, i figure layer T RiGenerative process following, if storm cloud cluster zone in reflectance value f T (p)>=R iDBz then makes it at T RiIn value f Tt (p)=R iDBz, otherwise make f Tt (p)Be background colour, wherein R i=25,30,35,40,45,50,55dBz.
Said each Zhang Danse subimage to the storm cloud cluster carries out piecemeal to be handled and to be decomposed into pocket and the bulk zone is specially:
(1) from the barycenter O of monochromatic subimage to border injection line;
(2) be that step-length rotates counterclockwise ray with 1 °, when ray and at least 3 intersection points of image outline formation, note first intersection point A of this ray and image outline;
(3) in the B point, AB is divided into two image to reverse extending AO intersection graph with line segment as profile, obtains two sub regions;
(4) for each subregion, repeat (1) to (3) process, until ray and profile intersection point situation no longer occurring greater than 1, with area less than 10 4Subregion as said pocket; With area more than or equal to 10 4Subregion as said bulk zone, piecemeal is finished dealing with.
The extrapolation result that said employing linear extrapolation revised law obtains said pocket and said bulk zone barycenter is specially:
If current time is t i, through t I-2Barycenter and t constantly I-1Barycenter linear extrapolation constantly obtains t iExtrapolation barycenter constantly calculates t iExtrapolation barycenter constantly is a displacement vector with said offset tag, through t to the side-play amount of ti actual barycenter constantly I-1The moment and t iBarycenter linear extrapolation constantly obtains t I+1Centroid position constantly, through said displacement vector to said t I+1Centroid position is constantly revised.
Said extrapolation result according to said pocket barycenter adopts the form extrapolation method based on scattering model to each said pocket, and the extrapolation result who obtains said pocket local configuration is specially:
1) evenly scatters 24 rays from the pocket barycenter, form 24 intersection points with the pocket border;
2) move previous moment pocket F I-1Up to barycenter and current time pocket F iBarycenter overlap;
3) with said t I+1Barycenter is as F constantly I+1Barycenter, establish F I-1And F iWith ray l i(i=1 ..., 4 (n t-1) intersection point) is
Figure BDA0000148424130000041
With
Figure BDA0000148424130000042
For all intersection points of falling on the current monochromatic subimage profile, calculate
Figure BDA0000148424130000043
Intersection point for falling on the Region Segmentation line makes Δ i=0 push away pocket at t I+14 (n constantly t-1) individual frontier point p Fl i ( t i + 1 ) = p Fl i ( t i ) + Δ i ;
4) with 4 (n t-1) individual frontier point
Figure BDA0000148424130000045
Connect into polygon as angle point, and polygon is carried out pixel fill, obtain the extrapolation image F of pocket I+1
5) move extrapolation image F I+1Up to barycenter and said t I+1Extrapolation barycenter constantly overlaps.
Said extrapolation result according to said bulk zone barycenter, the local fan-shaped edge to each said bulk zone adopts the form extrapolation method based on mathematical morphology, obtains the extrapolation result of said bulk Regional Bureau contouring;
1) moves previous moment bulk zone F I-1Up to barycenter p c(t I-1) and current time bulk zone F iBarycenter p c(t i) overlap;
2) stretching, extension or retraction zone are detected;
If the bulk cloud cluster of adjacent moment zone G I-1And G iFrontier point set be respectively P B1={ p B1And P (i) } B2={ p B2(i) }; Make that bulk regional background point value is 0, the object-point value is 1, by G I-1And G iComposograph G ' makes each pixel value of G ':
f ′ ( p i ) = f t i ( p i ) - f t i - 1 ( p i ) = 1 0 - 1
Definition f ' (p iThe point p of)=1 iFor stretching point, f ' (p iThe point p of)=-1 iBe retraction point, f ' (p iThe point p of)=0 iBe invariant point, stretching, extension point and retraction Vertex Coloring with image obtain stretching area S Ext, retraction district S RetAnd constant region S Inv
3) sector region is divided;
(1) search is stretched or the regional critical point set
Figure BDA0000148424130000047
that bounces back
To p B1(i) ∈ P B1And p B2(i) ∈ P B2, if p B1(i) ∈ P B2Set up, then p B1(i) ∈ P lIf p B2(i) ∈ P B1Set up, then p B2(i) ∈ P l
(2) from barycenter p cObtain a plurality of sector region AS to each critical point line i, i=1,2 ..., each sector region comprises a stretching area or a retraction district, and the sector region that will comprise the stretching area is defined as and stretches the fan section, and the sector region that will comprise the retraction district is defined as the retraction fan section;
4) corrosion expansion process;
Each is stretched fan section AS iCarry out differential expansion and handle, to each retraction fan section AS iCarrying out local corrosion handles;
(1) to said stretching, extension fan section AS iTwo ray limits make to forbid marks for treatment;
(2) read expansion or corrosion information through dye marker;
(3) to said stretching area S ExtAverage the calculating of span, to said retraction district S RetAverage the calculating of amount of recovery;
If S iFor detected certain stretching area or retraction district, if satisfy pixel (p ∈ S i) ∩ (p ∈ P B1) count and be N 1, satisfy (p ∈ S i) ∩ (p ∈ P B2) count and be N 2, satisfy p ∈ S iCount and be N, then region S iAverage span or amount of contraction D be:
D = N 0.5 ( N 1 + N 2 )
In the formula, denominator is a region S iThe outer edge average length;
(4) use yardstick as the circular configuration element of d to retraction sector region corrosion n time, to stretching, extension sector region expansion n time, obtain a plurality of new sector region AS ' i, wherein
d = D , D ≤ 2 2 , D > 2 n = int ( D 2 + 0.5 )
In the formula, int representes rounding operation;
5) zone is synthetic;
To a plurality of new sector region AS ' iWith all constant region S InvCarry out cup, splice by original relative position with the zone that remains unchanged in the zone that is about to handle, and obtains G iExtrapolation image G I+1
6) displacement;
Move image G I+1Up to barycenter and said t I+1Extrapolation barycenter constantly overlaps.
The beneficial effect of technical scheme provided by the invention is: this method is from the level formation characteristics of storm cloud cluster; Through being deep into the internal layer of cloud cluster; Utilization is based on the form Extrapolation method of scattering model with based on the form Extrapolation method of mathematical morphology; The preference policy and the subimage synthetic schemes that cooperate two kinds of methods; Realized keeping the extrapolation of detailed information such as the inner precipitation particles distribution of storm cloud cluster and each layer of cloud cluster border motif information; Filled up a blank can not releasing the storm cloud cluster that has structure and shape information outward, the method can adapt to objective differentiation phenomenons such as the division of storm cloud cluster, merging simultaneously, is of value to the forecast accuracy of strengthening the storm cloud cluster.
Description of drawings
Fig. 1 is the process flow diagram of a kind of storm cloud cluster Extrapolation method based on the radar Doppler albedo image provided by the invention;
