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211.
Karen M. Simon Thomas S. James Donald L. Forbes Alice M. Telka Arthur S. Dyke Joseph A. Henton 《Quaternary Research》2014
Thirty-six new and previously published radiocarbon dates constrain the relative sea-level history of Arviat on the west coast of Hudson Bay. As a result of glacial isostatic adjustment (GIA) following deglaciation, sea level fell rapidly from a high-stand of nearly 170 m elevation just after 8000 cal yr BP to 60 m elevation by the mid Holocene (~ 5200 cal yr BP). The rate of sea-level fall decreased in the mid and late Holocene, with sea level falling 30 m since 3000 cal yr BP. Several late Holocene sea-level measurements are interpreted to originate from the upper end of the tidal range and place tight constraints on sea level. A preliminary measurement of present-day vertical land motion obtained by repeat Global Positioning System (GPS) occupations indicates ongoing crustal uplift at Arviat of 9.3 ± 1.5 mm/yr, in close agreement with the crustal uplift rate inferred from the inferred sea-level curve. Predictions of numerical GIA models indicate that the new sea-level curve is best fit by a Laurentide Ice Sheet reconstruction with a last glacial maximum peak thickness of ~ 3.4 km. This is a 30–35% thickness reduction of the ICE-5G ice-sheet history west of Hudson Bay. 相似文献
212.
Chaitanya Akurathi Venkata Sai Vialard Jérôme Lengaigne Matthieu d’Ovidio Francesco Riotte Jean Papa Fabrice James Rathinam Arthur 《Ocean Dynamics》2021,71(11-12):1113-1139
Ocean Dynamics - We use satellite-derived currents and a Lagrangian approach to investigate the redistribution of the precipitation minus evaporation (P-E) and river freshwater inputs into Bay of... 相似文献
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214.
Arthur N. Strahler 《自然地理学》2013,34(1):1-27
Information used in systems is organized into a hierarchy of five levels, following W. H. Terjung; first, collected data; second, sets of morphological variables; third, flow systems of energy and matter; fourth, process-form systems; fifth, systems regulated by cybernetic feedback. System variables, rigorously defined by dimensional analysis, are grouped into four classes: A. dynamic variables related to energy force, and stress; B. mass-flow variables expressing rates of flow of matter; C. geometry variables describing size and form within systems; D. material-property variables, including environmental constants and regulator variables. The second level of systems analysis interrelates a set of morphological elements in a meaningful way in terms of system origin or function. Correlation and regression methods establish significant relationships among variables, which may be stated as empirical or rational equations based on field or laboratory observations. Open energy flow systems and open or closed material flow systems of the third level can be described by dimensionally correct equations or by schematic flow diagrams. Process-form systems of the fourth level are characterized by self-regulation through physical feedback loops. Cybernetic feedback characterizes the fifth level and links natural systems to those regulated or disturbed by human intervention. 相似文献
215.
Richard Arthur Reyment Isao Motoyama Miyuki Ota Yuichiro Tanaka 《Natural Resources Research》2008,17(3):187-195
A statistical analysis of two consecutive sequences of observations on radiolarian abundances in the western North Pacific,
by methods appropriate to data on the simplex (i.e., compositional data), show that although the overall graphical presentations
of the frequencies appear similar, there are substantial differences in the earlier part of each of the series. The results
of the multivariate analyses are used for identifying those species that contribute most to the analysis. A brief guide to
the mathematical properties of compositional data is given. 相似文献
216.
Evapotranspiration and canopy characteristics of two lodgepole pine stands following mountain pine beetle attack 总被引:1,自引:0,他引:1 下载免费PDF全文
Mathew G. Brown T. Andrew Black Zoran Nesic Vanessa N. Foord David L. Spittlehouse Arthur L. Fredeen Rebecca Bowler Nicholas J. Grant Philip J. Burton J. A. Trofymow Dominic Lessard Gesa Meyer 《水文研究》2014,28(8):3326-3340
Over the past decade, British Columbia (BC), has experienced the largest mountain pine beetle (MPB) outbreak on record. This study used the eddy‐covariance (EC) technique to examine the impact of the MPB attack on evapotranspiration (E) and associated canopy characteristics of two lodgepole pine stands with secondary structure (trees, saplings and seedlings surviving the attack) located in central BC. MPB‐06, an 85‐year‐old almost pure stand of pine trees, was first attacked in 2006, and by 2010, ~80% of the trees had been killed. MPB‐03, a 110‐year‐old stand with an overstory consisting of over 90% pine and a developed sub‐canopy, was first attacked in 2003 and by 2007 had > 95% pine canopy mortality. EC measurements began in August 2006 at MPB‐06 and in March 2007 at MPB‐03, and continued for four years. Annual total E ranged from 226 mm to 237 mm at MPB‐06, and from 280 to 297 mm at MPB‐03, showing relatively little year‐to‐year change at both sites over the four years. Increased E from the accelerated growth of the surviving vegetation (secondary structure, shrubs and herbs) compensated for reduction in E due to the death of the overstory. Monthly average daytime canopy conductance, the Priestley–Taylor (α), and the canopy–atmosphere decoupling coefficient (Ω) steadily increased during the growing season reaching approximate maximum values of 5 mm s?1, 0.75 and 0.12, respectively. Potential evapotranspiration was approximated using a vapour pressure deficit‐dependent α obtained at high soil water content. Calculated water deficits indicated some water‐supply limitation to the surviving trees and understory at both sites. Rates of root zone drainage during the growing season were low relative to precipitation. Copyright © 2013 John Wiley & Sons, Ltd. 相似文献
217.
