Hydrologic Evaluation of Landfill Performance (HELP) model: Para la DRAFT. Expansión Lateral Del Sistema de Rellenos Sanitarios Municipal de Juncos
|
|
- Jerome Walsh
- 5 years ago
- Views:
Transcription
1 Hydrologic Evaluation of Landfill Performance (HELP) model: Para la Expansión Lateral Del Sistema de Rellenos Sanitarios Municipal de Juncos Preparado para: Srta. Glenda Viera Por: Ing. Miguel Antonio García Campos, PE Designer and Consultant 14 de julio de 2008 Phone: Fax:
2 ****************************************************************************** ****************************************************************************** ** ** ** ** ** HYDROLOGIC EVALUATION OF LANDFILL PERFORMANCE ** ** HELP MODEL VERSION 3.07 (1 November 1997) ** ** DEVELOPED BY ENVIRONMENTAL LABORATORY ** ** USAE WATERWAYS EXPERIMENT STATION ** ** FOR USEPA RISK REDUCTION ENGINEERING LABORATORY ** ** ** ** ** ****************************************************************************** ****************************************************************************** PRECIPITATION DATA FILE: TEMPERATURE DATA FILE: C:\WHI\VHELP22\data\P286.VHP\_weather1.dat C:\WHI\VHELP22\data\P286.VHP\_weather2.dat SOLAR RADIATION DATA FILE: C:\WHI\VHELP22\data\P286.VHP\_weather3.dat EVAPOTRANSPIRATION DATA: C:\WHI\VHELP22\data\P286.VHP\_weather4.dat SOIL AND DESIGN DATA FILE: C:\WHI\VHELP22\data\P286.VHP\I_ inp OUTPUT DATA FILE: TIME: 11:07 DATE: 7/14/2008 C:\WHI\VHELP22\data\P286.VHP\O_ prt ****************************************************************************** TITLE: Designed Cell For Lateral Expansion SRSM Juncos ****************************************************************************** NOTE: INITIAL MOISTURE CONTENT OF THE LAYERS AND SNOW WATER WERE COMPUTED AS NEARLY STEADY-STATE VALUES BY THE PROGRAM. Page 1
3 LAYER TYPE 1 - VERTICAL PERCOLATION LAYER MATERIAL TEXTURE NUMBER 9 THICKNESS = CM POROSITY = VOL/VOL FIELD CAPACITY = VOL/VOL WILTING POINT = VOL/VOL INITIAL SOIL WATER CONTENT = VOL/VOL EFFECTIVE SAT. HYD. COND. = E-03 CM/SEC NOTE: SATURATED HYDRAULIC CONDUCTIVITY IS MULTIPLIED BY 5.00 FOR ROOT CHANNELS IN TOP HALF OF EVAPORATIVE ZONE. LAYER TYPE 1 - VERTICAL PERCOLATION LAYER MATERIAL TEXTURE NUMBER 18 THICKNESS = CM POROSITY = VOL/VOL FIELD CAPACITY = VOL/VOL WILTING POINT = VOL/VOL INITIAL SOIL WATER CONTENT = VOL/VOL EFFECTIVE SAT. HYD. COND. = E-02 CM/SEC NOTE: PERCENT OF THE DRAINAGE COLLECTED FROM LAYER # 4 IS RECIRCULATED INTO THIS LAYER. LAYER TYPE 2 - LATERAL DRAINAGE LAYER MATERIAL TEXTURE NUMBER 1 THICKNESS = CM POROSITY = VOL/VOL FIELD CAPACITY = VOL/VOL WILTING POINT = VOL/VOL INITIAL SOIL WATER CONTENT = VOL/VOL EFFECTIVE SAT. HYD. COND. = E-01 CM/SEC LAYER TYPE 2 - LATERAL DRAINAGE LAYER MATERIAL TEXTURE NUMBER 34 THICKNESS = 0.60 CM POROSITY = VOL/VOL FIELD CAPACITY = VOL/VOL WILTING POINT = VOL/VOL INITIAL SOIL WATER CONTENT = VOL/VOL EFFECTIVE SAT. HYD. COND. = CM/SEC SLOPE = 2.00 PERCENT DRAINAGE LENGTH = 45.7 METERS NOTE: PERCENT OF THE DRAINAGE COLLECTED FROM THIS Page 2
4 LAYER IS RECIRCULATED INTO LAYER # 2. LAYER TYPE 4 - FLEXIBLE MEMBRANE LINER MATERIAL TEXTURE NUMBER 35 THICKNESS = 0.10 CM POROSITY = VOL/VOL FIELD CAPACITY = VOL/VOL WILTING POINT = VOL/VOL INITIAL SOIL WATER CONTENT = VOL/VOL EFFECTIVE SAT. HYD. COND. = E-12 CM/SEC FML PINHOLE DENSITY = 2.00 HOLES/HECTARE FML INSTALLATION DEFECTS = 2.00 HOLES/HECTARE FML PLACEMENT QUALITY = 4 - POOR LAYER TYPE 3 - BARRIER SOIL LINER MATERIAL TEXTURE NUMBER 15 THICKNESS = CM POROSITY = VOL/VOL FIELD CAPACITY = VOL/VOL WILTING POINT = VOL/VOL INITIAL SOIL WATER CONTENT = VOL/VOL EFFECTIVE SAT. HYD. COND. = E-06 CM/SEC GENERAL DESIGN AND EVAPORATIVE ZONE DATA NOTE: SCS RUNOFF CURVE NUMBER WAS COMPUTED FROM DEFAULT SOIL DATA BASE USING SOIL TEXTURE # 9 WITH BARE GROUND CONDITIONS, A SURFACE SLOPE OF 0.% AND A SLOPE LENGTH OF 0. METERS. SCS RUNOFF CURVE NUMBER = 0.00 FRACTION OF AREA ALLOWING RUNOFF = 25.0 PERCENT AREA PROJECTED ON HORIZONTAL PLANE = HECTARES EVAPORATIVE ZONE DEPTH = 25.4 CM INITIAL WATER IN EVAPORATIVE ZONE = CM UPPER LIMIT OF EVAPORATIVE STORAGE = CM LOWER LIMIT OF EVAPORATIVE STORAGE = CM INITIAL SNOW WATER = CM INITIAL WATER IN LAYER MATERIALS = CM TOTAL INITIAL WATER = CM TOTAL SUBSURFACE INFLOW = 0.00 MM/YR EVAPOTRANSPIRATION AND WEATHER DATA Page 3
