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741.
Christian Saad Salaheddine El Adlouni André St-Hilaire Philippe Gachon 《Stochastic Environmental Research and Risk Assessment (SERRA)》2015,29(1):275-294
Floods have potentially devastating consequences on populations, industries and environmental systems. They often result from a combination of effects from meteorological, physiographic and anthropogenic natures. The analysis of flood hazards under a multivariate perspective is primordial to evaluate several of the combined factors. This study analyzes spring flood-causing mechanisms in terms of the occurrence, frequency, duration and intensity of precipitation as well as temperature events and their combinations previous to and during floods using frequency analysis as well as a proposed multivariate copula approach along with hydrometeorological indices. This research was initiated over the Richelieu River watershed (Quebec, Canada), with a particular emphasis on the 2011 spring flood, constituting one of the most damaging events over the last century for this region. Although some work has already been conducted to determine certain causes of this record flood, the use of multivariate statistical analysis of hydrologic and meteorological events has not yet been explored. This study proposes a multivariate flood risk model based on fully nested Archimedean Frank and Clayton copulas in a hydrometeorological context. Several combinations of the 2011 Richelieu River flood-causing meteorological factors are determined by estimating joint and conditional return periods with the application of the proposed model in a trivariate case. The effects of the frequency of daily frost/thaw episodes in winter, the cumulative total precipitation fallen between the months of November and March and the 90th percentile of rainfall in spring on peak flow and flood duration are quantified, as these combined factors represent relevant drivers of this 2011 Richelieu River record flood. Multiple plausible and physically founded flood-causing scenarios are also analyzed to quantify various risks of inundation. 相似文献
742.
743.
The POM-DOM piezophilic microorganism continuum(PDPMC)—The role of piezophilic microorganisms in the global ocean carbon cycle 总被引:1,自引:0,他引:1
FANG JiaSong ZHANG Li LI Jiang Tao Chiaki KATO Christian TAMBURINI ZHANG YuZhong DANG HongYue WANG GuangYi WANG FengPing 《中国科学:地球科学(英文版)》2015,(1):106-115
The deep ocean piezosphere accounts for a significant part of the global ocean,hosts active and diverse microbial communities which probably play a more important role than hitherto recognized in the global ocean carbon cycle.The conventional biological pump concept and the recently proposed microbial carbon pump mechanism provide a foundation for our understanding of the role of microorganisms in cycling of carbon in the ocean.However,there are significant gaps in our knowledge and a lack of mechanistic understanding of the processes of microbially-mediated production,transformation,degradation,and export of marine dissolved and particulate organic matter(DOM and POM)in the deep ocean and the ecological consequence.Here we propose the POM-DOM piezophilic microorganism continuum(PDPMC)conceptual model,to address these important biogeochemical processes in the deep ocean.We propose that piezophilic microorganisms(bacteria and archaea)play a pivotal role in deep ocean carbon cycle where microbial production of exoenzymes,enzymatic breakdown of DOM and transformation of POM fuels the rapid cycling of marine organic matter,and serve as the primary driver for carbon cycle in the deep ocean. 相似文献
744.
Tristan Garcia Gilbert Féraud Christophe Falguères Henry de Lumley Christian Perrenoud David Lordkipanidze 《Quaternary Geochronology》2010,5(4):443-451
Several hominid remains have been discovered in the open-air site of Dmanisi (Georgia), the oldest prehistoric site in Eurasia. Two major arguments prove that this site is close in age to the Plio-Pleistocene boundary: a Villafranchian fauna and the morphological characteristics of hominid remains recently ascribed to Homo georgicus. Direct dating of the lower hominid-bearing level was carried out on volcanic glass and minerals using the 40Ar/39Ar method. The concordant results from two different sampled locations allow the determination of the age of the earliest human presence in Eurasia. This radioisotopic result strengthens the argument that the first dispersal of hominids outside Africa occurred at least 1.8 Ma ago. 相似文献
745.
