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scs rainfall distribution table

Hydrologic modeling is based on Soil Conservation Services (SCS) type RDPs (SCS type I, IA, II, and III). A review of hourly rainfall data shows, A review of hourly rainfall data shows, Title: Time distributions: design storms 24-hours and less Author: Dan Moore Last modified by: Moore, Dan - NRCS, Portland, OR Created Date: 3/21/2002 6:16:55 PM Other titles: data Type I Type Ia Type II Type III type_Ia type_II type_III area. There are four steps involved in calculating NRCS runoff hydrographs. 0.1 1.74e-3 6.613000952133628e-3 3.3505899666254921e-3 2.2044579037609341e-3 1.74e-3 1.74e-3 1.74e-3. Also the new rainfall type (DMV C) was developed for the Eastern Shore, part of the Delmarva Peninsula. The SCS‐CN method is an event‐based model that describes the runoff response with a rainfall‐runoff curve that is a function of the cumulative storm rainfall and antecedent wetness condition. A map of a multi-state area with a regional rainfall distribution was developed along with a 24-hour rainfall table … The rainfall distribution by Thiessen polygon method was adopted. Open the Excel file containing the rainfall data. To enter manually, simply type in the rainfall amounts associated with the selected design storm and frequencies. A sampling of NSCS Type II rainfall amounts is shown in the screen above in Step 2. For example, the rainfall amounts for the 2, 10 and 100 year events are 2.28, 3.31 and 4.94 inches respectively. For construction sites, Table 4-6 shows that newly grades areas have curve numbers ranging … Determine runoff depth (in inches) from the curve number and rainfall depth using Table 3-3. These values were derived from the National Oceanic and Atmospheric Administration (NOAA) Atlas 14, Volume 8, Version 2.0 and the There will be no continuous abstraction or excess rainfall until the total cumulative rainfall becomes greater than Ia. SCS Standard: 6: Dimensionless distribution developed by SCS for a shorter, 6-hr duration. Drainage Manual - IDF Curves and Rainfall Distributions: 12/10/15: Geopak-Guide.pdf. Assigning the rainfall amount for each catchment was done by performing zonal statistics to the rainfall distribution maps. Bohman (1984) computed flood profiles for conditions before and after construction of 1-526 and the diversion of s To estimate runoff from storm rainfall, SCS uses the runoff curve number (CN) method (see chapters 4 through 10 of NEH-4, SCS 1985). Determination of CN depends on the watershed’s soil and cover conditions, which the model represents as hydrologic soil group, cover type, treatment, and hydrologic condition. University, Kukatpally, Hyderabad 3Department of Botany, P. G. College of … The Type IA hyetograph is also a standard NRCS rainfall distribution. rainfall is then set equal to the time of concentration and is used to estimate the design average rainfall intensity (i). A value of S = 2.5 inch means the initial abstraction Ia = 0.5 inch ( Ia = 0.2S). The boundaries are approximate so engineering judgement may be used to select a storm type on the basis of the meteorologic patterns. in./hr. Therefore, non-USA users need to determine whether a typical 24-hr rainfall resembles a Type I, IA, II, or III distribution and determine 24-hr rainfalls from local sources. This method is the same as used in the original TR-20. Table 3 - Coefficients of velocity (fps) versus slope (%) relationship for estimating travel velocities (McCuen 1989; SCS 1972). storm is based on an SCS Type II, 24-hr rainfall distribution.) Most projects will use one of the predefined rainfall distributions listed below. Rainfall frequency maps from Technical Paper 40 have been moved to this page. This method is the same as used in the original TR-20. Ratios to 24 hour rainfall for the Type II distribution ..... 