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  • 1
    Publication Date: 2014-03-26
    Description: Article Understanding and controlling the transport of light through random media is important for many applications. Here, Peña et al . demonstrate how in the deeply localized regime transport is mediated by a single transmission channel composed of a localized internal mode or a necklace state. Nature Communications doi: 10.1038/ncomms4488 Authors: A. Peña, A. Girschik, F. Libisch, S. Rotter, A. A. Chabanov
    Electronic ISSN: 2041-1723
    Topics: Biology , Chemistry and Pharmacology , Natural Sciences in General , Physics
    Published by Springer Nature
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  • 2
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    In:  Bull. Seism. Soc. Am., Edmonton, Conseil de l'Europe, vol. 81, no. 2, pp. 687-693, pp. B10410, (ISSN: 1340-4202)
    Publication Date: 1991
    Keywords: Micro-tremor (seismic noise) ; NOISE ; Site amplification ; Earthquake engineering, engineering seismology ; noksp ; BSSA ; Ibanez
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  • 3
    Publication Date: 2020-06-26
    Electronic ISSN: 2643-1564
    Topics: Physics
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  • 4
    Publication Date: 2015-09-16
    Description: Author(s): L. A. Peña Ardila and S. Giorgini We investigate the properties of an impurity immersed in a dilute Bose gas at zero temperature using quantum Monte Carlo methods. The interactions between bosons are modeled by a hard-sphere potential with scattering length a , whereas the interactions between the impurity and the bosons are modeled … [Phys. Rev. A 92, 033612] Published Tue Sep 15, 2015
    Keywords: Matter waves and collective properties of cold atoms and molecules
    Print ISSN: 1050-2947
    Electronic ISSN: 1094-1622
    Topics: Physics
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  • 5
    Publication Date: 2019
    Description: Variable retention (aggregated and dispersed retention) harvesting proposed for Nothofagus pumilio was designed for timber purposes and biodiversity conservation. Harvesting by opening canopy generates different ...
    Electronic ISSN: 2192-1709
    Topics: Energy, Environment Protection, Nuclear Power Engineering
    Published by Springer
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  • 6
    Publication Date: 2019
    Description: Abstract Investigated presently is how rare‐earth element dopants (samarium and erbium) affect the scale development of sintered ZrB2/SiC (ZBS) samples during ablation testing. ZBS billets with five different Sm to Er ratios, with a nominal total amount of 3 mol.% dopant incorporated, were prepared by sintering in vacuum to 2000 °C and subjected to 60s and 300s ablation cycles. Differences in surface temperatures between ZBS samples with different dopant ratios suggests differences in spectral absorptance/emittance between each of the five compositions investigated. ZBS billets co‐doped with Sm and Er form a beneficial c1‐(Sm/Er)0.2Zr0.8O1.9 oxide scale as the majority phase, with some glassy phase observed. The crystalline c1‐(Sm/Er)0.2Zr0.8O1.9 oxide scale is more thermally stable than the m‐ZrO2 oxide scale typically formed in oxidized ZBS systems, resulting in a more adherent oxide scale to the unreacted material. The crystalline oxide scale and the amorphous phase are formed by a convection cell mechanism where the c1‐(Sm/Er)0.2Zr0.8O1.9 crystalline islands precipitate, grow, and coalesce. This article is protected by copyright. All rights reserved.