Fig. 2 is the layering decomposing schematic representation of storm cloud cluster provided by the invention;
Fig. 3 is that the piecemeal of storm cloud cluster layered image provided by the invention is handled synoptic diagram;
Fig. 4-1, Fig. 4-2, Fig. 4-3 and Fig. 4-4 are the linear extrapolation revised law synoptic diagram of regional barycenter provided by the invention;
Fig. 5 is a scattering form Extrapolation method principle schematic provided by the invention;
Fig. 6 is the pocket extrapolation exemplary plot based on scattering model provided by the invention;
Fig. 7 is the form extrapolation method principle schematic of mathematical morphology provided by the invention;
Fig. 8 is the big zone extrapolation exemplary plot of the form extrapolation method based on mathematical morphology provided by the invention;
Fig. 9 is the synoptic diagram of 6 minutes test sample of extrapolation provided by the invention;
Figure 10 is the synoptic diagram of 6~18 minutes test sample of extrapolation provided by the invention.
Embodiment
For making the object of the invention, technical scheme and advantage clearer, embodiment of the present invention is done to describe in detail further below in conjunction with accompanying drawing.
The problem that people more are concerned about with regard to forecast is how on the radar Doppler image, accurately to predict moving and variation tendency of strong convection monomer cloud cluster; Problem comprises the cloud cluster processing of different appearance profiles, the centroid position in cloud cluster moment from the current time to the future and appearance profile evolutionary process etc.Small and Medium Sized diastrous weathers such as hail, hurricane line, wind spout and thunderstorm have take place to develop fast, move rapidly unusual and characteristics such as destructive power is huge; Wanting it is analyzed exactly and predicts is the difficult point problem that needs to be resolved hurrily in the weather forecast, also is simultaneously the problem that presses for solution in the diastrous weather prediction.In order to improve the accuracy of cloud cluster extrapolation, reduce rate of false alarm, the embodiment of the invention provides a kind of storm cloud cluster Extrapolation method based on radar Doppler, referring to Fig. 1, sees hereinafter for details and describes:
101: on the basis that utilizes the storm recognition technology, the albedo image of storm cloud cluster radar Doppler albedo image is carried out layering decompose, obtain 7 monochromatic subimages of storm cloud cluster, be i.e. 7 of the storm cloud cluster figure layers based on the different reflectivity threshold value;
Wherein, this step is specially:
Referring to Fig. 2,16 kinds of pseudo-colourss in the radar Doppler albedo image respectively with black background, 5dBZ, 10dBZ ..., the reflectivity intensity of 65dBZ is corresponding.And the outermost layer reflectivity intensity of storm cloud cluster is generally always greater than 25dBZ; And ecto-entad reflectivity intensity is elevated to more than the 55dBZ step by step; Area is corresponding to be reduced step by step; So this method is visualized as the two dimensional image of cloud cluster on the zone that the outer boundary by the 25dBz zone surrounds and constantly is superimposed with the more result of high reflectivity regions, forms 7 layers of branch layered scheme.To i figure layer, the reflectance value of subject area is " also " less than the zone of threshold value Ri of background area originally and reflectance value more than or equal to threshold value Ri, background area, and therefore, each figure layer all is a monochrome image.To any figure layer T Ri, if value is R iConnected domain area S≤50 of dBz are then with the direct result as extrapolation of this connected domain.Wherein, each figure layer T of storm cloud cluster RiThe generation method following:
To current time t iWith previous moment t I-1The radar Doppler albedo image of storm cloud cluster is divided into 7 figure layers according to different reflectivity threshold values respectively, at i figure layer T RiIn, if the reflectance value f in the storm cloud cluster zone T (p)>=R iDBz then makes it at T RiIn value f Tt (p)=R iDBz, otherwise make f Tt (p)Be background colour, wherein R i=25,30,35,40,45,50,55dBz.
102: each Zhang Danse subimage of storm cloud cluster is carried out piecemeal handle that to be decomposed into pocket regional with bulk;
With area in the storm cloud cluster less than 10 4Regional area be defined as pocket, area more than or equal to 10 4Regional area be defined as the bulk zone.
Wherein, this step is specially:
(1) from the barycenter O of monochromatic subimage to border injection line;
(2) be that step-length rotates counterclockwise ray with 1 °, when ray and at least 3 intersection points of image outline formation, note first intersection point A of this ray and image outline;
(3) in the B point, AB is divided into two image to reverse extending AO intersection graph with line segment as profile, obtains two sub regions;
(4) for each subregion, repeat (1) to (3) process, until ray and profile intersection point situation no longer occurring greater than 1, with area less than 10 4Subregion as pocket; With area more than or equal to 10 4Subregion as bulk zone, piecemeal is finished dealing with.
Referring to Fig. 3, establishing fine line is the exact shape profile of cloud cluster, O 1The barycenter of cloud cluster for this reason, ray O 1A is that article one and profile intersection point become a plurality of rays by one, notes the A point, reverse extending AO 1, meeting at B with profile, AB is divided into 2 to cloud cluster, wherein S 1All barycenter scattered rays all only and S 1Profile has an intersection point, need not divide again.Another piece then also will continue to be divided into 2 parts could satisfy all barycenter scattered rays all only have an intersection point with its profile condition, so this cloud cluster has been divided into S 1, S 2, S 3Three zones.Every zone is all surrounded by monochromatic subimage profile and Region Segmentation line.
103: adopt the linear extrapolation revised law to obtain the extrapolation result of pocket and bulk zone barycenter;
Wherein, this step is specially:
If current time is t i, through t I-2Barycenter and t constantly I-1Barycenter linear extrapolation constantly obtains t iExtrapolation barycenter constantly calculates t iExtrapolation barycenter constantly is to t iThe side-play amount of actual barycenter constantly is a displacement vector with offset tag, through t I-1The moment and t iBarycenter linear extrapolation constantly obtains t I+1Centroid position constantly, through displacement vector to t I+1Centroid position is constantly revised.
Referring to Fig. 4, the solid-line curve among Fig. 4-1,4-2 and the 4-3 is represented the profile that the storm cloud cluster is actual, and some D, some A and some B are their barycenter,
Figure BDA0000148424130000081
Be at t I-1Constantly push away moment t iThe displacement of barycenter A, the C point is t iThe physical location of moment cloud cluster barycenter,
Figure BDA0000148424130000082
Be the displacement vector of the reality of barycenter A, and
Figure BDA0000148424130000083
Be predicated error, will
Figure BDA0000148424130000084
