The Scripps Oceanography 100 Island Challenge Developing Conservation Targets for Coral Reefs Globally
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Basic Concepts in Oceanography
Chapter 1 XA0101461 BASIC CONCEPTS IN OCEANOGRAPHY L.F. SMALL College of Oceanic and Atmospheric Sciences, Oregon State University, Corvallis, Oregon, United States of America Abstract Basic concepts in oceanography include major wind patterns that drive ocean currents, and the effects that the earth's rotation, positions of land masses, and temperature and salinity have on oceanic circulation and hence global distribution of radioactivity. Special attention is given to coastal and near-coastal processes such as upwelling, tidal effects, and small-scale processes, as radionuclide distributions are currently most associated with coastal regions. 1.1. INTRODUCTION Introductory information on ocean currents, on ocean and coastal processes, and on major systems that drive the ocean currents are important to an understanding of the temporal and spatial distributions of radionuclides in the world ocean. 1.2. GLOBAL PROCESSES 1.2.1 Global Wind Patterns and Ocean Currents The wind systems that drive aerosols and atmospheric radioactivity around the globe eventually deposit a lot of those materials in the oceans or in rivers. The winds also are largely responsible for driving the surface circulation of the world ocean, and thus help redistribute materials over the ocean's surface. The major wind systems are the Trade Winds in equatorial latitudes, and the Westerly Wind Systems that drive circulation in the north and south temperate and sub-polar regions (Fig. 1). It is no surprise that major circulations of surface currents have basically the same patterns as the winds that drive them (Fig. 2). Note that the Trade Wind System drives an Equatorial Current-Countercurrent system, for example. -
World Ocean Thermocline Weakening and Isothermal Layer Warming
applied sciences Article World Ocean Thermocline Weakening and Isothermal Layer Warming Peter C. Chu * and Chenwu Fan Naval Ocean Analysis and Prediction Laboratory, Department of Oceanography, Naval Postgraduate School, Monterey, CA 93943, USA; [email protected] * Correspondence: [email protected]; Tel.: +1-831-656-3688 Received: 30 September 2020; Accepted: 13 November 2020; Published: 19 November 2020 Abstract: This paper identifies world thermocline weakening and provides an improved estimate of upper ocean warming through replacement of the upper layer with the fixed depth range by the isothermal layer, because the upper ocean isothermal layer (as a whole) exchanges heat with the atmosphere and the deep layer. Thermocline gradient, heat flux across the air–ocean interface, and horizontal heat advection determine the heat stored in the isothermal layer. Among the three processes, the effect of the thermocline gradient clearly shows up when we use the isothermal layer heat content, but it is otherwise when we use the heat content with the fixed depth ranges such as 0–300 m, 0–400 m, 0–700 m, 0–750 m, and 0–2000 m. A strong thermocline gradient exhibits the downward heat transfer from the isothermal layer (non-polar regions), makes the isothermal layer thin, and causes less heat to be stored in it. On the other hand, a weak thermocline gradient makes the isothermal layer thick, and causes more heat to be stored in it. In addition, the uncertainty in estimating upper ocean heat content and warming trends using uncertain fixed depth ranges (0–300 m, 0–400 m, 0–700 m, 0–750 m, or 0–2000 m) will be eliminated by using the isothermal layer. -
Introduction to Oceanography
