Search engine for discovering works of Art, research articles, and books related to Art and Culture
ShareThis
Javascript must be enabled to continue!

Warming-level dependent adaptation requirements and consequent limits to adaptation

View through CrossRef
<p>The level of detail to understand the impacts associated with different levels of global temperature increase across space and time is increasing with and since the publication of the IPCC Special Report on Global Warming of 1.5°C (SR1.5). However, current adaptation assessments are limited in picking up this information to understand what the implications of different impact pathways are for adaptation. Yet, the intensity, frequency and timing of impacts are critical determinants of the feasibility of different adaptation options and their associated costs.</p><p>There is increasing awareness that limits to adaptation are likely to be approached or crossed with higher levels of warming, however differential analyses of adaptation needs as a consequence of different warming pathways are so far limited. While case study based assessment of warming- and scenario-depend adaptation responses are emerging, so far an aggregated regional to global assessment is lacking.</p><p>Adaptation is often seen as a process that can draw on existing approaches that have been successfully implemented elsewhere, assuming that a linear increase of impacts would allow impacted regions to scale existing approaches to deal with hazards. However, climate impacts are unlikely to increase in a linear fashion across space and time and we are likely to enter new regimes of impacts in terms of intensity and frequency, with implications on recovery times. As a consequence, existing approaches are unlikely to be able to respond to these fundamentally changed conditions and limits to adaptation as we know it are likely to be reached. Understanding adaptation needs and potentials at different levels of global warming is therefore an urgent need in order to understand the full scale of the challenge. Such information is also critical in understanding the full cost of different mitigation pathway choices.</p><p>This contribution presents a framework for the systematic assessment of warming-level dependent adaptation needs and potentials across sectors and presents first results of this approach in the context of adaptation in the water sector. Our results highlight the need for differentiated approaches to planning adaptation, drawing a strong link to available impacts and vulnerability science to avoid mal-adaptation and to understand the full scope of the challenge. Where transformational adaptation will be required and current warming trajectories, early action may reduce associated costs of such measures across different dimensions, including financial, social or cultural aspects.</p>
Copernicus GmbH
Title: Warming-level dependent adaptation requirements and consequent limits to adaptation
Description:
<p>The level of detail to understand the impacts associated with different levels of global temperature increase across space and time is increasing with and since the publication of the IPCC Special Report on Global Warming of 1.
5°C (SR1.
5).
However, current adaptation assessments are limited in picking up this information to understand what the implications of different impact pathways are for adaptation.
Yet, the intensity, frequency and timing of impacts are critical determinants of the feasibility of different adaptation options and their associated costs.
</p><p>There is increasing awareness that limits to adaptation are likely to be approached or crossed with higher levels of warming, however differential analyses of adaptation needs as a consequence of different warming pathways are so far limited.
While case study based assessment of warming- and scenario-depend adaptation responses are emerging, so far an aggregated regional to global assessment is lacking.
</p><p>Adaptation is often seen as a process that can draw on existing approaches that have been successfully implemented elsewhere, assuming that a linear increase of impacts would allow impacted regions to scale existing approaches to deal with hazards.
However, climate impacts are unlikely to increase in a linear fashion across space and time and we are likely to enter new regimes of impacts in terms of intensity and frequency, with implications on recovery times.
As a consequence, existing approaches are unlikely to be able to respond to these fundamentally changed conditions and limits to adaptation as we know it are likely to be reached.
Understanding adaptation needs and potentials at different levels of global warming is therefore an urgent need in order to understand the full scale of the challenge.
Such information is also critical in understanding the full cost of different mitigation pathway choices.
</p><p>This contribution presents a framework for the systematic assessment of warming-level dependent adaptation needs and potentials across sectors and presents first results of this approach in the context of adaptation in the water sector.
Our results highlight the need for differentiated approaches to planning adaptation, drawing a strong link to available impacts and vulnerability science to avoid mal-adaptation and to understand the full scope of the challenge.
Where transformational adaptation will be required and current warming trajectories, early action may reduce associated costs of such measures across different dimensions, including financial, social or cultural aspects.
</p>.

Related Results

Adaptive Planning for Resilient Coastal Waterfronts
Adaptive Planning for Resilient Coastal Waterfronts
Many delta and coastal cities worldwide face increasing flood risk due to changing climate conditions and sea level rise. The question is how to develop measures and strategies for...
Seasonal dynamics and temperature sensitivity of soil CO2 efflux in a medium-term warmed subarctic grassland
Seasonal dynamics and temperature sensitivity of soil CO2 efflux in a medium-term warmed subarctic grassland
Climate warming is expected to occur stronger and faster in high-latitude terrestrial ecosystems compared to other regions of the world. It has been suggested that high-latitude sy...
Reduced spread of simulated global warming patterns among CMIP6 models with accelerated pace of warming
Reduced spread of simulated global warming patterns among CMIP6 models with accelerated pace of warming
Uneven economic impacts of climate change have been caused by differentiated warming rates across different geographical regions, threatening the well-being of millions to billions...
Untitled Document
Untitled Document
The pattern of surface warming plays a significant role in the Earth’s response to radiative forcing as it influences climate feedbacks. Distinct patterns of surface warming lead t...
Successful coastal adaptation projects? The role of multi-lateral climate funding.
Successful coastal adaptation projects? The role of multi-lateral climate funding.
<p><strong>This thesis investigates the evaluation of climate change adaptation success of projects in coastal zones of developing countries, specifically focusing on t...
Coupling between Free Tropospheric Warming and Elevated Surface Warming
Coupling between Free Tropospheric Warming and Elevated Surface Warming
Elevation-dependent warming (EDW) has been reported in observations and climate models, yet its magnitude and controlling mechanisms remain uncertain, particularly due to the compl...
Increased decomposition of root-derived biomass by warming in a temperate forest soil is depth-dependent
Increased decomposition of root-derived biomass by warming in a temperate forest soil is depth-dependent
Increased decomposition of root-derived biomass by warming in a temperate forest soil is depth-dependent&#160;Sun B, Zosso, C.U., Wiesenberg GLB, Pegoraro E., Torn MS, Schmidt ...
As different as day and night: evidence from root lifespan
As different as day and night: evidence from root lifespan
Abstract. Roots are key components of terrestrial ecosystem C cycling and play an important role in regulation of the response of terrestrial ecosystem to global climate warming, w...

Back to Top