As the amount of correcting of linear extrapolation to t I+1Predicting the outcome constantly revised.Fig. 4-4 has provided two kinds of barycenter extrapolation signals, and some O is the linear extrapolation result of barycenter C, and some R is the extrapolation result through revising on the basis of linear extrapolation, and correction is exactly at t iThe predicated error that obtains constantly, i.e. t iCloud cluster barycenter C is to t constantly I+1Displacement constantly CR → = CO → + OR → , Wherein, CO → = AC → , OR → = BC → .
104: according to the extrapolation result of pocket barycenter, each pocket is adopted the form extrapolation method based on scattering model, obtain the extrapolation result of pocket local configuration;
Wherein, this step is specially:
1) evenly scatters 24 rays from the pocket barycenter, form 24 intersection points with the pocket border;
2) move previous moment pocket F I-1Up to barycenter and current time pocket F iBarycenter overlap;
3) with t I+1Barycenter is as F constantly I+1Barycenter, establish F I-1And F iWith ray l i(i=1 ..., 4 (n t-1) intersection point) is
Figure BDA0000148424130000087
With For all intersection points of falling on the current monochromatic subimage profile, calculate
Figure BDA0000148424130000089
Intersection point for falling on the Region Segmentation line makes Δ i=0 push away pocket at t I+14 (n constantly t-1) individual frontier point p Fl i ( t i + 1 ) = p Fl i ( t i ) + Δ i ;
4) with 4 (n t-1) individual frontier point
Figure BDA00001484241300000811
Connect into polygon as angle point, and polygon is carried out pixel fill, obtain the extrapolation image F of pocket I+1
5) move extrapolation image F I+1Up to barycenter and t I+1Extrapolation barycenter constantly overlaps.
Referring to Fig. 5, thicker solid line (t I+1Constantly) be utilize other 2 than fine line (t I-1The moment and t iConstantly) according to the above-mentioned pocket profile that obtains based on the form extrapolation method of scattering model at (t constantly in future I+1Extrapolation result constantly).
It is generally acknowledged that the area of storm cloud cluster nucleus on the radar Doppler reflectance map is not less than 50 pixels (pixel is apart from being 1km), therefore gets scattering model parameter n t=7, number of rays then is 24.For the less cloud cluster of area; Through 24 rays are linked to each other as angle point with 24 intersection points of region contour successively; Can satisfy the appearance profile of sketching the contours of small size zone under the condition of certain precision, and for the bigger cloud cluster of area, can be very coarse through the extrapolation profile that connects the zone that 24 angle points obtaining through scattering model obtain successively; Tracing it to its cause is the increase along with region area; The distance of adjacent point-to-point transmission increases in 24 angle points, and for the large area region of band shape, each angle point has very big range difference to the distance of regional barycenter; These range differences are difficult to satisfy precision of prediction and couple together the point on an one magnitude not simply not on an one magnitude.Obviously, extrapolate and to become coarse along with the increase of cloud cluster area, so this method is suitable for the form extrapolation of pocket based on the cloud cluster form of scattering model.
Referring to Fig. 6, wherein, figure a, figure b, figure c are respectively certain cloudling group zone in t I-2T constantly, I-1The moment and t iThis cloud cluster zone that real image constantly, figure d obtain for the form extrapolation method based on scattering model is at t iExtrapolation image constantly; Can find out; Behind the enforcement scattering model of the less zone of area (figure Smalt zone); Region contour predict the outcome with actual conditions at form form basically identical, come the following form of prediction area so can utilize than the zonule based on the form extrapolation method of scattering model.
105: according to the extrapolation result of bulk zone barycenter, the local fan-shaped edge to each bulk zone adopts the form extrapolation method based on mathematical morphology, obtains the extrapolation result of bulk Regional Bureau contouring;
Wherein, this step is specially:
1) moves previous moment bulk zone F I-1Up to barycenter p c(t I-1) and current time bulk zone F iBarycenter p c(t i) overlap;
2) stretching, extension or retraction zone are detected;
If the bulk cloud cluster of adjacent moment zone G I-1And G iFrontier point set be respectively P B1={ p B1And P (i) } B2={ p B2(i) }; Make that bulk regional background point value is 0, the object-point value is 1, by G I-1And G iComposograph G ' makes each pixel value of G ':
f ′ ( p i ) = f t i ( p i ) - f t i - 1 ( p i ) = 1 0 - 1
Definition f ' (p iThe point p of)=1 iFor stretching point, f ' (p iThe point p of)=-1 iBe retraction point, f ' (p iThe point p of)=0 iBe invariant point, stretching, extension point and retraction Vertex Coloring with image obtain stretching area S Ext, retraction district S RetAnd constant region S Inv
3) sector region is divided;
(1) search is stretched or the regional critical point set
Figure BDA0000148424130000101
that bounces back
To p B1(i) ∈ P B1And p B2(i) ∈ P B2, if p B1(i) ∈ P B2Set up, then p B1(i) ∈ P lIf p B2(i) ∈ P B1Set up, then p B2(i) ∈ P l
(2) from barycenter p cObtain a plurality of sector region AS to each critical point line i, i=1,2 ..., each sector region comprises sector region that a stretching area or one retraction district will comprise the stretching area and is defined as and stretches the fan section, and the sector region that will comprise the retraction district is defined as the retraction fan section;
4) corrosion expansion process;
Each is stretched fan section AS iCarry out differential expansion and handle, to each retraction fan section AS iCarrying out local corrosion handles;
(1) to stretching fan section AS iTwo ray limits make to forbid marks for treatment;
(2) read expansion or corrosion information through dye marker;
(3) to stretching area S ExtAverage the calculating of span, to retraction district S RetAverage the calculating of amount of recovery;
If S iFor detected certain stretching area or retraction district, if satisfy pixel (p ∈ S i) ∩ (p ∈ P B1) count and be N 1, satisfy (p ∈ S i) ∩ (p ∈ P B2) count and be N 2, satisfy p ∈ S iCount and be N, then region S iAverage span or amount of contraction D be:
D = N 0.5 ( N 1 + N 2 )
In the formula, denominator is a region S iThe outer edge average length;
(4) use yardstick as the circular configuration element of d to retraction sector region corrosion n time, to stretching, extension sector region expansion n time, obtain a plurality of new sector region AS ' i, wherein
d = D , D ≤ 2 2 , D > 2 n = int ( D 2 + 0.5 )
In the formula, int representes rounding operation;
5) zone is synthetic;
To a plurality of new sector region AS ' iWith all constant region S InvCarry out cup, splice by original relative position with the zone that remains unchanged in the zone that is about to handle, and obtains G iExtrapolation image G I+1
6) displacement;
Move image G I+1Up to barycenter and said t I+1Extrapolation barycenter constantly overlaps.
