CN108304967A - The method that rainfall-flow-water level coupling interpolation solves mountain flood Critical Rainfall - Google Patents
The method that rainfall-flow-water level coupling interpolation solves mountain flood Critical Rainfall Download PDFInfo
- Publication number
- CN108304967A CN108304967A CN201810050370.4A CN201810050370A CN108304967A CN 108304967 A CN108304967 A CN 108304967A CN 201810050370 A CN201810050370 A CN 201810050370A CN 108304967 A CN108304967 A CN 108304967A
- Authority
- CN
- China
- Prior art keywords
- rainfall
- water level
- flow
- mountain flood
- flood
- 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
Links
- XLYOFNOQVPJJNP-UHFFFAOYSA-N water Substances O XLYOFNOQVPJJNP-UHFFFAOYSA-N 0.000 title claims abstract description 69
- 238000000034 method Methods 0.000 title claims abstract description 47
- 230000008878 coupling Effects 0.000 title claims abstract description 14
- 238000010168 coupling process Methods 0.000 title claims abstract description 14
- 238000005859 coupling reaction Methods 0.000 title claims abstract description 14
- 238000011156 evaluation Methods 0.000 claims abstract description 21
- 238000011835 investigation Methods 0.000 claims abstract description 15
- 238000010276 construction Methods 0.000 claims abstract description 4
- 238000004364 calculation method Methods 0.000 claims description 38
- 238000013461 design Methods 0.000 claims description 22
- 239000002689 soil Substances 0.000 claims description 19
- 238000004519 manufacturing process Methods 0.000 claims description 7
- 230000008569 process Effects 0.000 claims description 7
- 238000001556 precipitation Methods 0.000 claims description 2
- 235000013399 edible fruits Nutrition 0.000 claims 1
- 230000002265 prevention Effects 0.000 abstract description 3
- 230000007246 mechanism Effects 0.000 description 5
- 230000000694 effects Effects 0.000 description 4
- 238000004458 analytical method Methods 0.000 description 3
- 238000004836 empirical method Methods 0.000 description 3
- 230000015572 biosynthetic process Effects 0.000 description 2
- 239000003973 paint Substances 0.000 description 2
- 238000009825 accumulation Methods 0.000 description 1
- 230000009286 beneficial effect Effects 0.000 description 1
- 230000008901 benefit Effects 0.000 description 1
- 238000000205 computational method Methods 0.000 description 1
- 238000010219 correlation analysis Methods 0.000 description 1
- 238000013524 data verification Methods 0.000 description 1
- 230000001066 destructive effect Effects 0.000 description 1
- 238000005516 engineering process Methods 0.000 description 1
- 239000000463 material Substances 0.000 description 1
- 238000005259 measurement Methods 0.000 description 1
- 238000012986 modification Methods 0.000 description 1
- 230000004048 modification Effects 0.000 description 1
- 230000031877 prophase Effects 0.000 description 1
- 238000011160 research Methods 0.000 description 1
- 238000007619 statistical method Methods 0.000 description 1
Classifications
-
- G—PHYSICS
- G06—COMPUTING; CALCULATING OR COUNTING
- G06Q—INFORMATION AND COMMUNICATION TECHNOLOGY [ICT] SPECIALLY ADAPTED FOR ADMINISTRATIVE, COMMERCIAL, FINANCIAL, MANAGERIAL OR SUPERVISORY PURPOSES; SYSTEMS OR METHODS SPECIALLY ADAPTED FOR ADMINISTRATIVE, COMMERCIAL, FINANCIAL, MANAGERIAL OR SUPERVISORY PURPOSES, NOT OTHERWISE PROVIDED FOR
- G06Q10/00—Administration; Management
- G06Q10/04—Forecasting or optimisation specially adapted for administrative or management purposes, e.g. linear programming or "cutting stock problem"
-
- G—PHYSICS
- G06—COMPUTING; CALCULATING OR COUNTING
- G06Q—INFORMATION AND COMMUNICATION TECHNOLOGY [ICT] SPECIALLY ADAPTED FOR ADMINISTRATIVE, COMMERCIAL, FINANCIAL, MANAGERIAL OR SUPERVISORY PURPOSES; SYSTEMS OR METHODS SPECIALLY ADAPTED FOR ADMINISTRATIVE, COMMERCIAL, FINANCIAL, MANAGERIAL OR SUPERVISORY PURPOSES, NOT OTHERWISE PROVIDED FOR
- G06Q50/00—Information and communication technology [ICT] specially adapted for implementation of business processes of specific business sectors, e.g. utilities or tourism
- G06Q50/10—Services
- G06Q50/26—Government or public services
- G06Q50/265—Personal security, identity or safety
-
- Y—GENERAL 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
- Y02—TECHNOLOGIES OR APPLICATIONS FOR MITIGATION OR ADAPTATION AGAINST CLIMATE CHANGE
- Y02A—TECHNOLOGIES FOR ADAPTATION TO CLIMATE CHANGE
- Y02A10/00—TECHNOLOGIES FOR ADAPTATION TO CLIMATE CHANGE at coastal zones; at river basins
- Y02A10/40—Controlling or monitoring, e.g. of flood or hurricane; Forecasting, e.g. risk assessment or mapping
Landscapes
- Business, Economics & Management (AREA)
- Engineering & Computer Science (AREA)
- Economics (AREA)
- Strategic Management (AREA)
- Human Resources & Organizations (AREA)
- Tourism & Hospitality (AREA)
- Marketing (AREA)
- Physics & Mathematics (AREA)
- Theoretical Computer Science (AREA)
- General Physics & Mathematics (AREA)
- Development Economics (AREA)
- General Business, Economics & Management (AREA)
- Computer Security & Cryptography (AREA)
- Health & Medical Sciences (AREA)
- Primary Health Care (AREA)
- Educational Administration (AREA)
- General Health & Medical Sciences (AREA)
- Game Theory and Decision Science (AREA)
- Entrepreneurship & Innovation (AREA)
- Operations Research (AREA)
- Quality & Reliability (AREA)
- Alarm Systems (AREA)
Abstract
The present invention provides the methods that rainfall flow water level coupling interpolation solves mountain flood Critical Rainfall, include the following steps:Data assessment, model construction, index calculate, rainfall flow water level couples interpolation and solves the method for mountain flood Critical Rainfall according to the water level that causes disaster of mountain flood field investigation evaluation object, the flow that causes disaster is converted to through hydraulic method, influence the coupled relation of rainfall play crest discharge corresponding to being formed by the case of rainfall early period based on different basins in certain period, interpolation inquires into the mountain flood Critical Rainfall influenced different basin early periods in the case of rainfall, to provide technical support for the prevention of mountain flood forecasting and warning.
