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Drought in Travis County

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... spells and the value of the accumulated Z-index over those spells is determined ... The probability of the current spell ending is also calculated. shaw.ppt ... – PowerPoint PPT presentation

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Title: Drought in Travis County


1
Drought in Travis County
  • Chris Shaw
  • CE394K.2
  • Spring 2007

2
Outline of Presentation
  • Introduction/Objective
  • Drought
  • Indices
  • Methods
  • Results
  • Summary

3
Introduction
  • Water is important
  • Transportation
  • Agriculture
  • Domestic Use
  • Commercial and Industrial Use
  • Recreation
  • Drought negatively impacts these uses
  • Tools needed to predict and classify drought

4
Objective
  • I approached this project as an opportunity to
  • Learn more about drought
  • Learn more about tools available to classify and
    forecast drought.
  • As an exercise in determining drought conditions
    for a local area, in this case Travis County.

5
What is Drought
  • The immediate cause of drought is the predominant
    sinking motion of air (subsidence) that results
    in compressional warming or high pressure, which
    inhibits cloud formation and results in lower
    relative humidity and less precipitation.

6
Definitions
  • Conceptual vs. Operational
  • Conceptual definitions, help people understand
    the concept of drought.
  • Example Drought is a protracted period of
    deficient precipitation resulting in extensive
    damage to crops, resulting in loss of yield.
  • Operational definitions help people identify the
    beginning, end, and degree of severity of a
    drought.

7
Meteorological/Agricultural
  • Meteorological-usually an expression of
    precipitations departure from normal over time.
  • Agricultural-Links various characteristics of
    meteorological or hydrological drought to
    agricultural impacts.
  • precipitation shortages
  • differences between actual and potential
    evapotranspiration
  • soil water deficits,
  • reduced ground water or reservoir levels.

8
Hydrological
  • Hydrological drought refers to deficiencies in
    surface and subsurface water supplies. It is
    measured as streamflow and as lake, reservoir,
    and groundwater levels. There is a time lag
    between lack of rain and less water in streams,
    rivers, lakes, and reservoirs, so hydrological
    measurements are not the earliest indicators of
    drought.
  • Although climate is a primary contributor to
    hydrological drought, other factors such as
    changes in land use (deforestation), land
    degradation, and dam construction also
    contribute.

9
Socioeconomic
  • Socioeconomic- associates the supply and demand
    of some economic good with elements of
    meteorological, hydrological, and agricultural
    drought.
  • occurs when the demand for an economic good
    exceeds supply as a result of a weather-related
    shortfall in water supply.
  • occurs when physical water shortage starts to
    affect people, individually and collectively.

10
How is drought measured and represented?
  • No single operational definition of drought works
    in all circumstances, and this is a big part of
    why policy makers, resource planners, and others
    have more trouble recognizing and planning for
    drought than they do for other natural disasters.
    In fact, most drought planners now rely on
    mathematic indices to decide when to start
    implementing water conservation or drought
    response measures.

11
Drought models or indices
  • Percent of Normal
  • Standardized Precipitation Index (SPI)
  • Surface Water Supply Index (SWSI)
  • Reclamation Drought Index (RDI)
  • Deciles
  • Crop Moisture Index (CMI)
  • Palmer Drought Severity Index (PDSI)

12
Indices
  • Percent of Normal - a simple calculation suited
    to the needs of TV weathercasters and general
    audiences.
  • SPI - The SPI is an index based on the
    probability of precipitation for any time scale.
  • SWSI - designed to complement the Palmer in the
    state of Colorado
  • RDI - calculated at the river basin level

13
Indices
  • Deciles - Groups monthly precipitation into
    deciles, used in Australia
  • CMI Palmer derivative, reflects short term
    moisture supply across major crop-producing
    regions, not intended to assess long-term
    droughts
  • PDSI - Soil moisture algorithm calibrated for
    relatively homogeneous regions. U.S. government
    agencies and states rely on the Palmer.
  • Chose PDSI
  • 30 years data required

14
PDSI Calculation
  • Inputs Temperature, Precipitation, Normal
    Temperatures, Latitude, and Available Water
    Holding Capacity (AWC) of the soil.
  • The temperature values are the average daily
    temperature for each time period (month/week).
  • Precipitation the total amount received over each
    time period.
  • Normal temperatures are long-term average
    temperature for each period.
  • Latitude used to approximate the amount of
    sunlight the location receives, which is part of
    Thornthwaite's calculation of PET.

15
PDSI Calculation
  • For each period, the following values must be
    calculated
  • Potential Evapotranspiration
  • Potential Recharge
  • Potential Runoff
  • Potential Loss
  • Actual Evapotranspiration
  • Recharge
  • Runoff
  • Loss

16
PDSI Calculation
  • Calculate the moisture departure for each period
  • The moisture anomaly is calculated
  • To calibrate the PDSI, values of the duration
    factors and the climate characteristic must be
    determined
  • To determine the value of the duration factors p
    and q, the linear relationship between the length
    of extreme dry spells and the value of the
    accumulated Z-index over those spells is
    determined using the least-squares method.

17
PDSI Calculation
  • The PDSI is calculated for each period using the
    moisture anomaly that was approximated. Then each
    value of the Z-index is weighted according to
    where the 2nd and 98th percentiles of the PDSI
    fall compared with the expected -4.00 and 4.00.
  • The PDSI values are calculated iteratively using
    the Z-index and the duration factors. Each of the
    intermediate indices X1, X2, and X3 are
    calculated as necessary for each period in order.
    The probability of the current spell ending is
    also calculated.

18
Study Area Considerations
  • County chosen over HUC or watershed/basin
  • Location of measurement sites and length of
    records required for some data, most notably
    precipitation and soil moisture, limited the site
    data available.
  • Site location is relatively central to the county
    extents. Site moved to Camp Mabry in early part
    of this decade.

19
Site Location
20
PDSI Calculator
  • Fortunately I discovered a site that would do the
    calculation for me.
  • http//nadss.unl.edu/PDSIReport/index.jsp
  • SPI calculator available as well, but does not
    appear to work at this time.
  • Shortcomings outputs, limited sites

21
Results
22
Travis County, 1990-1997
23
Travis County 1998-2006
24
Summary
  • An abundance of indices available
  • Need to match the model to the job
  • As with most climate models there is a fair
    amount of uncertainty
  • Increasing availability of products like I used
  • Need more sites to support these kinds of
    efforts.

25
Questions?
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