Bibliografías temáticas / Plateau region

Literatura académica sobre el tema "Plateau region"

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Publicado: 26 de julio de 2024
Última modificación: 27 de julio de 2024

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Artículos de revistas sobre el tema "Plateau region"

1

Xu, Weixin. "Precipitation and Convective Characteristics of Summer Deep Convection over East Asia Observed by TRMM". Monthly Weather Review 141, n.º 5 (1 de mayo de 2013): 1577–92. http://dx.doi.org/10.1175/mwr-d-12-00177.1.

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Abstract This study examines precipitation and convective characteristics of summer deep convection for five distinct regions (plateau, foothill, lowland, south China, and ocean) in East Asia using 13 yr of Tropical Rainfall Measuring Mission (TRMM)-based precipitation features. Every region has its own unique features in terms of elevation, rainfall amount, and dynamic/thermodynamic environments. Results show that large, deep convective systems contribute the majority of precipitation totals over all regions except the plateau. Mixed-phase precipitation processes are more important in the south China and the lowland regions than in the foothill and ocean regions. The plateau region also shows substantial dependence upon mixed-phase processes, though the mixed-phase region has a smaller depth than the other regions. Most metrics indicate that the south China region has the most intense storms, followed by the lowland, plateau, foothill, and ocean regions. However, ice scattering signatures do show that the ocean region is more “intense” than the foothill and plateau regions. Deep convective systems over the plateau are the smallest and ocean systems the largest, while storms over the foothill, lowland, and south China regions are in between. Alternatively, convective intensity (storm size) in all regions strengthens (decreases) from early summer to midsummer. Both regional and intraseasonal variations in convective intensity and morphology are mainly modulated by changes in the meteorological environment, such as the convective available potential energy, height of neutral buoyancy, total water vapor, and vertical wind shear.
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2

Glassman, Irvin. "Plateau region of composite propellants". Journal of Propulsion and Power 12, n.º 2 (marzo de 1996): 434–36. http://dx.doi.org/10.2514/3.24050.

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Luo, Jing, Jianqiu Zheng, Lei Zhong, Chun Zhao y Yunfei Fu. "The Phenomenon of Diurnal Variations for Summer Deep Convective Precipitation over the Qinghai-Tibet Plateau and Its Southern Regions as Viewed by TRMM PR". Atmosphere 12, n.º 6 (9 de junio de 2021): 745. http://dx.doi.org/10.3390/atmos12060745.

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This study analyzed the diurnal variations of summer deep convective precipitation (DCP) over the Qinghai-Tibet Plateau (QTP) and its southern region. The results show that DCP is the main type of precipitation over the QTP. The precipitation intensity of DCP is less than 3 mm/h over the QTP, which is much lower than the precipitation intensity in non-plateau regions. DCP over non-plateau regions is related to the convergence of surface wind, but that over the QTP are not. The mean maximum echo of DCP is less than 26 dBZ over the QTP, less than in non-plateau regions. The mean altitude of maximum echo decreases from about 7.5 km in the western plateau to 6 km in the eastern plateau, while it reaches only 4.5–5 km in the non-plateau region. The DCP frequency peak occurs in the afternoon in the major area of the QTP including valley region. The peak time of DCP frequency is different from its intensity, and the former is 1 to 2 h earlier. Study also indicates strong diurnal variations in frequency, intensity, and the maximum echo over the QTP, which is consistent with diurnal changes of geopotential height fields of 500 hPa and 200 hPa.
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4

Tane, Masakazu, Tae Kawashima, Keitaro Horikawa, Hidetoshi Kobayashi y Hideo Nakajima. "Dynamic Compression Behavior of Lotus-Type Porous Iron". Materials Science Forum 658 (julio de 2010): 193–96. http://dx.doi.org/10.4028/www.scientific.net/msf.658.193.

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Dynamic and quasi-static compression tests were conducted on lotus-type porous iron with porosity of about 50% using the split Hopkinson pressure bar method and universal testing machine, respectively. In the dynamic compression parallel to the pore direction, a plateau stress region appears where deformation proceeds at nearly constant stress, while the plateau stress region does not appear in the quasi-static compression. The plateau stress region is probably caused by the buckling deformation of matrix iron which occurs only in the dynamic compression. In contrast, the compression perpendicular to the orientation direction of pores exhibits no plateau-stress regions in the both dynamic and quasi-static compression.
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Asai, Fumi, Hiroshi Fukazawa y Koichi Kitazono. "Energy Absorption Efficiency of Open-Cell Carbon Foams". Materials Science Forum 933 (octubre de 2018): 323–29. http://dx.doi.org/10.4028/www.scientific.net/msf.933.323.