Introduction to Oceanography Introduction to Oceanography Lecture 14: Tides, Biological Productivity Memorial Day holiday Monday no lab meetings Go to any other lab section this week (and let the TA know!) Bay of Fundy -- low tide, Photo by Dylan Kereluk, . Creative Commons A 2.0 Generic, Mudskipper (Periophthalmus modestus) at low tide, photo by OpenCage, Wikimedia Commons, Creative http://commons.wikimedia.org/wiki/File:Bay_of_Fundy_-_Tide_Out.jpg Commons A S-A 2.5, http://commons.wikimedia.org/wiki/File:Periophthalmus_modestus.jpg Tides Earth-Moon-Sun System Planet-length waves Cyclic, repeating rise & fall of sea level • Earth-Sun Distance – Most regular phenomenon in the oceans 150,000,000 km Daily tidal variation has great effects on life in & around the ocean (Lab 8) • Earth-Moon Distance 385,000 km Caused by gravity and Much closer to Earth, but between Earth, Moon & much less massive Sun, their orbits around • Earth Obliquity = 23.5 each other, and the degrees Earth’s daily spin – Seasons Photos by Samuel Wantman, Creative Commons A S-A 3.0, http://en.wikipedia.org/ wiki/File:Bay_of_Fundy_Low_Tide.jpg and Figure by Homonculus 2/Geologician, Wikimedia Commons, http://en.wikipedia.org/wiki/ Creative Commons A 3.0, http://en.wikipedia.org/wiki/ File:Bay_of_Fundy_High_Tide.jpg File:Lunar_perturbation.jpg Tides are caused by the gravity of the Moon and Sun acting on Scaled image of Earth-Moon distance, Nickshanks, Wikimedia Commons, Creative Commons A 2.5 Earth and its ocean. Pluto-Charon mutual orbit, Zhatt, Wikimedia Commons, Public -
Exploration of the Deep Gulf of Mexico Slope Using DSV Alvin: Site Selection and Geologic Character
Exploration of the Deep Gulf of Mexico Slope Using DSV Alvin: Site Selection and Geologic Character Harry H. Roberts1, Chuck R. Fisher2, Jim M. Brooks3, Bernie Bernard3, Robert S. Carney4, Erik Cordes5, William Shedd6, Jesse Hunt, Jr.6, Samantha Joye7, Ian R. MacDonald8, 9 and Cheryl Morrison 1Coastal Studies Institute, Louisiana State University, Baton Rouge, Louisiana 70803 2Department of Biology, Penn State University, University Park, Pennsylvania 16802-5301 3TDI Brooks International, Inc., 1902 Pinon Dr., College Station, Texas 77845 4Department of Oceanography and Coastal Sciences, Louisiana State University, Baton Rouge, Louisiana 70803 5Department of Organismic and Evolutionary Biology, Harvard University, 16 Divinity Ave., Cambridge, Massachusetts 02138 6Minerals Management Service, Office of Resource Evaluation, New Orleans, Louisiana 70123-2394 7Department of Geology, University of Georgia, Athens, Georgia 30602 8Department of Physical and Environmental Sciences, Texas A&M – Corpus Christi, Corpus Christi, Texas 78412 9U.S. Geological Survey, 11649 Leetown Rd., Keameysville, West Virginia 25430 ABSTRACT The Gulf of Mexico is well known for its hydrocarbon seeps, associated chemosyn- thetic communities, and gas hydrates. However, most direct observations and samplings of seep sites have been concentrated above water depths of approximately 3000 ft (1000 m) because of the scarcity of deep diving manned submersibles. In the summer of 2006, Minerals Management Service (MMS) and National Oceanic and Atmospheric Admini- stration (NOAA) supported 24 days of DSV Alvin dives on the deep continental slope. Site selection for these dives was accomplished through surface reflectivity analysis of the MMS slope-wide 3D seismic database followed by a photo reconnaissance cruise. From 80 potential sites, 20 were studied by photo reconnaissance from which 10 sites were selected for Alvin dives. -
Assessing Long-Term Changes in the Beach Width of Reef Islands Based on Temporally Fragmented Remote Sensing Data
Remote Sens. 2014, 6, 6961-6987; doi:10.3390/rs6086961 OPEN ACCESS remote sensing ISSN 2072-4292 www.mdpi.com/journal/remotesensing Article Assessing Long-Term Changes in the Beach Width of Reef Islands Based on Temporally Fragmented Remote Sensing Data Thomas Mann 1,* and Hildegard Westphal 1,2 1 Leibniz Center for Tropical Marine Ecology, Fahrenheitstrasse 6, D-28359 Bremen, Germany; E-Mail: [email protected] 2 Department of Geosciences, University of Bremen, D-28359 Bremen, Germany * Author to whom correspondence should be addressed; E-Mail: [email protected]; Tel.: +49-421-2380-0132; Fax: +49-421-2380-030. Received: 30 May 2014; in revised form: 7 July 2014 / Accepted: 18 July 2014 / Published: 25 July 2014 Abstract: Atoll islands are subject to a variety