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5,155 results for “resolution”

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zenodo36/100

Online Aerosol Chemical Characterization by Extractive Electrospray Ionization − Ultrahigh-Resolution Mass Spectrometry (EESI-Orbitrap)

<p>These datasets are the raw data presented in the presented work of &quot;Online Aerosol Chemical Characterization by Extractive Electrospray Ionization &minus; Ultrahigh-Resolution Mass Spectrometry (EESI-Orbitrap)&quot; in <em>Environmental Science &amp; Technology Journal</em>, doi:10.1021/acs.est.9b07090.</p> <p>Abstract:&nbsp;Current mass spectrometry techniques for the online&nbsp;measurement of organic aerosol (OA) composition are subjected to either&nbsp;thermal/ionization-induced artifacts or limited mass resolving power,&nbsp;hindering accurate molecular characterization. Here, we combined the soft&nbsp;ionization capability of extractive electrospray ionization (EESI) and the&nbsp;ultrahigh mass resolution of Orbitrap for real-time, near-molecular&nbsp;characterization of OAs. Detection limits as low as tens of ng m<sup>&minus;3</sup> with&nbsp;linearity up to hundreds of &mu;g m<sup>&minus;3</sup> at 0.2 Hz time resolution were&nbsp;observed for single- and mixed-component calibrations. The performance of the EESI-Orbitrap system was further evaluated with laboratory-generated secondary OAs (SOAs) and filter extracts of ambient particulate&nbsp;matter. The high mass accuracy and resolution (140 000 at <em>m/z</em> 200) of&nbsp;the EESI-Orbitrap system enable unambiguous identification of the&nbsp;aerosol components&rsquo; molecular composition and allow a clear separation&nbsp;between adjacent peaks, which would be significantly overlapping if a medium-resolution (20 000) mass analyzer was used.&nbsp;Furthermore, the tandem mass spectrometry (MS<sup>2</sup>) capability provides valuable insights into the compound structure. For instance,&nbsp;the MS<sup>2</sup> analysis of ambient OA samples and lab-generated biogenic SOAs points to specific SOA precursors in ambient air among a&nbsp;range of possible isomers based on fingerprint fragment ions. Overall, this newly developed and characterized EESI-Orbitrap system&nbsp;will advance our understanding of the formation and evolution of atmospheric aerosols.</p> <p>Structure of the datasets: The raw data are separated into individual file of&nbsp;excel format for the figures. Simulation data from Figure 4 can be generated using the matlab code named <em>Figure4PeakSimulation.m.</em>&nbsp;</p>

opencc-by-4.0Mar 2020View details →
zenodo36/100

High resolution deformation data from the surface of a Nickel-based superalloy: Fine precipitates

<p>High resolution digital image correlation (HRDIC) and electron backscattered diffraction (EBSD) data provided that quantifies the&nbsp;deformation on the surface of Nickel-based superalloy with fine gamma prime precipitates (70 nm diameter)&nbsp; after 2% strain in tension.</p>

openapache2.0Feb 2020View details →
zenodo36/100

High resolution WRF simulation of Hurricane Sandy (2012) wind during landfall

<p>A 96-hour high-resolution simulation of Hurricane Sandy was conducted using the Advanced Research version 3.3.1 of the Weather Research and Forecasting (WRF) model initialized at 1200 UTC 26 October 2012 (Johnsen et al., 2013) and using a horizontal resolution of 500 m. Domain size was 2,660x2,500 km with 150 vertical layers. The Yonsei University planetary boundary layer (PBL) scheme, the Noah land model, and the MM5 Monin-Obukhov similarity theory surface layer model were used. Cloud physics was modeled using WSM6 6-class microphysics with graupel. Convection parameterization was not used for this high-spatial-resolution simulation. National Centers for Environmental Prediction (NCEP) Global Forecast System (GFS) analyses were used for initialization and boundary conditions, with the latter updated every 6 hours.</p> <p>Data herein is a landfall-regime subset (Schiavone et al., 2016) of the full simulation. The spatial domain is 500x500 km containing the 50 lowest layers, with a time domain that spans the 12-hour period beginning at1200 UTC 29 October 2012 and with 3-hour time steps. Format is NetCDF containing detailed metadata. Three-dimensional meteorological field variables include the 3 wind components, potential temperature, water vapor mixing ratio, geopotential, and atmospheric pressure. Two-dimensional variables include horizontal wind components at 10 m AGL, potential temperature and water vapor mixing ratio at 2 m AGL, atmospheric pressure at the surface, terrain height, and the Coriolis sine latitude term, which is required to calculate potential vorticity.</p> <p>These WRF simulation data were used, along with WSR-88D Doppler radar data and surface wind observations, to demonstrate that roll vortices occurred in the atmospheric boundary layer over the landfall region during Hurricane Sandy&#39;s landfall period (Schiavone et al., 2020).</p>

opencc-by-4.0Apr 2020View details →
zenodo36/100

Dataset of "Gravity Wave Activity in the Atmosphere of Mars During the 2018 Global Dust Storm: Simulations With a High-Resolution Model" (2/2)