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Energy absorbing properties of open-cell carbon foams were evaluated by quasi-static and dynamic compression tests. Though carbon foams show brittle deformation behaviors, they have wide plateau region. The plateau stress linearly increases with increasing the relative density. Furthermore, the strain rate sensitivity is 0.03 and 0.15 at low and high strain rate region, respectively. Indentation tests were performed on cylindrical sample having porosity of 92.3 to 92.8% with different impact speeds. No plateau region is observed and macro cracks occur in the high speed indentation test. The energy absorption efficiency of carbon foams is higher than that of conventional aluminum foams because of their wide plateau regions.
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6

Sutton, Andrew, Adele Howe y L. Whitley. "Directed Plateau Search for MAX-k-SAT". Proceedings of the International Symposium on Combinatorial Search 1, n.º 1 (25 de agosto de 2010): 90–97. http://dx.doi.org/10.1609/socs.v1i1.18168.

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Local search algorithms for MAX-k-SAT must often explore large regions of mutually connected equal moves, or plateaus, typically by taking random walks through the region. In this paper, we develop a surrogate plateau "gradient" function using a Walsh transform of the objective function. This function gives the mean value of the objective function over localized volumes of the search space. This information can be used to direct search through plateaus more quickly. The focus of this paper is on demonstrating that formal analysis of search space structure can direct existing algorithms in a more principled manner than random walks. We show that embedding the gradient computation into a hill-climbing local search for MAX-k-SAT improves its convergence profile.
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Fujii, Toshiyuki, Shizuma Uju, Chihiro Watanabe, Susumu Onaka y Masaharu Kato. "Cyclic Deformation of Al-Mg Single Crystals with a Single Slip Orientation". Materials Science Forum 561-565 (octubre de 2007): 2213–16. http://dx.doi.org/10.4028/www.scientific.net/msf.561-565.2213.

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Fully reversed tension-compression fatigue tests were performed on solid-solutioned Al-0.7mass%Mg single crystals with a single slip orientation under constant plastic-strain amplitudes. Dislocation microstructures were quantitatively examined by transmission electron microscopy. The cyclic stress–strain curve (CSSC) exhibited three distinct regions with a short plateau region in the intermediate plastic-strain amplitude range, and the plateau stress was 26MPa. Characteristic microstructures were developed corresponding to the three regions in the CSSC. Vein structure was observed at the low strain-amplitude region. In the plateau regime, the persistent slip bands (PSBs) were observed. Labyrinth structure was also observed at the higher strain-amplitude region. The plateau stress, the cyclic flow stress of PSBs, can be explained by considering not only the Orowan bowing stress and the dipole passing stress of screw dislocations but also solid-solution hardening by Mg atoms.
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8

Oakley, J. C., P. C. Schwindt y W. E. Crill. "Dendritic Calcium Spikes in Layer 5 Pyramidal Neurons Amplify and Limit Transmission of Ligand-Gated Dendritic Current to Soma". Journal of Neurophysiology 86, n.º 1 (1 de julio de 2001): 514–27. http://dx.doi.org/10.1152/jn.2001.86.1.514.

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Long-lasting, dendritic, Ca2+-dependent action potentials (plateaus) were investigated in layer 5 pyramidal neurons from rat neocortical slices visualized by infrared-differential interference contrast microscopy to understand the role of dendritic Ca2+ spikes in the integration of synaptic input. Focal glutamate iontophoresis on visualized dendrites caused soma firing rate to increase linearly with iontophoretic current until dendritic Ca2+ responses caused a jump in firing rate. Increases in iontophoretic current caused no further increase in somatic firing rate. This limitation of firing rate resulted from the inability of increased glutamate to change evoked plateau amplitude. Similar nonlinear patterns of soma firing were evoked by focal iontophoresis on the distal apical, oblique, and basal dendrites, whereas iontophoresis on the soma and proximal apical dendrite only evoked a linear increase in firing rate as a function of iontophoretic current without plateaus. Plateau amplitude recorded in the soma decreased as the site of iontophoresis was moved farther from the soma, consistent with decremental propagation of the plateau to the soma. Currents arriving at the soma summed if plateaus were evoked on separate dendrites or if subthreshold responses were evoked from sites on the same dendrite. If plateaus were evoked at two sites on the same dendrite, only the proximal plateau was seen at the soma. Just-subthreshold depolarizations at two sites on the same dendrite could sum to evoke a plateau at the proximal site. We conclude that the plateaus prevent current from ligand-gated channels distal to the plateau-generating region from reaching the soma and directly influencing firing rate. The implications of plateau properties for synaptic integration are discussed.
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9