5 NOTE: EVAPOTRANSPIRATION DATA WAS OBTAINED FROM SAN JUAN/ISLA VE PUER STATION LATITUDE = DEGREES MAXIMUM LEAF AREA INDEX = 5.00 START OF GROWING SEASON (JULIAN DATE) = 85 END OF GROWING SEASON (JULIAN DATE) = 57 EVAPORATIVE ZONE DEPTH = 10.0 INCHES AVERAGE ANNUAL WIND SPEED = MPH AVERAGE 1ST QUARTER RELATIVE HUMIDITY = % AVERAGE 2ND QUARTER RELATIVE HUMIDITY = % AVERAGE 3RD QUARTER RELATIVE HUMIDITY = % AVERAGE 4TH QUARTER RELATIVE HUMIDITY = % NOTE: PRECIPITATION DATA WAS SYNTHETICALLY GENERATED USING COEFFICIENTS FOR SAN JUAN/ISLA VE PUER NORMAL MEAN MONTHLY PRECIPITATION (INCHES) JAN/JUL FEB/AUG MAR/SEP APR/OCT MAY/NOV JUN/DEC NOTE: TEMPERATURE DATA WAS SYNTHETICALLY GENERATED USING COEFFICIENTS FOR SAN JUAN/ISLA VE PUER NORMAL MEAN MONTHLY TEMPERATURE (DEGREES FAHRENHEIT) JAN/JUL FEB/AUG MAR/SEP APR/OCT MAY/NOV JUN/DEC NOTE: SOLAR RADIATION DATA WAS SYNTHETICALLY GENERATED USING COEFFICIENTS FOR SAN JUAN/ISLA VE PUER AND STATION LATITUDE = DEGREES HEAD #1: AVERAGE HEAD ON TOP OF LAYER 5 DRAIN #1: LATERAL DRAINAGE FROM LAYER 4 (RECIRCULATION AND COLLECTION) LEAK #1: PERCOLATION OR LEAKAGE THROUGH LAYER 6 ********************************************************************** DAILY OUTPUT FOR YEAR S DAY A O RAIN RUNOFF ET E. ZONE HEAD DRAIN LEAK I I WATER #1 #1 #1 Page 4
6 R L IN. IN. IN. IN./IN. IN. IN. IN E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E-07 Page 5
7 E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E-07 Page 6
8 E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E-07 Page 7
9 E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E-07 Page 8
10 E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E-07 Page 9
11 E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E-07 ********************************************************************** MONTHLY TOTALS (IN INCHES) FOR YEAR 1 Page 10
12 JAN/JUL FEB/AUG MAR/SEP APR/OCT MAY/NOV JUN/DEC PRECIPITATION RUNOFF EVAPOTRANSPIRATION LATERAL DRAINAGE RECIRCULATED INTO LAYER LATERAL DRAINAGE COLLECTED FROM LAYER LATERAL DRAINAGE RECIRCULATED FROM LAYER PERCOLATION/LEAKAGE THROUGH LAYER MONTHLY SUMMARIES FOR DAILY HEADS (INCHES) AVERAGE DAILY HEAD ON TOP OF LAYER STD. DEVIATION OF DAILY HEAD ON TOP OF LAYER ANNUAL TOTALS FOR YEAR 1 INCHES CU. FEET PERCENT PRECIPITATION RUNOFF EVAPOTRANSPIRATION RECIRCULATION INTO LAYER DRAINAGE COLLECTED FROM LAYER RECIRCULATION FROM LAYER PERC./LEAKAGE THROUGH LAYER AVG. HEAD ON TOP OF LAYER CHANGE IN WATER STORAGE Page 11
13 SOIL WATER AT START OF YEAR SOIL WATER AT END OF YEAR SNOW WATER AT START OF YEAR SNOW WATER AT END OF YEAR ANNUAL WATER BUDGET BALANCE HEAD #1: AVERAGE HEAD ON TOP OF LAYER 5 DRAIN #1: LATERAL DRAINAGE FROM LAYER 4 (RECIRCULATION AND COLLECTION) LEAK #1: PERCOLATION OR LEAKAGE THROUGH LAYER 6 ********************************************************************** DAILY OUTPUT FOR YEAR S DAY A O RAIN RUNOFF ET E. ZONE HEAD DRAIN LEAK I I WATER #1 #1 #1 R L IN. IN. IN. IN./IN. IN. IN. IN E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E-07 Page 12
14 E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E-06 Page 13
15 E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E-06 Page 14
16 E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E-06 Page 15
17 E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E-06 Page 16
18 E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E-06 Page 17
19 E E E E E E E E E E E E E E E E E E E E-06 ********************************************************************** MONTHLY TOTALS (IN INCHES) FOR YEAR 2 JAN/JUL FEB/AUG MAR/SEP APR/OCT MAY/NOV JUN/DEC PRECIPITATION RUNOFF EVAPOTRANSPIRATION LATERAL DRAINAGE RECIRCULATED INTO LAYER LATERAL DRAINAGE COLLECTED FROM LAYER LATERAL DRAINAGE RECIRCULATED FROM LAYER PERCOLATION/LEAKAGE THROUGH LAYER MONTHLY SUMMARIES FOR DAILY HEADS (INCHES) AVERAGE DAILY HEAD ON TOP OF LAYER Page 18
20 STD. DEVIATION OF DAILY HEAD ON TOP OF LAYER ANNUAL TOTALS FOR YEAR 2 INCHES CU. FEET PERCENT PRECIPITATION RUNOFF EVAPOTRANSPIRATION RECIRCULATION INTO LAYER DRAINAGE COLLECTED FROM LAYER RECIRCULATION FROM LAYER PERC./LEAKAGE THROUGH LAYER AVG. HEAD ON TOP OF LAYER CHANGE IN WATER STORAGE SOIL WATER AT START OF YEAR SOIL WATER AT END OF YEAR SNOW WATER AT START OF YEAR SNOW WATER AT END OF YEAR ANNUAL WATER BUDGET BALANCE HEAD #1: AVERAGE HEAD ON TOP OF LAYER 5 DRAIN #1: LATERAL DRAINAGE FROM LAYER 4 (RECIRCULATION AND COLLECTION) LEAK #1: PERCOLATION OR LEAKAGE THROUGH LAYER 6 ********************************************************************** DAILY OUTPUT FOR YEAR S DAY A O RAIN RUNOFF ET E. ZONE HEAD DRAIN LEAK I I WATER #1 #1 #1 R L IN. IN. IN. IN./IN. IN. IN. IN Page 19
