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Although many resource systems and populations exhibit high degrees of resilience
and adaptive capacity, there is a significant risk that critical thresholds
may be breached as a result of climate change, undermining this resilience.
The environmental risks in a region could vary significantly for different sectors,
depending on the degree of warming. To develop a risk profile for precautionary
management of climate change, it is necessary to assess the critical climate
threshold for a region for each of the relevant priority sectors, such as water
and agriculture. For instance, a small degree of surface warming could be beneficial
for agriculture in Russia but may be detrimental in India or Bangladesh. Increased
glacier melt in the Himalayas may cause serious floods in Nepal, India, and
Bangladesh. The potential environmental risks to water and marine resources
in marginal seas of Asia such as the Sea of Japan, Bohai Bay, and the Yellow
Sea also will depend on the degree of climate change—which could differ
significantly in these regions. For many countries in Asia, there is sparse
scientific research on the evaluation of sector-specific critical climatic thresholds.
The response of driving forces such as economic growth, population increase,
and technological progress in each country or region also should be included
in the determination of thresholds for precautionary risk management as an adaptation
strategy to climate change.
Rapid demographic transition accompanying significant economic growth is likely
in many Asian countries in the 21st century. These trends exacerbate pressures
on resource use, the climate system, and the natural environment. Population
growth and varying economic and technological conditions in Asia are likely
to affect some societies and resources more than changes in climate per se.
Moreover, socioeconomic and technological developments will interact with many
vulnerable sectors. However, predicting population growth rates and future economic
conditions is as uncertain an exercise as predicting the future climate. Institutional
and legal structures may change and will co-evolve with climatic risks. GHG
emission scenarios are especially important, but future emission trends will
depend on population growth and prevailing economic and technological conditions.
There have been limited studies that simultaneously take into account climate
change and other human-induced stresses. For vulnerability and adaptation to
be addressed comprehensively, they must be considered in a context of multiple
stresses caused by climate change and other anthropogenic activities.
Table 11-11 summarizes the vulnerability of key sectors,
from food and fiber through settlements, for subregions of Asia. This summary
is derived from a synthesis of available scientific research reviewed in this
chapter; it represents a consensus view of the authors. Levels of confidence
assigned to vulnerability also are shown in Table 11-11,
again based on iterative assessment of the available scientific evidence. Currently
available research synthesized in this table reveals a wide range of vulnerability,
as well as a wide range of uncertainties in the assessment of these vulnerabilities.
Geographical resolution as well as integration and scaling of basic physical
and biological responses are the key factors contributing to these uncertainties.
The limited database also makes it difficult to aggregate various responses
with only a few sample or spot assessments. Nevertheless, some key trends emerge
from the synthesis. A consistent message is the vulnerability of south and southeast
Asia across many sectors, as well as a high degree of confidence about this
assertion. Across virtually all subregions, water resources and natural ecosystems
are appraised as highly vulnerable to climate change, although the level of
confidence varies for some regions because of lack of data or greater complexity
in the resource systems. There may be some minor benefits to boreal Asia, making
it more resilient to potential impacts, but natural ecosystems clearly are under
threat in this subregion.
| Table 11-11: Vulnerability of key sectors to impacts
of climate change for select subregions in Asia. Vulnerability scale is
as follows: highly vulnerable (-2), moderately vulnerable (-1), slightly
or not vulnerable (0), slightly resilient (+1), and most resilient (+2).
Confidence levels abbreviated to VH (very high), H (high), M (medium), L
(low), and VL (very low). |
 |
| Regions |
Food and Fiber |
Biodiversity |
Water Resources |
Coastal Ecosystems |
Human Health |
Settlements |
|
| Boreal Asia |
+1 / H |
-2 / M |
+1 / M |
+1 / L |
-1 / L |
0 / M |
| |
|
|
|
|
|
|
| Arid and Semi-Arid Asia |
|
|
|
|
|
|
| - Central Asia |
-2 / H |
-1 / L |
-2 / H |
-1 / L |
-1 / M |
-1 / M |
| - Tibetan Plateau |
0 / L |
-2 / M |
-1 / L |
Not applicable |
No information |
No information |
| |
|
|
|
|
|
|
| Temperate Asia |
-2 / H |
-1 / M |
-2 / H |
-2 / H |
-2 / M |
-2 / H |
| |
|
|
|
|
|
|
| Tropical Asia |
|
|
|
|
|
|
| - South Asia |
-2 / H |
-2 / M |
-2 / H |
-2 / H |
-1 / M |
-2 / M |
| - Southeast Asia |
-2 / H |
-2 / M |
-2 / H |
-2 / H |
-1 / M |
-2 / M |
|
|