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Dive into the research topics where Ussif Rashid Sumaila is active.

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Featured researches published by Ussif Rashid Sumaila.


Science | 2015

Contrasting futures for ocean and society from different anthropogenic CO2 emissions scenarios

J.-P. Gattuso; Alexandre Magnan; R. Bille; William Wai Lung Cheung; Ella L. Howes; Fortunat Joos; D. Allemand; L. Bopp; S. R. Cooley; C. M. Eakin; Ove Hoegh-Guldberg; R. P. Kelly; Hans-Otto Pörtner; A. D. Rogers; J. M. Baxter; D. Laffoley; D. Osborn; A. Rankovic; J. Rochette; Ussif Rashid Sumaila; S. Treyer; Cm Turley

Carbon emissions and their ocean impacts Anthropogenic CO2 emissions directly affect atmospheric chemistry but also have a strong influence on the oceans. Gattuso et al. review how the physics, chemistry, and ecology of the oceans might be affected based on two CO2 emission trajectories: one business as usual and one with aggressive reductions. Ocean warming, acidification, sea-level rise, and the expansion of oxygen minimum zones will continue to have distinct impacts on marine communities and ecosystems. The path that humanity takes regarding CO2 emissions will largely determine the severity of these phenomena. Science, this issue 10.1126/science.aac4722 The amount and pace of our carbon dioxide emissions will determine how the oceans respond. BACKGROUND Although the ocean moderates anthropogenic climate change, this has great impacts on its fundamental physics and chemistry, with important consequences for ecosystems and people. Yet, despite the ocean’s critical role in regulating climate—and providing food security and livelihoods for millions of people—international climate negotiations have only minimally considered impacts on the ocean. Here, we evaluate changes to the ocean and its ecosystems, as well as to the goods and services they provide, under two contrasting CO2 scenarios: the current high-emissions trajectory (Representative Concentration Pathway 8.5, RCP8.5) and a stringent emissions scenario (RCP2.6) consistent with the Copenhagen Accord of keeping mean global temperature increase below 2°C in the 21st century. To do this, we draw on the consensus science in the latest assessment report of the Intergovernmental Panel on Climate Change and papers published since the assessment. ADVANCES Warming and acidification of surface ocean waters will increase proportionately with cumulative CO2 emissions (see figure). Warm-water corals have already been affected, as have mid-latitude seagrass, high-latitude pteropods and krill, mid-latitude bivalves, and fin fishes. Even under the stringent emissions scenario (RCP2.6), warm-water corals and mid-latitude bivalves will be at high risk by 2100. Under our current rate of emissions, most marine organisms evaluated will have very high risk of impacts by 2100 and many by 2050. These results—derived from experiments, field observations, and modeling—are consistent with evidence from high-CO2 periods in the paleorecord. Impacts to the ocean’s ecosystem services follow a parallel trajectory. Services such as coastal protection and capture fisheries are already affected by ocean warming and acidification. The risks of impacts to these services increase with continued emissions: They are predicted to remain moderate for the next 85 years for most services under stringent emission reductions, but the business-as-usual scenario (RCP8.5) would put all ecosystem services we considered at high or very high risk over the same time frame. These impacts will be cumulative or synergistic with other human impacts, such as overexploitation of living resources, habitat destruction, and pollution. Fin fisheries at low latitudes, which are a key source of protein and income for millions of people, will be at high risk. OUTLOOK Four key messages emerge. First, the ocean strongly influences the climate system and provides important services to humans. Second, impacts on key marine and coastal organisms, ecosystems, and services are already detectable, and several will face high risk of impacts well before 2100, even under the low-emissions scenario (RCP2.6). These impacts will occur across all latitudes, making this a global concern beyond the north/south divide. Third, immediate and substantial reduction of CO2 emissions is required to prevent the massive and mostly irreversible impacts on ocean ecosystems and their services that are projected with emissions greater than those in RCP2.6. Limiting emissions to this level is necessary to meet stated objectives of the United Nations Framework Convention on Climate Change; a substantially different ocean would result from any less-stringent emissions scenario. Fourth, as atmospheric CO2 increases, protection, adaptation, and repair options for the ocean become fewer and less effective. The ocean provides compelling arguments for rapid reductions in CO2 emissions and eventually atmospheric CO2 drawdown. Hence, any new global climate agreement that does not minimize the impacts on the ocean will be inadequate. Changes in ocean physics and chemistry and impacts on organisms and ecosystem services according to stringent (RCP2.6) and high business-as-usual (RCP8.5) CO2 emissions scenarios. Changes in temperature (∆T) and pH (∆pH) in 2090 to 2099 are relative to preindustrial (1870 to 1899). Sea level rise (SLR) in 2100 is relative to 1901. RCP2.6 is much more favorable to the ocean, although important ecosystems, goods, and services remain vulnerable, and allows more-efficient management options. l, m, h: low, mid-, and high latitudes, respectively. The ocean moderates anthropogenic climate change at the cost of profound alterations of its physics, chemistry, ecology, and services. Here, we evaluate and compare the risks of impacts on marine and coastal ecosystems—and the goods and services they provide—for growing cumulative carbon emissions under two contrasting emissions scenarios. The current emissions trajectory would rapidly and significantly alter many ecosystems and the associated services on which humans heavily depend. A reduced emissions scenario—consistent with the Copenhagen Accord’s goal of a global temperature increase of less than 2°C—is much more favorable to the ocean but still substantially alters important marine ecosystems and associated goods and services. The management options to address ocean impacts narrow as the ocean warms and acidifies. Consequently, any new climate regime that fails to minimize ocean impacts would be incomplete and inadequate.


