Ocean Acidification
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Drought and Ecosystem Carbon Cycling
Agricultural and Forest Meteorology 151 (2011) 765–773 Contents lists available at ScienceDirect Agricultural and Forest Meteorology journal homepage: www.elsevier.com/locate/agrformet Review Drought and ecosystem carbon cycling M.K. van der Molen a,b,∗, A.J. Dolman a, P. Ciais c, T. Eglin c, N. Gobron d, B.E. Law e, P. Meir f, W. Peters b, O.L. Phillips g, M. Reichstein h, T. Chen a, S.C. Dekker i, M. Doubková j, M.A. Friedl k, M. Jung h, B.J.J.M. van den Hurk l, R.A.M. de Jeu a, B. Kruijt m, T. Ohta n, K.T. Rebel i, S. Plummer o, S.I. Seneviratne p, S. Sitch g, A.J. Teuling p,r, G.R. van der Werf a, G. Wang a a Department of Hydrology and Geo-Environmental Sciences, Faculty of Earth and Life Sciences, VU-University Amsterdam, De Boelelaan 1085, 1081 HV Amsterdam, The Netherlands b Meteorology and Air Quality Group, Wageningen University and Research Centre, P.O. box 47, 6700 AA Wageningen, The Netherlands c LSCE CEA-CNRS-UVSQ, Orme des Merisiers, F-91191 Gif-sur-Yvette, France d Institute for Environment and Sustainability, EC Joint Research Centre, TP 272, 2749 via E. Fermi, I-21027 Ispra, VA, Italy e College of Forestry, Oregon State University, Corvallis, OR 97331-5752 USA f School of Geosciences, University of Edinburgh, EH8 9XP Edinburgh, UK g School of Geography, University of Leeds, Leeds LS2 9JT, UK h Max Planck Institute for Biogeochemistry, PO Box 100164, D-07701 Jena, Germany i Department of Environmental Sciences, Copernicus Institute of Sustainable Development, Utrecht University, PO Box 80115, 3508 TC Utrecht, The Netherlands j Institute of Photogrammetry and Remote Sensing, Vienna University of Technology, Gusshausstraße 27-29, 1040 Vienna, Austria k Geography and Environment, Boston University, 675 Commonwealth Avenue, Boston, MA 02215, USA l Department of Global Climate, Royal Netherlands Meteorological Institute, P.O. -
Slow-Onset Processes and Resulting Loss and Damage
Publication Series ADDRESSING LOSS AND DAMAGE FROM SLOW-ONSET PROCESSES Slow-onset Processes and Resulting Loss and Damage – An introduction Table of contents L 4 22 ist of a bbre Summary of Loss and damage via tio key facts and due to slow-onset ns definitions processes AR4 IPCC Fourth Assessment Report 6 22 What is loss and damage? Introduction AR5 IPCC Fifth Assessment Report COP Conference of the Parties to the 23 United Nations Framework Convention on 9 What losses and damages IMPRINT Climate Change can result from slow-onset Slow-onset ENDA Environment Development Action Energy, processes? Authors Environment and Development Programme processes and their Laura Schäfer, Pia Jorks, Emmanuel Seck, Energy key characteristics 26 Oumou Koulibaly, Aliou Diouf ESL Extreme Sea Level What losses and damages Contributors GDP Gross Domestic Product 9 can result from sea level rise? Idy Niang, Bounama Dieye, Omar Sow, Vera GMSL Global mean sea level What is a slow-onset process? Künzel, Rixa Schwarz, Erin Roberts, Roxana 31 Baldrich, Nathalie Koffi Nguessan GMSLR Global mean sea level rise 10 IOM International Organization on Migration What are key characteristics Loss and damage Editing Adam Goulston – Scize Group LLC of slow-onset processes? in Senegal due to IPCC Intergovernmental Panel on Climate Change sea level rise Layout and graphics LECZ Low-elevation coastal zone 14 Karin Roth – Wissen in Worten OCHA Office for the Coordination of Humanitarian Affairs What are other relevant January 2021 terms for the terminology on 35 RCP Representative -
Forestry As a Natural Climate Solution: the Positive Outcomes of Negative Carbon Emissions
PNW Pacific Northwest Research Station INSIDE Tracking Carbon Through Forests and Streams . 2 Mapping Carbon in Soil. .3 Alaska Land Carbon Project . .4 What’s Next in Carbon Cycle Research . 