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Chesapeake Bay Restoration: Background and Issues for Congress
Chesapeake Bay Restoration: Background and Issues for Congress Updated August 3, 2018 Congressional Research Service https://crsreports.congress.gov R45278 SUMMARY R45278 Chesapeake Bay Restoration: Background and August 3, 2018 Issues for Congress Eva Lipiec The Chesapeake Bay (the Bay) is the largest estuary in the United States. It is Analyst in Natural recognized as a “Wetlands of International Importance” by the Ramsar Convention, a Resources Policy 1971 treaty about the increasing loss and degradation of wetland habitat for migratory waterbirds. The Chesapeake Bay estuary resides in a more than 64,000-square-mile watershed that extends across parts of Delaware, Maryland, New York, Pennsylvania, Virginia, West Virginia, and the District of Columbia. The Bay’s watershed is home to more than 18 million people and thousands of species of plants and animals. A combination of factors has caused the ecosystem functions and natural habitat of the Chesapeake Bay and its watershed to deteriorate over time. These factors include centuries of land-use changes, increased sediment loads and nutrient pollution, overfishing and overharvesting, the introduction of invasive species, and the spread of toxic contaminants. In response, the Bay has experienced reductions in economically important fisheries, such as oysters and crabs; the loss of habitat, such as underwater vegetation and sea grass; annual dead zones, as nutrient- driven algal blooms die and decompose; and potential impacts to tourism, recreation, and real estate values. Congress began to address ecosystem degradation in the Chesapeake Bay in 1965, when it authorized the first wide-scale study of water resources of the Bay. Since then, federal restoration activities, conducted by multiple agencies, have focused on reducing pollution entering the Chesapeake Bay, restoring habitat, managing fisheries, protecting sub-watersheds within the larger Bay watershed, and fostering public access and stewardship of the Bay. -
Limits of Iron Fertilization
LIMITS OF IRON FERTILIZATION Anand Gnanadesikan1, John P. Dunne1 and Irina Marinov2 1: NOAA Geophysical Fluid Dynamics Laboratory, PO Box 308, Princeton, NJ 08542 [email protected], [email protected] 2: Department of Earth, Atmosphere and Planetary Sciences, Massachusetts Institute of Technology, Cambridge, MA, [email protected] ABSTRACT Iron fertilization has been proposed as a cheap, controllable, and environmentally benign method for removing carbon dioxide from the atmosphere. While this is in fact the case in simple, 3-box models of the carbon cycle, more realistic models show that these claims fall short of reality. The fact that the efficiency of iron fertilization depends on the long term fate of the added iron and on the carbon associated with it makes tracking the effects of iron fertilization much more difficult and expensive than has been asserted. Additionally, advection of low nutrient water away from iron-rich areas can result in lowering production remotely, with potentially serious consequences. INTRODUCTION The idea of offsetting anthropogenic carbon dioxide emissions by fertilizing the ocean with iron has a number of superficially attractive features. A host of iron fertilization experiments have demonstrated that adding iron to surface waters leads to a local increase in productivity [see for example Coale et al., 1996]. Our own survey of the literature [Dunne et al. subm.] shows that this should be expected to lead to a local increase in particle export. It is claimed however, that this local increase in particle export would necessarily lead to an easily verifiable drawdown in atmospheric carbon dioxide. It is further claimed that the increase in export is controllable and environmentally benign, implying that the effects cease as soon as the fertilization stops. -
Fertilizing the Ocean with Iron Is This a Viable Way to Help Reduce Carbon Dioxide Levels in the Atmosphere?
