Intra-week spatial-temporal patterns of crime

Since its original publication, routine activity theory has proven most instructive for understanding temporal patterns in crime. The most prominent of the temporal crime patterns investigated is seasonality: crime (most often assault) increases during the summer months and decreases once routine activities are less often outside. Despite the rather widespread literature on the seasonality of crime, there is very little research investigating temporal patterns of crime at shorter time intervals such as within the week or even within the day. This paper contributes to this literature through a spatial-temporal analysis of crime patterns for different days of the week. It is found that temporal patterns are present for different days of the week (more crime on weekends, as would be expected) and there is a spatial component to that temporal change. Specifically, aside from robbery and sexual assault at the micro-spatial unit of analysis (street segments) the spatial patterns of crime changed. With regard to the spatial pattern changes, we found that assaults and theft from vehicle had their spatial patterns change in predictable ways on Saturdays: assaults increased in the bar district and theft from vehicles increased in the downtown and recreational car park areas

The Early Nutritional Environment of Mice Determines the Capacity for Adipose Tissue Expansion by Modulating Genes of Caveolae Structure

While the phenomenon linking the early nutritional environment to disease susceptibility exists in many mammalian species, the underlying mechanisms are unknown. We hypothesized that nutritional programming is a variable quantitative state of gene expression, fixed by the state of energy balance in the neonate, that waxes and wanes in the adult animal in response to changes in energy balance. We tested this hypothesis with an experiment, based upon global gene expression, to identify networks of genes in which expression patterns in inguinal fat of mice have been altered by the nutritional environment during early post-natal development. The effects of over- and under-nutrition on adiposity and gene expression phenotypes were assessed at 5, 10, 21 days of age and in adult C57Bl/6J mice fed chow followed by high fat diet for 8 weeks. Under-nutrition severely suppressed plasma insulin and leptin during lactation and diet-induced obesity in adult mice, whereas over-nourished mice were phenotypically indistinguishable from those on a control diet. Food intake was not affected by under- or over-nutrition. Microarray gene expression data revealed a major class of genes encoding proteins of the caveolae and cytoskeleton, including Cav1, Cav2, Ptrf (Cavin1), Ldlr, Vldlr and Mest, that were highly associated with adipose tissue expansion in 10 day-old mice during the dynamic phase of inguinal fat development and in adult animals exposed to an obesogenic environment. In conclusion gene expression profiles, fat mass and adipocyte size in 10 day old mice predicted similar phenotypes in adult mice with variable diet-induced obesity. These results are supported by phenotypes of KO mice and suggest that when an animal enters a state of positive energy balance adipose tissue expansion is initiated by coordinate changes in mRNA levels for proteins required for modulating the structure of the caveolae to maximize the capacity of the adipocyte for lipid storage

Gyre formation in open and deep lacustrine embayments: the example of Lake Geneva, Switzerland

Numerical simulations were carried out to investigate gyres within open lacustrine embayments subjected to parallel-to-shore currents. In such embayments, gyre formation occurs due to flow separation at the embayment’s upstream edge. High momentum fluid from the mixing layer between the embayment and offshore flows into the embayment and produces recirculating flow. Systematic numerical experiments using different synthetic embayment configurations were used to examine the impact of embayment geometry. Geometries included embayments with different aspect ratios, depths and embayment corner angles. The magnitudes of the recirculation and turbulent kinetic energy (TKE) in the embayment vary significantly for angles in the range 40°–55°. Embayments with corner angles less than 50° have much stronger recirculation and TKE, other parameters remaining the same. The numerical findings are consistent with gyre formation observed in two embayments located in Lake Geneva, Switzerland, and thus help explain flow patterns recorded in lacustrine shoreline regions

