cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.6084/m9.figshare.24624069.v1
title: Supplementary Material for: Shikonin exerts an anti-leukemia effect against FLT3-ITD mutated acute myeloid leukemia cells via targeting FLT3 tyrosine kinase and its downstream pathways

description: Introduction: Acute myeloid leukemia (AML) with internal tandem duplication (ITD) mutations in Fms-like tyrosine kinase 3 (FLT3) has an unfavorable prognosis. Recently, using newly emerging inhibitors of FLT3 has led to improved outcomes of patients with FLT3-ITD mutations. However, drug resistance and relapse continue to be significant challenges in the treatment of patients with FLT3-ITD mutations. This study aimed to evaluate the anti-leukemic effects of shikonin (SHK) and its mechanisms of action against AML cells with FLT3-ITD mutations in vitro and in vivo. Methods: The CCK-8 assay was used to analyze cell viability, and flow cytometry was used to detect cell apoptosis and differentiation. Western blotting and real-time polymerase chain reaction (RT-PCR) were used to examine the expression of certain proteins and genes. Leukemia mouse model was created to evaluate the anti-leukemia effect of SHK against FLT3-ITD mutated leukemia in vivo. Results: After screening a series of leukemia cell lines, those with FLT3-ITD mutations were found to be more sensitive to SHK in terms of proliferation inhibition and apoptosis induction than those without FLT3-ITD mutations. SHK suppresses the expression and phosphorylation of FLT3 receptors and their downstream molecules. Inhibition of the NF-κB/miR-155 pathway is an important mechanism through which SHK kills FLT3-AML cells. Moreover, a low concentration of SHK promotes the differentiation of AML cells with FLT3-ITD mutations. Finally, SHK could significantly inhibit the growth of MV4-11 cells in leukemia bearing mice. Conclusion: The findings of this study indicate that SHK is a promising drug for the treatment of FLT3-ITD mutated AML.
DOI: 10.6084/m9.figshare.21944564.v1
title: Solar Tsunamis Southland MT data

description: Long period magnetotelluric data in the form of edi files measured in Southland/Otago in NZ South Island as part of the Solar Tsunamis project. Measured 2021-22. New Zealand Ministry of Business, Innovation and Employment Endeavour Fund Research Grant UOOX2002.
DOI: 10.3334/cdiac/ornlsfa.005
title: Fine-Root Ecology Database (FRED): A Global Collection of Root Trait Data with Coincident Site, Vegetation, Edaphic, and Climatic Data, Version 1

description: To address the need for a centralized root trait database, we are compiling the Fine-Root Ecology Database (FRED) from published literature and unpublished data. FRED Version 1 (FRED 1.0) currently houses more than 70,000 observations of root traits and their associated site, vegetation, edaphic, and climatic conditions from across the globe (see image below, which shows the more than 1000 distinct locations associated with observations in FRED 1.0). Data collection is ongoing and will continue for the foreseeable future. The more than 300 root traits currently housed in FRED 1.0 are described in detail here. FRED is focused on fine roots (less than 2 mm), as coarse roots are studied using different methodology, often at very different scales, and have different traits and trait interpretations.
DOI: 10.48443/xmbe-7b55
title: Root biomass and chemistry, Megapit (DP1.10066.001)
title: RELEASE-2022

description: This data product contains the quality-controlled, native sampling resolution data from NEON's belowground plant biomass stock and chemistry measurements from Megapits. Soil samples were collected at 10 cm depth increments to the first 100 cm below the surface, then 20 cm depth increments thereafter, along three vertical profiles from a single temporary soil pit at a location expected to be representative of NEON sensor-based soil plots. This sampling activity is expected to occur once at each NEON terrestrial site. Root material is sorted, dried, weighed, and analyzed, then any excess root sample material is archived in the NEON Biorepository and are available on request. For additional details, see the user guide, protocols, and science design listed in the Documentation section below. Products resulting from this sampling include root biomass by size class and live/dead status, as well as root chemistry and stable isotope ratios. A summary table of external lab precision and accuracy is included in the expanded package.

