Coastal and Marine Ecosystems & Global Climate Change
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Lasting Coastal Hazards from Past Greenhouse Gas Emissions COMMENTARY Tony E
COMMENTARY Lasting coastal hazards from past greenhouse gas emissions COMMENTARY Tony E. Wonga,1 The emission of greenhouse gases into Earth’satmo- 100% sphereisaby-productofmodernmarvelssuchasthe Extremely likely by 2073−2138 production of vast amounts of energy, heating and 80% cooling inhospitable environments to be amenable to human existence, and traveling great distances 60% Likely by 2064−2105 faster than our saddle-sore ancestors ever dreamed possible. However, these luxuries come at a price: 40% climate changes in the form of severe droughts, ex- Probability treme precipitation and temperatures, increased fre- 20% quency of flooding in coastal cities, global warming, RCP2.6 and sea-level rise (1, 2). Rising seas pose a severe risk RCP8.5 0% to coastal areas across the globe, with billions of 2020 2040 2060 2080 2100 2120 2140 US dollars in assets at risk and about 10% of the ’ Year when 50-cm sea-level rise world s population living within 10 m of sea level threshold is exceeded (3–5). The price of our emissions is not felt immedi- ately throughout the entire climate system, however, Fig. 1. Cumulative probability of exceeding 50 cm of sea-level rise by year (relative to the global mean sea because processes such as ice sheet melt and the level from 1986 to 2005). The yellow box denotes the expansion of warming ocean water act over the range of years after which exceedance is likely [≥66% course of centuries. Thus, even if all greenhouse probability (12)], where the left boundary follows a gas emissions immediately ceased, our past emis- business-as-usual emissions scenario (RCP8.5, red line) sions have already “locked in” some amount of con- and the right boundary follows a low-emissions scenario (RCP2.6, blue line). -
Sea-Level Rise for the Coasts of California, Oregon, and Washington: Past, Present, and Future
Sea-Level Rise for the Coasts of California, Oregon, and Washington: Past, Present, and Future As more and more states are incorporating projections of sea-level rise into coastal planning efforts, the states of California, Oregon, and Washington asked the National Research Council to project sea-level rise along their coasts for the years 2030, 2050, and 2100, taking into account the many factors that affect sea-level rise on a local scale. The projections show a sharp distinction at Cape Mendocino in northern California. South of that point, sea-level rise is expected to be very close to global projections; north of that point, sea-level rise is projected to be less than global projections because seismic strain is pushing the land upward. ny significant sea-level In compliance with a rise will pose enor- 2008 executive order, mous risks to the California state agencies have A been incorporating projec- valuable infrastructure, devel- opment, and wetlands that line tions of sea-level rise into much of the 1,600 mile shore- their coastal planning. This line of California, Oregon, and study provides the first Washington. For example, in comprehensive regional San Francisco Bay, two inter- projections of the changes in national airports, the ports of sea level expected in San Francisco and Oakland, a California, Oregon, and naval air station, freeways, Washington. housing developments, and sports stadiums have been Global Sea-Level Rise built on fill that raised the land Following a few thousand level only a few feet above the years of relative stability, highest tides. The San Francisco International Airport (center) global sea level has been Sea-level change is linked and surrounding areas will begin to flood with as rising since the late 19th or to changes in the Earth’s little as 40 cm (16 inches) of sea-level rise, a early 20th century, when climate. -
Resilience of Alternative States in Spatially Extended Ecosystems
RESEARCH ARTICLE Resilience of Alternative States in Spatially Extended Ecosystems Ingrid A. van de Leemput*, Egbert H. van Nes, Marten Scheffer Department of Environmental Sciences, Wageningen University, Wageningen, The Netherlands * [email protected] Abstract Alternative stable states in ecology have been well studied in isolated, well-mixed systems. However, in reality, most ecosystems exist on spatially extended landscapes. Applying ex- isting theory from dynamic systems, we explore how such a spatial setting should be ex- pected to affect ecological resilience. We focus on the effect of local disturbances, defining resilience as the size of the area of a strong local disturbance needed to trigger a shift. We show that in contrast to well-mixed systems, resilience in a homogeneous spatial setting does not decrease gradually as a bifurcation point is approached. Instead, as an environ- OPEN ACCESS mental driver changes, the present dominant state remains virtually ‘indestructible’, until at Citation: van de Leemput IA, van Nes EH, Scheffer a critical point (the Maxwell point) its resilience drops sharply in the sense that even a very M (2015) Resilience of Alternative States in Spatially Extended Ecosystems. PLoS ONE 10(2): e0116859. local disturbance can cause a domino effect leading eventually to a landscape-wide shift to doi:10.1371/journal.pone.0116859 the alternative state. Close to this Maxwell point the travelling wave moves very slow. Under Academic Editor: Emanuele Paci, University of these conditions both states have a comparable resilience, allowing long transient co-occur- Leeds, UNITED KINGDOM rence of alternative states side-by-side, and also permanent co-existence if there are mild Received: April 11, 2014 spatial barriers. -
Causes of Sea Level Rise