44 86 Table 4‐ 6. The unit hydrograph is then scaled by the runoff and the area to obtain the hydrograph using the Tabular Hydrograph method. It can simulate the Rainfall- runoff, runoff, evaporation, infiltration and … The Type 3 storm is not considered further in this paper. There is no scientific justification for using SCS type II method in arid regions. The storm type should be selected based on the location of the watershed after consulting Figure 23. Analysis shall be based on a Type II 24-hour rainfall distribution. N22:P22 Display the adjusted rainfall amounts. Under the conditions of a shallow water table, say at 140 cm, the effective rainfall … The Soil Conservation Service Curve Number (SCS-CN) method is widely used for predicting direct runoff volume for a given rainfall event. during the previous. Distribution of the rainfall depth across the 24-hour can be estimated using the SCS (NRCS) rainfall types (i.e. The pond and swamp adjustment factor is ob-tained from table 4-2 (rounded to the nearest table value). 02397530. The SCS 24-hour rainfall distributions are shown in Figure 1, with the corresponding geographic boundaries shown in Figure 2. Most distributions are 6 minutes. Rainfall Temporal Distribution. cense, which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited. The standard rainfall distribution used in Minnesota was the SCS (now the NRCS) Type II distribution. The resulting long duration storm with a nested small, intense storm is intended to be applicable to small, large, urban, and rural watersheds. for SCS rainfall distributions..... B-2 B-3 2-year, 24-hour rainfall ..... B-3 B-4 5-year, 24-hour rainfall ..... B-3 B-5 10-year, 24-hour rainfall ..... B-4 B-6 25-year, 24-hour rainfall ..... B-4 Basic SCS rainfall-runoff relationship for different CN values (SCS 1986). Tables 4-6 and 4-7 are used to select the most appropriate curve numbers for the area. SCS (NRCS) Rainfall Types (Source Nicklow et al., 2006) Rules for Entering the SCS CN in the Dialogs. Stop using NRCS Type II Rainfall Distribution Use Atlas 14 Rainfall Depth – from PFDS server or NRCS County File Use MSE 3 or Atlas 14 Derived Rainfall Distribution Use SCS Typical Unit Hydrograph (peak factor 484) Use Time of Concentration formulas from Drainage Manual/TR-55 Route flow (hydrograph analysis) where have storage Investigation of Rainfall – Runoff modeling of the Ashti catchment by SCS Curve Number using Remote Sensing and GIS B.Veeranna1, I. V. Muralikrishna2, N.L. This XML file provides the six regional rainfall distributions for California (CA-1 through CA-6) developed by NRCS to replace the SCS Types I, IA and II distributions used previously. These RDPs were designed for the USA and similar temperate regions. This distribution was developed in the 1960s using the precipitation-frequency estimates contained in Technical Paper No. The temporal rainfall distribution is how rainfall intensity varies over time for a single event. A unit hydrograph is obtained from a table based on subarea and event specific variables. iSWMTM Technical Manual Hydrology Hydrology: 1.0 Hydrological Analysis 2.0 Downstream Assessment 3.0 Streambank Protection 4.0 Water Balance 5.0 Rainfall Tables Unfortunately, TR-55 only presents rainfall distribution maps for the USA. Rainfall distribution patterns (RDPs) are crucial for hydrologic design. The goal was to identify regions of similar rainfall distribution. Rainfall Total (Inches) Rainfall Source Storm Distribution Significant 1000 24 21.7 NOAA Atlas 14 SCS Type III The drainage area for the Plant Barry Ash Pond was delineated based on LiDAR data acquired for the Plant in 2016. The SCS Runoff Curve Number method is developed by the United States Department of Agriculture (USDA) Soil Conservation Service (SCS) and is a method of estimating rainfall excess from rainfall (Hjelmfelt, 1991). Rainfall Distribution Figure B-2 Approximate geographic boundaries for NRCS (SCS) rainfall distributions Rainfall data sources This section lists the most current 24-hour rainfall data published by the National Weather Service (NWS) for various parts of the country. To partially compensate for this, the SCS Type I rainfall distribution has been used in place of the recommended, but more intense, Type II distribution. SCS 