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Journal articleWeijer W, van Sebille E, 2014,
Impact of Agulhas Leakage on the Atlantic Overturning Circulation in the CCSM4
, JOURNAL OF CLIMATE, Vol: 27, Pages: 101-110, ISSN: 0894-8755- Author Web Link
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- Citations: 26
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Journal articleSiegert MJ, Makinson K, Blake D, et al., 2014,
An assessment of deep hot-water drilling as a means to undertake direct measurement and sampling of Antarctic subglacial lakes: experience and lessons learned from the Lake Ellsworth field season 2012/13
, ANNALS OF GLACIOLOGY, Vol: 55, Pages: 59-73, ISSN: 0260-3055 -
Conference paperLucquiaud M, Fernandez ES, Chalmers H, et al., 2014,
Enhanced operating flexibility and optimised off-design operation of coal plants with post-combustion capture
, 12th International Conference on Greenhouse Gas Control Technologies (GHGT), Publisher: ELSEVIER SCIENCE BV, Pages: 7494-7507, ISSN: 1876-6102- Author Web Link
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- Citations: 20
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Conference paperAlonso-Alvarez D, Fuehrer M, Thomas T, et al., 2014,
Elements of modelling and design of multi-quantum well solar cells
, 40th IEEE Photovoltaic Specialists Conference (PVSC), Publisher: IEEE, Pages: 2865-2870- Author Web Link
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- Citations: 3
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Journal articleRoss N, Jordan TA, Bingham RG, et al., 2014,
The Ellsworth Subglacial Highlands: Inception and retreat of the West Antarctic Ice Sheet
, GEOLOGICAL SOCIETY OF AMERICA BULLETIN, Vol: 126, Pages: 3-15, ISSN: 0016-7606- Author Web Link
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- Citations: 37
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Journal articleWright AP, Young DA, Bamber JL, et al., 2014,
Subglacial hydrological connectivity within the Byrd Glacier catchment, East Antarctica
, JOURNAL OF GLACIOLOGY, Vol: 60, Pages: 345-352, ISSN: 0022-1430- Author Web Link
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- Citations: 16
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Journal articleJones IL, Bull JW, Milner-Gulland EJ, et al., 2014,
Quantifying habitat impacts of natural gas infrastructure to facilitate biodiversity offsetting
, ECOLOGY AND EVOLUTION, Vol: 4, Pages: 79-90, ISSN: 2045-7758- Author Web Link
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- Citations: 24
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Journal articleSilverwood IP, Keyworth CW, Brown NJ, et al., 2014,
An Attenuated Total Reflection Fourier Transform Infrared (ATR FT-IR) Spectroscopic Study of Gas Adsorption on Colloidal Stearate-Capped ZnO Catalyst Substrate
, APPLIED SPECTROSCOPY, Vol: 68, Pages: 88-94, ISSN: 0003-7028 -
Journal articleHirst LC, Fujii H, Wang Y, et al., 2014,
Hot Carriers in Quantum Wells for Photovoltaic Efficiency Enhancement
, IEEE JOURNAL OF PHOTOVOLTAICS, Vol: 4, Pages: 244-252, ISSN: 2156-3381- Author Web Link
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- Citations: 73
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Journal articleLei Y, Hoskins B, Slingo J, 2014,
Natural variability of summer rainfall over China in HadCM3
, CLIMATE DYNAMICS, Vol: 42, Pages: 417-432, ISSN: 0930-7575- Author Web Link
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- Citations: 20
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Journal articleVisram AR, Cotter CJ, Cullen MJP, 2014,
A framework for evaluating model error using asymptotic convergence in the Eady model
, Quarterly Journal of the Royal Meteorological Society, Pages: n/a-n/a, ISSN: 0035-9009 -
Journal articleBoot-Handford ME, Abanades JC, Anthony EJ, et al., 2014,
Carbon capture and storage update
, Energy and Environmental Science, Vol: 7, Pages: 130-189, ISSN: 1754-5692In recent years, Carbon Capture and Storage (Sequestration) (CCS) has been proposed as a potential method to allow the continued use of fossil-fuelled power stations whilst preventing emissions of CO2 from reaching the atmosphere. Gas, coal (and biomass)-fired power stations can respond to changes in demand more readily than many other sources of electricity production, hence the importance of retaining them as an option in the energy mix. Here, we review the leading CO2 capture technologies, available in the short and long term, and their technological maturity, before discussing CO2 transport and storage. Current pilot plants and demonstrations are highlighted, as is the importance of optimising the CCS system as a whole. Other topics briefly discussed include the viability of both the capture of CO2 from the air and CO2 reutilisation as climate change mitigation strategies. Finally, we discuss the economic and legal aspects of CCS.
