scholarly journals World Heritage on the Move: Abandoning the Assessment of Authenticity to Meet the Challenges of the Twenty-First Century

Heritage ◽  
2021 ◽  
Vol 4 (1) ◽  
pp. 371-386
Author(s):  
Roha W. Khalaf

At a time when climate change, conflicts, disasters, and other global crises and challenges are increasingly affecting World Heritage properties, the utility of conservation assessment standards must be rethought. This article proposes abandoning the assessment of authenticity to treat properties less as “things”, deemed authentic or not, and more as evolving “processes” that embrace continuity and compatible change, which, it is argued, helps meet the challenges of the twenty-first century, namely climate change mitigation and adaptation; building back better after conflicts, disasters, or pandemics; and, ultimately, achieving sustainable development goals. Drawing on policy analysis and a wide range of literature, the article explains why authenticity is not a useful concept and why the idea of “heritage as process” is more relevant to the contemporary world. It shows how this idea can be put into effect and linked to Outstanding Universal Value, integrity, protection and management, which are already requirements in UNESCO’s Operational Guidelines for the implementation of the World Heritage Convention. In doing so, it contributes to aligning the implementation of the Convention with that of the global agendas of our time.

Author(s):  
Ottavio Quirico

The international protection of tangible cultural heritage overlaps with that of the environment, ranging from the conservation of biodiversity to the prevention of desertification. Against this background, the phenomenon of climate change raises questions that challenge the fundamentals of the World Heritage Convention, which protects cultural heritage and interlinked natural heritage. Global warming critically affects cultural sites of outstanding universal value, such as the city of Venice, and depletes mixed cultural and natural sites inscribed on the World Heritage List, such as Tassili n’Ajjer. Arguably, the World Heritage Convention is lex specialis with respect to international environmental regulation as concerns localized adaptation and mitigation measures protecting sites of outstanding universal value. By contrast, environmental regulation, notably the UNFCCC regime as reviewed in Paris in December 2015, is lex specialis as concerns general mitigation and adaptation, systemically integrating the protection of tangible cultural heritage. This argument also applies to intangible cultural heritage, including a human rights perspective. In fact, the fundamental right to culture has been invoked in international jurisdictions to protect intangible heritage, but still remains lex generalis with respect to the UNFCCC regime. As in a set of nested boxes, such an interactive pattern outlines a basic paradigm to shape the broader intersection between the regulatory regimes protecting tangible cultural heritage and the environment in international law.


2021 ◽  
Vol 166 (3-4) ◽  
Author(s):  
Salah Basem Ajjur ◽  
Sami G. Al-Ghamdi

AbstractQuantifying the impact of climate change on evapotranspiration is necessary for devising accurate water and energy budgets in light of global warming. Nevertheless, in the Middle East and North Africa (MENA), little has been done to bridge this gap. This study, then, implements Penman and Budyko approaches to climatic data retrieved from the sixth phase of the Coupled Model Intercomparison Project (CMIP6) to assess evapotranspiration and water availability evolutions through the twenty-first century. Outcomes reveal that the MENA region is indeed vulnerable to a surge in temperature, which can increase evapotranspiration losses and decrease water availability. Under the shared socioeconomic pathway (SSP2-4.5), the potential evapotranspiration (PET) has been projected to increase throughout the MENA region by up to 0.37 mm per year during the middle of the twenty-first century (2021–2050) and by up to 0.51 mm per year during the end of the twenty-first century (2071–2100). Meanwhile, the actual evapotranspiration (AET) has been projected to increase by up to 0.3 (~0.2) mm per year before 2050 (2100). The trends in both projections (PET and AET) are exaggerated under SSP5-8.5. The analysis predicted a shortage of water availability (precipitation—AET), which is alarming for most MENA regions. Relative to the reference period (1981–2010), the decline in annual water availability would reach 26 (62) mm by 2100 under SSP2-4.5 (SSP5-8.5). The rise in temperatures appears to be the principal reason for MENA and water availability responses. This study’s outcomes can facilitate accurate and realistic predictions related to evapotranspiration and water availability, which are key elements in not only managing water resources but also in devising effective climate change mitigation and adaptation plans.


Author(s):  
Hyun Min Sung ◽  
Jisun Kim ◽  
Sungbo Shim ◽  
Jeong-byn Seo ◽  
Sang-Hoon Kwon ◽  
...  

AbstractThe National Institute of Meteorological Sciences-Korea Meteorological Administration (NIMS-KMA) has participated in the Coupled Model Inter-comparison Project (CMIP) and provided long-term simulations using the coupled climate model. The NIMS-KMA produces new future projections using the ensemble mean of KMA Advanced Community Earth system model (K-ACE) and UK Earth System Model version1 (UKESM1) simulations to provide scientific information of future climate changes. In this study, we analyze four experiments those conducted following the new shared socioeconomic pathway (SSP) based scenarios to examine projected climate change in the twenty-first century. Present day (PD) simulations show high performance skill in both climate mean and variability, which provide a reliability of the climate models and reduces the uncertainty in response to future forcing. In future projections, global temperature increases from 1.92 °C to 5.20 °C relative to the PD level (1995–2014). Global mean precipitation increases from 5.1% to 10.1% and sea ice extent decreases from 19% to 62% in the Arctic and from 18% to 54% in the Antarctic. In addition, climate changes are accelerating toward the late twenty-first century. Our CMIP6 simulations are released to the public through the Earth System Grid Federation (ESGF) international data sharing portal and are used to support the establishment of the national adaptation plan for climate change in South Korea.