<p>This dataset contains the GrADS data of high-resolution Mars GCM results used for figures in the paper &nbsp;&quot;Gravity Wave Activity in the Atmosphere of Mars During the 2018 Global Dust Storm: Simulations With a High-Resolution Model&quot; by T. Kuroda, A.S. Medvedev and E. Yiğit.</p> <p>Each file contains two-dimensional (X: longitude, Y: latitude) data of surface pressure (Ps) and dust opacity in infrared wavelength (tau), and three-dimensional (X: longitude, Y: latitude, Z:sigma-level) data of temperature (T), zonal wind velocity (u), meridional wind velocity (v) and vertical wind velocity (w). Each tar.xz file contains snapshots of those data in every 1/6 Sol for Ls of 30 degrees. The dust scenario implemented for producing this dataset is taken from Montabone et al. (2020).</p> <p>data270rdc-my34.tar.xz: for Ls=270-300 (48 Sols)</p> <p>data300rdc-my34.tar.xz: for Ls=300-330 (51 Sols)</p> <p>data330rdc-my34.tar.xz: for Ls=330-360 (56 Sols)</p>

opencc-by-4.0Apr 2020View details →
zenodo36/100

High-resolution wind power generation time series for Germany in the period 2000-2015

<p>High-resolution wind power generation time series for Germany in the period 2000-2015. A paper describing the applied methodology can be found in this repository as well.</p> <p>The final temporal resolution is hourly and the spatial resolution NUTS 3. The data is stored in csv and hdf5 files.</p> <p>More information on the data set, e.g. missing time stamps and versioning, can be found in readme.txt.</p>

opencc-by-4.0Mar 2018View details →
zenodo36/100

High resolution cryoEM structure of huntingtin in complex with HAP40

<p><strong>High resolution cryoEM structure of huntingtin in complex with HAP40</strong></p> <p>This dataset relates the following depositions in the&nbsp;PDB:&nbsp;6X9O and&nbsp;EMDB:&nbsp;EMD-22106 which are the structure solution of HTT-HAP40 complex at 2.6 angstrom resolution by cryoEM.&nbsp;</p> <p>Files contained within this dataset are detailed in the &quot;Upload_information.xlsx&quot; file.&nbsp;</p> <p>&nbsp;</p>

opencc-by-4.0Jun 2020View details →
zenodo36/100

Beef database for prediction of main environmental challenges to resilience and efficiency in cattle production systems at regional resolution

<p>The beef database comprises average values for a wide range of variables (110 or 119), available in 4 worksheets, and is further differentiated into All Beef, Breeders and Fatteners: BasicFarmType (18 rows), DetailedFarmType (75 rows), ClimateClass+BasicFarmType (270 rows), NUTS+BasicFarmType (2074 rows). Data are omitted when the sample size (n) is below 15, as per the confidentiality agreement under FADN data use rules.</p> <p>A combined farm characterisation database was constructed using two major data sources, the Farm Accountancy Data Network (FADN), and the Gridded Agro-Meteorological Data in Europe (AGRI4CAST). The database initially constructed was further enhanced through the addition of forage and crop yield data from the Food and Agriculture Organization of the United Nations (FAO) and the International Institute for Applied Systems Analysis (IIASA) developed Agro-Ecological Zones (AEZ) methodology database (FAO, 2012). The data was processed and is presented in D1.2 as two databases (dairy and beef), as averages for a wide range of variables at basic or detailed farm types, and at NUTS2 regional scale.</p> <p>Detailed FADN data (anonymised individual farm data) was requested for all ruminant and mixed farm types, over 10 years and the most recent data available at request (2011-2013) was utilised for the analysis. Following receipt of the data (~250k farms) this has been compiled into two consistent datasets, one for dairy (141,961) farms and one for beef farms (54,417). Each dataset comprises some values directly from the FADN data, but also a large number of calculated variables, to identify dairy or beef enterprise performance at per animal, per output product unit or per hectare. These values were calculated according to the respective dairy and beef enterprise allocation methodologies described by FADN. Further economic and structural variables have been calculated as necessary, as described in GenTORE D1.1 (Qui&eacute;deville et al., 2019).</p> <p>For each farm within the dataset, the structural, production and economic data from the FADN data is supplemented with the addition of meteorological data. The daily meteorological data was downloaded from the AGRI4STAT database web portal at a NUTS2 scale. For each NUTS2 region data was available for a number of weather stations. This large dataset was processed through scripts in STATA software to generate annual values for a wide range of climatic variables, including Temperature Humidity Index (THI), and indicators of drought and seasonality of weather. Furthermore, the altitude values per weather station allowed for a sub-grouping of weather station data by altitude zone (aligned with values available in the FADN dataset).</p> <p>Using a Latent Class Analysis process, the meteorological data was analysed to identify consistent environmental regions in Europe. Selected climatic variables, together with altitude zone, were utilised to statistically identify differing zones, and to classify each NUTS2 region to a zone, resulting in 6 lowland zones and 3 upland zones (above 600m) The LCA process enhanced an earlier method of manually overlaying the Metzger et al. (20054) pedo-climatic zone allocation, but closely correlates. Therefore for each farm in the dairy and beef datasets, meteorological and environmental zone data was allocated on a NUTS2 by altitude zone basis and this dataset has been subsequently assessed and submitted as papers; Qui&eacute;deville et al., (submitted May 2020) and Grovermann et al. (submitted May 2020).</p> <p>The GAEZ forage and crop yield data was downloaded from the GAEZ data portal as baseline and two future climate prediction periods: Baseline (1961-2000), 2020s (2011-2040), and 2050s (2041-2070), for the Hadley CM3 model and IPCC scenario A (the most extreme scenario). See: <a href="http://www.fao.org/nr/gaez/about-data-portal/agro-climatic-resources/en/">http://www.fao.org/nr/gaez/about-data-portal/agro-climatic-resources/en/#</a>). A zonal statistics was applied to the GAEZ layers to aggregate the data to NUT2 region and altitude zone (0-300m, 300-600m, 600m+) with raster package in R. The result is an average yield<a href="#_ftn1">[1]</a> for varying forages and crops for each altitude zone in each nuts2, for both the baseline and the future climate scenario. This data allows further analysis of the future impacts on cattle farming at both a regional scale, but also by farm type or system, which may be affected differently (Moakes et al. in preparation).</p> <p>All variable processing from FADN data is shown in the Annex, as performed in Stata software.</p> <p>&nbsp;</p> <p><a href="#_ftnref1">[1]</a> The mean was performed on non-zero yield pixels in order to exclude non-suitable areas from average.</p>

