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Data for: Zebker and Chen (2024), A robust method for selecting a high-quality interferogram subset in InSAR surface deformation analysis
No full textReplication data and readme for Figure 4 of M. S. Zebker and J. Chen, A robust method for selecting a high-quality interferogram subset in InSAR surface deformation analysis, Geophysical Research Letters. Includes the location and volumes of produced oil, produced gas, and produced water during the time period studied
CSR GRACE and GRACE-FO Ocean Mascons RL06.2EQ
No full textMonthly mass anomaly grids from GRACE and GRACE-FO determined from CSR RL06.2 processing with specific handling of the major earthquakes in Japan and Andaman Bay. The RL06.2EQ mascons are directly comparable to the CSR RL06.2 official mascon product.
The earthquake model is provided as a companion correction grid. Users interested in the mass anomaly signal, free of the contributions from the earthquake co-seismic and post-seismic signals, will substract the earthquake model grid from the RL06.2EQ mascon grid.
The grids are provided globally with a quarter degree sampling in longitude/latitude. Only the ocean mascons are reported. The land mascons are set to "NaN".
The grids cover the GRACE and GRACE-FO period from 04/2002 to 02/2023
ESCHER ice thickness, echo strength and specularity content data for the Exploration of Saline Cryospheric Habitats with Europa Relevance project
No full textESCHER (Exploration of Saline Cryospheric Habitats with Europa Relevance) is a NASA funded PSTAR (Planetary Science and Technology from Analog Research) program with the general geophysical goals of characterizing the subglacial environment of Devon Ice Cap in Nunavut, Canada as a potential planetary analog. The project seeks to gather additional evidence to infer properties of the chemistry of the subglacial hydrological system and to further the technical development of the scientific instrumentation. ESCHER represents the first field deployment of a multi-polarization radar system on an A-Star 350 B2 helicopter platform. This is the sixth polar deployment of this helicopter geophysical system, and the first in the Arctic. The previous helicopter-based systems expeditions were KRT1, KRT2, ASE2, ASE3, ASE4. Similar results for ASE3 are described in Pierce et al, 2024.
The science goals include characterizing the subglacial environment from the summit of Devon Ice Cap to Sverdrup Glacier’s marine termination. The study area includes three linked geographical regions: i) The summit area as described in Rutishauser et al. (2020), ii) the shoulder region of the ice cap, just upstream of the ice flow that enters the outlet valleys feeding the upper reaches of the Sverdrup Glacier, and iii) the Sverdrup valley glacier, tidewater terminus, and locations of subglacial discharge. The study region also includes the upper catchment of the Croker Bay Glaciers and some of the western land terminating flanks of the ice cap.
All data in this collection is derived from a multipolarization version of the Helicopter Radar (HERA) system (Lindzey et al., 2017, 2022). Included in this dataset are the Level 2 time registered geophysical observables for the entire study, including specific lines mentioned in Pierce et al., (2024); ice thickness, partial bed reflectivity, surface reflectivity, bed and surface elevation derived both from incoherent processing (IR2HI2) and focused processing (IRFOC2; Peters et al., 2007); no multipolarization processing is included here. Also included is specularity content (IRSPC2; Schroeder et al., 2014, Young et al, 2016).
Data consists of ASCII tab delimited tables, with header describing the columns and key metadata on a per transect basis. Images showing simple maps of values are also included.
