STATE of the CALIFORNIA CURRENT 2017–18: STILL NOT QUITE NORMAL in the NORTH and GETTING INTERESTING in the SOUTH Calcofi Rep., Vol

Total Page:16

File Type:pdf, Size:1020Kb

STATE of the CALIFORNIA CURRENT 2017–18: STILL NOT QUITE NORMAL in the NORTH and GETTING INTERESTING in the SOUTH Calcofi Rep., Vol STATE OF THE CALIFORNIA CURRENT 2017–18: STILL NOT QUITE NORMAL IN THE NORTH AND GETTING INTERESTING IN THE SOUTH CalCOFI Rep., Vol. 59, 2018 STATE OF THE CALIFORNIA CURRENT 2017–18: STILL NOT QUITE NORMAL IN THE NORTH AND GETTING INTERESTING IN THE SOUTH ANDREW R. THOMPSON* SAM MCCLATCHIE ROBERT M. SURYAN1, National Marine Fisheries Service 38 Upland Rd, Huia JANE DOLLIVER2, AND Southwest Fisheries Science Center Auckland 0604, New Zealand STEPHANIE LOREDO2 8901 La Jolla Shores Drive 1NOAA Alaska Fisheries Science Center La Jolla, CA 92037-1509 CLARE E. PEABODY Auke Bay Laboratories/ [email protected] National Marine Fisheries Service Ted Stevens Marine Research Institute Southwest Fisheries Science Center 17109 Pt. Lena Loop Road ISAAC D. SCHROEDER1,2, 8901 La Jolla Shores Drive Juneau, AK 99801 STEVEN J. BOGRAD1, ELLIOTT L. HAZEN1, La Jolla, CA 92037-1509 2Department of Fisheries and Wildlife MICHAEL G. JACOX1,3, ANDREW LEISING1, 4 Oregon State University AND BRIAN K. WELLS TIMOTHY R. BAUMGARTNER, Hatfield Marine Science Center 1Southwest Fisheries Science Center BERTHA E. LAVANIEGOS, AND Newport, OR 97365 National Marine Fisheries Service JOSE GOMEZ-VALDES 99 Pacific Street, Suite 255A Oceanology Division JEANNETTE E. ZAMON Monterey, CA 93940-7200 Centro de Investigación Científica y Northwest Fisheries Science Center 2Institute of Marine Sciences Educación Superior de Ensenada Point Adams Research Station University of California, Santa Cruz, CA Carretera Ensenada-Tijuana No. 3918 520 Heceta Place and Southwest Fisheries Science Center Zona Playitas C.P. 22860 Hammond OR 97121 NOAA Ensenada, Baja California, Mexico Monterey, CA STEPHANIE R. SCHNEIDER1 AND RICHARD D. BRODEUR1, 2 3 RICHARD T. GOLIGHTLY Earth System Research Laboratory 2 ELIZABETH A. DALY , 1 NOAA 2 2 Moss Landing Marine Labs CHERYL A. MORGAN , TOBY D. AUTH 8272 Moss Landing Road Boulder, CO 80305 AND BRIAN J. BURKE3 4 Moss Landing, CA 95039 Southwest Fisheries Science Center 1NOAA-Fisheries National Marine Fisheries Service 2Department of Wildlife Northwest Fisheries Science Center Humboldt State University NOAA Hatfield Marine Science Center Santa Cruz, CA 95064 1 Harpst Street Newport, OR 97365 Arcata, CA 95521 JOHN L. LARGIER 2Cooperative Institute for Bodega Marine Laboratory Marine Resources Studies PETE WARZYBOK AND JAIME JAHNCKE University of California Davis, Oregon State University Point Blue Conservation Science Bodega Bay, CA 94923 Hatfield Marine Science Center 3820 Cypress Drive, Suite 11 Newport, OR 97365 Petaluma, CA 94954 JENNIFER L. FISHER1, KYM JACOBSON2, 3Fish Ecology Division SAMANTHA ZEMAN1 Northwest Fisheries Science Center JARROD A. SANTORA1, 2 1 National Marine Fisheries Service SARAH ANN THOMPSON , AND Cooperative Institute for 2 Marine Resources Studies National Oceanic and WILLIAM SYDEMAN Oregon State University Atmospheric Administration 1Department of Applied Mathematics Hatfield Marine Science Center 2725 Montlake Boulevard E and Statistics Newport, OR 97365 Seattle, WA 98112 Center for Stock Assessment Research 2 University of California, Santa Cruz Northwest Fisheries Science Center JOHN FIELD AND KEITH SAKUMA Hatfield Marine Science Center Santa Cruz, CA 95060 Newport, OR 97365 Southwest Fisheries Science Center 2Farallon Institute for National Marine Fisheries Service Advanced Ecosystem Research ERIC P. BJORKSTEDT1 AND NOAA Petaluma, CA 94952 ROXANNE R. ROBERTSON2 Santa Cruz, CA 95064 SHARON R. MELIN 1Southwest Fisheries Science Center EDWARD D. WEBER AND National Marine Fisheries Service National Marine Fisheries Service WILLIAM WATSON NOAA Alaska Fisheries Science