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As the world moves with increasing urgency to mitigate climate change and catalyze energy transitions to net zero, understanding the governance mechanisms that will unlock barriers to energy transitions is of critical importance. This book examines how the clean energy regime complex-the fragmented, complex sphere of governance in the clean energy issue area characterized by proliferating and overlapping international institutions-can be effective in fostering energy transitions at the domestic level, particularly in emerging market and developing economies (EMDEs). Through comparative case studies of geothermal development in Indonesia and the Philippines, the chapters provide two different tales of energy transitions, demonstrating how domestic factors have hindered or facilitated progress. This book will be useful for students, researchers, and practitioners working in international relations, energy politics, political science, development studies, public policy, international law, and sociology. This title is also available as Open Access on Cambridge Core.
The family Glassiidae from Silurian and Devonian strata exhibits barrel-shaped and medially directed spiralia as primary characteristics. Membership in this family is small with five known genera, of which only two possess recognized spiralia. This paper aims to investigate the two Devonian glassiides: Karbous Havlíček, 1985 and Trigonatrypa Havlíček, 1990. In mature specimens, the type species K. aperinus Havlíček, 1985 and the species K. hassiacus (Siehl, 1962) show dorsally directed spiralia. Karbous is here placed in the family Karpinskiidae based on similar internal characteristics. The type species of Trigonatrypa was not available for study. A closely related species, T. baucis (Barrande, 1847), was sectioned and found to possess medially directed spiralia. The type species is likely to have the same kind of spiralia. Therefore, the case for placing Trigonatrypa in the Glassiidae is strengthened.
Elastic turbulence can lead to increased flow resistance, mixing and heat transfer. Its control – either suppression or promotion – has significant potential, and there is a concerted ongoing effort by the community to improve our understanding. Here we explore the dynamics of uncertainty in elastic turbulence, inspired by an approach recently applied to inertial turbulence in Ge et al. (J. Fluid Mech., vol. 977, 2023, A17). We derive equations for the evolution of uncertainty measures, yielding insight on uncertainty growth mechanisms. Through numerical experiments, we identify four regimes of uncertainty evolution, characterised by (i) rapid transfer to large scales, with large-scale growth rates of $\tau ^{6}$ (where $\tau$ represents time), (ii) a dissipative reduction of uncertainty, (iii) exponential growth at all scales and (iv) saturation. These regimes are governed by the interplay between advective and polymeric contributions (which tend to increase uncertainty), viscous, relaxation and dissipation effects (which reduce uncertainty) and inertial contributions. In elastic turbulence, reducing Reynolds number increases uncertainty at short times, but does not significantly influence the growth of uncertainty at later times. At late times, the growth of uncertainty increases with Weissenberg number, with decreasing polymeric diffusivity and with the logarithm of the maximum length scale, as large flow features adjust the balance of advective and relaxation effects. These findings provide insight into the dynamics of elastic turbulence, offering a new approach for the analysis of viscoelastic flow instabilities.
In this study, we experimentally investigate the stress field around a gradually contaminated bubble as it moves straight ahead in a dilute surfactant solution with an intermediate Reynolds number ($20 \lt {{\textit{Re}}} \lt 220$) and high Péclet number. Additionally, we investigate the stress field around a falling sphere unaffected by surface contamination. A newly developed polarisation measurement technique, highly sensitive to the stress field in the vicinity of the bubble or the sphere, was employed in these experiments. We first validated this method by measuring the flow around a solid sphere sedimenting in a quiescent liquid at a terminal velocity. The measured stress field was compared with established numerical results for ${{\textit{Re}}} = 120$. A quantitative agreement with the numerical results validated this technique for our purpose. The results demonstrated the ability to determine the boundary layer. Subsequently we measured a bubble rising in a quiescent surfactant solution. The drag force on the bubble, calculated from its rise velocity, was set to transiently vary from that of a clean bubble to a solid sphere within the measurement area. With the intermediate drag force between clean bubble and solid sphere, the stress field in the vicinity of the bubble front was observed to be similar to that of a clean bubble, and the structure near the rear was similar to that of a solid sphere. Between the front and rear of the bubble, the phase retardation exhibited a discontinuity around the cap angle at which the boundary conditions transitioned from no slip to slip, indicating an abrupt change in the flow structure. A reconstruction of the axisymmetric stress field from the phase retardation and azimuth obtained from polarisation measurements experimentally revealed that stress spikes occur around the cap angle. The cap angle (stress jump position) shifted as the drag on the bubble increased owing to surfactant accumulation on its surface. Remarkably, the measured cap angle as a function of the normalised drag coefficient quantitatively agreed with the numerical results at intermediate ${{\textit{Re}}} = 100$ of Cuenot et al. (1997 J.FluidMech.339, 25–53), exhibiting only a slight deviation from the curve predicted by the stagnant cap model at low ${\textit{Re}}$ (creeping flow) proposed by Sadhal & Johnson (1983 J.FluidMech.126, 237–250).
