San Diego County encompasses an area of over 4000 square miles in the southwest
corner of California. The County is bounded on the north by Orange and Riverside counties,
on the east by Imperial County, on the south by Mexico, and on the west by the Pacific
Ocean (map). The northwest to southeast trending Peninsular
Range, the most prominent topographic feature in the region divides the County into the
San Diego and Colorado hydrologic regions. The Peninsular Range includes the Santa Ana,
Agua Tibia, Palomar, Hot Springs, Aguanga, Volcan, Cuyamaca, and Laguna Mountain systems
and reaches a maximum elevation of over 6,500 feet above mean sea level.
The climate in coastal San Diego County is
generally mild with temperatures averaging about 65 degrees Fahrenheit and annual rainfall
totaling 10-14 inches. Proceeding inland from the coast, diurnal and seasonal temperatures
fluctuate to a greater degree and annual rainfall amounts typically increase. The
foothills west of the Peninsular Range average 16 20 inches of annual rainfall and
the western slope of the Peninsular Range receives as much as 45 inches of annual
precipitation. The region has a distinct rainy season with the vast majority of
precipitation occurring during the period October April.
There are a total of 11 hydrologic units (HUs) in the San
Diego Hydrologic Region (SDHR), encompassing a land area of nearly 3,000 square miles.
Eight major stream systems originate on the western slope of the Peninsular Range and
discharge into the Pacific Ocean. From north to south they are San Juan Creek, and the
Santa Margarita, San Luis Rey, San Dieguito, San Diego, Sweetwater, Otay, and Tijuana
Rivers. In addition, there are three HUs whose headwaters are located between the
Peninsular Range and the Pacific Ocean. These include the Carlsbad, Los Penasquitos, and
Pueblo San Diego units.
Spanish missionaries constructed the first dam
in San Diego County across the San Diego River in the 18th century and by 1923 every major
drainage system in the County included at least one reservoir. Today, numerous water
reservoirs capture and store surface flows throughout San Diego County however; the County
is unable to meet its water supply requirements solely through the storage of local
runoff. In 1947 the newly constructed San Vicente Reservoir was the first facility to
store water from the Colorado River. Today, the State Water Project also brings water from
Northern California rivers to San Diego County via a network of large-diameter pipelines.
The population of San Diego County grew slowly
until the later part of the 19th century when several regional water development projects
and a railroad were completed. The County population, which was less than 50,000 at the
turn of the 20th century, reached 200,000 by 1940 and passed 1 million in the late
1950s. The present population of San Diego County is approximately 2.7 million
residents. The San Diego HU is the Countys most populous with over 500,000
residents. The most densely populated HUs in the County are the Pueblo San Diego,
Penasquitos, and Carlsbad units with 13.09, 4.27, and 3.49 persons per acre, respectively.
Residential, agricultural and undeveloped land
uses are generally the most important in terms of area in the SDHR with substantial
variations occurring between the 11 hydrologic units (Table). Approximately 50% of the land
area west of the Peninsular Range is currently undeveloped. Of this vacant land, 40% is
planned for future development, mainly for residential use. The current land use
distribution in the SDHR also includes residential (15%), commercial/ industrial (5%),
parks/ open space (10%), freeways/ roads (6%), and agriculture (13%). The activities
associated with these land uses generate a variety of water pollutants.
The surface water, coastal, and groundwater
resources of the SDHR support numerous economic, water supply, recreational, and
habitat-related beneficial uses.
San Diego County is also host to a diverse array of natural habitats including montane
forests, chaparral covered hillsides, coastal sage scrub, riparian woodlands, freshwater
wetlands, coastal salt and brackish marshes, vernal pools, lagoons, enclosed bays, tide
pools, and open ocean. These areas support numerous unique and sensitive biological
habitats and are home to rare, threatened, and endangered animal and plant species like
the California gnatcatcher, the arroyo toad, the southwestern pond turtle, the salt marsh
daisy, and the Otay Mesa mint.
The regions rapid economic development
and urbanization has resulted in many of the water bodies in the SDHR being identified as
impaired on the California 303(d) list
for a host of conditions including elevated coliform bacteria and trace metals, aquatic
and sediment toxicity, nutrient enrichment, and sedimentation. Several water bodies are
impaired for multiple stressors including Mission Bay, Chollas Creek, and the Tijuana
River. (Graph of the 45 San Diego regional impaired waters grouped by water body type, and the graph of the total number of San Diego regional water bodies
affected by pollutant / stressor.) Mitigating the widespread impairments to beneficial
uses and protecting and restoring the ecological integrity of the Countys diverse
habitats will be among the regions most important future challenges. |