380 Fertilizing the Ocean with Iron Is this a viable way to help reduce carbon dioxide levels in the atmosphere? 360 ive me half a tanker of iron, and I’ll give you an ice Twenty years on, Martin’s line is still viewed alternately age” may rank as the catchiest line ever uttered by a as a boast or a quip—an opportunity too good to pass up or a biogeochemist.“G The man responsible was the late John Martin, misguided remedy doomed to backfire. Yet over the same pe- former director of the Moss Landing Marine Laboratory, who riod, unrelenting increases in carbon emissions and mount- discovered that sprinkling iron dust in the right ocean waters ing evidence of climate change have taken the debate beyond could trigger plankton blooms the size of a small city. In turn, academic circles and into the free market. the billions of cells produced might absorb enough heat-trap- Today, policymakers, investors, economists, environ- ping carbon dioxide to cool the Earth’s warming atmosphere. mentalists, and lawyers are taking notice of the idea. A few Never mind that Martin companies are planning new, was only half serious when larger experiments. The ab- 340 he made the remark (in his Ocean Iron Fertilization sence of clear regulations for “best Dr. Strangelove accent,” either conducting experiments he later recalled) at an infor- An argument for: Faced with the huge at sea or trading the results mal seminar at Woods Hole consequences of climate change, iron’s in “carbon offset” markets Oceanographic Institution outsized ability to put carbon into the oceans complicates the picture. -
The Economics of Dead Zones: Causes, Impacts, Policy Challenges, and a Model of the Gulf of Mexico Hypoxic Zone S
58 The Economics of Dead Zones: Causes, Impacts, Policy Challenges, and a Model of the Gulf of Mexico Hypoxic Zone S. S. Rabotyagov*, C. L. Klingy, P. W. Gassmanz, N. N. Rabalais§ ô and R. E. Turner Downloaded from Introduction The BP Deepwater Horizon oil spill in the Gulf of Mexico in 2010 increased public awareness and http://reep.oxfordjournals.org/ concern about long-term damage to ecosystems, and casual readers of the news headlines may have concluded that the spill and its aftermath represented the most significant and enduring environmental threat to the region. However, the region faces other equally challenging threats including the large seasonal hypoxic, or “dead,” zone that occurs annually off the coast of Louisiana and Texas. Even more concerning is the fact that such dead zones have been appearing worldwide at proliferating rates (Conley et al. 2011; Diaz and Rosenberg 2008). Nutrient over- enrichment is the main cause of these dead zones, and nutrient-fed hypoxia is now widely at Iowa State University on January 27, 2014 considered an important threat to the health of aquatic ecosystems (Doney 2010). The rather alarming term dead zone is surprisingly appropriate: hypoxic regions exhibit oxygen levels that are too low to support many aquatic organisms including commercially desirable species. While some dead zones are naturally occurring, their number, size, and *School of Environmental and Forest Sciences, University of Washington, Seattle, Washington, USA; e-mail: [email protected] yCenter for Agricultural and Rural Development, -
Marine Ecology Progress Series 601:77
Vol. 601: 77–95, 2018 MARINE ECOLOGY PROGRESS SERIES Published August 9 https://doi.org/10.3354/meps12685 Mar Ecol Prog Ser OPENPEN ACCESSCCESS Remarkable structural resistance of a nanoflagellate- dominated plankton community to iron fertilization during the Southern Ocean experiment LOHAFEX Isabelle Schulz1,2,3, Marina Montresor4, Christine Klaas1, Philipp Assmy1,2,5, Sina Wolzenburg1, Mangesh Gauns6, Amit Sarkar6,7, Stefan Thiele8,9, Dieter Wolf-Gladrow1, Wajih Naqvi6, Victor Smetacek1,6,* 1Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung, 27570 Bremerhaven, Germany 2MARUM − Center for Marine Environmental Sciences, University of Bremen, 28359 Bremen, Germany 3Biological and Environmental Science and Engineering Division, Red Sea Research Center, King Abdullah University of Science and Technology, 23955-6900 Thuwal, Kingdom of Saudi Arabia 4Stazione Zoologica Anton Dohrn, 80121 Naples, Italy 5Norwegian Polar Institute, Fram Centre, 9296 Tromsø, Norway 6CSIR National Institute of Oceanography, 403 004 Goa, India 