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1,826 results for “burn”
Data of the publication: Dispersive heterodyne probing method for laser frequency stabilization based on spectral hole burning in rare-earth doped crystals by O. Gobron et al.
<p>Data corresponding to the figures of the publication "Dispersive heterodyne probing method for laser frequency stabilization based on spectral hole burning in rare-earth doped crystals" by O. Gobron et al. (https://doi.org/10.1364/OE.25.015539). A text file describes data in each compressed folder, please refer to the caption in the publication for more details. </p>
Case Study Scenarios (CSS) 3 for Biomass Burning for Limb Nadir application
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Denoon Burn Graffiti Inscribed Stone
Slab of rock with graffiti lettering at OS 35455 41701 on E side of Denoon Burn ajacent to footpath . The letter J and inverted S, A + H, D + R, M, are visible. Lettering clearly visible on matcap. There are no visible cup marks and the lettering appears relatively modern. Canmore 281428 ScRAP ID 2441 Source: Objaverse 1.0 / Sketchfab
Stone 2mtr from Burn Betwixt the Laws Stone
This stone lies 2 mtrs from the Burn Betwixt the Laws Stone which was thought to have neolithic cup marks but on further examination it was determined the cup marks were natural geological anomalies. This smalller stone exhibited similar anomalies. NT 59450 59656 Canmore 342844 Shot with Huawei Mate Pro 10 mobile phone by Douglas Ledingham Source: Objaverse 1.0 / Sketchfab
Dataset of Evaluating the effects of biomass burning on severe haze formation in a megacity of Sichuan Basin, Southwestern China
<p><span>This dataset contain the concentrations of different chemical compositions, including organic aerosol, nitrate, sulfate, ammonium, chloride, BC, etc. The time series of different OA sources and meteorological parameters are also contained in the dataset.</span></p>
biomass burning emission contributions to ice nucleating particles
<p># Data for "<strong>Global biomass burning emission contributions to ice nucleating particles</strong>"</p> <p>This dataset contains ice nucleating particles emitted from biomass burning at -17°C to -30°C.</p>
Arid environmental manuscript for wildfire human opinion and burned area data
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Subspecies and Distribution. N. v. vison Schreber, 1776 — E Canada and NE USA (Allegheny Mts). N. v. aestuarina Grinnell, 1916 — SW USA (California & W Nevada). N. v. aniakensis Burns, 1964 — W Alaska. N. v. energumenos Bangs, 1896 — W Canada and NW USA. N. v. evagor Hall, 1932 — SW Canada (Vancouver I). N. v. evergladensis Hamilton, 1948 — SE USA (SW Florida). N. v. ingens Osgood, 1900 — most of Alaska and NW Canada (N Mackenzie & Yukon). N. v. lacustris Preble, 1902 — C Canada (Keewatin Region, Manitoba & Ontario). N. v. letifera Hollister, 1913 — Great Plains of USA. N. v. low Anderson, 1945 — E Canada (Labrador & Quebec). N. v. lutensis Bangs, 1898 — USA (S Carolina to Florida). N. v. melampeplus Elliot, 1903 — Alaska (Kenai Peninsula). N. v. mink Peale & Palisot de Beauvois, 1796 — SE USA. N. v. nesolestes Heller, 1909 — SW Alaska. N. v. vulgivaga Bangs, 1895 — USA (Arkansas & Louisiana). Introduced to Belarus, Belgium, China, Czech Republic, Denmark, Estonia, Finland, France, Germany, Great Britian, Iceland, Ireland, Italy, Japan (Hokkaido), Latvia, Lithuania, Netherlands, Norway, Poland, Portugal, Russia, Spain, and Sweden. in Mustelidae
Subspecies and Distribution. N. v. vison Schreber, 1776 — E Canada and NE USA (Allegheny Mts). N. v. aestuarina Grinnell, 1916 — SW USA (California & W Nevada). N. v. aniakensis Burns, 1964 — W Alaska. N. v. energumenos Bangs, 1896 — W Canada and NW USA. N. v. evagor Hall, 1932 — SW Canada (Vancouver I). N. v. evergladensis Hamilton, 1948 — SE USA (SW Florida). N. v. ingens Osgood, 1900 — most of Alaska and NW Canada (N Mackenzie & Yukon). N. v. lacustris Preble, 1902 — C Canada (Keewatin Region, Manitoba & Ontario). N. v. letifera Hollister, 1913 — Great Plains of USA. N. v. low Anderson, 1945 — E Canada (Labrador & Quebec). N. v. lutensis Bangs, 1898 — USA (S Carolina to Florida). N. v. melampeplus Elliot, 1903 — Alaska (Kenai Peninsula). N. v. mink Peale & Palisot de Beauvois, 1796 — SE USA. N. v. nesolestes Heller, 1909 — SW Alaska. N. v. vulgivaga Bangs, 1895 — USA (Arkansas & Louisiana). Introduced to Belarus, Belgium, China, Czech Republic, Denmark, Estonia, Finland, France, Germany, Great Britian, Iceland, Ireland, Italy, Japan (Hokkaido), Latvia, Lithuania, Netherlands, Norway, Poland, Portugal, Russia, Spain, and Sweden.
