125 research outputs found
Early-time Spitzer observations of the type II-Plateau supernova, 2004dj
We present mid-infrared observations with the Spitzer Space Telescope of the
nearby type II-P supernova, SN 2004dj, at epochs of 89 to 129 days. We have
obtained the first mid-IR spectra of any supernova apart from SN 1987A. A
prominent [NiII] 6.64 micron line is observed, from which we deduce that the
mass of stable nickel must be at least 2.2e10(-4) Msun. We also observe the red
wing of the CO-fundamental band. We relate our findings to possible progenitors
and favour an evolved star, most likely a red supergiant, with a probable
initial mass between ~10 and 15 Msun.Comment: ApJ Letters (accepted
Spitzer measurements of atomic and molecular abundances in the Type IIP SN 2005af
We present results based on Spitzer Space Telescope mid-infrared (3.6-30
micron) observations of the nearby IIP supernova 2005af. We report the first
ever detection of the SiO molecule in a Type IIP supernova. Together with the
detection of the CO fundamental, this is an exciting finding as it may signal
the onset of dust condensation in the ejecta. From a wealth of fine-structure
lines we provide abundance estimates for stable Ni, Ar, and Ne which, via
spectral synthesis, may be used to constrain nucleosynthesis models.Comment: ApJ Letters (accepted
Impact of urban canopy meteorological forcing on aerosol concentrations
The regional climate model RegCM4 extended with the land surface model CLM4.5
was coupled to the chemistry transport model CAMx to analyze the impact of
urban meteorological forcing on surface fine aerosol (PM2.5)
concentrations for summer conditions over the 2001â2005 period, focusing on
the area of Europe. Starting with the analysis of the meteorological
modifications caused by urban canopy forcing, we found a significant increase
in urban surface temperatures (up to 2â3 K), a decrease of specific humidity (by
up to 0.4â0.6 gkgâ1), a reduction of wind speed (up to â1 msâ1) and an enhancement of vertical turbulent diffusion coefficient
(up to 60â70 m2sâ1).These modifications translated into significant changes in surface aerosol
concentrations that were calculated by a cascading experimental approach.
First, none of the urban meteorological effects were considered. Then, the
temperature effect was added, then the humidity and the wind, and finally, the
enhanced turbulence was considered in the chemical runs. This facilitated the
understanding of the underlying processes acting to modify urban aerosol
concentrations. Moreover, we looked at the impact of the individual aerosol
components as well. The urbanization-induced temperature changes resulted in
a decrease of PM2.5 by â1.5 to â2 ”gâmâ3, while decreased
urban winds resulted in increases by 1â2 ”gâmâ3. The enhanced
turbulence over urban areas resulted in decreases of PM2.5 by â2 ”gâmâ3. The combined effect of all individual impact depends on
the competition between the partial impacts and can reach up to â3 ”gâmâ3 for some cities, especially when the temperature impact was stronger
in magnitude than the wind impact. The effect of changed humidity was found
to be minor. The main contributor to the temperature impact is the
modification of secondary inorganic aerosols, mainly nitrates, while the wind
and turbulence impact is most pronounced in the case of primary aerosol (primary
black and organic carbon and other fine particle matter). The overall as well
as individual impacts on secondary organic aerosol are very small, with the
increased turbulence acting as the main driver. The analysis of the vertical
extent of the aerosol changes showed that the perturbations caused by urban
canopy forcing, besides being large near the surface, have a secondary
maximum for turbulence and wind impact over higher model levels, which is
attributed to the vertical extent of the changes in turbulence over urban
areas. The validation of model data with measurements showed good agreement,
and we could detect a clear model improvement in some areas when including
the urban canopy meteorological effects in our chemistry simulations.</p
Improved Laboratory Transition Probabilities for Neutral Chromium and Re-determination of the Chromium Abundance for the Sun and Three Stars
Branching fraction measurements from Fourier transform spectra in conjunction
with published radiative lifetimes are used to determine transition
probabilities for 263 lines of neutral chromium. These laboratory values are
employed to derive a new photospheric abundance for the Sun: log (Cr
I) = 5.640.01 (). These Cr I solar abundances do
not exhibit any trends with line strength nor with excitation energy and there
were no obvious indications of departures from LTE. In addition, oscillator
strengths for singly-ionized chromium recently reported by the FERRUM Project
are used to determine: log (Cr II) = 5.770.03 (). Transition probability data are also applied to the spectra of three
stars: HD 75732 (metal-rich dwarf), HD 140283 (metal-poor subgiant), and CS
22892-052 (metal-poor giant). In all of the selected stars, Cr I is found to be
underabundant with respect to Cr II. The possible causes for this abundance
discrepancy and apparent ionization imbalance are discussed.Comment: 44 pages, 6 figure
Measurement of the Depth of Maximum of Extensive Air Showers above 10^18 eV
We describe the measurement of the depth of maximum, Xmax, of the
longitudinal development of air showers induced by cosmic rays. Almost four
thousand events above 10^18 eV observed by the fluorescence detector of the
Pierre Auger Observatory in coincidence with at least one surface detector
station are selected for the analysis. The average shower maximum was found to
evolve with energy at a rate of (106 +35/-21) g/cm^2/decade below 10^(18.24 +/-
0.05) eV and (24 +/- 3) g/cm^2/decade above this energy. The measured
shower-to-shower fluctuations decrease from about 55 to 26 g/cm^2. The
interpretation of these results in terms of the cosmic ray mass composition is
briefly discussed.Comment: Accepted for publication by PR
- âŠ