Deng, Min, Yong-Jian Wang, Yu Gang y Jian-Fei Chen. "Effect of uniaxial strain on the electronic transport through disordered graphene p–n junctions". Modern Physics Letters B 30, n.º 26 (30 de septiembre de 2016): 1650337. http://dx.doi.org/10.1142/s0217984916503371.

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Using the non-equilibrium Green’s function method, we investigated theoretically the electron transport through a disordered graphene p–n junction under a perpendicular magnetic field. A uniaxial strain is applied to the graphene sheet. It is found that the conductance versus the on-site energy of the right electrode exhibits the successive step-like structure in the n–n region, however, a zero value plateau followed by the successive oscillation peaks in the p–n region. When the longitudinal or transverse strain is applied, the zero value plateau almost remains intact, while the oscillation peaks are greatly enhanced with increasing the strain strength, and depending on the orientation of the applied strain, the oscillation peaks shift towards the positive or negative energy upon increasing the strain. In the presence of the disorder, the characteristic conductance plateaus emerge at [Formula: see text], [Formula: see text], etc. for the appropriate disorder strength. With the rise of the strain, the original plateau structure is destroyed, instead, the conductance exhibits new plateaus whose amplitude and position strongly depend on the strain strength and direction.
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10

Konikov, Yu V. y V. N. Oraevskii. "Hydrodynamic equations for a plasma in the region of the distribution-function plateau". Journal of Plasma Physics 42, n.º 2 (octubre de 1989): 257–68. http://dx.doi.org/10.1017/s0022377800014343.

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A hydrodynamic theory is presented for plasma particles whose distribution function is close to a plateau in some phase-space region for a finite one-dimensional phase-spase interval. In the framework of the methods of moments, a series expansion of the particle distribution function in an appropriate system of orthogonal (Legendre) polynomials near the state with a plateau is carried out. Deviations from the plateau are due to the presence of a heat flux. The expansion obtained for the distribution function is used to truncate the chain of hydrodynamic equations and to calculate the additional terms arising from the finiteness of the phase interval. The case of one-dimensional Langmuir turbulence is considered as an example. Expressions are presented for the moments of the quasilinear integral of collisions, which describe the variations of the macroscopic characteristics of resonant particles in the respective hydrodynamic equations. Criteria for applicability of the equations obtained are presented. Approximate invariants of motion are obtained in the extreme cases of narrow and broad plateaux.
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Tesis sobre el tema "Plateau region"

1

Wang, Baolai. "Some aspects of plateau permafrost, Qinghai-Xizang (Tibet) Plateau, China, and a comparison with the Mackenzie Delta region, Canada". Thesis, University of Ottawa (Canada), 1993. http://hdl.handle.net/10393/6840.

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Differences in permafrost conditions between the Qinghai-Xizang (Tibet) Plateau and the Mackenzie Delta region primarily relate to their Quaternary histories and their current climates. For example, the Tibetan Plateau has experienced uplift of at least 3,000 m during the last 2 million years. Under the present climatic conditions, the lower altitudinal limit of the plateau permafrost in the north is at 4,150 m a.s.l. This suggests that if the Plateau were 1,000 m lower than its present elevation, there would be no permafrost. During the Quaternary, the Tibetan Plateau remained unglaciated. This has meant that little water was available for the formation of massive ground ice, in contrast to the Mackenzie Delta region. Located at 68-69$\sp\circ$N, the Mackenzie Delta region experiences a combination of low air temperature in winter, a long solar night and a short thaw period in summer. The result is a relatively thin active layer. Located at 30-34$\sp\circ$N, the Tibetan Plateau experiences much higher solar insolation, and a diurnal temperature rhythm. The thickness of the active layer is much greater than in the Mackenzie Delta region and varies between 1.3 and 3 m or more. Permafrost on the Tibetan Plateau is much warmer and thinner than that in the Mackenzie Delta region. One consequence is that it is more sensitive to any changes in climate and surface conditions. Deep ground temperatures in the Pleistocene Mackenzie Delta indicate a recent warming trend, while a cooling trend in the Modern Delta likely relates to local factors such as channel shifting and emergence and/or sedimentation in the Mackenzie River. Water bodies are a cause of geothermal disturbances common to both regions. Numerical simulation of rapid coastal retreat in the Mackenzie Delta region indicates that subsea permafrost is at least 3$\sp\circ$C warmer than adjacent terrestrial permafrost. On the Tibetan Plateau, faulting also disturbs the geothermal regime. Measurements of in situ permafrost creep in the Fenghuo Shan area are one indicator of the warmer permafrost temperatures on the Tibetan Plateau. The average creep velocity ranges from 0.16 cm/year at 2.8 m depth to 0.54 cm/year at 1.6 m depth. These velocities are greater than those recently obtained from the High Arctic of Canada and are approximately of the order of magnitude as those obtained in the Mackenzie Valley. Inter-continental comparison of creep data suggests that climate controls the regional (large scale) magnitude of creep, and that ground ice is a local factor controlling creep rate in a particular area or site. A constitutive relationship (secondary creep power flow law) was applied to the field creep data; and creep parameters A and n were determined for each of the three different depths in the West Valley, Fenghuo Shan area, Tibetan Plateau.
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2