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Journal articleDaniels KA, Bastow ID, Keir D, et al., 2014,
Thermal models of dyke intrusion during development of continent–ocean transition
, Earth and Planetary Science Letters, Vol: 385, Pages: 145-153, ISSN: 0012-821XA consensus has emerged in recent years from a variety of geoscientific disciplines that extension during continental rifting is achieved only partly by plate stretching: dyke intrusion also plays an important role. Magma intrusion can accommodate extension at lower yield stresses than are required to extend thick, strong, unmodified continental lithosphere mechanically, thereby aiding the breakup process. Dyke intrusion is also expected to heat and thereby weaken the plate, but the spatial extent of heating and the effect of different rates of magmatic extension on the timescales over which heating occurs are poorly understood. To address this issue, a numerical solution to the heat-flow equation is developed here to quantify the thermal effects of dyke intrusion on the continental crust during rifting. The thermal models are benchmarked against a priori constraints on crustal structure and dyke intrusion episodes in Ethiopia. Finite difference models demonstrate that magmatic extension rate exerts a first-order control on the crustal thermal structure. Once dyke intrusion supersedes faulting and stretching as the principal extensional mechanism the crust will heat and weaken rapidly (less than 1 Ma).In the Main Ethiopian Rift (MER), the majority of present-day extension is focused on ∼20 km-wide Quaternary-Recent axial magmatic segments that are mostly seismogenic to mid-crustal depths and show P-wave seismic velocities characteristic of heavily intruded continental crust. When reviewed in light of our models, these observations require that no more than half of the MER's extension since ∼2 Ma has been achieved by dyke intrusion. Magmatic heating and weakening of the crust would have rendered it aseismic if dyke intrusion accounted for the entire 6 mm/yr extension rate. In the older, faster extending (16 mm/yr) Red Sea rift (RSR) in Afar, dyke intrusion is expected to have had a more dramatic impact on crustal rheology. Accordingly, effective elastic plate
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Journal articleD'Arcy M, Whittaker AC, 2014,
Geomorphic constraints on landscape sensitivity to climate in tectonically active areas
, Geomorphology, Vol: 204, Pages: 366-381The geomorphology of fluvial landscapes is known to record information about uplift rate, spatial patterns of faulting, and tectonic history. Data is far less available when addressing the sensitivity of common geomorphological metrics, such as channel steepness, to climatic boundary conditions. We test the relationship between channel steepness and precipitation rate by measuring a large number of channels in different mountainous areas. These regions exhibit a tenfold variation in precipitation rate between them (~ 100-1000 mm y- 1) but have similar uplift rates, allowing the tectonic variable to be controlled. By accounting for the orographic coupling of rainfall with uplifted topography, we find that channel steepness is significantly suppressed by higher precipitation rates in a measurable way that conforms to simple stream power erosion laws and empirical constraints on their parameters. We demonstrate this using modern and estimated glacial precipitation rates; and climate emerges as an important, quantifiable control on channel geometry. These findings help to explain why highly variable measurements of channel steepness are reported from different locations and provide important empirical constraints on how climate shapes tectonically active landscapes.
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Journal articleMcRae ATT, Cotter CJ, 2014,
Energy- and enstrophy-conserving schemes for the shallow-water equations, based on mimetic finite elements
, Quarterly Journal of the Royal Meteorological SocietyThis paper presents a family of spatial discretisations of the nonlinearrotating shallow-water equations that conserve both energy and potentialenstrophy. These are based on two-dimensional mixed finite element methods, andhence, unlike some finite difference methods, do not require an orthogonalgrid. Numerical verification of the aforementioned properties is also provided.