4 FINDINGS issue two hundred twenty-five / march 2020 “Science affects the way we think together.” Lewis Thomas Forestry as a Natural Climate Solution: The Positive Outcomes of Negative Carbon Emissions IN SUMMARY Forests are considered a natural solu- tion for mitigating climate change David D’A more because they absorb and store atmos- pheric carbon. With Alaska boasting 129 million acres of forest, this state can play a crucial role as a carbon sink for the United States. Until recently, the vol- ume of carbon stored in Alaska’s forests was unknown, as was their future car- bon sequestration capacity. In 2007, Congress passed the Energy Independence and Security Act that directed the Department of the Inte- rior to assess the stock and flow of carbon in all the lands and waters of the United States. In 2012, a team com- posed of researchers with the U.S. Geological Survey, U.S. Forest Ser- vice, and the University of Alaska assessed how much carbon Alaska’s An unthinned, even-aged stand in southeast Alaska. New research on carbon sequestration in the region’s coastal temperate rainforests, and how this may change over the next 80 years, is helping land managers forests can sequester. evaluate tradeoffs among management options. The researchers concluded that ecosys- tems of Alaska could be a substantial “Stones have been known to move sunlight, water, and atmospheric carbon diox- carbon sink. -
Carbon Cycling and Biosequestration Integrating Biology and Climate Through Systems Science March 2008 Workshop Report
Carbon Cycling and Biosequestration Integrating Biology and Climate through Systems Science March 2008 Workshop Report http://genomicsgtl.energy.gov/carboncycle/ ne of the most daunting challenges facing science in processes that drive the global carbon cycle, (2) achieve greater the 21st Century is to predict how Earth’s ecosystems integration of experimental biology and biogeochemical mod- will respond to global climate change. The global eling approaches, (3) assess the viability of potential carbon Ocarbon cycle plays a central role in regulating atmospheric biosequestration strategies, and (4) develop novel experimental carbon dioxide (CO2) levels and thus Earth’s climate, but our approaches to validate climate model predictions. basic understanding of the myriad tightly interlinked biologi- cal processes that drive the global carbon cycle remains lim- A Science Strategy for the Future ited. Whether terrestrial and ocean ecosystems will capture, Understanding and predicting processes of the global carbon store, or release carbon is highly dependent on how changing cycle will require bold new research approaches aimed at linking climate conditions affect processes performed by the organ- global-scale climate phenomena; biogeochemical processes of isms that form Earth’s biosphere. Advancing our knowledge ecosystems; and functional activities encoded in the genomes of of biological components of the global carbon cycle is crucial microbes, plants, and biological communities. This goal presents to predicting potential climate change impacts, assessing the a formidable challenge, but emerging systems biology research viability of climate change adaptation and mitigation strate- approaches provide new opportunities to bridge the knowledge gies, and informing relevant policy decisions. gap between molecular- and global-scale phenomena. -
The Carbon Cycle
The Carbon Cycle Overview of the Carbon Cycle The movement of carbon from one area to another is the basis for the carbon cycle. Carbon is important for all life on Earth. All living things are made up of carbon. Carbon is produced by both natural and human-made (anthropogenic) sources. Carbon Cycle Page 1 Nature’s Carbon Sources Carbon is found in the Carbon is found in the lithosphere Carbon is found in the Carbon is found in the atmosphere mostly as carbon in the form of carbonate rocks. biosphere stored in plants and hydrosphere dissolved in ocean dioxide. Animal and plant Carbonate rocks came from trees. Plants use carbon dioxide water and lakes. respiration place carbon into ancient marine plankton that sunk from the atmosphere to make the atmosphere. When you to the bottom of the ocean the building blocks of food Carbon is used by many exhale, you are placing carbon hundreds of millions of years ago during photosynthesis. organisms to produce shells. dioxide into the atmosphere. that were then exposed to heat Marine plants use cabon for and pressure. photosynthesis. The organic matter that is produced Carbon is also found in fossil fuels, becomes food in the aquatic such as petroleum (crude oil), coal, ecosystem. and natural gas. Carbon is also found in soil from dead and decaying animals and animal waste. Carbon Cycle Page 2 Natural Carbon Releases into the Atmosphere Carbon is released into the atmosphere from both natural and man-made causes. Here are examples to how nature places carbon into the atmosphere. -
