60 research outputs found
Hydrogen-poor superluminous stellar explosions
Supernovae (SNe) are stellar explosions driven by gravitational or
thermonuclear energy, observed as electromagnetic radiation emitted over weeks
or more. In all known SNe, this radiation comes from internal energy deposited
in the outflowing ejecta by either radioactive decay of freshly-synthesized
elements (typically 56Ni), stored heat deposited by the explosion shock in the
envelope of a supergiant star, or interaction between the SN debris and
slowly-moving, hydrogen-rich circumstellar material. Here we report on a new
class of luminous SNe whose observed properties cannot be explained by any of
these known processes. These include four new SNe we have discovered, and two
previously unexplained events (SN 2005ap; SCP 06F6) that we can now identify as
members. These SNe are all ~10 times brighter than SNe Ia, do not show any
trace of hydrogen, emit significant ultra-violet (UV) flux for extended periods
of time, and have late-time decay rates which are inconsistent with
radioactivity. Our data require that the observed radiation is emitted by
hydrogen-free material distributed over a large radius (~10^15 cm) and
expanding at high velocities (>10^4 km s^-1). These long-lived, UV-luminous
events can be observed out to redshifts z>4 and offer an excellent opportunity
to study star formation in, and the interstellar medium of, primitive distant
galaxies.Comment: Accepted to Nature. Press embargoed until 2011 June 8, 18:00 U
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Modeling the influence of open water surfaces on the summertime temperature and thermal comfort in the city
Due to the combination of rapid global urbanization and climate change, urban climate issues are becoming relatively more important and are gaining interest. Compared to rural areas, the temperature in cities is higher (the urban heat island effect) due to the modifications in the surface radiation and energy balances. This study hypothesizes that the urban heat island can be mitigated by introducing open surface water in urban design. In order to test this, we use the WRF mesoscale meteorological model in which an idealized circular city is designed. Herein, the surface water cover, its size, spatial configuration, and temperature are varied. Model results indicate that the cooling effect of water bodies depends nonlinearly on the fractional water cover, size, and distribution of individual lakes within the city with respect to wind direction. Relatively large lakes show a high temperature effect close to their edges and in downwind areas. Several smaller lakes equally distributed within the urban area have a smaller temperature effect, but influence a larger area of the city. Evaporation from open water bodies may lower the temperature, but on the other hand also increases the humidity, which dampens the positive effect on thermal comfort. In addition, when the water is warmer than the air temperature (during autumn or night), the water body has an adverse effect on thermal comfort. In those cases, the water body eventually limits the cooling and thermal comfort in the surrounding city, and thus diverges from the original intention of the intervention
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How do green roofs mitigate urban thermal stress under heat waves?
As the climate warms, heat waves (HW) are projected to be more intense and to last longer, with serious implications for public health. Urban residents face higher health risks because urban heat islands (UHIs) exacerbate HW conditions. One strategy to mitigate negative impacts of urban thermal stress is the installation of green roofs (GRs) given their evaporative cooling effect. However, the effectiveness of GRs and the mechanisms by which they have an effect at the scale of entire cities are still largely unknown. The Greater Beijing Region (GBR) is modeled for a HW scenario with the Weather Research and Forecasting (WRF) model coupled with a state-of-the-art urban canopy model (PUCM) to examine the effectiveness of GRs. The results suggest GR would decrease near-surface air temperature (ΔT2max = 2.5 K) and wind speed (ΔUV10max = 1.0 m s-1) but increase atmospheric humidity (ΔQ2max = 1.3 g kg-1). GRs are simulated to lessen the overall thermal stress as indicated by apparent temperature (ΔAT2max = 1.7 °C). The modifications by GRs scale almost linearly with the fraction of the surface they cover. Investigation of the surface-atmosphere interactions indicate that GRs with plentiful soil moisture dissipate more of the surface energy as latent heat flux and subsequently inhibit the development of the daytime planetary boundary layer (PBL). This causes the atmospheric heating through entrainment at the PBL top to be decreased. Additionally, urban GRs modify regional circulation regimes leading to decreased advective heating under HW
Evaluation of a Photosynthesis-Based Canopy Resistance Formulation in the Noah Land-Surface Model
Surface Energy Balance Measurements Above an Exurban Residential Neighbourhood of Kansas City, Missouri
Serological epitope profile of anti-Ro52–positive patients with systemic autoimmune rheumatic diseases
Exploring, exploiting and evolving diversity of aquatic ecosystem models: a community perspective
Review of ostrich (Struthio carmelis) production and its adaptability to the Nigerian poultry industry
This paper reviewed the available literature on ostrich (Struthio carmelis) and ostrich farming. The, origin, physical and physiological characteristics, breeding, management, nutrition, diseases, ostrich products and adaptability in Nigerian poultry industry were discussed. Ostrich originated from the Saharan region and South Africa. It is a tall, herbivorous bird, weighing on the average, 115 kg for the male and 100 kg for the female. The male has penis, which can only be differentiated from the female’s clitoris at about 7 months of age. Ostrich has Long digestive tract, which is about 24 meters without a crop. It can digest high levels of fiber. During breeding season, onset of which depends on location, females lay about 50-100 eggs of 2.0-3.0 kg depending on type of habitat. In the wild, female and male both incubate the eggs during the day and night respectively, for about 42 days. Good number of ostrich can be found living in the wild (60,000 wild ostriches in Botswana). Domestication is made possible by captive ostriches and little breeding takes place in South Africa, U.S.A. and Australia. Nutrients requirements have not been established. This is taken presently, to be little below the requirements for turkey and diet is compounded as whole life cycle diet. Newcastle disease, cocciodiosis, microsporidiosis and osteomalacia affect ostrich. Meat, eggs, feathers and tendons are obtained from ostrich. In some countries, ostrich meat is in high demand because of its low fat and cholesterol content. There is limited literature on the Nigerian ostrich and its meat is not popular. Ostrich can be found in zoos and parks in Nigeria. Few commercial and demonstration farms can be found in the Northern parts of the country.Keywords: ostrich, poultry industry, nutrition, domestication, Nigeri
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Seasonal dependence of the urban heat island on the street canyon aspect ratio
In this article we study the relation between the urban heat island (UHI) in the urban canyon and street geometry, in particular the aspect ratio. Model results and observations show that two counteracting processes govern the relation between the nocturnal UHI and the building aspect ratio: i.e. trapping of long-wave radiation and shadowing effects. In general, trapping of long-wave radiation supports the UHI, whereas shadowing effects reduce the UHI. The net effect depends on the UHI definition and the amount of available short-wave radiation penetrating the canyon. In summer, autumn and spring the shadowing effects can already reduce the UHI starting at an aspect ratio between 0.5 and 1. The analysis is carried out using several methods. Firstly, the single-column model version of the Weather Research and Forecasting (WRF) model is used extensively. Two separate runs, one rural and one urban, are used to estimate the UHI. Secondly, the urban canyon temperature at the 2 m level is introduced, which allows for direct comparison between modelled and observed air temperatures within the urban canyon. Finally, the model is evaluated for all four seasons. The results of this research provide important insights for urban planning on how to use the aspect ratio to mitigate the UHI in the urban canyon
Evaluation of the ‘local climate zone’ scheme using temperature observations and model simulations
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