Sen, Sumit Srivastava Puneet Clement Prabhakar Thangadurai. "Runoff generation in pastures of the Appalachian plateau region of North Alabama". Auburn, Ala, 2009. http://hdl.handle.net/10415/1714.

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Goutier, Françoise Mélanie. "Galena lead isotope study of mineral deposits in the Eagle Bay Formation, southeastern British Columbia". Thesis, University of British Columbia, 1986. http://hdl.handle.net/2429/26264.

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The Eagle Bay Formation in the Adams Plateau-Clearwater area, 35km northeast of Kamloops, hosts several economic and sub-economic mineralized occurrences. The age and genesis of these mineral deposits can be estimated by using a specific growth curve which depicts the lead evolution for the Eagle Bay Formation. This curve, named the remodeled curve, represents a local deviation from the average 'shale' curve of Godwin and Sinclair (1982) for the autochthonous part of the Canadian Cordillera. This remodeled curve is specifically applicable to the Adams Plateau-Clearwater area. The lead isotope data from the deposits of the Eagle Bay Formation plot in three distinct clusters along the curve indicating that the lead isotopic signature of the Eagle Bay Formation is upper crustal, and that three periods of mineralization can be recognized or 'fingerprinted'. Accordingly, mineralization cogenetic with Devonian volcanism, and veins related to Cretaceous magmatism can be distinguished by location of galena-lead isotope values within clusters 1 or 3 respectively. Cluster 2 reflects a Late Triassic pulse of mineralization and includes epigenetic veins and stratiform deposits. These deposits are either replacement or cogenetic with their host. The Triassic model age for mineralization that is apparently stratiform and cogenetic raises questions about the currently assigned Cambrian age of associated host rock. To accommodate the lead isotope data a new Upper Triassic unit (T-EBG) within the Eagle Bay Formation is defined. The distinctive lead isotopic signature between deposits hosted by the Eagle Bay Formation is valuable as a guide for future mineral exploration programs in the Adams Plateau-Clearwater area. Recognition of lead isotopic fields that fingerprint types of mineral deposits, provides a useful and practical framework for the classification and evaluation of new mineralized prospects in the area.
Science, Faculty of
Earth, Ocean and Atmospheric Sciences, Department of
Graduate
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Stewart, Ryan. "Physical and Chemical Parameters of Common Soils in the Central Plateau Region of Haiti". Thesis, Virginia Tech, 2003. http://hdl.handle.net/10919/32199.