Center Santa Cruz, CA 95064 National Marine Fisheries Service Marine Mammal Laboratory Southwest Fisheries Science Center NOAA 2CIMEC, Humboldt State University 8901 La Jolla Shores Drive 7600 Sand Point Way N. E. FRANCISCO P. CHAVEZ La Jolla, CA 92037-1509 Seattle, WA 98115 Monterey Bay Aquarium Research Institute JULIA COATES1, RYAN SCHOENBAUM1, Moss Landing, CA 95039 AND LAURA ROGERS-BENNETT2 1 MATI KAHRU AND RALF GOERICKE California Department of Fish and Wildlife 1933 Cliff Drive, Suite 9 Scripps Institution of Oceanography Santa Barbara, CA 93109 University of California, San Diego 2 La Jolla, CA 92093 California Department of Fish and Wildlife Bodega Marine Laboratory University of California, Davis 2099 Westshore Road Bodega Bay, CA 94923 1 STATE OF THE CALIFORNIA CURRENT 2017–18: STILL NOT QUITE NORMAL IN THE NORTH AND GETTING INTERESTING IN THE SOUTH CalCOFI Rep., Vol. 59, 2018 ABSTRACT at Yaquina Head, Oregon, and Castle Rock, Califor- Following the marine heat wave of 2014–16, the nia. In both cases, forage was scarce, birds conducted California Current System (CCS) trended towards long foraging excursions which left eggs unattended more typical conditions north of Point Conception, for extended periods, and many eggs were consumed California, from mid-2017 to mid-2018, but became by avian predators. Brandt’s (Phalacrocorax peniscillatus) highly abnormal in the south by mid-2018. Two basin- and pelagic (P. pelagicus) cormorants had above aver- scale indices (Pacific Decadal Oscillation and Oce- age reproductive success in 2017 at Yaquina Head, but anic Niño Index) were close to neutral, but the North Brandt’s cormorant also had total reproductive failure Pacific Gyre Oscillation was extremely low at the in 2017 at Castle Rock. At Southeast Farallon Island end of 2017 and beginning of 2018. Regional anal- murre, Brandt’s cormorant, and pelagic cormorant pro- yses demonstrated that upwelling was close to nor- ductivity was close to average in 2017, and Brandt’s mal throughout most of the CCS with the exception cormorant and murre were slightly above average in of high upwelling from northern California to Wash- 2018. Preliminary 2018 results from Yaquina Head also ington in summer and fall of 2017. Sea surface tem- indicated that murre successfully produced chicks for perature was close to normal throughout most of the the first time since 2014. At-sea bird surveys in the CCS but warmed to record levels in summer 2018 north demonstrated that sooty shearwater and common in southern California and northern Baja California. murre abundances were historically low in 2017, but In spring 2018, surface chlorophyll a was negatively increased to some of the highest values on record in anomalous throughout most of the US West Coast with 2018. By contrast, the at-sea surveys off central Califor- localized hot spots around the Columbia River, in the nia found that murre densities were anomalously high Gulf of Farallones, and Monterey Bay. Lipid-rich cope- in 2017 but fell to an average level in 2018. pod densities and sizes returned to normal levels in Improving California sea lion (Zalophus california- the northern CCS, and euphausiid abundances were nus) pup condition continued from 2016 into 2017 as above average in central California but below average live pup counts, pup weight, and rate of growth were in southern California in spring 2018. Abundances of above average. Augmented pup conditions in 2016–17 7 zooplankton taxa were slightly to well above aver- was likely driven by increased availability of anchovy, age off of northern Baja California in late 2017. Pyro- as anchovy remains were found in nearly 100% of sea somes, which are associated with warm water, were lion scat. There were record high encounters with found throughout the CCS. Humpback whales (Megaptera novaeangliae) off central The fish assemblage off Oregon and Washington was California in 2018. comprised