Description
Technical field
The present invention relates to mountain flood field more particularly to rainfall-flow-water level coupling interpolation solution mountain flood are critical
The method of rainfall.
Background technology
China has a vast territory, and geology and geomorphology complexity is various, based on the plateau of mountainous region, is mostly in Over East Asia Monsoon Area, by force
Rainfall takes place frequently, and extreme weather increases, and mountain flood occurs frequent.Mountain flood is the main disasters of China's flood causing death
Kind, sudden strong, destructive power is big, and it is difficult that forecasting and warning prevents, and mostly occurs in remote mountain areas, has inconvenient traffic, communicates unsmooth, is
The difficult point and weak link of China's work of flood prevention.Mountain flood warning index is generally divided into rainfall warning index and water level early warning refers to
Two classes are marked, wherein rainfall warning index element includes two elements of period and its corresponding rainfall, by analyzing the different early warning periods
Critical Rainfall obtain.
When Critical Rainfall guidance causes a basin or region that mountain stream flood occurs may to cause calamity, that is, reach when causing disaster water level,
The minimum level and intensity that rainfall is met or exceeded.The accuracy of Critical Rainfall depends on converging mountain flood formation mechenism, production
The in-depth degree for flowing law study occurs background complexity due to mountain flood and recognizes formation mechanism of disaster and production confluence rule
Knowledge is not deep, tries the application stage all in discussion greatly to the research of Critical Rainfall both at home and abroad at present.
In general, Critical Rainfall is influenced by rainfall, basin soil moisture content and three big factor of land-surface characteristics.Rainfall item
Part is by play rainfall, the play accumulation indexs such as rainfall and rainfall intensity description;Soil layer aqueous conditions include soil moisture content
Or prophase programming;Watershed system feature includes the factors such as landform, channel features, basin geometric properties, vegetation, soil, by
The effect of human activity.
The determination method type of mountain flood Critical Rainfall is various at present, and empirical method and theory side can be divided by being summed up
Method two major classes.Empirical method is not concerned with the physical mechanism of mountain flood generating process, directly according to rainfall data series and mountain torrents
Disaster data series inquires into Critical Rainfall, and the demand to data is relatively fewer, and method is simple, using convenient.As there is actual measurement in the country
Rainfall statistic law, the anti-pushing manipulation of water level-flow, heavy rain critical curve method, analogy method, Japanese soil pluvial index method, actual effect rain
Amount method, concentration time and rainfall intensity method, multiple discriminant analysis statistic law etc..Theoretical method is also known as hydrology hydraulic method, with
Hydrology that mountain flood is formed based on hydraulics process, has stronger physical mechanism, higher to data-requirements.Such as me
Hydrodynamics and calculation method, the distributed model calculating method of state, Flash Flood Guidance (FFG) method in the U.S. etc..
2015《Mountain torrents Critical Rainfall based on rainfall runoff relation curve interpolation method calculates》Considering the case where early period influences rainfall
Under, according to rainfall in certain period and formed flood crest discharge correlativity curve, the corresponding flow of early warning water level is existed
Interpolation on curve, obtains corresponding Critical Rainfall value, and the method is to indicate that early period influences rainfall Pa, Pa with soil moisture content<
0.5Wm, soil are more dry;0.5Wm≤Pa≤0.8Wm, soil are general;Pa>0.8Wm, soil are wetter.Different early periods influence in basin
It is basin tool that rainfall has the premise of the correlation of height with formed flood crest discharge in certain period under the conditions of rainfall
Having good rainfall runoff relation, (general drainage area is less than 200km2), and peb process is mountain stream, unimodal flood, and be somebody's turn to do
The applicable precondition of the unlisted method of document.
Existing empirical method is few to data-requirements, is based on statistical analysis, lacks theoretical foundation, it is difficult to be widely applied
Other areas.Though theoretical method has a physical mechanism, data-requirements are high, because of the requirement of data, technical merit, parameter etc.,
It is difficult to use on a large scale.
Invention content
It is an object of the invention in view of the above shortcomings of the prior art, provide rainfall-flow-water level coupling interpolation to ask
The method for solving mountain flood Critical Rainfall, this method without the complete hydrological data of demand, and with certain Physical Mechanism and
Universality, to solve the above problem present in existing computational methods.