Latency:
Data were collected once, at the establishment of each site. Data were published within one year of collection, and future collections at existing sites are not expected.
description: Each site is sampled a single time. At each site, a soil Megapit is dug in the dominant soil type to a maximum depth of 2 m. On the exposed face of the soil pit, a tape measure visually divides the soil profile into 10 cm depth increments. Each soil pit has three vertically-oriented sampling profiles, roughly corresponding to the left, center, and right of the pit sampling face. These profiles are referred to as profile number 1, 2 and 3, respectively. From each profile, a block of soil is removed from each 10 cm depth increment, starting from the surface down to 100 cm. Once a depth of 100 cm is reached, the each profile is divided into 20 cm depth increments. By the end of sampling, up to 45 soil samples are collected, 15 per profile. Roots are sieved and then divided into four categories distinguishing between status (alive or dead) and size (> 2mm and < 2 mm, unless otherwise noted). Once roots are weighed and dried, they are sent to an external laboratory for analysis of carbon and nitrogen concentrations and stable isotopes. Any remaining root material is held in the NEON Biorepository and available upon request.
DOI: 10.5281/zenodo.10002827
title: Forecasting Ionospheric foF2 using Bidirectional LSTM and attention mechanism
DOI: 10.6073/pasta/2035bdf3056d2efc676b702e81ffe008
title: Desert Fertilization Experiment: investigation of Sonoran desert ecosystem response to atmospheric deposition and experimental nutrient addition, ongoing since 2006

description: Launched in 2006 with support from the National Science Foundation (NSF) and leveraged by the CAP LTER, the Carbon and Nitrogen deposition (CNdep) project sought to answer the fundamental question of whether elemental cycles in urban ecosystems are qualitatively different from those in non-urban ecosystems. Ecosystem scientists, atmospheric chemists, and biogeochemists tested the hypothesis that distinct biogeochemical pathways result from elevated inorganic nitrogen and organic carbon deposition from the atmosphere to the land. To test the hypothesis, scientists examined the responsiveness of Sonoran desert ecosystems to nutrient enrichment by capitalizing on a gradient of atmospheric deposition in and around the greater Phoenix metropolitan area. Fifteen desert study sites were established, with five locations each west and east of the urban core, and in the urban core in desert preserves. In addition to the gradient of atmospheric deposition in and around the urban core, select study plots at each of the fifteen desert locations receive amendments of nitrogen, phosphorus, or nitrogen + phosphorus fertilizer. Measured variables include soil properties, perennial and annual plant growth, and atmospheric deposition of nitrogen. At the close of the initial grant period, the CAP LTER assumed responsibility for the project, renamed the Desert Fertilization Experiment, which provides a remarkable platform to study the long-term effects of nutrient enrichment on desert ecosystem properties.
DOI: 10.18715/ipgp.2021.kpmqrnz8
title: Interior Models of Mars from inversion of seismic body waves

description: This dataset contains 300 seismic models of Mars compatible with seismic travel times of marsquakes observed until January 2021. The inversion is described in detail in Stähler et al. (2021): Seismic detection of the Martian Core, Science. See the description therein. The provided zip file contains 100 models each of the "geophysical", "geodynamical" and "seismic" inversion. All model files are provided in the nd format of TauP. For compatibility reasons, each model has a small inner core. This is not a feature resolved by the inversion.
DOI: 10.17592/001.2021110901
title: Ice thickness around Dome Fuji, Antarctica, based on JARE ground-based radar surveys: a 500m resolution gridded data

description: This dataset contains the 500 m resolution ice thickness map around the Dome Fuji, East Antarctica, based on the ground-based radar surveys conducted by the Japanese Antarctic Research Expedition (JARE) from 1992 to 2018. The data projections are longitude/latitude and polar stereographic centered on 0E, 90S with a true scale at 71S.
DOI: 10.17592/001.2021110902
title: Ice thickness around Dome Fuji, Antarctica, based on JARE ground-based radar surveys: JARE33 data

description: This dataset contains the ice thickness data recorded in the Dome Fuji region, East Antarctica. The data was recorded by the 33rd Japanese Antarctic Research Expedition (JARE33) using a pulse-modulated VHF radar sounder with a peak transmission power of 1kW, a center frequency of 179 MHz and a transmitter pulse width of 1000 ns.
DOI: 10.48443/10dn-8031
title: Soil physical and chemical properties, Megapit (DP1.00096.001)
title: RELEASE-2022

description: Soil properties affect the movement of water, heat and gases into and out of the soil. They also influence the availability of nutrients to plants and soil organisms and the production and stabilization of soil organic matter. Soil physical and chemical properties are measured by horizon from a single temporary soil "Megapit" at each terrestrial site at depths of up to 200 cm at non-permafrost sites (up to 300 cm at Alaskan sites). The Megapit sampling location is expected to be representative of the NEON sensor-based soil plots and this sampling activity is expected to occur once at each NEON terrestrial site.