    Print ISSN: 0002-7820
    Electronic ISSN: 1551-2916
    Topics: Mechanical Engineering, Materials Science, Production Engineering, Mining and Metallurgy, Traffic Engineering, Precision Mechanics , Physics
    Published by Wiley
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  • 7
    Publication Date: 2011-02-24
    Description: The late Holocene in the central Ebro Depression is characterized by a number of morphodynamic stages that affected hillslopes and channels. Climate fluctuations and human activities together caused severe erosion and floods, resulting in alternating stages of accumulation and incision in the valley floors. Seven accumulation levels (N6-N0) correlated with Ebro River fluvial terraces have been identified in the secondary fluvial network of the central Ebro Depression. The main accumulation level (N3) corresponds to a long period of increased hillslope erosion and sedimentation in the valleys, from the Neolithic to the late Roman periods. The accumulation levels are evident throughout the valleys and extend to the valley mouths, where many connect with alluvial fans. The study of several sedimentological profiles, 14 C AMS dating, and many archaeological remnants, have enabled detailed assessment of sedimentation characteristics in the alluvial fans and the relationship thereof to the presence of human settlements. Four sedimentation stages have been identified: (i) pre-Bronze Age (〉 3800 years BP), (ii) Bronze Age/Iron Age (3800-2500 years BP), (iii) Roman/post-Roman period (2500-1500 years BP), and, (iv) the early Middle Ages, mainly during the Visigothic period (sixth century). The sedimentation dynamics of the alluvial fans are related to: (i) climate variability, (ii) human activities in the watershed, and (iii) the meandering character of the Ebro River, which has lateral displacements that change the local base level of tributaries and fans. Level N3 in the valley floors corresponds to stages i-iii of the alluvial fans, which are mostly related to human-induced transformation of characteristics of the secondary basins, coinciding with enhanced erosion under favorable (warm and humid) climatic conditions. In contrast, the Medieval stage, which corresponds to level N2 in the valleys, was caused by floods during a period of high climatic variability.
    Print ISSN: 0959-6836
    Electronic ISSN: 1477-0911
    Topics: Geography , Geosciences
    Published by Sage
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  • 8
    Publication Date: 2013-02-24
    Description: [1]  We investigate several lidar-type instruments and methodologies for boundary-layer height (BLH) estimation during two days at a coastal site for winds that experience marine upstream flow conditions. Wavelet and profile fitting procedures on the aerosol backscatter signals from a ceilometer and an aerosol lidar reveal similar BLHs, but their agreement depends on the presence of clouds and the instrument signal, among others. BLHs derived by a threshold on the carrier-to-noise profiles of a wind lidar agree well with those derived by using a threshold on the backscatter profile of the ceilometer and are used as reference for a 10-day BLH inter-comparison. Furthermore, the BLHs from the aerosol analysis are comparable to those derived from wind speed and direction profiles from combined mast/wind lidar measurements. The BLH derived from simulations performed with the Weather Research and Forecasting model (WRF) model show similar behavior compared to the lidar observations. [2]  The seasonal diurnal variation of the BLH for 2010, derived from the wind lidar and ceilometer thresholds, shows similar BLHs but generally higher values compared to that from WRF. No clear BLH diurnal variation is observed neither from the observations nor from the WRF model outputs, except in summer for the latter. Both observations and WRF model simulations reveal higher BLHs during autumn compared to spring time. These BLHs are used to evaluate the intra-annual variation and show high peaks in September, November and February.
    Print ISSN: 0148-0227
    Topics: Geosciences , Physics
    Published by Wiley on behalf of American Geophysical Union (AGU).
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  • 9
    Publication Date: 2014-04-18
    Description: The influence of baroclinicity on wind within the planetary boundary layer is investigated using two years of wind lidar measurements collected at a suburban site in northern Germany (Hamburg) and a rural-coastal site in western Denmark (Høvsøre). Measurements are made up to a height of 950 m. The surface geostrophic wind, the surface gradient wind and the gradient wind are estimated using the pressure and geopotential fields from a mesoscale model. At both sites the atmospheric flow was typically baroclinic. The distribution of the geostrophic wind shear was approximately Gaussian with a mean close to zero and a standard deviation of approximately 3 m s − 1 km − 1 . The geostrophic wind shear had a strong seasonal dependence because of temperature differences between land and sea. The mean wind profile in Hamburg, observed during an intensive campaign using radio sounding and during the whole year using the wind lidar, was influenced by baroclinicity. For easterly winds at Høvsøre, the estimated gradient wind decreased rapidly with height, resulting in a mean low-level jet. The turning of the wind in the boundary layer, the boundary-layer height and the empirical constants in the geostrophic drag law were found to be dependent on baroclinicity for neutral conditions.