opencc-by-4.0May 2020View details →
zenodo36/100

Dairy database for prediction of main environmental challenges to resilience and efficiency in cattle production systems at regional resolution

<p>The dairy database comprises average values for a wide range of variables (110 or 119), available in 4 worksheets: BasicFarmType (18 rows), DetailedFarmType (10 rows), ClimateClass+BasicFarmType (100 rows), NUTS+DetailedFarmType (1452 rows). Data are omitted when the sample size (n) is below 15, as per the confidentiality agreement under FADN data use rules.</p> <p>A combined farm characterisation database was constructed using two major data sources, the Farm Accountancy Data Network (FADN), and the Gridded Agro-Meteorological Data in Europe (AGRI4CAST). The database initially constructed was further enhanced through the addition of forage and crop yield data from the Food and Agriculture Organization of the United Nations (FAO) and the International Institute for Applied Systems Analysis (IIASA) developed Agro-Ecological Zones (AEZ) methodology database (FAO, 2012). The data was processed and is presented in D1.2 as two databases (dairy and beef), as averages for a wide range of variables at basic or detailed farm types, and at NUTS2 regional scale.</p> <p>Detailed FADN data (anonymised individual farm data) was requested for all ruminant and mixed farm types, over 10 years and the most recent data available at request (2011-2013) was utilised for the analysis. Following receipt of the data (~250k farms) this has been compiled into two consistent datasets, one for dairy (141,961) farms and one for beef farms (54,417). Each dataset comprises some values directly from the FADN data, but also a large number of calculated variables, to identify dairy or beef enterprise performance at per animal, per output product unit or per hectare. These values were calculated according to the respective dairy and beef enterprise allocation methodologies described by FADN. Further economic and structural variables have been calculated as necessary, as described in GenTORE D1.1 (Qui&eacute;deville et al., 2019).</p> <p>For each farm within the dataset, the structural, production and economic data from the FADN data is supplemented with the addition of meteorological data. The daily meteorological data was downloaded from the AGRI4STAT database web portal at a NUTS2 scale. For each NUTS2 region data was available for a number of weather stations. This large dataset was processed through scripts in STATA software to generate annual values for a wide range of climatic variables, including Temperature Humidity Index (THI), and indicators of drought and seasonality of weather. Furthermore, the altitude values per weather station allowed for a sub-grouping of weather station data by altitude zone (aligned with values available in the FADN dataset).</p> <p>Using a Latent Class Analysis process, the meteorological data was analysed to identify consistent environmental regions in Europe. Selected climatic variables, together with altitude zone, were utilised to statistically identify differing zones, and to classify each NUTS2 region to a zone, resulting in 6 lowland zones and 3 upland zones (above 600m) The LCA process enhanced an earlier method of manually overlaying the Metzger et al. (20054) pedo-climatic zone allocation, but closely correlates. Therefore for each farm in the dairy and beef datasets, meteorological and environmental zone data was allocated on a NUTS2 by altitude zone basis and this dataset has been subsequently assessed and submitted as papers; Qui&eacute;deville et al., (submitted May 2020) and Grovermann et al. (submitted May 2020).</p> <p>The GAEZ forage and crop yield data was downloaded from the GAEZ data portal as baseline and two future climate prediction periods: Baseline (1961-2000), 2020s (2011-2040), and 2050s (2041-2070), for the Hadley CM3 model and IPCC scenario A (the most extreme scenario). See: <a href="http://www.fao.org/nr/gaez/about-data-portal/agro-climatic-resources/en/">http://www.fao.org/nr/gaez/about-data-portal/agro-climatic-resources/en/#</a>). A zonal statistics was applied to the GAEZ layers to aggregate the data to NUT2 region and altitude zone (0-300m, 300-600m, 600m+) with raster package in R. The result is an average yield<a href="#_ftn1">[1]</a> for varying forages and crops for each altitude zone in each nuts2, for both the baseline and the future climate scenario. This data allows further analysis of the future impacts on cattle farming at both a regional scale, but also by farm type or system, which may be affected differently (Moakes et al. in preparation).</p> <p>All variable processing from FADN data is shown in the Annex, as performed in Stata software.</p> <p>&nbsp;</p> <p><a href="#_ftnref1">[1]</a> The mean was performed on non-zero yield pixels in order to exclude non-suitable areas from average.</p>

opencc-by-4.0May 2020View details →
zenodo36/100

The simulated dataset associated with the paper "Mesoscale modelling of optical turbulence in the atmosphere: The need for ultrahigh vertical grid resolution"