FACT SHEET Causes of Sea OUR COASTAL COMMUNITIES AT RISK Level Rise What the Science Tells Us HIGHLIGHTS From the rocky shoreline of Maine to the busy trading port of New Orleans, from Roughly a third of the nation’s population historic Golden Gate Park in San Francisco to the golden sands of Miami Beach, lives in coastal counties. Several million our coasts are an integral part of American life. Where the sea meets land sit some of our most densely populated cities, most popular tourist destinations, bountiful of those live at elevations that could be fisheries, unique natural landscapes, strategic military bases, financial centers, and flooded by rising seas this century, scientific beaches and boardwalks where memories are created. Yet many of these iconic projections show. These cities and towns— places face a growing risk from sea level rise. home to tourist destinations, fisheries, Global sea level is rising—and at an accelerating rate—largely in response to natural landscapes, military bases, financial global warming. The global average rise has been about eight inches since the centers, and beaches and boardwalks— Industrial Revolution. However, many U.S. cities have seen much higher increases in sea level (NOAA 2012a; NOAA 2012b). Portions of the East and Gulf coasts face a growing risk from sea level rise. have faced some of the world’s fastest rates of sea level rise (NOAA 2012b). These trends have contributed to loss of life, billions of dollars in damage to coastal The choices we make today are critical property and infrastructure, massive taxpayer funding for recovery and rebuild- to protecting coastal communities. -
Introduction to Theoretical Ecology
Introduction to Theoretical Ecology Natal, 2011 Objectives After this week: The student understands the concept of a biological system in equilibrium and knows that equilibria can be stable or unstable. The student understands the basics of how coupled differential equations can be analyzed graphically, including phase plane analysis and nullclines. The student can analyze the stability of the equilibria of a one-dimensional differential equation model graphically. The student has a basic understanding of what a bifurcation point is. The student can relate alternative stable states to a 1D bifurcation plot (e.g. catastrophe fold). Study material / for further study: This text Scheffer, M. 2009. Critical Transitions in Nature and Society, Princeton University Press, Princeton and Oxford. Scheffer, M. 1998. Ecology of Shallow Lakes. 1 edition. Chapman and Hall, London. Edelstein-Keshet, L. 1988. Mathematical models in biology. 1 edition. McGraw-Hill, Inc., New York. Tentative programme (maybe too tight for the exercises) Monday 9:00-10:30 Introduction Modelling + introduction Forrester diagram + 1D models (stability graphs) 10:30-13:00 GRIND Practical CO2 chamber - Ethiopian Wolf Tuesday 9:00-10:00 Introduction bifurcation (Allee effect) and Phase plane analysis (Lotka-Volterra competition) 10:00-13:00 GRIND Practical Lotka-Volterra competition + Sahara Wednesday 9:00-13:00 GRIND Practical – Sahara (continued) and Algae-zooplankton Thursday 9:00-13:00 GRIND practical – Algae zooplankton spatial heterogeneity Friday 9:00-12:00 GRIND practical- Algae zooplankton fish 12:00-13:00 Practical summary/explanation of results - Wrap up 1 An introduction to models What is a model? The word 'model' is used widely in every-day language. -
Multiple Stable States and Regime Shifts - Environmental Science - Oxford Bibliographies 3/30/18, 10:15 AM
Multiple Stable States and Regime Shifts - Environmental Science - Oxford Bibliographies 3/30/18, 10:15 AM Multiple Stable States and Regime Shifts James Heffernan, Xiaoli Dong, Anna Braswell LAST MODIFIED: 28 MARCH 2018 DOI: 10.1093/OBO/9780199363445-0095 Introduction Why do ecological systems (populations, communities, and ecosystems) change suddenly in response to seemingly gradual environmental change, or fail to recover from large disturbances? Why do ecological systems in seemingly similar settings exhibit markedly different ecological structure and patterns of change over time? The theory of multiple stable states in ecological systems provides one potential explanation for such observations. In ecological systems with multiple stable states (or equilibria), two or more configurations of an ecosystem are self-maintaining under a given set of conditions because of feedbacks among biota or between biota and the physical and chemical environment. The resulting multiple different states may occur as different types or compositions of vegetation or animal communities; as different densities, biomass, and spatial arrangement; and as distinct abiotic environments created by the distinct ecological communities. Alternative states are maintained by the combined effects of positive (or amplifying) feedbacks and negative (or stabilizing feedbacks). While stabilizing feedbacks reinforce each state, positive feedbacks are what allow two or more states to be stable. Thresholds between states arise from the interaction of these positive and negative feedbacks, and define the basins of attraction of the alternative states. These feedbacks and thresholds may operate over whole ecosystems or give rise to self-organized spatial structure. The combined effect of these feedbacks is also what gives rise to ecological resilience, which is the capacity of ecological systems to absorb environmental perturbations while maintaining their basic structure and function. -
Unifying Research on Social–Ecological Resilience and Collapse Graeme S