This study examines the reflection of a rightward-moving shock (RMS) over expansion waves, dividing the reflection structure into three components. The first component analyses the pre- and post-interaction parts of the expansion waves, categorising primary flow patterns into four types with defined transition criteria, visualised through Mach contours. The second component investigates the curved perturbed shock. Through numerical simulations, the influence of increasing shock strength on the flow structures is displayed. A triple point forms for an RMS of the first family, and the Mach stem height increases with the increase of shock strength. When the RMS is strong enough, a vortex forms in the near-wall region, which acts like a wedge to distort the near-foot part of the RMS. The third component, the near-foot region, is analysed using a one-dimensional Riemann problem approach. The calculated wave speeds are used to mark waves in Mach contours for eight cases. The position of the waves indicates that the left-going shock for an RMS of the first family or the right-going shock for an RMS of the second family corresponds to the foot of the RMS. This can explain the finding that the right-hand side of an RMS of the first family or the left-hand side of an RMS of the second family is disturbed. The regions to have different wave patterns solved from the one-dimensional Riemann problem are displayed in the original Mach number–shock speed Mach number plane.
The early stage of a gravity-driven flow resulting from the sudden removal of a floating body is investigated. Initially, the fluid is at rest, with a rigid, symmetric wedge floating on its surface. The study focuses on the initial evolution of the wedge-shaped depression formed on the water’s free surface. The fluid has finite depth, and the resulting flow is assumed to be governed by potential theory. The initial flow is described by a linear boundary-value problem, which is solved using conformal mapping and the theory of complex analytic functions. The behaviour of the flow velocity near the corner points of the fluid domain is analysed in detail. It is shown that the linear theory predicts a power-law singularity in the flow velocity at the vertex of the wedge-shaped depression, with the exponent depending on the wedge angle. As the cavity extends toward the bottom, the flow singularity at the vertex becomes stronger. The local flow near the vertex is shown to be self-similar at leading order in the short-time limit. At the other two corner points – where the initial free surface intersects the surface of the wedge – the linear theory predicts continuous velocities with singular velocity gradients. Theoretical predictions are compared with numerical results obtained using OpenFOAM. Good agreement is observed at short times, except in small vicinities of the corner points, where inner solutions are required. In practical applications, understanding the short-time behaviour of the depressions is important for predicting jet formation in regions of high surface curvature.
A model for galloping detonations is conceived as a sequence of very fast re-ignitions followed by long periods of evolution with quenched reactions. Numerical simulations of the one-dimensional Euler equations are conducted in this limit. While the mean speed and structure is found in reasonable agreement with Chapman–Jouguet theory, very strong pulsations of the lead shock appear, along with a train of rear-facing N-waves. These dynamics are analysed using characteristics. A closed-form solution for the lead shock dynamics is formulated, which is found in excellent agreement with numerics. The model relies on the presence of a single time scale of the process, the pulsation period, which controls the shock dynamics via the shock change equations and establishes a shock decay with a single time constant. These long periods of shock decay with known dynamics are punctuated by energy release events, with ‘kicks’ in the shocked speed controlled by the pressure increase and resulting lead shock amplification. Model predictions are found in excellent agreement with previous numerical results of pulsating detonations far from the stability limit.