The following transects are included:
DEV3/PER0a/X101a
DEV3/PER0a/X105a
DEV3/PER0a/X69a
DEV3/PER0a/X72a
DEV3/PER0a/X73a
DEV3/PER0a/X73b
DEV3/PER0a/X74a
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DEV3/PER0a/X76a
DEV3/PER0a/X77a
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DEV3/PER0a/X78a
DEV3/PER0a/X79a
DEV3/PER0a/X80a
DEV3/PER0a/X81a
DEV3/PER0a/X81b
DEV3/PER0a/X82a
DEV3/PER0a/X85a
DEV3/PER0a/X88a
DEV3/PER0a/X89a
DEV3/PER0a/X93a
DEV3/PER0a/X97a
DEV3/PER0a/Y68a
DEV3/PER0a/Y69a
DEV3/PER0a/Y71a
DEV3/PER0a/Y72a
DEV3/PER0a/Y79a
DEV3/PER0a/Y80a
DEV3/PER0a/Y81a
DEV3/PER0a/Y82a
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DEV3/PER0a/Y84a
DEV3/PER0a/Y85a
DEV3/PER0a/Y86a
DEV3/PER0a/Y87a
DEV/PER0a/X68a
DEV/PER0a/X69b
DEV/PER0a/X70a
DEV/PER0a/X75b
DEV/PER0a/Y66a
DEV/PER0a/Y80a
DEV/PER0a/Y88a
ESH1/PER0a/F02T01a
ESH1/PER0a/F02T02a
ESH1/PER0a/F02T03a
ESH1/PER0a/F02T04a
ESH1/PER0a/F02T05a
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ESH1/PER0a/F02T10a
ESH1/PER0a/F02T11a
ESH1/PER0a/F02T12a
ESH1/PER0a/F02T13a
ESH1/PER0a/F02T14a
ESH1/PER0a/F02T15a
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ESH1/PER0a/F04T01a
ESH1/PER0a/F04T02a
ESH1/PER0a/F04T03a
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ESH1/PER0a/F05a
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ESH1/PER0a/F05T14a
ESH1/PER0a/F05T15a
ESH1/PER0a/F05T16a
ESH1/PER0a/F05T17a
ESH1/PER0a/F05T18a
ESH1/PER0a/F05T19a
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ESH1/PER0a/F05T25a
ESH1/PER0a/F05T26a
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ESH1/PER0a/F05T28a
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ESH1/PER0a/F06T01a
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ESH1/PER0a/F06T07a
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ESH1/PER0a/F06T10a
NDEVON/PER0a/Y5b
SVG2/PER0a/Y167a
SVG2/PER0a/Y169a
SVG2/PER0a/Y174a
SVG2/PER0a/Y179a
SVG/PER0a/Flow01a
SVG/PER0a/Flow02a
SVG/PER0a/Flow03a
SVG/PER0a/Flow04a
SVG/PER0a/Y72a
SVG/PER0a/Y73a
SVG/PER0a/Y74a
SVG/PER0a/Y75a
SVG/PER0a/Y76a
SVG/PER0a/Y77a
SVG/PER0a/Y78a
SVG/PER0a/Y79a
SVG/PER0a/Y80a
SVG/PER0a/Y81a
SVG/PER0a/Y82a
SVG/PER0a/Y83a
SVG/PER0a/Y84a
SVG/PER0a/Y85a
SVG/PER0a/Y86a
SVG/PER0a/Y87a
SVG/PER0a/Y88a
References:
Pierce, C., 2024, Advanced Analysis of the Sub-Glacial Environment Using Radar Echo Sounding Simulations, Ph. D. Thesis, Montana State University
Pierce, C., Gerekos, C., Skidmore, M., Beem, L., Blankenship, D., Lee, W. S., Adams, E., Lee, C.-K., and Stutz, J., 2024, Characterizing sub-glacial hydrology using radar simulations, The Cryosphere, 18, 4, 1495--1515, 10.5194/tc-18-1495-2024
Pierce, C., Skidmore, M., Beem, L., Blankenship, D., Adams, E., and Gerekos, C., 2024, Exploring canyons beneath Devon Ice Cap for sub-glacial drainage using radar and thermodynamic modeling, Journal Of Glaciology, 1--18, 10.1017/jog.2024.49
Lindzey, L., Quartini, E., Buhl, D., Blankenship, D., Richter, T., Greenbaum, J., and Young, D., 2017, KRT1/LGV1 Season Field Report, 237 10.26153/tsw/11620
Lindzey, L. E., Beem, L. H., Young, D. A., Quartini, E., Blankenship, D. D., Lee, C.-K., Lee, W. S., Lee, J. I., and Lee, J., 2020, Aerogeophysical characterization of an active subglacial lake system in the David Glacier catchment, Antarctica, The Cryosphere, 14, 7, 2217--2233, 10.5194/tc-14-2217-2020
Peters, M. E., Blankenship, D. D., Carter, S. P., Young, D. A., Kempf, S. D., and Holt, J. W., 2007, Along-track Focusing of Airborne Radar Sounding Data From West Antarctica for Improving Basal Reflection Analysis and Layer Detection, IEEE Transactions On Geoscience And Remote Sensing, 45, 9, 2725-2736, 10.1109/TGRS.2007.897416Rutishauser, A., Blankenship, D. D., Young, D. A., Wolfenbarger, N. S., Beem, L. H., Skidmore, M. L., Dubnick, A., and Criscitiello, A. S., 2022, Radar sounding survey over Devon Ice Cap indicates the potential for a diverse hypersaline subglacial hydrological environment, The Cryosphere, 16, 379-395, https://doi.org/10.5194/tc-16-379-2022
Schroeder, D. M., Blankenship, D. D., Raney, R. K., and Grima, C., 2015, Estimating subglacial water geometry using radar bed echo specularity: application to Thwaites Glacier, West Antarctica, IEEE Geoscience And Remote Sensing Letters, 12, 3, 443-447, 10.1109/LGRS.2014.2337878
Young, D. A., Schroeder, D. M., Blankenship, D. D., Kempf, S. D., and Quartini, E., 2016, The distribution of basal water between Antarctic subglacial lakes from radar sounding, Philosophical Transactions Of The Royal Society A, 374, 20140297, 1-21, 10.1098/rsta.2014.0297
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Replication Data for: Cation–polymer interactions and local heterogeneity determine the relative order of alkali cation diffusion coefficients in PEGDA hydrogels
No full textSupporting data for this publication
