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1. How does climate change affect world fisheries? give 5 examples

1. How does climate change affect world fisheries? give 5 examples

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2.1. Overview of the Impact of Climate Change on Fisheries Natural climatic fluctuations, particularly those at medium (decadsuch as the Nile and Zambezi Rivers; and coastal habitats including estuaries, mangrove swamps, and deltas (Hlohowskyjl et a, 1996). The diversity of the habitats and the species they support respond differently to different impacts of climate change. Even though it is not possible to generalize the impacts of climate change on fisheries in SSA, they share something in common climate change is very likely going to lead to fluctuations in fish stocks. Fluctuations in fish stocks will have major economic consequences for many vulnerable communities and national economies that heavily depend on fisheries (Brander, 2010). The impacts of climate change on fish stocks in SSA can be classified as physical and biological changes. Physical changes include sea surface temperature rise, sea level rise, changes in salinity and ocean acidification. Biological changes include changes in primary production, and fish stock distribution. These factors when combined together will have adverse impacts on the already strained resource. 2.1.1. Physcal Changes 2.1.1.1. Water Surface Temperature Rise The oceans play a significant role in regulating global climate. Their heat capacity (and thus net heat uptake) is about 1000 times larger than that of the atmosphere (Barange and Perry, 2010) and they therefore absorb significant amount of heat emitted globally. Such changes in ocean temperatures can change the dynamics of aquatic environments of the region. Changes in ocean dynamics could lead to changes in migration patterns of fish and possibly reduce fish landings, especially in coastal fisheries (African Action, 2007) For example, increased ocean temperature may affect upwelling along the Gulf of Guinea, which can make the ocean waters become unsuitable for fisheries, causing a reduction in and possible collapse of fishing activities (African Action, 2007 in Urama and Ozor, 2010). Inland waters are also equally vulnerable and could be impacted strongly by climate change (IPCC, 2007). The international Dialogue on Water and Climate (2004) noted that water stress will increase significantly in those regions that are already relatively dry such as SSA. One of the stresses that inland waters of SSA are facing is increasing water surface temperature According to Christensen et al. (2007 in Barange and Perry, 2010) warming in Africa is very likely going to be larger than the global annual mean warming throughout the region and in all seasons, with drier subtropical regions warming more than the wetter tropics with a consequent decline in rainfall. Rising water temperature also threatens biodiversity. Generally, fish have a thermal preference that optimizes physiological processes (Abowei, 2010). If water temperature rises above the maximum tolerable threshold of a species, then its existence is thrcatened. Urama and Ozor (2010) provide an example from the Lebialem Highlands in Cameroon where women have started to hunt for tadpoles and frogs because there are no fish in most of Bangwa Rivers.However, even the number of tadpoles and frogs have significantly declined (partly) due to the warming rivers that have increased the amount of predator fish in an area they have never inhabited before2.1.1.2. Sea Level Rise Globally, sea level has already risen by 10 to 20 cm during the 20th century, largely duc to thermal expansion, and by 2100 a global rise in sea level of between 9 cm and 88 cm has been predicted, based on the Intergovernmental Panel on Climate Changes full range of 35 climate projection scenarios (Church et al., 2001 in OECD, 2010). In coastal areas, sea level rise may alter the salinity of estuarine habitats, inundate wetlands, and reduce or eliminate the abundance of submerged vegetation, adversely affecting those species which rely on these coastal habitats for reproduction and recruitment (Hlohowskyjl e a, 1996). In addition, with high sea levels, sea ports, existing fishing facilities like jetties and fish storage centers built on the coastal fringes slightly above the mean high tide line l be subjected to more frequent tidal and storm inundation (Ibe and Awosika, 1991). Therefore, sea level rise is very likely going to have a negative impact on fishery production (due to salt stresses on the fish stock and its habitat) and fish landing, processing and marketing facilities. There are very limited studies done to assess the impacts of sea level rise in the coastal zones of SSA. There is, however, some information on the impact of sea level rise in some of the most populous coastal cities in West and East Africa. For example, Nigerias 800 kilometer low-lying coastline from Lagos to Calabar makes the region prone to seawater intrusion into coastal freshwater resources. This will have a negative impact on inland fisheries and aquaculture. The people in the coastal areas who used to depend on fishing have seen their livelihoods destroyed by the rising waters (Urama and Ozor, 2010). In another report by the UN-HABITAT (2008), a sea level rise in Abidjan is likely to swamp 562 square kilometers along the coastline of the region, as lowland marshes and lagoons dominate the coastal zone. The same report also predicts that Mombasa, in the East African coastal zonc, could be submerged by a sea level rise of 0.3 meters, with a large area becoming uninhabitable and less productive due to salt stresses. 