cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.5281/zenodo.8264513
title: Configuration files for WRF and rain-producing storm identification model

description: This repository hosts necessary configuration files to reproduce the manuscript "Studying Brown Ocean Re-intensification of Hurricane Florence Using CYGNSS and SMAP Soil Moisture Data and a Numerical Weather Model". Model description: WRF v4.4: https://github.com/wrf-model/WRF/tree/release-v4.4 MET v10.0: https://github.com/dtcenter/MET/tree/main_v10.0 modify_SM.ncl: NCL tool to multiply initial soil moisture and soil temperature by a factor MTDConfig: configuration file for MET MTD analysis namelist.input: input configuration for WRF model namelist.wps: configuration file for WPS preprocessing model
DOI: 10.5281/zenodo.8284810
title: L2LFlows: Generating High-Fidelity 3D Calorimeter Images

description: This upload contains the datasets used in arXiv:2302.11594. The file <em>g4-showers_950k_10x10_train_val_test.pt</em> contains the <strong>760k training</strong>, <strong>95k validation</strong> and <strong>95k test</strong> showers as well as their incident energies. It should be loaded as follows: - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - <em>import torch </em> <em>list_tensors = torch.load(args.file_path)</em> <em>for (idx, tensor) in enumerate(list_tensors):</em> <em> [showers_train, showers_val, showers_test, inc_energies_train, inc_energies_val, inc_energies_test] = list_tensors</em> - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - The file <em>g4-showers_665k_10x10_test.pt</em> contains 665k additional showers that were used for the classifier scaling studies, in addition to the 95k test showers from the file <em>g4-showers_950k_10x10_train_val_test.pt</em>. It should be loaded as follows: - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - <em>import torch</em> <em>list_tensors = torch.load("g4-showers_950k_10x10_train_val_test.pt") </em> <em>[showers_geant, inc_energies_geant] = list_tensors</em> - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - A detailed description of how the datasets were simulated can be found in the paper.
DOI: 10.6073/pasta/5c34f47415f55eb4e030f22c91299ad9
title: Denitrification losses in response to N fertiliser rates - integrating high temporal resolution N2O, in-situ 15N2O and 15N2 measurements and fertiliser 15N recoveries in intensive sugarcane systems

description: Denitrification is a key process in the global nitrogen (N) cycle, causing both nitrous oxide (N2O) and dinitrogen (N2) emissions. However, estimates of seasonal denitrification losses (N2O+N2) are scarce, reflecting methodological difficulties in measuring soil-borne N2 emissions against the high atmospheric N2 background and challenges regarding their spatio-temporal upscaling. This study investigated N2O+N2 losses in response to N fertiliser rates (0, 100, 150, 200 and 250 kg N ha-1) on two intensively managed tropical sugarcane farms in Australia, by combining automated N2O monitoring, in-situ N2 and N2O measurements using the 15N gas flux method and fertiliser 15N recoveries at harvest. Dynamic changes in the N2O/(N2O+N2) ratio (&lt; 0.01 to 0.768) were explained by fitting generalised additive mixed models (GAMMs) with soil factors to upscale high temporal-resolution N2O data to daily N2 emissions over the season. Cumulative N2O+N2 losses ranged from 12 to 87 kg N ha-1, increasing non-linearly with increasing N fertiliser rates. Emissions of N2O+N2 accounted for 31–78% of fertiliser 15N losses and were dominated by environmentally benign N2 emissions. The contribution of denitrification to N fertiliser loss decreased with increasing N rates, suggesting increasing significance of other N loss pathways including leaching and runoff at higher N rates. This study delivers a blueprint approach to extrapolate denitrification measurements at both temporal and spatial scales, which can be applied in fertilised agroecosystems. Robust estimates of denitrification losses determined using this method will help to improve cropping system modelling approaches, advancing our understanding of the N cycle across scales.
DOI: 10.6084/m9.figshare.22809653.v1
title: <strong>Impact of Mars GDS 2018 on the chemistry of water, nitrogenated and deuterated cluster ions: NOMAD observations</strong>

description: This file containing the readme file and all figures data
DOI: 10.18157/qogbasjan20
title: QoG Basic Dataset 2020
DOI: 10.5067/vp1m6og1x7m1
title: Aqua/AIRS L2 Standard Physical Retrieval (AIRS-only) V7.0
DOI: 10.5281/zenodo.8015379
title: Supplemental Data Set for "Constraining Changes in Surface Dust Thickness on Mars Using Diurnal Surface Temperature Observations from EMIRS"