of both northern and southern/offshore Overall, much of the CCS was in more of a nor- species. In the central region (near Monterey Bay) most mal state through mid-2018 relative to the past 5 years. fishes were close to long-term mean abundances; how- However, remnants of the 2014–16 marine heat wave ever, adult northern anchovy (Engraulis mordax) abun- were still resonating in the north, and another highly dance was the highest on record. The ichthyoplankton anomalously warm water event affected the southern assemblage off southern California had a tropical signal part of the CCS in summer 2018. Thus, while the CCS similar to 2014–15 as warm-water associated mesope- was returning to typical conditions in the north, it was lagic abundances were close to record highs and cold anything but normal in the south in 2018. water mesopelagics abundances were very low. Anchovy larvae abundances in southern California were the INTRODUCTION highest since the 1960s. The California Current System (CCS; fig. 1) is noth- Indicators that can affect salmon survival were mixed ing if not dynamic with physical and biological condi- in 2018. On the one hand, several indices forecast high tions often changing greatly between years. Analyses of salmon return (moderate-high salmon yearling abun- data from the earliest days of the California Cooperative dance, high larval fish (salmon prey) abundance, normal Oceanic Fisheries Investigations (CalCOFI) program in lipid-rich copepod abundances). On the other hand, the 1950s demonstrated that oceanographic conditions low survival was predicted by high fall PDO, high can be highly variable from year to year, leading to sub- abundances of offshore larval fishes, and above average stantial changes in the distributions and abundances of abundance of lipid-poor copepods. This unusual mix of marine organisms (Moser et al. 1987; Hsieh et al. 2005). indicators makes it difficult to forecast salmon returns Changes can either be confined to particular regions in upcoming
Recommended publications
  • Fronts in the World Ocean's Large Marine Ecosystems. ICES CM 2007
    - 1 - This paper can be freely cited without prior reference to the authors International Council ICES CM 2007/D:21 for the Exploration Theme Session D: Comparative Marine Ecosystem of the Sea (ICES) Structure and Function: Descriptors and Characteristics Fronts in the World Ocean’s Large Marine Ecosystems Igor M. Belkin and Peter C. Cornillon Abstract. Oceanic fronts shape marine ecosystems; therefore front mapping and characterization is one of the most important aspects of physical oceanography. Here we report on the first effort to map and describe all major fronts in the World Ocean’s Large Marine Ecosystems (LMEs). Apart from a geographical review, these fronts are classified according to their origin and physical mechanisms that maintain them. This first-ever zero-order pattern of the LME fronts is based on a unique global frontal data base assembled at the University of Rhode Island. Thermal fronts were automatically derived from 12 years (1985-1996) of twice-daily satellite 9-km resolution global AVHRR SST fields with the Cayula-Cornillon front detection algorithm. These frontal maps serve as guidance in using hydrographic data to explore subsurface thermohaline fronts, whose surface thermal signatures have been mapped from space. Our most recent study of chlorophyll fronts in the Northwest Atlantic from high-resolution 1-km data (Belkin and O’Reilly, 2007) revealed a close spatial association between chlorophyll fronts and SST fronts, suggesting causative links between these two types of fronts. Keywords: Fronts; Large Marine Ecosystems; World Ocean; sea surface temperature. Igor M. Belkin: Graduate School of Oceanography, University of Rhode Island, 215 South Ferry Road, Narragansett, Rhode Island 02882, USA [tel.: +1 401 874 6533, fax: +1 874 6728, email: [email protected]].
