Why Do We Care?

  • Deaths
    • Floods and storms resulted in 257,400 deaths
      globally from 1988 to 1997
  • Economic Loss
    • $434 billion in damages were caused by floods
      and storms globally from 1988 to 1997
  • Water Quality
    • Floods and storms can overload sewage systems
      leading to bacterial contamination in water bodies

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Photo Credit: NBC News

Southern California

  • Rainfall
    • A majority of the storms
      occur in the winter months
    • These storms coincide with
      landfalling atmospheric rivers
    • Atmospheric rivers have a strong
      correlation with increased flooding
      (Young et al. 2017)
  • Urbanization (Sheng & Wilson 2009)
    • Urban watersheds in Los Angeles County
      lose 90% of rainfall from storms to runoff
    • Impervious surface cover is greater
      than 45% in five Los Angeles watersheds
    • Four of the five watersheds
      have shown significant increases in
      peak stream discharge from 1921 to 2000

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Map Credit: Guide of US

San Diego County

  • Location
    • Riverside and Orange County is to the north, Imperial
      County is to the east, Mexico is to the south, and
      the Pacific Ocean is to the west
    • Roughly 30 percent is classified as developed land use
    • Urban development is seen in the western third,
      rural areas are seen in the eastern two-thirds,
      and deserts are seen beyond that
  • Recent Rain Events and Droughts
    • Tropical Storm Hilary led to $900 million in damages
      in the United States
    • Up to three inches of precipitation fell within a span
      of three hours on January 22, 2024 in San Diego
      • This event had a return period of every 1,000
        years and resulted in severe flash flooding
    • From 2012 to 2014 California experienced an
      unprecedented drought so severe that the return
      interval was estimated at once every 10,000 years

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Map Credit: printablemapaz.com

Objectives


  1. Determine if climate change has had a significant
    impact on streamflow characteristics and flood
    behavior in San Diego County

    – North and South County sites were
       analyzed to answer this




  2. Determine if watershed urbanization has had a
    significant impact on streamflow characteristics
    and flood behavior in San Diego County

    – South and Upstream South County sites
       were analyzed to answer this

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Source: University of North Carolina

Sites Analyzed

  • North County
    • USGS Site 11042000:
      San Luis Rey River
      at Oceanside
  • South County
    • USGS Site 11023000:
      San Diego River at
      Fashion Valley
  • Upstream South County
    • USGS Site 11022480:
      San Diego River near
      Mast Road at Santee

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Data Collection & Analysis

  • Precipitation & Discharge
    • The Parameter-elevation Regressions on Independent Slopes Model (PRISM)
      spatial dataset was used to collect daily precipitation data
    • The dataRetrieval package in R was used to collect daily stream discharge data
      • The grwat package in R was used to separate quickflow from baseflow
    • Time frame: October 1, 1986 to September 30, 2023
    • The Sens slope package in R was used to determine trends over time
  • Watershed Characteristics
    • Site locations and watershed delineations were derived from USGS StreamStats
    • Land cover data was collected from USGS LCMAP for both 1985 and 2021
  • Flood Days
    • Top 1% rainfall event
      OR
      Top 1% streamflow event

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Climate Change – Storms

  • Calculation for Baseflow
    • Baseflow is compared with stream discharge during the 2023 water year to demonstrate the accuracy of the calculation
  • Storm Runoff
    • Quickflow is compared with precipitation (dotted line) during two top 1% rainfall events
      • 1986: Peak discharge occurs on the same day as peak precipitation
      • 2023: Peak discharge occurs two days after peak precipitation
    • The timing of peak flows during storms may have been impacted by climate change
      • Soil moisture percentage should be explored in future analyses as it likely influenced runoff magnitude during these two events

Climate Change – Storms

Climate Change – Storms

Climate Change – Floods

  • Top 1% Precipitation
    • Greater in North County than South County for the same return period
    • More events are observed from 2005 to 2023 for both sites
    • Increasing at 2, 4, and 8 year return periods for both sites
      • But not significantly increasing for all return periods
  • Top 1% Stream Discharge
    • Greater in South County than North County for the same return period
    • More events are observed from 2005 to 2023 in North County
    • Increasing at 2, 4, and 8 year return periods in North County
      • But remains mostly unchanged for all return periods

Climate Change – Floods

name Sens Slope P-value
North County 0.041 0.079
South County 0.019 0.258
Upstream South County 0.018 0.322