<p>The WRF model-generated meteorological profiles are available in netcdf format. More information will be provided shortly.&nbsp;</p>

opencc-by-4.0Jul 2020View details →
zenodo36/100

Global soil saturated hydraulic conductivity map using random forest in a Covariate-based GeoTransfer Functions (CoGTF) framework at 1 km resolution

<p>The global Ksat map at 1 km resolution was developed by harnessing the technological advances in machine learning and availability of remotely sensed surrogate information such as terrain, climate, vegetation, and soil covariates. We merge concepts of predictive soil mapping with a large data set of Ksat measurements and local information (soil, vegetation, climate) into covariate-based &ldquo;Geo Transfer Functions&#39;&#39; (CoGTFs) to generate global estimates of Ksat values (to highlight the impact of Geo-referenced covariates including various remote sensing maps, we use the term Geotransfer function GTF and not pedotransfer function PTF; in the latter case, typically only soil properties are used to estimate Ksat).</p> <p>The Ksat dataset is provided in GeoTIFF format. A total of 4 files that represent different soil depths (0, 30, 60, and 100 cm) are provided. The Ksat values are log-transformed (log10 Ksat) and cm/day was selected as a standardized unit.</p> <p>The Global Ksat training dataset used for this study is available here:<br> <a href="https://doi.org/10.5281/zenodo.3752721">https://doi.org/10.5281/zenodo.3752721</a></p> <p>The R code used for this study is available here:<br> <a href="https://github.com/ETHZ-repositories/Ksat_mapping_2020">https://github.com/ETHZ-repositories/Ksat_mapping_2020</a></p> <p>For more details / to cite this dataset please use:</p> <ul> <li>Gupta, S.,&nbsp;Lehmann, P., Bonetti, S., Papritz, A., and Or, D., (2020):&nbsp;<strong>Global prediction of soil saturated hydraulic conductivity using random forest in a Covariate-based Geo Transfer Functions (CoGTF) framework</strong>. Journal of Advances in Modeling Earth Systems,<strong> </strong>13(4), e2020MS002242. https://agupubs.onlinelibrary.wiley.com/doi/full/10.1029/2020MS002242</li> </ul> <p>Other datasets related to this project:</p> <p>The Global vG training dataset &nbsp;is available here:</p> <p><a href="https://doi.org/10.5281/zenodo.5547338">10.5281/zenodo.5547338</a></p> <p>Examples of using this dataset&nbsp;to generate van Genuchten parameters maps&nbsp;can be found in&nbsp;<a href="https://doi.org/10.5281/zenodo.6343570">10.5281/zenodo.6343570</a>.</p> <p>The study was supported by ETH Zurich (Grant ETH-18 18-1). We would like to thank Zhongwang Wei, Samuel Bickel and Simone Fatichi (ETH Zurich) for insightful discussions.</p> <p>&nbsp;</p> <p>&nbsp;</p>

opencc-by-4.0Dec 2019View details →
zenodo36/100

A 30-year high resolution simulation of the future climate over the Interior Western United States

<p>A high-resolution (4 km) convection-permitting regional climate simulation is conducted in the Interior Western United States (IWUS) using the Weather Research and Forecasting (WRF) model.&nbsp;The model integration is conducted over a 30-year period from&nbsp;October 1981 through September 2011, and over a 30-year future period centered at 2050 using the Pseudo&ndash;Global Warming (PGW)&nbsp;technique.&nbsp;The IWUS model output&nbsp;for the retrospective climate&nbsp;is available&nbsp;from https://doi.org/10.5281/zenodo.1157112.</p> <p>This repository contains a 30-year gridded dataset of&nbsp;precipitation, surface (2 m) temperature, surface pressure, water vapor mixing ratio at 2 m, and 10 m wind speed&nbsp;at a daily frequency from the IWUS simulation of future climate centered at 2050.&nbsp;Anyone interested in the full dataset of the IWUS&nbsp;simulation is encouraged to contact the lead author at&nbsp;yongganga.wang@gmail.com.</p>