Referring to Fig. 7, F T1And F T2Represent the real image of certain cloud cluster zone, move F in two adjacent moment T1Their barycenter is overlapped, obtain containing the F of stretching area, retraction district, constant region T12, wherein, the fan section that has the linear shadow district is " stretching, extension fan section ", and the fan section that has solid shaded is " retraction fan section ", and the sector region of losing the border is a constant region.
Referring to Fig. 8, wherein, figure a, figure b, figure c are respectively certain big cloud cluster zone in t I-2T constantly, I-1The moment and t iThis cloud cluster zone that real image constantly, figure d obtain for the form extrapolation method based on mathematical morphology is at t iExtrapolation image constantly can be found out, figure d is higher to the form degree of fitting of figure c.For area bigger bulk cloud cluster zone, particularly bulk belt-like zone, be suitable for the contour prediction in bulk cloud cluster zone based on the form extrapolation method of mathematical morphology.
Wherein, the embodiment of the invention does not limit the execution sequence of step 104 and step 105.
106: the extrapolation result of every layer pocket local configuration and the extrapolation result of bulk Regional Bureau contouring are merged, obtain the integral body extrapolation result of each monochromatic subimage;
107: with the reflectivity threshold value is that the integral body extrapolation result of the monochromatic subimage of 25dBz is substrate; With the integral body extrapolation result of the monochromatic subimage of high reflectance threshold value the integral body extrapolation result of the monochromatic subimage of antiradar reflectivity threshold value is covered successively; High reflectivity regions is finally covered, obtain the extrapolation image of storm cloud cluster in the radar Doppler albedo image;
Wherein, smaller or equal to 50 units, the reflectivity threshold value is defined as high reflectivity regions greater than the reflectivity regions of 55dBz with area.
108: the next one is regarded as current time constantly, and repeating step 101-step 107 realizes the lasting extrapolation to the storm cloud cluster, obtains the extrapolation image of storm cloud cluster in the farther moment.
Wherein, utilizing the time interval is two real image T of 6 minutes I-1And T iOrganize the scheme of laddering lasting extrapolation to be: to use T I-1And T iRelease is apart from T iImage T after 6 minutes I+1, use T iAnd T I+1Release is apart from T I+1Image T after 6 minutes I+2, by that analogy.
The feasibility of a kind of storm cloud cluster Extrapolation method based on radar Doppler of verifying that the embodiment of the invention provides with a concrete test below, see hereinafter for details and describe:
With the radar base data is data source, gets 100 albedo images that are multinuclear band shape, multinuclear bulk and each two storm process of monokaryon bulk and makees sample, this method is tested, and make similarity assessment, and evaluation index designs as follows.
If t 3The true picture of cloud cluster is F (t constantly 3), the extrapolation image is F 12(t 3), their nuclear district area is respectively S h(t 3) and S h 12(t 3), the region area when descending successively from examining district's beginning intensity is respectively S 50(t 3), S 45(t 3) ..., S 25(t 3) and S 50 12(t 3), S 45 12(t 3) ..., S 25 12(t 3), note by abridging and be S 6, S 5..., S 1And S 6 12, S 5 12..., S 1 12
(1) nuclear district area similarity
ρ 1 = min { S h ( t 3 ) , S h 12 ( t 3 ) } max { S h ( t 3 ) , S h 12 ( t 3 ) }
(2) cloud cluster area similarity
ρ 2 = 1 n Σ i = 1 n min { S i , S i 12 } max { S i , S i 12 } , n ≤ 6
Be positioned at F simultaneously if satisfy the some p of strength condition " R (p)>=i " 12With the quantity among the F be n i, only be positioned at F 12Or the quantity among the F is n ' i, then
(3) high intensity region shape similarity
ρ 3 = Σ i = 40,45,50 , ≥ 55 dbz n i n i + n i ′
(4) hypo-intense regions shape similarity
ρ 4 = Σ i = 25,30,35 dbz n i n i + n i ′
(5) comprehensive similarity
With ρ i, i=1 ..., 4 carry out weighted sum, the comprehensive similarity ρ of the cloud cluster that obtains extrapolating:
ρ = Σ i = 1 4 k i ρ i , Σ i = 1 4 k i = 1
Consider that the availability of the high reflectivity region domain information of storm cloud cluster always is better than the information availability of low reflectivity regions, gets k={k especially 1, k 2, k 3, k 4}={ 0.4,0.2,0.3,0.1}.
Referring to Fig. 9; It has provided the test sample of extrapolating 6 minutes, wherein, and with regard to the zone of 35dBz; The sub-yellow area of figure (a) upside develops into figure (c) and constantly with the below yellow area merging has taken place; With regard to the zone of 50dBz, figure red subregion in the middle of (c) again from figure (a) constantly the below red area split off, the division in above-mentioned this cloud cluster zone be incorporated in 6 minutes and all obtained reflection more accurately among the extrapolation figure.
Referring to Figure 10, this is the test sample that another one was extrapolated 6~18 minutes preferably.Table 1 has provided the comprehensive assessment result based on extrapolation in 6 minutes of test sample book, and table 2 is based on extrapolations in 6~18 minutes of test sample book and assesses the table of comparisons and average operating time thereof.
The evaluation index of table 1 pair extrapolation in 6 minutes
Figure BDA0000148424130000131
The evaluation index of table 2 pair extrapolation in 6~18 minutes
The extrapolation time 6min 12min 18min
Average similarity 0.94 0.90 0.81
Average operating time 870ms 1.51s 2.43s
With regard to test sample book, the average similarity of its 6 minutes extrapolate image and true pictures surpasses 92%, and along with the increasing of extrapolation time, average similarity decreases, but 18 minutes average similarity has been verified the feasibility of this method still greater than 80%.
In sum; The embodiment of the invention provides a kind of Extrapolation method of the storm cloud cluster based on radar Doppler; This method is on the basis of it being carried out the hierarchical block decomposition; Proposed to cooperate the preference policy and the subimage synthetic schemes of two kinds of methods, realized keeping the extrapolation of detailed information such as the inner precipitation particles distribution of storm cloud cluster and each layer of cloud cluster border motif information based on the form Extrapolation method of scattering model with based on the form Extrapolation method of mathematical morphology; Filled up the blank that outer release has the storm cloud cluster of structure and shape information, the method can adapt to objective differentiation phenomenons such as the division of storm cloud cluster, merging simultaneously; And has higher similarity through the extrapolation cloud cluster that this method obtains through experimental verification.
It will be appreciated by those skilled in the art that accompanying drawing is the synoptic diagram of a preferred embodiment, the invention described above embodiment sequence number is not represented the quality of embodiment just to description.
The above is merely preferred embodiment of the present invention, and is in order to restriction the present invention, not all within spirit of the present invention and principle, any modification of being done, is equal to replacement, improvement etc., all should be included within protection scope of the present invention.

