Figure 1. Comparison of inundation of Elkhorn Slough in 2005 versus 95 years later in 2100. [View Larger]
Storms, Waves, and Coastal ErosionMonterey Bay's southern coast is already eroding more rapidly than any other region in the state of California. Erosion at the coastal dunes between the mouth of the Salinas River and Monterey Harbor has been measured at rates between 1.0 and 6.0 feet per year (reference here). In northern Monterey Bay, Santa Cruz County's sea cliffs are experiencing average retreat rates of 0.17 to 2.1 feet per year. A statewide study by the California Energy Commission found that approximately 4.4 square miles of coastline in Monterey County is susceptible to erosion from expected sea level rise, and predicted that coastal dunes and cliffs will retreat by up to 1,300 feet and 720 feet, respectively. In Santa Cruz County, 1.8 square miles of shoreline may be lost by 2100 (Heberger et al. 2009).
More severe storms with larger waves will accelerate coastal erosion as has happened recently in Pacifica, CA. Photo credit: Unknown.Erosion caused by sea level rise and an expected increase in storm and wave intensity will place many oceanfront facilities at risk and may cause permanent damage to transportation infrastructure, major sewage pipelines, beachfront hotels, condominiums, and private residences. Large, episodic events (such as storms that occur at extreme high tides) pose the greatest erosion threats, and these are forecast to become more frequent (reference here). Forecasts suggest that over 4,600 properties along the Monterey Bay shoreline may be lost, and that 3,420 people in Santa Cruz and Monterey Counties may lose their homes. Coastal armoring strategies such as sea walls, bulkheads and revetments are already common in the sanctuary and may have long-term impacts on natural processes such as sediment transport. As private landowners and local governments become aware of increased risks associated with sea level rise, coastal armoring projects will likely become more common. More information on sanctuary involvement with coastal armoring can be found here.
Coastal Inundation and RunoffCoastal areas adjacent to the sanctuary may become inundated with seawater as sea level rises. Naturally low-lying habitats will be the most impacted as expected increases in storm intensity combine with sea level rise to cause storm surge, high tides, waves, and floods to reach areas further inland than they have in the past. Areas that will be affected include critical habitat areas such as Elkhorn Slough and other estuaries. If salt marsh accretion (as a result of sediment deposition) or transgression (upland migration) cannot keep pace with sea level rise, marsh areas will become permanently submerged. At Elkhorn Slough, which provides habitat for hundreds of species including more than 340 species of birds, extensive salt marsh restoration is underway to counteract extensive habitat loss due to river diversion, drainage-induced subsidence, and the construction of Moss Landing Harbor. More frequent and more severe flooding events threaten these habitat restoration efforts.
In addition, coastal inundation threatens transportation infrastructure and will subject low-lying coastal agricultural properties to salinization. As storm-induced floodwaters recede, they will draw debris, fertilizers, and other contaminants into the bay, compromising coastal water quality. Such an increase in runoff has the potential to increase the frequency and intensity of harmful algal blooms (HABs) in the sanctuary, posing serious threats to local fisheries, birds and marine mammal populations.
Saltwater IntrusionAnother threat associated with rising sea level is an acceleration of saltwater intrusion, the process by which coastal groundwater aquifers become contaminated by seawater. Local groundwater reserves provide over 80 percent of Monterey County's total water use. Overdrafts of wells have already caused saltwater intrusion in the Salinas River and Pajaro River groundwater basins (reference here). The current rate of saltwater intrusion in the Pajaro Valley basin is estimated at 100-250 feet per year. Sea level rise will further speed this process, further limiting communities' supply of usable fresh water for drinking and irrigation.
Research and Monitoring
Red pelagic crabs (<em>Pleuroncodes planipes</em>) washed up on Coral Street Beach in Pacific Grove, CA beginning October 7, 2015. This is an exceedingly unusual event for the Monterey area, as these crabs are normally offshore of Baja California, but warm waters have transported them north. These crabs haven't washed ashore in this area since 1982-1983, an El Nino year. NOAA is tracking a current El Nino that has contributed to the warm water plume, and it is assumed the two events are once again related. <em>Pleuroncodes</em> stranding events are rare occurrences in Monterey Bay and usually coincide with ENSO events. The species was first discovered in 1859 during a mass-stranding event in Monterey. Further stranding events in Monterey occurred later in 1959 and again in 1969. Dr. Steve Webster, senior marine biologist at the Monterey Bay Aquarium, noted that when present, seagulls were feeding on so many crabs that they could not get airborne. Pleuroncodes are also a source of food for fishes, rays, and pinnipeds (seals and sea lions).
Visual impact caused by shoddy concrete riprap along Westcliff Drive in Santa Cruz.
• Ocean CO2 and Ocean Acidification Research The Monterey Bay region is home to research institutions that are world leaders in oceanographic research, including the effects of increased levels of ocean CO2 and ocean acidification. Oceanographers at MBARI and Moss Landing Marine Labs have studied how anthropogenic climate change interacts with large-scale physical and biological ocean cycles, while MBARI chemists and biologists have coordinated a series of experiments on the potential effects of more acidic waters on a variety of marine organisms. Oceanic pH (an indicator of acidity) measurements over the last 20 years show that ocean pH is on the decline in Monterey Bay and correlates with trends in global ocean pH. Some of this research, such as the Free-Ocean Carbon Enrichment (FOCE) experiment, has occurred at the MARS cabled ocean observatory, 900 m below the surface of Monterey Bay.
FOCE is comprised of a semi-enclosed test area on the seafloor where the seawater's pH can be precisely controlled for extended periods. Small seafloor animals are placed in the test chamber, where their behavior and physiological responses can be monitored. Local research has also investigated the effects that efforts to sequester carbon dioxide in the oceans would have on deep-sea biological communities.