Data from: A burning issue: Savanna fire management can generate enough carbon revenue to help restore Africa's rangelands and fill protected area funding gaps
<p>Many savanna-dependent species in Africa including large herbivores and apex predators are at increasing risk of extinction. Achieving effective management of protected areas (PAs) in Africa where lions live will cost an estimated USD >$1-2 B/year in new funding. We explored the potential for fire management-based carbon-financing programs to fill this funding gap and benefit degrading savanna ecosystems. We demonstrated how introducing early dry season fire management programs could produce potential carbon revenues (PCR) from either a single carbon-financing method (avoided emissions) or from multiple sequestration methods ranging from USD $59.6-$655.9 M/year (at USD $5/ton) or USD $155.0 M–$1.7 B/year (at USD $13/ton). We highlighted variable but significant PCR for savanna PAs from USD $1.5–$44.4 M/year per PA. We suggest investing in fire management programs to jump-start the United Nations Decade of Ecological Restoration to help restore degraded African savannas and conserve imperiled keystone herbivores and apex predators. </p>
dataset for "Importance of phenols from biomass burning for aqSOA formation"
<p>These is dataset for manuscript titled "Importance of phenols from biomass burning for aqSOA formation".</p>
Data of publication "Impact of biomass burning and stratospheric intrusions in the remote South Pacific Ocean troposphere" by N. Daskalakis et al.
<p>Modeled data and measured data as used for the publication " Impact of biomass burning and stratospheric intrusions in the remote South Pacific Ocean troposphere" by N. Daskalakis et al. All measured data were obtained from the official sources, and model results are described in the publication. Please refer to the manuscript for further information for the data and the model.</p>
County-level of particle and gases emission inventory for animal dung burning in the Qinghai–Tibetan Plateau, China
<p><strong>County-level of particle and gases emission inventory for animal dung burning in the Qinghai–Tibetan Plateau, ChinaCounty-level of particle and gases emission inventory for animal dung burning in the Qinghai–Tibetan Plateau, China</strong></p>
Measurement report: The importance of biomass burning in light extinction and direct radiative effect of urban aerosol during the COVID-19 lockdown in Xi'an, China
<p>To explore the impacts of anthropogenic emissions on aerosol optical properties and direct radiative effect (DRE), a series of real-time measurements was conducted in an urban area of China before and during the lockdown of Coronavirus Disease 2019. The generalized addictive model analysis shows that the light extinction coefficient (<em>b</em><sub>ext</sub>) decreased largely during the lockdown due to the sharp reductions in anthropogenic emissions. Organic aerosol was the largest contributor to <em>b</em><sub>ext</sub> based on the ridge regression analysis. A hybrid environmental receptor model combining with chemical and optical variables shows that <em>b</em><sub>ext</sub> from biomass burning increased in the lockdown due to the undiminished needs of residential cooking and heating in winter. Biomass burning contributed the largest positive effect to aerosol DRE in the atmosphere during the lockdown, highlighting the importance of controlling biomass burning for mitigating climate change in China in the future.</p>
Data from: Size, species, and fire behavior predict tree and liana mortality from experimental burns in the Brazilian Amazon
<p>Anthropogenic understory fires have affected large areas of tropical forest in recent decades, particularly during severe droughts. Yet, the mechanisms that control fire-induced mortality of tropical trees and lianas remain ambiguous due to the challenges associated with documenting mortality given variation in fire behavior and forest heterogeneity. In a seasonally dry Amazon forest, we conducted a burn experiment to quantify how increasing understory fires alter patterns of stem mortality. From 2004 to 2007, tree and liana mortality was measured in adjacent 50-ha plots that were intact (B0 – control), burned once (B1), and burned annually for 3 years (B3). After 3 years, cumulative tree and liana mortality (≥1 cm dbh) in the B1 (5.8% yr<sup>−1</sup>) and B3 (7.0% yr<sup>−1</sup>) plots significantly exceeded mortality in the control (3.2% yr<sup>−1</sup>). However, these fire-induced mortality rates are substantially lower than those reported from more humid Amazonian forests. Small stems were highly vulnerable to fire-induced death, contrasting with drought-induced mortality (measured in other studies) that increases with tree size. For example, one low-intensity burn killed >50% of stems <10 cm within a year. Independent of stem size, species-specific mortality rates varied substantially from 0% to 17% yr<sup>−1</sup> in the control, 0% to 26% yr<sup>−1</sup> in B1, and 1% to 23% yr<sup>−1</sup> in B3, with several species displaying high variation in their vulnerability to fire-induced mortality. <em>Protium guianense</em> (Burseraceae) exhibited the highest fire-induced mortality rates in B1 and B3, which were 10- and 9-fold greater than the baseline rate. In contrast, <em>Aspidosperma excelsum</em> (Apocynaceae), appeared relatively unaffected by fire (0.3% to 1.0% mortality yr<sup>−1</sup> across plots), which may be explained by fenestration that protects the inner concave trunk portions from fire. For stems ≥10 cm, both char height (approximating fire intensity) and number of successive burns were significant predictors of fire-induced mortality, whereas only the number of consecutive annual burns was a strong predictor for stems <10 cm. Three years after the initial burn, 62 ± 26 Mg ha<sup>−1</sup> (s.e.) of live biomass, predominantly stems <30 cm, was transferred to the dead biomass pool, compared with 8 ± 3 Mg ha<sup>−1</sup> in the control. This biomass loss from fire represents ∼30% of this forest's aboveground live biomass (192 (±3) Mg ha<sup>−1</sup>; >1 cm DBH). Although forest transition to savanna has been predicted based on future climate scenarios, our results indicate that wildfires from agricultural expansion pose a more immediate threat to the current carbon stocks in Amazonian forests.</p>
Core outcome set for burn care research: Delphi survey data
<p><strong>Background:</strong> Collated evidence from systematic reviews supports clinicians in identifying optimal treatment for patients. Evidence is created from outcomes that, in burn care, include survival, function, cosmesis, pain, and psychological well-being. Currently, this is limited because of variation in outcomes reported across trials. Improved selection and reporting of outcomes in primary research in burn care could improve treatment globally by improving data synthesis and the quality of evidence. The availability of a Core Outcome Set (COS), a minimum set of the most important outcomes to be reported in all trials of a medical condition, would resolve this issue. The aim of this study is to develop a COS for international burn care research.</p> <p><strong>Methods and findings</strong>: Candidate outcomes were identified from systematic reviews and stakeholder interviews. Through two rounds of a Delphi survey, international multi-disciplinary clinicians, researchers, and UK patients and carers prioritised the outcomes. Anonymised feedback aimed to achieve consensus. Pre-defined criteria for retaining and dropping outcomes were agreed upon. A consensus meeting with voting was held to finalise the COS.</p> <p>Examination of all data sources identified 1,021 unique outcomes grouped into 88 candidate outcomes. Stakeholders included 668 health professionals from 77 countries and 126 UK patients/carers; 25% of clinical participants were from low- or low-middle-income countries. After Round 1, one outcome was discarded, and 13 new outcomes were added. After Round 2, 69 items were discarded, leaving 31 outcomes for the consensus meeting.<em> </em>Discussion and voting agreed on seven core outcomes: death, specified complications, ability to do daily tasks, time to wound healing, neuropathic pain and itch, psychological well-being, and time to return to school/work.</p> <p><strong>Conclusions</strong>: This is the first COS for international burn care research. Implementation is now needed to improve data synthesis, and support evidence-based clinical decision-making in global burn care. It is recommended that future trials include measures of these seven outcomes.</p>
Supplementary Material: Fire trapped in ice - An introduction to biomass burning records from high-alpine and polar ice cores
<p>Compilation of fire records in ice cores: supplementary material to “Fire trapped in ice - An introduction to biomass burning records from high-alpine and polar ice cores.” This document includes a table of selected paleofire records from ice cores by region with indication of measured proxies and time span.</p>