Claims (6)

1. the Extrapolation method based on the storm cloud cluster of radar Doppler albedo image is characterized in that, said method comprising the steps of:
(1) storm cloud cluster radar Doppler albedo image is carried out layering and decompose, obtain 7 monochromatic subimages of storm cloud cluster based on the different reflectivity threshold value;
(2) each Zhang Danse subimage of storm cloud cluster is carried out piecemeal and handle that to be decomposed into pocket regional with bulk; Wherein, with area in the storm cloud cluster less than 10 4Regional area be defined as said pocket; With area more than or equal to 10 4Regional area be defined as said bulk zone;
(3) adopt the linear extrapolation revised law to obtain the extrapolation result of said pocket and said bulk zone barycenter;
(4) according to the extrapolation result of said pocket barycenter, each said pocket is adopted the form extrapolation method based on scattering model, obtain the extrapolation result of said pocket local configuration;
(5) according to the extrapolation result of said bulk zone barycenter, the local fan-shaped edge to each said bulk zone adopts the form extrapolation method based on mathematical morphology, obtains the extrapolation result of said bulk Regional Bureau contouring;
(6) the extrapolation result to the extrapolation result of every layer said pocket local configuration and said bulk Regional Bureau contouring merges, and obtains the integral body extrapolation image of each monochromatic subimage;
(7) be that the integral body extrapolation result of the monochromatic subimage of 25dBz is substrate with the reflectivity threshold value; With the integral body extrapolation result of the monochromatic subimage of high reflectance threshold value the integral body extrapolation result of the monochromatic subimage of antiradar reflectivity threshold value is covered successively; Again high reflectivity regions is finally covered, obtain the extrapolation image of storm cloud cluster in the radar Doppler albedo image; Wherein, smaller or equal to 50 units, the reflectivity threshold value is defined as high reflectivity regions greater than the reflectivity regions of 55dBz with area;
(8) next one is regarded as current time constantly, repeats the step of (1) to (7), realize lasting extrapolation, obtain the extrapolation image of storm cloud cluster in the farther moment to the storm cloud cluster.
2. the Extrapolation method of a kind of storm cloud cluster based on the radar Doppler albedo image according to claim 1 is characterized in that, saidly storm cloud cluster radar Doppler albedo image is carried out layering decomposes and is specially:
To current time t iWith previous moment t I-1The radar Doppler albedo image of storm cloud cluster is divided into 7 figure layers according to different reflectivity threshold values respectively, i figure layer T RiGenerative process following, if storm cloud cluster zone in reflectance value f T (p)>=R iDBz then makes it at T RiIn value f Tt (p)=R iDBz, otherwise make f Tt (p)Be background colour, wherein R i=25,30,35,40,45,50,55dBz.
3. the Extrapolation method of a kind of storm cloud cluster based on the radar Doppler albedo image according to claim 1 is characterized in that, said each Zhang Danse subimage to the storm cloud cluster carries out piecemeal to be handled and be decomposed into pocket and the bulk zone is specially:
(1) from the barycenter O of monochromatic subimage to border injection line;
(2) be that step-length rotates counterclockwise ray with 1 °, when ray and at least 3 intersection points of image outline formation, note first intersection point A of this ray and image outline;
(3) in the B point, AB is divided into two image to reverse extending AO intersection graph with line segment as profile, obtains two sub regions;
(4) for each subregion, repeat (1) to (3) process, until ray and profile intersection point situation no longer occurring greater than 1, with area less than 10 4Subregion as said pocket; With area more than or equal to 10 4Subregion as said bulk zone, piecemeal is finished dealing with.
4. the Extrapolation method of a kind of storm cloud cluster based on the radar Doppler albedo image according to claim 1 is characterized in that, the extrapolation result that said employing linear extrapolation revised law obtains said pocket and said bulk zone barycenter is specially:
If current time is t i, through t I-2Barycenter and t constantly I-1Barycenter linear extrapolation constantly obtains t iExtrapolation barycenter constantly calculates t iExtrapolation barycenter constantly is to t iThe side-play amount of actual barycenter constantly is a displacement vector with said offset tag, through t I-1The moment and t iBarycenter linear extrapolation constantly obtains t I+1Centroid position constantly, through said displacement vector to said t I+1Centroid position is constantly revised.
