排序方式： 共有31条查询结果，搜索用时 281 毫秒
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P. A. MAYEWSKI T. BRACEGIRDLE I. GOODWIN D. SCHNEIDER N. A. N. BERTLER S. BIRKEL A. CARLETON M. H. ENGLAND J‐H. KANG A. KHAN J. RUSSELL J. TURNER I. VELICOGNA 《第四纪科学杂志》2015,30(5):391-395
Climate model results suggest that future climate change in Antarctica will be accompanied by continued strengthening and poleward contraction of the Southern Ocean westerly wind belt. Paleoclimate records suggest past changes in the westerly winds can be abrupt and that healing of the Antarctic ozone hole could lead to poleward contraction of the westerlies and increased meridional atmospheric transport of warm air regionally into Antarctica. An abrupt shift to more meridional circulation could lead to notable changes in moisture availability for extra‐Antarctic regions, increased Antarctic ice sheet disintegration and more rapid sea‐level rise. 相似文献
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Spatial autocorrelation in marine birds 总被引：1，自引：0，他引：1
DAVID C. SCHNEIDER 《Polar research》1990,8(1):89-97
All marine organisms exhibit some degree of spatial autocorrelation, which is the tendency for high (or low) densities to occur in proximity, rather than at random in the ocean. Autocorrelation occurs at scales ranging from the length of the organism to thousands of kilometres. Autocorrelation results from a wide variety of mechanisms, many of which act at characteristic scales. Consequently, some insight into causal mechanisms can be obtained from exploratory analysis of the scale and intensity of autocorrelation of abundance or behaviour, and the scale and intensity (coherence) of cross-correlation with environmental variables such as water temperature or prey abundance. This paper uses seabird counts along extended transects to illustrate standard measures of autocorrelation and cross-correlation. A brief discussion of exploratory and confirmatory analysis of autocorrelated data on marine birds follows. 相似文献
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Résumé Le débit de pointe de la crue annuelle de période de retour donnée T est estimé à l'aide de la formule QT=ATpSα pour le tronçon supérieur du cours d'eau Aar à l'amont de Berne. S représente la surface du bassin versant et ATα sont les paramètres du bassin. Le débit QT est déterminé sur la base des mesures faites en chaque station, après correction des courtes séries et des erreurs d'échantillonage éventuelles. Les paramètres AT et a sont calculés à partir d'une régression linéaire établie entre le logarithme des valeurs de QT et de S. Connaissant la relation qui lie l'abscisse curviligne l à la surface du bassin versant en un point quelconque du cours d'eau, la relation QT = QT(S) permet de déterminer le profil de la pointe de la crue annuelle de période T le long de la rivière: QT = QT(l). 相似文献
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The current study focuses on the application of a three-dimensional numerical model for the prediction of morphological bed changes. The sediment deposition in a reservoir during a 10-year-flood was investigated and the results of the simulation were validated with data derived from a physical model study. Because of the small grain sizes in the prototype, synthetic granulate was used in the physical model. The numerical computation domain was a reproduction of the physical model, including the grain sizes and the density of the particles, in order to ensure comparability. The CFD code SSIIM, which solves the RANS-equations in three-dimensions, was used for the simulations. The sediment transport in SSIIM is divided into suspended sediment transport, computed by solving the convection-diffusion equation, and bed-load transport, calculated by an empirical formula. The results of the numerical simulation correspond well to the results of the physical model study. The simulated location and the pattern of the sediment deposition in the reservoir are an accurate representation of the observed distribution in the physical model. 相似文献
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陆相盆地中的海侵层序特征:中欧盆地三叠系与松辽盆地白垩系对比研究 总被引：5，自引：0，他引：5
中欧盆地三叠系是典型的海陆过渡相沉积，松辽盆地白垩系是含有海侵事件记录的陆相河湖盆地。两盆地的共同特点是：①大陆克拉通上长期发育的大型坳陷盆地；②靠近古大洋和（或）有向海通道；③主要由互层状泥岩、粉砂岩、碳酸盐岩和膏盐层组成；④无典型海相化石，可能发育有半咸水和（或）高盐度生物；⑤海侵层中自生矿物的δ^34S,δ^13C,δ^18O同位素比值及介质盐度指数（Sr/Ba）、碱度指数（Ca Mg)／（Si Al）、还原性指标（Zn Ni)/Ga、硫沉积通量指数（归一化硫含量）等显著高于相邻层位背景值。 相似文献
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Pervasive early- to late-stage dolomitization of Lower Ordovician Ellenburger Group carbonates in the deep Permian Basin of west Texas and southeastern New Mexico is recorded in core samples having present-day burial depths of 1.5–7.0 km. Seven dolomite-rock textures are recognized and classified according to crystal-size distribution and crystal-boundary shape. Unimodal and polymodal planar-s (subhedral) mosaic dolomite is the most widespread type, and it replaced allochems and matrix or occurs as void-filling cement. Planar-e (euhedral) dolomite crystals line pore spaces and/or fractures, or form mosaics of medium to coarse euhedral crystals. This kind of occurrence relates to significant intercrystalline porosity. Non-planar-a (anhedral) dolomite replaced a precursor limestone/dolostone only in zones that are characterized by original high porosity and permeability. Non-planar dolomite cement (saddle dolomite) is the latest generation and is responsible for occlusion of fractures and pore space. Dolomitization is closely associated with the development of secondary porosity; dolomitization pre-and post-dates dissolution and corrosion and no secondary porosity generation is present in the associated limestones. The most common porosity types are non-fabric selective moldic and vuggy porosity and intercrystalline porosity. Up to 12% effective porosity is recorded in the deep (6477 m) Delaware basin. These porous zones are characterized by late-diagenetic coarse-crystalline dolomite, whereas the non-porous intervals are composed of dense mosaics of early-diagenetic dolomites. The distribution of dolomite rock textures indicates that porous zones were preserved as limestone until late in the diagenetic history, and were then subjected to late-stage dolomitization in a deep burial environment, resulting in coarse-crystalline porous dolomites. In addition to karst horizons at the top of the Ellenburger Group, exploration for Ellenburger Group reservoirs should consider the presence of such porous zones within other Ellenburger Group dolomites. 相似文献
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The effect of egg volume on body mass, body composition and growth rate in arctic tern Sterna paradisaea chicks was studied at Ny-Ålesund, on Svalbard (78°55'N, 12°00'E), in order to investigate whether differences in egg size influence the physiological characteristics of the hatchlings. The relative content of yolk and albumen in eggs did not vary in proportion to egg volume. Hatchlings from large eggs had larger body masses than hatchlings from small eggs, with 71% of the overall variation in body mass accounted for egg volume. In newly-hatched chicks, water content, lean body and total lipid mass, as well as both leg and pectoral muscles, changed isometrically in proportion to egg volume. Hatchlings from large eggs, however, had disproportionately larger yolk sacs. The leg muscles of small chicks contained a lower proportion of water than the leg muscles of large chicks, indicating that the leg muscles of small hatchlings were functionally more mature. There was a weak, but significant, correlation between egg volume and growth rate. However, a residual analysis made to eliminate the effect of egg volume showed no correlation between hatchling body mass and growth rate. The results of the present study show that Arctic tern hatchlings from large eggs emerge with more yolk sac reserves, enabling them to better withstand periods of food-scarcity. During embryonic growth in small eggs, however, there seems to be a greater relative usage of yolk, resulting in a more developed leg musculature. This may partly compensate for the higher mass-specific heat loss in small hatchlings. 相似文献
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