description: Supporting data set for manuscript "Constraining Changes in Surface Dust Thickness on Mars Using Diurnal Surface Temperature Observations from EMIRS". Provides the binned and averaged EMIRS surface temperatures acquired before and after the January 2022 dust storm for each region of interest to derive changes in surface dust thickness.
DOI: 10.17632/2pbhnrfkpr.1
title: afes-venus-4d-5d-waves

description: The data presented in the manuscript of "A GCM study on the 4-day and 5-day waves in the Venus atmosphere" submitted to Journal of Geophysical Research - Planets.
DOI: 10.17632/hn2cy35wxh.1
title: SEM images: cut resistance of climbing ropes

description: The dataset consists of over 1500 raw images from scanning electron microscopy of broken nylon 6 fibers. Fibers were taken from climbing ropes after undergoing laboratory cut resistance tests and an accident simulation. 
The images are divided into folders by: 
1) test type: Accident simulation, Edelrid test, Elmenzwick test, and UIAA 101 Sharp Edge test
2) the type of rope and the location in its cross-section from which the images were taken. 

The fiber fractography revealed four main failure modes. These failure modes included lateral pressure with high-stress concentration, lateral pressure with low-stress concentration, high-speed tensile break, and molten and fused fiber ends. In isolated cases, ductile breaks were found. None of the laboratory test methods could comprehensively mimic the overall breaking mechanism of the accident simulation.
DOI: 10.5281/zenodo.10068104
title: The code and data used for Mango-GPP

description: The source code, inputs, and outputs of Mango-GPP and observed GPP at NS and ZJ sites.
DOI: 10.5281/zenodo.8014410
title: EPMA data of Dong Ujimqin Qi mesosiderite

description: This is our measured EMPA data including olivine, pyroxene, plagioclase, phosphate, chromite, troilite and FE-Ni metal.
DOI: 10.5281/zenodo.8310560
title: Interplay of Three-Dimensional Instabilities and Magnetic Reconnection in the Explosive Onset of Magnetospheric Substorms

description: Datasets for "Interplay of Three-Dimensional Instabilities and Magnetic Reconnection in the Explosive Onset of Magnetospheric Substorms".
DOI: 10.17632/bdgy972gkm.1
title: afes-venus-7d-wave

description: The data presented in the manuscript of "Quasi-periodic variation of equatorial jet produced by planetary-scale waves in the Venusian lower cloud layer" submitted to Journal of Geophysical Research - Planets.
DOI: 10.17632/fs2npvfx54.1
title: Summary of data for size-resolved organic nitrates

description: The data in this file is for the manuscript entitled "Size-dependent formation of secondary organic nitrates in urban air" in JGR-A journal.
DOI: 10.17632/x4b54znvwt.1
title: Organic carbon, water-soluble organic carbon, dicarboxylic acids, oxocarboxylic acids, dicarbonyls, benzoic acid and citric acid concentrations in PM1.1 aerosols at a tropical hill station in the Western Ghats

description: Organic carbon, water-soluble organic carbon, dicarboxylic acids, oxocarboxylic acids, dicarbonyls, benzoic acid and citric acid concentrations in PM1.1 aerosols at a tropical hill station in the Western Ghats
DOI: 10.18140/flx/1669642
title: FLUXNET-CH4 HK-MPM Mai Po Mangrove

description: This is the FLUXNET-CH4 version of the carbon flux data for the site HK-MPM Mai Po Mangrove.
DOI: 10.18739/a2f76683d
title: Organic-Matter Accumulation and Degradation in Holocene Permafrost Deposits Along a Central Alaska Hillslope, 2020-2022

description: The quantity and preservation of carbon-rich organic matter (OM) underlying permafrost uplands, and the evolution of carbon accumulation with millennial climate change, are large sources of uncertainty in carbon cycle feedbacks on climate change. We investigated permafrost OM accumulation and degradation over the Holocene using a transect of sediment cores dating back to at least c. 6-8 ka, from a hillslope in the Eight Mile Lake watershed, central Alaska. This dataset collected from four permafrost sediment cores includes a variety of biogeochemical datasets including radiocarbon, carbon, nitrogen, particle size, amino acids (concentrations and D:L), bulk density and water content.
DOI: 10.18739/a2g15tc4j
title: Collaborative Research: Climate controls on carbon accumulation in upland permafrost at millennial scales