To achieve the above object, present invention employs following technical solutions:
The present invention provides rainfall-flow-water levels to couple the method that interpolation solves mountain flood Critical Rainfall, including following
Step:
S1, data assessment
It is less than 200km to calculating drainage area2Small watershed influence the rainfall runoff relation under the conditions of rainfall different early period
It is assessed;
S2, model construction
The design storm lasted according to small watershed difference is calculated considers that different basin early periods influence the typical scene of rainfall,
According to rainfall, production stream, confluence, the link of evolution, the mountain flood field investigation evaluation object typical frequency of control section nearby is calculated
Rate design flood, according to heavy rain and corresponding play crest discharge data, drawing influences rainfall-flow of rainfall different basin early periods
Relation curve builds curve model;
S3, index calculate
1) water level that, causes disaster corresponds to flow rate calculation:Control section number near the evaluation object measured according to mountain flood investigation
It according to achievement, converts and calculates through hydraulic method, obtain water level-discharge relation of evaluation object and the flow that causes disaster;
2), calculation interval determines:It is typical according to National Technical requirement, existing heavy rain isogram, mountain flood early warning
It is period, small watershed concentration time, comprehensive to determine calculation interval;
3), design storm calculates:Calculate design rainfall value and the rainstorm duration under each storm frequency;
4), net rainfall is analyzed:Consider that three kinds of typically different basin early periods influence rainfall situation and rainfall intensity, basin soil
Type, vegetation state land surface condition calculate the rainfall button damage during Flood of small drainage area, obtain net rainfall time distribution;
5), Design Flood Calculation:Rainfall situation is influenced according to three kinds of typically different basin early periods, calculates each storm frequency allusion quotation
The peb process that type calculation interval rainfall is formed includes mainly crest discharge, rise lasts and the duration of flood;
6), rainfall-flow-water level coupled relation Drawing of Curve:According to the water level-flow for the evaluation object that step 1) calculates
Relationship, different basins influence the design rainfall value of rainfall situation typical calculation period, corresponding play crest discharge early period, paint respectively
The rainfall magnitudes of different periods processed, crest discharge value, water level value point are away from analyzing its correlativity, be fitted to rainfall-stream
Amount-water level coupled relation curve finally obtains rainfall-stream in the case of each typical calculation period difference basin influence early period rainfall
Amount-water level coupled relation curve graph;
7) reading Critical Rainfall, is looked into:According to the evaluation object of mountain flood field investigation cause disaster water level, the typical calculation period letter
Breath, in rainfall-flow-water level coupled relation curve graph that typical calculation period difference basin influences rainfall early period,
It looks into and is read as calamity flow, further according to influencing basin early period rainfall situation and look into read corresponding rainfall to get to Critical Rainfall.
Further, in step 2), the existing heavy rain isogram has 10min, 1h, 6h, for 24 hours.
Further, in step 2), the small watershed concentration time is 7.9h.
Further, in step 2), the mountain flood early warning typical period of time is 1h, 3h, 6h, 12h, for 24 hours.
Further, in step 2), the comprehensive determining calculation interval is 1h, 3h, 6h, 12h.
Further, in step 5), three kinds of typically different basin early periods influence rainfall situation and are respectively:The more dry Pa of soil
The general Pa=0.5Wm of=0.2Wm, soil, the wetter Pa=0.8Wm of soil.
Beneficial effects of the present invention are:Rainfall-flow-water level coupling interpolation solves the method root of mountain flood Critical Rainfall
According to the water level that causes disaster of mountain flood field investigation evaluation object, the flow that causes disaster is converted to through hydraulic method, is based on certain period
Interior difference basin influences the coupled relation of rainfall play crest discharge corresponding to being formed by the case of rainfall early period, and interpolation pushes away
Ask influence the mountain flood Critical Rainfall in the case of rainfall different basin early periods, to be provided for the prevention of mountain flood forecasting and warning
Technical support.
Description of the drawings
Fig. 1 is certain small watershed 12h rainfall-flow-water level coupled relation curve graphs;
Fig. 2 is the flood hydrograph figure that basin influences rainfall Pa=0.8Wm early periods;
Fig. 3 is the flood hydrograph figure that basin influences rainfall Pa=0.5Wm early periods;
Fig. 4 is the flood hydrograph figure that basin influences rainfall Pa=0.2Wm early periods;
Fig. 5 is one small watershed 1h rainfall-flow-water level coupled relation curve graphs of embodiment;
Fig. 6 is one small watershed 3h rainfall-flow-water level coupled relation curve graphs of embodiment;
Fig. 7 is one small watershed 6h rainfall-flow-water level coupled relation curve graphs of embodiment;
Wherein, Pa, which is basin, influences rainfall early period;Wm is basin reservoir capacity.
Specific implementation mode
In order to make the purpose , technical scheme and advantage of the present invention be clearer, with reference to the accompanying drawings and embodiments, right
The present invention is further elaborated.It should be appreciated that described herein, specific examples are only used to explain the present invention, not
For limiting the present invention.
According to correlation analysis method, mass data verification result shows when watershed system condition is constant, rainfall,
Basin influences rainfall with depth of runoff there are certain correlativity early period, and can establish rainfall-early period of experience influences rainfall-diameter
Related figure (P~the P of streama~R correlations figure), related figure reflects the production stream rule in basin.