opencc-by-4.0Jul 2020View details →
zenodo36/100

Using Resolution Proofs to Analyse CDCL SAT solvers

<p>Data for the article Janne I. Kokkala, Jakob Nordstr&ouml;m: Using Resolution Proofs to Analyse CDCL SAT solvers, accepted to the 26th International Conference on Principles and Practice of Constraint Programming.</p> <p>Files:</p> <ul> <li><strong>solver.tgz</strong> &ndash; Source code of the modified Glucose 3.0 used in the experiments</li> <li><strong>instances.tar</strong> &ndash; All CNF instances used in the experiments (compressed individually using xz). Note that these are the formulas obtained after preprocessing, so they are not the same as used in the SAT races and competitions they are obtained from.</li> <li><strong>data-instances.txt</strong> &ndash; List of all benchmark instance filenames and IDs used to refer to them in other data files.</li> <li><strong>data-solvers.txt</strong> &ndash; Parameters used for each solver configuration (see the paper for explanation of where they were used).</li> <li><strong>data-solverstats.txt</strong> &ndash; For each solver configuration and instance, some data of the run</li> <li><strong>data-proofsizes.txt</strong> &ndash; For each solver configuration and instance, sizes of untrimmed proof, the trimmed solver proof, and the proof output by DRAT-trim, measured both in number of learnt clauses and in number of clause usages &ndash; note that for the clause usage counts, all unit clauses are considered to be used only once at the end (since that would result to a shorter resolution proof and is more related to the solver performance)</li> <li><strong>data-features.txt</strong> &ndash; For the solver used in the clause feature experiments, this file contains for each instance the frequency distribution of each feature (both absolute and percentile rank)</li> <li><strong>plots-features.pdf</strong> &ndash; Larger versions of the feature plots in the paper, including plots not shown in the paper.</li> <li><strong>plots-proofsizes.pdf</strong> &ndash; Plots of the data for the pairwise solver proof size comparison experiments.</li> </ul> <p>&nbsp;</p>

opencc-by-4.0Jul 2020View details →
zenodo36/100

SCRINSHOT, a spatial method for single-cell resolution mapping of cell states in tissue sections (Revision data)

<p>The submitted dataset, correspond to the RAW&nbsp;(*.czi format) and analysis files of the <strong>revisions</strong> of manuscript &quot;SCRINSHOT, a spatial method for single-cell resolution mapping of cell states in tissue sections&quot;, which has been processed for revision (2020-01-31) by PLOS Biology.</p> <p>The files are in *.zip format and the naming&nbsp;follows thenumbering of the manuscript figures, which will be found in bioRxiv.org (<strong>ID#: BIORXIV/2020/938571</strong>).&nbsp; Each *.zip files contains a document with the description of&nbsp; all the provided files.</p>

opencc-by-4.0Aug 2020View details →
dryad36/100

Data From: TERRA-REF, An open reference data set from high resolution genomics, phenomics, and imaging sensors

<p>The ARPA-E funded TERRA-REF project is generating open-access reference datasets for the study of plant sensing, genomics, and phenomics. Sensor data were generated by a field scanner sensing platform that captures color, thermal, hyperspectral, and active flourescence imagery as well as three dimensional structure and associated environmental measurements. This dataset is provided alongside data collected using traditional field methods in order to support calibration and validation of algorithms used to extract plot level phenotypes from these datasets.</p> <p>Data were collected at the University of Arizona Maricopa Agricultural Center in Maricopa, Arizona. <br> This site hosts a large field scanner with fifteen sensors, many of which are capable of capturing mm-scale images and point clouds at daily to weekly intervals.</p> <p>These data are intended to be re-used, and are accessible as a combination of files and databases linked by spatial, temporal, and genomic information. In addition to providing open access data, the entire computational pipeline is open source, and we enable users to access high-performance computing environments.</p> <p>The study has evaluated a sorghum diversity panel, biparental cross populations, and elite lines and hybrids from structured sorghum breeding populations. <br> In addition, a durum wheat diversity panel was grown and evaluated over three winter seasons.<br> The initial release includes derived data from from two seasons in which the sorghum diversity panel was evaluated.<br> Future releases will include data from additional seasons and locations.</p> <p>The TERRA-REF reference dataset can be used to characterize phenotype-to-genotype associations, on a genomic scale, that will enable knowledge-driven breeding and the development of higher-yielding cultivars of sorghum and wheat. <br> The data is also being used to develop new algorithms for machine learning, image analysis, genomics, and optical sensor engineering.</p>

opencc-zeroAug 2020View details →
dryad36/100

Comparing Lifeact and Phalloidin for super-resolution imaging of actin in fixed cells

<p>Visualizing actin filaments in fixed cells is of great interest for a variety of topics in cell biology such as cell division, cell movement, and cell signaling. We investigated the possibility of replacing phalloidin, the standard reagent for super-resolution imaging of F-actin in fixed cells, with the actin binding peptide `lifeact'. We compared the labels for use in single molecule based super-resolution microscopy, where AlexaFluor 647 labeled phalloidin was used in a (d)STORM modality and Atto 655 labeled lifeact was used in a single molecule imaging, reversible binding modality. We found that imaging with lifeact had a comparable resolution in reconstructed images and provided several advantages over phalloidin including lower costs, the ability to image multiple regions of interest on a coverslip without degradation, simplified sequential super-resolution imaging, and more continuous labeling of thin filaments.</p>

opencc-zeroAug 2020View details →
zenodo36/100

Data for GRL manuscript "Vertical Coordinate and Resolution Dependence of the Second Moment Turbulent Closure Models"

