Project
ShutterstockTowards an end to subsidies that promote overfishing
Overfishing is one of the main problems for the health of our ocean. And the provision of negative subsidies to the fishing sector is one of the fundamental causes of overfishing.
Fishing subsidies are financial contributions, direct or indirect, that public entities grant to the industry.
Depending on their impacts, they can be beneficial when they promote the growth of fish stocks through conservation and fishery resource management tools. And they are considered negative or detrimental when they promote overfishing with support for, for example, increasing the catch capacity of a fishing fleet.
It is estimated that every year, governments spend approximately 22 billion dollars in negative subsidies to compensate costs for fuel, fishing gear and vessel improvements, among others.
Recent data show that, as a result of this support, 63% of fish stocks worldwide must be rebuilt and 34% are fished at "biologically unsustainable" levels.
Although negotiations on fisheries subsidies, within the framework of the World Trade Organization, officially began in 2001, it was not until the 2017 WTO Ministerial Conference that countries committed to taking action to reach an agreement.
This finally happened in June 2022, when member countries of the World Trade Organization reached, after more than two decades, a binding agreement to curb some harmful fisheries subsidies. It represents a fundamental step toward achieving the effective management of our fisheries resources, as well as toward ensuring global food security and the livelihoods of coastal communities.
The agreement reached at the 12th WTO Ministerial Conference provides for the creation of a global framework to reduce subsidies for illegal, unreported and unregulated fishing; subsidies for fishing overexploited stocks; and subsidies for vessels fishing on the unregulated high seas. It also includes measures aimed at greater transparency and accountability in the way governments support their fisheries sector.
The countries agreed to continue negotiating rules to curb other harmful subsidies, such as those that promote fishing in other countries' waters, overfishing and the overcapacity of a fleet to catch more fish than is sustainable.
If we want to have abundant and healthy fishery resources, it is time to change the way we have conceived fishing until now. We must focus our efforts on creating models of fishery use that allow for long-term conservation.
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Short-Lived Climate Pollutants: A great opportunity to put the brakes on climate change
By Florencia Ortuzar, legal advisor, AIDA While many of us are alarmed by climate change and its already tangible effects, concern becomes even greater when learning the fact that all the CO2 accumulated in the atmosphere cannot be removed, even if we were to shut down all the sources of emissions today. This reality was confirmed in the Fifth Assessment Report on the state of the climate, issued by the Intergovernmental Panel on Climate Change (IPCC). The explanation for this is simple: CO2, in contrast to other gases and pollutants, remains in the atmosphere for millennia after being released. It is stuck in the atmosphere for what is eternal for human standards, implying that its greenhouse effect does not end even with an immediate halt in emissions. The good news is that CO2 is not the only cause of global warming. There are other pollutants that, unlike CO2, only stay in the atmosphere for a relatively short time. These “other” agents are responsible for 40-45% of global warming, and they remain in the atmosphere for a minimum of a few hours to a maximum of a few decades. They are called short-lived climate pollutants, or SLCPs. Like CO2, SLCP emissions have a negative impact on humans and ecosystems. So a reduction in these pollutants would bring immediate relief to the worst affected by climate change and would bring important benefits to the environment and people. The main SLCPs Although all SLCPs contribute significantly to climate change and share the trait of being short-lived, each has its unique characteristics and emission sources. Black carbon or soot, is a particulate substance produced by the incomplete combustion of fossil fuels, mainly from motor vehicles, domestic stoves, fires and factories. The dark particles heat the atmosphere as they absorb light, and when the particles land on snow and ice they accelerate melting. Black carbon also affects human health by causing respiratory problems such as lung cancer and asthma. Tropospheric ozone is a gas formed by the reaction of the sun with other gases called "precursors," which can be man made or naturally occurring. One of these precursors is methane, another SLCP. Tropospheric ozone is associated with diseases including bronchitis, emphysema, asthma and permanent scarring of the lung tissue. Studies also show that this gas has a direct impact on vegetation, reducing crop yields and the ability of plants to absorb CO2. Methane is a powerful greenhouse gas, and 60% of its emissions come from human activities like rice farming, coal mining, landfill and oil combustion. Two important sources of methane include cattle farming, whose effect has dangerously increased with industrial meat production (Spanish), and large dams, especially those in tropical areas. Hydrofluorocarbons (HFCs) are man-made gases used in the production of air conditioners, refrigerators and aerosols. They have replaced chlorofluorocarbons (CFCs), which were banned under the