description: Organic-rich surficial materials of the Arctic are a storehouse of frozen carbon (C) of global consequence. Climate ultimately controls the exchange of carbon between this reservoir and the atmosphere, but the long-term relation between climate and permafrost carbon is highly uncertain. This study draws from climate changes that occurred during the recent geologic past (late glacial and Holocene), which serve as natural experiments, to quantify the long-term (millennial-scale) relation between climate and the mass of carbon that accumulated under distinctly different climate states. Whereas previous studies of the effects of climate changes on permafrost carbon have generally focused on lakes and peatlands of low-lying terrain, this study provides complementary information from upland deposits that mantle hilly terrain, possibly the least-well known component of the arctic frozen organic carbon inventory. The project applies and develops new approaches to investigating the relation between climate and carbon sequestration in an understudied setting and at long time scales by bringing together expertise in Arctic paleoecology, paleoclimatology, surficial geology, geochronology and quantitative geomorphology. This paleo perspective provides a unique approach to help infer how permafrost and its C reservoir may react in the future.
DOI: 10.25422/azu.data.22964729.v1
title: Supporting Information for "Evidence for Extrusive Mg-Suite Magmatism on the Moon? Fine-Grained Magnesian Clasts in an Apollo 16 Impact Melt Breccia"

description: Electron probe microanalyses (EPMA) data for Apollo 16 sample 68815, calculated bulk compositions for samples in study, literature data, and model outputs for thermodynamic modeling of composition similar to calculated bulk compositions. Photoshop files contain locations of all EPMA data points. The PNG files are previews that represent a sample of the available layers in the Photoshop files. This dataset supplements Stadermann et al. in the Journal of Geophysical Research: Planets.<br><br> <em>For inquiries regarding the contents of this dataset, please contact the Corresponding Author listed in the README.txt file. Administrative inquiries (e.g., removal requests, trouble downloading, etc.) can be directed to data-management@arizona.edu</em><br> <br>
DOI: 10.35003/nerhu3
title: Mid-infrared spectroscopy of sulfidation reaction products and implications for sulfur on Mercury

description: This dataset includes electron microprobe measurements and mid-IR spectra of silicate glasses and minerals sulfidized at 800-1200 °C under reducing conditions. Table S1 includes all EPMA measurements of the silicate and sulfide phases in the polished cross-sections of the experiments. Measurements were made at 15 kV and 15 nA. The beam-size varied from 2-10 µm, depending on the grain sizes. Na, Mg, Al, Si were measured on TAP crystals, Mn, Fe, Ti on a LIF crystal, and K, Ca, S on a PETL crystal. We measured 10s on peaks, and 5s on background for all elements. Table S2 is a compilation of all mid-IR spectra recorded on bulk and in-situ experimental materials, as they are shown in the figures of the manuscript. The spectra were collected over a spectral range of 7.7 to 12.5 µm wavelengths.The spectra are normalized to the respective highest reflectances over this spectral range. The full spectral data is also available on the Infrared and Raman for Interplanetary Spectroscopy (IRIS) database at http://bc-mertis-pi.uni-muenster.de/ and searchable by the ID number and the mineral/glass name.
DOI: 10.48443/8w20-r938
title: NCAR-NEON gap-filled data

description: The atm data are gap-filled NEON observations of meteorological conditions from each tower site that are used as input drivers to the CLM simulations. The eval files are neon flux observations of water, energy and CO2 that are measured at each NEON flux tower that have additional quality assurance and quality control (QAQC) applied, including range and spike tests on post-processed data, gap-filling, and partitioning to calculate GPP.   

Repositories: 
* https://github.com/ESCOMP/CTSM 
* https://github.com/NEONScience/NCAR-NEON 
* https://github.com/NCAR/NEON-visualization 

NSF Award Number 2039932 Project Title: Data CI Pilot: NCAR and NEON Cyberinfrastructure Collaborations to Enable Convergence Research Linking the Atmospheric and Biological Sciences https://www.nsf.gov/awardsearch/showAward?AWD_ID=2039932.
description: These gap-filled NEON observations are used to run and evaluate the NCAR CTSM model at NEON tower sites.
DOI: 10.48443/pnt4-pk88
title: Reaeration field and lab collection (DP1.20190.001)
title: RELEASE-2021