<p>The zipped&nbsp;directory contains data used for analysis and figures in the GRL manuscript &quot;Vertical Coordinate and Resolution Dependence of the Second Moment Turbulent Closure Models&quot;</p> <p>### OSP observations:</p> <p>Air Temperature: airt50n145w_hr.ascii&nbsp; &nbsp;</p> <p>Ocean Temperature: t50n145w_hr.ascii&nbsp;</p> <p>Ocean Salinity: s50n145w_hr.ascii</p> <p>Total Heat Flux:&nbsp; heatflux_papa.dat</p> <p>10m Wind Speed: wspd_papa.dat</p> <p>u and v components of Stokes drift velocity hourly time series given on vertical grid vertical_grid_128: uvstk_papa.dat</p> <p>### NCOM simulation results</p> <p>out_Model_LayerGrid.dat</p> <p>Model:</p> <p>&nbsp; h15 - use harcourt (2015) &nbsp;</p> <p>&nbsp; kc04 - use Kantha &amp; Clayson (2004)</p> <p>&nbsp; myl2p5 - use Mellor &amp; Yamda (1982) level 2.5</p> <p>Layer:</p> <p>&nbsp; 030, 040, 050, 080, 100</p> <p>Grid:</p> <p>&nbsp; s - uniform stretched grid</p> <p>&nbsp; u - uniform grid</p> <p>&nbsp; y - mixed layer enhanced grid</p> <p>The following variables are provied in all out_*.dat files as given in their headers</p> <p>&nbsp;depth (m) tke (cm2/s2) dis (cm2/s3) tl (cm)&nbsp; zkm (cm2/s)&nbsp; zkh (cm2/s) T (C) S (psu) pd (kg/m3) z-mid (m)</p> <p>### LES output</p> <p>Eddy viscosity computed using LES model</p> <p>&nbsp; LES simulation with all foring - Km_les_AllForcing.dat</p> <p>&nbsp; LES simulation without Stokes drift - Km_les_NoStk.dat</p> <p>&nbsp; LES simulation without Heat Flux - Km_les_NoHF.dat</p>

opencc-by-4.0Sep 2020View details →
zenodo36/100

Dataset of "Gravity Wave Activity in the Atmosphere of Mars During the 2018 Global Dust Storm: Simulations With a High-Resolution Model" (1/2)

<p>This dataset contains the GrADS data of high-resolution Mars GCM results used for figures in the paper &quot;Gravity Wave Activity in the Atmosphere of Mars During the 2018 Global Dust Storm: Simulations With a High-Resolution Model&quot; by T. Kuroda, A.S. Medvedev and E. Yiğit.</p> <p>Each file with the name starting &#39;data&#39; contains two-dimensional (X: longitude, Y: latitude) data of surface pressure (Ps) (unit: hPa) and dust opacity in infrared wavelength (tau), and three-dimensional (X: longitude, Y: latitude, Z:sigma-level) data of temperature (T) (unit: K), zonal wind velocity (u) (unit: m/s), meridional wind velocity (v) (unit: m/s) and vertical wind velocity (w) (unit: m/s), in snapshots of every 1/6 Sol for the periods of 30 degrees in Ls per a file as described below. The dust scenario implemented for producing this dataset is taken from Montabone et al. (2020), which is based on the observed dust opacity in Mars Year 24 (MY34).</p> <p>data180rdc-my34.tar.xz: for Ls=180-210 (49 Sols)</p> <p>data210rdc-my34.tar.xz: for Ls=210-240 (47 Sols)</p> <p>data240rdc-my34.tar.xz: for Ls=240-270 (46 Sols)</p> <p>The .tar.xz files can be extracted in Linux with &#39;tar Jxvf&#39; command, and .grd and .ctl files with the same stem are generated.</p> <p>The file &#39;flux61ls5-my34.tar.xz&#39; contains the three-dimensional fluxes and physical parameters calculated from the model output with the MY34 dust scenario. The contents are (T&#39;)^2, (u&#39;)^2, (v&#39;)^2, u&#39;v&#39;, u&#39;w&#39;, v&#39;w&#39; T(bar), u(bar), v(bar), squared Brunt-Vaisala frequency, and geopotential height. (bar) denotes the sum of the total wavenumber s=0-60 components, and the dash denotes the deviation from (bar), i.e. sum of the total wavenumber s=61-106 components. There are 36 time grids between Ls=182.5 and Ls=357.5 with the step of Ls=5 degrees. Kinetic and potential energies can be derived from these values using the formulae in the paper.</p> <p>The file &#39;flux61ls5-lowdust.tar.xz&#39; is the same as &#39;flux61ls5-my34.tar.xz&#39;, except the model output with the &#39;low-dust&#39; scenario (Kuroda et al., 2019; Kuroda, 2019a, 2019b).</p> <p>The file &#39;scripts.zip&#39; contains the FORTRAN scripts to derive the fluxes and physical parameters equivalent to the file &#39;flux61ls5-my34.tar.xz&#39; from the model outputs in this dataset and Kuroda (2020), i.e. data180rdc-my34.tar.xz, data210rdc-my34.tar.xz, data240rdc-my34.tar.xz, data270rdc-my34.tar.xz, data300rdc-my34.tar.xz and data330rdc-my34.tar.xz. Also, the fluxes and physical parameters equivalent to the file &#39;flux61ls5-lowdust.tar.xz&#39; can be derived with those scripts from the model outputs data180rdc.tar.xz, data210rdc.tar.xz, data240rdc.tar.xz, data270rdc.tar.xz, data300rdc.tar.xz and data330rdc.tar.xz which are available in Kuroda (2019a, 2019b).</p>

