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climate change on UAE - Stockholm Environment Institute-US Center

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populate itself, and imbalances in the food-web,<br />

meaning that there is either not enough food for<br />

top predators or there are too few predators to<br />

c<strong>on</strong>trol the populati<strong>on</strong> of prey species. In these<br />

circumstances, the imbalances can quickly<br />

stack up synergistically in a positive feedback<br />

cycle: for example, as top predators dwindle,<br />

prey species multiply quickly and begin to<br />

deplete food sources for other species or <str<strong>on</strong>g>change</str<strong>on</strong>g><br />

the physical or chemical properties of their<br />

ecosystem. For example, overfishing of Codfish<br />

in the rich kelp (seaweed) forests of the Gulf of<br />

Maine allowed sea urchins to prosper, which in<br />

turn destroyed the kelp habitat (Jacks<strong>on</strong> et al,<br />

2001). Cod is now extinct in the North Atlantic,<br />

and the habitat has, for all intensive purposes,<br />

<str<strong>on</strong>g>change</str<strong>on</strong>g>d permanently.<br />

Habitat destructi<strong>on</strong> results in the loss of<br />

ecosystem area or an impedance in ecosystem<br />

functi<strong>on</strong>, and is, by far, the most pressing threat<br />

to biodiversity worldwide. Polluti<strong>on</strong> and habitat<br />

misuse can destroy or impede key elements of<br />

an ecosystem, lending to severe imbalances and<br />

loss of ecosystem functi<strong>on</strong>ality. For example,<br />

overgrazing in arid ecosystems comm<strong>on</strong>ly leads<br />

to the trampling of biogenic crusts and the loss<br />

of critical vegetati<strong>on</strong> cover, which, in turn, leads<br />

to increased runoff and erosi<strong>on</strong>, nutrient losses,<br />

and can promote invasive species.<br />

The direct loss of habitat by land use <str<strong>on</strong>g>change</str<strong>on</strong>g> can<br />

also result in the loss of biodiversity as parts of<br />

an ecosystem are transformed for another use,<br />

there is less area for the native ecosystem to<br />

use. The relati<strong>on</strong>ship between species diversity<br />

and area has been recognized since at least<br />

the early 20 th century, and was formalized by<br />

Williams (1964) and, later, Rosenzsweig (1995)<br />

as a logarithmic curve. In numerous studies, as<br />

larger areas are examined, the number of species<br />

increases (i.e. from a small plot to a c<strong>on</strong>tinent).<br />

Geographical c<strong>on</strong>straints, the ability to move,<br />

migrate, and compete, and the ability to<br />

escape small-scale disturbances all govern the<br />

relati<strong>on</strong>ship between area and speciati<strong>on</strong>.<br />

Within a specific type of biome or ecosystem, as<br />

the physical size of the ecosystem is reduced,<br />

the number of species which can be supported<br />

in the ecosystem is also reduced. Expansi<strong>on</strong><br />

of urban areas, deforestati<strong>on</strong>, sedimentati<strong>on</strong>,<br />

and agricultural expansi<strong>on</strong> are all mechanisms<br />

of direct habitat destructi<strong>on</strong>. Fragmentati<strong>on</strong><br />

restricts the ability for species to migrate or<br />

expand. Thus, even if total habitat space is<br />

large, but is subdivided into small fragments,<br />

the net effect results in small, n<strong>on</strong>-diverse (and<br />

often functi<strong>on</strong>ally deficient) ecosystems.<br />

Finally, <str<strong>on</strong>g>climate</str<strong>on</strong>g> <str<strong>on</strong>g>change</str<strong>on</strong>g> may already be<br />

resp<strong>on</strong>sible for some species losses and<br />

threatens to lead to rampant reducti<strong>on</strong>s in<br />

biodiversity globally. Climate <str<strong>on</strong>g>change</str<strong>on</strong>g> shifts the<br />

basic substrates up<strong>on</strong> which ecosystems rely:<br />

as temperatures increase and precipitati<strong>on</strong><br />

patterns are altered, ecosystems which used to<br />

thrive in <strong>on</strong>e regi<strong>on</strong> may be displaced to other<br />

areas or disappear altogether. For many biomes<br />

around the world, this shift may look like a mass<br />

movement of ecosystems towards the poles or<br />

higher elevati<strong>on</strong>s, while ecosystems already<br />

near the poles or at high elevati<strong>on</strong> may be lost<br />

completely.<br />

While the story is both complicated and<br />

uncertain, it is likely that many sedentary<br />

or n<strong>on</strong>-migrating species will be unable to<br />

move at the pace of <str<strong>on</strong>g>climate</str<strong>on</strong>g> <str<strong>on</strong>g>change</str<strong>on</strong>g>, and even<br />

migratory species may find their migratory<br />

routes falling out of synchr<strong>on</strong>y with weather<br />

and food patterns. For all of these reas<strong>on</strong>s, it<br />

is likely that <str<strong>on</strong>g>climate</str<strong>on</strong>g> <str<strong>on</strong>g>change</str<strong>on</strong>g> al<strong>on</strong>e will lead to<br />

significant biodiversity losses (Sala et al., 2000),<br />

and the effect will be compounded where there<br />

are already significant envir<strong>on</strong>mental stresses,<br />

such as those described previously (Thomas et<br />

al, 2004).<br />

8.1. Biodiversity and ecological<br />

thresholds<br />

In 2000, Sala and others predicted that<br />

“Mediterranean <str<strong>on</strong>g>climate</str<strong>on</strong>g> and grassland<br />

ecosystems likely will experience the greatest<br />

proporti<strong>on</strong>al <str<strong>on</strong>g>change</str<strong>on</strong>g> [loss] in biodiversity”<br />

by 2100 due to the combined influence of<br />

<str<strong>on</strong>g>climate</str<strong>on</strong>g> <str<strong>on</strong>g>change</str<strong>on</strong>g>, land use <str<strong>on</strong>g>change</str<strong>on</strong>g>, <str<strong>on</strong>g>change</str<strong>on</strong>g>s in<br />

atmospheric CO 2<br />

, and introduced (invasive)<br />

species. Except for far northern and southern<br />

latitudes, where <str<strong>on</strong>g>climate</str<strong>on</strong>g> <str<strong>on</strong>g>change</str<strong>on</strong>g> is expected to<br />

have the most significant impacts, <str<strong>on</strong>g>change</str<strong>on</strong>g>s in<br />

land use are expected to be resp<strong>on</strong>sible for the<br />

heaviest toll <strong>on</strong> biodiversity. According to the<br />

Sala et al. (2000) analysis, if we assume that<br />

interacti<strong>on</strong>s am<strong>on</strong>gst the drivers of biodiversity<br />

<str<strong>on</strong>g>change</str<strong>on</strong>g> are synergistic and multiplicative,<br />

164<br />

Climate Change Impacts, Vulnerability & Adaptati<strong>on</strong>

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