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Soil degradation is a common occurrence in Haiti that is mainly caused by the cultivation of marginal lands and deforestation, which both contribute to the excessive erosion rate seen in the country today. The Central Plateau of Haiti is a mountainous region in which a majority of the population is rural and practices subsistence agriculture on hillsides and steeply-sloping land. Essential plant nutrients, such as nitrogen (N) and phosphorus (P), are commonly a limiting factor in crop production, yet fertilizer is unavailable or is too expensive for smallholder farmers to purchase. This study was conducted to a) evaluate organic matter and nutrient stocks of various soils in the Central Plateau region, along with other chemical and physical characteristics and b) to evaluate the phosphorus-scavenging ability of commonly-grown crops to isolate those that may benefit subsequent smallholder yields. Soils from four locations in the Central Plateau were assessed for organic matter in labile and non-labile fractions as well as for cation exchange capacity (CEC), total organic carbon (C) and N, pH, texture, and other characteristics. Results indicated that most of the soil (92%) was contained within aggregates, and organic matter was mainly present in stable, slowly-decomposing fractions. Seven species were evaluated in a controlled-environment pot experiment for bulk and rhizosphere soil P and pH, plant dry weight, and above- and below-ground P tissue content as indicators of the speciesâ ability to solubilize P from the soil. Velvet bean (Mucuna pruriens (L.) DC) produced the most biomass and was able to take up the most P, though lablab (Lablab purpureous (L.) Sweet), took up comparable amounts of P.
Master of Science
LTRA-6 (A CAPS program for the Central Plateau of Haiti)
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Stewart, Ryan D. "Physical and Chemical Parameters of Common Soils in the Central Plateau Region of Haiti". Thesis, Virginia Tech, 2012. http://hdl.handle.net/10919/32199.

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Soil degradation is a common occurrence in Haiti that is mainly caused by the cultivation of marginal lands and deforestation, which both contribute to the excessive erosion rate seen in the country today. The Central Plateau of Haiti is a mountainous region in which a majority of the population is rural and practices subsistence agriculture on hillsides and steeply-sloping land. Essential plant nutrients, such as nitrogen (N) and phosphorus (P), are commonly a limiting factor in crop production, yet fertilizer is unavailable or is too expensive for smallholder farmers to purchase. This study was conducted to a) evaluate organic matter and nutrient stocks of various soils in the Central Plateau region, along with other chemical and physical characteristics and b) to evaluate the phosphorus-scavenging ability of commonly-grown crops to isolate those that may benefit subsequent smallholder yields. Soils from four locations in the Central Plateau were assessed for organic matter in labile and non-labile fractions as well as for cation exchange capacity (CEC), total organic carbon (C) and N, pH, texture, and other characteristics. Results indicated that most of the soil (92%) was contained within aggregates, and organic matter was mainly present in stable, slowly-decomposing fractions. Seven species were evaluated in a controlled-environment pot experiment for bulk and rhizosphere soil P and pH, plant dry weight, and above- and below-ground P tissue content as indicators of the speciesâ ability to solubilize P from the soil. Velvet bean (Mucuna pruriens (L.) DC) produced the most biomass and was able to take up the most P, though lablab (Lablab purpureous (L.) Sweet), took up comparable amounts of P.
Master of Science
LTRA-6 (A CAPS program for the Central Plateau of Haiti)
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6

Curtis, Andrew. "Shear wave studies and elastic models of extensional zones : the Tibetian Plateau and Aegean region". Thesis, University of Oxford, 1994. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.294273.

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Bischoff, Kristen L. "Examination of Water Drilling Success Rate Using Satellite Imagery in the Central Plateau Region, Haiti". Bowling Green State University / OhioLINK, 2008. http://rave.ohiolink.edu/etdc/view?acc_num=bgsu1210703963.

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Schaub, Matthias. "Lateglacial environmental conditions on the Swiss Plateau : a multi-proxy approach using tree rings and sediment-based proxies /". Zürich : Geographisches Institut der Universität Zürich, 2007. http://bvbr.bib-bvb.de:8991/F?func=service&doc_library=BVB01&doc_number=016135853&line_number=0002&func_code=DB_RECORDS&service_type=MEDIA.

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Sanchez, Maria Teresa Hernandez. "Productivity Variations around a Naturally Iron-Fertilised Region of the Ocean : The Crozet Plateau, Southern Ocean". Thesis, University of Bristol, 2009. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.500071.

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Mehalic, David Steven. "The Archaeological Geography of Small Architectural Sites of the Mogollon Plateau Region of East-Central Arizona". Diss., The University of Arizona, 2012. http://hdl.handle.net/10150/265814.