24-hour rainfall distributions (SCS, 1986): (y-axis reads "Fraction of 24-hour rainfall" and x-axis reads "Time, hours") 1 hour 6 hours 12 hours 24 hours 7 days. It is Although we recommend going to the NOAA site for rainfall information, we've provided rainfall frequency plots for several locations in Minnesota. Bulletin 71 (MCC Research Report 92-03) RAINFALL FREQUENCY ATLAS OF THE MIDWEST by Floyd A. Huff and James R. Angel Title: Rainfall Frequency Atlas of the Midwest. The Soil Conservation Service (SCS) (Wilkes 1980) has indicated that the SCS 24-hour Type" IIa rainfall distribution and 4 . SCS type II method is widely used by hydrologists in arid regions. The rainfall simulator’s performance was also validated through three, 60 minute bare soil control tests. Initial Design Rainfall (50 yr-24 hr) = 5.13” (TP-40 – Type II) Peak Q = 139.5 cfs Revised Design Rainfall = 5.53” (NOAA 14 – MSE 3 MN) Peak Q = 151 cfs Old TR-20 Input Data and use in New TR-20 System Input Table 5.3. Distribution of the rainfall depth across the 24-hour can be estimated using the SCS (NRCS) rainfall types (i.e. A Unit Hydrograph is constructed based on the drainage area’s characteristics, i.e., Curve Number (CN), Tc, etc. The easiest way to use these distributions is to define your rainfall events using the built-in event lookup table. With HydroCAD-10, you can also generate a synthetic rainfall distribution based on local precipitation frequency data. Details here. For special applications, you can create a custom rainfall table by hand. The distribution is the result of a calibration process performed by the District to provide, in conjunction with SCS (NRCS) Rainfall Types (Source Nicklow et al., 2006) Rules for Entering the SCS CN in the Dialogs. The cumulative 24-hour rainfall distributions for SCS Storm Types 1, 1A, and 2 are presented in Figure 1. Verification Tables Table 3.3. Table 4-1 lists the 24-hour point rainfall depths for various frequency storm events. The pond and swamp adjustment factor is ob-tained from table 4-2 (rounded to the nearest table value). A Design Storm is selected (Typically an NRCS 24-hr distribution). Time of concentration is only applied to surface runoff and shall be no less than 5 minutes for hydrologic analysis. Slide Chart Hydraulic Calculator for Pipe Flow. Table 2.1 Rainfall Characteristics in the District. • Soil Conservation Service (SCS) Unit Hydrograph Method; ... regarding intensity and distribution of the storm over the specified timeframe (24-hours for this scenario). Storm Type 3 is similar to the Type 2 distribution, and applies to eastern and south-eastern USA. Synthetic, Nested, Balanced, IDF-based: 1, 2, 3, 6 12, 24: Dimensionless distribution is automatically developed using current IDF curves and symmetrically arranged rainfall depths. SCS Method The SCS Method of time of concentration is a valid method to use for either the Rational Method, Usually the distributions are listed as tables of time vs cumulative percent of total rainfall (S curves when plotted). A Unit Hydrograph is constructed based on the drainage area’s characteristics, i.e., Curve Number (CN), Tc, etc. For larger drainage systems, the Austin Standard Method or the Soil Conservation Service hydrologic methods (available in TR-20, HEC-1 or the Tabular/Graphical methods) should be used. The monthly wise rainfall data has been converted as ... (Table-1). The SCS has developed several standard distributions that cover the entire US, commonly known as the Type I, IA, II, and III storms. For situations where a standard rainfall distribution is not available or appropriate, you can create a localized rainfall distribution table in the SCS Rainfall Library. A map of a multi-state area with a regional rainfall distribution was developed along with a 24-hour rainfall table … North Charleston. B-1. The Type II hyetograph is a standard SCS (NRCS) rainfall distribution that has a high-intensity peak. Rainfall Distribution Built-in Tables Table 3.2. Variable Rainfall Intensity Method are accepted as adequate for drainage areas totaling 100 acres or less. To develop a flood hydrograph, however, a time variable distribution (hyetograph) is required. standard 24-hour NRCS rainfall distributions 6-minute interval. A collection network can be developed in the graphical interface using a variety of methods. The goal was to identify regions of similar rainfall distribution. Methods listed in Table 2-1 have been selected for use in Lincoln, Nebraska based on several considerations, ... 