Ocean Acidification in Washington State
University of Washington • Washington Sea Grant Ocean Acidification in Washington State What is Ocean Acidification? OA in Washington State cean Acidification (or ‘OA’) is a long-term decrease ur region is experiencing ocean acidification sooner Oin seawater pH that is primarily caused by the Oand more severely than expected, due to a combina- ocean’s uptake of carbon dioxide (CO2 ) from the atmo- tion of human and natural causes. In the spring and sum- sphere. CO2 generated by humans’ use of fossil fuels and mer, acidification along our coast is compounded by up- deforestation has been accumulating in the atmosphere welling, which mixes deep, naturally low-pH seawater into since the industrial revolution. About one quarter of this the already acidified surface layer. In Puget Sound, nutri- CO2 is absorbed by the oceans, pH describes the acidity of a liquid ents generated by human activities (mostly where it reacts with water to form nitrogen and phosphorus from sewage, carbonic acid. As a result, the aver- fertilizers and manure) fuel processes that age pH of seawater at the ocean add even more CO2 to this ‘doubly-acidified’ surface has already dropped by ~0.1 seawater. The combination can be deadly units, a 30% increase in acidity. If to vulnerable organisms. pH levels as low atmospheric CO2 levels continue as 7.4 have been recorded in Hood Canal, to climb at the present rate, ocean an important shellfish-growing region. acidity will double by the end of this State and federal agencies, scientists, tribes, century. shellfish growers and NGOs are working together to address OA in our region. -
Ocean Acidification Due to Increasing Atmospheric Carbon Dioxide
Ocean acidification due to increasing atmospheric carbon dioxide Policy document 12/05 June 2005 ISBN 0 85403 617 2 This report can be found at www.royalsoc.ac.uk ISBN 0 85403 617 2 © The Royal Society 2005 Requests to reproduce all or part of this document should be submitted to: Science Policy Section The Royal Society 6-9 Carlton House Terrace London SW1Y 5AG email [email protected] Copy edited and typeset by The Clyvedon Press Ltd, Cardiff, UK ii | June 2005 | The Royal Society Ocean acidification due to increasing atmospheric carbon dioxide Ocean acidification due to increasing atmospheric carbon dioxide Contents Page Summary vi 1 Introduction 1 1.1 Background to the report 1 1.2 The oceans and carbon dioxide: acidification 1 1.3 Acidification and the surface oceans 2 1.4 Ocean life and acidification 2 1.5 Interaction with the Earth systems 2 1.6 Adaptation to and mitigation of ocean acidification 2 1.7 Artificial deep ocean storage of carbon dioxide 3 1.8 Conduct of the study 3 2 Effects of atmospheric CO2 enhancement on ocean chemistry 5 2.1 Introduction 5 2.2 The impact of increasing CO2 on the chemistry of ocean waters 5 2.2.1 The oceans and the carbon cycle 5 2.2.2 The oceans and carbon dioxide 6 2.2.3 The oceans as a carbonate buffer 6 2.3 Natural variation in pH of the oceans 6 2.4 Factors affecting CO2 uptake by the oceans 7 2.5 How oceans have responded to changes in atmospheric CO2 in the past 7 2.6 Change in ocean chemistry due to increases in atmospheric CO2 from human activities 9 2.6.1 Change to the oceans -
Permafrost Soils and Carbon Cycling
SOIL, 1, 147–171, 2015 www.soil-journal.net/1/147/2015/ doi:10.5194/soil-1-147-2015 SOIL © Author(s) 2015. CC Attribution 3.0 License. Permafrost soils and carbon cycling C. L. Ping1, J. D. Jastrow2, M. T. Jorgenson3, G. J. Michaelson1, and Y. L. Shur4 1Agricultural and Forestry Experiment Station, Palmer Research Center, University of Alaska Fairbanks, 1509 South Georgeson Road, Palmer, AK 99645, USA 2Biosciences Division, Argonne National Laboratory, Argonne, IL 60439, USA 3Alaska Ecoscience, Fairbanks, AK 99775, USA 4Department of Civil and Environmental Engineering, University of Alaska Fairbanks, Fairbanks, AK 99775, USA Correspondence to: C. L. Ping ([email protected]) Received: 4 October 2014 – Published in SOIL Discuss.: 30 October 2014 Revised: – – Accepted: 24 December 2014 – Published: 5 February 2015 Abstract. Knowledge of soils in the permafrost region