By production confluence principle it is found that during watershed concentration, interflow subsurface drainage and interflow, the diameter that net rainfall is formed are not considered
Flow depth and magnanimity are there are correlativity, and the mountain stream flood caused by heavy showers generally lasts for shorter, and flood peak is larger, and magnanimity is main
It is to be influenced by crest discharge, there are certain correlativities with crest discharge for magnanimity, and then in certain period before different basins
There are correlativities for rainfall play crest discharge corresponding to being formed by the case of phase influences rainfall.
For certain small watershed, according to evaluation object water level-discharge relation, different basins influence rainfall early period in certain period
In the case of rainfall play crest discharge correlativity corresponding to being formed by, obtain rainfall-flow-water level connecting curve, will
Interpolation on the curves of water level that causes disaster of mountain flood field investigation evaluation object obtains corresponding rainfall, i.e. Critical Rainfall value.
The method that rainfall-flow-water level coupling interpolation solves mountain flood Critical Rainfall, includes the following steps:
S1, data assessment
By runoff principle it is found that the method that rainfall-flow-water level coupling interpolation solves mountain flood Critical Rainfall
In the small watershed with more reliable rainfall runoff relation curve, (drainage area is less than 200km2) use, effect is more preferable.Cause
This, need to assess the rainfall runoff relation under the conditions of the different influence early period rainfall of calculating small watershed;
S2, model construction
The design storm lasted according to small watershed difference is calculated considers that different basin early periods influence the typical scene of rainfall,
According to rainfall, production stream, confluence, the link of evolution, the mountain flood field investigation evaluation object typical frequency of control section nearby is calculated
Rate design flood, according to heavy rain and corresponding play crest discharge data, drawing influences rainfall-stream of rainfall different basin early periods
Amount-water level coupled relation curve builds curve model;
S3, index calculate
1) water level that, causes disaster corresponds to flow rate calculation:Control section number near the evaluation object measured according to mountain flood investigation
It according to achievement, converts and calculates through hydraulic method, obtain water level-discharge relation of evaluation object and the flow that causes disaster;
2), calculation interval determines:It is typical according to National Technical requirement, existing heavy rain isogram, mountain flood early warning
It is period, small watershed concentration time, comprehensive to determine calculation interval;
3), design storm calculates:Calculate 10min, 1h under each storm frequency (a-hundred-year, fifty year return period ... etc.),
3h, 6h, 12h, design rainfall value for 24 hours and rainstorm duration;
4), net rainfall is analyzed:Consider that three kinds of typically different basin early periods influence rainfall situation and rainfall intensity, basin soil
Type, vegetation state land surface condition calculate the rainfall button damage during Flood of small drainage area, obtain net rainfall time distribution;
5), Design Flood Calculation:Rainfall situation is influenced according to three kinds of typically different basin early periods, calculates each storm frequency allusion quotation
The peb process that type calculation interval rainfall is formed includes mainly crest discharge, rise lasts and the duration of flood;
6), rainfall-flow-water level coupled relation Drawing of Curve:According to the water level-flow for the evaluation object that step 1) calculates
Relationship, different basins influence the design rainfall value of rainfall situation typical calculation period, corresponding play crest discharge early period, paint respectively
The rainfall magnitudes of different periods processed, crest discharge value, water level value point are away from analyzing its correlativity, be fitted to rainfall-stream
Amount-water level coupled relation curve finally obtains rainfall-stream in the case of each typical calculation period difference basin influence early period rainfall
Amount-water level coupled relation curve graph;Such as Fig. 1.
7) reading Critical Rainfall, is looked into:According to the evaluation object of mountain flood field investigation cause disaster water level, the typical calculation period letter
Breath, in rainfall-flow-water level coupled relation curve graph that typical calculation period difference basin influences rainfall early period,
It looks into and is read as calamity flow, further according to influencing basin early period rainfall situation and look into read corresponding rainfall to get to Critical Rainfall.Such as Fig. 1 institutes
Show, certain small watershed evaluation object causes disaster water level for 371.8m, and it is 182m that the flow that causes disaster is checked according to water level-discharge relation3/ s, then
Rainfall-flow-water level coupled relation the curve graph for reading basin 12h is looked into, the Critical Rainfall of basin 12h is obtained, such as table 1.
Certain the small watershed evaluation object Critical Rainfall outcome table of table 1
In step 2), the existing heavy rain isogram has 10min, 1h, 6h, for 24 hours.
In step 2), the small watershed concentration time is 7.9h.
In step 2), the mountain flood early warning typical period of time is 1h, 3h, 6h, 12h, for 24 hours.
In step 2), the comprehensive determining calculation interval is 1h, 3h, 6h, 12h.
Embodiment one
Selecting Huangmei County great river town, village is example along the river, and Yuan Shanhe wears village and mistake, in history repeatedly by mountain flood
It threatens.1 river vertical section and 3 are measured according to village house distribution and river situation according to mountain flood Investigation requirements
Cross section, water collection basin area more than control section are 30.9km2, the long 12.4km in river, than drop about 14.96 ‰.
(1) data is assessed
The moneys such as rainfall-runoff correlation figure, rainfall isopleth, storm flood handbook are influenced according to the rainfall being collected into-early period
Material analysis is it is found that small watershed difference influences the rainfall runoff relation good relationship under the conditions of rainfall early period.
