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DESIGNING PROJECTS IN A RAPIDLY CHANGING WORLD

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1.3 WHAT IS RAPTA?<br />

BOX A<br />

Key Terms and concepts*<br />

There is a Glossary and key concepts section<br />

in Appendix B. We present some fundamental<br />

concepts here, consistent with the ecological<br />

resilience literature.<br />

• Resilience is the capacity of a social–ecological<br />

system to absorb shocks and trends (e. g. like<br />

drought) and to reorganise so as to retain the<br />

same functions, structure, and feedbacks (i.e. the<br />

same identity). Resilience is neither good nor bad<br />

– a system can be in an undesirable state yet still<br />

be resilient to shocks, e.g. a grassland that has<br />

been invaded by unpalatable shrubs.<br />

• Adaptation refers to the process of change that<br />

enables a system to maintain its identity, so that<br />

it is better able to cope with trends and shocks,<br />

or to reduce vulnerability to disturbance.<br />

• Transformation is a shift from the current system<br />

to a substantively new and different one. For example,<br />

the transformation of a cropping system<br />

to an agro-pastoral system.<br />

• Adaptation and transformation may be planned<br />

(intentional) or unplanned (autonomous), wanted<br />

or unwanted, imposed by a government,<br />

community-led, or the result of a government-community<br />

partnership. It may happen at<br />

community-wide scale, or one household at a<br />

time. RAPTA helps to design interventions which<br />

are intentional adaptations and transformations.<br />

• Changes that adapt or transform a system can<br />

be fast (shocks) or slow (trends), or a combination<br />

of both. A controlling variable may change<br />

in a slow, predictable way (e.g. such as a rising<br />

groundwater table), but the impacts of that<br />

change may not be smooth and can exhibit<br />

threshold effects. For example, once saline<br />

groundwater rises to within a certain distance<br />

of the surface, capillary action draws it to the<br />

surface creating saline topsoil where trees and<br />

plants struggle to survive even if the water table<br />

falls again. In this case the controlling variable<br />

(groundwater level) changes smoothly,<br />

but the rapid change in soil condition causes<br />

a sudden, often irreversible, shock to land use.<br />

• It’s all a matter of scale, in time and space. Big<br />

changes such as a decline in soil fertility, or a rise<br />

in greenhouse gases, may be called “trends”<br />

when viewed against the time frame of the decisions<br />

of a person, or a government. However,<br />

over longer timescales they can be viewed as<br />

“shocks”. Likewise, a sequence of actions which<br />

are labelled “incremental adaptation” over the<br />

shorter term, may be seen as transformational<br />

over the longer term. Sometimes, in order to<br />

maintain the same system at one scale, transformations<br />

may have to occur at a finer scale. For<br />

example, if a river basin is to continue to supply<br />

irrigation water and the overall amount of rainfall<br />

is reducing due to climate change, some irrigation<br />

areas within that river basin may have to be<br />

closed down (i.e. transformed to dryland agriculture),<br />

in order to maintain an irrigation industry at<br />

the river basin scale.<br />

*Distilled from many sources in the social-ecological<br />

resilience literature, including Walker, BH &<br />

Salt, D 2012. Resilience Practice: Building capacity<br />

to absorb disturbance and maintain function,<br />

Island Press, Washington, D.C., USA.<br />

Introduction to RAPTA 19

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