Paleontology provides insights into the history of the planet, from the origins of life billions of years ago to the biotic changes of the Recent. The scope of paleontological research is as vast as it is varied, and the field is constantly evolving. In an effort to identify “Big Questions” in paleontology, experts from around the world came together to build a list of priority questions the field can address in the years ahead. The 89 questions presented herein (grouped within 11 themes) represent contributions from nearly 200 international scientists. These questions touch on common themes including biodiversity drivers and patterns, integrating data types across spatiotemporal scales, applying paleontological data to contemporary biodiversity and climate issues, and effectively utilizing innovative methods and technology for new paleontological insights. In addition to these theoretical questions, discussions touch upon structural concerns within the field, advocating for an increased valuation of specimen-based research, protection of natural heritage sites, and the importance of collections infrastructure, along with a stronger emphasis on human diversity, equity, and inclusion. These questions offer a starting point—an initial nucleus of consensus that paleontologists can expand on—for engaging in discussions, securing funding, advocating for museums, and fostering continued growth in shared research directions.
This numerical investigation focuses on the mechanisms, flow topology and onset of Kelvin–Helmholtz instabilities (KHIs), that drive the leading-edge shear-layer destabilisation in the wake of wall-mounted long prisms. Large-eddy simulations are performed at ${\textit{Re}} = 2.5\times 10^3, 5\times 10^3$ and $1\times 10^4$ for prisms with a range of aspect ratio (AR, height-to-width) between $0.25$ and $1.5$, and depth ratios (DR, length-to-width) of $1{-}4$. Results show that shear-layer instabilities enhance flow irregularity and modulate spanwise vortex structures. The onset of KHI is strongly influenced by depth ratio, such that long prisms (${\textit{DR}}= 4$) experience earlier initiation compared with shorter ones (${\textit{DR}}= 1$). At higher Reynolds numbers, the onset of KHI shifts upstream towards the leading-edge, intensifying turbulence kinetic energy and increasing flow irregularity, especially for long prisms. The results further show that in this configuration, energy transfer from the secondary recirculation region contributes to the destabilisation of the leading-edge shear layer by reinforcing low-frequency modes. A feedback mechanism is identified wherein energetic flow structures propagate upstream through reverse boundary-layer flow, re-energising the leading-edge shear layer. Quantification using probability density functions reveals rare, intense upstream energy convection events, driven by this feedback mechanism. These facilitate the destabilisation process regardless of Reynolds number. This study provides a comprehensive understanding of the destabilisation mechanisms for leading-edge shear layers in the wake of wall-mounted long prisms.
Large-scale circulation involves the interaction of the lower and middle-upper troposphere, influencing synoptic-scale circulation, regional climate, teleconnections, and paleoclimate proxies. Described by the westerly vortex and jetstreams, the subtropical ridge, vortex asymmetry, and the South Pacific Split Jet, it is a framework for interpreting the natural archive and proxies. Southern and Northern Hemisphere pressure fields are described through planetary wave modes and zonal wave number indices. Anticyclone, cyclone, subtropical, mid-latitude, and subpolar storm-track and blocking climatologies and their influence on climate and hydrological change are presented. The chapter covers synoptic circulation, classical air-mass types, their source regions and temperature/humidity characteristics, and air-mass streamline trajectories; tropical depressions and cyclone storm tracks, easterly waves, blocking, and subtropical cyclones; mid-latitude synoptic systems including frontal lows, cut-off lows, and cold air outbreaks; and tropical–extratropical interaction with cloud bands, tropical–temperate troughs, atmospheric rivers, and warm-air incursions to the poles.
Undulatory slender objects have been a central theme in the hydrodynamics of swimming at low Reynolds number, where the slender body is usually assumed to be inextensible, although some microorganisms and artificial microrobots largely deform with compression and extension. Here, we theoretically study the coupling between the bending and compression/extension shape modes, using a geometrical formulation of kinematic microswimmer hydrodynamics to deal with the non-commutative effects between translation and rotation. By means of a coarse-grained minimal model and systematic perturbation expansions for small bending and compression/extension, we analytically derive the swimming velocities and report three main findings. First, we revisit the role of anisotropy in the drag ratio of the resistive force theory, and generally demonstrate that no motion is possible for uniform compression with isotropic drag. We then find that the bending–compression/extension coupling generates lateral and rotational motion, which enhances the swimmer’s manoeuvrability, as well as changes in progressive velocity at a higher order of expansion, while the coupling effects depend on the phase difference between the two modes. Finally, we demonstrate the importance of often-overlooked Lie bracket contributions in computing net locomotion from a deformation gait. Our study sheds light on compression as a forgotten degree of freedom in swimmer locomotion, with important implications for microswimmer hydrodynamics, including understanding of biological locomotion mechanisms and design of microrobots.
