Coastal Observatory Research Arrays: a Framework for Implementation Planning

Total Page:16

File Type:pdf, Size:1020Kb

Coastal Observatory Research Arrays: a Framework for Implementation Planning Coastal Observatory Research Arrays: A Framework for Implementation Planning CoOP Report Number 9December 2003 Richard Jahnke, John Bane, Andrew Barnard, John Barth, Francisco Chavez, Hans Dam, Ed Dever, Paul DiGiacomo, James Edson, Rocky Geyer, Scott Glenn, Ken Johnson, Mark Moline, James O’Donnell, Joan Oltman-Shay, Ola Persson, Oscar Schofield, Heidi Sosik, Eric Terrill SkIO TR-03-01 Coastal Observatory Research Arrays: A Framework for Implementation Planning Report on the CoOP CORA Workshop 12-13 November 2003 Chicago, Illinois Richard Jahnke, John Bane, Andrew Barnard, John Barth, Francisco Chavez, Hans Dam, Ed Dever, Paul DiGiacomo, James Edson, Rocky Geyer, Scott Glenn, Ken Johnson, Mark Moline, James O’Donnell, Joan Oltman-Shay, Ola Persson, Oscar Schofield, Heidi Sosik, Eric Terrill Coastal Ocean Processes (CoOP) Program Report Number 9 December 2003 Technical Report Funding provided by the National Science Foundation under Grant No. OCE-0301872 and by the Office of Naval Research under Grant No. N00014010129. Reproduction in whole or in part is permitted for any purpose of the United States Government. This report should be cited as: Skidaway Institute of Oceanography Technical Report TR-03-01. Table of Contents Executive Summary 1 I. Introduction and Background 3 II. Design Elements of Coastal Observatory Research Arrays 5 A. Endurance Array 5 B. Pioneer Arrays 6 C. Supporting Remote Sensing and Measurements from Mobile Platforms 6 III. Implementation 8 A. Implementation Plans and Timing 8 B. Summary of Required Array Elements 9 C. Relationship to Other Programs and OOI Elements 10 D. Summary of Candidate Locations for Implementation 12 IV. Critical Research Questions/Science Themes 24 A. Ocean Climate and Biogeochemical Cycling 25 B. Ecosystem Dynamics, Turbulent Mixing and Biophysical Interactions 27 C. Fluids and Life in Continental Margin Sediments 28 D. Cross-cutting Coastal Ocean Processes 30 V. Regional Settings and Justification of Candidate Locations 31 A. Middle Atlantic Bight/Gulf of Maine 31 B. South Atlantic Bight 35 C. Gulf of Mexico 40 D. Southern California Bight 45 E. Central California 50 F. Pacific Northwest 54 G. Gulf of Alaska/Arctic 60 H. Great Lakes 67 I. Hawaii Region 70 VI. Acknowledgements 73 VII. References 74 VIII. Participants 76 Executive Summary The design of coastal observatories presents a in particular, that there was no community significant challenge - how to incorporate the consensus concerning the proportion of fixed vast range of relevant scales required to ad- and relocatable observatory elements. vance our understanding of important coastal processes. Cross-margin exchanges and The Coastal Observatory Research Array transport may often be focused or aligned by (CORA) Workshop (Chicago IL, 12 - 13 Novem- local topography and yet interactions of pro- ber 2003) was convened specifically to develop cesses may change regionally in response to consensus regarding the design of coastal differences in larger-scale environmental factors. observatories. The goal of the workshop was to provide an overall vision of the mix of required In the previous 18 months, numerous work- coastal Ocean Observatories Initiative (OOI) shops and reports have concluded that the elements, thereby providing a framework upon development of coastal ocean observatories which future implementation plans could be would significantly advance ocean research. built. These reports include: the CoOP Coastal Obser- vatory Science (COS) report, the Scientific CORA attendees agreed that the scientific Cables for Oceanographic Time-Series justification for developing comprehensive (SCOTS) report, the Cabled Regional Observa- coastal observatories for research is well estab- tory Workshop (CROW) and the National Re- lished in the preceding documents and that search Council report entitled “Enabling Ocean there is a need to develop a broad portfolio of Research in the 21st Century: Implementation of observational capabilities based on fixed, a Network of Ocean Observatories”. moored and cabled technologies; mobile plat- forms, such as gliders, autonomous underwater These reports identified or acknowledged vehicles, and ships; and land, air and space- compelling science