(2) water level that causes disaster corresponds to flow rate calculation
The control section data measured according to village's mountain flood investigation calculate the water level-in the village using Manning formula method
Discharge relation must cause disaster flow for 189m according to the water level 31.87m that causes disaster of investigation3/s。
(3) calculation interval determines
It is required according to National Technical, mountain flood early warning typical period of time is 1h, 3h, 6h, 12h, for 24 hours, Hubei Province's heavy rain etc.
The value line chart period is 10min, 1h, 6h, for 24 hours, and the concentration time of the small watershed is 5.2h, it is comprehensive determine calculation interval be 1h, 3h,
6h。
(4) design storm calculates
Calculate 10min, 1h under each storm frequency of the small watershed (a-hundred-year, fifty year return period ... etc.), 3h, 6h,
The design rainfall value and rainstorm duration value of 12h, the calculation intervals such as 24 hours.Such as table 2 and table 3.
The design rainfall value of each storm frequency of 2 small watershed of table
3 rainstorm duration value (only listing 6h) of table
(5) net rainfall is analyzed
Consider that 3 kinds of typically different basin early periods influence rainfall situation and rainfall intensity, basin soil types, vegetation state
Equal land surface conditions calculate the rainfall button damage during Flood of small drainage area, obtain net rainfall time distribution (only listing 6h).As table 4,
Table 5 and table 6.
4 basin of table influences the net rainfall outcome table of rainfall Pa=0.8Wm early period
5 basin of table influences the net rainfall outcome table of rainfall Pa=0.5Wm early period
Net rainfall outcome table when 6 basin influence early period rainfall Pa=0.2Wm of table
(6) Design Flood Calculation
Influence rainfall situations according to 3 kinds of typically different basin early periods, calculate each storm frequency (it is a-hundred-year, 50 years one
Meet ... etc.) typical calculation hourly precipitation formed peb process (only listing 6h).Such as Fig. 2, Fig. 3, Fig. 4.
(7) rainfall-flow-water level coupled relation Drawing of Curve
Influence the design of rainfall situation typical calculation period early period according to the small watershed water level-discharge relation, different basins
Rainfall value, corresponding play crest discharge, the rainfall magnitude of drafting different periods, crest discharge value, water level value point are away from analysis respectively
Its correlativity is fitted to rainfall-flow-water level coupled relation curve.Such as Fig. 5, Fig. 6, Fig. 7.
(8) reading Critical Rainfall is looked into
According to the flow 189m that causes disaster3/ s influences rainfall-stream of rainfall early period in typical calculation period difference basin
It in amount-water level coupled relation curve graph, looks into and is read as calamity flow, looked into further according to basin influence early period rainfall situation and read corresponding rain
Amount is to get to Critical Rainfall.Such as Fig. 6, Fig. 7 and table 7.
7 Critical Rainfall outcome table of table
Embodiments of the present invention above described embodiment only expresses, the description thereof is more specific and detailed, but can not
Therefore it is interpreted as the limitation to the scope of the claims of the present invention.It should be pointed out that for those of ordinary skill in the art,
Without departing from the inventive concept of the premise, various modifications and improvements can be made, these belong to the protection model of the present invention
It encloses.Therefore, the protection domain of patent of the present invention should be determined by the appended claims.
Claims (6)
1. the method that rainfall-flow-water level coupling interpolation solves mountain flood Critical Rainfall, which is characterized in that including following step
Suddenly:
S1, data assessment
It is less than 200km to calculating drainage area2Small watershed influence the rainfall runoff relation under the conditions of rainfall different early period and commented
Estimate;
S2, model construction
The design storm lasted according to small watershed difference is calculated considers that different basin early periods influence the typical scene of rainfall, according to
Rainfall, production stream, confluence, the link of evolution, calculating mountain flood field investigation evaluation object, nearby control section typical frequencies are set
Flood is counted, according to heavy rain and corresponding play crest discharge data, drawing influences rainfall-discharge relation of rainfall different basin early periods
Curve builds curve model;
S3, index calculate
1) water level that, causes disaster corresponds to flow rate calculation:According to mountain flood investigation measure evaluation object near control section data at
Fruit converts through hydraulic method and calculates, and obtains water level-discharge relation of evaluation object and the flow that causes disaster;
2), calculation interval determines:According to National Technical requirement, existing heavy rain isogram, mountain flood early warning typical period of time,
It is the small watershed concentration time, comprehensive to determine calculation interval;
3), design storm calculates:Calculate design rainfall value and the rainstorm duration under each storm frequency;
4), net rainfall is analyzed:Consider to influence three kinds of typically different basin early periods rainfall situations and rainfall intensity, basin soil types,
Vegetation state land surface condition calculates the rainfall button damage during Flood of small drainage area, obtains net rainfall time distribution;
5), Design Flood Calculation:Rainfall situation is influenced according to three kinds of typically different basin early periods, calculates each storm frequency typical case meter
The peb process that hourly precipitation is formed is calculated, includes mainly corresponding play crest discharge, rise lasts and the duration of flood;
6), rainfall-flow-water level coupled relation Drawing of Curve:Water level-flow of the evaluation object calculated according to step 1) closes
System, different basins influence the design rainfall value of rainfall situation typical calculation period, corresponding play crest discharge early period, draw respectively
The rainfall magnitudes of different periods, crest discharge value, water level value point are away from analyzing its correlativity, be fitted to rainfall-flow-
Water level coupled relation curve finally obtains rainfall-flow-water in the case of different basins influence early period rainfall under each calculation interval
Position coupled relation curve graph;
7) reading Critical Rainfall, is looked into:It is caused disaster water level, typical calculation period information according to the evaluation object of mountain flood field investigation,
In rainfall-flow-water level coupled relation curve graph that typical calculation period difference basin influences rainfall early period, reading is looked into
Cause disaster flow, further according to influencing basin early period rainfall situation and look into read corresponding rainfall to get to Critical Rainfall.
