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672 results for “August”
Data pertaining to lobster phyllosoma, Panulirus interruptus, collection methods, locations, identification and staging (1951-2008, months of July and August)
The very large collection of plankton hauls taken in connection with the California Cooperative Oceanic Fisheries Investigations (CalCOFI) has afforded a unique opportunity to study the occurrence and distribution of the phyllosoma larvae of the spiny lobster. JOHNSON, MARTIN W. 1960. The Distribution of Larvae of the Spiny Lobster, Panulirus interruptus (Randall) with Records on P. Gracilis Streets. California Cooperative Fisheries Investigation 7: 413-46.
Numerical (No m-3) concentrations (mg m-3) of subsurface microplastic debris collected by bongo net aboard the Scripps Environmental Accumulation of Plastic Expedition (SEAPLEX) cruise, August 2009.
Microplastic was collected using a standard bongo net tow. Each sample was sorted at 6-12x magnification under a Wild M-5 dissecting microscope, and plastic particles and removed for further analysis. Plastic particles were soaked in deionized water to remove salts, dried at 60°C, and stored in a desiccator. Dry mass was measured on an analytical balance. Particles were then digitally imaged with a Zooscan digital scanner (Gorsky et al. 2010). The total number of particles was measured using NIH ImageJ-based tools in the Zooprocess software, calibrated against manual measurements (Gilfillan et al. 2009, Gorsky et al. 2010)
Feret diameter (mm), area (mm2), and circularity of microplastic debris collected by manta net aboard the Scripps Environmental Accumulation of Plastic Expedition (SEAPLEX) cruise, August 2009, and NOAA Okeanos Explorer expedition, 2010.
Microplastic was collected using a standard manta net tow. Each sample was sorted at 6-12x magnification under a Wild M-5 dissecting microscope, and plastic particles and H. sericeus removed for further analysis. Plastic particles were soaked in deionized water to remove salts, dried at 60°C, and stored in a desiccator. Particles were then digitally imaged with a Zooscan digital scanner (Gilfillan et al. 2009, Gorsky et al. 2010)
Microplastic measurements including, mass, color, particle type and plastic type collected aboard the Scripps Environmental Accumulation of Plastic Expedition (SEAPLEX) cruise, August 2009.
Microplastic was collected using a standard manta net tow. Each sample was sorted at 6-12x magnification under a Wild M-5 dissecting microscope, and plastic particles and H. sericeus removed for further analysis. Plastic particles were soaked in deionized water to remove salts, dried at 60°C, and stored in a desiccator. Particles were then digitally imaged with a Zooscan digital scanner (Gilfillan et al. 2009, Gorsky et al. 2010)
Pyrocumulonimbus Events over British Columbia in August 2017: Results from the NASA GEOS Earth System Model
Model data associated with the manuscript submitted in Atmospheric Chemistry and Physics Journal, titled, " Pyrocumulonimbus Events over British Columbia in 2017: The Long-term Transport and Radiative Impacts of Smoke Aerosols in the Stratosphere". Abstract. Interactions of meteorology with wildfires in British Columbia, Canada during August 2017 led to three major pyrocumulonimbus (pyroCb) events that resulted in the injection of large amounts of smoke aerosols and other combustion products at the local upper troposphere and lower stratosphere (UTLS). These plumes of UTLS smoke with elevated values of aerosol extinction and backscatter compared to the background state were readily tracked by multiple satellite-based instruments as they spread across the Northern Hemisphere (NH). The plumes resided in the lower stratosphere for about 8-10 months following the fire injections. To investigate the radiative impacts of these events on the Earth system, we performed a number of simulations with the Goddard Earth Observing System (GEOS) atmospheric general circulation model (AGCM). Observations from multiple remote-sensing instruments were used to calibrate the injection parameters (location, amount, composition, and heights) and optical properties of the smoke aerosols in the model. The resulting simulations of three-dimensional smoke transport were evaluated for a year from the day of injections using daily observations from OMPS-LP (Ozone Mapping Profiler Suite Limb Profiler). The model simulated rate of ascent, hemispheric spread, and residence time of the smoke aerosols in the stratosphere are in close agreement with OMPS-LP observations. We found that both aerosol self-lofting and the large-scale atmospheric motion play important roles in lifting the smoke plumes from near the tropopause altitudes (~12 km) to about 22-23 km into the atmosphere. Further, our estimations of the radiative impacts of the pyroCb-emitted smoke aerosols showed that the smoke caused additional warming of the atmosphere by about 0.6-1 W/m2 (zonal mean) that persisted for about 2-3 months after the injections in regions north of 40oN. The surface experienced a comparable magnitude of cooling. The atmospheric warming is mainly located in the stratosphere, coincident with the location of the smoke plumes, leading to an increase in zonal mean shortwave (SW) heating rates of 0.02-0.04 K/day during September 2017.