23 SCS is the Soil Conservation Service Method. c (chapter 3), rainfall distribution type, and I a /P ratio. 2.2.2 Rainfall Hyetographs The rainfall data presented in Section 2.2.1 identify average depth or intensity over specific durations. Table 3 provides values of k for various land uses. Date/Time. 0 0 0 0 0 0 0 0. Create a column to store the cumulative rainfall values as shown below: Next, find S by using the equation above and CN = 80 to get S = 2.5 inch. Fig. The latitude, longitude, elevation, average rainfall of the rain gauge stations were discussed in the table 2.1. WinTR-20 Capabilities and Limitations Table 3.1. 40 (described in Precipitation). … Rainfall Frequency & Design Rainfall Distributions for Selected Pacific Islands (2008) SCS Standard Rainfall Distributions (.xlsx, 61.2 kb) SCS Rainfall Distributions, Time Transformations (.xlsx, 223 kb) Storm Distribution Developed from World Curve Data & Its Potential Areal Application (2003) Synthetic Regional Rainfall Time Distributions (1981) The SCS 24-hr. Parameter Estimation. Bhavani3 and E. G. Rajan4 1Department of Civil Engineering, Vasavi College of Engineering, Hyderabad, 2Institute of Science and Technology, J.N.T. Type I, Type IA, Type II and Type III) shown in the following figure. Different The Y-axis is dimensionless so that different rainfall depths can be applied to the distributions to create rainfall curves for various storm magnitudes and geographic locations. Rainfall … First-, second-, third-, and fourth-quartile median distributions ... including the SCS Type-II (supposedly applicable to the central and eastern United 2. The NRCS, in the supplement attached to the New Jersey Bulletin No. SCS 24-hour rainfall distributions. Multiply the percentages by the total (126.5 or 5.06) to get the rainfall accumulation for each time for your study. Therefore, a design storm event is used to estimate actual storm events even though it ... Table 3-5. Procedure - Find out the initial abstraction for the rainfall amount, P, using the table provided below or using the formula S=[(1000/CN)-10] with I a =0.2S. - Then depending on your region of study, use one of the exhibit for either Type I, IA, II or III rainfall distribution for … GEOPAK Drainage Course Guide/Users Manual (Link to PDF File) DIRECT LINK: Hydraulic Calculator. The SCS 24-hour rainfall distributions are shown in Figure 1, with the corresponding geographic boundaries shown in Figure 2. Hydrographs were roupd downstream using SCS methodology. R3:T27 Calculations for the adjustment of point rainfall distributed over drainage areas greater than 10 square miles. interpolation tool is used to distribute the rainfall data in each rain gauge stations spatially. Hourly rainfall data and distribution at Columbus Ohio, August 30, 2005 ..... 46 87 88 Table 4A‐ 1. Mass rainfall is converted to mass runoff by using a runoff CN that is based on soil type, plant cover, amount of impervious areas, interception, and surface storage. V23:W106 Table which associates each county with a precipitation region. The rules are listed below but in paragraph style. Type I, Type IA, Type II and Type III) shown in the following figure. Time distribution of point rainfall in fourth-quartile storms..... 13 13. Tables Table 1.1. iSWMTM Technical Manual Hydrology Hydrology: 1.0 Hydrological Analysis 2.0 Downstream Assessment 3.0 Streambank Protection 4.0 Water Balance 5.0 Rainfall Tables 6.0 Hydrologic Soils Data Also known as Balanced Storm. For your 24 hr Type III distribution, the total rainfall from your table is 126.5 mm or 5.06 inches. Control / Editor for WinTR-20 Input File Table 3.4. 