Caveolins in the repair phase of acute renal failure after oxidative stress

Ischaemia-reperfusion and toxic injury are leading causes of acute renal failure (ARF). Both of these injury initiators use secondary mediators of damage in oxygen-derived free radicals. Several recent publications about ischaemia-reperfusion and toxin-induced ARF have indicated that plasma membrane structures called caveolae, and their proteins, the caveolins, are potential participants in protecting or repairing renal tissues. Caveolae and caveolins have previously been ascribed many functions, a number of which may mediate cell death or survival of injured renal cells. This review proposes possible pathophysiological mechanisms by which altered caveolin-1 expression and localization may affect renal cell survival following oxidative stress

Gas Transfer at Water Surfaces 2010

PrefaceSection 1: Interfacial Turbulence and Air-Water Scalar TransferJ. Hunt, S. Belcher, D. Stretch, S. Sajjadi, J. Clegg [1]S.A. Kitaigorodskii [13]S.A. Kitaigorodskii [29]Y. Toba [38]D. Turney, S. Banerjee [51]J.G. Janzen, H.E. Schulz, G.H. Jirka [65]S. Komori, R. Kurose, N. Takagaki, S. Ohtsubo, K. Iwano, K. Handa, S. Shimada [78]J. Beya, W. Peirson, M. Banner [90]S. Mizuno [104]M. Sanjou, I. Nezu, A. Toda [119]M. Sanjou, I. Nezu, Y. Akiya [129]K. Takehara, Y. Takano, T.G. Etoh [138]G. Caulliez [151]Section 2: Numerical Studies on Interfacial Turbulence and Scalar TransferL.-P. Hung, C.S. Garbe, W.-T. Tsai [165]A. E. Tejada-Martínez, C. Akan, C.E. Grosch [177]W.-T. Tsai, L.-P. Hung [193]P.G. Jayathilake, B.C. Khoo, Zhijun Tan [200]H.E. Schulz, A.L.A. Simões, J.G. Janzen [208]Section 3: Bubble-Mediated Scalar TransferD.P. Nicholson, S.R. Emerson, S. Khatiwala, R.C. Hamme [223]W. Mischler, R. Rocholz, B. Jähne [238]R. Patro, I. Leifer [249]K. Loh, K.B. Cheong, R. Uittenbogaard [262]N. Mori, S. Nakagawa [273]Section 4: Effects of Surfactants and Molecular Diffusivity on Turbulence and Scalar TransferA. Soloviev, S. Matt, M. Gilman, H. Hühnerfuss, B. Haus, D. Jeong, I. Savelyev, M. Donelan [285]S. Matt, A. Fujimura, A. Soloviev, S.H. Rhee [299]P. Vlahos, E.C. Monahan, B.J.Huebert, J.B. Edson [313]K.E. Richter, B. Jähne [322]X. Yan, W.L. Peirson, J.W. Walker, M.L. Banner [333]Section 5: Field MeasurementsP.M. Orton, C.J. Zappa, W.R. McGillis [343]U.Schimpf, L. Nagel, B. Jähne [358]C.L. McNeil, E.A. D'Asaro, J.A. Nystuen [368]D. Turk, B. Petelin, J.W. Book [377]M. Ribas-Ribas, A. Gómez-Parra, J.M. Forja [394]A. Rutgersson, A.-S. Smedman, E. Sahlée [406]H. Pettersson, K. K. Kahma, A. Rutgersson, M. Perttilä [420]Section 6: Global Air-Sea CO2 FluxesR. Wanninkhof, G.-H. Park, D.B. Chelton, C.M. Risien [431]N. Suzuki, S. Komori, M.A. Donelan [445]Y. Suzuki, Y. Toba [452]M.T. Johnson, C. Hughes, T.G. Bell, P.S. Liss [464]Section 7: Advanced Measuring TechniquesO. Tsukamoto, F. Kondo [485]R. Rocholz, S. Wanner, U. Schimpf, B. Jähne [496]B.C.G. Gonzalez, A.W. Lamon, J.G. Janzen, J.R. Campos, H.E. Schulz [507]E. Sahlée, K. Kahma, H. Pettersson, W.M. Drennan [516]D. Kiefhaber, R. Rocholz, G. Balschbach, B. Jähne [524]C.S. Garbe, A. Heinlein [535]Section 8: Environmental Problems Related to Air-Water Scalar TransferW.L. Peirson, G.A. Lee, C. Waite, P. Onesemo, G. Ninaus [545]Y.J. Choi, A. Abe, K. Takahashi [559]Y. Baba, K. Takahashi [571]R. Onishi, K. Takahashi, S. Komori [582][593]Turbulence and wave dynamics across gas-liquid interfacesThe calculation of the gas transfer between the ocean and atmosphereThe influence of wind wave breaking on the dissipation of the turbulent kinetic energy in the upper ocean and its dependence on the stage of wind wave developmentMarvellous