This chapter covers methods used to extract and interpret paleoclimate time series of climate modes, surface ocean, hydroclimate, and sea-level variability. The coral reef environment is explored as an archive of sea-surface temperature and salinity, hydroclimate, tradewinds, cloud cover and ocean circulation, storms, and regional and global sea-level variability, using stable isotopes, trace element analysis, radioisotopes, ultraviolet, and x-ray stratigraphic methods. The comparative tropical terrestrial hydroclimate record is investigated through the tree-ring and speleothem archive using traditional (dendrochronology and stable isotopes) and emerging methods such as biomarkers. Tropical hydroclimate reconstructions are presented, with the current understanding of decadal-scale variability due to the PDO/IPO. The coral and bivalve shell archive is presented as a record of boundary current, variability of continental shelf wind and current, and marine heat waves. Case studies reconstruct coastal jet modes and marine heat wave events for the Peruvian Current, Peru–Chile, and the Ningaloo Current, western Australia, in conjunction with ENSO variability during the Holocene.
Weather regime type and frequency are key diagnostics to interpret regional climate. The statistical methods used to downscale the centres of action in the mean atmospheric state to their family of weather regimes (WR) according to climate mode phases are presented in detail. The North Atlantic–European region is used as an example of WR decomposition of the mean climate. The chapter focuses on the identification of WR types for each region of the Southern Hemisphere and their spatio-temporal variability in relation to climate mode phase. These are the reference WRs for the interpretation of synoptic paleoclimate in each of the climate proxy chapters that follow. WRs are presented for the Maritime Continent, northern and central Australia, South Pacific Convergence Zone, Tasman Sea, New Zealand and southwest Pacific, eastern Pacific, Brazil to Uruguay, southwest Africa, southern Africa, eastern Africa, subtropical western Australia, southwestern Australia, southeastern Australia, the south Indian, south Pacific, and south Atlantic sectors of the Southern Ocean, and coastal Antarctica, including Patagonian South America, the Antarctic Peninsula, and the East Antarctic.
The unique reproductive strategies of botryllid ascidians, which include both asexual and sexual mechanisms as well as an extensive capacity for regeneration, contribute to their fast population growth and wide-ranging ecological effects. These colonial organisms have unique ecological adaptations and responses to environmental factors, yet comprehensive comparative studies on their environmental preferences remain scarce. We conducted an experimental study to explore the asexual reproduction and regeneration response of Botrylloides niger and Botryllus humilis colonies to varying salinity (36.5–39.5 PSU) and temperature (26 ± 1–30 ± 1°C) levels. Experimental findings highlighted species-specific preferences and stress responses: B. niger demonstrated higher tolerance to elevated salinity (39.5 PSU) with optimal growth rates at 26 ± 1–30 ± 1°C, whereas B. humilis displayed a preference for lower salinity and tendencies towards vascular budding at higher temperatures (30 ± 1°C). These observations suggest potential niche differentiation and ecological success, particularly in Mediterranean conditions, implying possible coexistence without intense competition in similar habitats. This research offers insights into the adaptive mechanisms of these ascidians, shedding light on their ecological roles and potential implications in coastal ecosystems amid changing environmental scenarios.
This chapter focuses on the glaciochemistry of Antarctic ice cores and their applications as aerosol tracers of atmospheric, sea ice, and oceanic variability. Marine aerosol–climate relationships are discussed using marine boundary layer, air–sea exchange, and cloud science. Glaciochemistry theory is presented for interpreting marine ion concentrations in ice cores as circumAntarctic wind-field and paleoweather tracers, sea ice extent, concentration, and polynya tracers. Similarly, non-marine aerosol ion glaciochemistry is examined, with applications including nitrate concentration as polar stratosphere and katabatic wind-field proxies; non-sea-salt sulphate as a volcanism proxy; and mineral dust as long-range air-mass tracers. Dust typing and mineral fingerprinting methods are discussed to identify Southern Hemisphere source areas. Air mass trajectory methods, both forward and backward, are presented to relate ice core ion glaciochemistry and dust particles as aerosol tracers to reconstruct large-scale atmospheric circulation, climate mode, and regional weather regime history during the interglacial and glacial periods.