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The Introduction sets out the research question of the book viz: the question of whether future generations ought to be represented in the global legal order and institutions to address the climate change challenge and, assuming a positive answer to this, how best such representation should occur. The massive bias against the interests of future generations in current climate law and policy-making is demonstrated. This provides a powerful rationale as to why there is an urgent need to explore proxy-style mechanisms to represent future generations. The pragmatist methodology (in the tradition of John Dewey) of the book is explained. This involves analysing existing practices, and values which are incorporated into these values, and extending them to deal with new problems. The legal realism methodology of the book is also explained, including its application to the sources of international law. The strong links between the book and Earth System Governance scholarship are set out; finally, the structure of the book is explained.
The Conclusion reiterates the overarching argument of the book, namely that the search for – and collective experimentation with – new forms of representation are immensely important forms of sustainable climate policy. Through proxy representation, future generations can be practically and institutionally involved in climate law and policy-making, considering both the vulnerability of future generations and their distinctive interests. The chapter discusses the need to find synergies between proposals for proxy-style mechanisms to represent future generations and development policy. New avenues for research are suggested, including the way in which science and scientific discourse can be a proxy for future generations’ interests, and also the way in which proxy representation of future generations features in climate treaty making processes and climate activism more generally.
Traditional pastoral practices have maintained Alpine grasslands over thousands of years, and Alpine biodiversity now depends on these practices. Grasslands are also central to the identity of pastoral communities: They are biocultural landscapes. Across the Alps, these landscapes are now threatened by high rates of agricultural land abandonment as traditional, labor-intensive agricultural methods become uneconomic, and small-scale development increases. The Autonomous Province of Bozen/Bolzano-South Tyrol, Italy, experiences some of the lowest rates of land abandonment and high rates of grassland retention. The case study explores the functions of regulatory intervention and coordination, two of the regulatory functions advanced by this book’s CIRCle Framework of regulatory functions for addressing cumulative environmental problems. It investigates how a diverse set of regulatory interventions provides for maintaining and restoring grasslands in South Tyrol, and how diverse forms of coordination – links between areas of laws, coordinating institutions, and dispute resolution processes – facilitate implementation in a context of deep multilevel governance.
In Chapter 3, firstly, we reconstruct central theoretical models of democracy and enquire how an expansion of representation mechanisms for future generations could be conceptualised within these justificatory narratives. Secondly, we analyse the values that underlie democratic practices which can be helpful for advancing proxy representation at the international level by providing ethical criteria for such reforms. This involves analysing the discourses of intergenerational justice, solidarity and vulnerability. The chapter then turns to examine how these discourses can be translated into political forms of proxy representation by drawing on the all affected principle which requires that those affected by a decision have a role in the making of that decision, which is argued to be an element of most, if not all theories of democracy. This in turn is hypothesised to provide a basis for extension of the demos to include future generations, which then justifies proxy forms of representation to enable their representation . Human rights are argued to constitute a practice of global values which provides a powerful normative orientation for climate law and policy-making.
Cumulative environmental impacts are a central problem that contemporary environment-related laws must face, from laws that allocate natural resources such as forests and water, to rights-based approaches to nature and human health. This introduction sketches the basic characteristics of a cumulative environmental problem – accumulating, incremental harms at different scales, caused by many and diverse actors, with the added complexity of interacting and uncertain effects addressed by multiple legal regimes. It explains why addressing cumulative environmental problems requires reaching across disciplines, legal contexts, and jurisdictions. The CIRCle Framework is introduced - a Framework of four integrated functions of formal rules for responding to cumulative environmental problems – conceptualization, information, regulatory intervention, and coordination. The chapter also introduces case studies of laws addressing environmental justice concerns related to groundwater in the Central Valley of California, cumulative harms to the biodiversity of the Great Barrier Reef, Australia, and cumulative impacts to grasslands as biocultural landscapes in South Tyrol, Italy.
Chapter 7 involves an analysis of the 2019 case brought to the UN committee on the rights of the child by 16 young people (Saachi et al. 2019). The case is assessed in terms of its legitimacy and effectiveness in promoting intergenerational justice discourses and its capacity to act as an indirect proxy representative for future generations. The chapter argues that while there are distinct limitations in the rights of the child complaints system (with an asymmetry in power between children and the states involved, with decisions being non-binding), the Saachi case, nevertheless, has the potential to have both a political and legal impact. It is one of the few avenues at the international level which allows young people increasingly impacted by climate change to have a voice. It can also allow young people to act as proxy representatives for future generations, while the Committee to date has been reticent to move in this direction. Finally, some elements of the decision are likely to be taken up in future climate litigation at the international and national levels.