21 E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E E-06 Page 20
12 SWAT USER S MANUAL, VERSION 98.1
12 SWAT USER S MANUAL, VERSION 98.1 CANOPY STORAGE. Canopy storage is the water intercepted by vegetative surfaces (the canopy) where it is held and made available for evaporation. When using the curve
More informationSOUTH MOUNTAIN WEATHER STATION: REPORT FOR QUARTER 2 (APRIL JUNE) 2011
SOUTH MOUNTAIN WEATHER STATION: REPORT FOR QUARTER 2 (APRIL JUNE) 2011 Prepared for ESTANCIA BASIN WATERSHED HEALTH, RESTORATION AND MONITORING STEERING COMMITTEE c/o CLAUNCH-PINTO SOIL AND WATER CONSERVATION
More informationONE DIMENSIONAL CLIMATE MODEL
JORGE A. RAMÍREZ Associate Professor Water Resources, Hydrologic and Environmental Sciences Civil Wngineering Department Fort Collins, CO 80523-1372 Phone: (970 491-7621 FAX: (970 491-7727 e-mail: Jorge.Ramirez@ColoState.edu
More informationAppendix D. Model Setup, Calibration, and Validation
. Model Setup, Calibration, and Validation Lower Grand River Watershed TMDL January 1 1. Model Selection and Setup The Loading Simulation Program in C++ (LSPC) was selected to address the modeling needs
More informationEvapotranspiration. Rabi H. Mohtar ABE 325
Evapotranspiration Rabi H. Mohtar ABE 325 Introduction What is it? Factors affecting it? Why we need to estimate it? Latent heat of vaporization: Liquid gas o Energy needed o Cooling process Saturation
More informationThe Climate of Marshall County
The Climate of Marshall County Marshall County is part of the Crosstimbers. This region is a transition region from the Central Great Plains to the more irregular terrain of southeastern Oklahoma. Average
More informationThe Climate of Bryan County
The Climate of Bryan County Bryan County is part of the Crosstimbers throughout most of the county. The extreme eastern portions of Bryan County are part of the Cypress Swamp and Forest. Average annual
More informationThe Climate of Pontotoc County
The Climate of Pontotoc County Pontotoc County is part of the Crosstimbers. This region is a transition region from the Central Great Plains to the more irregular terrain of southeast Oklahoma. Average
More informationThe Climate of Payne County
The Climate of Payne County Payne County is part of the Central Great Plains in the west, encompassing some of the best agricultural land in Oklahoma. Payne County is also part of the Crosstimbers in the
More informationThe Climate of Kiowa County
The Climate of Kiowa County Kiowa County is part of the Central Great Plains, encompassing some of the best agricultural land in Oklahoma. Average annual precipitation ranges from about 24 inches in northwestern
More informationThe Climate of Murray County
The Climate of Murray County Murray County is part of the Crosstimbers. This region is a transition between prairies and the mountains of southeastern Oklahoma. Average annual precipitation ranges from
More informationThe Climate of Seminole County
The Climate of Seminole County Seminole County is part of the Crosstimbers. This region is a transition region from the Central Great Plains to the more irregular terrain of southeastern Oklahoma. Average
More informationThe Climate of Texas County
The Climate of Texas County Texas County is part of the Western High Plains in the north and west and the Southwestern Tablelands in the east. The Western High Plains are characterized by abundant cropland
More informationThe Climate of Grady County
The Climate of Grady County Grady County is part of the Central Great Plains, encompassing some of the best agricultural land in Oklahoma. Average annual precipitation ranges from about 33 inches in northern
More informationSoil Water Atmosphere Plant (SWAP) Model: I. INTRODUCTION AND THEORETICAL BACKGROUND
Soil Water Atmosphere Plant (SWAP) Model: I. INTRODUCTION AND THEORETICAL BACKGROUND Reinder A.Feddes Jos van Dam Joop Kroes Angel Utset, Main processes Rain fall / irrigation Transpiration Soil evaporation
More informationThe Climate of Haskell County
The Climate of Haskell County Haskell County is part of the Hardwood Forest. The Hardwood Forest is characterized by its irregular landscape and the largest lake in Oklahoma, Lake Eufaula. Average annual
More information2. Irrigation. Key words: right amount at right time What if it s too little too late? Too much too often?