2.1.1.3. Increasing Water Salinity Climate change can cause an increase or decrease in water salinity in multiple ways. While tropical oceans are increasingly becoming saltier, oceans closer to the poles have become fresher. This highlights that tropical oceans are very likely to suffer more from the potential impacts of increasing water salinity relative to waters in higher latitudes. Changes in water salinity have different effects depending on the tolerance level of the organisms and the nature of their ecosystem whether freshwater, marine or estuarine. The salinity of some freshwater ecosystems are predicted to increase as a result of anthropogenic climate change 1PCC, 2001). Such physical changes will negatively impact the population of both plankton and bigger prey fish species by affecting the organisms ability to osmoregulate (Schallenberg et al., 2003). Some empirical studies illustrate that change in salinity has a negative impact on zooplankton population, particularly in freshwater ecosystems. Schallenberg et a. (2003) depict hat zooplankton communities of low-lying, coastal, tidal lake and wetlands are adversely affected by sma increases in salinity levels. They further warn that such changes in zooplankton abundance may further disturb the ecological functioning of these valuable but vulnerable ecosystems. As is discussed in the subsequent section, changes in zooplankton populations or other planktonic primary and secondary producers disrupt the food chain, thus having a considerable negative impact on fisherySalinity is also considered one of the most important variables determining the survival of organisms in estuarine ecosystemsnations: (2) reducing jobs for many fishers involved in mollusk farming and harvest; or (3) increasing mollusk prices which may exclude marginal consumers further widening protein and wealth gaps between the rich and poor. A study done by Cooley et al. (2011) to assess the vulnerability of nations to occan acidification-driven decreases in mollusc harvests, suggests that countries with low adaptability, high nutritional or economic dependence on mollusks, and rapidly growing populations will be most vulnerable. These are common characteristics of most SSA countries. Thus, the region is very likely to be more, if not the most, vulnerable to ocean acidification. 2.1.2. Biological Changes Climate change is already affecting the trends of some important biological processes, resulting in changes in primary production (Taucher and Oschlies, 2011) and changes in fish distribution (Sumeila et al., 2011). Climate induced changes in primary production and fish stock distribution have negative implication on food security in many tropical coastal states in general and SSA in particular 2.1.2.1. Changes in Primary Production The relationship between climate change and future ocean primary production is likely to be a key constraint on fish and fisheries production (Dulvy et al., 2010). Survival of fish larvae during the planktonic stage is thought to depend strongly on the availability of sufficient and suitable food. Therefore, in addition to effects of changes in production, climate induced changes in distribution and phenology of fish larvae and their prey can also affect recruitment and production of fish stocks (Brander, 2010) Even though there are some studies done to assess the impact of climate change on primary productivity of aquatic environments in high latitude waters, there is very limited study done in the tropics. One of the very few studies available is the case of Lake Tanganyika. Lake Tanganyika has historically supported one of the worlds most productive pelagic fisheries, which provided an annual harvest in recent years of between 165,000 and 200,000 metric tons, representing 25 40 per cent of animal protein supply for the populations of the surrounding countries (Molsa et al 1999). A rise in surface-water temperature coupled with a regional decrease in wind velocity has increased the stability of the water column restricting mixing and deep-water nutrient upwelling and entertainment into surface waters (OReilly et al., 2003). This has led to a decrease in primary production by about 20 per cent over the past 80 years (Bates et al., 2008). According to OReilly et al. (2003), a 20 per cent reduction in primary productivity can be translated as a roughly 30 per cent decrease in fish yields. The decline in catch was accompanied by breakdown of the previously strong seasonal patterns in catch, suggesting decoupling from ecosystem processes driven by the weakening of hydrodynamic patterns. These changes in the pelagic fishery are consistent with a lake-wide shift in ecosystem functioning (Brander, 2010). Even though there are multiple factors that affect primary production in aquatic environment, one of the main factors is surface temperature rise. OReilly et al. (2003) suggest that if air temperature increases by about 1.7 degrees, as predicted for the next 80 years, therel be further increases in thermal stability and reductions in productivity in these large lakes. They further warn that the human implications of such faint but progressive environmental changes are potentially dire in this region of the world, where large lakes are essential natural resources for regional economies.2.1.2.2. Changes in Fish Distribution Change in fish distribution is among the most commonly reported ecological responses of

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