This chapter provides a bird’s eye view of the landscape of laws that can deliver the CIRCle Framework functions of conceptualization, information, regulatory intervention, and coordination to address cumulative environmental problems. Its scope is broad, covering traditional and customary laws; environmental impact assessment and strategic environmental assessment; natural resources, land use planning, conservation, pollution, and other environment-related laws; and broader areas of public law, including constitutional environmental rights. It also discusses the way international treaties and development bank policies deal with cumulative impacts. The chapter provides a simple compass for navigating this landscape: considering whether the dominant focus of the law is a matter of concern that is threatened by cumulative impacts (e.g., environmental justice, national parks), impacts (e.g., environmental impact assessment, water pollution), or activities (e.g., road construction, mining), or whether it instead indirectly influences a cumulative environmental problem (e.g., laws for intergovernmental coordination).
Australia’s World Heritage-listed Great Barrier Reef experiences cumulative impacts from diverse activities, including regional catchment-sourced water pollution and the impacts of climate change. Regulating these threats engages a wide range of laws for intervention, which have been influenced by a regulatory mechanism for information – a strategic environmental assessment (SEA) undertaken a decade ago at the request of UNESCO. This chapter explores how the strategic assessment and associated interventions influence impacts from two major activities that contribute to water pollution and climate change – cattle grazing and coal mining. It shows that regulatory SEA can provide for entrenching and integrating ongoing information collection, analysis, and sharing. Moreover, SEA can directly influence diverse regulatory interventions to address cumulative impacts. It can link the functions of information and intervention, two of the regulatory functions advanced by this book’s CIRCle Framework. At the same time, opportunities remain to build stronger links between interventions for water quality and climate adaptation, and between climate change mitigation interventions and the Reef context.
Laminar–turbulent transition in shear flow is complicated and follows many possible routes. In this study, we seek to examine a scenario based on three-dimensional (3-D) waves (Jiang et al., 2020, J. Fluid Mech., vol. 890, A11) in compressible mixing layers, and elucidate the role of 3-D waves in generating streamwise vorticity. The Eulerian–Lagrangian coupled method is used to track the evolution of flow structures. Qualitative evidence shows that localised 3-D waves travel coherently with vortex structures at the early transition stage, which is consistent with the behaviours of 3-D waves in boundary layer transitions. To examine the local flow events surrounding 3-D waves and investigate the cause and effect relationships inherent in wave–vortex interaction, the finite-time Lyapunov exponent and components of the strain rate tensor are integrated into evolving Lagrangian material surfaces. The formation of high-shear layers in the flanks of the 3-D waves is observed, driven by fluid ejection and sweep motions induced by the amplification of 3-D waves. The $\Lambda$-shaped vortices are found born in the vicinity of high-shear regions and then stretched into hairpin-shaped vortices farther downstream. Statistical findings reveal that streamwise vorticity develops concurrently with the significant growth of the oblique mode, while the normal motion of wave structures induces a high strain rate layer in the surrounding region. In addition, conditional statistics underscore the significance of high shear in enstrophy generation. Finally, a conceptual model is proposed to depict the evolution of coherent structures based on the relationship among the 3-D waves, high-shear/strain layers, and $\varLambda$-vortices, providing insights into their collective dynamics within transitional mixing layers.
Finite-amplitude spiral vortex flows are obtained numerically for the Taylor–Couette system in the narrow limit of the gap between two concentric rotating cylinders. These spiral vortex flows bifurcate from circular Couette flow before axisymmetric Taylor vortex flow sets in when the ratio $\mu$ of the angular velocities of the outer to the inner cylinder is less than −0.78, consistent with the results of linear stability analysis by Krueger et al. (J. Fluid Mech., vol. 24, 1966, pp. 521–538), while the boundary of existence of spiral vortex flows is determined not by the linear critical point, but by the saddle-node point of the subcritical spiral vortex flow branch for $\mu \lessapprox -0.75$, when the axial wavenumber $\beta =2.0$. It is found that the nonlinear spiral vortex flows exhibit the mean flow in the axial direction as well as in the azimuthal direction, and that the profiles of both mean-flow components are asymmetric about the centre plane between the gap.
