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221.
Multiscale modeling of coastal, shelf, and global ocean dynamics 总被引:1,自引:1,他引:0
Pierre F. J. Lermusiaux Jens Schröter Sergey Danilov Mohamed Iskandarani Nadia Pinardi Joannes J. Westerink 《Ocean Dynamics》2013,63(11-12):1341-1344
222.
Viktor V. Korokhin Yuriy I. Velikodsky Yuriy G. Shkuratov Vadym G. Kaydash Sergey Y. Gerasimenko Nikolai V. Opanasenko Gorden Videen Carle Pieters 《Planetary and Space Science》2010,58(10):1298-1306
Lunar images acquired at non-zero phase angles show brightness variations caused by both albedo heterogeneities and local topographic slopes of the surface. To distinguish between these two factors, altimetry measurements or photoclinometry data can be used. The distinction is especially important for imagery of phase-function parameters of the Moon. The imagery is a new tool that can be used to study structural anomalies of the lunar surface. To illustrate the removal of the topographic effects from photometric images, we used Earth-based telescopic observations, altimetry measurements carried out with the Kaguya (JAXA) LALT instrument, and a new photoclinometry technique that includes analysis of several images of the same scenes acquired at different phase angles. Using this technique we have mapped the longitudinal component of lunar topography slopes (the component measured along the lines of constant latitude). We have found good correlations when comparing our map with the corresponding data from Kaguya altimetry. The removal of the topographic surface properties allows for the study of the phase-function parameters of the lunar surface, not only for flat mare regions, but for highlands as well. 相似文献
223.
Irina Molodtsova Sergey Bastrukov Kuan-Ting Chen Hsiang-Kuang Chang 《Astrophysics and Space Science》2010,327(1):1-7
In the context of white dwarf asteroseismology, we investigate the vibrational properties of a non-convective solid star with
an axisymmetric purely toroidal intrinsic magnetic field of two different shapes. Focus is laid on the regime of node-free
global Lorentz-force-driven vibrations about the symmetry axis at which material displacements have one and the same form
as those for nodeless spheroidal and torsional vibrations restored by Hooke’s force of elastic shear stresses. Particular
attention is given to the even-parity poloidal Alfvén modes whose frequency spectra are computed in analytic form, showing
how the purely toroidal magnetic fields completely buried beneath the star surface can manifest itself in seismic vibrations
of non-magnetic white dwarfs. The spectral formulae obtained are discussed in juxtaposition with those for Alfvén modes in
the solid star model with the poloidal, homogeneous internal and dipolar external, magnetic field whose inferences are relevant
to Alfvén vibrations in magnetic white dwarfs. 相似文献
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226.
Elie Verleyen Dominic A. Hodgson Koen Sabbe Holger Cremer Steven D. Emslie John Gibson Brenda Hall Satoshi Imura Sakae Kudoh Gareth J. Marshall Andrew McMinn Martin Melles Louise Newman Donna Roberts Steve J. Roberts Shiv M. Singh Mieke Sterken Ines Tavernier Sergey Verkulich Evelien Van de Vyver Wim Van Nieuwenhuyze Bernd Wagner Wim Vyverman 《Earth》2011,104(4):199-212
We review the post-glacial climate variability along the East Antarctic coastline using terrestrial and shallow marine geological records and compare these reconstructions with data from elsewhere. Nearly all East Antarctic records show a near-synchronous Early Holocene climate optimum (11.5–9 ka BP), coinciding with the deglaciation of currently ice-free regions and the optimum recorded in Antarctic ice and marine sediment cores. Shallow marine and coastal terrestrial climate anomalies appear to be out of phase after the Early Holocene warm period, and show complex regional patterns, but an overall trend of cooling in the terrestrial records. A Mid to Late Holocene warm period is present in many East Antarctic lake and shallow coastal marine records. Although there are some differences in the regional timing of this warm period, it typically occurs somewhere between 4.7 and 1 ka BP, which overlaps with a similar optimum found in Antarctic Peninsula terrestrial records. The differences in the timing of these sometimes abrupt warm events in different records and regions points to a number of mechanisms that we have yet to identify. Nearly all records show a neoglacial cooling from 2 ka BP onwards. There is no evidence along the East Antarctic coastline for an equivalent to the Northern Hemisphere Medieval Warm Period and there is only weak circumstantial evidence in a few places for a cool event crudely equivalent in time to the Northern Hemisphere's Little Ice Age. There is a need for well-dated, high resolution climate records in coastal East Antarctica and particularly in Terre Adélie, Dronning Maud Land and Enderby Land to fully understand the regional climate anomalies, the disparity between marine and terrestrial records, and to determine the significance of the heterogeneous temperature trends being measured in the Antarctic today. 相似文献
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228.