issues that will require based remote sensing systems. The OOI will advanced observational techniques and agreed need to work with other agencies and initiatives that emerging observatory infrastructure will to ensure that the full spectrum of observational permit the exploration of ocean processes at tools are available to meet future research time and space scales previously not possible. needs. Because there was generally only a small overlap in the participants at the various work- To achieve the range of observing scales identi- shops, these activities demonstrated significant fied in the science issues, the three-tiered, community-wide support for establishing coastal nested organization of coastal observatories observatories. was again adopted. It is recommended that permanent and relocatable observing arrays be The COS report suggested a nested, three- installed in the US coastal ocean. The fixed tiered approach in which observatories with array, termed the Endurance Array, would be multiple observation nodes are installed in comprised of a set of observing locations ar- widely-distributed regions. In addition, relocat- ranged as cross-shelf lines and individual able mooring arrays (Pioneer Arrays) were moorings that would be installed throughout the recommended for development to provide major coastal regions of the US. detailed information about targeted processes. The COS report did not specify numbers of the For implementation purposes, the US coastal different components, nor did it recommend an area was subdivided into geographic provinces implementation schedule. The subsequent NRC consisting of: Middle Atlantic Bight/Gulf of report noted that the scientific justification was Maine, South Atlantic Bight, Gulf of Mexico, well established for coastal observatories, but Southern California Bight, Central California, that there was no clear implementation path and Pacific Northwest, Gulf of Alaska/Arctic, Hawai- 1 ian Region and Great Lakes. Because these tories. To support this early implementation, regions encompass a range of margin geom- there is an immediate need for detailed design etries and process interactions, distributed studies to more firmly establish cost estimates observatories are required to provide the diver- and focus the discussion on specific deployment sity of observations necessary to advance our sites and configurations. understanding of coastal physical and bio- geochemical dynamics. Finally, it is envisioned that once the observato- ries are installed and operating, research fund- To achieve the widely distributed array that is ing to use this infrastructure will continue to be envisioned, it is recommended that Endurance based on the NSF peer-review system to ensure Array elements be installed in each region that the highest quality of research is supported. during the first five-year phase of the OOI. A subset of Endurance Array locations must be equipped with high power and communications bandwidth capabilities to support diverse inter- disciplinary sensors, observatory operations and engineering development activities. It is further recommended that four arrays of relocatable sensor moorings capable of real- time data telemetry (Pioneer Arrays) be devel- oped. The design of these arrays should be optimized for environmental conditions such as those characterizing the East coast, Gulf of Mexico coast, Great Lakes, West coast, and Gulf of Alaska coast, which will provide a signifi- cant logistical benefit. As the Pioneer Arrays are a relocatable technology, they are available for use in all coastal regions and all areas will benefit from their development. It must be stressed that these permanent and relocatable components synergistically support each other. The Pioneer Arrays provide detailed information of the interactions among processes and spatial variability not achievable from limited, fixed locations while the Endurance Array provides the temporal context in which to interpret the process study observations. As such, these two arrays form the complete vision of the OOI coastal effort. We recommend that the funding profile for the Endurance and Pioneer Arrays be concentrated in the beginning of the OOI support period. This frontloading reflects the state of readiness of coastal observatory technologies and the imme- diate need for test sites for engineering design and development of the components for the regional cabled