The
assessment of adaptation turning points starts from the perspective
that management aims to sustain conditions for society and nature. A
critical threshold is reached, the moment that climate change renders
policy untenable or results in conditions that society perceives as
undesirable. At such a threshold situation, it is not only important to
know the extent of the impact, but at least equally important is to
know when and how likely it is that this situation occurs. Thus the
analysis focusses on the question of whether or not current management
is sustainable under a changing climate, and when adjustments are
required.
Assessing climate impacts in terms of
the finiteness of policy objectives has the important consequence that
it invites to elicit and discuss the thresholds that society should not
transgress. Ultimately, this question is a normative one –
how much change and risk is society willing to accept? Many studies of
adaptation view the legal and political system as boundary conditions.
Yet, by focusing on those boundaries and how to move them, greater
realisation of adaptation can be achieved (c.f. Cosens and Williams,
2012; Adger et al., 2013). The focus on thresholds highlights that
adaptation operates at two distinct levels: changes to the physical
environment, and changes to the decision environment, including policy
objectives. An often overlooked strategy in adaptation planning is for
actors to accept changes and adjust policy objectives accordingly.
Starting
from the threshold situation where the current management strategy can
no longer meet its objectives, the concept of ‘adaptation
tipping points’ was advanced for a policy study of long-term
water management in the Netherlands (Kwadijk et al., 2010). It has
proven successful in assessing and communicating water related risks,
and it has become one of the scientific concepts underpinning the Dutch
longterm water strategy (Haasnoot et al., 2013). A similar planning
approach was developed and tested for flood risk in the Thames estuary
(Lavery and Donovan, 2005; Smith et al., 2011). Reported studies so far
have focused on hydrological and technical thresholds for policy
success (Kwadijk et al., 2010; Reeder and Ranger, 2011; Lempert, 2013).
More recently, cases with social-ecologically defined policy objectives
have become available (Bölscher et al., 2013; Werners et al.,
2013b).
- Although the studies differ
methodologically, they address at least the following
questions:
- What defines unacceptable change:
which targets and thresholds exist for
different actors?
- Under which climatic
conditions are thresholds reached?
- When
are thresholds reached (including capturing uncertainty in a
time range)?
- When and how to respond?
To
avoid confusion with the popular term ‘tipping
point’ that people tend to associate with major change in
biophysical systems, MEDIATION uses ‘adaptation turning
point’ for the situation in which a social-political
threshold is reached due to climate change. Social-political thresholds
include formal policy objectives as well as informal societal
preferences, stakes and interests, such as willingness to invest and
protection of cultural identity (Werners et al., 2013a). Importantly,
reaching a turning point can be due to a biophysical tipping point, but
not necessarily so. Essentially, an adaptation turning point signifies
a moment in time at which a threshold of concern is likely to be
exceeded. Figure 1a illustrates that an adaptation turning point does
not mean that management is impossible and that catastrophic
consequences are to be faced. Yet, it implies progressive failure of
the current management (the “rocky road”), such
that actors may wish to turn to alternative strategies (the
“unexplored land”). Figure 1b illustrates how
scenario uncertainty can be translated into a time range in which the
adaptation turning point is likely to occur.
Illustration of an adaptation
turning pointFigure
1: a) the current direction is becoming unattractive in time (the
“rocky road”) and a turn to alternative routes is
for consideration (the “unexplored land”), b) a
threshold (here: failing safety standards at a sea level rise of 0.2 m
relative to 1990) is translated into a time range in which it is likely
to be reached. The figure uses projected global-averaged sea-level rise
for the 21st century from the IPCC assessment report (2001) (the dark
shading is the model average envelope for all IPCC SRES greenhouse gas
scenarios, the light shading is the envelope for all models and all
SRES scenarios, and the outer lines include an allowance for an
additional land-ice uncertainty (Church et al., 2008))