Chapter One Averaging Precipitation over a watershed.

Slides:



Advertisements
Similar presentations
Weather and Climate.
Advertisements

Global Precipitation Precipitation averages just about 1 meter per year over Earth but, like wealth, varies widely from place to place and from time to.
Oklahoma’s Facts and Climate
Why do we need to measure rainfall?
Urbanization Minnesota, New Jersey and most other states are facing population and development increases. Flood water is increasingly difficult to handle:
CE 394K.2 Precipitation Precipitation mechanisms Rainall maps Rainfall hyetographs Nexrad measurement of rainfall Reading: Applied Hydrology Sections 3.5.
1 Precipitation and IDF Curves. 2 Objectives Know different forms of precipitation Know what a return frequency is Know what an IDF curve is Know how.
Estimation of Rainfall Areal Reduction Factors Using NEXRAD Data Francisco Olivera, Janghwoan Choi and Dongkyun Kim Texas A&M University – Department of.
Hydrologic Theory One of the principal objectives in hydrology is to transform rainfall that has fallen over a watershed area into flows to be expected.
Climate Lesson What factors contribute to a region’s climate? Directions: - Click “Slide Show” then “View Show” to view the power point. -Record all notes.
WHAT IS Z?  Radar reflectivity (dBZ)  Microwave energy reflects off objects (e.g. hydrometeors) and the return is reflectivity WHAT IS R?  Rainfall.
Digital weather recording instruments
Climate and Vegetation Patterns
January 26 th, 2015 READ: Priceless Florida Chapter 2, pages
World Climates Chapter 21, Section 2.
Basic Hydrology & Hydraulics: DES 601
Estimation of Areal Precipitation from point measurements Most often interested in quantifying rainfall over an entire watershed. Has to be inferred from.
Areal Estimation techniques Two types of technique: 1. Direct weighted averages 2. Surface fitting methods DIRECT WEIGHTED AVERAGE METHODS use the equation:
Precipitation Precipitation: water falling from the atmosphere to the earth. –Rainfall –Snowfall –Hail, sleet Requires lifting of air mass so that it cools.
World Geography Chapter 3 Notes
Precipitation Types Important for Real Time Input and Forecasting
Figure (p. 202) Precipitation formation. Water droplets in clouds are formed by nucleation of vapor on aerosols, then go through many condensation-evaporation.
Hydrologic Design Storms
Chapter 8 Air Masses The Atmosphere 10e Lutgens & Tarbuck.
Climate. What is the difference between Climate and Weather? "Climate is what you expect; weather is what you get" Weather- the current condition of the.
How to Generate Theissen Weights Example 8 – Supplement.
Climate Factors Sun & Latitude Atmospheric Pressure Global Wind Belts Oceans & Currents Elevation.
Climates of the World. World Climate Regions High Latitude Middle Latitude Low Latitude Middle Latitude High Latitude Arctic Circle Antarctic Circle Tropic.
DES 606 : Watershed Modeling with HEC-HMS Module 8 Theodore G. Cleveland, Ph.D., P.E 29 July 2011.
Design Storms CE 365K Hydraulic Engineering Design Spring 2015.
R EADINGS Read Chapter 20 in the textbook if you are confused about: Air masses (page 436) Fronts and Lows (pg 439) Thunderstorms and Tornadoes (pg 445)
Introduction to Hydrologic Processes - Rainfall & Streamflow Dr. Philip B. Bedient Civil and Environmental Eng Rice University.
Elementary Engineering Hydrology BY Deodhar M. J.
BEGIN Precipitation as the Input. Some Huge Rainfalls.
CE 3354 Engineering Hydrology
Basic Hydrology: Rainfall-Runoff – I
Local Weather Patterns. Weather Patterns Weather changes from day to day and from season to season. These changes typically happen in the same way, following.
Weather, Climate, & Seasons
Introduction to Rainfall & Streamflow Philip B. Bedient January, 2007.
Climate Social Studies. Tropical Wet Tropical Wet is only found along the equator. Examples include: Brazil, Indonesia, and the Philippines. Seasons don’t.
Rain gauge Lathiya milan. Methods of Measuring Rainfall: Remote Tipping bucket rain gauge -The bucket tips when precipitation of 0.2 mm,
Module 10: Average Rainfall Theodore G. Cleveland, Ph.D., P.E, M. ASCE, F. EWRI August 2015 Module 10 1.
World Climates. The Köppen Climate Classification System The Köppen climate classification system uses mean monthly and annual values of temperature and.
Rainfall-Runoff modeling
World Climates Chapter 21, Section 2.
A Study of the Extremity of the October 1998 Rainfall Event
CE 394K.2 Hydrology Precipitation
Flooding in the Amite River Basin (August 12- August 22, 2016)
Finishing Precipitation
Climate.
UK Climate is Temperature – Cool, Wet Winters and Warm, Wet Summers
World Climates Chapter 21, Section 2.
Climate Zones An Overview Wessel ~ 2017
Rainfall Averaging Methods
Climate and Weather.
World Climate Regions.
Introduction to Rainfall & Streamflow
What factors contribute to a region’s climate?
Precipitation Precipitation: water falling from the atmosphere to the earth. Rainfall Snowfall Hail, sleet Requires lifting of air mass so that it cools.
Climates.
INTRODUCTION TO HYDROLOGY
Test 1 Results Mean 29.8 Std dev 3.5.
Precipitation and IDF Curves
Precipitation Single strongest variable driving hydrologic processes
Climates of the Earth Ch. 3: Climates of the Earth
Climate.
UNIT 3 Climates and Ecosystems
Hydrology CIVL341.
Monitoring the Weather
Australia, Oceania, and Antarctica
Presentation transcript:

Chapter One Averaging Precipitation over a watershed

The NW windward precip., Western interior rain shadow arid, east dominated by mT versus cP invasions. Gulf Coast very rainy due hurricanes. Red Subtropical desert in summer. Annual Rainfall CONUS lower 48

Seasonal Rainfall The west coast windward precip in fall- winter, snowmelt in spring, east of cordillera arid with May rain, eastern US year round precip +/- mid- year rain.

Precipitation is generally recorded automatically in increments Transmitter Reed switch activated by magnet

For our purposes, a wide can will do

A Hyetograph On a rainy day, rainfall intensity varies with time. Plot called a hyetograph.

Intensity-duration-frequency (IDF) curves. How frequently do you get a storm of a particular intensity and duration? Here is a summary for Houston. Every five years, on average, they get an inch of rain per hour lasting 4 hours. Every 100 years they about half an inch of rain per hour lasting 24 hours.

Notice only the gages within the watershed are used for the average. All gages used There are almost never enough reliable rainfall records inside the basin you are working on. Until Nexrad archives improve, three averaging methods are used: taking the mean, Thiessen method, and the Isohyetal method, similar to making a contour map.

For Thiessen, find the rain gauges near your watershed

Draw triangles between adjacent rain gages and draw perpendicular bisectors for each side

Thiessen Figure E1-4b This breaks up the area around each gauge into regions. CONSIDER ONLY the area of each region that belongs to your watershed. Here the area around gage D is the largest, then B, then F, then A, etc. Measure these areas by drawing a grid onto the map, by tracing/printing them on gridded paper, or by some other method.

Add all the small grid areas together to get the total area of the watershed, then calculate the fractional area for each gauge. Multiply the proportionate area for each polygon by the rainfall for that gage, and add them up for the weighted average total rainfall over your watershed.

NEXRAD (Next-Generation Radar) gives you fine resolution data with area squares. These are available real time (current weather), but the online archives are still unwieldy for past storm events.

Thiessen Method We will stop here to work on averaging and Theissen method.