    [Show full text]
  • Tube-Nosed Seabirds) Unique Characteristics
    PELAGIC SEABIRDS OF THE CALIFORNIA CURRENT SYSTEM & CORDELL BANK NATIONAL MARINE SANCTUARY Written by Carol A. Keiper August, 2008 Cordell Bank National Marine Sanctuary protects an area of 529 square miles in one of the most productive offshore regions in North America. The sanctuary is located approximately 43 nautical miles northwest of the Golden Gate Bridge, and San Francisco California. The prominent feature of the Sanctuary is a submerged granite bank 4.5 miles wide and 9.5 miles long, which lay submerged 115 feet below the ocean’s surface. This unique undersea topography, in combination with the nutrient-rich ocean conditions created by the physical process of upwelling, produces a lush feeding ground. for countless invertebrates, fishes (over 180 species), marine mammals (over 25 species), and seabirds (over 60 species). The undersea oasis of the Cordell Bank and surrounding waters teems with life and provides food for hundreds of thousands of seabirds that travel from the Farallon Islands and the Point Reyes peninsula or have migrated thousands of miles from Alaska, Hawaii, Australia, New Zealand, and South America. Cordell Bank is also known as the albatross capital of the Northern Hemisphere because numerous species visit these waters. The US National Marine Sanctuaries are administered and managed by the National Oceanic and Atmospheric Administration (NOAA) who work with the public and other partners to balance human use and enjoyment with long-term conservation. There are four major orders of seabirds: 1) Sphenisciformes – penguins 2) *Procellariformes – albatross, fulmars, shearwaters, petrels 3) Pelecaniformes – pelicans, boobies, cormorants, frigate birds 4) *Charadriiformes - Gulls, Terns, & Alcids *Orders presented in this seminar In general, seabirds have life histories characterized by low productivity, delayed maturity, and relatively high adult survival.
    [Show full text]
  • Film Flight: Lost Production and Its Economic Impact on California
    I MILKEN INSTITUTE California Center I July 2010 Film Flight: Lost Production and Its Economic Impact on California by Kevin Klowden, Anusuya Chatterjee, and Candice Flor Hynek Film Flight: Lost Production and Its Economic Impact on California by Kevin Klowden, Anusuya Chatterjee, and Candice Flor Hynek ACKnowLEdgmEnts The authors gratefully acknowledge Armen Bedroussian and Perry Wong for their expert assistance in preparing this study. We also thank our editor, Lisa Renaud. About tHE mILKEn InstItutE The Milken Institute is an independent economic think tank whose mission is to improve the lives and economic conditions of diverse populations in the United States and around the world by helping business and public policy leaders identify and implement innovative ideas for creating broad-based prosperity. We put research to work with the goal of revitalizing regions and finding new ways to generate capital for people with original ideas. We focus on: human capital: the talent, knowledge, and experience of people, and their value to organizations, economies, and society; financial capital: innovations that allocate financial resources efficiently, especially to those who ordinarily would not have access to them, but who can best use them to build companies, create jobs, accelerate life-saving medical research, and solve long-standing social and economic problems; and social capital: the bonds of society that underlie economic advancement, including schools, health care, cultural institutions, and government services. By creating ways to spread the benefits of human, financial, and social capital to as many people as possible— by democratizing capital—we hope to contribute to prosperity and freedom in all corners of the globe.