Stephanie Kastner Christian Ohlendorf Torsten Haberzettl Andreas Lücke Christoph Mayr Nora I. Maidana Frank Schäbitz Bernd Zolitschka 《Journal of Paleolimnology》2010,44(4):887-902
We studied the internal lake processes that control the spatial distribution and characteristics of modern sediments at the
ICDP (International Continental Scientific Drilling Program) deep drilling site in Laguna Potrok Aike, southern Patagonia,
Argentina. Sediment distribution patterns were investigated using a dense grid of 63 gravity cores taken throughout the lake
basin and 40 additional shoreline samples. Analysis of the surficial sediment distribution points to distinct internal depositional
dynamics induced by wind-driven lake internal currents. Distribution maps illustrate that the spatial characteristics of analysed
variables are linked to high erosional wave activity. Persistent wave action and littoral erosion along all shores, especially
the eastern shore, is caused by prevailing Southern Hemispheric Westerlies. Several sediment variables (grain size, benthic
diatoms, total inorganic carbon and calcium) indicate re-suspension of littoral sediment followed by re-distribution to profundal
accumulation areas near the eastern shore. Variations within the catchment influence sediment characteristics in the north-eastern
bay. That area is characterized by different mineralogical and sedimentological conditions as well as greater accumulation
of pollen, inorganic carbon and diatoms. These findings are related to the influence of episodic inflow into this bay. Spatial
differences in stable isotope values throughout the lake suggest that ephemeral tributaries around the lake basin may also
contribute to the detected spatial sediment variations. 相似文献
746.
Snow cover strongly influences plant growth in Arctic and alpine ecosystems. Snow characteristics and snowmelt timing are likely to change in a warmer climate. We studied year rings and shoot growth of the dwarf shrub bilberry ( Vaccinium myrtillus ), and species abundances of the vegetation, in response to early or late snowmelt at a study site in the Central Alps, near Davos, Switzerland. Snowmelt was manipulated on experimental plots for 3 and 30 years. Additional plots were set up along a natural snowmelt gradient, and at high and low elevation. Growth ring data showed an increasing trend in annual growth increment over the last 20 years, especially in the extraordinarily hot summer of 2003. Comparing high and low elevation sites, growth rings were wider at low elevation, but only in cold years. In years with relatively cold summers, however, xylem ring width was greater in plots with late rather than early snowmelt along the natural snowmelt gradient, possibly indicating drought stress in early snowmelt plots. Snow cover had a strong influence on species abundances along the natural snowmelt gradient, and change (not yet significant) was beginning to be seen in plots with 30 years of snow manipulation. Our results indicate that beneficial effects of early snowmelt for shrub growth may be offset in cold summers. Although early snowmelt prolongs the growing season, harsh conditions and frost events early in the growing season may become more likely, and hamper plant growth, and this could affect plant growth in all Arctic and alpine snow-dominated ecosystems. 相似文献
747.
Christian Poppeliers 《Mathematical Geosciences》2009,41(7):761-777
This paper presents a scheme to invert reflected seismic wave fields for vertical spatial statistics of the Earth’s continuous
stochastic velocity distribution. The forward model is based on a single scattering theory, where a seismogram is modeled
as a convolution of a source wavelet and stochastic reflectivity, which obeys a von Kármán autocorrelation function. Tests
with synthetic data indicate that the method presented here recovers vertical characteristic length from seismic reflection
data that is similar to that of the original velocity model; however, the inversion does not reliably recover the Hurst exponent,
ν. The input wavelet’s power spectrum is a free parameter in the inversion and is estimated as well, but is band-limited relative
to the original source wavelet. Noise degrades the quality of the estimates of the stochastic parameters such that the recovered
stochastic parameters are biased according to the power spectrum of the noise. 相似文献
748.
