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Book Cover

DROUGHT & Flood

The History of Water in Santa Barbara and Montecito

The History of Drought & Flood in Santa Barbara

Since the 1800s, Santa Barbara, Montecito, and Goleta have been home to the wealthy and a destination for tourists, drawn to this picturesque coastline by the mountain views and its temperate climate. But unfortunately the natural resources of this idyllic portion of central California have never been capable of supporting a population that doubled every few decades. Water shortages, described in the 1800s as “water famines,” are common occurrences. The problem is that the vast majority of Santa Barbara’s rainfall occurs in a scant 6 months, with most local streams drying up during the summer months. Virtually all streams and springs dry up during drought.

Droughts 6 years to 16 years in duration have impacted Santa Barbara and Goleta over the 151 years of recorded rainfall. Santa Barbara, Montecito, and Goleta responded to these water shortages by constructing dams, pipelines, and tunnels which linked the populated coastal areas to a distant watershed, and with much the same legal and environmental consequences that Los Angeles encountered when diverting water from the Owens Valley to Southern California. Lawsuits pitting Santa Barbara and Montecito against the landowners living downstream of the dams on the Santa Ynez River raged for decades, ending only when the California Supreme Court rendered its final decision.

Legal controversy continues today concerning a third dam built by the U.S. Bureau of Reclamation for the benefit of Santa Barbara and other South Coast communities. But this time, the advocates for the endangered species have taken a seat at the table, along with the downstream landowners. The waterworks constructed for the benefit of Santa Barbara and Montecito are modern-day engineering marvels, including a recently constructed 200-mile-long pipeline that connects a river in Northern California to Santa Barbara County, yet Santa Barbara and Montecito had to declare another water short emergency during the most recent drought.

While the mountains that make up the picturesque backdrop of Santa Barbara and Montecito typically disgorge winter rains in the form of springs and gentle streamflow, cyclic drought led to eight large fires in the mountain watersheds over the last 60 years, each of which denuded the steep hillsides. When severe rainfall events follow the brush fires, the normally quiescent streams become torrents of water that mobilize the topsoil and become what geologists call mudflows or debris flows.

In the early hours of January 9, 2018, dense mudflows developed into debris flows, pushing boulders and vegetation down the steep mountain watersheds of Montecito, destroying over 100 residences, damaging many others and causing the largest single loss of life event in the history of Santa Barbara County. Geologists examining Montecito’s geologic history knew that events like those that occurred on January 9th had occurred on numerous occasions in the geologic past, but it was not possible for them to predict when the next event would occur.

Compounding the problems of flood and drought is the environmental community’s desire to keep more water in what is called the “watersheds of origin.” What this means is that over time less water will be available to Santa Barbara and Montecito, which have historically imported water from distant watersheds. In order to address future water shortages, Santa Barbara developed a new water supply in the form of desalination. The City’s desalination plant uses state of the art technology, and takes advantage of the surplus of energy that exists in California, resulting in a drought-proof supply of water that is expected to address Santa Barbara and Montecito’s water needs for the foreseeable future.

Historical Journey: Drought, Fire & Montecito Floods

Thomas Fire (2018)

Flood, fire, and drought are inextricably interconnected. During a drought cycle the moisture content of the vegetation decreases, making the back country vegetation drier and more susceptible to wildfire. Then, if a wildfire occurs, the opportunity for flood will significantly increase in succeeding years. Scientists studying the occurrence of forest fires in California have determined that over the last 2,900 years the frequency of major forest fires varied from once per decade to eight times per decade, depending on the climate.