self-consistency inherent in wind waves : Its origin and some items related to air-sea transfersNear surface turbulence and its relationship to air-water gas transfer ratesTurbulent gas flux measurements near the air-water interface in an oscillating-grid tankSensible and latent heat transfer across the air-water interface in wind-driven turbulenceRainfall-generated, near-surface turbulenceEffects of the mechanical wave propagating in the wind direction on currents and stresses across the air-water interfaceTurbulent transport in closed basin with wind-induced water wavesPIV measurements of Langumuir circulation generated by wind-induced water wavesStudy of vortices near wind wave surfaces using high-speed video camera and MLSWind wave breaking from micro to macroscaleValidation of Eddy-renewal model by numerical simulationMass transfer at the surface in LES of wind-driven shallow water flow with Langmuir circulationCharacteristics of gas-flux density distribution at the water surfacesNumerical simulation of interfacial mass transfer using the immersed interface methodStatistical approximations in gas-liquid mass transferAn inverse approach to estimate bubble-mediated air-sea gas flux from inert gas measurementsExperimental setup for the investigation of bubble mediated gas exchangeGas transfer velocity of single CO2 bubblesMass transfer across single bubblesAeration of surf zone breaking wavesModification of turbulence at the air-sea interface due to the presence of surfactants and implications for gas exchange. Part I: laboratory experimentModification of turbulence at the air-sea interface due to the presence of surfactants and implications for gas exchange. Part II: numerical simulationsWind-dependence of DMS transfer velocity: Comparison of model with recent southern ocean observationsA laboratory study of the Schmidt number dependency of air-water gas transferOn transitions in the Schmidt number dependency of low solubility gas transfer across air-water interfacesAn autonomous self-orienting catamaran (SOCa) for measuring air-water fluxes and forcingThe 2009 SOPRAN active thermography pilot experiment in the Baltic SeaObservations of air-sea exchange of N2 and O2 during the passage of Hurricane Gustav in the Gulf of Mexico during 2008The effect of high wind Bora events on water pCO2 and CO2 exchange in the coastal Northern AdriaticSeasonal sea-surface CO2 fugacity in the north-eastern shelf of the Gulf of Cádiz (southwest Iberian Peninsula)Including mixed layer convection when determining air-sea CO2 transfer velocityAir-sea carbon dioxide exchange during upwellingImpact of small-scale variability on air-sea CO2 fluxesThe effect of wind variability on the air-sea CO2 gas flux estimationFuture global mapping of air-sea CO2 flux by using wind and wind-wave distribution of CMIP3 multi-model ensembleA Rumsfeldian analysis of uncertainty in air-sea gas exchangeAccurate measurement of air-sea CO2 flux with open-path Eddy-CovarianceCombined Visualization of wind waves and water surface temperatureMicroscopic sensors for oxygen measurement at air-water interfaces and sediment biofilmsDamping of humidity fluctuations in a closed-path systemImproved Optical Instrument for the Measurement of Water Wave Statistics in the FieldFriction Velocity from Active Thermography and Shape AnalysisEvaporation mitigation by storage in rock and sandDevelopment of oil-spill simulation system based on the global ocean-atmosphere modelStructure variation dependence of tropical squall line on the tracer advection scheme in cloud-resolving modelHigh-resolution simulations for turbulent clouds developing over the oceAuthor Inde