has advanced immensely in recent decades, despite the remoteness and inaccessibility of most of the region and the sampling limitations posed by the severe environ- ment. These efforts significantly increased estimates of the amount of organic carbon stored in permafrost-region soils and improved understanding of how pedogenic processes unique to permafrost environments built enor- mous organic carbon stocks during the Quaternary. This knowledge has also called attention to the importance of permafrost-affected soils to the global carbon cycle and the potential vulnerability of the region’s soil or- ganic carbon (SOC) stocks to changing climatic conditions. In this review, we briefly introduce the permafrost characteristics, ice structures, and cryopedogenic processes that shape the development of permafrost-affected soils, and discuss their effects on soil structures and on organic matter distributions within the soil profile. -
9. AM Ecocide
Amendments to draft resolution On the crime of Ecocide № Party Line Action Current Text Proposed Amendment Explanation 1 Bündnis 90/ 1 replace On an international recognition of the Tackle environmental destruction: Die Grünen crime of ecocide: 2 Bündnis 90/ 25 replace that global warming must be limited to agreed to holding the increase in the global Die Grünen 1,5°C. average temperature to well below 2°C above pre-industrial levels and pursuing efforts to limit the temperature increase to 1.5°C above pre-industrial levels, recognising that this would significantly reduce the risks and impacts of climate change. Amendments on Draft Resolution on an international recognition of the crime of ecocide European Green Party - 5th Congress, Liverpool, UK, 30 March-2 April 2017 1 № Party Line Action Current Text Proposed Amendment Explanation 3 Vihreät - De 30-36 delete According to environmental scientists Not necessary for making the point, Gröna Johan Rockström (Stockholm Resilience the chapter draws the attention Centre) and Will Steffen (Australian away from the point of the National University), these are two among resolution making it unnecessarily four “planetary boundaries” that have long. 4 Strana 30-36 replace already been exceeded. These “planetary These present two out of nine “planetary The original text presents the zelenych boundaries” involve nine thresholds on boundaries”, or nine thresholds on core concept of "planetary boundaries" (Czech core environmental issues (greenhouse gas environmental issues, beyond which human only as an opinion of Rockstrom Greens) amount in atmosphere, biodiversity, but existence would be threatened. The concept and Steffen and, moreover, it does also ocean acidification, land use for crop, has been introduced by a group of not state any source, that this consumption of freshwater...) beyond international scientists, led by Johan opinion is based on. -
Ocean Acidification and the Permo- Triassic Mass Extinction: Process and Manifestation
Goldschmidt2015 Abstracts Ocean acidification and the permo- Triassic mass extinction: Process and manifestation S. A. KASEMANN1, R. WOOD2*, M. O. CLARKSON3, T. M. LENTON4, S. J. DAINES4, S. RICHOZ5, F. OHNEMUELLER1, A. MEIXNER1, S. W. POULTON6 AND E. T. TIPPER7 1Department of Geosciences & MARUM-Center for Marine Environmental Sciences, Univ. of Bremen, Germany 2School of GeoSciences, University of Edinburgh, UK (*[email protected]) 3Department of Chemistry, Univ. of Otago, New Zealand 4College of Life and Environmental Sciences, Univ. of Exeter 5Institute of Earth Sciences, University of Graz, Austria 6School of Earth and Environment, University of Leeds, UK 7Dept. of Earth Sciences, University of Cambridge, UK Ocean acidification triggered by Siberian Trap volcanism was a possible kill mechanism for the Permian-Triassic Boundary (PTB) mass extinction, but direct evidence for an acidification event is lacking. We present a high resolution seawater pH record across this interval, utilizing boron isotope data (δ11B) combined with petrographic analysis and a quantitative modeling approach. Through this integration we are able to produce an envelope that encompasses the most realistic range in pH, which then allows us to resolve three distinct chronological phases of carbon cycle perturbation, each with very different environmental consequences for the Late Permian-Early Triassic Earth system. In the latest Permian, increased ocean alkalinity, primed the Earth system with a low level of atmospheric CO2 and a high ocean buffering capacity. The first phase of extinction was coincident with a slow injection of carbon into the atmosphere and ocean pH remained stable. During the second extinction pulse, however, a rapid and large injection of carbon caused an abrupt acidification event that drove the preferential loss of heavily calcified marine biota. -