7National Centre for Antarctic and Ocean Research, 403 804 Goa, India 8Max Planck Institute for Marine Microbiology, 28359 Bremen, Germany 9Institute for Inorganic and Analytical Chemistry, Friedrich Schiller University, 07743 Jena, Germany ABSTRACT: The genesis of phytoplankton blooms and the fate of their biomass in iron-limited, high-nutrient−low-chlorophyll regions can be studied under natural conditions with ocean iron fertilization (OIF) experiments. The Indo-German OIF experiment LOHAFEX was carried out over 40 d in late summer 2009 within the cold core of a mesoscale eddy in the productive south- west Atlantic sector of the Southern Ocean. Silicate concentrations were very low, and phyto- plankton biomass was dominated by autotrophic nanoflagellates (ANF) in the size range 3−10 µm. -
Ocean Iron Fertilization Experiments – Past, Present, and Future Looking to a Future Korean Iron Fertilization Experiment in the Southern Ocean (KIFES) Project
Biogeosciences, 15, 5847–5889, 2018 https://doi.org/10.5194/bg-15-5847-2018 © Author(s) 2018. This work is distributed under the Creative Commons Attribution 3.0 License. Reviews and syntheses: Ocean iron fertilization experiments – past, present, and future looking to a future Korean Iron Fertilization Experiment in the Southern Ocean (KIFES) project Joo-Eun Yoon1, Kyu-Cheul Yoo2, Alison M. Macdonald3, Ho-Il Yoon2, Ki-Tae Park2, Eun Jin Yang2, Hyun-Cheol Kim2, Jae Il Lee2, Min Kyung Lee2, Jinyoung Jung2, Jisoo Park2, Jiyoung Lee1, Soyeon Kim1, Seong-Su Kim1, Kitae Kim2, and Il-Nam Kim1 1Department of Marine Science, Incheon National University, Incheon 22012, Republic of Korea 2Korea Polar Research Institute, Incheon 21990, Republic of Korea 3Woods Hole Oceanographic Institution, MS 21, 266 Woods Hold Rd., Woods Hole, MA 02543, USA Correspondence: Il-Nam Kim ([email protected]) Received: 2 November 2016 – Discussion started: 15 November 2016 Revised: 16 August 2018 – Accepted: 18 August 2018 – Published: 5 October 2018 Abstract. Since the start of the industrial revolution, hu- providing insight into mechanisms operating in real time and man activities have caused a rapid increase in atmospheric under in situ conditions. To maximize the effectiveness of carbon dioxide (CO2) concentrations, which have, in turn, aOIF experiments under international aOIF regulations in the had an impact on climate leading to global warming and future, we therefore suggest a design that incorporates sev- ocean acidification. Various approaches have been proposed eral components. (1) Experiments conducted in the center of to reduce atmospheric CO2. The Martin (or iron) hypothesis an eddy structure when grazing pressure is low and silicate suggests that ocean iron fertilization (OIF) could be an ef- levels are high (e.g., in the SO south of the polar front during fective method for stimulating oceanic carbon sequestration early summer). -
Geoengineering Research Under U.S. Law
Geoengineering Research Under U.S. Law Rob James Pillsbury Winthrop Shaw Pittman LLP Geoengineering: The Legal Challenges of Climate Mitigation LACBA Environmental Law 34th Annual Spring Super Symposium March 18, 2021 2020-21 has been an (involuntary) geoengineering experiment .2020 tied 2016 as the warmest year on record .Less sulfate pollution, more warming (a “reverse volcano”) .CO2 emissions are down, but expected to bounce back with post- pandemic economic activity .“Clean air warms the planet a tiny bit, but it kills a lot fewer people with air pollution.” Legal precursors . Weather modification—permits, practices as well as litigation o 27 OKLA. L. REV. 409 (1973) o Friedrich et al. PNAS (2020) . Studies of hurricane diversion (and accompanying ethical dilemmas) . Geoengineering, adaptation, and climate change . Unspeakable for years? o “[Adaptation is] a kind of laziness, an arrogant faith in our ability to react in time to save our own skin.” Al Gore, EARTH IN THE BALANCE (1992) Legal precursors . Royal Society (2009) and other studies . Bipartisan Policy Center, 2011 (Dole, Daschle, Mitchell, Baker) . Individual experiments . Debates in international forums . But what is the legal framework? . And what are the legal exposures and benefits? Government activity . March 5, 2021 – DOE Secretary Granholm approves $24 million for direct air capture research . Appropriations Act of 2020—$4 million for NOAA’s Office of Oceanic and Atmospheric Research (OAR) to investigate “Earth’s radiation budget” and “solar climate interventions” o NOAA is currently working with Arizona company to advance study of stratosphere . Carbon capture and sequestration tax credit (IRC, 26 U.S.C. § 45Q) . California Low Carbon Fuel Standard (LCFS) . -