5. the Extrapolation method of a kind of storm cloud cluster based on the radar Doppler albedo image according to claim 1; It is characterized in that; Said extrapolation result according to said pocket barycenter; Each said pocket is adopted the form extrapolation method based on scattering model, and the extrapolation result who obtains said pocket local configuration is specially:
1) evenly scatters 24 rays from the pocket barycenter, form 24 intersection points with the pocket border;
2) move previous moment pocket F I-1Up to barycenter and current time pocket F iBarycenter overlap;
3) with said t I+1Barycenter is as F constantly I+1Barycenter, establish F I-1And F iWith ray l i(i=1 ..., 4 (n t-1) intersection point) is
Figure FDA0000148424120000021
With For all intersection points of falling on the current monochromatic subimage profile, calculate Intersection point for falling on the Region Segmentation line makes Δ i=0 push away pocket at t I+14 (n constantly t-1) individual frontier point p Fl i ( t i + 1 ) = p Fl i ( t i ) + Δ i ;
4) with 4 (n t-1) individual frontier point
Figure FDA0000148424120000025
Connect into polygon as angle point, and polygon is carried out pixel fill, obtain the extrapolation image F of pocket I+1
5) move extrapolation image F I+1Up to barycenter and said t I+1Extrapolation barycenter constantly overlaps.
6. the Extrapolation method of a kind of storm cloud cluster based on the radar Doppler albedo image according to claim 1; It is characterized in that; Said extrapolation result according to said bulk zone barycenter; Local fan-shaped edge to each said bulk zone adopts the form extrapolation method based on mathematical morphology, obtains the extrapolation result of said bulk Regional Bureau contouring;
1) moves previous moment bulk zone F I-1Up to barycenter p c(t I-1) and current time bulk zone F iBarycenter p c(t i) overlap;
2) stretching, extension or retraction zone are detected;
If the bulk cloud cluster of adjacent moment zone G I-1And G iFrontier point set be respectively P B1={ p B1And P (i) } B2={ p B2(i) }; Make that bulk regional background point value is 0, the object-point value is 1, by G I-1And G iComposograph G ' makes each pixel value of G ':
f ′ ( p i ) = f t i ( p i ) - f t i - 1 ( p i ) = 1 0 - 1
Definition f ' (p iThe point p of)=1 iFor stretching point, f ' (p iThe point p of)=-1 iBe retraction point, f ' (p iThe point p of)=0 iBe invariant point, stretching, extension point and retraction Vertex Coloring with image obtain stretching area S Ext, retraction district S RetAnd constant region S Inv
3) sector region is divided;
(1) search is stretched or the regional critical point set
Figure FDA0000148424120000032
that bounces back
To p B1(i) ∈ P B1And p B2(i) ∈ P B2, if p B1(i) ∈ P B2Set up, then p B1(i) ∈ P lIf p B2(i) ∈ P B1Set up, then p B2(i) ∈ P l
(2) from barycenter p cObtain a plurality of sector region AS to each critical point line i, i=1,2 ..., each sector region comprises a stretching area or a retraction district, and the sector region that will comprise the stretching area is defined as and stretches the fan section, and the sector region that will comprise the retraction district is defined as the retraction fan section;
4) corrosion expansion process;
Each is stretched fan section AS iCarry out differential expansion and handle, to each retraction fan section AS iCarrying out local corrosion handles;
(1) to said stretching, extension fan section AS iTwo ray limits make to forbid marks for treatment;
(2) read expansion or corrosion information through dye marker;
(3) to said stretching area S ExtAverage the calculating of span, to said retraction district S RetAverage the calculating of amount of recovery;
If S iFor detected certain stretching area or retraction district, if satisfy pixel (p ∈ S i) ∩ (p ∈ P B1) count and be N 1, satisfy (p ∈ S i) ∩ (p ∈ P B2) count and be N 2, satisfy p ∈ S iCount and be N, then region S iAverage span or amount of contraction D be:
D = N 0.5 ( N 1 + N 2 )
In the formula, denominator is a region S iThe outer edge average length;
(4) use yardstick as the circular configuration element of d to retraction sector region corrosion n time, to stretching, extension sector region expansion n time, obtain a plurality of new sector region AS ' i, wherein
d = D , D ≤ 2 2 , D > 2 n = int ( D 2 + 0.5 )
In the formula, int representes rounding operation;
5) zone is synthetic;
To a plurality of new sector region AS ' iWith all constant region S InvCarry out cup, splice by original relative position with the zone that remains unchanged in the zone that is about to handle, and obtains G iExtrapolation image G I+1
6) displacement;
Move image G I+1Up to barycenter and said t I+1Extrapolation barycenter constantly overlaps.
CN2012100882563A 2012-03-29 2012-03-29 Stormy cloud cluster extrapolation method based on Doppler radar reflectivity image Pending CN102662172A (en)