ALMA Titan image cubes for CH3CN, HC3N and HNC observed August 2016 and May 2017
<p>These 3D FITS files contain spectral line emission flux from Titan (in Janskys per beam) as a function of RA, dec. and frequency, observed using Atacama Large Millimeter/submillimeter Array (ALMA).</p> <p>ALMA observations of Titan were obtained on 2017-05-08 and 2017-05-16 (as part of ALMA program 2016.A.00014.S; PI: Cordiner) and on 2016-08-18 and 2016-08-19 (as part of ALMA program 2015.1.01023.S; PI: Gurwell). The HNC (J=4-3), HC3N (J=40-39) and CH3CN (J=19-18) transitions were observed in 2017, whereas the HNC (J=4-3), HC3N (J=39-38) and CH3CN (J=19-18) were observed in 2016.</p> <p>The raw observations were calibrated using standard scripts supplied by the observatory. The resulting measurement sets were continuum-subtracted using low-order polynomial fits to the line-free spectral regions adjacent to our lines of interest. The data were then imaged and cleaned (deconvolved) using the tclean algorithm in CASA 5.6. This routine implicitly corrects for the time-variability of Titan's position and radial velocity with respect to the observer, so the resulting image cubes are in the rest frame of Titan's center-of-mass. To facilitate meaningful intercomparisons, accounting for Titan's varying Geocentric distance, the 2016 and 2017 datasets were convolved to common circular beam dimensions, as projected in the plane of the sky. The image cubes were then cropped to isolate the emission lines of interest.</p>
Metabolomics.Info People Portal Data as of 3 August 2020
<p>Metabolomics.Info People Portal Data as of 3 August 2020 in <a href="https://www.w3.org/TR/n-triples/">N-Triples</a> format.</p>
Earthquakes in Spain - August to October 2020
<p>Earthquakes in Spain from 1st August 2020 to 30th October 2020.</p> <p>Fields:</p> <ul> <li>Date (DD/MM/YYYY)</li> <li>Time UTC (hh:mm:ss)</li> <li>Latitude (signed float)</li> <li>Latitude Cardinal (character)</li> <li>Longitude (signed float)</li> <li>Longitude Cardinal (character)</li> <li>Depth (integer)</li> <li>Magnitude Type (string)</li> <li>Magnitude (unsigned float)</li> <li>Region (string)</li> <li>Last Update (DD/MM/YYYY hh:mm:ss)</li> <li>Earthquake ID (integer)</li> </ul>
Turbulence profiles from the R/V Sanna cruise to Northwest Greenland fjords, August 11-31, 2016
<p>The data set contains micro-scale turbulence measurements from six fjords along northwestern Greenland carried out on the R/V Sanna cruise in August 2016. The data set is described and analysed in:</p> <p>Bendtsen, J., Rysgaard, S., Carlson, D. F., Meire, L., & Sejr, M. K. (2021). Vertical mixing in stratified fjords near tidewater outlet glaciers along Northwest Greenland. <em>Journal of Geophysical Research: Oceans</em>, 126, e2020JC016898. <a href="https://doi.org/10.1029/2020JC016898">https://doi.org/10.1029/2020JC016898</a></p> <p>Please cite this publication when using the data.</p>
PheKnowLator Human Disease KG Benchmarks: Instance-Standard Relations-OWL (v2.1.0 - August 2021)
<p><strong>PKT Human Disease Knowledge Graph Benchmark Builds (v2.1.0)</strong></p><p><strong>Build Type: </strong><i>Instance-Standard Relations-OWL</i></p><p><strong>Build Date: </strong>August 01, 2021</p><p> </p><h3><strong>Important Build Information</strong></h3><p>The benchmarks were originally built and stored using Google Cloud Platform (GCP) resources. For details and a complete description of this process, can be found on GitHub (<a href="https://github.com/callahantiff/PheKnowLator/tree/master/builds#readme">here</a>). Note that we have developed an archive for the builds on Zenodo. While the original GCP resources contained all associated files, due to the file size upload limits associated with each archive, we have limited the uploaded files to the KGs, associated metadata, and log files. The list of resources, including their URLs, and date of download, can all be found in the associated logs.</p><p>Details on each of the files generated by the build process can be found in the file associated with this directory (<a href="https://zenodo.org/records/10065431/files/PheKnowLator_HumanDiseaseKG_Output_FileInformation.xlsx?download=1">PheKnowLator_HumanDiseaseKG_Output_FileInformation.xlsx</a>).</p><p> </p><p>🚨 <strong>AVAILABLE FILES </strong>🚨 </p><ul><li>Available KG benchmark files are zipped and listed below.</li><li>For additional details on what each file contains, please see the associated Wiki page 👉 <a href="https://github.com/callahantiff/PheKnowLator/wiki/August-01%2C-2021">here</a>.</li></ul>