of processes that influence their geomorphological development. Analysis of historical shoreline changes using remotely sensed images has become an efficient approach to both quantify past changes and estimate future island response. However, the detection of long-term changes in beach width is challenging mainly for two reasons: first, data availability is limited for many remote Pacific islands. Second, beach environments are highly dynamic and strongly influenced by seasonal or episodic shoreline oscillations. Consequently, remote-sensing studies on beach morphodynamics of atoll islands deal with dynamic features covered by a low sampling frequency. Here we present a study of beach dynamics for nine islands on Takú Atoll, Papua New Guinea, over a seven-decade period. A considerable chronological gap between aerial photographs and satellite images was addressed by applying a new method that reweighted positions of the beach limit by identifying “outlier” shoreline positions. -
Nature Parks Snorkeling Surfing Fishing
Things to do in Florida Nature Parks Snorkeling Surfing Fishing Nature Parks Green Cay This nature center is the county’s newest nature canter that over- looks 100 acres of constructed wetland. Wakodahatchee Wetlands Is a park in Delray Beach with a three-quarter mile boardwalk that crosses between open water ponds and marches. Patch Reef Park & DeHoernle Park Parks in Boca Raton that have an abundant of sports and recreation facilities. Morikami Museum & Japanese Gardens The gardens at this Japanese cultural center in Delray Beach in- clude paradise garden, various styles of rock and Zen gardens, and a museum. Gumbo Limbo This Nature Center and Environmental Complex includes an indoor museum with fish tanks with fish, turtles, and other sea life. It is also known for rehabilitating and protecting sea turtles. *More information and website links are located on the last page. Snorkeling Blowing Rocks This is an environmental preserve on Jupiter Island in Hobe Sound. This peaceful, barrier island sanctuary is known for large-scale, native coastal habitat restoration. Lantana Beach Lantana is a coastal community in Palm Beach and 10 feet off shore there is a pretty good areas to snorkel. Red Reef Park A 67-acre oceanfront park in Boca Raton for swimming, snorkeling, and surf fishing that includes a nature center. Lauderdale-by-the-Sea Is known as “The Shore Diving Capital of South Florida”. There are two coral reef lines that are just a short swim from the beach. John Pennekamp Coral Reef State Park The first undersea park that encompasses about 70 natural square miles. -
The Economic, Social and Icon Value of the Great Barrier Reef Acknowledgement
At what price? The economic, social and icon value of the Great Barrier Reef Acknowledgement Deloitte Access Economics acknowledges and thanks the Great Barrier Reef Foundation for commissioning the report with support from the National Australia Bank and the Great Barrier Reef Marine Park Authority. In particular, we would like to thank the report’s Steering Committee for their guidance: Andrew Fyffe Prof. Ove Hoegh-Guldberg Finance Officer Director of the Global Change Institute Great Barrier Reef Foundation and Professor of Marine Science The University of Queensland Anna Marsden Managing Director Prof. Robert Costanza Great Barrier Reef Foundation Professor and Chair in Public Policy Australian National University James Bentley Manager Natural Value, Corporate Responsibility Dr Russell Reichelt National Australia Bank Limited Chairman and Chief Executive Great Barrier Reef Marine Park Authority Keith Tuffley Director Stephen Fitzgerald Great Barrier Reef Foundation Director Great Barrier Reef Foundation Dr Margaret Gooch Manager, Social and Economic Sciences Stephen Roberts Great Barrier Reef Marine Park Authority Director Great Barrier Reef Foundation Thank you to Associate Professor Henrietta Marrie from the Office of Indigenous Engagement at CQUniversity Cairns for her significant contribution and assistance in articulating the Aboriginal and Torres Strait Islander value of the Great Barrier Reef. Thank you to Ipsos Public Affairs Australia for their assistance in conducting the primary research for this study. We would also like -