    [Show full text]
  • Seasonal and Spatial Fluctuations of the Phytoplankton in Monterey Bay
    SEASONAL AND SPATIAL FLUCTUATIONS OF THE PHYTOPLANKTON IN MONTEREY BAY A Thesis Presented to the Graduate Faculty of California State University, Hayward In Partial Fulfillment of the Requirements for the Degree Master of Arts in Biological Science by Russ Waidelich January, 1976 ABSTRACT The seasonal and spatial fluctuations of phyto­ plankton in Monterey Bay were described for an 18-month period. Low winter levels were mainly due to instabi­ lity of the water column, while the spring bloom was brought a·bout by the commencement of upwelling and the subsequent stabilization of the water column, with resi­ dence time of water regulating chlorophyll concentra­ tions. The summer minimum shortly followed the cessa­ tion of upwelling, when it appeared that nitrates were limiting, although zooplankton was a major factor in re­ ducing the algal standing stock at this time. Adequate illumination and relaxation of grazing pressure rather than specificity of water type appeared to be the major factors regulating the occurrence of the fall bloom, indicating that the seasonal pattern of Monterey Bay conforms generally to that of the mid­ latitude marine ecosystems. An examination of the spatial distribution o.f phytoplankton revealed lower values over the canyon during upwelling months due to advection of water to the shelf areas, and lower values in the same area during non-upwelling months due to subsidence or downwelling and tur·bul enc e . ii ACENOWLEDGlVJENTS Many people were responsible for helping to make this thesis possible. I would first like to thank my major advisors, Dr. Mary Silver and Dr. John Martin, for their valuable advice and support.
    [Show full text]
  • Upper Ocean Hydrology of the Northern Humboldt Current System
    Progress in Oceanography 165 (2018) 123–144 Contents lists available at ScienceDirect Progress in Oceanography journal homepage: www.elsevier.com/locate/pocean Upper ocean hydrology of the Northern Humboldt Current System at T seasonal, interannual and interdecadal scales ⁎ Carmen Gradosa, , Alexis Chaigneaub, Vincent Echevinc, Noel Domingueza a Instituto del MAR de PErú (IMARPE), Callao, Peru b Laboratoire d'Études en Géophysique et Océanographie Spatiale (LEGOS), Université de Toulouse, CNES, CNRS, IRD, UPS, Toulouse, France c Laboratoire d'Océanographie et de Climatologie: Expérimentation et Analyse Numérique (LOCEAN), LOCEAN-IPSL, IRD/CNRS/Sorbonnes Universités (UPMC)/MNHN, UMR 7159, Paris, France ARTICLE INFO ABSTRACT Keywords: Since the 1960s, the Instituto del Mar del Perú (IMARPE) collected tens of thousands of in-situ temperature and North Humboldt Current System salinity profiles in the Northern Humboldt Current System (NHCS). In this study, we blend this unique database Hydrology with the historical in-situ profiles available from the World Ocean Database for the period 1960–2014 and apply Water masses a four-dimensional interpolation scheme to construct a seasonal climatology of temperature and salinity of the Seasonal variations NHCS. The resulting interpolated temperature and salinity fields are gridded at a high spatial resolution Geostrophic currents (0.1° × 0.1° in latitude/longitude) between the surface and 1000 m depth, providing a detailed view of the ENSO Interdecadal variability hydrology and geostrophic circulation of this region. In particular, the mean distribution and characteristics of the main water-masses in the upper ocean of the NHCS are described, as well as their seasonal variations be- tween austral summer and winter.