Christian Creixell Miguel Ángel Parada Diego Morata Pierrick Roperch César Arriagada 《International Journal of Earth Sciences》2009,98(1):177-201
Five mafic dike swarms between 30° and 33°45′S were studied for their geochemical signature and kinematics of magma flow directions
by means of AMS data. In the Coastal Range of central Chile (33°−33°45′S), Middle Jurassic dike swarms (Concón and Cartagena
dike swarms, CMDS and CrMDS, respectively) and an Early Cretaceous dike swarm (El Tabo Dike Swarm, ETDS) display the presence
of dikes of geochemically enriched (high-Ti) and depleted (low-Ti) basaltic composition. These dikes show geochemical patterns
that are different from the composition of mafic enclaves of the Middle Jurassic Papudo-Quintero Complex, and this suggests
that the dikes were injected from reservoirs not related to the plutonic complex. The mantle source appears to be a depleted
mantle for Jurassic dikes and a heterogeneous-enriched lithospheric mantle for Cretaceous dikes. In the ETDS, vertical and
gently plunging magma flow vectors were estimated for enriched and depleted dikes, respectively, which suggest, together with
variations in dike thickness, that reservoirs were located at different depths for each dike family. In the Elqui Dike Swarm
(EDS) and Limarí Mafic Dike Swarm (LMDS), geochemical patterns are similar to those of the mafic enclaves of the Middle Jurassic
plutons. In the LMDS, east to west magma flow vectors are coherent with injection from neighbouring pluton located to the
east. In the EDS, some dikes show geochemical and magma flow patterns supporting the same hypothesis. Accordingly, dikes do
not necessarily come from deep reservoir; they may propagate in the upper crust from coeval shallow pluton chamber.
Electronic supplementary material The online version of this article (doi:) contains supplementary material, which is available to authorized users. 相似文献
749.
Horst R. Marschall Christian Meyer Bernd Wunder Thomas Ludwig Wilhelm Heinrich 《Contributions to Mineralogy and Petrology》2009,158(5):675-681
Tourmaline synthesised in an experiment with low boron excess was analysed in situ by secondary ion mass spectrometry. It
revealed significant B isotope zonation with 11B/10B ratios increasing in the growth direction of the crystals. Trend, magnitude and absolute values strongly support results
from high-B-excess isotope fractionation experiments. Furthermore, the closed system B-isotopic evolution of the experimental
fluid was modelled by Rayleigh fractionation. The model results are in excellent agreement with the measured B-isotope composition
of the run-product fluid. Consequently, low-element-excess experiments are proposed as an ideal approach to determine fluid-solid
isotope fractionation factors for systems that are characterised by Rayleigh fractionation. 相似文献
750.
Denis Scholz Christian Mühlinghaus Augusto Mangini 《Geochimica et cosmochimica acta》2009,73(9):2592-695
We derive equations describing the evolution of the carbon and oxygen isotope composition of the bicarbonate in a calcite precipitating solution on the surface of a stalagmite using a classical Rayleigh approach. The combined effects of calcite precipitation, degassing of CO2 and the buffering effect of the water reservoir are taken into account. Whereas δ13C shows a progressive increase to a final constant value, δ18O shows an initial isotopic enrichment, which exponentially decays due to the buffering effect of the water reservoir. The calculated evolution is significantly different for both carbon and oxygen isotopes than derived in a recent paper [Dreybrodt W. (2008) Evolution of the isotopic composition of carbon and oxygen in a calcite precipitating H2O-CO2-CaCO3 solution and the related isotopic composition of calcite in stalagmites. Geochim. Cosmochim. Acta72, 4712-4724.].Furthermore, we discuss the isotopic evolution of the bicarbonate in the solution for long residence times on the stalagmite surface, i.e., for t→∞. The equilibrium isotope ratio of the bicarbonate is then determined by isotopic exchange between the cave atmosphere and the bicarbonate in the solution and can be calculated by equilibrium isotope fractionation. For strongly ventilated caves exchange with the cave atmosphere will result in higher δ13C and δ18O values than those observed in a pure Rayleigh distillation scenario, for sparsely ventilated caves it will result in lower δ13C and δ18O values. 相似文献