Gorstian sediments in south-central Wales preserve an asymmetric, compound mixed-process delta system north of the Carreg Cennen Disturbance and east of the Golden Grove Axis. The 30 km SW-NE outcrop, extending from the Cennen Valley to Y Pigwn, is oblique to the NNE delta progradation direction. The Hafod Fawr Formation comprises subaqueous delta slope deposits. Sandstone bed amalgamation indicates shoaling and wave/storm influence within the overlying subaqueous delta platform deposits of the Cwar Glas Member. The succeeding Mynydd Myddfai Sandstone Formation contains shoreline delta lithofacies within three geographical tracts. An embryonic Golden Grove Axis shed shoal water shoreline fan-delta and alluvial fan lithofacies (of the Trichrug Formation) in the Cennen Valley Tract. The SW Tract (Cilmaenllwyd to Banc Celynog) was deposited on the updrift flank of the asymmetric delta, with longshore drift to the NE. Amalgamated sandstone bedsets dominate in the mouth bar and terminal distributary channel lithofacies. Pen y Bicws preserves the axial gravel bed distributary channel lithofacies, which created a headland and palaeogeographic divide between the SW and NE tracts. The latter (Sawdde Gorge to Y Pigwn) records deposition in a low-energy bay that hosted cycles of heterolithic lithofacies. Collectively, these tracts occupied part of a sediment supply route to deeper facies of the subsidence-prone Clun Forest Sub-Basin. Emergent delta plain deposits become dominant within the overlying Trichrug Formation. Thin, locally preserved deposits of the Cribyn Du Member record delta abandonment and transgression during the Ludfordian associated with basin reconfiguration and expansion of the Caer’r mynach Seaway.
In this work the fascinating dynamics of a two-layered channel flow characterised by the dispersion in composite media within its layers is investigated in depth. The top layer comprises of a fluid zone that allows the fluid to travel along its surface easily (with relatively higher velocity), while the bottom layer is packed with porous media. The primary objective of this research is to do an in-depth investigation of the complex two-dimensional concentration distribution of a passive solute discharged from the inflow region. A multi-scale perturbation analysis approach has been implemented to address the system’s inherent complexity. This accurate determination of the dispersion coefficient, mean concentration distribution and two-dimensional concentration distribution is accomplished deftly using Mei’s homogenisation approach up to second-order approximation, which satisfactorily capture the minor variations in the solute dynamics also. The influence of various flow and porous media elements on these basic parameters is thoroughly investigated, expanding our comprehension of the complex interaction between flow dynamics and porous media’s properties. The effect of Darcy number and the ratio of two viscosities ($M$) on the dispersion coefficient depends on the height of the porous layer. As the Péclet number ratio increases, the dispersion coefficient experiences a concurrent increase, resulting in a decline in the concentration peak. The results of the analytical studies have also been compared with those results obtained using a purely computational method to establish the validity of our studies. Both the sets of results show quite good agreement with each other. In this study, alternate flow models have been used for the porous region, and the outcomes are compared to determine which approach yields more suitable results under different conditions.
The full understanding of the parasite fauna of a host species requires sampling individuals across their entire distribution range. However, very few studies include an analysis considering such geographical coverage. The Ocellated killifish, Floridichthys polyommus, is an endemic estuarine fish whose distribution spans from the southwestern Gulf of Mexico to Belize. Here, we aimed at describing the metazoan parasite fauna of F. polyommus in localities across the Yucatán Peninsula to assess the parasite species richness at regional and local scales. From 2022 to 2024, 409 specimens of F. polyommus were collected from six localities. Data from three localities from a previous study were also included. Individuals were dissected, and examined for ecto and endoparasites. Twenty-four metazoan parasite taxa were identified using morphological characters and/or molecular data. Thirteen parasite taxa correspond to larval stages. Nine parasite taxa represent new host records, increasing to 35 the total number of metazoan parasites known for F. polyommus. The nematode Contracaecum sp. was found in all sampled localities, whereas the cestode Glossocercus caribaensis and the copepod Ergasilus sp. were found in seven, with variable prevalence and mean intensity of infection values. Two general patterns were uncovered irrespective of the geographical scale of the analyses (local or regional): (1) Digeneans were the most species-rich parasite group and (2) F. polyommus harboured more larval parasite taxa than adults. It seems that the parasite fauna of the Ocellated killifish in each sampling site represent a subsample of the total species richness at the regional level.