opencc-by-4.0Apr 2020View details →
zenodo36/100

Global High Resolution Dust Emission Inventory for Chemical Transport Models

<p><strong>Overview:</strong><br> ==================================================================================</p> <p>Offline dust emissions in 2016 are now available at 0.25&deg; x 0.3125&deg; resolution. This dataset is&nbsp;calculated&nbsp;using the native resolution <a href="http://wiki.seas.harvard.edu/geos-chem/index.php/GEOS-FP">GMAO meteorology (GEOS-FP) fields</a>.&nbsp;</p> <p>Codes and Instructions (README file in the GitHub repository)&nbsp;to generate these&nbsp;offline emissions can be found on <a href="https://github.com/Jun-Meng/geos-chem/tree/v11-01-Patches-UniCF-vegetation">GitHub</a>.</p> <p>The offline emissions in this database&nbsp;have no scale factor applied,&nbsp;so users should apply the required scale factor in their application.&nbsp;Suggested scale factor&nbsp;to make the global&nbsp;total annual dust emission to 2000 Tg is&nbsp;5.7141e-4.&nbsp;</p> <p><br> <strong>Zip File Details:</strong><br> ===============================================================================</p> <p>2016.zip&nbsp;contains daily (366 in total)&nbsp;netCDF files (stored in monthly folders)&nbsp;of global gridded&nbsp;hourly mineral dust emission&nbsp;flux&nbsp;rate.&nbsp;&nbsp;</p> <p>&nbsp;</p> <p>Individual file:&nbsp;</p> <p>/YYYY/MM/dust_emissions_025x0.3125.YYYYMMDD.nc</p> <p>&nbsp; &nbsp; &nbsp;Resolution &nbsp;: 0.25 x 0.3125 grid (721 x 1152 boxes)<br> &nbsp; &nbsp; &nbsp;Units &nbsp; &nbsp; &nbsp; : kg m-2 s-1<br> &nbsp; &nbsp; &nbsp;Timestamps &nbsp;: Hourly, 2016<br> &nbsp; &nbsp; &nbsp;Compression : Level 1 (nccopy -d1)<br> &nbsp; &nbsp; &nbsp;Chunking &nbsp; &nbsp;: nccopy -c lon/1152,lat/721,time/24</p> <p>&nbsp;</p> <p>Variables in each file:&nbsp;</p> <p>EMIS_DST1,&nbsp;EMIS_DST2,&nbsp;EMIS_DST3&nbsp;and&nbsp;EMIS_DST4 represent dust emission flux rate in&nbsp;four size bins (0.1-1.0, 1.0-1.8, 1.8-3.0, and 3.0-6.0 micro in&nbsp;radius).&nbsp;</p> <p>&nbsp;</p> <p>*<em>Version 2020_v1.0 of this&nbsp;dataset was produced to accompany the following manuscript:<br> Meng, Jun, R. V. Martin, P. Ginoux, M. Hammer, M. P. Sulprizio, D. A. Ridley, and A. van Donkelaar,&nbsp;Grid-independent high resolution dust emissions (v1.0) for chemical transport models: application to GEOS-Chem (version 12.5.0),&nbsp;Geoscientific Model Development, Submitted</em></p>

opencc-by-4.0Sep 2020View details →
zenodo36/100

Results of "Sensitivity of Greenland ice sheet projections to spatial resolution in higher-order simulations: the AWI contribution to ISMIP6-Greenland using ISSM"

<p>This archive provides ice sheet model output produced as part of the publication:</p> <p>R&uuml;ckamp, M., Goelzer, H., and Humbert, A.: Sensitivity of Greenland ice sheet projections to spatial resolution in higher-order simulations: the AWI contribution to ISMIP6-Greenland using ISSM, The Cryosphere Discuss., https://doi.org/10.5194/tc-2019-329, in review, 2020.</p> <p>About the data:<br> The archive contains 4 tar-files for the 4 different resolutions. Each tar-file contains Matlab files for the dfferent scenarios. An examplary file structure looks as follows:</p> <p>results =</p> <p>&nbsp; struct with fields</p> <p>mesh_description: {&#39;x=x_EPSG3413(m)&#39;&nbsp; &#39;y=y_EPSG3413(m)&#39;}<br> inputs_description: {&#39;friction coefficient k^2 (s/m)&#39;&nbsp; &#39;bedrock (m)&#39;}<br> data_description: {1x13 cell}<br> mesh: [1x1 struct]<br> inputs: [1x1 struct]<br> data: [1x87 struct]<br> model_description: {&#39;output from ISMIP6 AWI-ISSM, simulation: G4000 ctrl_proj, correspondence Martin Rueckamp (AWI): marin.rueckamp@awi.de&#39;}<br> data_citation: {&#39;R&uuml;ckamp, M., Goelzer, H., and Humbert, A.: Results of &quot;Sensitivity of Greenland ice sheet projections to spatial resolution in higher-order simulations: the AWI contribution to ISMIP6-Greenland using ISSM&quot;, Zenodo, https://doi.org/10.5281/zenodo.3992605, 2020.&#39;}<br> model_citation: {&#39;R&uuml;ckamp, M., Goelzer, H., and Humbert, A.: Sensitivity of Greenland ice sheet projections to spatial resolution in higher-order simulations: the AWI contribution to ISMIP6-Greenland using ISSM, The Cryosphere Discuss., https://doi.org/10.5194/tc-2019-329, in review, 2020.&#39;}</p> <p>The fields results.[mesh,input,data]_description contain header information. The field results.mesh contains [x,y]-coordinates of the grid. The field results.inputs contains time-independent quantities such as bedrock. The field results.data contains results of the transient simulations, such as ice thickness or surface velocity. The fields results.[model,data]_citation contain information about data citation.</p>