description: This data product contains the quality-controlled, native sampling resolution data from NEON's wadeable stream reaeration sampling protocol. During most reaeration experiments, grab samples of stream water at NEON aquatic sites are collected in streams at 4 sampling locations downstream of a continuous injection of an inert gas (SF6) and conservative tracer (NaCl or NaBr). Background samples are collected prior to tracer injection and are analyzed for background salt tracer concentrations. Plateau samples are collected once the tracer concentration reaches a constant concentration (as measured by conductivity) and 5 replicate samples from each station are analyzed for both salt and gas tracer concentrations. Data users should refer to the user guide for reaeration and salt-based discharge see `NEON_ReaerSaltBasedQ_userGuide` for suggestions on how to calculate reaeration rates from the published data packages. For additional details, see the user guide, protocols, and science design listed in the Documentation section in this data product's details webpage. During some reaeration experiments, denoted by injectionType “model - slug” or “model - CRI”, only the conservative tracer is injected, either via slug or constant rate, (i.e., inert gas is not injected). See NEON Data Product User Guide to Reaeration (DP1.20190.001) and Salt-based Discharge Sampling (DP1.20193.001) for more detail about when and where model type injections are used.

Latency:
The expected time from data and/or sample collection in the field to data publication is as follows, for each of the data tables (in days) in the downloaded data package. See the Data Product User Guide for more information.

rea_backgroundFieldCondData:  30

rea_backgroundFieldSaltData:  30

rea_conductivityFieldData:  30

rea_externalLabDataGas:  120

rea_externalLabDataSalt:  120

rea_fieldData:  30

rea_plateauMeasurementFieldData:  30

rea_plateauSampleFieldData:  30

rea_widthFieldData:  30

sdg_externalLabSummaryData:  14
description: Tracer injections are completed 6 times per year to capture a range of flows at NEON wadeable stream sites. The first sampling station is located near sensor set #1 and the fourth sampling station is located near sensor set #2. Sampling stations #2 and #3 are approximately evenly spaced between sampling stations #1 and #4. The injection (drip) station is located far enough upstream of sampling station #1 that the tracer is well mixed within the stream channel for all sampling stations. Conductivity data loggers are located near sampling stations #1 and #4 to capture the rising limb and plateau (for constant rate injections) and falling limb (for slug injections) in situ conductivity values. Instrumentation: YSI Pro2030, HOBO U24
DOI: 10.48443/xz4k-5j04
title: Continuous discharge (DP4.00130.001)
title: RELEASE-2022

description: This data product describes the volume of water flowing through a stream or river cross-section during a given period of time. For each NEON stream or river site, site-specific stage-discharge rating curve equations are derived from point observations of gauge height and discharge. Continuous sensor measurements of surface water pressure are used to derive water column height. The rating curve equations are applied to water column height to derive continuous stream discharge.

Latency:
Data collected in any given month are published during the second full week of the following month.
description: NEON calculates continuous stream discharge in all rivers and wadeable stream sites within the Observatory. Stream discharge data are calculated using pressure of surface water L0 data (DP0.20016; the raw, level 0 inputs used to calculate Elevation of surface water, DP1.20016), stream discharge rating curve data (DP4.00133), gauge height data (DP1.20267.001) and geolocation information. Continuous discharge data are reported once per minute. Instrumentation: Level TROLL 500
DOI: 10.5066/p9fj3g0l
title: Spectral cubes, maps, and data from Moon Mineralogy Mapper for the Montes Apenninus region of the Moon

description: Data for Journal article:�Relationship between explosive and effusive volcanism in the Montes Apenninus region of the Moon�in JGR: Planets
DOI: 10.5281/zenodo.10054316
title: UV Reflectance of Spacecraft Materials and Analog Soils: Implications for Bioburden Reductions on the Undersides of Mars Rovers

description: Abstract
The Mars Sample Return mission architecture will utilize three spacecraft to collect, cache, recover, launch, and return to Earth a diversity of regolith and rock samples. However, no comprehensive Mars Microbial Survival (MMS) model currently exists.  As an initial effort in building a MMS model, we examined the UV reflectance of 15 spacecraft materials and seven Mars analog soils within the context of the Perseverance mission. Data were used to predict the times required to achieve one lethal dose (syn., Sterility Assurance Level [SAL]; def. as a bioburden reduction of ‒12 logs).  Results suggest that a single SAL dosage of UVC was achieved on exposed surfaces on the upper deck of Perseverance within a few hours to a few sols post-landing at Jezero Crater. The overall average for UVC reflectance from spacecraft materials was approx. 10%.  The overall UVC reflectance from Mars analog soils was measured at 1.3%.  The Adaptive Caching Assembly (ACA) on Perseverance is located on the forward edge of the underbelly of the spacecraft.  Modeling of the accumulated UVC dosage for the ACA yielded a prediction of reaching one SAL for downward facing surfaces at 93 sols that receive 'single bounce' UVC photons from the local terrain.  The SAL increases to 930 sols, if an additional 'bounce' of the solar UV irradiation is required to reach a partially protected site in the ACA hardware.  The current study is the first to report on the UVC reflectance from a diversity of spacecraft materials. 
description: The manuscript is in review (as of 30-Oct-2023) at Journal of Geophysical Research, Planets.
DOI: 10.5281/zenodo.7892332
title: Dataset for "State-dependence of the equilibrium climate sensitivity in a clear-sky GCM" by Matthew Henry et al. (2023).