2-IA Unit peak discharge (q, ) for SCS Type IA rainfall distribution ..... 2-12 2-11 Unit peak discharge (q, ) for SCS Type I1 rain- fall distribution ... storm duration and associated synthetic rainfall distribution can be used to estimate peak discharges for a wide range ... as shown in table … The design rainfall for this site was derived using the SCS (NRCS) Type IA 24-Hr Storm Distributions as this project site is located within the geographic boundaries of the specified Type IA rainfall distribution. To partially compensate for this, the SCS Type I rainfall distribution has been used in place of the recommended, but more intense, Type II distribution. table f-1 design storm rainfall amount figure f-1 alternating block method for rainfall distribution figure f-2 penndot delineated regions figure f-3 nrcs (scs) type ii rainfall distribution – s curve figure f-4 penndot region 5 storm intensity-duration-frequency curve table f-2 runoff curve numbers The rainfall distribution values were taken from the February 2013 tables provided by … table f-1 design storm rainfall amount figure f-1 alternating block method for rainfall distribution figure f-2 penndot delineated regions figure f-3 nrcs (scs) type ii rainfall distribution – s curve figure f-4 penndot region 5 storm intensity-duration-frequency curve table f-2 runoff curve numbers Over the years, use of the SCS dimensionless hydrograph consistently overestimates discharges when compared to recorded gage flows for Michigan streams. Because the SCS CN method is based on computing excess rainfall from total rainfall, the given rainfall hyetograph is first converted into a cumulative rainfall hyetograph or rainfall mass curve so it will represent the total amount of rainfall after each time step since the beginning of the storm. This program will take a cumulative rainfall total and distribute it incrementally over a set storm time period. SCS Runoff Curve Number Method. The method is described in detail in National Engineering Handbook (2004). The most common are the SCS/NRCS rainfalls listed at the top of the table. To see a comparison of Atlas 14 and TP-40, link here. Because NWS Technical Paper 40 (TP-40) is out of print, the 24-hour rainfall For example, if the total rainfall is 100 mm, the depth of water application is 50 mm and consumptive use is 150 mm, then the effective rainfall under the deep water table conditions is 2.97 x 0.93 x 25» 69 mm. Graphic Output Table 5.1. Note** If you are interested in obtaining an h-calculator, please contact the Drainage Section. For example, a fully described storm would be: 4.5 inches of rain, of 24 hour duration, having a type III distribution and a return frequency of 10 years. Runoff characteristics were developed based on the Soil Conservation Service (SCS) methodologies as outlined in TR-55. It will distribute rainfall over SCS Type I, II, or III storm patterns or a user specified pattern. 2.2 SCS-CN Runoff Estimation Runoff was estimated using the SCS Runoff CN Method which relies on a composite curve number of an average antecedent moisture condition, assigned to each catchment and rainfall depth Y23:AB40 Precipitation amounts for each region. Rainfall Distribution Tables HydroCAD provides several options for defining the rainfall distribution to be used with the SCS or SBUH runoff procedures. Equations (SCS, … The SCS CN Method begins with a rainfall amount uniformly imposed on the watershed over a specified time distribution. Figure 3-6 The Modified NOAA—SCS Rainfall Distribution Worksheet 3 … 85 Table 4‐ 5. rainfall distributions are classic examples of dimensionless depth rainfall distributions. They are the amount of rain, the storm duration, the rainfall distribution, and the return frequency. Over the years, use of the SCS dimensionless hydrograph consistently overestimates discharges when compared to recorded gage flows for Michigan streams. Figure 1: Cumulative 24-hour Rainfall Distributions for SCS Storm Types 1, 1A, and 2 (after SCS, 1986) Type 2 rainfall distribution (Figure 4-1) will be used. The rules are listed below but in paragraph style. Hydrographs were synthesized using Soil Conservation Service (SCS) unit hydrographs and the SCS recommended 5-year, 24-hour rainfall distribution. Use worksheet 4 in appendix D to aid in com-puting the peak discharge using the Graphical method. depth used to develop the design storm. The monthly wise rainfall data has been converted as ... (Table-1). Runoff is then The 24-hour rainfall distribution includes the maximum rainfall distribution … Volume 2 (Technical Handbook) Georgia Stormwater Management Manual 3.1-1 CHAPTER 3 STORMWATER HYDROLOGY Table of Contents SECTION 3.1 METHODS FOR ESTIMATING STORMWATER RUNOFF In Part 1, you will learn how to utilize XP tools to layout a collection system network over GIS background images and develop input data from information in GIS files. Cherokee County, Alabama. Soil Conservation Service Type II Storm Distribution Time/Total Time Rainfall/Total Rainfall Time/Total Time Rainfall/Total Rainfall 0.000 0.000 0.520 0.730 0.040 0.010 0.530 0.750 0.100 0.025 0.540 0.770 0.150 0.040 0.550 0.780 0.200 0.060 0.560 0.800 area. c (chapter 3), rainfall distribution type, and I a /P ratio. Rainfall: To fully describe a precipitation event, four parameters must be used. Top of page Old TR-20 Input Data Methods listed in Table 2-1 have been selected for use in Lincoln, Nebraska based on several considerations, includ- ... 3 SCS is the Soil Conservation Service Method. The temporal distribution presented in Table RA-2 represents a design storm for use with a distributed rainfall-runoff routing model. It has been used in eastern Washington since the 1970s and is also used throughout much of the United States. Commands vs. Data Sections Table 5.2. A land use grid layer will be eventually be deployed, which will provide similar land use types and corresponding k values as illustrated in Table 3. The United States Environmental Protection Agency (EPA) Storm Water Management Model is a dynamic rainfall–runoff–subsurface runoff simulation model used for single-event to long-term (continuous) simulation of the surface/subsurface hydrology quantity and quality from primarily urban/suburban areas. The method of analysis must remain distribution characteristics of rainfall during heavy storms.Since the previous demand had not been strong, this information was not readily available.Some limited work on storm rainfall profiles (time distributions) had been done by the U.S. Army Corps of The mass rainfall curve, illustrated in Figure 4-13, is the cumulative precipitation up to a specific time. Use worksheet 4 in appendix D to aid in com-puting the peak discharge using the Graphical method. There are four steps involved in calculating NRCS runoff hydrographs. Here are all of the SCS rainfall distributions in a text file that can be imported into XP-SWMM directly or opened and parsed in Excel, etc. The advantage of the SCS Type II profile is in the distribution. Do not be alarmed. Precipitation in inches. 2.1-2 Columbia County Stormwater Management Design Manual Chapter 2 Section 2.1 For contributing drainage areas of 100 acres or greater, the SCS Unit Hydrograph Method shall be used as a minimum. Maps of these rainfall ratios were developed using Geographic Information System (GIS) technology. 2.2 Huff Temporal Rainfall Distribution When using the Kinematic Wave Method or SCS Method for runoff computations, the Huff rainfall distribution shall be used for the temporal distribution. SCS 24-hour rainfall distributions (SCS, 1986). TABLE 3-3 Runoff Depth Rainfall Curve Number (CN)1 (inches) The rainfall is converted to runoff with the Runoff Curve Number method. formerly the Soil Conservation Service (SCS) in Janu-ary 1975, TR-55 incorporates current SCS procedures. The design rainfall for this site was derived using the SCS (NRCS) Type IA 24-Hr Storm Distributions as this project site is located within the geographic boundaries of the specified Type IA rainfall distribution. HydroCAD provides several options for defining the rainfall distribution to be used with the SCS or SBUH runoff procedures. Most projects will use one of the predefined rainfall distributions listed below. The most common are the SCS/NRCS rainfalls listed at the top of the table. (c) Rainfall Distribution Types Four new rainfall distribution types (NOAA A, NOAA B, NOAA C, and NOAA D) were developed from the NOAA 14 data for the standard SCS unit hydrograph (dimensionless unit hydrograph peak factor of 484). The output is a HEC-1 input ready table of incremental rainfall depths. Time distribution of point rainfall in third-quartile storms ..... 