2. Irrigation Key words: right amount at right time What if it s too little too late? 2-1 Too much too often? To determine the timing and amount of irrigation, we need to calculate soil water balance.
More informationCHAPTER-11 CLIMATE AND RAINFALL
CHAPTER-11 CLIMATE AND RAINFALL 2.1 Climate Climate in a narrow sense is usually defined as the "average weather", or more rigorously, as the statistical description in terms of the mean and variability
More informationClimatic Change Implications for Hydrologic Systems in the Sierra Nevada
Climatic Change Implications for Hydrologic Systems in the Sierra Nevada Part Two: The HSPF Model: Basis For Watershed Yield Calculator Part two presents an an overview of why the hydrologic yield calculator
More informationQuick Reference Guide
Vantage PRO Davis Instruments 3465 Diablo Ave, Hayward, CA 94545 U.S.A. Phone (510) 732 9229 Fax (510) 732 9188 www.davisnet.com E-mail: sales@davisnet.com support@davisnet.com Quick Reference Guide Part
More informationUNIT 12: THE HYDROLOGIC CYCLE
UNIT 12: THE HYDROLOGIC CYCLE After Unit 12 you should be able to: o Effectively use the charts Average Chemical Composition of Earth s Crust, Hydrosphere and Troposphere, Selected Properties of Earth
More informationAppendix 2: Hydrometeorology and Hydroclimatology of Baseflow. Page 1 of 19
Appendix 2: Hydrometeorology and Hydroclimatology of Baseflow Page 1 of 19 A time series of end of month soil moisture data was developed for each climate division in the United States from 1931 to present
More information1., annual precipitation is greater than annual evapotranspiration. a. On the ocean *b. On the continents
CHAPTER 6 HUMIDITY, SATURATION, AND STABILITY MULTIPLE CHOICE QUESTIONS 1., annual precipitation is greater than annual evapotranspiration. a. On the ocean *b. On the continents 2., annual precipitation
More informationRegional Precipitation and ET Patterns: Impacts on Agricultural Water Management
Regional Precipitation and ET Patterns: Impacts on Agricultural Water Management Christopher H. Hay, PhD, PE Ag. and Biosystems Engineering South Dakota State University 23 November 2010 Photo: USDA-ARS
More informationClimate Dataset: Aitik Closure Project. November 28 th & 29 th, 2018
1 Climate Dataset: Aitik Closure Project November 28 th & 29 th, 2018 Climate Dataset: Aitik Closure Project 2 Early in the Closure Project, consensus was reached to assemble a long-term daily climate
More informationForest Hydrology: Lect. 9. Contents. Runoff, soil water and infiltration
Forest Hydrology: Lect. 9 Contents Runoff, soil water and infiltration Learning objectives:. - Hillslope runoff generation processes; - Dynamics of runoff generation processes; - Hortonian and Dunnian
More informationBreak Time. Cornell Short Course
Break Time Poor Plant Health Root Depth & Soil Type Active Root Zone The depth of soil containing the majority of feeder roots } Soil type Basic infiltration rate (mm/hour) } Sand > 30 (1.2-4 in./hr.)
