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A box and a Gaussian plume model including gas-phase photochemistry and with plume dispersion parameters estimated from the few available plume observations are proposed and used for evaluation of photochemical transformations of exhausts from a single subsonic transport aircraft. The effects of concentration inhomogeneities in the plume cross section on the photochemical sources and sinks in the plume are analyzed for various groups of compounds. The influence of these inhomogeneities on the rate and on the mass of ambient air entrainment into the plume are studied also by comparing the box and the Gaussian plume model simulations during the first hours of their life. Due to the enterance of HOX and NOX from ambient air into the plume with rates varying from the wind shear and turbulence conditions, the rate of emitted NOX oxidation in the plume is dependent on these and also on the background concentration levels of HOX and NOX. 相似文献
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I. L. Karol’ A. A. Kiselev V. A. Frol’kis 《Izvestiya Atmospheric and Oceanic Physics》2011,47(4):415-429
Radiative forcing, the global warming potential, and the recently proposed global temperature potential are widely used not only in scientific studies but also in a number of economic and political evaluations of the effects of an increase in the contents of greenhouse gases and aerosols and other factors that form climate and its changes. New indices have appeared, and, to calculate them, information is required on the quantitative characteristics of the climate system’s components—current and expected—within standard periods of 20, 100, and 500 years. The calculations of some of these indices and potentials require consideration for variations in the rate of energy exchange between the atmosphere and the underlying surface (ocean) within the indicated periods. This leads to a more general problem of analyzing the sensitivity of the climate system to external (radiative) forcing and its response to such a forcing for the conditions of both stationary (equilibrium) and nonstationary “greenhouse” climates. A brief review of the few existing studies of such a response is given. 相似文献
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I. L. Karol’ A. A. Kiselev E. L. Genikhovich S. S. Chicherin 《Izvestiya Atmospheric and Oceanic Physics》2013,49(5):461-478
The current state of studies on short-lived atmospheric constituents (greenhouse gases and aerosols) is reviewed. They have short atmospheric lifetimes (from several days to a few years) and can significantly affect the environment and climate. We propose reducing the emissions of these constituents as an alternative to the reduction of man-made carbon dioxide releases. We consider methane, hydrofluorocarbons, tropospheric ozone, and various aerosols (primarily, black carbon); discuss their atmospheric sources and destruction mechanisms; evaluate their content, atmospheric emissions, and climate impacts; and recommend efficient actions for the nearest future. 相似文献
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Karol Tylmann Jan A. Piotrowski Wojciech Wysota 《Boreas: An International Journal of Quaternary Research》2013,42(2):428-441
The glacial sediment succession exposed close to the southern margin of the Late Weichselian Scandinavian Ice Sheet in Poland reveals a mosaic consisting of isolated patches of heavily deformed deposits separated by areas lacking any visible evidence of deformation. In the studied outcrop, the subglacial deforming spots composed of outwash deposits intercalated with till stringers are about 2–10 m wide and 20–60 cm thick. They rest on outwash sediments and are covered by a basal till. Based on structural and textural characteristics, the deforming spots are interpreted as previous R‐channels filled with meltwater deposits. Lack of deformation in outwash sediment immediately beneath the deforming spots and in the intervening areas between the channels suggests that the ice‐bed was frozen and the deformation of the channel infill was facilitated by high pore‐water pressure arising because water drainage into the bed was impeded by permafrost. Channel infill deposits and the till immediately above were coevally deformed to a strain of less than 9. This study documents the possible co‐existence of deforming and stable areas under an ice sheet, generated by spatially varying thermal and hydrological conditions affecting sediment rheology. 相似文献
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Our aim is to introduce the Coupled Finite-Infinite Element Method (CFIEM) as a new alternative approach to the Earth’s gravity
field modelling. We show that if the computational domain is large enough in radial direction, one can obtain the qualitatively
and quantitatively comparable solution to the solution by the Finite Element Method (FEM). We study the influence of the size
of the computational domain on the final CFIEM solution as well as the successive refinement of the discretization and its
convergence to the exact solution. As an input data we use the synthetic boundary conditions computed from a Synthetic Earth
Gravity Model (SEGM) and we test the CFIEM solution by the data generated directly from SEGM and the solution by the FEM. 相似文献
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Karol Kozieł 《Earth, Moon, and Planets》1979,21(3):351-359
This paper presents historical stages of the development of methods concerning observation and theory of the Moon's rotation around its centre of mass from the beginning of the 17th century up to the present day. The accuracy and usefulness of these methods is estimated and a critical attitude is assumed towards the results concerning the values of constants of the Moon's physical libration. 相似文献
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Having applied the method of discriminant analysis to the TOMS data of satellite sounding of the total ozone content (TOC) in the March months of 1979–2008, the authors could make a new estimate of the TOC field variability in the Northern Hemisphere and interlongitudinal regularities of its changes under the action of climatic variability. The effects of temperature variations in the polar stratosphere, El Niño, and quasi-biennial oscillation (QBO) have proven comparable and reach 80 DU in some regions. The influence of the Arctic Oscillation (AO) reaches 40 DU. The regions of TOC variations and their location and dimensions change depending on the phases of QBO, AO, and El Niño-Southern Oscillation (ENSO). Three regions of increased TOC—over Europe, Eastern Siberia, and the Pacific Ocean—are formed in years with a warm stratosphere. A compensating TOC decrease takes place in the tropics and over Greenland. In the years of El Niño and the easterly QBO phase, the TOC increases over Europe and drops over the central Pacific, as well as to the south from 45° N. The AO controls the ozone growth over most of Eurasia at temperate latitudes and its weak drop over the Atlantic. It was impossible to obtain such quantitative estimates with the use of methods based on an independent analysis of the TOC series at individual points of the coordinate grid. Testing with the Monte Carlo method confirmed that the results obtained are significant with a probability of 95–99.9%. 相似文献
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