2. the method that rainfall-flow according to claim 1-water level coupling interpolation solves mountain flood Critical Rainfall,
It is characterized in that:In step 2), the existing heavy rain isogram has 10min, 1h, 6h, for 24 hours.
3. the method that rainfall-flow according to claim 1-water level coupling interpolation solves mountain flood Critical Rainfall,
It is characterized in that:In step 2), the small watershed concentration time is 7.9h.
4. the method that rainfall-flow according to claim 1-water level coupling interpolation solves mountain flood Critical Rainfall,
It is characterized in that:In step 2), the mountain flood early warning typical period of time is 1h, 3h, 6h, 12h, for 24 hours.
5. the method that rainfall-flow according to claim 1-water level coupling interpolation solves mountain flood Critical Rainfall,
It is characterized in that:In step 2), the comprehensive determining calculation interval is 1h, 3h, 6h, 12h.
6. the method that rainfall-flow according to claim 1-water level coupling interpolation solves mountain flood Critical Rainfall,
It is characterized in that:In step 5), three kinds of typically different basin early periods influence rainfall situation and are respectively:The more dry Pa=of soil
The general Pa=0.5Wm of 0.2Wm, soil, the wetter Pa=0.8Wm of soil.
Priority Applications (1)
Application Number | Priority Date | Filing Date | Title |
---|---|---|---|
CN201810050370.4A CN108304967A (en) | 2018-01-18 | 2018-01-18 | The method that rainfall-flow-water level coupling interpolation solves mountain flood Critical Rainfall |
Applications Claiming Priority (1)
Application Number | Priority Date | Filing Date | Title |
---|---|---|---|
CN201810050370.4A CN108304967A (en) | 2018-01-18 | 2018-01-18 | The method that rainfall-flow-water level coupling interpolation solves mountain flood Critical Rainfall |
Publications (1)
Publication Number | Publication Date |
---|---|
CN108304967A true CN108304967A (en) | 2018-07-20 |
Family
ID=62865563
Family Applications (1)
Application Number | Title | Priority Date | Filing Date |
---|---|---|---|
CN201810050370.4A Pending CN108304967A (en) | 2018-01-18 | 2018-01-18 | The method that rainfall-flow-water level coupling interpolation solves mountain flood Critical Rainfall |
Country Status (1)
Country | Link |
---|---|
CN (1) | CN108304967A (en) |
Cited By (22)
Publication number | Priority date | Publication date | Assignee | Title |
---|---|---|---|---|
CN109118721A (en) * | 2018-10-31 | 2019-01-01 | 河海大学 | The method, apparatus and method for early warning of compound warning index are inquired into based on Critical Rainfall |
CN109190263A (en) * | 2018-09-10 | 2019-01-11 | 柳创新 | Method based on full Basin Rainfall runoff and hydrodynamic model prediction precipitation flow |
CN109242336A (en) * | 2018-09-28 | 2019-01-18 | 郑州大学 | Mountain flood Critical Rainfall method for early warning under Scenario mode |
CN109671248A (en) * | 2018-12-12 | 2019-04-23 | 河北省水利水电勘测设计研究院 | Mountain flood method for early warning based on object of taking precautions against natural calamities |
CN109785979A (en) * | 2019-01-07 | 2019-05-21 | 三峡大学 | A kind of play flood rainfall-runoff process confining method |
CN109829584A (en) * | 2019-02-02 | 2019-05-31 | 中国水利水电科学研究院 | A kind of mountain torrents risk dynamic assessment method |
CN109961613A (en) * | 2019-03-04 | 2019-07-02 | 四川大学 | Water level method for early warning based on the rise variation of small watershed in mountain Storm Flood water level |
CN109993350A (en) * | 2019-03-13 | 2019-07-09 | 河海大学 | A kind of Critical Rainfall evaluation method based on spatially distributed rainfall |
CN110298480A (en) * | 2019-05-20 | 2019-10-01 | 济南大学 | A kind of mountain flood Critical Rainfall index calculating method and system |
CN110737875A (en) * | 2019-09-24 | 2020-01-31 | 浙江省水利河口研究院 | medium-and-long-term torrential flood disaster early warning and prejudging method |
CN111047213A (en) * | 2019-12-25 | 2020-04-21 | 长江水利委员会水文局 | Middle and long term water resource critical early warning index method based on multi-factor joint discrimination |
CN111260159A (en) * | 2020-02-26 | 2020-06-09 | 刘祖敏 | Meteorological-hydrological coupling flood measuring and reporting method |
CN111339711A (en) * | 2020-02-24 | 2020-06-26 | 三峡大学 | Small watershed design flood calculation method |
CN111582755A (en) * | 2020-05-20 | 2020-08-25 | 中国水利水电科学研究院 | Mountain torrent disaster comprehensive risk dynamic assessment method based on multi-dimensional set information |
CN111625993A (en) * | 2020-05-25 | 2020-09-04 | 中国水利水电科学研究院 | Small watershed surface rainfall interpolation method based on mountainous terrain and rainfall characteristic prediction |
CN111861014A (en) * | 2020-07-23 | 2020-10-30 | 广东省水文局梅州水文分局 | Distributed unit line flood forecasting method |
CN112381285A (en) * | 2020-11-12 | 2021-02-19 | 中国科学院空天信息创新研究院 | Flood inundation prediction method based on remote sensing |