More informationResearch Note COMPUTER PROGRAM FOR ESTIMATING CROP EVAPOTRANSPIRATION IN PUERTO RICO 1,2. J. Agric. Univ. P.R. 89(1-2): (2005)
Research Note COMPUTER PROGRAM FOR ESTIMATING CROP EVAPOTRANSPIRATION IN PUERTO RICO 1,2 Eric W. Harmsen 3 and Antonio L. González-Pérez 4 J. Agric. Univ. P.R. 89(1-2):107-113 (2005) Estimates of crop
More informationLOCAL CLIMATOLOGICAL DATA Monthly Summary July 2013
Deg. Days Precip Ty Precip Wind Solar Hu- Adj. to Sea Level mid- ity Avg Res Res Peak Minute 1 fog 2 hvy fog 3 thunder 4 ice plt 5 hail 6 glaze 7 duststm 8 smk, hz 9 blw snw 1 2 3 4A 4B 5 6 7 8 9 12 14
More informationPresented by Jerry A. Gomez, P.E. National Hydropower Association Northeast Regional Meeting - September 17, 2009
Presented by Jerry A. Gomez, P.E. National Hydropower Association Northeast Regional Meeting - September 17, 2009 Defining Probable Maximum Precipitation (PMP) PMP is the theoretically greatest depth of
More informationHydrologic Modelling of the Upper Malaprabha Catchment using ArcView SWAT
Hydrologic Modelling of the Upper Malaprabha Catchment using ArcView SWAT Technical briefs are short summaries of the models used in the project aimed at nontechnical readers. The aim of the PES India
More informationLOCAL CLIMATOLOGICAL DATA Monthly Summary September 2016
Deg. Days Precip Ty Precip Wind Solar Hu- Adj. to Sea Level mid- ity Avg Res Res Peak 2 Minute 1 fog 2 hvy fog 3 thunder 4 ice plt 5 hail 6 glaze 7 duststm 8 smk, hz 9 blw snw 1 2 3 4A 4B 5 6 7 8 9 11
More informationAtmospheric Sciences 321. Science of Climate. Lecture 14: Surface Energy Balance Chapter 4
Atmospheric Sciences 321 Science of Climate Lecture 14: Surface Energy Balance Chapter 4 Community Business Check the assignments HW #4 due Today, HW#5 is posted Quiz Today on Chapter 3, too. Mid Term
More informationGreat Lakes Update. Volume 199: 2017 Annual Summary. Background
Great Lakes Update Volume 199: 2017 Annual Summary Background The U.S. Army Corps of Engineers (USACE) tracks and forecasts the water levels of each of the Great Lakes. This report is primarily focused
More informationTable 1 - Infiltration Rates
Stantec Consulting Ltd. 100-300 Hagey Boulevard, Waterloo ON N2L 0A4 November 14, 2017 File: 161413228/10 Attention: Mr. Michael Witmer, BES, MPA, MCIP, RPP City of Guelph 1 Carden Street Guelph ON N1H
More informationVermont Soil Climate Analysis Network (SCAN) sites at Lye Brook and Mount Mansfield
Vermont Soil Climate Analysis Network (SCAN) sites at Lye Brook and Mount Mansfield 13 Years of Soil Temperature and Soil Moisture Data Collection September 2000 September 2013 Soil Climate Analysis Network
More informationName the surface winds that blow between 0 and 30. GEO 101, February 25, 2014 Monsoon Global circulation aloft El Niño Atmospheric water
GEO 101, February 25, 2014 Monsoon Global circulation aloft El Niño Atmospheric water Name the surface winds that blow between 0 and 30 What is the atmospheric pressure at 0? What is the atmospheric pressure
More informationAssimilation of satellite derived soil moisture for weather forecasting
Assimilation of satellite derived soil moisture for weather forecasting www.cawcr.gov.au Imtiaz Dharssi and Peter Steinle February 2011 SMOS/SMAP workshop, Monash University Summary In preparation of the
More informationNIDIS Intermountain West Drought Early Warning System July 18, 2017
NIDIS Drought and Water Assessment NIDIS Intermountain West Drought Early Warning System July 18, 2017 Precipitation The images above use daily precipitation statistics from NWS COOP, CoCoRaHS, and CoAgMet
More informationVantage PRO2 Quick. Reference Guide
Vantage PRO2 Quick Reference Guide INTRO This Quick Reference Guide will provide you with abbreviated instructions for all functions of the Vantage Pro2 console. For more detailed instructions, see Vantage
More informationColorado State University, Fort Collins, CO Weather Station Monthly Summary Report
Colorado State University, Fort Collins, CO Weather Station Monthly Summary Report Month: December Year: 2016 Temperature: Mean T max was 39.7 F which is 3.1 below the 1981-2010 normal for the month. This
More informationVariability of Reference Evapotranspiration Across Nebraska
Know how. Know now. EC733 Variability of Reference Evapotranspiration Across Nebraska Suat Irmak, Extension Soil and Water Resources and Irrigation Specialist Kari E. Skaggs, Research Associate, Biological
More informationLake Tahoe Watershed Model. Lessons Learned through the Model Development Process
Lake Tahoe Watershed Model Lessons Learned through the Model Development Process Presentation Outline Discussion of Project Objectives Model Configuration/Special Considerations Data and Research Integration
More informationLOCAL CLIMATOLOGICAL DATA Monthly Summary November 2006
Deg. Days Precip Ty Precip Wind Sun Hu- Adj. to Sea Level mid- ity Avg Res Res Peak Minute 1 fog 2 hvy fog 3 thunder 4 ice plt 5 hail 6 glaze 7 duststm 8 smk, hz 9 blw snw 1 2 3 4A 4B 5 6 7 8 9 12 14 15
More informationHyMet Company. Streamflow and Energy Generation Forecasting Model Columbia River Basin
HyMet Company Streamflow and Energy Generation Forecasting Model Columbia River Basin HyMet Inc. Courthouse Square 19001 Vashon Hwy SW Suite 201 Vashon Island, WA 98070 Phone: 206-463-1610 Columbia River
More informationStream Discharge and the Water Budget
Regents Earth Science Unit 6: Water Cycle & Climate Name: Lab # Stream Discharge and the Water Budget Introduction: The United States Geological Survey (USGS) measures and publishes values for the daily
More informationColorado State University, Fort Collins, CO Weather Station Monthly Summary Report
Colorado State University, Fort Collins, CO Weather Station Monthly Summary Report Month: January Year: 2019 Temperature: Mean T max was 47.2 F which is 3.0 above the 1981-2010 normal for the month. This