    [Show full text]
  • California Current Integrated Ecosystem
    Agenda Item G.1.a IEA Team Report 1 March 2020 CALIFORNIA CURRENT INTEGRATED ECOSYSTEM ASSESSMENT (CCIEA) CALIFORNIA CURRENT ECOSYSTEM STATUS REPORT, 2020 A report of the NOAA CCIEA Team to the Pacific Fishery Management Council, March 5, 2020. Editors: Dr. Chris Harvey (NWFSC), Dr. Toby Garfield (SWFSC), Mr. Greg Williams (PSMFC), and Dr. Nick Tolimieri (NWFSC) 1 INTRODUCTION Section 1.4 of the 2013 Fishery Ecosystem Plan (FEP) established a reporting process wherein NOAA provides the Pacific Fishery Management Council (Council) with a yearly update on the status of the California Current Ecosystem (CCE), as derived from environmental, biological, economic and social indicators. NOAA’s California Current Integrated Ecosystem Assessment (CCIEA) team is responsible for this report. This is our 8th report, with prior reports in 2012 and 2014-2019. This report summarizes CCE status based on data and analyses that generally run through 2019. Highlights are summarized in Box 1.1. Appendices provide additional information or clarification, as requested by the Council, the Scientific and Statistical Committee (SSC), or other advisory bodies. Box 1.1: Highlights of this report • In 2019, the system experienced weak to neutral El Niño conditions, average to slightly positive Pacific Decadal Oscillation (PDO), and very weak North Pacific circulation • A large marine heatwave emerged in mid 2019, similar in size and intensity to the 2013- 2016 “Blob,” but it weakened by December, and we do not yet know what effects it had • Several ecological indicators
    [Show full text]
  • Climate Change and Seabirds of the California Current and Pacific Islands Ecosystems: Observed and Potential Impacts and Management Implications
    Climate Change and Seabirds of the California Current and Pacific Islands Ecosystems: Observed and Potential Impacts and Management Implications Final Report to the U.S. Fish and Wildlife Service, Region 1 Lindsay Young Pacific Rim Conservation Honolulu, Hawaii Robert M. Suryan Oregon State University Newport, Oregon David Duffy University of Hawaii Honolulu, Hawaii William J. Sydeman Farallon Institute Petaluma, California 3 May 2012 1 Contents Executive Summary ....................................................................................................................................... 3 Introduction .................................................................................................................................................. 6 Climate Change and Seabirds ................................................................................................................... 6 Geographic Scope ..................................................................................................................................... 7 Natural Climate Variability and North Pacific Ecosystems........................................................................ 8 The California Current ................................................................................................................................... 9 Climate Change factors ........................................................................................................................... 10 Atmospheric circulation .....................................................................................................................
    [Show full text]
  • STATE of the CALIFORNIA CURRENT 2018–19: a NOVEL ANCHOVY REGIME and a NEW MARINE HEATWAVE? Calcofi Rep., Vol