Pineapple Express

Historic floods are well documented in the Santa Barbara area: the years 1862; 1914; 1964; 1967; 1969; 1995; and 2018 are just a few examples. Most periods of heavy rainfall result in flood water, but floods following fires that burn off the vegetative cover on the hillsides metamorphose the flood waters into mudflows and debris flows. That is exactly what happened in Montecito on January 9, 2018. In 2017, the Thomas Fire burned 281,893 acres in Ventura and Santa Barbara Counties, including most of the vegetation in the watersheds above Montecito. Smaller fires had occurred in previous decades, impacting portions of Goleta, Santa Barbara, and western Montecito, but the last time that the brush in the majority of Montecito’s watersheds had burned was in 1964 when the Coyote Fire consumed 67,000 acres. But the Coyote Fire was not followed by an extensive and intense rainstorm such as the one that occurred in January 2018. And since much of the Montecito backcountry had not burned in over 40 years, there was substantial fuel for the Thomas Fire. Then on the evening of January 8th and 9th, 2018, 4 inches of rain fell in downtown Montecito, more in the upper watershed. But the real problem was that over a half inch of rain fell in 5 minutes: a 200-year rain event causing mud and debris to advance down Montecito’s steep watersheds at a speed of 30 miles per hour. The likelihood of a wildfire with a return frequency of 40 to 50 years, followed by a 200-year rain event, in any given year is 1 in 9,000, which is probably why geologists see only a handful of such events in the sediments that have been deposited beneath Montecito in the 781,000-year geologic record.

The 2018 Montecito Flood & Debris Flow

Geologists examining deep borings drilled in Montecito have known for many years that ancient debris flows disgorged mud and huge boulders over large areas of Montecito, well beyond the banks of the streams, but it was not possible for geologists to predict when such an event would occur next. In the early morning hours of January 9, 2018 over 100 homes were destroyed by debris flows and 23 people were killed. It was the largest single loss of life in the history of Sant Barbara County. Historic floods, mudflows and debris flows had occurred in 1862, 1914, 1964, 1967, 1969, and 1995, but were not as destructive as the 2018 Montecito flood and debris flow.

Montecito Mudslides vs. Mudflows

A mudflow is a flow of water that contains large amounts of suspended particles and silt. It has a higher density and viscosity than a streamflow and can deposit only the coarsest part of its load; this causes irreversible sediment entrainment. Its high viscosity will not allow it to flow as far as a water flow. Source: Britannica.com. A MUDSLIDE is not a term that refers to a geologic event. It is a mix of Vodka, Kahlua and Bailey’s Irish Cream. Source: Liquor.com. This photograph was taken following the 2018 Montecito flood event, when the atmospheric river and subsequent mudflows closed US 101 for several weeks. ‘You must go through a winter to understand’ —Ken Kesey, Sometimes a Great Notion.

The Mission Water Works

The Santa Barbara Mission Water Works were constructed adjacent to Mission Creek in the early 1800s. Water was diverted from upper Mission Creek and conveyed to the Mission in stone aqueducts which are still visible today.

The Mission Canyon Dam

Franciscan missionaries at The Mission Dam. The dam, located near the present-day botanical gardens, was constructed using Chumash Indian labor in 1806. The water diverted from Mission Creek served the Mission and Santa Barbara from the early 1800s until the early 1900s.

Santa Ynez River Dams

Santa Barbara and Montecito had exhausted all local water resources by the end of the 19th century, and like the City of Los Angeles, set about capturing water from distant watersheds utilizing a system of dams, tunnels and pipelines. These waterworks were the engineering marvels of their day, but fraught with legal and environmental consequences that still persist today. This is a photograph of Gibraltar Dam completed in 1919. The dam stores water in the Santa Ynez Rivrer watershed, which is then conveyed through the Santa Ynez mountains to the South Coast.

Tunnel Construction

As early as 1897, Santa Barbara and Montecito, as well as several private ranches, began excavating tunnels in the mountains that formed the backdrop of Santa Barbara and Montecito. Tunneling continued into the 20th century, with the completion of the Tecolote Tunnel in 1958. The tunnels, one to six miles in length, and bored through solid rock, brought water from inland watersheds to coastal Santa Barbara. This photograph depicts workers and a photographer from the Santa Barbara News Press at the entrance to the Mission Tunnel in 1911.

Lake Cachuma During Drought

By 1897, Santa Barbara's rapidly growing population had caused what a local newspaper called a "water famine." This was not the first water crisis in Santa Barbara. In 1862-1863, nearly all of the region's cattle died when virtually no rain fell for 2 years. Over the last 151 years six droughts have impacted Santa Barbara and Montecito, lasting from six years to sixteen years, with the last water shortage emergency ending just a few years ago. Lake Cachuma (pictured), provides the South Coast of Santa Barbara County with 42% of its water supply, but is susceptible to drought.