More informationLecture 6: Precipitation Averages and Interception
Lecture 6: Precipitation Averages and Interception Key Questions 1. How much and when does Whatcom County receive rain? 2. Where online can you find rainfall data for the state? 3. How is rainfall averaged
More information5) The amount of heat needed to raise the temperature of 1 gram of a substance by 1 C is called: Page Ref: 69
Homework #2 Due 9/19/14 1) If the maximum temperature for a particular day is 26 C and the minimum temperature is 14 C, what would the daily mean temperature be? (Page Ref: 66) 2) How is the annual mean
More informationCIMIS. California Irrigation Management Information System
CIMIS California Irrigation Management Information System What is CIMIS? A network of over 130 fully automated weather stations that collect weather data throughout California and provide estimates of
More informationCARFFG System Development and Theoretical Background
CARFFG Steering Committee Meeting 15 SEPTEMBER 2015 Astana, KAZAKHSTAN CARFFG System Development and Theoretical Background Theresa M. Modrick, PhD Hydrologic Research Center Key Technical Components -
More informationWater Year Day 2010
mm mm SCA, % Storage, mm Sto, 1 mm Sat def, 1 mm 25 2 15 1 5 4 3 2 1 2 5 25 2 Saturation deficit depth (water table) Saturation deficit volume Root zone storage Unsaturated soil storage Groundwater storage
More information5. General Circulation Models
5. General Circulation Models I. 3-D Climate Models (General Circulation Models) To include the full three-dimensional aspect of climate, including the calculation of the dynamical transports, requires
More informationThe Hydrologic Cycle
The Hydrologic Cycle Monthly precipitation for the central Arctic Ocean based on data from the Russian North Pole manned camps with daily bias adjustments. Raw precipitation totals are shown along with
More informationMET 3102-U01 PHYSICAL CLIMATOLOGY (ID 17901) Lecture 14
MET 3102-U01 PHYSICAL CLIMATOLOGY (ID 17901) Lecture 14 The hydrologic cycle evaporation vapor transport precipitation precipitation evaporation runoff Evaporation, precipitation, etc. in cm Vapor transported
More informationAnticipated and Observed Trends in the Global Hydrological Cycle. Kevin E. Trenberth NCAR
Anticipated and Observed Trends in the Global Hydrological Cycle Kevin E. Trenberth NCAR The presence of moisture affects the disposition of incoming solar radiation: Evaporation (drying) versus temperature
More information2003 Water Year Wrap-Up and Look Ahead
2003 Water Year Wrap-Up and Look Ahead Nolan Doesken Colorado Climate Center Prepared by Odie Bliss http://ccc.atmos.colostate.edu Colorado Average Annual Precipitation Map South Platte Average Precipitation
More informationWATER ON AND UNDER GROUND. Objectives. The Hydrologic Cycle
WATER ON AND UNDER GROUND Objectives Define and describe the hydrologic cycle. Identify the basic characteristics of streams. Define drainage basin. Describe how floods occur and what factors may make
More informationGEOG415 Mid-term Exam 110 minute February 27, 2003
GEOG415 Mid-term Exam 110 minute February 27, 2003 1 Name: ID: 1. The graph shows the relationship between air temperature and saturation vapor pressure. (a) Estimate the relative humidity of an air parcel
More informationstation) on the serial port
Connects a Davis VantagePro2 or Vantage Vue to a BACnet network BACnet MS/TP over RS-485 compatible Easy BACnet network configuration via onboard switches Various selectable metric and imperial unit conversions
More informationClimate Roles of Land Surface
Lecture 5: Land Surface and Cryosphere (Outline) Climate Roles Surface Energy Balance Surface Water Balance Sea Ice Land Ice (from Our Changing Planet) Surface Albedo Climate Roles of Land Surface greenhouse
More informationENGINEERING HYDROLOGY
ENGINEERING HYDROLOGY Prof. Rajesh Bhagat Asst. Professor Civil Engineering Department Yeshwantrao Chavan College Of Engineering Nagpur B. E. (Civil Engg.) M. Tech. (Enviro. Engg.) GCOE, Amravati VNIT,
More informationPrecipitation. Standardized Precipitation Index. NIDIS Intermountain West Regional Drought Early Warning System January 3, 2017
1/3/2017 NIDIS Drought and Water Assessment NIDIS Intermountain West Regional Drought Early Warning System January 3, 2017 Precipitation The images above use daily precipitation statistics from NWS COOP,
More informationDrought Monitoring with Hydrological Modelling
st Joint EARS/JRC International Drought Workshop, Ljubljana,.-5. September 009 Drought Monitoring with Hydrological Modelling Stefan Niemeyer IES - Institute for Environment and Sustainability Ispra -
More informationEstimating Evaporation : Principles, Assumptions and Myths. Raoul J. Granger, NWRI
Estimating Evaporation : Principles, Assumptions and Myths Raoul J. Granger, NWRI Evaporation So what is it anyways? Evaporation is the phenomenon by which a substance is converted from the liquid or solid
More informationUnderstanding Michigan snowfall. Jim Keysor - NWS Gaylord
Understanding Michigan snowfall Jim Keysor - NWS Gaylord Presentation Outline Topics Background information on lake effect Radar and lake effect snow Wind direction and lake effect Lake Enhanced snow Elevation
More informationColorado State University, Fort Collins, CO Weather Station Monthly Summary Report
Colorado State University, Fort Collins, CO Weather Station Monthly Summary Report Month: December Year: 2017 Temperature: Mean T max was 47.2 F which is 4.4 above the 1981-2010 normal for the month. This
More informationLand Surface Processes and Their Impact in Weather Forecasting
Land Surface Processes and Their Impact in Weather Forecasting Andrea Hahmann NCAR/RAL with thanks to P. Dirmeyer (COLA) and R. Koster (NASA/GSFC) Forecasters Conference Summer 2005 Andrea Hahmann ATEC
More informationComparative analysis of data collected by installed automated meteorological stations and manual data in Central Asia.