August-September maximum temperature reconstruction for the Southeastern United States (1760-2022 CE)
<p>Over recent decades, the southeastern United States (Southeast) has become increasingly well represented by the terrestrial climate proxy record. However, while the paleo proxy records capture the region's hydroclimatic history over the last several centuries, the understanding of near-surface air temperature variability is confined to the comparatively shorter observational period (1895-present). Here, we detail the application of blue intensity (BI) methods on a network of tree-ring collections and examine their utility for producing robust paleotemperature estimates. Results indicate that maximum latewood BI (LWBI) chronologies exhibit positive and temporally stable correlations (<em>r </em>= 0.28- 0.54<em>, p </em>< 0.01) with summer maximum temperatures. As such, we use a network of LWBI chronologies to reconstruct the August-September average maximum temperatures for the Southeast spanning the period 1760-2010 CE. Our work demonstrates the utility of applying novel dendrochronological techniques to improve the understanding of the longer-term temperature history of the Southeast.</p>
FIGURE 3 in Avian type localities and the type specimens collected by Johan August Wahlberg in southern Africa
FIGURE 3. Wahlberg's camps and collecting sites (red dots) in the North West Province 1842–1844.
Figure 1 from: Jansen JJFJ (2017) René Maugé's ornithological collections from Kupang Bay, West-Timor, Indonesia, August-November 1801, with special regard to type-specimens. Zoosystematics and Evolution 93(2): 467-492. https://doi.org/10.3897/zse.93.19964
Figure 1 - MNHN A.C. 6490: Pedestal underside of Loxia fuscata. It shows a sticker glued. The same stickers are used on multiply specimens collected in either Australia and Timor. The handwriting is from Louis Dufresne and only used on specimens brought back with Le Naturaliste.
21 August 2017 total solar eclipse penumbra
<p>Projection of the 19.3nm penumbra 300 km altitude.</p>
Figure 5 from: Murphy JC, Braswell AL, Charles SP, Auguste RJ, Rivas GA, Borzée A, Lehtinen RM, Jowers MJ (2019) A new species of Erythrolamprus from the oceanic island of Tobago (Squamata, Dipsadidae). ZooKeys 817: 131-157. https://doi.org/10.3897/zookeys.817.30811
Figure 5 A, B Variations in the olive color morph of Erythrolampruszweifeli from Trinidad (photographs by Michael Patrikeev) C the middle photo shows the "salt and pepper" morph that occurs at higher elevation (photograph by JCM). Both color morphs are included in our molecular sample DE.zweifeli Rancho Grande, Parque Nacional Henri Pittier, Luis A. Rodriguez J. E the Royal Snake, Erythrolamprusreginae from Kaiteur, Guyana (photograph by P Kok).
Figure 6 from: Murphy JC, Braswell AL, Charles SP, Auguste RJ, Rivas GA, Borzée A, Lehtinen RM, Jowers MJ (2019) A new species of Erythrolamprus from the oceanic island of Tobago (Squamata, Dipsadidae). ZooKeys 817: 131-157. https://doi.org/10.3897/zookeys.817.30811
Figure 6 Erythrolampruspseudoreginae.AUWIZM 2016.22.45, holotype B–D FLMNH 91621 from Gilpin Trace, on Tobago's Main Ridge. B Profile. Of the four specimens examined this was the only one that had nine upper labials (on one side only) C The posterior lateral stripe bordered by a dorsal light stripe D Venter mostly uniform with patches of scattered pigment.