Queries for this data product will return field collection metadata, soil taxonomy, bulk density, coarse fragment content, and particle size distribution, and a host of geochemical measurements on a per horizon basis. For additional details, see the user guide, protocols, and ATBDs listed in the Documentation section below. Associated with these data are soil pedon descriptions and photos. These documents can be found on the NEON Data Portal under the Resources section, or here: https://data.neonscience.org/megapit-info Additional soil samples collected from the same soil pit are archived in the [NEON Megapit Soil Archive](https://www.neonscience.org/samples/soil-archive) and are available upon request.

Latency:
Data were collected once, at the establishment of each site. Data were published within one year of collection, and future collections at existing sites are not expected
description: The Soil physical and chemical properties, Megapit data product is available at each terrestrial site. The soil pit location was chosen to be representative of the sensor-based Soil Plots based on soil type, vegetation and topography, as well as being accessible by a backhoe and outside the main measurement zone of other sensors. The soil pit is usually within a few hundred meters of the sensor-based Soil Plots and NEON tower. Soil samples were collected by soil horizon up to 200 cm at non-permafrost sites (up to 300 cm at Alaskan sites). Laboratory analyses were conducted at the Kellogg Soil Survey Laboratory in Lincoln, Nebraska following the standard operating procedures outlined in the Soil Survey Laboratory Methods Manual, Report No. 42, Version 5, 2014.
DOI: 10.5067/gflnd-3g614
title: GFZ TELLUS GRACE-FO Level-3 Monthly Land Water-Equivalent-Thickness Surface Mass Anomaly Release 6.1 version 04
DOI: 10.5281/zenodo.8384168
title: DATA: Solute dispersion in accelerating flows

description: The data set (images, openFoam solver, plottings) of the journal paper.
DOI: 10.17592/001.2021110904
title: Ice thickness around Dome Fuji, Antarctica, based on JARE ground-based radar surveys: JARE40 data

description: This dataset contains the ice thickness data recorded in the Dome Fuji region, East Antarctica. The data was recorded by the 40th Japanese Antarctic Research Expedition (JARE40) using a pulse-modulated VHF radar sounder with a peak transmission power of 1kW, a center frequency of 179 MHz and a transmitter pulse width of 250 ns.
DOI: 10.17592/001.2021110906
title: Ice thickness around Dome Fuji, Antarctica, based on JARE ground-based radar surveys: JARE49 VHF 60 MHz data

description: This dataset contains the ice thickness data recorded in the Dome Fuji region, East Antarctica. The data was recorded by the 49th Japanese Antarctic Research Expedition (JARE49) using a pulse-modulated VHF radar sounder with a peak transmission power of 1kW, a center frequency of 60 MHz and a transmitter pulse width of 250 ns.
DOI: 10.18465/f53efa35-ebed-4ec6-870b-3fda081b5635
title: MNT Saint-Nazaire 2022

description: Modèle Numérique de Terrain obtenu par LiDAR sur la côte ligérienne au niveau de Saint-Nazaire
DOI: 10.5281/zenodo.8220670
title: PlayNet: Real-time Handball Play Classification with Kalman Embeddings and Neural Networks Dataset

description: Handball play classification dataset. On one hand we have player position and direction (x, y, vx, vy) estimated with a Kalman Filter, and on the other the ball position. For each tuple there is an associated play (right_attack, left_attack, right_transition, left_transition, time_out, right_penal, left_penal). There are two splits train and test.
DOI: 10.17592/001.2021110903
title: Ice thickness around Dome Fuji, Antarctica, based on JARE ground-based radar surveys: JARE37 data

description: This dataset contains the ice thickness data recorded in the Dome Fuji region, East Antarctica. The data was recorded by the 37th Japanese Antarctic Research Expedition (JARE37) using a pulse-modulated VHF radar sounder with a peak transmission power of 1kW, a center frequency of 179 MHz and a transmitter pulse width of 250 ns.
DOI: 10.17592/001.2021110905
title: Ice thickness around Dome Fuji, Antarctica, based on JARE ground-based radar surveys: JARE49 POL 179 MHz data

