Sam McClatchie
National Oceanic and Atmospheric Administration
Network
Latest external collaboration on country level. Dive into details by clicking on the dots.
Publication
Featured researches published by Sam McClatchie.
Royal Society Open Science | 2016
Sam McClatchie; John C. Field; Andrew R. Thompson; Tim Gerrodette; Mark Lowry; Paul C. Fiedler; William Watson; Karen Nieto; Russell D. Vetter
California sea lions increased from approximately 50 000 to 340 000 animals in the last 40 years, and their pups are starving and stranding on beaches in southern California, raising questions about the adequacy of their food supply. We investigated whether the declining sea lion pup weight at San Miguel rookery was associated with changes in abundance and quality of sardine, anchovy, rockfish and market squid forage. In the last decade off central California, where breeding female sea lions from San Miguel rookery feed, sardine and anchovy greatly decreased in biomass, whereas market squid and rockfish abundance increased. Pup weights fell as forage food quality declined associated with changes in the relative abundances of forage species. A model explained 67% of the variance in pup weights using forage from central and southern California and 81% of the variance in pup weights using forage from the female sea lion foraging range. A shift from high to poor quality forage for breeding females results in food limitation of the pups, ultimately flooding animal rescue centres with starving sea lion pups. Our study is unusual in using a long-term, fishery-independent dataset to directly address an important consequence of forage decline on the productivity of a large marine predator. Whether forage declines are environmentally driven, are due to a combination of environmental drivers and fishing removals, or are due to density-dependent interactions between forage and sea lions is uncertain. However, declining forage abundance and quality was coherent over a large area (32.5–38° N) for a decade, suggesting that trends in forage are environmentally driven.
PLOS ONE | 2012
Andrew R. Thompson; William Watson; Sam McClatchie; Edward D. Weber
To resolve the capacity of Marine Protected Areas (MPA) to enhance fish productivity it is first necessary to understand how environmental conditions affect the distribution and abundance of fishes independent of potential reserve effects. Baseline fish production was examined from 2002–2004 through ichthyoplankton sampling in a large (10,878 km2) Southern Californian oceanic marine reserve, the Cowcod Conservation Area (CCA) that was established in 2001, and the Southern California Bight as a whole (238,000 km2 CalCOFI sampling domain). The CCA assemblage changed through time as the importance of oceanic-pelagic species decreased between 2002 (La Niña) and 2003 (El Niño) and then increased in 2004 (El Niño), while oceanic species and rockfishes displayed the opposite pattern. By contrast, the CalCOFI assemblage was relatively stable through time. Depth, temperature, and zooplankton explained more of the variability in assemblage structure at the CalCOFI scale than they did at the CCA scale. CalCOFI sampling revealed that oceanic species impinged upon the CCA between 2002 and 2003 in association with warmer offshore waters, thus explaining the increased influence of these species in the CCA during the El Nino years. Multi-scale, spatially explicit sampling and analysis was necessary to interpret assemblage dynamics in the CCA and likely will be needed to evaluate other focal oceanic marine reserves throughout the world.
Journal of Geophysical Research | 2014
Karen Nieto; Sam McClatchie; Edward D. Weber; Cleridy E. Lennert-Cody
We quantified the effect of mesoscale eddies and streamers on the spatial distribution of Pacific sardine spawning habitat using a merged altimetry data set and a statistical spawning habitat model. The distribution of eggs could be predicted using sea-surface temperature, chlorophyll concentration, and eddy kinetic energy (EKE) similarly to previous studies. Eddies alone did not have a significant additional or emergent effect on the probability of capturing eggs beyond these predictors. Rather, mesoscale features (eddies and streamers) entrained water with the appropriate conditions in terms of temperature, chlorophyll, and EKE. These dynamic features moved appropriate spawning habitat for sardine offshore to areas where appropriate habitat otherwise would not exist. Using centroids of predicted sardine habitat, we showed that sardine recruitment success was inversely correlated with distance from shore of predicted sardine habitat centroids. This indicates that offshore transport has a negative effect on sardine recruitment, despite expanding favorable spawning habitat further offshore.
PLOS ONE | 2012
David R. Currie; Sam McClatchie; John F. Middleton; S. Nayar
We sampled the demersal fish community of the Bonney Canyon, South Australia at depths (100–1,500 m) and locations that are poorly known. Seventy-eight species of demersal fish were obtained from 12 depth-stratified trawls along, and to either side, of the central canyon axis. Distributional patterns in species richness and biomass were highly correlated. Three fish assemblage groupings, characterised by small suites of species with narrow depth distributions, were identified on the shelf, upper slope and mid slope. The assemblage groupings were largely explained by depth (ρw = 0.78). Compared to the depth gradient, canyon-related effects are weak or occur at spatial or temporal scales not sampled in this study. A conceptual physical model displayed features consistent with the depth zonational patterns in fish, and also indicated that canyon upwelling can occur. The depth zonation of the fish assemblage was associated with the depth distribution of water masses in the area. Notably, the mid-slope community (1,000 m) coincided with a layer of Antarctic Intermediate Water, the upper slope community (500 m) resided within the core of the Flinders Current, and the shelf community was located in a well-mixed layer of surface water (<450 m depth).
Royal Society Open Science | 2016
Sam McClatchie; John C. Field; Andrew R. Thompson; Tim Gerrodette; Mark Lowry; Paul C. Fiedler; William Watson; Karen Nieto; Russell D. Vetter
[This corrects the article DOI: 10.1098/rsos.150628.].
Geophysical Research Letters | 2010
Sam McClatchie; Ralf Goericke; R. Cosgrove; G. Auad; R. Vetter
Journal of Geophysical Research | 2006
Sam McClatchie; John F. Middleton; Tim M. Ward
Progress in Oceanography | 2015
Kenneth A. Rose; Jerome Fiechter; Enrique N. Curchitser; Kate Hedstrom; Miguel Bernal; Sean Creekmore; Alan C. Haynie; Shin-ichi Ito; Salvador E. Lluch-Cota; Bernard A. Megrey; Christopher A. Edwards; Dave Checkley; Tony Koslow; Sam McClatchie; Francisco E. Werner; Alec D. MacCall; Vera N. Agostini
Archive | 2010
Eric P. Bjorkstedt; Ralf Goericke; Sam McClatchie; Edward D. Weber; William Watson; Nancy Lo; Bill Peterson; B Emmett; Jay O. Peterson; Reginaldo Durazo; Gilberto Gaxiola-Castro; Francisco P. Chavez; Jt Pennington; Curtis A. Collins; John C. Field; Keith M. Sakuma; Steven J. Bograd; Franklin B. Schwing; Y Xue; William J. Sydeman; Sarah Ann Thompson; Jarrod A. Santora; John L. Largier; Chris Halle; Steven G. Morgan; Sy Kim; Kpb Merkens; John A. Hildebrand; Lisa Munger
Journal of Geophysical Research | 2012
Sam McClatchie; Robert K. Cowen; Karen Nieto; Adam T. Greer; Jessica Y. Luo; Cedric M. Guigand; David A. Demer; David Griffith; Daniel L. Rudnick