Figure 4 from: Murphy JC, Braswell AL, Charles SP, Auguste RJ, Rivas GA, Borzée A, Lehtinen RM, Jowers MJ (2019) A new species of Erythrolamprus from the oceanic island of Tobago (Squamata, Dipsadidae). ZooKeys 817: 131-157. https://doi.org/10.3897/zookeys.817.30811
Figure 4 Geographic distribution of the five species of Erythrolamprus under discussion in this paper. A The distribution of the species of Erythrolamprus under discussion in northern Venezuela and Trinidad and Tobago B More detailed view of the distribution on Trinidad and Tobago C Tobago with the known localities for E.pseudoreginae sp. n. Note that two of the markers closely overlap. Key: black stars = E.zweifeli from Cordillera de Costa in Venezuela and the island of Trinidad; green circles = E.epinephalus from the Cordillera de Mérida, Venezuela. Note that these markers denote the closest population to Tobago based on Roze (1966). Specimens examined came from several different locations. Purple stars = E.reginae from the Guianas including Orinoco Delta in Venezuela; red stars = E.melanotus from Venezuela, Trinidad, and Tobago; blue star = Erythrolampruspseudoreginae sp. n. on Tobago.
Figure 3 from: Murphy JC, Braswell AL, Charles SP, Auguste RJ, Rivas GA, Borzée A, Lehtinen RM, Jowers MJ (2019) A new species of Erythrolamprus from the oceanic island of Tobago (Squamata, Dipsadidae). ZooKeys 817: 131-157. https://doi.org/10.3897/zookeys.817.30811
Figure 3 A comparison of the scale arrangements on the crowns and ventral heads of the Erythrolamprus taxa under discussion. AE.pseudoreginae sp. n. from Tobago BE.epinephalus from Venezuela MBLUZ 1501 (dorsal view) and 1500 (ventral view) C, D Salt and pepper morph of E.zweifeli from Trinidad and Venezuela E An olive-brown morph of E.zweifeli Trinidad, FMNH 215827 F A melanistic morph of E.zweifeli from Venezuela EBRG 2745.
Figure 2 from: Murphy JC, Braswell AL, Charles SP, Auguste RJ, Rivas GA, Borzée A, Lehtinen RM, Jowers MJ (2019) A new species of Erythrolamprus from the oceanic island of Tobago (Squamata, Dipsadidae). ZooKeys 817: 131-157. https://doi.org/10.3897/zookeys.817.30811
Figure 2 A comparison of the five members of the Erythrolamprusreginae group. AE.reginae for Guyana (FMNH 30959) BE.zweifeli from Venezuela (FMNH 204477) CE.melanotus from Tobago (UWIZM.2012.42.19) DE.pseudoreginae sp. n. from Tobago (FLMNH 91621) EE.epinephalus from Venezuela (MBLUZ 1502).
Figure 1 from: Murphy JC, Braswell AL, Charles SP, Auguste RJ, Rivas GA, Borzée A, Lehtinen RM, Jowers MJ (2019) A new species of Erythrolamprus from the oceanic island of Tobago (Squamata, Dipsadidae). ZooKeys 817: 131-157. https://doi.org/10.3897/zookeys.817.30811
Figure 1 Bayesian inference tree of Erythrolamprus species from Genbank MtDNA 12S+16SrDNA+c-mos sequences (1332 bp). Red stars indicate Bayesian inference and ML posterior probabilities (> 95%) and bootstrap (> 70%) support values above and below nodes, respectively. Clade in orange shows E.zweifeli, in green E.melanotus, and in blue E.pseudoreginae sp. n. (AF158433) is from French Guiana, and E.reginae (JQ598983) is from Brazil.
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Allen Brain Atlas
Allen Brain Atlas is an Allen Institute collection of brain map atlases, datasets, APIs, and analysis tools covering mouse, human, and non-human primate brain resources.
Annotated Behaviour and Observability Dataset (ABODe)
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