description: This dataset contains the ice thickness data recorded in the Dome Fuji region, East Antarctica. The data was recorded by the 49th Japanese Antarctic Research Expedition (JARE49) using a pulse-modulated POL radar sounder with a peak transmission power of 1kW, a center frequency of 179 MHz and a transmitter pulse width of 500 or 60 ns.
DOI: 10.17592/001.2021110907
title: Ice thickness around Dome Fuji, Antarctica, based on JARE ground-based radar surveys: JARE54 data

description: This dataset contains the ice thickness data recorded in the Dome Fuji region, East Antarctica. The data was recorded by the 54th Japanese Antarctic Research Expedition (JARE54) using a pulse-modulated POL radar sounder with a peak transmission power of 1kW, a center frequency of 179 MHz and a transmitter pulse width of 500 or 60 ns.
DOI: 10.48443/ghry-qw46
title: Soil water content and water salinity (DP1.00094.001)
title: RELEASE-2022

description: Soil volumetric water content and an index of soil water ion content (salinity) are measured at various depths below the soil surface from approximately 2 cm up to 200 cm at non-permafrost sites (up to 300 cm at Alaskan sites). Soil moisture is an important component of the hydrologic cycle and is the dominant source of water for most plants and soil organisms making it a key indicator of drought. In addition, soil moisture status influences the severity of flooding and temperature extremes, as well as physical, chemical and biological processes in the soil. Measurements are made in vertical profiles consisting of up to eight depths in all five instrumented soil plots at each terrestrial site, and presented as 1-minute and 30-minute averages.

Latency:
Data collected in any given month are published during the second full week of the following month.
description: When possible the soil plots were arranged in a transect with the first plot approximately 15-40 m from the tower in the expected dominant airshed. The middle of airshed was used as the transect vector and plot spacing was based on the distance required for surface soil temperature and moisture measurements to be spatially independent at the 1 hectare scale during site characterization (capped at approximately 40 m due to logistical constraints). Soil plots were microsited as necessary to avoid obstacles (e.g., boulders, streams, and paths) and more compact plot layouts were used at small sites. Soil moisture and salinity index are measured at up to eight depths within each plot, with the mid-point of the shallowest sensors at approximately 6, 16, and 26 cm. Depths for deeper sensors vary among sites and are based on megapit soil horizon data (NEON.DP1.00097) and depth to restrictive feature (see NEON.DOC.003146). Instrumentation: Sentek - EnviroSCAN TriSCAN
DOI: 10.17592/001.2021110909
title: Ice thickness around Dome Fuji, Antarctica, based on JARE ground-based radar surveys: JARE59 VHF 179 MHz data

description: This dataset contains the ice thickness data recorded in the Dome Fuji region, East Antarctica. The data was recorded by the 59th Japanese Antarctic Research Expedition (JARE59) using a pulse-modulated VHF radar sounder with a peak transmission power of 1kW, a center frequency of 179 MHz and a transmitter pulse width of 250 or 60 ns.
DOI: 10.5067/gflnd-3c614
title: CSR TELLUS GRACE-FO Level-3 Monthly Land Water-Equivalent-Thickness Surface Mass Anomaly Release 6.1 version 04
DOI: 10.5067/viirs/aerdb_l2_viirs_snpp.002
title: VIIRS/SNPP Deep Blue Aerosol L2 6-Min Swath 6 km
DOI: 10.18739/a26688j9z
title: Seasonal maximum ice thickness data for rivers and lakes in Alaska from 1962 to 2019

description: Ice growth through the winter integrates air and water temperature, snow conditions, wind, and hydrology. Thus the maximum thickness of ice provides an integrative measure of winter conditions that can be compared among years, regions, and water bodies. Estimates of maximum ice thickness (MIT) are provided for many rivers and lakes in Alaska. MIT estimates are based on late winter observations of ice thickness from numerous data sources fit to a temperature driven ice growth model (modified Stefan equation) for each year and site. These estimates provide a standardized comparison of ice thickness among water bodies and regions over a time when winter climate has been changing in Alaska.
DOI: 10.6084/m9.figshare.24552880.v1
title: Pavia et al. Supplementary Table S1

description: Supplementary Table S1 from Pavia et al., GCA. Locations, depths, calcium carbonate content, organic carbon content, and preliminary coretop age estimates from the model output of Restreppo et al. (2020) for cores used in this study.
DOI: 10.6084/m9.figshare.24552901.v1
title: Pavia et al. (GCA) Supplemental Table S2