CN113298305A (en) * | 2021-05-24 | 2021-08-24 | 四川大学 | Double-threshold rainstorm mountain torrent flood disaster early warning method based on different rainfall time-course characteristics |
CN113642794A (en) * | 2021-08-16 | 2021-11-12 | 浙江大学 | Mountain torrent forecasting method combining rainfall and soil water observation |
CN117113236A (en) * | 2023-10-20 | 2023-11-24 | 广东申创光电科技有限公司 | Smart city monitoring system and data processing method |
CN117291061A (en) * | 2023-11-24 | 2023-12-26 | 福建省水利水电勘测设计研究院有限公司 | Embankment safety and stability analysis and early warning method under variable water flow environment |
CN112381285B (en) * | 2020-11-12 | 2024-06-07 | 中国科学院空天信息创新研究院 | Flood inundation prediction method based on remote sensing |
Citations (1)
Publication number | Priority date | Publication date | Assignee | Title |
---|---|---|---|---|
CN102693215A (en) * | 2012-04-24 | 2012-09-26 | 江苏建筑职业技术学院 | Method for fitting power function type stage-discharge relation |
-
2018
- 2018-01-18 CN CN201810050370.4A patent/CN108304967A/en active Pending
Patent Citations (1)
Publication number | Priority date | Publication date | Assignee | Title |
---|---|---|---|---|
CN102693215A (en) * | 2012-04-24 | 2012-09-26 | 江苏建筑职业技术学院 | Method for fitting power function type stage-discharge relation |
Non-Patent Citations (2)
Title |
---|
张细艳 等: "李家河河段水位流量关系初步分析", 《企业技术开发》 * |
徐少军 等: "基于降雨径流关系曲线插值法的山洪临界雨量计算", 《研究探讨》 * |
Cited By (34)
Publication number | Priority date | Publication date | Assignee | Title |
---|---|---|---|---|
CN109190263A (en) * | 2018-09-10 | 2019-01-11 | 柳创新 | Method based on full Basin Rainfall runoff and hydrodynamic model prediction precipitation flow |
CN109242336A (en) * | 2018-09-28 | 2019-01-18 | 郑州大学 | Mountain flood Critical Rainfall method for early warning under Scenario mode |
CN109242336B (en) * | 2018-09-28 | 2021-09-10 | 郑州大学 | Critical rainfall early warning method for torrential flood disasters in multi-scenario mode |
CN109118721A (en) * | 2018-10-31 | 2019-01-01 | 河海大学 | The method, apparatus and method for early warning of compound warning index are inquired into based on Critical Rainfall |
CN109671248A (en) * | 2018-12-12 | 2019-04-23 | 河北省水利水电勘测设计研究院 | Mountain flood method for early warning based on object of taking precautions against natural calamities |
CN109785979A (en) * | 2019-01-07 | 2019-05-21 | 三峡大学 | A kind of play flood rainfall-runoff process confining method |
CN109829584A (en) * | 2019-02-02 | 2019-05-31 | 中国水利水电科学研究院 | A kind of mountain torrents risk dynamic assessment method |
CN109961613A (en) * | 2019-03-04 | 2019-07-02 | 四川大学 | Water level method for early warning based on the rise variation of small watershed in mountain Storm Flood water level |
CN109993350A (en) * | 2019-03-13 | 2019-07-09 | 河海大学 | A kind of Critical Rainfall evaluation method based on spatially distributed rainfall |
CN109993350B (en) * | 2019-03-13 | 2021-04-27 | 河海大学 | Critical rainfall estimation method based on rainfall spatial distribution |
CN110298480A (en) * | 2019-05-20 | 2019-10-01 | 济南大学 | A kind of mountain flood Critical Rainfall index calculating method and system |
CN110298480B (en) * | 2019-05-20 | 2021-10-26 | 济南大学 | Method and system for calculating critical rainfall index of mountain torrent disaster |
CN110737875A (en) * | 2019-09-24 | 2020-01-31 | 浙江省水利河口研究院 | medium-and-long-term torrential flood disaster early warning and prejudging method |
CN110737875B (en) * | 2019-09-24 | 2023-05-12 | 浙江省水利河口研究院 | Early warning and pre-judging method for mountain torrent disasters in medium and long periods |
CN111047213A (en) * | 2019-12-25 | 2020-04-21 | 长江水利委员会水文局 | Middle and long term water resource critical early warning index method based on multi-factor joint discrimination |
CN111339711B (en) * | 2020-02-24 | 2021-12-07 | 三峡大学 | Small watershed design flood calculation method |
CN111339711A (en) * | 2020-02-24 | 2020-06-26 | 三峡大学 | Small watershed design flood calculation method |
CN111260159A (en) * | 2020-02-26 | 2020-06-09 | 刘祖敏 | Meteorological-hydrological coupling flood measuring and reporting method |
CN111260159B (en) * | 2020-02-26 | 2023-06-06 | 刘祖敏 | Meteorological hydrologic coupling flood forecasting method |
CN111582755B (en) * | 2020-05-20 | 2020-12-22 | 中国水利水电科学研究院 | Mountain torrent disaster comprehensive risk dynamic assessment method based on multi-dimensional set information |
CN111582755A (en) * | 2020-05-20 | 2020-08-25 | 中国水利水电科学研究院 | Mountain torrent disaster comprehensive risk dynamic assessment method based on multi-dimensional set information |
CN111625993A (en) * | 2020-05-25 | 2020-09-04 | 中国水利水电科学研究院 | Small watershed surface rainfall interpolation method based on mountainous terrain and rainfall characteristic prediction |
CN111861014B (en) * | 2020-07-23 | 2021-03-16 | 广东省水文局梅州水文分局 | Distributed unit line flood forecasting method |