Author(s):  
Dionysia Katelouzou ◽  
Peer Zumbansen

This chapter explores corporate governance as a transnational regulatory field. Mirroring the rise in importance of the idea of shareholder wealth maximization as a firm’s definitive performance measure, corporate governance became a hotly contested field of competing visions of firms’ institutional and normative infrastructure in search of creating the most advantageous conditions to attract capital in volatile markets. This shift occurred at the same time that regulatory transformations in Western postindustrial societies since the early 1980s had begun to significantly shift public service provision and state-organized frameworks for old-age security guarantees and access to health services. Today’s corporate governance laboratory is a transnational force field, fought over by a host of different state and nonstate actors and also by private actors such as institutional investors. Meanwhile, following the financial crises in 2001, 2008 and 2020 and the simultaneously growing pressure on corporations from human rights, gender equality, and environmental groups, the corporate governance debate again is shifting. This time, a diversity of issues are being discussed under the corporate governance rubric, indicating a more comprehensive engagement with the firm’s purpose and functions and its societal obligations and responsibilities. Given the crucial role of firms as the residual claimants of a wide-ranging retreat of the state from its role in guaranteeing and providing a wide range of social functions, corporate governance is a mirror for the transformation of public and private power, and it has to address the twenty-first-century challenges, including global value chains and the proliferation of institutional investors, unfolding on a planetary scale.


2017 ◽  
Vol 30 (17) ◽  
pp. 6701-6722 ◽  
Author(s):  
Daniel Bannister ◽  
Michael Herzog ◽  
Hans-F. Graf ◽  
J. Scott Hosking ◽  
C. Alan Short

The Sichuan basin is one of the most densely populated regions of China, making the area particularly vulnerable to the adverse impacts associated with future climate change. As such, climate models are important for understanding regional and local impacts of climate change and variability, like heat stress and drought. In this study, climate models from phase 5 of the Coupled Model Intercomparison Project (CMIP5) are validated over the Sichuan basin by evaluating how well each model can capture the phase, amplitude, and variability of the regionally observed mean, maximum, and minimum temperature between 1979 and 2005. The results reveal that the majority of the models do not capture the basic spatial pattern and observed means, trends, and probability distribution functions. In particular, mean and minimum temperatures are underestimated, especially during the winter, resulting in biases exceeding −3°C. Models that reasonably represent the complex basin topography are found to generally have lower biases overall. The five most skillful climate models with respect to the regional climate of the Sichuan basin are selected to explore twenty-first-century temperature projections for the region. Under the CMIP5 high-emission future climate change scenario, representative concentration pathway 8.5 (RCP8.5), the temperatures are projected to increase by approximately 4°C (with an average warming rate of +0.72°C decade−1), with the greatest warming located over the central plains of the Sichuan basin, by 2100. Moreover, the frequency of extreme months (where mean temperature exceeds 28°C) is shown to increase in the twenty-first century at a faster rate compared to the twentieth century.


2017 ◽  
Vol 56 (9) ◽  
pp. 2393-2409 ◽  
Author(s):  
Rick Lader ◽  
John E. Walsh ◽  
Uma S. Bhatt ◽  
Peter A. Bieniek

AbstractClimate change is expected to alter the frequencies and intensities of at least some types of extreme events. Although Alaska is already experiencing an amplified response to climate change, studies of extreme event occurrences have lagged those for other regions. Forced migration due to coastal erosion, failing infrastructure on thawing permafrost, more severe wildfire seasons, altered ocean chemistry, and an ever-shrinking season for snow and ice are among the most devastating effects, many of which are related to extreme climate events. This study uses regional dynamical downscaling with the Weather Research and Forecasting (WRF) Model to investigate projected twenty-first-century changes of daily maximum temperature, minimum temperature, and precipitation over Alaska. The forcing data used for the downscaling simulations include the European Centre for Medium-Range Weather Forecasts (ECMWF) interim reanalysis (ERA-Interim; 1981–2010), Geophysical Fluid Dynamics Laboratory Climate Model, version 3 (GFDL CM3), historical (1976–2005), and GFDL CM3 representative concentration pathway 8.5 (RCP8.5; 2006–2100). Observed trends of temperature and sea ice coverage in the Arctic are large, and the present trajectory of global emissions makes a continuation of these trends plausible. The future scenario is bias adjusted using a quantile-mapping procedure. Results indicate an asymmetric warming of climate extremes; namely, cold extremes rise fastest, and the greatest changes occur in winter. Maximum 1- and 5-day precipitation amounts are projected to increase by 53% and 50%, which is larger than the corresponding increases for the contiguous United States. When compared with the historical period, the shifts in temperature and precipitation indicate unprecedented heat and rainfall across Alaska during this century.


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