The Journal of Environment & Development | 2004

Western Africa: A Fish Basket of Europe Past and Present

Jacqueline Alder; Ussif Rashid Sumaila

This article shows that despite increasing catches by foreign fishing fleets, the economic growth and social benefits from marine resources have not been met for many western African countries that host these fleets. A meta-analysis of changes in catches, market values, exports, imports, employment, access, and domestic supplies in western Africa since 1960 illustrates the impact of the expansion of distant-water fleets on not only the status of the marine resources and their ecosystems but also on the economic and social conditions of the people of western Africa. Finally, recommendations are made on appropriate management options for foreign fishing fleets and the key initiatives that could be considered by regional fish bodies and governments in western Africa.


Nature | 2016

Bright spots among the world’s coral reefs

Joshua E. Cinner; Cindy Huchery; M.A. MacNeil; Nicholas A. J. Graham; Tim R. McClanahan; Joseph Maina; Eva Maire; John N. Kittinger; Christina C. Hicks; Camilo Mora; Edward H. Allison; Stéphanie D'agata; Andrew S. Hoey; David A. Feary; Larry B. Crowder; Ivor D. Williams; Michel Kulbicki; Laurent Vigliola; Laurent Wantiez; Graham J. Edgar; Rick D. Stuart-Smith; Stuart A. Sandin; Alison Green; Marah J. Hardt; Maria Beger; Alan M. Friedlander; Stuart J. Campbell; K. E. Holmes; Shaun K. Wilson; Eran Brokovich

Ongoing declines in the structure and function of the world’s coral reefs require novel approaches to sustain these ecosystems and the millions of people who depend on them. A presently unexplored approach that draws on theory and practice in human health and rural development is to systematically identify and learn from the ‘outliers’—places where ecosystems are substantially better (‘bright spots’) or worse (‘dark spots’) than expected, given the environmental conditions and socioeconomic drivers they are exposed to. Here we compile data from more than 2,500 reefs worldwide and develop a Bayesian hierarchical model to generate expectations of how standing stocks of reef fish biomass are related to 18 socioeconomic drivers and environmental conditions. We identify 15 bright spots and 35 dark spots among our global survey of coral reefs, defined as sites that have biomass levels more than two standard deviations from expectations. Importantly, bright spots are not simply comprised of remote areas with low fishing pressure; they include localities where human populations and use of ecosystem resources is high, potentially providing insights into how communities have successfully confronted strong drivers of change. Conversely, dark spots are not necessarily the sites with the lowest absolute biomass and even include some remote, uninhabited locations often considered near pristine. We surveyed local experts about social, institutional, and environmental conditions at these sites to reveal that bright spots are characterized by strong sociocultural institutions such as customary taboos and marine tenure, high levels of local engagement in management, high dependence on marine resources, and beneficial environmental conditions such as deep-water refuges. Alternatively, dark spots are characterized by intensive capture and storage technology and a recent history of environmental shocks. Our results suggest that investments in strengthening fisheries governance, particularly aspects such as participation and property rights, could facilitate innovative conservation actions that help communities defy expectations of global reef degradation.


Canadian Medical Association Journal | 2009

Are dietary recommendations for the use of fish oils sustainable

David J.A. Jenkins; John L. Sievenpiper; Daniel Pauly; Ussif Rashid Sumaila; Cyril W.C. Kendall; Farley M. Mowat

People in developed countries have been encouraged in recent years to increase their intakes of fatty fish by at least 2–3-fold. The goal is to consume adequate amounts of the long-chain polyunsaturated omega-3 fatty acids, eicosapentaenoic acid (EPA) and docosahexaenoic acid (DHA) for optimal


PLOS ONE | 2012

Benefits of rebuilding global marine fisheries outweigh costs.

Ussif Rashid Sumaila; William W. L. Cheung; Andrew Dyck; Kamal Gueye; Ling Huang; Vicky W. Y. Lam; Daniel Pauly; Thara Srinivasan; Wilf Swartz; Reginald Watson; Dirk Zeller

Global marine fisheries are currently underperforming, largely due to overfishing. An analysis of global databases finds that resource rent net of subsidies from rebuilt world fisheries could increase from the current negative US


Marine Policy | 1999

A review of game-theoretic models of fishing

Ussif Rashid Sumaila

13 billion to positive US


Fisheries Research | 1997

Bioeconomics and catchability: fish and fishers behaviour during stock collapse

Steven Mackinson; Ussif Rashid Sumaila; Tony J. Pitcher

54 billion per year, resulting in a net gain of US


Fisheries Research | 2007

The World Trade Organization and global fisheries sustainability

Ussif Rashid Sumaila; Ahmed Khan; Reg Watson; Gordon R. Munro; Dirk Zeller; Nancy Baron; Daniel Pauly

600 to US


Environmental and Resource Economics | 1997

Cooperative and Non-Cooperative Exploitation of the Arcto-Norwegian Cod Stock

Ussif Rashid Sumaila

1,400 billion in present value over fifty years after rebuilding. To realize this gain, governments need to implement a rebuilding program at a cost of about US


Fisheries | 2011

Potential Impact of the Deepwater Horizon Oil Spill on Commercial Fisheries in the Gulf of Mexico

Ashley McCrea-Strub; Kristin M. Kleisner; Ussif Rashid Sumaila; Wilf Swartz; Reg Watson; Dirk Zeller; Daniel Pauly

203 (US

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Daniel Pauly

University of British Columbia

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Reg Watson

University of Tasmania

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Dirk Zeller

University of British Columbia

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Tony J. Pitcher

Departamento de Oceanografia e Pescas

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William W. L. Cheung

University of British Columbia

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Gordon R. Munro

University of British Columbia

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Louise Teh

University of British Columbia

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Jackie Alder

University of British Columbia

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Vicky W. Y. Lam

University of British Columbia

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