    STATE OF THE CALIFORNIA CURRENT 2018–19: A NOVEL ANCHOVY REGIME AND A NEW MARINE HEATWAVE? CalCOFI Rep., Vol. 60, 2019 STATE OF THE CALIFORNIA CURRENT 2018–19: A NOVEL ANCHOVY REGIME AND A NEW MARINE HEAT WAVE? ANDREW R. THOMPSON* MATI KAHRU EDWARD D. WEBER National Marine Fisheries Service AND RALF GOERICKE AND WILLIAM WATSON Southwest Fisheries Science Center Scripps Institution of Oceanography National Marine Fisheries Service 8901 La Jolla Shores Drive University of California, San Diego Southwest Fisheries Science Center La Jolla, CA, 92037-1509 La Jolla, CA 92093 8901 La Jolla Shores Drive [email protected] La Jolla, CA 92037-1509 CLARE E. PEABODY ISAAC D. SCHROEDER1,2, National Marine Fisheries Service JESSICA M. PORQUEZ1, STEVEN J. BOGRAD1, ELLIOTT L. HAZEN1, Southwest Fisheries Science Center JANE DOLLIVER1, MICHAEL G. JACOX1,3, ANDREW LEISING1, 8901 La Jolla Shores Drive DONALD E. LYONS1,2, AND AND BRIAN K. WELLS4 La Jolla, CA 92037-1509 RACHAEL A. ORBEN1 1Southwest Fisheries Science Center 1Department of Fisheries and Wildlife National Marine Fisheries Service TIMOTHY R. BAUMGARTNER, Oregon State University 99 Pacific Street, Suite 255A BERTHA E. LAVANIEGOS, Hatfield Marine Science Center Monterey, CA 93940-7200 LUIS E. MIRANDA, Newport, OR 97365 ELIANA GOMEZ-OCAMPO, 2Institute of Marine Sciences 2National Audubon Society University of California AND JOSE GOMEZ-VALDES 104 Nash Hall Santa Cruz, CA Oceanology Division Corvallis, OR 97331 and Centro de Investigación Científica y Southwest Fisheries Science Center Educación Superior de Ensenada JEANNETTE E. ZAMON NOAA Carretera Ensenada-Tijuana No. 3918 Northwest Fisheries Science Center Monterey, CA Zona Playitas C.P.
    [Show full text]
  • Phytoplankton Species in the California Current System Off Southern California: the Spatial Dimensions Calcofi Rep., Vol
    VENRICK: PHYTOPLANKTON SPECIES IN THE CALIFORNIA CURRENT SYSTEM OFF SOUTHERN CALIFORNIA: THE SPATIAL DIMENSIONS CalCOFI Rep., Vol. 56, 2015 PHYTOPLANKTON SPECIES IN THE CALIFORNIA CURRENT SYSTEM OFF SOUTHERN CALIFORNIA: THE SPATIAL DIMENSIONS ELIZABETH L. VENRICK Integrative Oceanography Division Scripps Institution of Oceanography University of California, San Diego La Jolla, CA 92093-0227 ph: (858) 534-2068 fax: (858) 534-6500 [email protected] ABSTRACT temporal cycles have been defined and studied, includ- This paper examines 16 years of microscopic infor- ing the seasonal cycle (Lynn and Simpson 1987; Legaard mation about phytoplankton taxonomic composition and Thomas 2006); the El Niño–Southern Oscillation and abundances from each of four regions in the Cal- (ENSO; Chelton et al. 1982; Bograd and Lynn 2001); COFI area. The NE region is approximately the region and two decadal cycles, the Pacific Decadal Oscilla- of the Southern California Bight; the SE region is the tion (Ebesmeyer et al. 1991; Roemmich and McGowan lower edge of the bight; the Offshore is the western- 1995a, b; Mantua et al. 1997); and the North Pacific most region; and the Alley is the path between the NE Gyre Oscillation (Bond et al. 2003; Di Lorenzo et al. and the Offshore through which the California Cur- 2008). Information on these scales of variability pro- rent meanders. vides a background against which to evaluate longer The NE region and the Alley consistently had the period changes. highest phytoplankton abundances, dominated by dia- Routine sampling for phytoplankton species on toms. These two areas were most similar with respect ­CalCOFI cruises began in 1990.