Over the past two decades, the Canadian Arctic Archipelago has undergone significant glacier mass loss, driven primarily by surface melt. This study presents a detailed analysis of supraglacial drainage evolution along Ellesmere Island’s ∼830 km latitudinal extent using satellite imagery, historical aerial photographs and DEMs from 1959 to 2020. Analysis of five glaciers shows that drainage density (Dd) has increased over time, driven by the expansion of perennial rivers, especially at higher elevations. Far northern glaciers exhibit stable, well-developed drainage systems, while southern glaciers show a relatively greater increase in canyon development since 1959. Cold surface ice in the north supports higher Dd, while southern glaciers with extensive sinks (moulins and large crevasses) exhibit stronger surface-to-bed connectivity. Despite increased channelization, sinuosity changes remain statistically insignificant, reflecting dynamic canyon behavior governed by surface slope and meltwater discharge. Results align with modeled increases in melt, especially on southern glaciers where supraglacial systems have expanded most rapidly. Continued equilibrium line altitude rise under future warming is expected to intensify melt and result in the expansion of supraglacial drainage systems up-glacier, particularly for glaciers with large amounts of ice at mid-elevation.
The paper discusses the stochastic dynamics of the vortex shedding process in the presence of external harmonic excitation and coloured multiplicative noise. The situation is encountered in a turbulent practical combustor experiencing combustion instability. Acoustic feedback and turbulent flow are imitated by the harmonic and stochastic excitations, respectively. The Ornstein–Uhlenbeck process is used to generate the noise. A low-order model for vortex shedding is used. The Fokker–Planck framework is used to obtain the evolution of the probability density function of the shedding time period. Stochastic lock-in and resonance characteristics are studied for various parameters associated with the harmonic (amplitude, frequency) and noise (amplitude, correlation time, multiplicative noise factor) excitations. We observed that: (i) the stochastic lock-in (s-lock-in) boundary strongly depends on the noise correlation time; (ii) the parameter sites for s-lock-in can be approximately identified from the noise-induced shedding statistics; and (iii) stochastic resonance is significant for some intermediate correlation times. The effects of the above-mentioned observations are discussed in the context of combustion instability.
A deep-learning-based closure model to address energy loss in low-dimensional surrogate models based on proper-orthogonal-decomposition (POD) modes is introduced. Using a transformer-encoder block with an easy-attention mechanism, the model predicts the spatial probability density function of fluctuations not captured by the truncated POD modes. The methodology is demonstrated on the wake of the Windsor body at yaw angles of $\delta = [2.5^\circ ,5^\circ ,7.5^\circ ,10^\circ ,12.5^\circ ]$, with $\delta = 7.5^\circ$ as a test case, and in a realistic urban environment at wind directions of $\delta = [-45^\circ ,-22.5^\circ ,0^\circ ,22.5^\circ ,45^\circ ]$, with $\delta = 0^\circ$ as a test case. Key coherent modes are identified by clustering them based on dominant frequency dynamics using Hotelling’s $T^2$ on the spectral properties of temporal coefficients. These coherent modes account for nearly $60 \,\%$ and $75 \,\%$ of the total energy for the Windsor body and the urban environment, respectively. For each case, a common POD basis is created by concatenating coherent modes from training angles and orthonormalising the set without losing information. Transformers with different size on the attention layer, (64, 128 and 256), are trained to model the missing fluctuations in the Windsor body case. Larger attention sizes always improve predictions for the training set, but the transformer with an attention layer of size 256 slightly overshoots the fluctuation predictions in the Windsor body test set because they have lower intensity than in the training cases. A single transformer with an attention size of 256 is trained for the urban flow. In both cases, adding the predicted fluctuations close the energy gap between the reconstruction and the original flow field, improving predictions for energy, root-mean-square velocity fluctuations and instantaneous flow fields. For instance, in the Windsor body case, the deepest architecture reduces the mean energy error from $37 \,\%$ to $12 \,\%$ and decreases the Kullback–Leibler divergence of velocity distributions from ${\mathcal{D}}_{\mathcal{KL}}=0.2$ to below ${\mathcal{D}}_{\mathcal{KL}}=0.026$.