Climate Change – Floods

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Climate Change – Flashiness

  • North County
    • Flashiness is not significantly increasing
    • Upstream diversions from 2013 to 2016 led to zero flow
      • Water rights issues were exacerbated due to the drought
      • This could explain why the P-value was not significant
  • South County
    • Flashiness is not significantly decreasing
      • Stormwater management improvements could be responsible
        for the observed decrease in flashiness

Climate Change – Flashiness

Watershed Sens Slope P-value
North County 0.003 0.195
South County -0.002 0.200

Watershed Urbanization – Land Cover

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Watershed Urbanization – Storms

  • Peak Q vs. Peak P
    • South County has a moderate linear correlation: Adjusted R Squared = 0.74
    • Upstream South County also has a moderate linear correlation: Adjusted R Squared = 0.76
    • Both watersheds experience a step change when precipitation > 40 mm/d
  • Events: Step Change
    • Initial peak precipitation slightly increases stream discharge (solid line)
    • Final peak precipitation greatly increases stream discharge
      • Soil moisture percentage and dams above Upstream South County are influencing peak discharge during storms
  • El Capitan Dam
    • In poor condition and could fail during an earthquake or heavy rainfall event so water levels are kept low (NPR 2022)
    • Short-term repairs are being made (Garrick 2023)
    • Reservoir release in addition to soil saturation may be the cause of the flashiness
    • Future analyses should investigate the relationship between flood frequency and reservoir release

Watershed Urbanization – Storms

Watershed Urbanization – Flashiness

  • Upstream South County
    • Flashiness is significantly increasing
      • This alone is not enough to show an increase in flooding
      • Hourly or 15 minute precipitation and stream discharge data is necessary
      • Forest cover loss and its impact on flashiness in San Diego County should
        be explored in future analyses

Watershed Urbanization – Flashiness

Watershed Sens Slope P-value
Upstream South County 0.004 0.017

Conclusions

  • North County
    • Flood magnitude is increasing at 2, 4, and 8 year return periods, but I cannot
      definitively say that flood frequency is increasing
  • South County
    • Flood magnitude and frequency have not been significantly impacted due to
      climate change and/or watershed urbanization
  • Upstream South County
    • Flashiness has been significantly increasing but this alone is not enough to
      demonstrate urbanization’s impacts on flood magnitude and frequency
  • Limitations
    • Very few USGS sites have current stream discharge data in San Diego County
    • Hourly and 15 minute data is not current or easily accessible and high resolution
      spatial imagery is not open to the public
  • Next Steps
    • Even though significance was not demonstrated in my results, they should prove useful to
      water utility agencies and support further research on flood behavior in Southern California
    • The impacts of forest cover loss, reservoir release, and peak flow timing on flood behavior
      in San Diego County should be explored in future analyses

Key Takeaways



  • San Diego County has experienced a major climatic shift in the last decade
    • Ten years ago drought mitigation was the primary topic,
      but now flood mitigation is the core subject



  • There is difficulty in making concrete conclusions about flood behavior
    when using daily data instead of hourly or 15 minute
    • This type of data should be current and easily accessible
      as it is crucial for more than just flood analyses

Reference

Cosgrove, William & Rijsberman, Frank & Water, Council. (2000). World Water Vision: Making Water Everybody’s Business. https://doi.org/10.4324/9781315071763.

Young, A. M., Skelly, K. T., & Cordeira, J. M. (2017). High-impact hydrologic events and atmospheric rivers in California: An investigation using the NCEI Storm Events Database. Geophysical Research Letters, 44(7), 3393–3401. https://doi.org/10.1002/2017GL073077

Sheng, J., & Wilson, J. P. (2009). Watershed urbanization and changing flood behavior across the Los Angeles metropolitan region. Natural Hazards, 48(1), 41–57. https://doi.org/10.1007/s11069-008-9241-7

NPR. (2022, May 5). More than 2,200 dams are in poor condition, posing danger to communities. NPR. https://www.npr.org/2022/05/05/1096940224/dams-poor-condition-hazardous-dangerous-infrastructure

Garrick, D. (2023, September 12). San Diego spending $9M on repairs to structurally vulnerable dams—El Capitan, Lake Morena. The San Diego Union-Tribune. https://www.sandiegouniontribune.com/news/politics/story/2023-09-12/san-diego-spending-9m-on-repairs-to-structurally-vulnerable-dams-el-capitan-lake-morena