Near-infrared sky background fluctuations at mid- and low latitudes     

G. Moreels  J. Clairemidi  M. Faivre  D. Pautet  F. Rubio da Costa  P. Rousselot  J.W. Meriwether  G.A. Lehmacher  E. Vidal  J.L. Chau  G. Monnet 《Experimental Astronomy》2008,22(1-2):87-107

The emission of the upper atmosphere introduces an additional variable component into observations of astronomical objects in the NIR 700–3,000 nm range. The subtraction of this component is not easy because it varies during the night by as much as 100% and it is not homogeneous over the sky. A program aimed at measuring and understanding the main characteristics of the atmospheric NIR emission was undertaken. A 512?×?512 CCD camera equipped with a RG780/2 mm filter is used to obtain images of the sky in a 36°?×?36° field of view. The intensities of a given star and of the nearby region devoid of star in a 439 arcmin² area are monitored during periods of time of several hours. The sky intensity measured in the 754–900 nm bandpass, reduced to zenith and zero airmass is comprised between mag20 and mag18.5 per arcsecond². A diminution by a factor of two during the night is frequently observed. Intensity fluctuations having an amplitude of 15% and periods of 5–40 min are present in the images with a structure of regularly spaced stripes. The fluctuations of the NIR sky background intensity are due to (1) the chemical evolution of the upper atmosphere composition during the night and (2) dynamical processes such as tides with periods of 3–6 h or gravity waves with periods of several tens of minutes. We suggest that a monitoring of the sky background intensity could be set up when quantitative observations of astronomical objects require exposure times longer than ~10 min. The publication is illustrated with several video films accessible on the web site http://www.obs-besancon.fr/nirsky/. Enter username: nirsky and password: skynir.  相似文献   

Development of a fish-based index to assess the ecological quality of transitional waters: The case of French estuaries     

C. Delpech  A. Courrat  J. Lobry  D. Nicolas  M. Girardin 《Marine pollution bulletin》2010,60(6):908-233

The Water Framework Directive requires the assessment of the ecological status of transitional waters considering the fish component. An original methodology, based on a pressure-impact approach, was established to develop a multimetric fish-based index to characterize the ecological quality of French estuaries. An index of contamination, based on the chemical pollution affecting aquatic systems, was used as a proxy of anthropogenic pressure. The fish metric selection was based on their response to disturbances tested via statistical models (generalized linear models) taking into account sampling strategy and estuarine features. Four metrics, for which discriminating responses to level of pressure were demonstrated, were retained to constitute the estuarine multimetric fish index. This new tool appeared particularly relevant to detect the contamination effects on fish communities in estuaries. It could help managers to take decisions in order to maintain or reach the good status required by the Water Framework Directive for 2015.  相似文献   

Stable isotopes reveal food web modifications along the upstream–downstream gradient of a temperate stream     

Nicolas Hette-Tronquart  Jérôme Belliard  Evelyne Tales  Thierry Oberdorff 《Aquatic Sciences - Research Across Boundaries》2016,78(2):255-265

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Strong intrusions of the Northern Mediterranean Current on the eastern Gulf of Lion: insights from in-situ observations and high resolution numerical modelling     

Nicolas Barrier  Anne A. Petrenko  Yann Ourmières 《Ocean Dynamics》2016,66(3):313-327

The Northern Mediterranean Current is the return branch of the cyclonic circulation of the northwestern Mediterranean Sea. Because of geostrophic constraints, this warm and oligotrophic current is forced to flow westward along the continental slope of the Gulf of Lion. But, occasionally, it penetrates on the shelf and strongly impacts the local biogeochemistry and in turn the primary production. By combining in situ observations and high-resolution modelling, it is shown that intrusions on the eastern part of the gulf are mainly forced by easterly or northwesterly wind events, through physical mechanisms that are very different in nature. Easterlies induce a piling of water along the Gulf of Lion coast that drives, through geostrophy, an alongshore shelf-intruding current. This intrusive current occurs independently of the stratification and is concomitant with the wind forcing. On the other hand, intrusions due to northwesterlies only occur during stratified conditions and are related to the development of upwellings along the Gulf of Lion coasts. When the upwelling develops, a northwestward alongshore pressure force balances the Coriolis force associated with the onshore flow at depth. When the winds drop, the upwelling relaxes and the onshore flow weakens. Consequently, the Coriolis force no longer counterbalances the pressure force that ultimately dominates the momentum balance, causing the displacement of the Northern Current on the Gulf of Lion shelf approximately 1 day after the wind relaxation. This time lag between the northwesterlies decrease and the intrusions permits to anticipate possible changes in the biogeochemistry of the Gulf of Lion.  相似文献   

Filament Recognition and Image Cleaning on Meudon Hα Spectroheliograms     

Nicolas?FullerEmail author  Jean?Aboudarham  R.?D.?Bentley 《Solar physics》2005,227(1):61-73