Duncroisk Burn 1, Glen Lochay, Perthshire
A large boulder in Glen Lochay with multiple cups and several eroded cup and ring motifs on its upper surface. Source: Objaverse 1.0 / Sketchfab
Day of burning dataset: Biogeography of daily wildfire progression
<p><strong>Introduction</strong></p> <p>Climate change is predicted to increase the frequency of extreme single-day fire spread events, with major ecological and social implications. In contrast with well-documented spatio-temporal patterns of wildfire ignitions and perimeters, daily progression remains poorly understood across continental spatial scales, particularly for extreme single-day events ("blow ups"). Here, we characterize daily wildfire spread across North America, including occurrence of extreme single-day events, duration and seasonality of fire and extremes, and ecoregional climatic niches of fire in terms of Actual Evapotranspiration (AET) and Climatic Water Deficit (CWD) annual climate normals.</p> <p><strong>Methods</strong></p> <p>Remotely sensed daily progression of 9,636 wildfires ≥400 ha was used to characterize ecoregional patterns of fire growth, extreme single-day events, duration, and seasonality. To explore occurrence, extent, and impacts of single-day extremes among ecoregions, we considered complementary ecoregional and continental extreme thresholds (Ecoregional or Continental Mean Daily Area Burned + 2SD). Ecoregional spread rates were regressed against AET and CWD to explore climatic influence on spread.</p> <p><strong>Results</strong></p> <p>We found three-fold differences in mean daily area burned among 10 North American ecoregions, ranging from 260 ha day<sup>-1</sup> in the Marine West Coast Forests to 751 ha day<sup>-1 </sup>in Mediterranean California. Ecoregional single-day extreme thresholds ranged from 3829 ha day<sup>-1</sup> to 16626 ha day<sup>-1</sup>, relative to a continental threshold of 7173 ha day<sup>-1</sup>. The ~3% of single-day events classified as extreme cumulatively account for 16-55% of ecoregional total area burned. There were four-fold differences in mean fire duration, ranging from 2.7 days in the Great Plains to 10.5 days in the Northwestern Forested Mountains. CWD had a weak positive relationship with ecoregional spread, and there was no pattern for AET.</p> <p><strong>Discussion</strong></p> <p>Regions with shorter fire durations had greater daily area burned, suggesting a paradigm of fast-growing short-duration fires in some regions and slow-growing long-duration fires elsewhere. Although climatic conditions can set the stage for ignition and influence vegetation and fuels, finer-scale mechanisms likely drive variation in daily spread. Daily fire progression offers valuable insights into the regional and seasonal distributions of extreme single-day spread events, and how these events shape net fire effects.</p>
Figure 6. Burned area per month detected between 1985 and 2020 in Breeding biology of the Ochre-breasted pipit (Anthus nattereri), with notes on its conservation in the Upper Rio Grande Grasslands, south-eastern Brazil
Figure 6. Burned area per month detected between 1985 and 2020 in São João del-Rei, south-eastern Brazil. Data from the MapBiomas (2022). The dotted line indicates the average across months.
On Carbon Burning in Super Asymptotic Giant Branch Stars
<p>This entry contains input files to reproduce the results of the paper: <a href="https://ui.adsabs.harvard.edu/#abs/2015ApJ...807..184F/abstract">On Carbon Burning in Super Asymptotic Giant Branch Stars </a></p> <p>MESA version used: 6794</p>
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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)
ABODe is a University of Edinburgh DataShare dataset for behavior classification in group-housed mice using home-cage video, identities, bounding boxes, ground-plate positions, and annotator labels.
DANDI Archive for NWB datasets
DANDI is a BRAIN Initiative archive for publishing and sharing neurophysiology data, including electrophysiology, optophysiology, and behavioral data packaged as NWB and related standards.
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.
OpenNeuro
OpenNeuro is a free, open platform for sharing neuroimaging datasets, with public search, dataset pages, and download paths for web, S3, DataLad, and the OpenNeuro CLI.