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How are data collected

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Title: How are data collected


1
How are data collected transmitted?
Stage is the easiest data to collect. It is the
height of the water surface above a reference
elevation. Users of streamflow data find it
necessary to have discharge information about a
stream. Discharge is the volume of flow passing a
specified point in a given interval of time and
it is usually measured in cubic feet per second
(cfs).
  • Image and information from http//www.state.nj.us
    /drbc/gage/gageshp.htm

2
Questions from Flood Frequency Analysis
  • Why 2 peak flows in the same calendar year?
  • Do the peak flows appear to occur at a particular
    time of year? If so when?
  • Excel, , decimals, wrap text
  • How are measurements made? gt How do stream gages
    work?

3
Stage gt Discharge
  • Discharge is usually estimated from
    stage/discharge relations known as rating curves.
  • In order to develop a rating curve, USGS field
    personnel must visit a gaging station to measure
    river discharge and compare it to the stage.
  • A Current Meter is the instrument that is
    frequently used to perform discharge
    measurements. Year after year, discharge and
    stage data are gathered in the field, sometimes
    as often as once a month. Over time, a
    stage/discharge rating curve is gradually
    developed. Unfortunately, rating curves are never
    fully complete due to the constant changes
    occurring in rivers and streams.

Example of a Current Meter http//water.usgs.gov/p
ubs/circ/circ1123/
4
  • The width of the stream is divided into a number
    of increments
  • the size of the increments depends on the depth
    and velocity of the stream.
  • The purpose is to divide the section into about
    25 increments with approximately equal
    discharges.
  • For each incremental width, the stream depth and
    average velocity of flow are measured.
  • For each incremental width, the meter is placed
    at a depth where average velocity is expected to
    occur.
  • That depth has been determined to be about 0.6 of
    the distance from the water surface to the
    streambed when depths are shallow.
  • When depths are large, the average velocity is
    best represented by averaging velocity readings
    at 0.2 and 0.8 of the distance from the water
    surface to the streambed.
  • The product of the width, depth, and velocity of
    the section is the discharge through that
    increment of the cross section. The total of the
    incremental section discharges equals the
    discharge of the river.

5
Developing a Rating Curve
  • USGS makes over 60,000 discharge measurements
    each year.
  • The more unstable the river bed the more often
    measurements need to be made.

Image from http//water.usgs.gov/pubs/circ/circ11
23/collection.htmlHDR9
6
Uses of Streamflow Data
  • Enhancing the public safety by providing data for
    forecasting and managing floods
  • Characterizing current water-quality conditions
  • Determining input rates of various pollutants
    into lakes, reservoirs, or estuaries
  • Computing the loads of sediment and chemical
    constituents
  • Understanding the biological effects of
    contamination
  • Delineating and managing flood plains
  • Operating and designing multipurpose reservoirs
  • Setting permit requirements for discharge of
    treated wastewater
  • Designing highway bridges and culverts
  • Setting minimum flow requirements for meeting
    aquatic life goals
  • From http//water.usgs.gov/pubs/circ/circ1123/ove
    rview.htmlHDR4

7
Uses of Streamflow Data
  • Monitoring compliance with minimum flow
    requirements
  • Developing or operating recreation facilities
  • Scheduling power production
  • Designing, operating, and maintaining navigation
    facilities
  • Allocating water for municipal, industrial, and
    irrigation uses
  • Administering compacts or resolving conflicts on
    interstate rivers
  • Defining and apportioning the water resources at
    our international borders
  • Evaluating surface- and ground-water interaction
  • Undertaking scientific studies of long-term
    changes in the hydrologic cycle
  • From http//water.usgs.gov/pubs/circ/circ1123/ove
    rview.htmlHDR4

8
Possible Letter to a Legislator MA, RI, NY
  • http//waterdata.usgs.gov/ma/nwis/rt
  • This national network is the principal tool used
    to measure surface-water supplies in each state.

9
Water Quality
10
Clean Water a Billion Growth Industry
  • The calcium scaling in a water cooling pipe is
    one example of the industrial casualties on
    display in the lab's lobby.
  • From http//www.nytimes.com/2004/02/15/business/y
    ourmoney/15water.html?pagewanted2th

11
Growth/Development in Colorado
12
Waste water flow into CT River How bad?
  • January - 55 mgal in one day flowed largely
    untreated, into the CT River from the Cromwell
    (Mattabesset) waste water treatment plant
  • How does this compare with the flow in the river?
  • cubic foot of water contains 7.48 gallons

13
(No Transcript)
14
  • 1cf 7.48 gallons
  • 55,000,000gallons
  • 7,352,941 cf
  • How much water passed by the outflow area?
  • cfs 60 s/min 60 min/hr 24 hr/day
  • If cfs 30,000 then
  • Cf/minute 1,800,000
  • Cf/hr108,000,000 hr
  • Cf/day 2,592,000,000

15
Hectares Available - roughly
  • Earth surface area 51 billion hectares
  • 13.1 billion hectares not covered by ice or water
  • 8.9 billion hectares ecologically productive
    cropland, permanent pastures, forests and
    woodland.
  • 1.5 billion hectares occupied by large deserts
  • 1.2 billion hectares semi-arid areas
  • 1.5 billion includes grassland not used for
    pasture, wasteland (includes 0.2 billion hectares
    built up areas)

16
Ten Simple Steps to ReducingYour Family's Global
Warming Impact
  • Union of Concerned Scientists http//www.ucsusa.or
    g/greatlakes/glsolutionsperson.html
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