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This dissertation explores some of the thousands of smaller Native American archaeological sites with meager architectural elements commonly found along part of the southern edge of the Colorado Plateau in east-central Arizona in an area known as the Mogollon Plateau. Small surface structures of less than five rooms were typically built of a combination of stone masonry and wattle and daub, and they are generally interpreted as evidence of repeated occupations of limited duration, primarily dating between AD 800 and 1300. Accordingly, these small sites have also served a number of roles in ongoing discussions of settlement systems and land use, and they present challenges for cultural resources management. The fundamental characteristics (or lack thereof) typically used to classify small sites have traditionally relegated them to settlement pattern studies rather than extensive excavation, generating a broad range of hypotheses concerning their significance and drawing heavily upon historical ecology. GIS methods are used to explore several ecologically and socially-driven models and examine the roles of small architectural sites in archaeological and systemic landscapes. Common pool resources offer some explanatory power regarding small sites, but some have suggested competition and conflict led to a "tragedy of the commons" and environmental degradation. Two primary site concentrations are identified, and the evidence supports an interpretation of extensive and sustainable use of the area, much of which seems to have been a frontier. Recommendations for research-driven management and preservation of cultural resources are provided.
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Libros sobre el tema "Plateau region"

1

Boulé, Mary Null. Plateau region: Yakama people. Vashon, WA: Merryant Publishers, 1997.

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Boulé, Mary Null. Plateau region: Nez Percé people. Vashon, WA: Merryant Publishers, 1998.

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Weaver, H. Dwight. The wilderness underground: Caves of the Ozark plateau. Columbia: University of Missouri Press, 1992.

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Hereford, Richard. Precipitation history of the Colorado Plateau region, 1900-2000. [Reston, Va.?]: U.S. Dept. of the Interior, U.S. Geological Survey, 2002.

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Jetson, Tim. History of the Midlands-Central Plateau region: Printed sources. Hobart, Tas: Centre for Tasmanian Historical Studies, University of Tasmania, 1991.

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Hereford, Richard. Precipitation history of the Colorado Plateau region, 1900-2000. [Reston, Va.?]: U.S. Dept. of the Interior, U.S. Geological Survey, 2002.

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Hereford, Richard. Precipitation history of the Colorado Plateau region, 1900-2000. [Reston, Va.?]: U.S. Dept. of the Interior, U.S. Geological Survey, 2002.

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Hereford, Richard. Precipitation history of the Colorado Plateau region, 1900-2000. [Reston, Va.?]: U.S. Dept. of the Interior, U.S. Geological Survey, 2002.

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Andreas, Barbara K. The vascular flora of the glaciated Allegheny plateau region of Ohio. Columbus, Ohio: College of Biological Sciences, Ohio State University, 1989.

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Johnson, David W. Wildlife of the canyons: Colorado National Monument and the Colorado Plateau region. [Colorado]: Colorado National Monument Association, 1990.

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Capítulos de libros sobre el tema "Plateau region"

1

Baiping, Zhang. "Kunlun Mountains Region". En Mountain Geoecology and Sustainable Development of the Tibetan Plateau, 349–72. Dordrecht: Springer Netherlands, 2000. http://dx.doi.org/10.1007/978-94-010-0965-2_17.

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Christiansen, Robert L. "The Yellowstone Plateau—Island Park region". En Snake River Plain-Yellowstone Volcanic Province: Jackson, Wyoming to Boise, Idaho July 21–29, 1989, 13–37. Washington, D. C.: American Geophysical Union, 1989. http://dx.doi.org/10.1029/ft305p0013.

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Baud, Aymon. "The Western End of the Tibetan Plateau". En Tectonic Evolution of the Tethyan Region, 505–6. Dordrecht: Springer Netherlands, 1989. http://dx.doi.org/10.1007/978-94-009-2253-2_20.

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Buzhuo, Peng, Bao Haosheng y Pu Lijie. "Geo-Ecology of Mts. Namjagbarwa Region". En Mountain Geoecology and Sustainable Development of the Tibetan Plateau, 265–82. Dordrecht: Springer Netherlands, 2000. http://dx.doi.org/10.1007/978-94-010-0965-2_13.

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Qinye, Yang. "Dry Valleys in Hengduan Mts Region". En Mountain Geoecology and Sustainable Development of the Tibetan Plateau, 283–302. Dordrecht: Springer Netherlands, 2000. http://dx.doi.org/10.1007/978-94-010-0965-2_14.

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Chang, Chen-Fa, Yu-Sheng Pan y Yi-Ying Sun. "The Tectonic Evolution of Qinghai-Tibet Plateau: A Review". En Tectonic Evolution of the Tethyan Region, 415–76. Dordrecht: Springer Netherlands, 1989. http://dx.doi.org/10.1007/978-94-009-2253-2_18.