TREE 2271 No. of Pages 19 Review Unifying Research on Social–Ecological Resilience and Collapse Graeme S. Cumming1,* and Garry D. Peterson2 Ecosystems influence human societies, leading people to manage ecosystems Trends for human benefit. Poor environmental management can lead to reduced As social–ecological systems enter a ecological resilience and social–ecological collapse. We review research on period of rapid global change, science resilience and collapse across different systems and propose a unifying social– must predict and explain ‘unthinkable’ – ecological framework based on (i) a clear definition of system identity; (ii) the social, ecological, and social ecologi- cal collapses. use of quantitative thresholds to define collapse; (iii) relating collapse pro- cesses to system structure; and (iv) explicit comparison of alternative hypoth- Existing theories of collapse are weakly fi integrated with resilience theory and eses and models of collapse. Analysis of 17 representative cases identi ed 14 ideas about vulnerability and mechanisms, in five classes, that explain social–ecological collapse. System sustainability. structure influences the kind of collapse a system may experience. Mechanistic Mechanisms of collapse are poorly theories of collapse that unite structure and process can make fundamental understood and often heavily con- contributions to solving global environmental problems. tested. Progress in understanding col- lapse requires greater clarity on system identity and alternative causes of Sustainability Science and Collapse collapse. Ecology and human use of ecosystems meet in sustainability science, which seeks to understand the structure and function of social–ecological systems and to build a sustainable Archaeological theories have focused and equitable future [1]. Sustainability science has been built on three main streams of on a limited range of reasons for sys- tem collapse. -
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, -
OCEAN WARMING • the Ocean Absorbs Most of the Excess Heat from Greenhouse Gas Emissions, Leading to Rising Ocean Temperatures
NOVEMBER 2017 OCEAN WARMING • The ocean absorbs most of the excess heat from greenhouse gas emissions, leading to rising ocean temperatures. • Increasing ocean temperatures affect marine species and ecosystems. Rising temperatures cause coral bleaching and the loss of breeding grounds for marine fishes and mammals. • Rising ocean temperatures also affect the benefits humans derive from the ocean – threatening food security, increasing the prevalence of diseases and causing more extreme weather events and the loss of coastal protection. • Achieving the mitigation targets set by the Paris Agreement on climate change and limiting the global average temperature increase to well below 2°C above pre-industrial levels is crucial to prevent the massive, irreversible impacts of ocean warming on marine ecosystems and their services. • Establishing marine protected areas and putting in place adaptive measures, such as precautionary catch limits to prevent overfishing, can protect ocean ecosystems and shield humans from the effects of ocean warming. The distribution of excess heat in the ocean is not What is the issue? uniform, with the greatest ocean warming occurring in The ocean absorbs vast quantities of heat as a result the Southern Hemisphere and contributing to the of increased concentrations of greenhouse gases in subsurface melting of Antarctic ice shelves. the atmosphere, mainly from fossil fuel consumption. The Fifth Assessment Report published by the Intergovernmental Panel on Climate Change (IPCC) in 2013 revealed that the ocean had absorbed more than 93% of the excess heat from greenhouse gas emissions since the 1970s. This is causing ocean temperatures to rise. Data from the US National Oceanic and Atmospheric Administration (NOAA) shows that the average global sea surface temperature – the temperature of the upper few metres of the ocean – has increased by approximately 0.13°C per decade over the past 100 years. -
Accessible Professional Development for Teaching Aquatic Science Inquiry: Final Report
Accessible Professional Development for Teaching Aquatic Science Inquiry: Final Report Curriculum Research & Development Group College of Education University of Hawai‘i at Mānoa Honolulu, Hawai‘i August 2014 Accessible Professional Development for Teaching Aquatic Science Inquiry: Final Report ________________________ Edited by Kanesa Duncan Seraphin Curriculum Research & Development Group College of Education University of Hawai‘i at Mānoa Honolulu, Hawai‘i August 2014 This is the final report of a project funded by the U.S. by the Institute of Education Sciences, U.S. Department of Education, through Grant R305A100091 to the University of Hawai‘i (UH) at Mānoa Curriculum Research & Development Group (CRDG), College of Education, Kanesa Duncan Seraphin, Principal Investigator (PI), Paul R. Brandon, co-PI, Thanh Truc Nguyen, co-PI. Supplementary funding was provided by the National Oceanic and Atmospheric Administration to the University of Hawai‘i (UH) Sea Grant College Program, Kanesa Duncan Seraphin, PI, Darren Okimoto, co-PI, and Darren Learner, co- PI. Authors of this final report include members of the TSI Aquatic PD project team (Duncan Seraphin and Philippoff), the learning technology team (Nguyen), and the evaluation team (Brandon, Harrison, Vallin, and Lawton). The project team developed and provided the professional development and associated materials for the PD recipients in addition to working with the learning technology team and the evaluation team. The learning technology team developed and assessed the online learning community. The research team conducted research and evaluation activities. Chapters of this summative final report were prepared by their corresponding team members. The project itself was an inquiry-based, year-long, modularized professional development (PD) for middle and high school teachers focused on aquatic science. -
Is Ecological Succession Predictable?