Priority Applications (1)

Application Number Priority Date Filing Date Title
CN2012100882563A CN102662172A (en) 2012-03-29 2012-03-29 Stormy cloud cluster extrapolation method based on Doppler radar reflectivity image

Applications Claiming Priority (1)

Application Number Priority Date Filing Date Title
CN2012100882563A CN102662172A (en) 2012-03-29 2012-03-29 Stormy cloud cluster extrapolation method based on Doppler radar reflectivity image

Publications (1)

Publication Number Publication Date
CN102662172A true CN102662172A (en) 2012-09-12

Family

ID=46771700

Family Applications (1)

Application Number Title Priority Date Filing Date
CN2012100882563A Pending CN102662172A (en) 2012-03-29 2012-03-29 Stormy cloud cluster extrapolation method based on Doppler radar reflectivity image

Country Status (1)

Country Link
CN (1) CN102662172A (en)

Cited By (15)

* Cited by examiner, † Cited by third party
Publication number Priority date Publication date Assignee Title
CN102915470A (en) * 2012-09-20 2013-02-06 中国电力科学研究院 Cloud cluster movement estimation method facing to photovoltaic power prediction
CN104237890A (en) * 2014-09-03 2014-12-24 天津大学 Recognition and forecast method for rainstorm caused by train effect
CN105023292A (en) * 2015-06-24 2015-11-04 陕西宝成航空仪表有限责任公司 Digital cloud cluster simulation and modeling method
CN105678846A (en) * 2016-02-22 2016-06-15 武汉华信联创技术工程有限公司 Three-dimensional visualization method and system for real-time meteorological networking radar data
CN105717491A (en) * 2016-02-04 2016-06-29 象辑知源(武汉)科技有限公司 Prediction method and prediction device of weather radar echo image
CN105738873A (en) * 2015-11-16 2016-07-06 象辑知源(武汉)科技有限公司 Weather radar echo image processing method and device
CN106125057A (en) * 2016-06-20 2016-11-16 安徽省气象科学研究所 A kind of radar return mobile vector field processing method
CN106526558A (en) * 2016-09-27 2017-03-22 天津大学 Gust front automatic recognition method based on Doppler weather radar data
CN107229084A (en) * 2017-06-08 2017-10-03 天津大学 A kind of automatic identification, tracks and predicts contracurrent system mesh calibration method
CN107436987A (en) * 2016-05-26 2017-12-05 江苏省气象台 A kind of thermal convection storm develops the method for building up of forecast conceptual model
CN109164450A (en) * 2018-09-12 2019-01-08 天津大学 A kind of downburst prediction technique based on Doppler Radar Data
CN110297246A (en) * 2019-07-16 2019-10-01 上海市气象信息与技术支持中心 A kind of cooperative self-adapted control method of networking X-band weather radar and system
CN112232674A (en) * 2020-10-16 2021-01-15 中国气象局气象探测中心 Meteorological disaster assessment method, device and system
CN113298808A (en) * 2021-06-22 2021-08-24 哈尔滨工程大学 Method for repairing building shielding information in tilt-oriented remote sensing image
CN114004426A (en) * 2021-12-31 2022-02-01 浙江省气象台 Dynamic adjustment method of short-time rainstorm forecast release model

Citations (6)

* Cited by examiner, † Cited by third party
Publication number Priority date Publication date Assignee Title
JPH0843545A (en) * 1994-07-27 1996-02-16 Hitachi Ltd Rainfall prediction system
EP0962890A1 (en) * 1998-06-05 1999-12-08 Thomson-Csf Process for dynamic following of the evolution of deformable structures and evolution prediction
WO2010042757A1 (en) * 2008-10-09 2010-04-15 Colorado State University Research Foundation Gaussian model adaptive processing in the time domain
CN102129566A (en) * 2011-03-09 2011-07-20 国家卫星气象中心 Method for identifying rainstorm cloud cluster based on stationary meteorological satellite
US20110234453A1 (en) * 2010-03-25 2011-09-29 Mizutani Fumihiko Weather radar apparatus and weather observation method
CN102279424A (en) * 2011-05-12 2011-12-14 福建省电力有限公司 Early warning system for power grid meteorological disaster

Patent Citations (6)

* Cited by examiner, † Cited by third party
Publication number Priority date Publication date Assignee Title
JPH0843545A (en) * 1994-07-27 1996-02-16 Hitachi Ltd Rainfall prediction system
EP0962890A1 (en) * 1998-06-05 1999-12-08 Thomson-Csf Process for dynamic following of the evolution of deformable structures and evolution prediction
WO2010042757A1 (en) * 2008-10-09 2010-04-15 Colorado State University Research Foundation Gaussian model adaptive processing in the time domain
US20110234453A1 (en) * 2010-03-25 2011-09-29 Mizutani Fumihiko Weather radar apparatus and weather observation method
CN102129566A (en) * 2011-03-09 2011-07-20 国家卫星气象中心 Method for identifying rainstorm cloud cluster based on stationary meteorological satellite
CN102279424A (en) * 2011-05-12 2011-12-14 福建省电力有限公司 Early warning system for power grid meteorological disaster

Non-Patent Citations (6)

* Cited by examiner, † Cited by third party
Title
MICHAEL DIXON等: "TITAN:Thunderstorm Identification,Tracking,Analysis,and Nowcasting-A radar-based methodology", 《JOURNAL OF ATMOSPHERIC AND OCEANIC TECHNOLOGY》, vol. 10, no. 6, 31 December 1993 (1993-12-31), pages 785 - 797 *
WANG PING等: "Study on Shape and Formation Extrapolation Algorithm for Cloud of Storm", 《2012 INTERNATIONAL WORKSHOP ON INFORMATION AND ELECTRONICS ENGINEERING》, vol. 29, 10 March 2012 (2012-03-10), pages 1856 - 1861, XP028457429, DOI: doi:10.1016/j.proeng.2012.01.226 *
兰红平等: "雷暴云团自动识别和边界相关追踪技术研究", 《气象》, vol. 35, no. 7, 31 July 2009 (2009-07-31), pages 101 - 111 *
刘恒: "强对流天气潜势信息提取及其演变预测", 《中国优秀硕士学位论文全文数据库(电子期刊)》, 31 July 2009 (2009-07-31), pages 44 - 46 *
武娜等: "基于TREC的临近预报", 《成都信息工程学院学报》, vol. 23, no. 6, 31 December 2008 (2008-12-31), pages 642 - 647 *
王敏等: "基于FY2C卫星的暴雨云团自动预警方法", 《计算机工程》, vol. 36, no. 14, 31 July 2010 (2010-07-31) *

Cited By (25)