opencc-by-4.0Sep 2020View details →
zenodo36/100

iSDAsoil: soil total Carbon for Africa predicted at 30 m resolution at 0-20 and 20-50 cm depths

<p>iSDAsoil dataset soil&nbsp;total carbon in permilles (g/kg) log-transformed predicted at 30 m resolution for 0&ndash;20 and 20&ndash;50 cm depth intervals. Data has been projected in WGS84 coordinate system and compiled as <a href="https://gdal.org/drivers/raster/cog.html">COG</a>.&nbsp;Predictions have been generated using multi-scale Ensemble Machine Learning with 250 m (MODIS, PROBA-V, climatic variables and similar) and 30 m (DTM derivatives, Landsat, Sentinel-2 and similar) resolution covariates. For model training we use a pan-African compilations of soil samples and profiles (<a href="https://www.isda-africa.com/national-soil-services/">iSDA points</a>, <a href="https://www.isric.org/projects/africa-soil-profiles-database-afsp">AfSPDB</a>, and other national and regional soil datasets). Cite as:</p> <p>Hengl, T., Miller, M.A.E., Križan, J.&nbsp;<em>et al.</em>&nbsp;African soil properties and nutrients mapped at 30&nbsp;m spatial resolution using two-scale ensemble machine learning.&nbsp;<em>Sci Rep</em>&nbsp;<strong>11,&nbsp;</strong>6130 (2021). <a href="https://doi.org/10.1038/s41598-021-85639-y">https://doi.org/10.1038/s41598-021-85639-y</a></p> <p>To open the maps in QGIS and/or directly compute with them, please use the <a href="https://gitlab.com/openlandmap/africa-soil-and-agronomy-data-cube"><strong>Cloud-Optimized GeoTIFF version</strong></a>.</p> <p>Layer description:</p> <ul> <li>sol_log.c_tot_mehlich3_m_30m_*..*cm_2001..2017_v0.13_wgs84.tif = predicted soil total Carbon mean value,</li> <li>sol_log.c_tot_mehlich3_md_30m_*..*cm_2001..2017_v0.13_wgs84.tif = predicted soil total Carbon model (prediction) errors,</li> </ul> <p>Model errors were derived using bootstrapping: md is derived as standard deviation of individual learners from 5-fold cross-validation (using spatial blocking). The model 5-fold cross-validation (<a href="https://mlr.mlr-org.com/reference/makeStackedLearner.html">mlr::makeStackedLearner</a>) for this variable indicates:</p> <pre><code>Variable: log.c_tot R-square: 0.794 Fitted values sd: 0.571 RMSE: 0.291 Random forest model: Call: stats::lm(formula = f, data = d) Residuals: Min 1Q Median 3Q Max -2.70312 -0.16714 -0.00549 0.15691 3.01116 Coefficients: Estimate Std. Error t value Pr(&gt;|t|) (Intercept) 0.025841 0.032713 0.790 0.429570 regr.ranger 0.902240 0.008462 106.619 &lt; 2e-16 *** regr.xgboost 0.066535 0.008145 8.169 3.18e-16 *** regr.cubist 0.145730 0.006927 21.039 &lt; 2e-16 *** regr.nnet -0.048957 0.013466 -3.636 0.000278 *** regr.cvglmnet -0.075212 0.005556 -13.537 &lt; 2e-16 *** --- Signif. codes: 0 '***' 0.001 '**' 0.01 '*' 0.05 '.' 0.1 ' ' 1 Residual standard error: 0.291 on 50140 degrees of freedom Multiple R-squared: 0.7938, Adjusted R-squared: 0.7938 F-statistic: 3.861e+04 on 5 and 50140 DF, p-value: &lt; 2.2e-16 </code></pre> <p>To back-transform values (y) to g/kg use the following formula:</p> <pre><code>g/kg = expm1( y / 10 )</code></pre> <p>To submit an issue or request support please visit <a href="https://isda-africa.com/isdasoil"><strong>https://isda-africa.com/isdasoil</strong></a></p>

opencc-by-4.0Oct 2020View details →

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International Brain Laboratory public data

The International Brain Laboratory public data releases expose standardized mouse decision-making experiments, including Neuropixels recordings, widefield calcium imaging, behavior, and session metadata accessed through the ONE API.

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OpenNeuro

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