Coastal Upwelling Revisited: Ekman, Bakun, and Improved 10.1029/2018JC014187 Upwelling Indices for the U.S
Journal of Geophysical Research: Oceans RESEARCH ARTICLE Coastal Upwelling Revisited: Ekman, Bakun, and Improved 10.1029/2018JC014187 Upwelling Indices for the U.S. West Coast Key Points: Michael G. Jacox1,2 , Christopher A. Edwards3 , Elliott L. Hazen1 , and Steven J. Bograd1 • New upwelling indices are presented – for the U.S. West Coast (31 47°N) to 1NOAA Southwest Fisheries Science Center, Monterey, CA, USA, 2NOAA Earth System Research Laboratory, Boulder, CO, address shortcomings in historical 3 indices USA, University of California, Santa Cruz, CA, USA • The Coastal Upwelling Transport Index (CUTI) estimates vertical volume transport (i.e., Abstract Coastal upwelling is responsible for thriving marine ecosystems and fisheries that are upwelling/downwelling) disproportionately productive relative to their surface area, particularly in the world’s major eastern • The Biologically Effective Upwelling ’ Transport Index (BEUTI) estimates boundary upwelling systems. Along oceanic eastern boundaries, equatorward wind stress and the Earth s vertical nitrate flux rotation combine to drive a near-surface layer of water offshore, a process called Ekman transport. Similarly, positive wind stress curl drives divergence in the surface Ekman layer and consequently upwelling from Supporting Information: below, a process known as Ekman suction. In both cases, displaced water is replaced by upwelling of relatively • Supporting Information S1 nutrient-rich water from below, which stimulates the growth of microscopic phytoplankton that form the base of the marine food web. Ekman theory is foundational and underlies the calculation of upwelling indices Correspondence to: such as the “Bakun Index” that are ubiquitous in eastern boundary upwelling system studies. While generally M. G. Jacox, fi [email protected] valuable rst-order descriptions, these indices and their underlying theory provide an incomplete picture of coastal upwelling. -
Artificial Reef Observations from a Manned Submersible Off Southeast Florida
BULLETIN OF MARINE SCIENCE, 44(2): 1041-1050, 1989 ARTIFICIAL REEF OBSERVATIONS FROM A MANNED SUBMERSIBLE OFF SOUTHEAST FLORIDA Eugene A, Shinn and Robert I. Wicklund ABSTRACT Examination of 16artificial reef structures with a two-person submersible in depths ranging from 30 to 120 m (100-400 ft) indicated that the highest numbers offish are found around reefs in water shallower .than 46 m (150 ft). Fewer fish, especially those with tropical coral reef affinities, below 46 m was probably caused by a thermocline, observed on all dives deeper than 43 m (140 ft). During 4 days in September 1987, temperatures from the surface down to approximately 43 m were 30° to 31°C (86°-88°F), whereas below 43 m the temperature dropped as low as 1O.6°C(51°F) at 120 m (390 ft). Algae and reef community encrusters (gorgonians, bryozoans, branching sponges, and corals), abundant on shallower structures, were absent below 46 m. Structures that penetrated above the thermocline, such as two upright oil "rigs" and a hopper barge, were also effective reefs. The open structure and high profile of the rigs enhance their use as artificial reefs by providing a range of well-aerated habitats. Any effect of substrate or post-deployment age on fish abundance could not be documented. Wood appeared to be a more effective fish-concentrating material but has a shorter useful life than does steeL The greatest diversity and numbers of fish were observed at the Miami sewer outfalL Numerous derelict ships and other material have been placed off southeast Florida for the purpose of enhancing fish stocks and sportsfishing. -
Upwelling As a Source of Nutrients for the Great Barrier Reef Ecosystems: a Solution to Darwin's Question?