Montreal Protocol. Although HFCs represent a small proportion of the greenhouse gases emitted into the atmosphere, their use is growing at an alarming speed of an average of 10-15% each year, according to a United Nations Environment Programme (UNEP) report. Everyone wins According to the IPCC, the reduction of these pollutants could avert a rise in average global temperatures by approximately 0.5 degrees Celsius by 2050, cutting the current rate of global warming in half and helping to protect some of the areas most susceptible to climate change like the Arctic, the high Himalayan regions and Tibet. The mitigation of SLCPs is also crucial for decelerating glacial melting and rising sea levels, a serious situation for the world’s population that lives in coastal areas. The reduction of SLCPs would also bring important socio-environmental benefits. Black carbon and tropospheric ozone harm human health and reduce crop yields. This in turn affects ecosystems, food security, human welfare and the entire natural cycle that keeps the planet healthy. Some talking points Given that SLCPs stem from different sources, effective mitigation requires a series of comprehensive actions that deal with each pollutant separately. Fortunately, the road is already laid out. Many of the technologies, laws and institutions needed to cut SLCP emissions already exist. In the case of black carbon, new technologies are inexpensive and available. Developed countries have already reduced emissions significantly through the use of green technologies. Ideas include the modernization of domestic cooking systems in the region, introducing the use of solar cookers and new transport systems with improved exhaust filters to reduce greenhouse gas emissions. The amount of methane in the atmosphere, which affects the level of tropospheric ozone, is largely dependent on industrial activities. To reduce emissions, effective regulations should be implemented to control the industries that emit the most methane, including intensive cattle farming, mining, hydrocarbons and large dams. For HFCs, an alternative already exists. There need to be regulations that encourage people to substitute HFCs for greener alternatives, no matter the commercial barriers. Some countries have proposed incorporating HFCs in the Montreal Protocol, an international agreement recognized as one of the most successful initiatives to significantly and rapidly reduce CFC emissions, addressing a similar challenge, to the one we face today. To find out more about SLCPs, you can read a briefing paper (Spanish) put together by AIDA, CEDHA, CEMDA and RedRacc.
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Report from COP19: Warsaw, Poland
A terrifying nightmare came true before their eyes. Waves of up to seven meters (23 feet), propelled by winds that reached 315 kilometers per hour (196 miles per hour), caught the inhabitants of the Philippines off guard, devouring everything in their path. Typhoon Haiyan was the most devastating of the climate shocks that frequently hit the Asian country. “We can stop this madness.” With those words, Yeb Saño, the Philippine’s climate change commissioner, demanded “climate justice“ for his people during the inauguration of the 19th Conference of the Parties (COP19) on climate change in Warsaw, Poland. The tragedy was palpable in his eyes and voice. The effects of climate change are unmistakable. Ocean levels and temperatures are rising, and this is provoking storms surges of such intensity that they’re impossible to ignore. No more time can be wasted in coming up with the financing needed to fight this problem. And we must set the rules for the effective use of these funds. AIDA is pushing for this. At the COP19, we worked with other civil society organizations to encourage the governments of developing countries to draft an action plan next year designed to fulfill a vital commitment: making US$100 billion available to developing countries from 2020 for fighting climate change. Part of these funds will be channeled through the Green Climate Fund (GCF). AIDA has assisted in putting pressure on the governments of developed countries to provide certainty about the contributions they will make to this financing mechanism. We also have taken part in the creation of GCF by participating at meetings of its Board of Directors. Our short-term goal is to ensure that the role of civil society is effective and meaningful in the GCF decision-making process. Long term, we want the GCF to support effective actions for climate change mitigation and adaptation that will not only help reduce emissions but also benefit the most vulnerable communities that already are being affected by the phenomenon. Our presence at the COP19 also made it possible for AIDA to form alliances with groups from different sectors – civil society, youth, indigenous peoples, among others – in order to develop and strengthen a joint position ahead of the COP20 to be held in Peru. We hope that the COP20 will set the foundation for a new and hopefully successful climate agreement at the COP21 in Paris. We also worked with partner organizations to develop a briefing paper (in Spanish) on short-lived climate pollutants (SLCPs), which we distributed in Warsaw. As SLCPs remain in the atmosphere less time than CO2, reducing these contaminants is a valuable opportunity for a short-term solution to global warming and an important element that should enter into the new climate agreement. With your support we will continue fighting to prevent typhoons and other natural disasters from becoming a way of life.