Comparative analysis of data collected by installed automated meteorological stations and manual data in Central Asia. Merkushkin Aleksandr Uzhydromet 71 K. Makhsumov str., 100052 Tashkent, Uzbekistan
More informationSnow II: Snowmelt and energy balance
Snow II: Snowmelt and energy balance The are three basic snowmelt phases 1) Warming phase: Absorbed energy raises the average snowpack temperature to a point at which the snowpack is isothermal (no vertical
More informationNIDIS Intermountain West Regional Drought Early Warning System February 7, 2017
NIDIS Drought and Water Assessment NIDIS Intermountain West Regional Drought Early Warning System February 7, 2017 Precipitation The images above use daily precipitation statistics from NWS COOP, CoCoRaHS,
More informationNIDIS Intermountain West Drought Early Warning System January 15, 2019
NIDIS Drought and Water Assessment NIDIS Intermountain West Drought Early Warning System January 15, 2019 Precipitation The images above use daily precipitation statistics from NWS COOP, CoCoRaHS, and
More informationRegional offline land surface simulations over eastern Canada using CLASS. Diana Verseghy Climate Research Division Environment Canada
Regional offline land surface simulations over eastern Canada using CLASS Diana Verseghy Climate Research Division Environment Canada The Canadian Land Surface Scheme (CLASS) Originally developed for the
More informationGeostatistical Analysis of Rainfall Temperature and Evaporation Data of Owerri for Ten Years
Atmospheric and Climate Sciences, 2012, 2, 196-205 http://dx.doi.org/10.4236/acs.2012.22020 Published Online April 2012 (http://www.scirp.org/journal/acs) Geostatistical Analysis of Rainfall Temperature
More informationUGRC 144 Science and Technology in Our Lives/Geohazards
UGRC 144 Science and Technology in Our Lives/Geohazards Flood and Flood Hazards Dr. Patrick Asamoah Sakyi Department of Earth Science, UG, Legon College of Education School of Continuing and Distance Education
More informationNIDIS Intermountain West Drought Early Warning System April 16, 2019
NIDIS Intermountain West Drought Early Warning System April 16, 2019 Precipitation The images above use daily precipitation statistics from NWS COOP, CoCoRaHS, and CoAgMet stations. From top to bottom,
More informationPrecipitation. Standardized Precipitation Index. NIDIS Intermountain West Drought Early Warning System September 5, 2017
9/6/2017 NIDIS Drought and Water Assessment NIDIS Intermountain West Drought Early Warning System September 5, 2017 Precipitation The images above use daily precipitation statistics from NWS COOP, CoCoRaHS,
More informationNIDIS Intermountain West Drought Early Warning System May 23, 2017
NIDIS Drought and Water Assessment NIDIS Intermountain West Drought Early Warning System May 23, 2017 Precipitation The images above use daily precipitation statistics from NWS COOP, CoCoRaHS, and CoAgMet
More informationThe TexasET Network and Website User s Manual
The TexasET Network and Website http://texaset.tamu.edu User s Manual By Charles Swanson and Guy Fipps 1 September 2013 Texas AgriLIFE Extension Service Texas A&M System 1 Extension Program Specialist;
More information5B.1 DEVELOPING A REFERENCE CROP EVAPOTRANSPIRATION CLIMATOLOGY FOR THE SOUTHEASTERN UNITED STATES USING THE FAO PENMAN-MONTEITH ESTIMATION TECHNIQUE
DEVELOPING A REFERENCE CROP EVAPOTRANSPIRATION CLIMATOLOGY FOR THE SOUTHEASTERN UNITED STATES USING THE FAO PENMAN-MONTEITH ESTIMATION TECHNIQUE Heather A. Dinon*, Ryan P. Boyles, and Gail G. Wilkerson
More informationNIDIS Intermountain West Drought Early Warning System November 14, 2017
NIDIS Intermountain West Drought Early Warning System November 14, 2017 Precipitation The images above use daily precipitation statistics from NWS COOP, CoCoRaHS, and CoAgMet stations. From top to bottom,
More informationHelp Models. Overview. 1. Base Map. 2. HELP Model for Paved Location A (near Bldg G-1)
Help Models SAIC May 25, 2005 Overview 1. Base Map 2. HELP Model for Paved Location A (near Bldg G-1) Soil Column Surface Conditions Subsurface Properties Basecase Model 3. HELP Model for Unpaved Location
More informationEach basin is surrounded & defined by a drainage divide (high point from which water flows away) Channel initiation
DRAINAGE BASINS A drainage basin or watershed is defined from a downstream point, working upstream, to include all of the hillslope & channel areas which drain to that point Each basin is surrounded &
More informationThree main areas of work:
Task 2: Climate Information 1 Task 2: Climate Information Three main areas of work: Collect historical and projected weather and climate data Conduct storm surge and wave modeling, sea-level rise (SLR)
More informationWatershed simulation and forecasting system with a GIS-oriented user interface
HydroGIS 96: Application of Geographic Information Systems in Hydrology and Water Resources Management (Proceedings of the Vienna Conference, April 1996). IAHS Publ. no. 235, 1996. 493 Watershed simulation
More informationAdvanced Hydrology Prof. Dr. Ashu Jain Department of Civil Engineering Indian Institute of Technology, Kanpur. Lecture 6
Advanced Hydrology Prof. Dr. Ashu Jain Department of Civil Engineering Indian Institute of Technology, Kanpur Lecture 6 Good morning and welcome to the next lecture of this video course on Advanced Hydrology.