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Mitchell, A. H. G. "The Shan Plateau And Western Burma: Mesozoic-Cenozoic Plate Boundaries and Correlations with Tibet". En Tectonic Evolution of the Tethyan Region, 567–83. Dordrecht: Springer Netherlands, 1989. http://dx.doi.org/10.1007/978-94-009-2253-2_24.

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Burke, Kevin y Lynette Lucas. "Thrusting on the Tibetan Plateau within the Last 5 Ma". En Tectonic Evolution of the Tethyan Region, 507–12. Dordrecht: Springer Netherlands, 1989. http://dx.doi.org/10.1007/978-94-009-2253-2_21.

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Zheng, Fenli y Bin Wang. "Soil Erosion in the Loess Plateau Region of China". En Ecological Research Monographs, 77–92. Tokyo: Springer Japan, 2013. http://dx.doi.org/10.1007/978-4-431-54481-4_6.

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Wei, He, Honglei Li, Zhibing Pang, Cheng Jin, Yuankang Sun y Xingbin Zhu. "Research on Environmental Suitability of Operation Staffs at Frigid Plateau Region". En Proceedings of the 14th International Conference on Man-Machine-Environment System Engineering, 285–92. Berlin, Heidelberg: Springer Berlin Heidelberg, 2014. http://dx.doi.org/10.1007/978-3-662-44067-4_35.

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Actas de conferencias sobre el tema "Plateau region"

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Aedla, Raju, G. S. Dwarakish y D. Venkat Reddy. "Satellite image contrast enhancement algorithm based on plateau histogram equalization". En 2014 IEEE Region 10 Symposium. IEEE, 2014. http://dx.doi.org/10.1109/tenconspring.2014.6863028.

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Li, Hongjian. "Study on Construction Technology for Tunnelling in the Plateau Permafrost Region". En 14th Conference on Cold Regions Engineering. Reston, VA: American Society of Civil Engineers, 2009. http://dx.doi.org/10.1061/41072(359)3.

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Meng, Jingjing, Jingyu Liu y Shaopeng Huang. "Soil carbon sequestration of Chinese Loess Plateau and Northeast Phaeozem Region". En 2011 International Conference on Electrical and Control Engineering (ICECE). IEEE, 2011. http://dx.doi.org/10.1109/iceceng.2011.6058300.

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Karlstrom, Karl E., Lijun Liu, Andres Aslan, Zhou Quan y Matthew T. Heizler. "ONGOING MANTLE-DRIVEN UPLIFT OF THE COLORADO PLATEAU-ROCKY MOUNTAIN REGION". En Joint 70th Annual Rocky Mountain GSA Section / 114th Annual Cordilleran GSA Section Meeting - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018rm-314379.

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Agrawal, Bharat, Matthias Preindl, Berker Bilgin y Ali Emadi. "Estimating switching losses for SiC MOSFETs with non-flat miller plateau region". En 2017 IEEE Applied Power Electronics Conference and Exposition (APEC). IEEE, 2017. http://dx.doi.org/10.1109/apec.2017.7931075.

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Han, Jing, Teng Ma, Xirui Wang, Yang Rui y Simin Zhao. "Research on the Spatial Pattern of Traditional Villages in Loess Plateau Region". En 2018 2nd International Conference on Education, Economics and Management Research (ICEEMR 2018). Paris, France: Atlantis Press, 2018. http://dx.doi.org/10.2991/iceemr-18.2018.127.

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Wen, Yuliang, Yonghong Yi, Tong Hao, Tian Chang, Ping Lu y Rongxing Li. "Large-scale Soil Moisture Mapping on the Tibetan Plateau (TP) Using Bias-corrected ERA5-Land Product". En TENCON 2022 - 2022 IEEE Region 10 Conference (TENCON). IEEE, 2022. http://dx.doi.org/10.1109/tencon55691.2022.9977908.

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M.A. de Brito, Paula, Marcelo B. de Padua, Antonio L. Padilha y Icaro Vitorello. "The Conductive Characteristics of the Lithospheric Region Under the Serra do Mar Plateau". En 5th International Congress of the Brazilian Geophysical Society. European Association of Geoscientists & Engineers, 1997. http://dx.doi.org/10.3997/2214-4609-pdb.299.249.

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Sumit Sen, Puneet Srivastava, Kyung H Yoo, Jacob H Dane, Joey N Shaw y Moon S Kang. "Runoff Generation Mechanism in the Appalachian Plateau Region of Alabama - A Field Investigation". En 2007 Minneapolis, Minnesota, June 17-20, 2007. St. Joseph, MI: American Society of Agricultural and Biological Engineers, 2007. http://dx.doi.org/10.13031/2013.23548.