Caroline Beghein J. Arthur Snoke Matthew J. Fouch 《Earth and Planetary Science Letters》2010,289(3-4):467-478
We present fundamental-mode Rayleigh-wave azimuthally anisotropic phase velocity maps obtained for the Great Basin region at periods between 16 s and 102 s. These maps offer the first depth constraints on the origin of the semi-circular shear-wave splitting pattern observed in central Nevada, around a weak azimuthal anisotropy zone. A variety of explanations have been proposed to explain this signal, including an upwelling, toroidal mantle flow around a slab, lithospheric drip, and a megadetachment, but no consensus has been reached. Our phase velocity study helps constrain the three-dimensional anisotropic structure of the upper mantle in this region and contributes to a better understanding of the deformation mechanisms taking place beneath the western United States. The dispersion measurements were made using data from the USArray Transportable Array. At periods of 16 s and 18 s, which mostly sample the crust, we find a region of low anisotropy in central Nevada coinciding with locally reduced phase velocities, and surrounded by a semi-circular pattern of fast seismic directions. Away from central Nevada the fast directions are ~ N–S in the eastern Great Basin, NW–SE in the Walker Lane region, and they transition from E–W to N–S in the northwestern Great Basin. Our short-period phase velocity maps, combined with recent crustal receiver function results, are consistent with the presence of a semi-circular anisotropy signal in the lithosphere in the vicinity of a locally thick crust. At longer periods (28–102 s), which sample the uppermost mantle, isotropic phase velocities are significantly reduced across the study region, and fast directions are more uniform with an ~ E–W fast axis. The transition in phase velocities and anisotropy can be attributed to the lithosphere–asthenosphere boundary at depths of ~ 60 km. We interpret the fast seismic directions observed at longer periods in terms of present-day asthenospheric flow-driven deformation, possibly related to a combination of Juan de Fuca slab rollback and eastward-driven mantle flow from the Pacific asthenosphere. Our results also provide context to regional SKS splitting observations. We find that our short-period phase velocity anisotropy can only explain ~ 30% of the SKS splitting times, despite similar patterns in fast directions. This implies that the origin of the regional shear-wave splitting signal is complex and must also have a significant sublithospheric component. 相似文献
218.
Eldo E. Ávila Rodrigo E. Bürgesser Nesvit E. Castellano Andrew B. Collier Rosa H. Compagnucci Arthur R.W. Hughes 《Journal of Atmospheric and Solar》2010,72(14-15):1114-1121
Satellite observations of cloud top temperature and lightning flash distribution are used to examine the relationship between deep convection and lightning activity over the tropical regions of the northern and southern hemispheres. In agreement with previous work, the analysis of the results shows that, in the summer of both hemispheres, the lightning activity in continental deep convective storms is more intense than that in marine deep convective storms by a factor of between 7 and 10. Furthermore, it was observed that on average the daily lightning rate per 1°×1° grid cell for the southern hemisphere (SH) is about 20% greater than that of the northern hemisphere (NH), which can be attributed to a larger fractional cover by deep convective clouds in the SH. By using a set of independent indicators, it is shown that deep convection and lightning activity over land are well correlated (with correlation coefficients of 0.8 and 0.6 for NH and SH, respectively). This suggests the capacity for observations to act as a possible method of monitoring continental deep convective clouds, which play a key role in regulating the Earth’s climate. Since lightning can be monitored easily from ground networks and satellites, it could be a useful tool for validating the performance of model convective schemes and for monitoring changes in climate parameters. 相似文献
219.
220.
The transport of woody debris from urban surfaces,through local urban waterways,to constriction and blockage risk locations is not well understood.Flume trials have identified debris and watercourse dimensions as influential factors on debris movement,and large woody debris movement has been traced in the natural rural environment using time series photography,active transponders,and field surveys.Using novel passive transponder technology,small woody debris has been traced through an urban case study watercourse to establish key influential factors on urban debris transport.Through incorporating urban debris transport detail into the source and deposition process,a complete picture of urban debris transport can be created,supporting effective culvert and trash screen design,watercourse maintenance and blockage risk assessment.This case study highlights that factors beyond watercourse depth and velocity are influential in debris movement within an urban watercourse.Debris dimension and source location upstream are shown to significantly affect the potential for debris to reach a downstream constriction,illustrating a possible distance limitation in nuisance flow debris blockage risk. 相似文献