971 resultados para 314-C0001B
Resumo:
The State of Connecticut owns a LIght Detection and Ranging (LIDAR) data set that was collected in 2000 as part of the State’s periodic aerial reconnaissance missions. Although collected eight years ago, these data are just now becoming ready to be made available to the public. These data constitute a massive “point cloud”, being a long list of east-north-up triplets in the State Plane Coordinate System Zone 0600 (SPCS83 0600), orthometric heights (NAVD 88) in US Survey feet. Unfortunately, point clouds have no structure or organization, and consequently they are not as useful as Triangulated Irregular Networks (TINs), digital elevation models (DEMs), contour maps, slope and aspect layers, curvature layers, among others. The goal of this project was to provide the computational infrastructure to create a first cut of these products and to serve them to the public via the World Wide Web. The products are available at http://clear.uconn.edu/data/ct_lidar/index.htm.
Resumo:
u.a.: Schopenhauer-Portraits; Biographie von Hermann Rollett; Rezeption Schopenhauers; Wilhelm Gwinner; Arthur Schopenhauer; Valentin Schertle; Jules Lunteschütz; Angilbert Göbel; Hermann Rollett; Benno Erdmann; Johann Karl Friedrich Rosenkranz;
Resumo:
Alois Henninger
Resumo:
1 Brief von Frederick Pollock an Max Hürlimann, 09.04.1938; 1 Brief von Frederick Pollock an R. Aron, 11.04.1938; 1 Telegramm von Frederick Pollock an Juliette Favez, 28.08.1937; 1 Brief von Bernhard Reichenbach an Frederick Pollock, 11.08.1937;
Resumo:
2 Briefe zwischen Frederick Pollock und der Southern Counties Gas Company of California (Santa Monica), Dezember 1946; 1 Brief von Frederick Pollock an Pacific Electric Railway Co. (West Los Angeles), 16.05.1946;
Resumo:
Atmospheric fluxes of iron (Fe) over the past 200 kyr are reported for the coastal Antarctic Talos Dome ice core, based on acid leachable Fe concentrations. Fluxes of Fe to Talos Dome were consistently greater than those at Dome C, with the greatest difference observed during interglacial climates. We observe different Fe flux trends at Dome C and Talos Dome during the deglaciation and early Holocene, attributed to a combination of deglacial activation of dust sources local to Talos Dome and the reorganisation of atmospheric transport pathways with the retreat of the Ross Sea ice shelf. This supports similar findings based on dust particle sizes and fluxes and Rare Earth Element fluxes. We show that Ca and Fe should not be used as quantitative proxies for mineral dust, as they all demonstrate different deglacial trends at Talos Dome and Dome C. Considering that a 20 ppmv decrease in atmospheric CO2 at the coldest part of the last glacial maximum occurs contemporaneously with the period of greatest Fe and dust flux to Antarctica, we confirm that the maximum contribution of aeolian dust deposition to Southern Ocean sequestration of atmospheric CO2 is approximately 20 ppmv.
Resumo:
Fil: Introna, Ana María.
Resumo:
Fil: Recchia Paez, Juan. Universidad Nacional de La Plata. Facultad de Humanidades y Ciencias de la Educación; Argentina.
Resumo:
Fil: Bisignano, Julia Alejandra. Universidad Nacional de La Plata. Facultad de Humanidades y Ciencias de la Educación; Argentina.
Resumo:
Fil: Bisignano, Julia Alejandra. Universidad Nacional de La Plata. Facultad de Humanidades y Ciencias de la Educación; Argentina.
Resumo:
Fil: Recchia Paez, Juan. Universidad Nacional de La Plata. Facultad de Humanidades y Ciencias de la Educación; Argentina.
Resumo:
Fil: Bisignano, Julia Alejandra. Universidad Nacional de La Plata. Facultad de Humanidades y Ciencias de la Educación; Argentina.