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Xie, Changwei, Jianmin Feng y T. Wang. "Land Desertification in the Source Region of the Yellow River, Northeast Qinghai Xizang Plateau". En 2006 IEEE International Symposium on Geoscience and Remote Sensing. IEEE, 2006. http://dx.doi.org/10.1109/igarss.2006.394.

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Informes sobre el tema "Plateau region"

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Pyle, L. J., A. L. Jones, L. P. Gal, J. G. Abbott, A D McCracken, M. G. Fowler y L D Stasiuk. 2005 reconnaissance field program in Peel Plateau and Peel Plain region, Northwest Territories and Yukon Territory. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2006. http://dx.doi.org/10.4095/223682.

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Lemieux, Y., L. P. Gal, L. J. Pyle, T. Hadlari y W. Zantvoort. Report of activities on the structural geology of southern Peel Plateau and Peel Plain region, Northwest Territories and Yukon. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2007. http://dx.doi.org/10.4095/222257.

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Xiong, Zhihua, Jiaqi Li, Jianbing Chen, Jinping Li y Dongpeng Zhu. Comparative study of seismic resilience between PC and steel-concrete bridges in a permafrost region on the Qinghai-Tibet Plateau. International Permafrost Association (IPA), junio de 2024. http://dx.doi.org/10.52381/icop2024.79.1.

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Jefferson, C. W. y D. Pare. New Placer Gold Anomalies in the northern Liard Range - southern Ram Plateau area, South Nahanni River Region, District of Mackenzie, Northwest Territories. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1991. http://dx.doi.org/10.4095/132621.

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Jabado, Rima, Emiliano García-Rodríguez, Peter Kyne, Ryan Charles, Asia Armstrong, Jenny Bortoluzzi, Théophile Mouton et al. Mediterranean and Black Seas: A regional compendium of Important Shark and Ray Areas. IUCN SSC Shark Specialist Group, septiembre de 2023. http://dx.doi.org/10.59216/ssg.isra.2023.r3.

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Resumen
The second Important Shark and Ray Areas (ISRA) regional expert workshop was held in hybrid mode (in person and online) in Thessaloniki, Greece from 8–12 May, 2023. The goal was to identify and delineate three-dimensional and discrete portions of habitat that are critical to the survival of sharks, rays, and chimaeras (hereafter ‘sharks’), and that have the potential to be managed for conservation. The region covered included the Mediterranean and Black Seas. This scientific collaboration amongst regional and global experts resulted in the identification of 65 Important Shark and Ray Areas, 6 candidate ISRAs, and 20 Areas of Interest. Identified ISRAs range in size from small underwater areas of 0.09 km2 at depths of 1,100–1,150 m (Palmahim Brine Pools ISRA in Israel) to large areas of 219,913 km2 (Strait of Sicily and Tunisian Plateau ISRA which is transboundary in nature encompassing waters of Italy, Libya, Malta, and Tunisia) from surface waters to a depth of 2,000 m. This compendium provides an overview of all areas delineated.
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Sandvol, Eric, Ayoub Kaviani, Rengin Gok, Wenfei Ku y Xueyang Bao. High-Resolution Regional Phase Attenuation Models of the Iranian Plateau and Surrounding Regions. Fort Belvoir, VA: Defense Technical Information Center, marzo de 2014. http://dx.doi.org/10.21236/ada606587.

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Teskey, D., P. Stone, P. S. Mustard y P. Metcalfe. High-resolution regional aeromagnetic survey - Interior Plateau, British Columbia. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1997. http://dx.doi.org/10.4095/208983.

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Solano, E. R. y R. D. Hazeltine. Neoclassical kinetic theory near an X-point: Plateau regime. Office of Scientific and Technical Information (OSTI), agosto de 1993. http://dx.doi.org/10.2172/10182295.

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Best, M. E., V. M. Levson y L. J. Diakow. Electromagnetic mapping in drift covered regions of the Nechako Plateau, British Columbia. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1997. http://dx.doi.org/10.4095/208984.

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Sandvol, Eric A., Ayoub Kaviani, Rengin Gok y Georg Rumpker. High-Resolution Regional Phase Attenuation Models of the Iranian Plateau and Zagros (Postprint). Fort Belvoir, VA: Defense Technical Information Center, mayo de 2012. http://dx.doi.org/10.21236/ada564091.

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