This paper presents the techniques developed for the automated detection of filaments on Meudon H spectroheliograms, and, by extension, on any full-disk H Sun observations. Some cleaning processes are first applied to the images to correct them from defects characteristic of the instrument. Indeed, these defects may lead to spurious detections. From the cleaned images, filament areas are then segmented using a region growing method which efficiently returns the full extent of these dark areas. The filaments are finally described by means of their pruned skeleton. This representation allows one to compare the automatically segmented filaments with those manually recorded for Meudon Synoptic Maps. The very good agreement observed on a representative set of images confirms that this method can effectively be used in the frame of the EGSO (European Grid of Solar Observations) project in order to produce a reliable catalog dedicated to solar features.  相似文献   

Earthquakes in Switzerland and surrounding regions during 2003     

Nicolas Deichmann  Manfred Baer  Jochen Braunmiller  Cécile Cornou  Donat Fäh  Domenico Giardini  Monika Gisler  Sarah Huber  Stephan Husen  Philipp Kästli  Urs Kradolfer  Martin Mai  Silvio Maraini  Ivo Oprsal  Thomas Schler  Danijel Schorlemmer  Stefan Wiemer  Jochen Wössner  Adrian Wyss 《Eclogae Geologicae Helvetiae》2004,97(3):447-458

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EPR microplates, a model for the Oman Ophiolite     

F. Boudier  A. Nicolas  B. Ildefonse  D. Jousselin 《地学学报》1997,9(2):79-82

Structural mapping in the Southern half of the Oman ophiolite has revealed a palaeoridge organization with similarities to an EPR microplate, forming in superfast spreading conditions. A NW-trending propagator was rapidly opening in a lithosphere no more than 1 Myr older and itself created in a NE-SW ridge system. The NW-trending propagator, underlined by small mantle diapirs, was active or dying when detached as part of a future ophiolite. Local thrusting of the future ophiolite was also initiated very early, between 1 and 5 Myr after ridge accretion; it was accompanied by a 40° rotation within this time lapse. Such an activity supports the comparison of the Oman palaeoridge system with an oceanic microplate, and provides evidence to suggest the existence of thrusts at active microplates.  相似文献   

IO and Its Plasma Torus     

Nicolas Thomas 《紫金山天文台台刊》1996,(3)

A brief review of our courrent understanding of the interaction between the innermost Galilean satellite,Io,and Jupiter's magnetosphere is presented.Particular consideration is given to the neutral clouds and lo plasma torus which have been monitored by ground-based and Earth-orbiting observations for the past 25 years.Detailed investigation of observed phenomena in the neutral clouds has revealed several processes which have a direct bearing on the nature of the interaction and suggest that a revision of the existing concept is necessary.Similarly.observed variability in the torus indicates the presence of complex plasma processes which at present remain unexplained.Areas where further research is necessary are outlined.  相似文献   

Determination of mercury in seawater at sub-nanogram per liter levels     

Nicolas S. Bloom  Eric A. Crecelius 《Marine Chemistry》1983,14(1):49-59

Using a refined two-stage gold amalgamation preconcentration technique in conjunction with cold vapor atomic absorption (CVAA) detection, mercury in various Pacific Northwest coastal waters has been determined. Through the use of extremely clean reagents and special handling techniques, the blank has been reduced and reproducibility greatly improved for both “easily reducible mercury” and “total mercury”.Samples of unfiltered water, taken at the surface, as well as at 10 m, 100 m, and 175 m have all yielded “easily reducible mercury” at between 0.1 and 0.5 ng l^?1, and “total mercury” between 0.2 and 1.0 ng l^?1. Variability within replicate field samples is less than 10%, although variations of greater than 100% may be seen over a period of hours in Sequim Bay.  相似文献   

Along strike changes in the structural evolution over a brittle detachment fault: Example of the Pleistocene Corinth–Patras rift (Greece)     

Nicolas Flott  Denis Sorel  Carla Müller  Julien Tensi 《Tectonophysics》2005,403(1-4):77-94

The Patras, Corinth, and northern Saronic gulfs occupy a 200-km-long, N120° trending Pleistocene rift zone, where Peloponnese drifts away from mainland Greece. The axes of Patras and Corinth basins are 25 km apart and linked by two transfer-fault zones trending N040°. The older one defines the western slope of Panachaïkon mountain, and the younger one limits the narrow Rion–Patras littoral plain. Between these two faults, the ca. 4-km-thick Rion–Patras series dips 20–30° SSW. It is part of the Patras gulf synrift deposits, which pile in an asymmetric basin governed by a fault dipping ca. 25–35° NNE, located in the southern Gulf of Patras. Mapping of this fault to the east in northern Peloponnese shows that it is an inactive north-dipping low-angle normal fault (0° to 30°N), called the northern Peloponnese major fault (NPMF). The structural evolution of the NPMF was different in the gulfs of Patras and Corinth. In the Gulf of Patras, it is still active. In northern Peloponnese, footwall uplift and coeval southward tilting flattened the fault and locked its southern part. Steeper normal faults formed north of the locked area, connecting the still active northern part of the NPMF to the surface. After several locks, the presently active normal faults (Psathopyrgos, Aigion, Helike) trend along the southern shore of the Gulf of Corinth. This migration of faults caused the relative 25 km northward shift of the Corinth basin, and the formation of NE–SW trending transfer-faults between the Corinth and Patras gulfs.  相似文献