and global buoy-based observa- 2 I. Introduction and Background Coastal observatories will contribute to the Because the COS workshop preceded the success of the Ocean Observatories Initiative in SCOTS workshop which was specifically three fundamental ways. First, many of today’s charged to address the issue of cable-based compelling science issues and emerging re- observatories and because the definition of a search programs require a significantly im- national “backbone” to be implemented as part proved understanding of the physical dynamics, of the Integrated Ocean Observing System biogeochemistry and ecology of ocean margins. (IOOS) was in its infancy, much of the COS The range of space and time scales involved discussion focused on the design of the Pioneer and the diversity of necessary measurements Array. This array was envisioned as a relocat- require the establishment of coastal
Recommended publications
  • Methane Cold Seeps As Biological Oases in the High‐
    LIMNOLOGY and Limnol. Oceanogr. 00, 2017, 00–00 VC 2017 The Authors Limnology and Oceanography published by Wiley Periodicals, Inc. OCEANOGRAPHY on behalf of Association for the Sciences of Limnology and Oceanography doi: 10.1002/lno.10732 Methane cold seeps as biological oases in the high-Arctic deep sea Emmelie K. L. A˚ strom€ ,1* Michael L. Carroll,1,2 William G. Ambrose, Jr.,1,2,3,4 Arunima Sen,1 Anna Silyakova,1 JoLynn Carroll1,2 1CAGE - Centre for Arctic Gas Hydrate, Environment and Climate, Department of Geosciences, UiT The Arctic University of Norway, Tromsø, Norway 2Akvaplan-niva, FRAM – High North Research Centre for Climate and the Environment, Tromsø, Norway 3Division of Polar Programs, National Science Foundation, Arlington, Virginia 4Department of Biology, Bates College, Lewiston, Maine Abstract Cold seeps can support unique faunal communities via chemosynthetic interactions fueled by seabed emissions of hydrocarbons. Additionally, cold seeps can enhance habitat complexity at the deep seafloor through the accretion of methane derived authigenic carbonates (MDAC). We examined infaunal and mega- faunal community structure at high-Arctic cold seeps through analyses of benthic samples and seafloor pho- tographs from pockmarks exhibiting highly elevated methane concentrations in sediments and the water column at Vestnesa Ridge (VR), Svalbard (798 N). Infaunal biomass and abundance were five times higher, species richness was 2.5 times higher and diversity was 1.5 times higher at methane-rich Vestnesa compared to a nearby control region. Seabed photos reveal different faunal associations inside, at the edge, and outside Vestnesa pockmarks. Brittle stars were the most common megafauna occurring on the soft bottom plains out- side pockmarks.
    [Show full text]
  • Coastal and Marine Ecological Classification Standard (2012)
    FGDC-STD-018-2012 Coastal and Marine Ecological Classification Standard Marine and Coastal Spatial Data Subcommittee Federal Geographic Data Committee June, 2012 Federal Geographic Data Committee FGDC-STD-018-2012 Coastal and Marine Ecological Classification Standard, June 2012 ______________________________________________________________________________________ CONTENTS PAGE 1. Introduction ..................................................................................................................... 1 1.1 Objectives ................................................................................................................ 1 1.2 Need ......................................................................................................................... 2 1.3 Scope ........................................................................................................................ 2 1.4 Application ............................................................................................................... 3 1.5 Relationship to Previous FGDC Standards .............................................................. 4 1.6 Development Procedures ......................................................................................... 5 1.7 Guiding Principles ................................................................................................... 7 1.7.1 Build a Scientifically Sound Ecological Classification .................................... 7 1.7.2 Meet the Needs of a Wide Range of Users ......................................................
