climate change on UAE - Stockholm Environment Institute-US Center
climate change on UAE - Stockholm Environment Institute-US Center
climate change on UAE - Stockholm Environment Institute-US Center
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is based <strong>on</strong> a theoretical understanding of<br />
system dynamics (bottom-up) or if it is built <strong>on</strong><br />
empirical observati<strong>on</strong>s (top-down).<br />
Models built from the top down are more<br />
comm<strong>on</strong>, if <strong>on</strong>ly because the line between an<br />
experimental c<strong>on</strong>struct and a model is blurred<br />
when using empirical data. Empirical models can<br />
be as simple as deriving a functi<strong>on</strong> to describe<br />
a relati<strong>on</strong>ship through a set of variables, or<br />
can be as complex a system which predicts<br />
spatial patterns of vegetati<strong>on</strong> under changing<br />
<str<strong>on</strong>g>climate</str<strong>on</strong>g> c<strong>on</strong>diti<strong>on</strong>s (see the CASA model,<br />
below). Empirical models may be methods of<br />
interpreting or simplifying datasets with rich<br />
temporal or spatial informati<strong>on</strong>, such as l<strong>on</strong>g<br />
time series or satellite data; or may use dense<br />
datasets to compile statistical relati<strong>on</strong>ships,<br />
which may then be used for predictive purposes.<br />
The advantages of empirically-based models is<br />
that they can be relatively simple to c<strong>on</strong>struct<br />
and interpret, are often highly explicit in their<br />
assumpti<strong>on</strong>s, and, most importantly, are based<br />
directly <strong>on</strong> data.<br />
Broadly, the bottom-up modeling approach<br />
relies <strong>on</strong> established theories <strong>on</strong> how individual<br />
comp<strong>on</strong>ents of an ecosystem operate at the<br />
micro-scale. These mechanistic models are<br />
often built to be as general as possible, such<br />
that they are not c<strong>on</strong>strained by data (collected<br />
by fallible observers) or limited by the way<br />
communities and ecosystems are structured<br />
today. The point of these models is to explore<br />
relati<strong>on</strong>ships between ecosystem comp<strong>on</strong>ents<br />
and forcing factors, understand dynamics, and<br />
impose c<strong>on</strong>diti<strong>on</strong>s <strong>on</strong> a simulated ecosystem<br />
which may not exist today. Some of the most<br />
developed versi<strong>on</strong>s of these models are able<br />
to predict the structure and functi<strong>on</strong> of major<br />
biomes from first principles (i.e. photosynthesis,<br />
respirati<strong>on</strong>, and nutrient requirements), and are<br />
now being used to explore how <str<strong>on</strong>g>climate</str<strong>on</strong>g> <str<strong>on</strong>g>change</str<strong>on</strong>g>,<br />
land use, and disturbance may impact future<br />
biomes.<br />
Model limitati<strong>on</strong>s<br />
All ecosystem models are severely limited by<br />
scale, scope, and assumpti<strong>on</strong>s. Key aspects of<br />
each are briefly described below.<br />
Scale: The most fundamental processes in<br />
an ecosystem occur at micro-scales, where<br />
photosynthesis and respirati<strong>on</strong> occur,<br />
nutrients are utilized, and water is cycled. There<br />
are, however, also important processes which<br />
happen at the scale of the leaf (for example,<br />
growth, senescence, shading, herbivory), the<br />
stem (individual mortality, light and water<br />
availability), the patch (disturbances), the<br />
community (competiti<strong>on</strong>), and the regi<strong>on</strong><br />
(<str<strong>on</strong>g>climate</str<strong>on</strong>g>, light availability). The levels to<br />
which these processes are simulated are<br />
computati<strong>on</strong>ally and data limited, and many<br />
processes operate across scales.<br />
Scope: The broader a model strives to be,<br />
the more general its assumpti<strong>on</strong>s must<br />
become. To simulate a single type of biome<br />
effectively, <strong>on</strong>e might choose to model or<br />
simulate a modest number of individual<br />
floristic species with known characteristics;<br />
to then include yet more diverse biomes in<br />
the model, <strong>on</strong>e often has to reduce the level<br />
of detail down to functi<strong>on</strong>al plant types<br />
rather than individual species. Models which<br />
are global in scope often reduce plant types<br />
down to simple plant functi<strong>on</strong>al types which<br />
distinguish between physiognomy (tree or<br />
grass), leaf form (broadleaf or needle-leaf),<br />
leaf l<strong>on</strong>gevity (evergreen or deciduous), and<br />
photosynthetic pathway (C 3<br />
or C 4<br />
) (i.e. Wang<br />
et al., 2004). Models which effectively capture<br />
global-scale dynamics may be ineffective or<br />
irrelevant for studies at the sub-biome scale.<br />
Assumpti<strong>on</strong>s: Every form of ecosystem model<br />
has (or should have) a well developed list of<br />
general assumpti<strong>on</strong>s. Empirical models, for<br />
example, often assume that relati<strong>on</strong>ships<br />
between correlated variables are causal, or<br />
at least replicable, and rarely model discrete<br />
pathways or mechanisms. First-principles<br />
(bottom-up) models are rarely entirely<br />
mechanistic: at some level, even the most<br />
rigorous models simplify processes and<br />
mechanisms with empirical relati<strong>on</strong>ships.<br />
9.2 Types of ecosystem models<br />
Ecosystem models span a wide range of<br />
functi<strong>on</strong>s, but several types may be useful for<br />
evaluating the impacts of <str<strong>on</strong>g>climate</str<strong>on</strong>g> <str<strong>on</strong>g>change</str<strong>on</strong>g> <strong>on</strong><br />
ecosystems and biodiversity in the <strong>UAE</strong>.<br />
Impacts, Vulnerability & Adaptati<strong>on</strong> for<br />
Dryland Ecosystems in Abu Dhabi<br />
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