* Cited by examiner, † Cited by third party
Publication number Priority date Publication date Assignee Title
CN102915470A (en) * 2012-09-20 2013-02-06 中国电力科学研究院 Cloud cluster movement estimation method facing to photovoltaic power prediction
CN104237890A (en) * 2014-09-03 2014-12-24 天津大学 Recognition and forecast method for rainstorm caused by train effect
CN104237890B (en) * 2014-09-03 2016-06-08 天津大学 The heavy rain identification that one is caused by " train effect " and forecasting procedure
CN105023292A (en) * 2015-06-24 2015-11-04 陕西宝成航空仪表有限责任公司 Digital cloud cluster simulation and modeling method
CN105738873A (en) * 2015-11-16 2016-07-06 象辑知源(武汉)科技有限公司 Weather radar echo image processing method and device
CN105738873B (en) * 2015-11-16 2018-05-08 象辑知源(武汉)科技有限公司 The processing method and processing unit of Weather Radar image
CN105717491B (en) * 2016-02-04 2018-09-21 象辑知源(武汉)科技有限公司 The prediction technique and prediction meanss of Weather Radar image
CN105717491A (en) * 2016-02-04 2016-06-29 象辑知源(武汉)科技有限公司 Prediction method and prediction device of weather radar echo image
CN105678846B (en) * 2016-02-22 2018-09-28 武汉华信联创技术工程有限公司 A kind of three-dimensional visualization method and system of real-time weather radar network data
CN105678846A (en) * 2016-02-22 2016-06-15 武汉华信联创技术工程有限公司 Three-dimensional visualization method and system for real-time meteorological networking radar data
CN107436987B (en) * 2016-05-26 2021-03-12 江苏省气象台 Method for establishing concept model for forecasting evolution of heat convection storm
CN107436987A (en) * 2016-05-26 2017-12-05 江苏省气象台 A kind of thermal convection storm develops the method for building up of forecast conceptual model
CN106125057A (en) * 2016-06-20 2016-11-16 安徽省气象科学研究所 A kind of radar return mobile vector field processing method
CN106125057B (en) * 2016-06-20 2018-11-02 安徽省气象科学研究所 A kind of radar return mobile vector field processing method
CN106526558A (en) * 2016-09-27 2017-03-22 天津大学 Gust front automatic recognition method based on Doppler weather radar data
CN107229084A (en) * 2017-06-08 2017-10-03 天津大学 A kind of automatic identification, tracks and predicts contracurrent system mesh calibration method
CN107229084B (en) * 2017-06-08 2019-08-27 天津大学 A kind of automatic identification tracks and predicts contracurrent system mesh calibration method
CN109164450A (en) * 2018-09-12 2019-01-08 天津大学 A kind of downburst prediction technique based on Doppler Radar Data
CN109164450B (en) * 2018-09-12 2022-11-22 天津大学 Downburst prediction method based on Doppler radar data
CN110297246A (en) * 2019-07-16 2019-10-01 上海市气象信息与技术支持中心 A kind of cooperative self-adapted control method of networking X-band weather radar and system
CN110297246B (en) * 2019-07-16 2021-04-02 上海市气象信息与技术支持中心 Networking X-waveband weather radar collaborative self-adaptive control method and system
CN112232674A (en) * 2020-10-16 2021-01-15 中国气象局气象探测中心 Meteorological disaster assessment method, device and system
CN113298808A (en) * 2021-06-22 2021-08-24 哈尔滨工程大学 Method for repairing building shielding information in tilt-oriented remote sensing image
CN113298808B (en) * 2021-06-22 2022-03-18 哈尔滨工程大学 Method for repairing building shielding information in tilt-oriented remote sensing image
CN114004426A (en) * 2021-12-31 2022-02-01 浙江省气象台 Dynamic adjustment method of short-time rainstorm forecast release model

Similar Documents

Publication Publication Date Title
CN102662172A (en) Stormy cloud cluster extrapolation method based on Doppler radar reflectivity image
CN105335966B (en) Multiscale morphology image division method based on local homogeney index
CN101800890B (en) Multiple vehicle video tracking method in expressway monitoring scene
CN108550133A (en) A kind of cancer cell detection method based on Faster R-CNN
CN103197299B (en) Extraction and quantitative analysis system of weather radar radial wind information
CN104463164B (en) It is a kind of based on umbrella frame method and crown height than trees canopy structure information extracting method
CN101419706B (en) Jersey wear flokkit and balling up grading method based on image analysis
CN101976504B (en) Multi-vehicle video tracking method based on color space information
CN102279929B (en) Remote-sensing artificial ground object identifying method based on semantic tree model of object
CN105869178A (en) Method for unsupervised segmentation of complex targets from dynamic scene based on multi-scale combination feature convex optimization
CN103198302A (en) Road detection method based on bimodal data fusion
CN111191628B (en) Remote sensing image earthquake damage building identification method based on decision tree and feature optimization
CN107330898B (en) Quantitative marking calculation method and system for vegetation vertical zone
CN108254750B (en) Down-blast intelligent identification early warning method based on radar data
CN102628944A (en) Stratus cloud and convective cloud automatic recognition method based on Doppler radar data
CN102509104A (en) Confidence map-based method for distinguishing and detecting virtual object of augmented reality scene
CN104504709A (en) Feature ball based classifying method of three-dimensional point-cloud data of outdoor scene
CN105654516A (en) Method for detecting small moving object on ground on basis of satellite image with target significance
CN102662173A (en) Thunderstorm forecasting method based on level set
CN102737542B (en) Automatic water depth annotation selection method with consideration of multi-restriction conditions
CN100555326C (en) A kind of image partition method of dimension self-adaption
CN107656278A (en) Based on dense precipitation station Quantitative Precipitation estimating and measuring method
Medhi et al. On identifying relationships between the flood scaling exponent and basin attributes
Zhang et al. Building channel networks for flat regions in digital elevation models
CN102609721B (en) Remote sensing image clustering method

Legal Events

Date Code Title Description
C06 Publication
PB01 Publication
C10 Entry into substantive examination
SE01 Entry into force of request for substantive examination
C02 Deemed withdrawal of patent application after publication (patent law 2001)
WD01 Invention patent application deemed withdrawn after publication

Application publication date: 20120912