Descripción topográfica de la Jurisdicción del Real y Minas de Zimapán, 1789 enero 28
No full textEl texto proporciona una descripción detallada de las Minas Reales de Zimapán, conocidas como "damabuezta" en el idioma otomí. La descripción incluye su contexto histórico, gobierno, demografía (compuesta por españoles, indígenas y negros), autoridades religiosas y lugares de culto, geografía, clima, flora, fauna y actividades económicas. La principal actividad económica es la minería de plata, con varias minas en operación, incluyendo la mina Cañas y la mina Lomo de Toro. Otros minerales encontrados en la región incluyen oro, plomo, azufre, arsénico, salitre y varios tipos de piedra adecuados para la construcción y la ornamentación. El informe también describe las hierbas medicinales de la región. Concluye con detalles sobre las estadísticas demográficas recientes de la jurisdicción y la elección de Diputados Mineros. Se adjuntan dos mapas: "Plano iconográfico horizontal de toda la jurisdicción de las Minas Reales de Zimapán" y "Plano horizontal del trazado del Real de Zimapán"; las transcripciones incluyen texto escrito en los mapas. —— The text provides a detailed overview of the Royal Mines of Zimapán, which are known as "damabuezta" in the Otomi language. The description includes its historical background, governance, population demographics (comprising of Spanish, Indigenous, and Black people), religious officials and places of worship, geography, climate, flora, fauna, and economic activities. The main economic activity is silver mining, with various mines in operation, including the Cañas and the Lomo de Toro mine. Other minerals found in the region include gold, lead, sulfur, arsenic, saltpeter, and various types of stone suitable for construction and ornamentation. The report also describes the region's medicinal herbs. The report concludes with details about the jurisdiction's recent demographic statistics and the election of Mining Deputies. Appended are two maps: "Horizontal iconographic plan of the entire jurisdiction of the Royal Mines of Zimapán" and "Horizontal plan of the layout of the Real de Zimapán"; the transcriptions include text written on the maps. 6 f. (12 p.
Chapter III: Roosting Behaviors and Differences
No full textData associated with… Langlois, G. D., & Stevens, R. D. (2024). Comparison of Roosting Behavior Between Two Disparate Landscapes by a Neotropical Bat (Artibeus lituratus) in the Atlantic Forest of Paraguay. Behavioral Ecology and Sociobiology [Featured Student Research Paper], 78 (10), 106
Replication Data for: Polymer Architecture-Induced Trade-off between Conductivities and Transference Numbers in Salt-Doped Polymeric Ionic Liquids
No full textSupporting data for this publication
Manuscript Matrix, data collection, and analysis
No full textThis manuscript matrix was used to screen articles, extract data, and analyze the data
Data to Support Automated Georeferencing Workflow for Historical Sanborn Fire Insurance Maps of Texas
No full textThis dataset contains the input data files that were required for implementing an automated Sanborn Fire Insurance map georeferencing workflow
Real cédula sobre la creación de un colegio clerical en la diócesis de Durango, 1819 enero 30
No full textCédula real al Virrey de Nueva España sobre la creación de un colegio clerical en la diócesis de Durango. El obispo, Don Juan Francisco de Castañiza y Larrea, Marqués de Castañiza, propuso erigir el Colegio Clerical de San Luis Gonzaga para instruir a los eclesiásticos de su obispado, corregir a los extraviados y permitir la vida retirada para aquellos que lo deseen. Basó su propuesta en el modelo del Colegio de Tepotzotlán, erigido por el Arzobispo Alonso Núñez de Haro. El Rey remitió la propuesta al Consejo de las Indias, el cual la consideró muy favorablemente. Se decidió encargar al Virrey de México, junto con el obispo, la formación de un expediente instructivo para adoptar los medios necesarios para el colegio clerical. —— Royal decree to the Viceroy of New Spain regarding the creation of a clerical college in the diocese of Durango. The bishop, Don Juan Francisco de Castañiza y Larrea, Marquess of Castañiza, proposed to establish the Clerical College of San Luis Gonzaga to educate the clergy of his diocese, correct those who have gone astray, and provide a retreat for those who wish to lead a secluded life. He based his proposal on the model of the College of Tepotzotlán, founded by Archbishop Alonso Núñez de Haro. The King referred the proposal to the Council of the Indies, which viewed it very favorably. It was decided to instruct the Viceroy of Mexico, along with the bishop, to prepare an instructive record to adopt the necessary measures for the clerical college. 2 f. (4 p.