    [Show full text]
  • Grade 3 Unit 2 Overview Open Ocean Habitats Introduction
    G3 U2 OVR GRADE 3 UNIT 2 OVERVIEW Open Ocean Habitats Introduction The open ocean has always played a vital role in the culture, subsistence, and economic well-being of Hawai‘i’s inhabitants. The Hawaiian Islands lie in the Pacifi c Ocean, a body of water covering more than one-third of the Earth’s surface. In the following four lessons, students learn about open ocean habitats, from the ocean’s lighter surface to the darker bottom fl oor thousands of feet below the surface. Although organisms are scarce in the deep sea, there is a large diversity of organisms in addition to bottom fi sh such as polycheate worms, crustaceans, and bivalve mollusks. They come to realize that few things in the open ocean have adapted to cope with the increased pressure from the weight of the water column at that depth, in complete darkness and frigid temperatures. Students fi nd out, through instruction, presentations, and website research, that the vast open ocean is divided into zones. The pelagic zone consists of the open ocean habitat that begins at the edge of the continental shelf and extends from the surface to the ocean bottom. This zone is further sub-divided into the photic (sunlight) and disphotic (twilight) zones where most ocean organisms live. Below these two sub-zones is the aphotic (darkness) zone. In this unit, students learn about each of the ocean zones, and identify and note animals living in each zone. They also research and keep records of the evolutionary physical features and functions that animals they study have acquired to survive in harsh open ocean habitats.
    [Show full text]
  • 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.
    [Show full text]
  • Seafloor Mapping of the Continental Slope of the U.S. Atlantic Margin to Study Submarine Landslides That Could Trigger Tsunamis
    Seafloor Mapping of the Continental Slope of the U.S. Atlantic Margin to Study Submarine Landslides that Could Trigger Tsunamis An additional Report to the Nuclear Regulatory Commission Job Code Number: N6480 By Atlantic and Gulf of Mexico Tsunami Hazard Assessment Group Seafloor Mapping of the Continental Slope of the U.S. Atlantic Margin to Study Submarine Landslides that Could Trigger Tsunamis An Additional Report to the Nuclear Regulatory Commission By Atlantic and Gulf of Mexico Tsunami Hazard Assessment Group: Uri ten Brink, David Twichell, Jason Chaytor, Bill Danforth, Brian Andrews, and Elizabeth Pendleton U.S. Geological Survey, Woods Hole Coastal and Marine Science Center, Woods Hole, Massachusetts, USA This reports provides additional information to the report Evaluation of Tsunami Sources with Potential to Impact the U.S. Atlantic and Gulf Coasts, submitted to the Nuclear Regulatory Commission on August 22, 2008. October 15, 2010 NOTICE FROM USGS This publication was prepared by an agency of the United States Government. Neither the United States Government nor any agency thereof, nor any of their employees, make any warranty, expressed or implied, or assumes any legal liability or responsibility for the accuracy, completeness, or usefulness of any information, apparatus, product, or process disclosed in this report, or represent that its use would not infringe privately owned rights. Reference therein to any specific commercial product, process, or service by trade name, trademark, manufacturer, or otherwise does not necessarily constitute or imply its endorsement, recommendation, or favoring by the United States Government or any agency thereof. Any views and opinions of authors expressed herein do not necessarily state or reflect those of the United States Government or any agency thereof.
    [Show full text]
  • 18 Exchanges of Carbon in the Coastal Seas Chen-Tung Arthur Chen
    Scope 62-II.qxd 11/12/03 4:20 PM Page 341 18 Exchanges of Carbon in the Coastal Seas Chen-Tung Arthur Chen In the natural carbon cycle, the time period for atmosphere-biosphere exchange ranges from only a few months to a few decades. The exchange of CO2 between the atmos- phere and the hydrosphere, by contrast, takes several hundred years if the interior of the oceans is taken into consideration. The exchange is much more rapid, however, on a time scale of a few years or even less, for only the terrestrial hydrosphere and the sur- face mixed layer of the oceans. The time for the atmosphere-lithosphere exchange is very long, requiring many thousands of years or more. The shallow sediments on the conti- nental shelves interact relatively readily with the atmosphere. Some terrestrial material even crosses the shelves, which have a mean width of 70 kilometers (km) and a total area of 26 × 106 km2, and efficiently reaches the slopes, which start at an average depth of 130 meters (m) (Gattuso et al. 1998). Dissolved organic matter may also be swiftly car- ried to the interior of the oceans through intermediate bodies of water in certain areas, including the Arctic, Okhotsk, Mediterranean, and Red Seas (Walsh 1995; Chen et al. 2003). The specific rates of productivity, biogeochemical cycling, and sequestration of CO2 are higher in the continental margins than in the open oceans. The end result is that it may take only years, as opposed to hundreds of years, for the atmosphere, lith- osphere, biosphere, and hydrosphere to interact in the continental margins.
