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Tuvalu is
a small reef island nation in the central Pacific, home to 11,000
Tuvaluans. Like most low-lying, island
or coastal states, Tuvalu is plagued by the threats of climate change with predicted
sea-level rise (SLR) and increased storm severity and frequency potentially causing
severe impacts, particularly as the island is already prone to risk of flood
and storm damage. This article does not
seek to outline the predicted impacts of climate change on Tuvalu, although
this may be incidental, but instead focuses on representations of the issue,
particularly related to migration as a prospective solution. Media reports on the fate of Tuvalu
have increased significantly over the last two decades, but the media portrayals
are not always accurate and often lack scientific support. Climate change predictions do not always
correlate to the observed impacts, and instead of addressing other social,
economic, or development issues unrelated to climate change, many issues get
put under the climate change umbrella, in a form of ‘garbage can anarchy’
(Connell, 2003). These issues, along
with consideration as to whether climate change really is motivation for
migration for the people of Tuvalu,
will be explored further below, using key papers as support of the case
study.
Tuvalu
consists of 24.4 km2 located on 3 small reef islands, and 6 coral atolls,
spread over 750,000 km2 (Connell, 2003). The capital, Funafuti, is becoming
increasingly built-up and overcrowded, resulting in environmental stressors
associated with cyclones, droughts, and flooding becoming even more challenging
(Connell, 2003). Because Tuvalu is very
low-lying (average 2m above sea level), it is highly susceptible to storm and
flood damage (Mortreux & Barnett, 2009).
Like most small Pacific island states, Tuvalu exhibits restricted social
and economic development, with a large portion of its economy based on aid
through the Tuvalu Trust Fund, and remittances from nationals working abroad in
mines or as seamen on overseas fishing lines (Connell, 2003).
The predicted impacts from climate change on
Tuvalu
include a lifting of the flooding zone associated with SLR, and an increase in
the impacts of coastal erosion from storms (Connell, 2003). Associated land-loss will lead to a decline
in agriculture production, an increase in competition for scarce land, and
reduced availability of important resources such as wood. Erosion of fringing reefs will disturb lagoon
ecology, reducing fishing potential, and damage mangrove habitats. (Connell,
2003). Opportunities for response and
adaptation to these impacts can be highly restricted in such small, fragmented,
impoverished states as Tuvalu,
and it is here that proposal for mass resettlement is often raised.
Migration has a history of significance in Tuvalu; post war, for work opportunities in
mines or as merchant seamen, or other remittance-based ventures in places such
as New Zealand
(Connell, 2003). There are widely held
assumptions that climate change will result in large scale migration from
Tuvalu, but Mortreux and Barnett (2009) challenge these assumptions by
identifying a multitude of variables that shape an individuals decision to
migrate, including issues at the origin, destination, in-between and personal
issues. Additional stressors such as
high population growth and density, low GDP, unemployment, unequal access to
resources and services, and poverty should be considered as ‘push’ factors for
migration alongside environmental change (Mortreux & Barnett, 2009). Mortreux and Barnett (2009) conducted
extensive field work in Funafuti in order to assess people’s risk perceptions
to anticipate future possible migration movements in relation to climate
change. They found that the majority of
those questioned wanted to stay, for reasons such as lifestyle, culture, and
identity, and those that expressed interest in leaving the island cited reasons
such as employment, opportunities, and access to services, before climate
change. Many people claimed they have
not seen the affects of climate change personally and therefore don’t see it as
a threat (Mortreux & Barnett, 2009).
This disparity between predicted and
observed impacts is something explored by Connell (2003) also. He reports that Australia’s National Tidal
Facility stated in 2002 they are yet to see the acceleration of sea levels that
climatologists have predicted. Short
term fluctuations in tidal levels have been observed, particularly in response
to El Niño events that
may have been accentuated by high spring tides, but this is unrelated to long
term climate changes (Connell, 2003). A
considerable range of environmental and social changes have been attributed to
climate change even when science says they are not related, and this, Connell
(2003) states, is an example of ‘garbage can anarchy’, where new problems are
grafted onto old ones and given a single cause with once isolated phenomena
becoming systematically interrelated.
The media plays
a crucial role in representing the issues.
The media has been used as a tool for popularizing and encouraging the
idea Tuvaluans need to migrate, when they need more to focus on adaptation (Mortreux & Barnett, 2009), and has accentuated concerns over
accelerated global warming and its impact (Connell, 2003). Popular media, such as The Sydney Morning Herald and Time
Magazine, have been quoted using emotive language, such as ‘sinking
feeling,’ ‘vanishing worlds,’ and ‘imminent peril of paradise’, often
concerning unspecified details, to try attach certainty to their reports,
usually with no supporting scientific notes (Connell, 2003). In an extreme example, Connell (2003) reports
an article in the Appalachian Trailway
News (2002) stated:
‘Global warming caused the
waters of the Pacific Ocean to rise; drowning the country’s (Tuvalu) nine coral
atolls and making its 11,000 people flee their homeland forever’
An example of unhelpful sensationalization
with an absence of evidence; this is absolutely untrue.
From the above I argue there can be disparity
between predicted climate change and what is observed in reality, and that at
times unrelated social, environmental, or development issues are attributed to
climate change. I further argue the
media adds to this by misrepresenting information, and often local fears and
distant media perceptions accentuate and emphasise each other, leading to a
false portrayal of the issues. It has
also been shown that for Tuvaluans at least, climate change is not necessarily
a motivator for migration.
In light of these explorations, I propose there
are other issues unrelated to climate change, such as overpopulation and unemployment,
which presently need to be addressed. However, SLR is likely to occur in the
future, and emphasis now should be on reducing greenhouse gas emissions on a
global trend to slow the rate of climate change. Research should seek to explore methods for developing
and adopting adaptive and redevelopment strategies to avoid migration and allow
people to sustain existing lifestyles wherever possible. Media representations, emotions, or politics should
not overpower or replace science and reality.
References
Connell, J., (2003).
Losing Ground? Tuvalu,
the greenhouse effect and the garbage can. Asia Pacific Viewpoint 44(2):
89-107.
Mortreux, C. and Barnett, J., (2009). Climate change, migration and adaptation in Funafuti, Tuvalu. Global Environmental Change 19: 105-112.