Vol. 8: 257-269, 1982 MARINE ECOLOGY - PROGRESS SERIES Published May 28 Mar. Ecol. Prog. Ser. / I Upwelling as a Source of Nutrients for the Great Barrier Reef Ecosystems: A Solution to Darwin's Question? John C. Andrews and Patrick Gentien Australian Institute of Marine Science, Townsville 4810, Queensland, Australia ABSTRACT: The Great Barrier Reef shelf ecosystem is examined for nutrient enrichment from within the seasonal thermocline of the adjacent Coral Sea using moored current and temperature recorders and chemical data from a year of hydrology cruises at 3 to 5 wk intervals. The East Australian Current is found to pulsate in strength over the continental slope with a period near 90 d and to pump cold, saline, nutrient rich water up the slope to the shelf break. The nutrients are then pumped inshore in a bottom Ekman layer forced by periodic reversals in the longshore wind component. The period of this cycle is 12 to 25 d in summer (30 d year round average) and the bottom surges have an alternating onshore- offshore speed up to 10 cm S-'. Upwelling intrusions tend to be confined near the bottom and phytoplankton development quickly takes place inshore of the shelf break. There are return surface flows which preserve the mass budget and carry silicate rich Lagoon water offshore while nitrogen rich shelf break water is carried onshore. Upwelling intrusions penetrate across the entire zone of reefs, but rarely into the Lagoon. Nutrition is del~veredout of the shelf thermocline to the living coral of reefs by localised upwelling induced by the reefs. -
WOODS HOLE OCEANOGRAPHIC INSTITUTION Deep-Diving
NEWSLETTER WOODS HOLE OCEANOGRAPHIC INSTITUTION AUGUST-SEPTEMBER 1995 Deep-Diving Submersible ALVIN WHOI Names Paul Clemente Sets Another Dive Record Chief Financial Officer The nation's first research submarine, the Deep Submergence Paul CI~mente, Jr., a resident of Hingham Vehicle (DSV) Alvin. passed another milestone in its long career and former Associate Vice President for September 20 when it made its 3,OOOth dive to the ocean floor, a Financial Affairs at Boston University, as· record no other deep-diving sub has achieved. Alvin is one of only sumed his duties as Associate Director for seven deep-diving (10,000 feet or more) manned submersibles in the Finance and Administration at WHOI on world and is considered by far the most active of the group, making October 2. between 150 and 200 dives to depths up to nearly 15,000 feet each In his new position Clemente is respon· year for scientific and engineering research . sible for directing all business and financial The 23-1001, three-person submersible has been operated by operations of the Institution, with specifIC Woods Hole Oceanographic Institution since 1964 for the U.S. ocean resp:>nsibility for accounting and finance, research community. It is owned by the OffICe of Naval Research facilities, human resources, commercial and supported by the Navy. the National Science Foundation and the affairs and procurement operations. WHOI, National Oceanic and Atmospheric Administration (NOAA). Alvin the largest private non· profit marine research and its support vessel, the 21 0-100t Research Vessel Atlantis II, are organization in the U.S., has an annual on an extended voyage in the Pacific which began in January 1995 operating budget of nearly $90 million and a with departure from Woods Hole. -
Coral Populations on Reef Slopes and Their Major Controls
Vol. 7: 83-115. l982 MARINE ECOLOGY - PROGRESS SERIES Published January 1 Mar. Ecol. Prog. Ser. l l REVIE W Coral Populations on Reef Slopes and Their Major Controls C. R. C. Sheppard Australian Institute of Marine Science, P.M.B. No. 3, Townsville M.S.O.. Q. 4810, Australia ABSTRACT: Ecological studies of corals on reef slopes published in the last 10-15 y are reviewed. Emphasis is placed on controls of coral distributions. Reef slope structures are defined with particular reference to the role of corals in providing constructional framework. General coral distributions are synthesized from widespread reefs and are described in the order: shallowest, most exposed reef slopes; main region of hermatypic growth; deepest studies conducted by SCUBA or submersible, and cryptic habitats. Most research has concerned the area between the shallow and deep extremes. Favoured methods of study have involved cover, zonation and diversity, although inadequacies of these simple measurements have led to a few multivariate treatments of data. The importance of early life history strategies and their influence on succession and final community structure is emphasised. Control of coral distribution exerted by their dual nutrition requirements - particulate food and light - are the least understood despite being extensively studied Well studied controls include water movement, sedimentation and predation. All influence coral populations directly and by acting on competitors. Finally, controls on coral population structure by competitive processes between species, and between corals and other taxa are illustrated. Their importance to general reef ecology so far as currently is known, is described. INTRODUCTION ecological studies of reef corals beyond 50 m to as deep as 100 m.