Is ecological succession predictable? Commissioned by Prof. dr. P. Opdam; Kennisbasis Thema 1. Project Ecosystem Predictability, Projectnr. 232317. 2 Alterra-Report 1277 Is ecological succession predictable? Theory and applications Koen Kramer Bert Brinkman Loek Kuiters Piet Verdonschot Alterra-Report 1277 Alterra, Wageningen, 2005 ABSTRACT Koen Kramer, Bert Brinkman, Loek Kuiters, Piet Verdonschot, 2005. Is ecological succession predictable? Theory and applications. Wageningen, Alterra, Alterra-Report 1277. 80 blz.; 6 figs.; 0 tables.; 197 refs. A literature study is presented on the predictability of ecological succession. Both equilibrium and nonequilibrium theories are discussed in relation to competition between, and co-existence of species. The consequences for conservation management are outlined and a research agenda is proposed focusing on a nonequilibrium view of ecosystem functioning. Applications are presented for freshwater-; marine-; dune- and forest ecosystems. Keywords: conservation management; competition; species co-existence; disturbance; ecological succession; equilibrium; nonequilibrium ISSN 1566-7197 This report can be ordered by paying € 15,- to bank account number 36 70 54 612 by name of Alterra Wageningen, IBAN number NL 83 RABO 036 70 54 612, Swift number RABO2u nl. Please refer to Alterra-Report 1277. This amount is including tax (where applicable) and handling costs. © 2005 Alterra P.O. Box 47; 6700 AA Wageningen; The Netherlands Phone: + 31 317 474700; fax: +31 317 419000; e-mail: [email protected] No part of this publication may be reproduced or published in any form or by any means, or stored in a database or retrieval system without the written permission of Alterra. Alterra assumes no liability for any losses resulting from the use of the research results or recommendations in this report. -
Harnessing Remote Sensing Derived Sea Level Rise Models to Assess Cultural Heritage Vulnerability: a Case Study from the Northwest Atlantic Ocean
sustainability Article Harnessing Remote Sensing Derived Sea Level Rise Models to Assess Cultural Heritage Vulnerability: A Case Study from the Northwest Atlantic Ocean Meghan C. L. Howey 1,2 1 Department of Anthropology, University of New Hampshire, 73 Main Street, Durham, NH 03824, USA; [email protected] 2 Earth Systems Research Center, Institute for the Study of Earth, Oceans, and Space, University of New Hampshire, 8 College Road, Durham, NH 03824, USA Received: 20 October 2020; Accepted: 10 November 2020; Published: 12 November 2020 Abstract: Climate change threatens cultural heritage across the globe. Of its varied impacts, sea level rise is critically pressing because of the long relationship between humans and the ocean. Numerous cultural heritage sites lie on the world’s fragile coasts. Identifying cultural heritage sites at risk is an urgent need, but archaeological research programs do not always have the resources available to conduct large-scale cultural heritage vulnerability assessments. Given sea level rise poses myriad pressing issues, entities around the globe are developing sea level rise models for various management purposes (ecology, hydrology, real estate, etc.). These remote sensing-derived sea level rise models can be harnessed by archaeologists to assess cultural heritage site vulnerability. Here, such an analysis is realized for a northwest Atlantic Ocean coastal area experiencing relative sea level rise and with robust cultural heritage, including economically significant maritime heritage tourism. Combining archaeological and historic geospatial databases with LIDAR (Light Detection and Ranging)-derived relative sea level rise models illuminates coastal New Hampshire’s cultural heritage vulnerability. This is informative for risk monitoring, mitigation, and preservation planning, especially for cultural heritage tourism.