Marine Dead Zones
Marine Dead Zones: Case Study # 2 Presented By: Blair Dudeck, September 24, 2010 Materials Included in the Reading Package: 1. World Resources institute, Aqriculture and ‘dead zones’”, http://archive.wri.org/jlash/letters.cfm?ContentID=4283 accessed Sept 22, 2010 2. NOLA.com, “Despite promises to fix it, the Gulf's dead zone is growing”, http://blog.nola.com/times‐picayune/2007/06/despite_promises_to_fix_it_the.html, Accessed 10/20/2010 3. National Ocean Service, “What is a Dead zone?”, http://oceanservice.noaa.gov/facts/deadzone.html Accessed 10/15/2010 4. How Stuff Works, “Should we be worried about the dead zone in the Gulf of Mexico?”, http://science.howstuffworks.com/environmental/earth/oceanography/dead‐ zone1.htm , Accessed 10/15/2010. 5. NOAA, “Hypoxia in the gulf of Mexico”, by Nancy N. Rablais, Louisiana Universities Marine Consortium, http://www.csc.noaa.gov/products/gulfmex/html/rabalais.htm Accessed 10/16/2010 6. Environmental Chemistry aglobal perspective, “10.2 Two‐Variable Diagrams‐pE/pH Diagrams”, by Gary W.vanLoon, Stephen J. Duffy, 2008, 7. Science News, “Ocean 'Dead Zones' Trigger Sex Changes In Fish, Posing Extinction Threat”, http://www.sciencedaily.com/releases/2006/04/060402220803.htm, Accessed 10/17/2010 8. DAILY NEWS, “UBC professor wins award for developing phosphorus recycling technology”, http://www.solidwastemag.com/issues/story.aspx?aid=1000385128, Accessed 10/15/2010 • Ecosystem thresholds with hypoxia, affects on biochemistry”. Daniel J.Conley, Jacob Carstensen. Assessed sept 15/2010 • Answer Guide to -
Iron Fertilization: a Scientific Review with International Policy Recommendations
Iron Fertilization: A Scientific Review with International Policy Recommendations By Jennie Dean* TABLE OF CONTENTS INTRODUCTION ................................ ....... .322 I. CLIMATE CHANGE AND THE OCEAN ......................................... 322 A . D escribing the problem ................................................................ 322 B. Identifying a potential solution .................................................... 323 II. IRON FERTILIZATION EXAMINED ............................................... 326 A . Potential benefits .......................................................................... 326 B . Potential problem s ........................................................................ 328 C. Synthesis and suggested action .................................................... 333 III. IRON FERTILIZATION AND INTERNATIONAL LAW ................. 334 A . Introduction .................................................................................. 334 B. Coverage under pollution and dumping regulations ..................... 334 C. Coverage under biological conservation regulations .................... 336 D. Coverage under global climate change mitigation regulations ..... 338 IV. RECOM M ENDATION S ..................................................................... 339 A . Suggested modifications ............................................................. 339 B . F easibility ..................................................................................... 340 C O N C L U SIO N ............................................................................................... -
Thick-Shelled, Grazer-Protected Diatoms Decouple Ocean Carbon