    [Show full text]
  • Carbon Cycling in the North American Coastal Ocean: a Synthesis
    Biogeosciences, 16, 1281–1304, 2019 https://doi.org/10.5194/bg-16-1281-2019 © Author(s) 2019. This work is distributed under the Creative Commons Attribution 4.0 License. Carbon cycling in the North American coastal ocean: a synthesis Katja Fennel1, Simone Alin2, Leticia Barbero3, Wiley Evans4, Timothée Bourgeois1, Sarah Cooley5, John Dunne6, Richard A. Feely2, Jose Martin Hernandez-Ayon7, Xinping Hu8, Steven Lohrenz9, Frank Muller-Karger10, Raymond Najjar11, Lisa Robbins10, Elizabeth Shadwick12, Samantha Siedlecki13, Nadja Steiner14, Adrienne Sutton2, Daniela Turk15, Penny Vlahos13, and Zhaohui Aleck Wang16 1Department of Oceanography, Dalhousie University, 1355 Oxford Street, Halifax B3H 4R2, Nova Scotia, Canada 2NOAA Pacific Marine Environmental Laboratory, Seattle, WA 98115, USA 3NOAA Atlantic Oceanographic and Meteorological Laboratory, Miami, FL 33149, USA 4Hakai Institute, Campbell River, BC, V9W 0B7, Canada 5Ocean Conservancy, USA 6NOAA Geophysical Fluid Dynamics Laboratory, Princeton, NJ 08540, USA 7Department of Marine Science, Autonomous University of Baja California, Ensenada, Baja California, CP 228600, Mexico 8Department of Physical and Environmental Sciences, Texas A&M University, Corpus Christi, TX 78412, USA 9School for Marine Science and Technology, University of Massachusetts, Dartmouth, MA 02747, USA 10Department of Marine Science, University of South Florida, Tampa, FL 33620, USA 11Department of Meteorology and Atmospheric Sciences, University Park, Pennsylvania 16802, USA 12The Department is Oceans & Atmosphere. The Institution is CSIRO, Hobart, TAS 7000, Australia 13Marine Sciences, University of Connecticut, Groton, CT 06340, USA 14Department of Fisheries and Oceans Canada, Sidney, BC V8L 4B2, Canada 15Lamont-Doherty Earth Observatory, Palisades, NY 10964, USA 16Woods Hole Oceanographic Institution, Woods Hole, MA 02543, USA Correspondence: Katja Fennel ([email protected]) Received: 19 September 2018 – Discussion started: 20 September 2018 Revised: 28 February 2019 – Accepted: 8 March 2019 – Published: 27 March 2019 Abstract.