de la Vara Alba Cabos William Sein Dmitry V. Sidorenko Dmitry Koldunov Nikolay V. Koseki Shunya Soares Pedro M. M. Danilov Sergey 《Climate Dynamics》2020,54(11-12):4733-4757
Climate Dynamics - Despite the efforts of the modelling community to improve the representation of the sea surface temperature (SST) over the South Eastern Tropical Atlantic, warm biases still... 相似文献
229.
Sergey Oladyshkin Holger Class Rainer Helmig Wolfgang Nowak 《Computational Geosciences》2011,15(3):565-577
CO2 storage in geological formations is currently being discussed intensively as a technology with a high potential for mitigating
CO2 emissions. However, any large-scale application requires a thorough analysis of the potential risks. Current numerical simulation
models are too expensive for probabilistic risk analysis or stochastic approaches based on a brute-force approach of repeated
simulation. Even single deterministic simulations may require parallel high-performance computing. The multiphase flow processes
involved are too non-linear for quasi-linear error propagation and other simplified stochastic tools. As an alternative approach,
we propose a massive stochastic model reduction based on the probabilistic collocation method. The model response is projected
onto a higher-order orthogonal basis of polynomials to approximate dependence on uncertain parameters (porosity, permeability,
etc.) and design parameters (injection rate, depth, etc.). This allows for a non-linear propagation of model uncertainty affecting
the predicted risk, ensures fast computation, and provides a powerful tool for combining design variables and uncertain variables
into one approach based on an integrative response surface. Thus, the design task of finding optimal injection regimes explicitly
includes uncertainty, which leads to robust designs with a minimum failure probability. We validate our proposed stochastic
approach by Monte Carlo simulation using a common 3D benchmark problem (Class et al., Comput Geosci 13:451–467, 2009). A reasonable compromise between computational efforts and precision was reached already with second-order polynomials.
In our case study, the proposed approach yields a significant computational speed-up by a factor of 100 compared with the
Monte Carlo evaluation. We demonstrate that, due to the non-linearity of the flow and transport processes during CO2 injection, including uncertainty in the analysis leads to a systematic and significant shift of the predicted leakage rates
toward higher values compared with deterministic simulations, affecting both risk estimates and the design of injection scenarios. 相似文献
230.
An assessment of Arctic Ocean freshwater content changes from the 1990s to the 2006-2008 period 总被引:2,自引:0,他引:2
Benjamin Rabe Michael KarcherUrsula Schauer John M. TooleRichard A. Krishfield Sergey PisarevFrank Kauker Rüdiger GerdesTakashi Kikuchi 《Deep Sea Research Part I: Oceanographic Research Papers》2011,58(2):173-185
Unprecedented summer-season sampling of the Arctic Ocean during the period 2006-2008 makes possible a quasi-synoptic estimate of liquid freshwater (LFW) inventories in the Arctic Ocean basins. In comparison to observations from 1992 to 1999, LFW content relative to a salinity of 35 in the layer from the surface to the 34 isohaline increased by 8400±2000 km3 in the Arctic Ocean (water depth greater than 500 m). This is close to the annual export of freshwater (liquid and solid) from the Arctic Ocean reported in the literature.Observations and a model simulation show regional variations in LFW were both due to changes in the depth of the lower halocline, often forced by regional wind-induced Ekman pumping, and a mean freshening of the water column above this depth, associated with an increased net sea ice melt and advection of increased amounts of river water from the Siberian shelves. Over the whole Arctic Ocean, changes in the observed mean salinity above the 34 isohaline dominated estimated changes in LFW content; the contribution to LFW change by bounding isohaline depth changes was less than a quarter of the salinity contribution, and non-linear effects due to both factors were negligible. 相似文献