    [Show full text]
  • Selected BOEM-Funded Research Informing Renewable Energy Offshore California JUNE 2021
    Selected BOEM-Funded Research Informing Renewable Energy Offshore California JUNE 2021 Biological Studies ................................................................................. PAGE 1 Cultural & Archaeological Studies ................................................................. PAGE 6 Information Synthesis Studies .................................................................... PAGE 7 Physical Oceanography & Geology Studies ....................................................... PAGE 8 Resource, Technology & Infrastructure Studies ................................................... PAGE 9 Socioeconomic Studies .......................................................................... PAGE 10 Biological Studies Ongoing (2014–2022) — Potential Impacts of Submarine Power Cables on Crab Harvest This two-part research effort is to learn more about whether the electromagnetic fields (EMF) emitted from subsea power- transmission cables may affect the movement and harvest of commercial crab species. The first part was conducted by the University of California, Santa Barbara, which collected data on red rock crab in the Santa Barbara Channel and Dungeness crab in Puget Sound. The second part is collecting and analyzing additional data. Study Profile: https://www.boem.gov/pc-19-02/ Ongoing (2017-2022) — Seabird and Marine Mammal Surveys Near Potential Renewable Energy Sites Offshore Central and Southern California This study by the U.S. Geological Survey will provide up-to-date information on species composition, distribution,
    [Show full text]
  • The California Current System: a Multiscale Overview And
    Dynamics of Atmospheres and Oceans 52 (2011) 131–169 Contents lists available at ScienceDirect Dynamics of Atmospheres and Oceans journal homepage: www.elsevier.com/locate/dynatmoce The California Current System: A multiscale overview and the development of a feature-oriented regional modeling system (FORMS) a,∗ b c Avijit Gangopadhyay , Pierre F.J. Lermusiaux , Leslie Rosenfeld , d e f Allan R. Robinson , Leandro Calado , Hyun Sook Kim , b b Wayne G. Leslie , Patrick J. Haley Jr. a School for Marine Science and Technology, University of Massachusetts at Dartmouth, Suite 325, 200 Mill Road, Fairhaven, MA 02719, United States b Department of Mechanical Engineering, Massachusetts Institute of Technology, Cambridge, MA, United States c Naval Postgraduate School, Monterey, CA, United States d Division of Applied Sciences, Harvard University, Cambridge, MA, United States e Marinha do Brasil, Instituto de Estudos do Mar Almirante Paulo Moreira-IEAPM, Rua Kioto, 253-Praia dos Anjos, Arraial do Cabo, RJ 28930-000, Brazil f National Centers for Environmental Prediction (NCEP), Silver Springs, MD, United States a r t i c l e i n f o a b s t r a c t Available online 19 May 2011 Over the past decade, the feature-oriented regional modeling methodology has been developed and applied in several ocean domains, including the western North Atlantic and tropical North Keywords: Atlantic. This methodology is model-independent and can be uti- California Current System lized with or without satellite and/or in situ observations. Here we Feature models develop new feature-oriented models for the eastern North Pacific ◦ ◦ FORMS from 36 to 48 N – essentially, most of the regional eastern bound- Upwelling ary current.
    [Show full text]
  • Near-Shore Circulation in the California Current
    Calif.Mar. Res. Comm., CalCOFZ Rept., 16 : 5i-65, 1972 NEAR-SHORE CIRCULATION IN THE CALIFORNIA CURRENT RICHARD A. SCHWARTZLOSE and JOSEPH 1. REID Scripps Institution of Oceanography La Jolla, California A great many of you are very familiar with the Figure 4 shows drift-bottle results for December major current along the California Coast. What we 1969. The Davidson Current was very well developed. wish to do today is to review the currents closer to the There was water moving out of southern California coast, since they are equally pertinent to the problem northward along the coast. One drift bottle went to of pollution along the coast. Alaska. The minimum speed of some of the December Figure 1 is a 16-year mean chart of the surface cur- 1969 drift bottles that moved northward in the David- rents (relative to geostrophic flow) along the Califor- son Current was about .3 knot (15 cm/sec). nia coast in winter (January). The normal offshore We have records from other drift bottles in other flow all during the year is towards the southeast. In years during the winter that indicated minimum the wintertime the Davidson Current nearshore moves speeds in the Davidson Current of .6 knot (30 cm/sec) northward opposite to the current farther offshore. for long periods of time, up to 2 to 3 months. This This northward flow in winter is attributed to the Davidson Current is usually a very strong current seasonal change in the wind patterns across California, compared to the offshore California Current and it Oregon and Washington.
    [Show full text]