    [Show full text]
  • Save the Reef
    Save the Reef A member group of Lock the Gate Alliance www.savethereef.net.au Committee Secretary Senate Standing Committees on Environment and Communications PO Box 6100 Parliament House Canberra ACT 2600 Phone: +61 2 6277 3526 Fax: +61 2 6277 5818 [email protected] Submission to the Senate Inquiry on The adequacy of the Australian and Queensland Governments’ efforts to stop the rapid decline of the Great Barrier Reef, including but not limited to: Points a–k. Save the Reef would like to thank this committee for the opportunity to make a submission and would also like to speak further if there is an opportunity at any public hearings. The Great Barrier Reef is Australia’s greatest natural asset. It is a tourism mecca, a 6 billion dollar economic boon as well as a scientific wonderland. It is a World Heritage Listed property and an acknowledged world wonder. The Great Barrier Reef is part of Australia’s very identity. We are failing to protect the Great Barrier Reef. The efforts to stop the rapid decline of the Great Barrier Reef are grossly inadequate. It demonstrates that our current system for protecting the environment is broken. Environmental impact statements, conditions, offsets, regulations, enforcement and even the EPBC act, processes meant to protect the environment are being subverted and the impact is apparent. The holes in the “Swiss Cheese” are lining up and have allowed and are continuing to allow further destruction of the Great Barrier Reef when it needs our protection the most. The recent developments in Gladstone are a clear demonstration of the failure of our systems.
    [Show full text]
  • Ocean Depths: the Mesopelagic and Implications for Global Warming
    Current Biology Dispatches Ocean Depths: The Mesopelagic and Implications for Global Warming Mark J. Costello1,* and Sean Breyer2 1Institute of Marine Science, University of Auckland, Auckland, 1142, New Zealand 2ESRI, Redlands, CA 92373, USA *Correspondence: [email protected] http://dx.doi.org/10.1016/j.cub.2016.11.042 The mesopelagic or ‘twilight zone’ of the oceans occurs too deep for photosynthesis, but is a major part of the world’s carbon cycle. Depth boundaries for the mesopelagic have now been shown on a global scale using the distribution of pelagic animals detected by compiling echo-soundings from ships around the world, and been used to predict the effect of global warming on regional fish production. Depth Zonation Analyses were at 5 m depth intervals to However, it remains to be clearly shown The classical concepts for depth zonation 1,000 m deep, and a spatial resolution of whether the abyssal zone is ecologically [1] in the ocean begin at the seashore 300 km2. distinct from the bathyal. (Table 1). Distinct communities are visible The environment changes less as we The data shown in Figure 1 are global on the rocky seashore, and reflect the go deeper (Figure 1), so we expect the averages, and local exceptions will occur, adaptations of their animals and plants vertical extent of ecological zones to particularly in more enclosed waters such to exposure to air and wave action, increase with depth. While the rocky as the Mediterranean and Black Seas [6]. as well as the effects of grazing and seashore may have distinct habitats only The seabed-resident fauna (benthos) will predation [2].
    [Show full text]
  • Sample Chapter Algal Blooms
    ALGAL BLOOMS 7 Observations and Remote Sensing. http://dx.doi.org/10.1109/ energy and material transport through the food web, and JSTARS.2013.2265255. they also play an important role in the vertical flux of Pack, R. T., Brooks, V., Young, J., Vilaca, N., Vatslid, S., Rindle, P., material out of the surface waters. These blooms are Kurz, S., Parrish, C. E., Craig, R., and Smith, P. W., 2012. An “ ” overview of ALS technology. In Renslow, M. S. (ed.), Manual distinguished from those that are deemed harmful. of Airborne Topographic Lidar. Bethesda: ASPRS Press. Algae form harmful algal blooms, or HABs, when either Sithole, G., and Vosselman, G., 2004. Experimental comparison of they accumulate in massive amounts that alone cause filter algorithms for bare-Earth extraction from airborne laser harm to the ecosystem or the composition of the algal scanning point clouds. ISPRS Journal of Photogrammetry and community shifts to species that make compounds Remote Sensing, 59,85–101. (including toxins) that disrupt the normal food web or to Shan, J., and Toth, C., 2009. Topographic Laser Ranging and Scanning: Principles and Processes. Boca Raton: CRC Press. species that can harm human consumers (Glibert and Slatton, K. C., Carter, W. E., Shrestha, R. L., and Dietrich, W., 2007. Pitcher, 2001). HABs are a broad and pervasive problem, Airborne laser swath mapping: achieving the resolution and affecting estuaries, coasts, and freshwaters throughout the accuracy required for geosurficial research. Geophysical world, with effects on ecosystems and human health, and Research Letters, 34,1–5. on economies, when these events occur. This entry Wehr, A., and Lohr, U., 1999.