description: Dataset for "State-dependence of the equilibrium climate sensitivity in a clear-sky GCM" by Matthew Henry, Geoffrey K. Vallis, Nicholas J. Lutsko, Jacob T. Seeley, and Brett A. McKim.
DOI: 10.5281/zenodo.7912742
title: Brightness Temperature Spectra 400-1200 cm**-1 from satellite METEOR-29 instrument SI-1 in February 1979 along with radiative transfer simulations from 4 different reanalyses, clear scenes only over ocean

description: This dataset is published in support of a tentative journal publication in a peer-reviewed journal. The full data record is scheduled for release under DOI:10.15770/EUM_SEC_CLM_0086
DOI: 10.5281/zenodo.8056396
title: Dataset for Evidence of Topographic Change Recorded by Lava Flows at Atete and Aruru Coronae on Venus

description: GIS shapefiles, python script, and .csv files for Evidence of Topographic Change Recorded by Lava Flows at Atete and Aruru Coronae on Venus. Submitted to JGR: Planets
DOI: 10.5281/zenodo.8363118
title: Bulk chemical composition of rock samples used to calculate their seismic velocity at lower crustal conditions

description: These data are linked to a published study, whose aim is to compare the seismic velocity variations, derived from tomographic models (here the CIFALPS profile in the Alps, derived from Nouibat et al., 2022) and interpreted as rock transformations, with the seismic velocities of field samples. One way to predict seismic velocity at lower crustal conditions is to consider natural rocks as isotropic and to calculate their seismic properties from the relative abundance of mineral phases using their acknowledged properties (Abers and Hacker, 2016). In this process, the bulk chemical composition of the samples constitutes the starting data for this study. The subsequent work is based solely on thermodynamic models (here mainly using Holland and Powel, 1998 database) and the physical properties of the mineral phases (database from Abers and Hacker, 2016).
DOI: 10.5281/zenodo.8415384
title: juan9715/WaveVelocitiesSoftwareAndSpreadsheet: Wave Velocities Data Release

description: Contains data for articles: Article 1: Wave Velocities and Poisson Ratio in Loose Sandy Martian Regolith Under Low Stresses. Part 1: Laboratory Investigation Article 2: Wave Velocities and Poisson Ratio in Loose Sandy Martian Regolith Under Low Stresses. Part 2: Theoretical Analysis
DOI: 10.6073/pasta/556872ebc0fdb9dde5b0fddf4e778378
title: Seasonality Drives Carbon Emissions along a Stream Network

description: Headwater stream networks contribute a significant amount to the global carbon dioxide terrestrial flux because of high turbulence and coupling with terrestrial environments. Heterogeneity within headwater stream networks, both spatially and temporally, makes measuring and upscaling these emissions challenging because measurements of carbon dioxide in streams are often limited to a few monitoring points. We modified a stream network model to reflect real measurements made under base flow and high flow conditions at Martha Creek in Stabler, WA in the US Pacific Northwest. We found that under high flow conditions, the stream network had much greater total carbon emissions than during low flow conditions (1.22 Mg C day-1 vs. 0.034 Mg C day-1). We attribute this increase to a larger overall stream network area (0.04 km2 vs 0.01 km2) and discharge (1.9 m3/s vs. 0.005 m3/s) in November versus August. Our results demonstrate the need to understand the nonperennial nature of streams when calculating carbon emissions. We compared the stream network emissions with the terrestrial net ecosystem exchange (NEE) estimated by local eddy covariance measurements per area of the watershed (-5.5 Mg C day-1 in August and -2.2 Mg C day-1 in November). Daily stream emissions in November accounted for a much larger percentage of NEE in August (54% vs. 0.62%). We concluded that the stream network can emit a large percentage of the forest NEE in the winter months, and annual estimates of stream network emissions must consider the flow regime throughout the year.