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Los Padres National Forest
Effects of off-road vehicles in Ballinger Canyon, California
Assessment of a Post-Fire Debris Flow Impacting El Capitan Watershed, Santa Barbara County, California, U.S.A.
DEDICATION TO THOMAS WILSON DIBBLEE, JR.
A landslide in Tertiary marine shale with superheated fumaroles, Coast Ranges, California
The Challenge of Improving Identification of Rockfall Hazard after Wildfires
The effects of wildfire on the sediment yield of a coastal California watershed
Minutes of the meeting of the Board of Directors of the Seismological Society of America, April 18, 1946
Phylogeny and Taxonomy of the Patagonian Miocene Falcon Thegornis musculosus Ameghino, 1895 (Aves: Falconidae)
AMERICA’S FIRST CENTURY OF MARINE NATIONAL PARK STEWARDSHIP
Developments in South Texas in 1977
Body Mass Estimations and Paleobiological Inferences on a New Species of Large Caracara (Aves, Falconidae) from the Late Pleistocene of Uruguay
Members of the Seismological Society of America
Members of the Seismological Society of America
Observations and Analyses of the 9 January 2018 Debris-Flow Disaster, Santa Barbara County, California
Inundation, flow dynamics, and damage in the 9 January 2018 Montecito debris-flow event, California, USA: Opportunities and challenges for post-wildfire risk assessment
Increased xenarthran diversity of the Great American Biotic Interchange: a new genus and species of ground sloth (Mammalia, Xenarthra, Megalonychidae) from the Hemphillian (late Miocene) of Jalisco, Mexico
An engineering study of the southern California earthquake of July 21, 1952 and its aftershocks
Insights on the controls on floodplain-dominated fluvial successions: a perspective from the Early–Middle Miocene Santa Cruz Formation in Río Chalía (Patagonia, Argentina)
SPARASSODONTA (METATHERIA) COPROLITES FROM THE EARLY-MID MIOCENE (SANTACRUCIAN AGE) OF PATAGONIA (ARGENTINA) WITH EVIDENCE OF EXPLOITATION BY COPROPHAGOUS INSECTS
The role of wildfires in the recovery strategy for the endangered southern California steelhead
ABSTRACT Southern California steelhead ( Oncorhynchus mykiss ) occupy wildfire-prone watersheds from the Santa Maria River in Santa Barbara County to the Tijuana River at the U.S.-Mexico border. This tectonically active landscape is characterized by a Mediterranean climate, highly erosive soils, and a fire-dependent chaparral/coastal sage scrub-dominated plant community. These features create an unstable landscape to which the southernmost steelhead populations have adapted over the past 20 m.y. Wildfires help to create and maintain essential features of the species’ freshwater habitats, including boulder-forced and step pools, which provide oversummering rearing habitat, and spawning gravels, which are essential for reproduction. Disturbance events can also periodically render steelhead spawning and rearing habitat locally inaccessible or unsuitable for the freshwater reproductive phase of their life-history. The episodic nature of wildfires, floods, and droughts characteristic of southern California is reflected in river and stream evolution as a cyclical rather than a linear process. These disturbance events have become more frequent, intense, and extensive as a result of anthropogenic climate change and the increased extent of the urban-wildland human interface with chaparral/coastal sage scrub and forested lands, including the four U.S. national forests in southern California. The long-term viability of southern California steelhead populations requires that they be able to persist under the foreseeable natural disturbance regime characteristic of southern California. The recovery strategy pursued by the National Marine Fisheries Service (NMFS) for the listed endangered southern California steelhead has recognized the essential role of wildfire in the species’ life-history and its role as one of the major natural disturbances that pose a risk to the listed species. Using a wildfire-frequency analysis, NMFS has adopted a recovery strategy consisting of population redundancy and spatial separation to maximize the persistence of the species in the face of wildfire and associated geomorphic processes and facilitate the species’ ability to evolve adaptations in response to changing environmental conditions.