More information1. Water in Soils: Infiltration and Redistribution
Contents 1 Water in Soils: Infiltration and Redistribution 1 1a Material Properties of Soil..................... 2 1b Soil Water Flow........................... 4 i Incorporating K - θ and ψ - θ Relations
More informationNIDIS Intermountain West Drought Early Warning System September 4, 2018
NIDIS Drought and Water Assessment NIDIS Intermountain West Drought Early Warning System September 4, 2018 Precipitation The images above use daily precipitation statistics from NWS COOP, CoCoRaHS, and
More information12 10 8 6 4 2 0 40-50 50-60 60-70 70-80 80-90 90-100 Fresh Water What we will cover The Hydrologic Cycle River systems Floods Groundwater Caves and Karst Topography Hot springs Distribution of water in
More informationSavannah River Site Mixed Waste Management Facility Southwest Plume Tritium Phytoremediation
Savannah River Site Mixed Waste Management Facility Southwest Plume Tritium Phytoremediation Evaluating Irrigation Management Strategies Over 25 Years Prepared November 2003 Printed February 27, 2004 Prepared
More informationColorado State University, Fort Collins, CO Weather Station Monthly Summary Report
Colorado State University, Fort Collins, CO Weather Station Monthly Summary Report Month: February Year: 2017 Webcam catching a hawk watching over the station. Temperature: Mean T max was 54.4 F which
More informationNovember 2018 Weather Summary West Central Research and Outreach Center Morris, MN
November 2018 Weather Summary Lower than normal temperatures occurred for the second month. The mean temperature for November was 22.7 F, which is 7.2 F below the average of 29.9 F (1886-2017). This November
More informationURBAN WATERSHED RUNOFF MODELING USING GEOSPATIAL TECHNIQUES
URBAN WATERSHED RUNOFF MODELING USING GEOSPATIAL TECHNIQUES DST Sponsored Research Project (NRDMS Division) By Prof. M. GOPAL NAIK Professor & Chairman, Board of Studies Email: mgnaikc@gmail.com Department
More informationGreat Lakes Update. Volume 191: 2014 January through June Summary. Vol. 191 Great Lakes Update August 2014
Great Lakes Update Volume 191: 2014 January through June Summary The U.S. Army Corps of Engineers (USACE) monitors the water levels of each of the Great Lakes. This report provides a summary of the Great
More informationSTREUVER FIDELCO CAPPELLI, LLC YONKERS DOWNTOWN DEVELOPMENT PHASE 1. DRAFT ENVIRONMENTAL IMPACT STATEMENT For: PALISADES POINT
STREUVER FIDELCO CAPPELLI, LLC YONKERS DOWNTOWN DEVELOPMENT PHASE 1 DRAFT ENVIRONMENTAL IMPACT STATEMENT For: PALISADES POINT Prepared by: PAULUS, SOKOLOWSKI & SARTOR STORMWATER MANAGEMENT 1. Methodology
More informationClimates of NYS. Definitions. Climate Regions of NYS. Storm Tracks. Climate Controls 10/13/2011. Characteristics of NYS s Climates
Definitions Climates of NYS Prof. Anthony Grande 2011 Weather and Climate Weather the state of the atmosphere at one point in time. The elements of weather are temperature, air pressure, wind and moisture.
More informationWater information system advances American River basin. Roger Bales, Martha Conklin, Steve Glaser, Bob Rice & collaborators UC: SNRI & CITRIS
Water information system advances American River basin Roger Bales, Martha Conklin, Steve Glaser, Bob Rice & collaborators UC: SNRI & CITRIS Opportunities Unprecedented level of information from low-cost
More informationFlood Forecasting Tools for Ungauged Streams in Alberta: Status and Lessons from the Flood of 2013
Flood Forecasting Tools for Ungauged Streams in Alberta: Status and Lessons from the Flood of 2013 John Pomeroy, Xing Fang, Kevin Shook, Tom Brown Centre for Hydrology, University of Saskatchewan, Saskatoon
More informationNIDIS Intermountain West Drought Early Warning System January 22, 2019
NIDIS Drought and Water Assessment NIDIS Intermountain West Drought Early Warning System January 22, 2019 Precipitation The images above use daily precipitation statistics from NWS COOP, CoCoRaHS, and
More informationGreat Lakes Update. Volume 188: 2012 Annual Summary
Great Lakes Update Volume 188: 2012 Annual Summary Background The U.S. Army Corps of Engineers (USACE) tracks the water levels of each of the Great Lakes. This report highlights hydrologic conditions of
More information