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Latin America and its little-known biodiversity
By Tania Paz, general assistant, AIDA, @TaniaNinoshka Latin America and the Caribbean stretches over more than two billion hectares, or about 15% of the earth’s total land surface area. The region possesses the richest persity of species and ecoregions in the world. It is home to one third of the world’s renewable water resources and close to 30% of the world’s total runoff, or the free flow of surface water into a drainage basin, according to the Economic Commission for Latin America and the Caribbean (ECLAC, 2002). Even so, there are still many ecosystems that we don’t know much about despite their important role in maintaining the health and wellbeing of the environment and human society. These include mangrove forests, glaciers and páramos. Mangroves According to Mexico’s National Commission for the Knowledge and Use of Biopersity (CONABIO, in Spanish), mangroves are plant formations grouped into a distinct biome known as mangal, or a tree or shrub with branches that reach down and take root in the ground. They are a unique plant species for their resistance to salt and for growing in tropical coastal environments near estuaries and coastal lagoons. They are the transition between terrestrial and marine ecosystems. Mangrove forests form a natural protective barrier that prevents wind and tide erosion. They play an important role in the environment by filtering water and allowing it to flow into underground aquifers, and they act as carbon sinks that helpmitigate the effects of climate change. The major threats to mangrove ecosystems stem from urban, industrial, tourism and agricultural development given that they compete for land with these fragile ecosystems and cause heavy pollution. This is happening in Marismas Nacionales and Laguna Huizache-Caimanero, where a mega-tourism resort is threatening a wetland ecosystem that protects Mexico’s last remaining mangrove forests and 60 endangered species. Páramos Páramos (in Spanish) are wetlands found between 2,500 and 3,600 meters above sea level in a climate of high rainfall and dry winds. Páramos are known as water factories for their capacity to generate clean water. They also act as a climate regulator with capacity to absorb carbon dioxide. Colombia is home to the largest surface area of páramo ecosystems in the world, holding 98% of páramo plant species. These ecosystems also are home to an immense persity of flora and fauna, including the spectacled bear and Andean condor, the world’s largest flying land bird. Rich in precious metals, the páramos are threatened by mining developments, both existing and planned. In Colombia, for example, miners are looking to undertake extractive activities in the Santurbán páramo, which would put in peril a vital source of fresh water for millions of Colombians. AIDA is leading a campaign (in Spanish) that calls for a proper demarcation of the Santurbán páramo’s territorial boundaries in an effort to stop mining development, an activity prohibited in officially declared páramo zones. Glaciers Glaciers are large bodies of dense ice, snow and rocks. They can stretch down or across mountainsides -- depending on their weight -- as they flow into the water system. They can melt, evaporate or break up into icebergs. In Latin America, 70% of the earth’s tropical glaciers are found high in the Andes mountain range of Bolivia, Ecuador and Peru (OLCA, 2013, in Spanish). Glaciers regulate water supplies by releasing water in the form of meltwater in the hot and dry seasons and by storing it as ice during cold and wet periods. In Ecuador, the city of Quito gets 50% of its water from glacier reservoirs and likewise Bolivia’s La Paz gets 30% from glacier catchment areas. Glacier melt, caused by the effects of climate change, is the greatest threat to the glaciers. Since 1970 the Andean glaciers have lost 20% of their volume, according to a report by Peru’s National Meteorology and Hydrology Service (SENAMHI, in Spanish). See the documentary La Era del Deshielo (The Age of the Thawing) by Señal Colombia. Source: YouTube Glacier melt is putting the water production of Andean countries at risk. In Peru, for example, the volume of surface ice that has been lost as a consequence of melting equates to seven billion cubic meters of water, a quantity that represents around 10 years worth of water supplies for the city of Lima. If all the world’s glaciers melted, sea levels could rise by some 66 meters, causing catastrophic impacts on coastal cities (OLCA, 2013, in Spanish). Como vemos, América Latina es una región totalmente rica en biopersidad que juega un papel importante en el mundo y en la continuidad de la especie humana. La belleza y riqueza del continente quedan expresadas en la letra de América, canción de Nino Bravo: “Cuando Dios hizo el Edén, pensó en América”. ¡Defendamos y preservemos nuestro Edén!
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