CN111861014A (en) * | 2020-07-23 | 2020-10-30 | 广东省水文局梅州水文分局 | Distributed unit line flood forecasting method |
CN112381285A (en) * | 2020-11-12 | 2021-02-19 | 中国科学院空天信息创新研究院 | Flood inundation prediction method based on remote sensing |
CN112381285B (en) * | 2020-11-12 | 2024-06-07 | 中国科学院空天信息创新研究院 | Flood inundation prediction method based on remote sensing |
CN113298305A (en) * | 2021-05-24 | 2021-08-24 | 四川大学 | Double-threshold rainstorm mountain torrent flood disaster early warning method based on different rainfall time-course characteristics |
CN113298305B (en) * | 2021-05-24 | 2023-04-07 | 四川大学 | Double-threshold rainstorm mountain torrent flood disaster early warning method based on different rainfall time-course characteristics |
CN113642794B (en) * | 2021-08-16 | 2023-11-24 | 浙江大学 | Mountain torrent forecasting method combining rainfall and soil water observation |
CN113642794A (en) * | 2021-08-16 | 2021-11-12 | 浙江大学 | Mountain torrent forecasting method combining rainfall and soil water observation |
CN117113236A (en) * | 2023-10-20 | 2023-11-24 | 广东申创光电科技有限公司 | Smart city monitoring system and data processing method |
CN117113236B (en) * | 2023-10-20 | 2023-12-22 | 广东申创光电科技有限公司 | Smart city monitoring system and data processing method |
CN117291061A (en) * | 2023-11-24 | 2023-12-26 | 福建省水利水电勘测设计研究院有限公司 | Embankment safety and stability analysis and early warning method under variable water flow environment |
CN117291061B (en) * | 2023-11-24 | 2024-02-09 | 福建省水利水电勘测设计研究院有限公司 | Embankment safety and stability analysis and early warning method under variable water flow environment |
Similar Documents
Publication | Publication Date | Title |
---|---|---|
CN108304967A (en) | The method that rainfall-flow-water level coupling interpolation solves mountain flood Critical Rainfall | |
Eder et al. | Comparative calculation of suspended sediment loads with respect to hysteresis effects (in the Petzenkirchen catchment, Austria) | |
Brocca et al. | On the estimation of antecedent wetness conditions in rainfall–runoff modelling | |
Bartley et al. | A sediment budget for a grazed semi-arid catchment in the Burdekin basin, Australia | |
Yitayew et al. | Using GIS for facilitating erosion estimation | |
Modrick et al. | Regional bankfull geometry relationships for southern California mountain streams and hydrologic applications | |
Cognard-Plancq et al. | The role of forest cover on streamflow down sub-Mediterranean mountain watersheds: a modelling approach | |
Pruski et al. | Improved regionalization of streamflow by use of the streamflow equivalent of precipitation as an explanatory variable | |
Baffaut et al. | Comparative analysis of water budgets across the US long-term agroecosystem research network | |
Doody et al. | Overland flow initiation from a drumlin grassland hillslope | |
Nyholm et al. | Estimation of stream flow depletion and uncertainty from discharge measurements in a small alluvial stream | |
Letcher et al. | Methods for the analysis of trends in streamflow response due to changes in catchment condition | |
López-Vicente et al. | A new distributed rainfall-runoff (DR2) model based on soil saturation and runoff cumulative processes | |
Wilkinson et al. | A multi-scale nested experiment for understanding flood wave generation across four orders of magnitude of catchment area | |
Shamir et al. | Geomorphology-based index for detecting minimal flood stages in arid alluvial streams | |
Herma | Data processing and model choice for flood prediction | |
Deb et al. | Simulating deep percolation in flood-irrigated mature pecan orchards with RZWQM2 | |
CN111101477B (en) | Method for determining flow of low-grade water during supplement actual measurement of data-free design basin | |
Smith et al. | Evaluating the Performance of Bay Irrigation in the GMID | |
Canfield et al. | Studies of scale and processes in hydrologic modeling on the lucky hills watershed | |
Peng et al. | Experimental study on the influence of vegetation on the slope flow concentration time | |
Fiala et al. | Changes in a river's regime of a watercourse after a small water reservoir construction. | |
Gwak et al. | The relationships between drought indices (SPI, API) and in-situ soil moisture in forested hillslopes | |
CN106801400B (en) | A kind of quantitative estimation method of Mountain Area ephemeral stream length | |
Watson et al. | Water budget and vertical conductance for Magnolia Lake |
Legal Events
Date | Code | Title | Description |
---|---|---|---|
PB01 | Publication | ||
PB01 | Publication | ||
SE01 | Entry into force of request for substantive examination | ||
SE01 | Entry into force of request for substantive examination | ||
RJ01 | Rejection of invention patent application after publication | ||
RJ01 | Rejection of invention patent application after publication |
Application publication date: 20180720 |