Thick-shelled, grazer-protected diatoms decouple SEE COMMENTARY ocean carbon and silicon cycles in the iron-limited Antarctic Circumpolar Current Philipp Assmya,b,1, Victor Smetacekb,c,1, Marina Montresord, Christine Klaasb, Joachim Henjesb, Volker H. Strassb, Jesús M. Arrietae,f, Ulrich Bathmannb,g, Gry M. Bergh, Eike Breitbarthi, Boris Cisewskib,j, Lars Friedrichsb, Nike Fuchsb, Gerhard J. Herndle,k, Sandra Jansenb, Sören Krägefskyb, Mikel Latasal,m, Ilka Peekenb,n, Rüdiger Röttgerso, Renate Scharekl,m, Susanne E. Schüllerp, Sebastian Steigenbergerb,q, Adrian Webbr, and Dieter Wolf-Gladrowb aNorwegian Polar Institute, 9296 Tromsø, Norway; bAlfred Wegener Institute Helmholtz Centre for Polar and Marine Research, 27570 Bremerhaven, Germany; cNational Institute of Oceanography, Dona Paula, Goa 403 004, India; dStazione Zoologica Anton Dohrn, 80121 Napoli, Italy; eDepartment of Biological Oceanography, Royal Netherlands Institute for Sea Research, 1790AB, Den Burg, Texel, The Netherlands; fDepartment of Global Change Research, Instituto Mediterraneo de Estudios Avanzados, Consejo Superior de Investigaciones Científicas–Universidad de las Islas Baleares, 07190 Esporles, Mallorca, Spain; gLeibniz Institute for Baltic Sea Research Warnemünde, 18119 Rostock, Germany; hDepartment of Geophysics, Stanford University, Stanford, CA 94305; iHelmholtz Centre for Ocean Research Kiel, 24105 Kiel, Germany; jThünen Institute of Sea Fisheries, 22767 Hamburg, Germany; kDepartment of Marine Biology, Faculty Center of Ecology, University of Vienna, 1090 Vienna, -
50 Ways to Save the Ocean a Teacher's Guide for Grades 9-12
50 Ways to Save the Ocean Teacher’s Guide Supplemental Lesson Plans A Project of Blue Frontier Campaign Table of Contents Introduction .................................................................................................................................................. 4 How to Use this Guide .................................................................................................................................. 5 1: Go to the Beach ........................................................................................................................................ 6 Coastal Clash .............................................................................................................................................................. 7 Currents: Bad for Divers, Good for Ocean ................................................................................................................. 7 3: Dive Responsibly ....................................................................................................................................... 8 Dive In! ....................................................................................................................................................................... 9 Designing an Underwater Habitat for Humans ......................................................................................................... 9 8: Take Kids Surfing, or Have Them Take You ............................................................................................. 10 Motion -
Status of the Flower Garden Banks of the Northwestern Gulf of Mexico
STATUSSTATUS OFOF THETHE FLOWERFLOWER GARDENGARDEN BANKSBANKS OFOF THETHE NORTHWESTERNNORTHWESTERN GULFGULF OFOF MEXICOMEXICO GeorgeGeorge P.P. SchmahlSchmahl Introduction which about 0.4 km2 is coral reef (Gardner et al. 1998). The Flower Garden Banks are two prominent geo- logical features on the edge of the outer continental Structurally, the Flower Garden Banks coral reefs shelf in the northwest Gulf of Mexico, approxi- are composed of large, closely spaced heads up to mately 192 km southeast of Galveston, Texas. three or more meters in diameter and height. Reef Created by the uplift of underlying salt domes of topography is relatively rough, with many vertical Jurassic origin, they rise from surrounding water and inclined surfaces. If the relief of individual FLOWER GARDENS FLOWER GARDENS FLOWER GARDENS FLOWER GARDENS FLOWER GARDENS FLOWER GARDENS FLOWER GARDENS FLOWER GARDENS depths of over 100 m to within 17 m of the surface coral heads is ignored, the top of the reef is rela- FLOWER GARDENS FLOWER GARDENS (Fig. 205). Stetson Bank, 48 km to the northwest of tively flat between the reef surface and about 30 m. the Flower Gardern Banks, is a separate claystone/ It slopes steeply between 30 m and the reef base. siltstone feature that harbors a low diversity coral Between groups of coral heads, there are sand community. Fishermen gave the Flower Garden patches and channels from 1-100 m long. Sand Banks their name because they could see the bright areas are typically small patches or linear channels. colors of the reef from the surface and pulled the Probably due to its geographic isolation and other brightly colored corals and sponges up on their factors, there are only about 28 species of reef- lines and in their nets.