Ocean Acidification During the Early Toarcian
https://doi.org/10.1130/G47781.1 Manuscript received 20 April 2020 Revised manuscript received 29 June 2020 Manuscript accepted 6 July 2020 © 2020 The Authors. Gold Open Access: This paper is published under the terms of the CC-BY license. Published online 13 August 2020 Ocean acidification during the early Toarcian extinction event: Evidence from boron isotopes in brachiopods Tamás Müller1*, Hana Jurikova2,3, Marcus Gutjahr2, Adam Tomašových1, Jan Schlögl4, Volker Liebetrau2, Luís v. Duarte5, Rastislav Milovský1, Guillaume Suan6, Emanuela Mattioli6,7, Bernard Pittet6 and Anton Eisenhauer2 1 Earth Science Institute, Slovak Academy of Sciences, Dˇ umbierska 1, 974 01 Banská Bystrica, Slovakia 2 GEOMAR Helmholtz-Zentrum für Ozeanforschung Kiel, Wischhofstr. 1-3, 24148 Kiel, Germany 3 GFZ Deutsches GeoForschungsZentrum–Helmholtz-Zentrum Potsdam, Telegrafenberg, 14473 Potsdam, Germany 4 Department of Geology and Paleontology, Faculty of Natural Sciences, Comenius University in Bratislava, Mlynská dolina, Ilkovicˇova 6, SK-842 15 Bratislava, Slovakia 5 University of Coimbra, MARE–Marine and Environmental Sciences Centre–Department of Earth Sciences, Polo II, Rua Sílvio Lima, 3030-790 Coimbra, Portugal 6 Univ Lyon, Univ Lyon 1, ENSL, CNRS, LGL-TPE, F-69622, Villeurbanne, France 7 Institut Universitaire de France (IUF), 75231 Paris Cedex 05, France ABSTRACT methane, have also been postulated (Hesselbo The loss of carbonate production during the Toarcian Oceanic Anoxic Event (T-OAE, ca. et al., 2000; Them et al., 2017). 183 Ma) is hypothesized to have been at least partly triggered by ocean acidification linked The changes in the carbon cycle are globally to magmatism from the Karoo-Ferrar large igneous province (southern Africa and Antarc- expressed as a short negative shift in the car- tica). -
Ocean Acidification and Climate Change: Synergies and Challenges
n synthesis 5 Ocean acidification and climate change: synergies and challenges of addressing both under the UNFCCC ELLYCIA R. HARROULD-KOLIEB1, DOROTHE´E HERR2* 1 10 School of Land and Environment, University of Melbourne, Melbourne, VIC 3010, Australia 2 Global Marine and Polar Programme, International Union for Conservation of Nature (IUCN), Suite 300, 1630 Connecticut Avenue NW, Washington, DC 20001, USA 15 Ocean acidification and climate change are linked by their common driver: CO2. Climate change is the consequence of a range of GHG emissions, but ocean acidification on a global scale is caused solely by increased concentrations of atmospheric CO2. Reducing CO2 emissions is therefore the most effective way to mitigate ocean acidification. Acting to prevent further ocean acidification by reducing CO2 emissions will also provide simultaneous benefits by alleviating future climate change. Although it is possible that reducing CO2 emissions to a level low enough to address ocean acidification will simultaneously address climate change, the reverse is unfortunately not necessarily true. Despite the ocean’s integral role in the climate system and the 20 potentially wide-ranging impacts on marine life and humans, the problem of ocean acidification is largely absent from most policy discussions pertaining to CO2 emissions. The linkages between ocean acidification, climate change and the United Nations Framework Convention on Climate Change (UNFCCC) are identified and possible scenarios for developing common solutions to reduce and adapt to ocean acidification and climate change are offered. Areas where the UNFCCC is currently lacking capacity to effectively tackle rising ocean acidity are also highlighted. 25 Keywords: climate change; climate policy; ocean acidification; oceans; UNFCCC L’acidification des oce´ans et le changement climatique sont lie´s par leur cause commune : le CO2.