description: Supplementary Table S1 from Pavia et al., GCA. Coretop uranium, thorium, and helium isotope data. The <sup>230</sup>Th<sub>xs,0</sub>, <sup>230</sup>Th<sub>xs,0</sub>-based MARs, and F/P values are computed using age corrections derived from the Restreppo et al. (2020) global sediment accumulation rate model.
DOI: 10.5281/zenodo.7002869
title: Dataset in GMD-2022-55

description: Dataset and plotting codes to reproduce the figures 5,9,10 and 11 in "Atmospherically relevant chemistry and aerosol box model – ARCA box (version 1.2)" (https://gmd.copernicus.org/preprints/gmd-2022-55/)
DOI: 10.5281/zenodo.8301052
title: Suspended sediment concentration mapping of a multi-channel system Songzi River of the Yangtze River Basin

description: We used Google Earth Engine and observed hydrological data to create a multiple linear regression model to map SSC in the multi-channel system Songzi River of the Yangtze. 

Hydrological data from gauging stations and Landsat surface reflectance data were collected in the study area. Water discharge and suspended sediment data were obtained from four hydrological stations, including Zhicheng, Xinjiangkou, Shadaoguan and Guanwan. Such water and sediment data were obtained from the Changjiang Water Resources Commission (CWRC). Before these datasets are released to the public, they undergo rigorous verification following the relevant government protocols. 

The Landsat program with nine satellites launched from 1972 to 2021 operated by National Aeronautics and Space Administration (NASA) and United States Geological Survey (USGS) is aimed at to detect changes in the Earth's resources and environments (https://earthexplorer.usgs.gov/). It provides the longest, continuous, moderate resolution earth observation data, which is currently free, globally available. According to the data availability the GEE platform, our study used the surface reflectance data ("LANDSAT/LT05/C01/T1_SR" and "LANDSAT/LC08/C01/ T1_SR") of Landsat 5 and Landsat 8 to investigate the spectral characteristics of SSC for the Songzi River.
DOI: 10.6084/m9.figshare.22769147.v1
title: Data for article simulation of Io plasma torus around Jupiter in perspective of Lenghu

description: The literature data is for the article simulation of Io plasma torus around Jupiter in perspective of Lenghu, include figure 2，4，6，7，8
DOI: 10.5281/zenodo.7579181
title: Modeling Flocculation Processes of Cohesive Sediment Through Moment Methodology

description: The data were used in the paper "Modeling Flocculation Processes of Cohesive Sediment Through Moment Methodology" which was submitted to "<em>Water Resources Research</em>". In this paper, a new mechanistic Lagrangian-type flocculation dynamic model was proposed by solving the population balance equation with moment methodology and similarity transformation, and the influence of particles' surface heterogeneities (<em>F</em><sub>2a</sub>) was incorporated. Furthermore, the roles of shear rate, sediment concentration, particle size and surface heterogeneity were investigated theoretically.
DOI: 10.17592/001.2021110908
title: Ice thickness around Dome Fuji, Antarctica, based on JARE ground-based radar surveys: JARE59 POL 179 MHz data

description: This dataset contains the ice thickness data recorded in the Dome Fuji region, East Antarctica. The data was recorded by the 59th Japanese Antarctic Research Expedition (JARE59) using a pulse-modulated POL radar sounder with a peak transmission power of 1kW, a center frequency of 179 MHz and a transmitter pulse width of 500, 100 or 60 ns.
DOI: 10.18739/a20p0ws3k
title: Saline permafrost degradation below a shallow thermokarst lake in northern Alaska, 2008-2023

description: This dataset supports the findings of the research paper submitted to the journal Geophysical Research Letters that documents the rapid thaw of saline permafrost below a shallow thermokarst lake near Utqiagvik, Alaska. The lake, East Twin Lake, is located in the Barrow Environmental Observatory. We conducted repeat drilling-based surveys at East Twin Lake in the Barrow Environmental Observatory near Utqiagvik, Alaska between 2008 and 2023. These field data were integrated with transient electromagnetic (TEM) near-surface geophysics soundings in 2016 and 2022 and analysis of a time-series of wintertime Synthetic Aperture Radar (SAR) satellite imagery from 2015 to 2023 to assess changes in lake and sub-lake properties. Finally, we assessed the impact of thawing saline permafrost on shore erosion by quantifying a regime shift in the lateral expansion rate of East Twin Lake between 1948 and 2022. The datasets consist of a CSV file with the point measurements from the drilling campaign, processed TEM data along with the script, a table of SAR backscatter values extracted for three lakes, and a table with lake expansion rates for East Twin Lake.