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Journal articleSkea J, 2014,
The renaissance of energy innovation
, ENERGY & ENVIRONMENTAL SCIENCE, Vol: 7, Pages: 21-24, ISSN: 1754-5692- Author Web Link
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- Citations: 10
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Journal articlePiper RB, Yoshida M, Farrell DJ, et al., 2014,
Kinetic insight into bimolecular upconversion: experiment and simulation
, RSC ADVANCES, Vol: 4, Pages: 8059-8063- Author Web Link
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- Citations: 16
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Journal articleChung D-W, Shearing PR, Brandon NP, et al., 2014,
Particle Size Polydispersity in Li-Ion Batteries
, JOURNAL OF THE ELECTROCHEMICAL SOCIETY, Vol: 161, Pages: A422-A430, ISSN: 0013-4651- Author Web Link
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- Citations: 83
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Journal articleWoodhouse E, McGowan P, Milner-Gulland EJ, 2014,
Fungal gold and firewood on the Tibetan plateau: examining access to diverse ecosystem provisioning services within a rural community
, ORYX, Vol: 48, Pages: 30-38, ISSN: 0030-6053- Author Web Link
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- Citations: 17
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Journal articleMoia D, Vaissier V, Lopez-Duarte I, et al., 2014,
The reorganization energy of intermolecular hole hopping between dyes anchored to surfaces
, CHEMICAL SCIENCE, Vol: 5, Pages: 281-290, ISSN: 2041-6520- Author Web Link
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- Citations: 54
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Journal articleGuerra C, Lanzini A, Leone P, et al., 2014,
Optimization of dry reforming of methane over Ni/YSZ anodes for solid oxide fuel cells
, JOURNAL OF POWER SOURCES, Vol: 245, Pages: 154-163, ISSN: 0378-7753- Author Web Link
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- Citations: 47
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Journal articleRios O, Jahn W, Rein G, 2014,
Forecasting wind-driven wildfires using an inverse modelling approach
, NATURAL HAZARDS AND EARTH SYSTEM SCIENCES, Vol: 14, Pages: 1491-1503, ISSN: 1561-8633- Author Web Link
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- Citations: 22
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Journal articleMargolin AR, Robinson LF, Burke A, et al., 2014,
Temporal and spatial distributions of cold-water corals in the Drake Passage: Insights from the last 35,000 years
, DEEP-SEA RESEARCH PART II-TOPICAL STUDIES IN OCEANOGRAPHY, Vol: 99, Pages: 237-248, ISSN: 0967-0645- Author Web Link
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- Citations: 28
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Journal articleRobinson LF, Adkins JF, Frank N, et al., 2014,
The geochemistry of deep-sea coral skeletons: A review of vital effects and applications for palaeoceanography
, DEEP-SEA RESEARCH PART II-TOPICAL STUDIES IN OCEANOGRAPHY, Vol: 99, Pages: 184-198, ISSN: 0967-0645- Author Web Link
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- Citations: 72
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Journal articleVandeginste V, John CM, Beckert J, 2014,
Diagenetic geobodies: Fracture-controlled burial dolomite bodies in outcrops from Northern Oman
, Society of Petroleum Engineers - International Petroleum Technology Conference 2014, IPTC 2014: Unlocking Energy Through Innovation, Technology and Capability, Vol: 2, Pages: 1142-1152Diagenetic heterogeneities are difficult to predict in subsurface. Nevertheless, such heterogeneities can be crucial in hydrocarbon exploration. Diagenetic processes can significantly alter petrophysical properties of reservoir rocks, especially in carbonate rocks because of the reactive nature of the carbonate minerals. Dolomitization, i.e. the transformation of calcite (limestone) into dolomite, is a common diagenetic process in carbonate rocks. Description: an overview of the learning outcomes gained by studying fracture-related dolomite in outcrops of Oman and subsequent laboratory analysis over the last four years. A combined structural, petrographic and geochemical approach was taken to study three dolomite systems occurring in different stratigraphic host rock intervals. Application: Structurally-controlled dolomitization (i.e. dolomitization along faults and fractures) typically occurs in burial conditions, and the resulting strong permeability