Fishing on the Santa Ynez River 1912

Hilton Creek, a small tributary of the Santa Ynez River near Lake Cachuma, is the location of a project intended to enhance the population of steelhead trout. Since the Bradbury Dam began operating in 1953, steelhead access to natural upstream spawning grounds has been eliminated and populations in the river have plummeted from approximately 25,000 steelhead to fewer than 20—a decrease of more than 99%. Southern California steelhead are a form of rainbow trout that spawn in coastal streams before migrating to the Pacific Ocean to mature. To ensure species survival, the Federal Bureau of Reclamation has been charged with keeping water flowing into Hilton Creek, designated by the National Marine Fisheries Service as critical habitat for the steelhead. Pictured is a day's catch from the Santa Ynez River in 1912 prior to the construction of the upstream dams on the Santa Ynez River.

Hot Springs Hotel

Montecito's Hot Springs were a gathering place for Chumash Indians prior to European settlement, and for the rich and famous from the 1800s to the 1920s. A hotel built at the mountain retreat called the Hot Springs Club existed for some time, burned down, was rebuilt, then burned down again. The hot springs water is currently being used by the Montecito Creek Water Company (founded 1897) to irrigate several large estates in Montecito and can be accessed using the Hot Springs Trail.

The City of Santa Barbara's Desal Plant

For many years, the local water agencies hadn't paid very much for water, regardless of whether the water came from local wells reservoirs on Santa Ynez river or tunnels in the mountains. But unfortunately, there wasn't any more cheap water. So in 1992, Santa Barbara built a desalination plant. The initial desal plant was rebuilt in 2018, and is one of the largest desalination plants in the United States. The City's desal plant satisfies 30% of the City's water demand and it is scheduled to be expanded.

The definitive history of the South Coast's Water

Historical Context

Understand the cycles of drought and flood that have defined Santa Barbara, Montecito, and Goleta for centuries.

Engineering Insight

Learn about the massive infrastructure projects built to tame an arid landscape.

Future Perspective

Grasp the challenges and solutions for modern water management in a changing climate.

Praise for Drought & Flood

★★★★★

Lovely!!!!

“The book is fascinating and very informative. I enjoyed it tremendously.”

— Scaswell

★★★★★

Amazingly interesting

“Never heard of horizontal wells before! Great read, research and photos. Highly recommend this book.”

— Sitka

★★★★★

Very interesting

“The book is fascinating and very informative. I enjoyed it tremendously.”

— David N.

Independent

‘Drought & Flood’

Mike Hoover’s New History of South Coast Water Predicts Drought in Santa Barbara and Beyond

By Melinda Burns

Montecito Journal

Drought & Flood

Feature Article Review

By James Buckley

About the Author

Michael F. Hoover, PG, CHG

Michael F. Hoover Portrait

Michael Hoover grew up in central and southern California, attending the University of California at Santa Barbara, where he earned a Bachelor’s Degree in Geology in 1971, and a Master’s Degree in 1974.

In 1974 he went to work for a worldwide earth science consulting firm as an engineering geologist, gaining experience in Alaska and California. In 1980 Mr. Hoover founded his own consulting firm, which was based in Santa Barbara. He was a consulting geologist for over 40 years before retiring in 2018.

Michael F. Hoover in the field

Mr. Hoover is a California licensed Professional Geologist with certifications in Engineering Geology and Hydrogeology. During his career, Mr. Hoover supervised the drilling of over 300 water wells and conducted numerous hydrologic and geological hazard investigations on the south coast of Santa Barbara County.

His clients included 400 cities, counties, corporations, and individuals, located primarily on the central coast of California. Mr. Hoover was a consultant to the City of Santa Barbara, County of Santa Barbara, the Goleta Water District, Montecito Water District, and the La Cumbre Mutual Water Company (which serves Hope Ranch).

In 2004 Mr. Hoover received the Outstanding Alumni Award from the Department of Geological Sciences, University of California Santa Barbara.

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