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排序方式: 共有221条查询结果,搜索用时 15 毫秒
181.
182.
Ocean Dynamics - Für eine Bewertung des Zustands der Meeresumwelt sind die Richtigkeit und die Vergleichbarkeit der im marinen Monitoring erhobenen Daten wesentliche Voraussetzungen. Ein... 相似文献
183.
P. A. Curran R. L. C. Starling A. J. van der Horst R. A. M. J. Wijers 《Monthly notices of the Royal Astronomical Society》2009,395(1):580-592
The complex structure of the light curves of Swift Gamma-Ray Bursts (GRBs) has made the identification of breaks, and the interpretation of the blast wave caused by the burst, more difficult than in the pre- Swift era. We aim to identify breaks, which are possibly hidden, and to constrain the blast wave parameters; electron energy distribution, p , density profile of the circumburst medium, k , and the continued energy injection index, q . We do so by comparing the observed multiwavelength light curves and X-ray spectra of our sample to the predictions of the blast wave model. We can successfully interpret all of the bursts in our sample of 10, except two, within this framework and we can estimate, with confidence, the electron energy distribution index for 6 of the sample. Furthermore, we identify jet breaks in a number of the bursts. A statistical analysis of the distribution of p reveals that, even in the most conservative case of least scatter, the values are not consistent with a single, universal value. The values of k suggest that the circumburst density profiles are not drawn from only one of the constant density or wind-like media populations. 相似文献
184.
E. Bissaldi A. von Kienlin G. Lichti H. Steinle P. N. Bhat M. S. Briggs G. J. Fishman A. S. Hoover R. M. Kippen M. Krumrey M. Gerlach V. Connaughton R. Diehl J. Greiner A. J. van der Horst C. Kouveliotou S. McBreen C. A. Meegan W. S. Paciesas R. D. Preece C. A. Wilson-Hodge 《Experimental Astronomy》2009,24(1-3):47-88
One of the scientific objectives of NASA’s Fermi Gamma-ray Space Telescope is the study of Gamma-Ray Bursts (GRBs). The Fermi Gamma-Ray Burst Monitor (GBM) was designed to detect and localize bursts for the Fermi mission. By means of an array of 12 NaI(Tl) (8 keV to 1 MeV) and two BGO (0.2 to 40 MeV) scintillation detectors, GBM extends the energy range (20 MeV to > 300 GeV) of Fermi’s main instrument, the Large Area Telescope, into the traditional range of current GRB databases. The physical detector response of the GBM instrument to GRBs is determined with the help of Monte Carlo simulations, which are supported and verified by on-ground individual detector calibration measurements. We present the principal instrument properties, which have been determined as a function of energy and angle, including the channel-energy relation, the energy resolution, the effective area and the spatial homogeneity. 相似文献
185.
Horst Meesenburg 《GeoJournal》1996,39(2):143-151
This article describes the influence of man on the coastal landscapes along the Danish and part of the German west coast. While the tidal coast south of Blåvandshuk was formed by man since premedieval times, the northern part of Jutlands coast nearly avoided human influence until the late 19th century when dune plantation and coast protection was begun. At the same time, the first harbours were built by the Danish state, mainly for fishing purposes. The human influence increased through the 20th century, with tourism as a main factor. The article highlights the radical changes and the fragile balance between human action and natural processes on a debris coast. The article summarizes some of the authors contributions in the Danish landscape magazine Bygd, of which he is editor. 相似文献
186.
Footprint estimation for scalar flux measurements in the atmospheric surface layer 总被引:12,自引:2,他引:12
The flux footprint is the contribution, per unit emission, of each element of a surface area source to the vertical scalar flux measured at height z
m
; it is equal to the vertical flux from a unit surface point source. The dependence of the flux footprint on crosswind location is shown to be identical to the crosswind concentration distribution for a unit surface point source; an analytic dispersion model is used to estimate the crosswind-integrated flux footprint. Based on the analytic dispersion model, a normalized crosswind-integrated footprint is proposed that principally depends on the single variable z/z
m
, where z is a measure of vertical dispersion from a surface source. The explicit dependence of the crosswind-integrated flux footprint on downwind distance, thermal stability and surface roughness is contained in the dependence of z on these variables. By also calculating the flux footprint with a Lagrangian stochastic dispersion model, it is shown that the normalized flux footprint is insensitive to the analytic model assumption of a self-similar vertical concentration profile.The National Center for Atmospheric Research is funded by the National Science Foundation. 相似文献
187.
188.
Horst R. Marschall Rainer Altherr Angelika Kalt Thomas Ludwig 《Contributions to Mineralogy and Petrology》2008,155(6):703-717
The boron isotopic composition of zoned tourmaline in two metasediments from the island of Syros, determined by secondary-ion
mass spectrometry (SIMS), reflects the sedimentary and metamorphic record of the rocks. Tourmaline from a silicate-bearing
marble contains small (≤20 μm) detrital cores with highly variable δ
11B values (−10.7 to +3.6‰), pointing to a heterogeneous protolith derived from multiple sources. The sedimentary B isotopic
record survived the entire metamorphic cycle with peak temperatures of ∼500°C. Prograde to peak metamorphic rims are homogeneous
and similar among all analysed grains (δ
11B ≈ +0.9‰). The varying δ
11B values of detrital cores in the siliceous marble demonstrate that in situ B isotope analysis of tourmaline by SIMS is a
potentially powerful tool for provenance studies not only in sediments but also in metasediments. A meta-tuffitic blueschist
bears abundant tourmaline with dravitic cores of detrital or authigenic origin (δ
11B ≈ −3.3‰), and prograde to peak metamorphic overgrowth zones (−1.6‰). Fe-rich rims, formed during influx of B-bearing fluids
under retrograde conditions, show strongly increasing δ
11B values (up to +7.7‰) towards the margins of the grains. The δ
11B values of metamorphic tourmaline from Syros, formed in mixed terrigenous–marine sediments, reflect the B signal blended
from these two different sources, and was probably not altered by dehydration during subduction. 相似文献
189.
190.