13 12. COOSA RIVER AT … The rainfall distribution by Thiessen polygon method was adopted. intense rainfall at the beginning and end of the rainfall distribution. Maps of these rainfall ratios were developed using Geographic Information System (GIS) technology. EPA/600/R-13/085g Revised July 2019 NATIONAL STORMWATER CALCULATOR USER’S GUIDE – VERSION 2.0.0.1 By Lewis A. Rossman Water Systems … Soil Conservation Service Type II Storm Distribution Time/Total Time Rainfall/Total Rainfall Time/Total Time Rainfall/Total Rainfall 0.000 0.000 0.520 0.730 0.040 0.010 0.530 0.750 0.100 0.025 0.540 0.770 0.150 0.040 0.550 0.780 The Huff distribution is presented in Table RO-3 and is expressed as cumulative percentages of total duration and total rainfall accumulation. The hyetograph is a graph of the time distribution of rainfall (usually expressed as an intensity) over a watershed. A Design Storm is selected (Typically an NRCS 24-hr distribution). triangular unit hydrographs are suitable for flood predictions for the rural watersheds in … TABLE 3-2 RAINFALL DATA TABLE DESIGN STORM 24-HOUR PRECIPITATION (YEARS) (INCHES) 2 3.5 5 4.5 10 5.2 25 6.0 50 6.8 100 7.5 b. Uniformity of rainfall distribution ranged from 79-81%. SCS 24-hr rainfall distribution type graph Geographic boundaries within the USA for SCS rainfall distributions 24-hr duration rainfall maps of USA with return periods of: 2-yr 5-yr 10-yr 25-yr 50-yr 100-yr .

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Amennyiben Önt letartóztatják, előállítják, akkor egy meggondolatlan mondat vagy ésszerűtlen döntés később az eljárás folyamán óriási hátrányt okozhat Önnek.

Tapasztalatom szerint már a kihallgatás első percei is óriási pszichikai nyomást jelentenek a terhelt számára, pedig a „tiszta fejre” és meggondolt viselkedésre ilyenkor óriási szükség van. Ez az a helyzet, ahol Ön nem hibázhat, nem kockáztathat, nagyon fontos, hogy már elsőre jól döntsön!

Védőként én nem csupán segítek Önnek az eljárás folyamán az eljárási cselekmények elvégzésében (beadvány szerkesztés, jelenlét a kihallgatásokon stb.) hanem egy kézben tartva mérem fel lehetőségeit, kidolgozom védelmének precíz stratégiáit, majd ennek alapján határozom meg azt az eszközrendszert, amellyel végig képviselhetem Önt és eredményül elérhetem, hogy semmiképp ne érje indokolatlan hátrány a büntetőeljárás következményeként.

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Még mindig él a cégvezetőkben az a tévképzet, hogy ügyvédet választani egy vállalkozás vagy társaság számára elegendő akkor, ha bíróságra kell menni.

Semmivel sem árthat annyit cége nehezen elért sikereinek, mint, ha megfelelő jogi képviselet nélkül hagyná vállalatát!

Irodámban egyedi megállapodás alapján lehetőség van állandó megbízás megkötésére, melynek keretében folyamatosan együtt tudunk működni, bármilyen felmerülő kérdés probléma esetén kereshet személyesen vagy telefonon is.  Ennek nem csupán az az előnye, hogy Ön állandó ügyfelemként előnyt élvez majd időpont-egyeztetéskor, hanem ennél sokkal fontosabb, hogy az Ön cégét megismerve személyesen kezeskedem arról, hogy tevékenysége folyamatosan a törvényesség talaján maradjon. Megismerve az Ön cégének munkafolyamatait és folyamatosan együttműködve vezetőséggel a jogi tudást igénylő helyzeteket nem csupán utólag tudjuk kezelni, akkor, amikor már „ég a ház”, hanem előre felkészülve gondoskodhatunk arról, hogy Önt ne érhesse meglepetés.

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