    [Show full text]
  • Harmful Algal Bloom Response Program
    What are HABs? • Blue-green algae are bacteria that grow in water, contain chlorophyll, and can photosynthesize. They are not a new occurrence. WHEN IN DOUBT, STAY OUT! Kansas Department of Health • When these bacteria reproduce rapidly, For additional information: and Environment it can create a Harmful Algal Bloom (HAB). Please visit • HABs can sometimes produce toxins www.kdheks.gov/algae-illness. Harmful that affect people, pets, livestock, and Or call the KDHE HAB Hotline at wildlife. The toxins can affect the skin, 785-296-1664. liver, and nervous system. Algal Bloom • People and animals may be exposed to toxins via ingestion, skin contact, or Response inhalation of contaminated water. Program • The most common human health effects from HABs can include vomiting, diarrhea, skin rashes, eye irritation, and respiratory symptoms. • Boiling water does not remove or Department of Health inactivate toxins from blue-green algae, and Environment and there is no known antidote. • Animal deaths due to HAB toxins have Department of Health been documented, so: and Environment When in doubt, stay out! To protect and improve the health and environment of all Kansans. How else is KDHE working to What causes HABs? HAB Advisory Levels prevent HABs? Blue-green algae are a natural part of water- Threshold Levels based ecosystems. They become a problem Harmful Algal Blooms thrive in the presence when nutrients (phosphorus and nitrogen) are Watch Warning Closure of excess nutrients such as nitrogen and present in concentrations above what would phosphorus. Thus, KDHE continually works to occur naturally. Under these conditions, algae blue green reduce nutrient input and improve overall can grow very quickly to extreme numbers, cell counts 80,000 250,000 10,000,000 water quality through a series of interrelated resulting in a Harmful Algal Bloom.
    [Show full text]
  • Active Continental Margin
    Encyclopedia of Marine Geosciences DOI 10.1007/978-94-007-6644-0_102-2 # Springer Science+Business Media Dordrecht 2014 Active Continental Margin Serge Lallemand* Géosciences Montpellier, University of Montpellier, Montpellier, France Synonyms Convergent boundary; Convergent margin; Destructive margin; Ocean-continent subduction; Oceanic subduction zone; Subduction zone Definition An active continental margin refers to the submerged edge of a continent overriding an oceanic lithosphere at a convergent plate boundary by opposition with a passive continental margin which is the remaining scar at the edge of a continent following continental break-up. The term “active” stresses the importance of the tectonic activity (seismicity, volcanism, mountain building) associated with plate convergence along that boundary. Today, people typically refer to a “subduction zone” rather than an “active margin.” Generalities Active continental margins, i.e., when an oceanic plate subducts beneath a continent, represent about two-thirds of the modern convergent margins. Their cumulated length has been estimated to 45,000 km (Lallemand et al., 2005). Most of them are located in the circum-Pacific (Japan, Kurils, Aleutians, and North, Middle, and South America), Southeast Asia (Ryukyus, Philippines, New Guinea), Indian Ocean (Java, Sumatra, Andaman, Makran), Mediterranean region (Aegea, Cala- bria), or Antilles. They are generally “active” over tens (Tonga, Mariana) or hundreds (Japan, South America) of millions of years. This longevity has consequences on their internal structure, especially in terms of continental growth by tectonic accretion of oceanic terranes, or by arc magmatism, but also sometimes in terms of continental consumption by tectonic erosion. Morphology A continental margin generally extends from the coast down to the abyssal plain (see Fig.
    [Show full text]