Article 2 ͉ UNFCCC ͉ climate change impacts A rticle 2 of the United Nations Framework Convention on Climate Change (UNFCCC) commits signatory nations to stabilizing greenhouse gas concentrations in the atmosphere at a level that ''would prevent dangerous anthropogenic interference (DAI) with the climate system.'' The UNFCCC also highlights 3 broad metrics with which decision-makers are to assess the pace of progress toward this goal: allow ''ecosystems to adapt naturally to climate change,'' ensure that ''food production is not threatened,'' and enable ''economic development to proceed in a sustainable manner.'' In an effort to provide some insight into impacts that might be considered DAI, authors of the Third Assessment Report (TAR) of the Intergovernmental Panel on Climate Change (IPCC) identified 5 ''reasons for concern'' (RFCs) in (1). Each RFC categorizes impacts of a similar type, providing a set of metrics reflecting severity of risk. Relationships between various impacts reflected in each RFC and increases in global mean temperature (GMT) were portrayed in what has come to be called the ''burning embers diagram''; the image was also included in the Summary for Policy Makers of the contribution of Working Group II to the TAR and highlighted in the Synthesis Report.In presenting the ''embers'' in the TAR, IPCC authors did not assess whether any single RFC was more important than any other; nor, as they noted, did they conclude what level of impact or what atmospheric concentrations of greenhouse gases would constitute DAI, a value judgment that would be policyprescriptive. The ''embers'' were designed primarily to communicate the associations of impacts with increases in GMT and facilitate examination of the underlying evidence for use by decision-makers contemplating responses to these concerns.The IPCC Fourth Assessment Report (AR4) states that ''the 'reasons for concern' identified in the TAR remain a viable framework for assessing key vulnerabilities'' (2). In this article, we revise sensitivities of the RFCs to increases in GMT, based on our expert judgment about new findings in the growing literature since the publication of the TAR in 2001.* Furthermore, our judgments are supported by a more thorough understanding of the concept of vulnerability that has evolved over the past 8 years, † as well as a more careful articulation of the criteria by which any specific vulnerability can be labeled ''key,'' and thus contribute to a reason for concern (3). ‡ Section 1 defines and reviews the RFCs and ''burning embers'' figure as presented in the IPCC TAR. Section 2 presents the 1 To whom correspondence may be addressed. E-mail: jsmith@stratusconsulting.com or shs@stanford.edu. *These judgments were vetted by 3 rounds of IPCC review and were approved in the Summary for Policymakers of both the AR4 Working Group 2 and Synthesis Reports by the IPCC Plenary. † Vulnerability to climate change is the degree to which geophysical, biological and socioeconomic systems are susceptible to and unable to cope with adve...
The Reasons for Concern (RFC) framework communicates scientific understanding about risks in 1 relation to varying levels of climate change. The framework, now a cornerstone of the IPCC 2 assessments, aggregates global risks into five categories as a function of global mean temperature 3 change (GMT). We review the RFC's conceptual basis and the risk judgments made in the most recent 4 IPCC report, confirming those judgments in most cases in the light of more recent literature and 5 identifying their limitations. We point to extensions of the framework that offer complementary 6 climate change metrics to GMT and better account for possible changes in social and ecological 7 system vulnerability. Further research should systematically evaluate risks under alternative scenarios 8 of future climatic and societal conditions. 9The RFC framework was developed in the IPCC Third Assessment Report (TAR) to inform discussions 10 relevant to implementation of Article 2 of the UN Framework Convention on Climate Change (UNFCCC). 11Article 2 presents the Convention's long-term objective of avoiding "dangerous anthropogenic 12 interference with the climate system." The RFC framework and the associated "Burning Embers" 13 diagram illustrating authors' risk judgments have since been widely discussed and used to inform policy 14 decisions. For example, they informed a recent dialog between Parties to the UNFCCC and experts 1, 2 on 15 the adequacy of the long-term goal of avoiding a warming of 2°C relative to pre-industrial, contributing 16 to a strengthening of that goal in the recent Paris Agreement 3 . Elaborations of the Burning Embers have 17 been used to represent climate impacts and risks at the regional level 4 and for specific systems (e.g., 18ocean systems 5 ). 19This article reviews the conceptual basis for the RFCs (Box 1) and offers an explanation of the reasoning 20 behind associated risk judgments that is complementary to, but goes beyond, the treatment in the IPCC 21Fifth Assessment Report 6 . We focus explicitly on the evidence base for transitions from one risk level to 22 the next, incorporate post-AR5 literature in those discussions, and offer thoughts about limitations of 23 the subjective judgments behind each RFC. We also improved the synthesis of RFC-related material 24 across AR5, and in turn provide both a clearer connection to evidence from AR5 that supports the RFC 25 judgments, as well as a comparison of the RFCs to similar approaches employing metrics other than 26 GMT for characterizing risk. Perhaps most importantly, we consider improvements in the framework, 27 particularly emphasizing the dynamic nature of exposure and vulnerability, two key components of risk 28 not sufficiently covered in the current approach. 29 TEXT BOX 1: Conceptual Basis 30The Reasons for Concern (RFCs) reported in AR5 are: 31 Types of risk included in each category are discussed in the next section. The categories share an 37 emphasis on going beyond changes in biophysical systems to possible consequences for society and 38...
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The 1990 and 1991 ablation seasons over Greenland are simulated with a coupled atmosphere-snow regional climate model with a 25 km horizontal resolution. The simulated snow water content allows a direct comparison with the satellite derived melt signal. The model is forced with 6-hourly ERA-40 reanalysis at its boundaries. An evaluation of the simulated precipitation and a comparison of the modelled melt zone and the surface albedo with remote sensing observations are presented. Both the distribution and quantity of the simulated precipitation agree with observations from coastal weather stations, estimates from other models and the ERA-40 reanalysis. There are overestimations along the steep eastern coast which are most likely due to the "topographic barrier effect".The simulated extent and time evolution of the wet snow zone compare generally well with satellite derived data, except during rainfall events on the ice sheet and because of a bias in the passive microwave retrieved melt signal. Although satellite based surface albedo retrieval is only valid in the case of clear sky, the interpolation and the correction of these data enable us to validate the simulated albedo on the scale of the whole Greenland. These two comparisons highlight a large sensitivity of the remote sensing observations to weather conditions. Our high resolution climate model has been used to improve the retrieval algorithms by taking more fully into account the atmosphere variability. Finally the good agreement of the simulated melting surface with the improved satellite signal allows a detailed estimation of the melting volume from the simulation.
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