    Print ISSN: 0035-9009
    Electronic ISSN: 1477-870X
    Topics: Geography , Physics
    Published by Wiley
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  • 10
    Publication Date: 2009-03-07
    Description: Amazon forests are a key but poorly understood component of the global carbon cycle. If, as anticipated, they dry this century, they might accelerate climate change through carbon losses and changed surface energy balances. We used records from multiple long-term monitoring plots across Amazonia to assess forest responses to the intense 2005 drought, a possible analog of future events. Affected forest lost biomass, reversing a large long-term carbon sink, with the greatest impacts observed where the dry season was unusually intense. Relative to pre-2005 conditions, forest subjected to a 100-millimeter increase in water deficit lost 5.3 megagrams of aboveground biomass of carbon per hectare. The drought had a total biomass carbon impact of 1.2 to 1.6 petagrams (1.2 x 10(15) to 1.6 x 10(15) grams). Amazon forests therefore appear vulnerable to increasing moisture stress, with the potential for large carbon losses to exert feedback on climate change.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Phillips, Oliver L -- Aragao, Luiz E O C -- Lewis, Simon L -- Fisher, Joshua B -- Lloyd, Jon -- Lopez-Gonzalez, Gabriela -- Malhi, Yadvinder -- Monteagudo, Abel -- Peacock, Julie -- Quesada, Carlos A -- van der Heijden, Geertje -- Almeida, Samuel -- Amaral, Ieda -- Arroyo, Luzmila -- Aymard, Gerardo -- Baker, Tim R -- Banki, Olaf -- Blanc, Lilian -- Bonal, Damien -- Brando, Paulo -- Chave, Jerome -- de Oliveira, Atila Cristina Alves -- Cardozo, Nallaret Davila -- Czimczik, Claudia I -- Feldpausch, Ted R -- Freitas, Maria Aparecida -- Gloor, Emanuel -- Higuchi, Niro -- Jimenez, Eliana -- Lloyd, Gareth -- Meir, Patrick -- Mendoza, Casimiro -- Morel, Alexandra -- Neill, David A -- Nepstad, Daniel -- Patino, Sandra -- Penuela, Maria Cristina -- Prieto, Adriana -- Ramirez, Fredy -- Schwarz, Michael -- Silva, Javier -- Silveira, Marcos -- Thomas, Anne Sota -- Steege, Hans Ter -- Stropp, Juliana -- Vasquez, Rodolfo -- Zelazowski, Przemyslaw -- Alvarez Davila, Esteban -- Andelman, Sandy -- Andrade, Ana -- Chao, Kuo-Jung -- Erwin, Terry -- Di Fiore, Anthony -- Honorio C, Euridice -- Keeling, Helen -- Killeen, Tim J -- Laurance, William F -- Pena Cruz, Antonio -- Pitman, Nigel C A -- Nunez Vargas, Percy -- Ramirez-Angulo, Hirma -- Rudas, Agustin -- Salamao, Rafael -- Silva, Natalino -- Terborgh, John -- Torres-Lezama, Armando -- New York, N.Y. -- Science. 2009 Mar 6;323(5919):1344-7. doi: 10.1126/science.1164033.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Ecology and Global Change, School of Geography, University of Leeds, Leeds LS2 9JT, UK. o.phillips@leeds.ac.uk〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/19265020" target="_blank"〉PubMed〈/a〉
    Keywords: Atmosphere ; *Biomass ; Brazil ; Carbon ; Carbon Dioxide ; Climate ; *Droughts ; *Ecosystem ; South America ; *Trees/growth & development ; Tropical Climate
    Print ISSN: 0036-8075
    Electronic ISSN: 1095-9203
    Topics: Biology , Chemistry and Pharmacology , Computer Science , Medicine , Natural Sciences in General , Physics
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