anisotropies caused by the dolomite textures can cause major challenges for hydrocarbon exploration. Results and Conclusions: Dolomite bodies in the Precambrian Khufai Formation are related to N-S to NNE-SSW fractures, whereas dolomite bodies that mainly occur in the Jurassic host rocks occur along reactivated WNW-ESE normal faults. These fracture-related dolomite bodies are generally less than 15 m wide, but can be up to a few hundred meters long. Late-diagenetic dolomite bodies were also recognized in Permian host rocks, where they occur at or close to the contact between Permian limestone and early-diagenetic dolomite. This late diagenetic dolomite system can be traced laterally for at least hundreds of meters and occurs in wadi's about 40 km apart. Our data indicate that there were several dolomitization events in the geological history, generating dolomite bodies with different characteristics. Technical Contributions: This highlights the needs to understand the timing and structural setting of dolomite bodies in
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Journal articleJohn CM, Vandeginste V, Jourdan AL, et al., 2014,
Carbonate reservoir analogues and clumped isotopes: How combined geometries and geochemistry of outcrops help reservoir management in the Middle East
, Society of Petroleum Engineers - International Petroleum Technology Conference 2014, IPTC 2014: Unlocking Energy Through Innovation, Technology and Capability, Vol: 1, Pages: 533-539Petroleum geologists working in carbonate plays are facing two common and inter-connected challenges linked to optimizing production. First, constraining the geometry, spatial distribution and inter-connectivity of reservoir geobodies is crucial as these properties can control the permeability anisotropy of reservoirs zones. This is difficult to do at the inter-well scale due to the limited resolution of seismic methods (20 meters or higher) compared to the size of typical reservoir geobodies (tens of centimers to meters and higher) and the very heterogeneous nature of carbonate reservoirs. Furthermore, diagenetic transformations are very important in carbonate reservoirs. Being able to fingerprint the process and timing of diagenetic transformation is crucial to a correct assessement of the distribution of cemented zones in the subsurface. The issue of diagenesis is also important for organic matter maturation and the timing of oil migration, and therefore the second challenge faced by reservoir geologists in carbonate plays is one of constraining as well as possible the thermal history of the targeted basin. This paper reports on the results of a major long-term research effort that addresses some aspects of this double challenge in the Middle East, and that focused on novel isotopic methods to constrain the thermal history of carbonate phases in the context of the geometry of geobodies measured at the outcrop. Geological work under the Qatar Carbonates and Carbon Storage Centre (QCCSRC), funded jointly by Qatar Petroleum, Shell and the Qatar Science & Technology Park, has as its long-term research goals to improve characterization of subsurface anisotropies in carbonate reservoirs, notably for CCS operations. Copyright 2014, International Petroleum Technology Conference.
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Journal articleGraesvik J, Hallett JP, Trang QT, et al., 2014,
A quick, simple, robust method to measure the acidity of ionic liquids
, CHEMICAL COMMUNICATIONS, Vol: 50, Pages: 7258-7261, ISSN: 1359-7345- Author Web Link
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- Citations: 19
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Journal articleHollaender HM, Bormann H, Blume T, et al., 2014,
Impact of modellers' decisions on hydrological a priori predictions
, HYDROLOGY AND EARTH SYSTEM SCIENCES, Vol: 18, Pages: 2065-2085, ISSN: 1027-5606- Author Web Link
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- Citations: 20
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Journal articleParpas P, Wiesemann W, 2014,
Editorial to computational techniques in management science
, Computational Management Science, Vol: 11, Pages: 3-4, ISSN: 1619-697X -
Journal articleNuno A, Bunnefeld N, Milner-Gulland EJ, 2014,
Managing social-ecological systems under uncertainty: implementation in the real world
, ECOLOGY AND SOCIETY, Vol: 19, ISSN: 1708-3087- Author Web Link
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- Citations: 23
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