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396 results for “Humidity”

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dryad36/100

Great Basin National Park, NV air temperature and relative humidity

Hourly air temperature and relative humidity data has been collected from a network of 29 data-logging sensors installed within radiation shields ~1.5 m above ground level at discrete sites within the Great Basin National Park (GBNP), NV, USA from August 2006 to August 2023. The sensors are "embedded" – suspended in trees or atop wooden stakes – within diverse ecosystem types spanning over 2,000 m of elevation, and are maintained/downloaded during annual visitations by collaborating teams of students and staff from the Ohio State University, University of Georgia, and Sinclair Community College, assisted by GBNP staff. This dataset can be utilized to assess the microclimates and weather patterns within the GBNP. The dataset comprises daily mean, maximum, and minimum temperature and relative humidity collected between Aug 2006 – Aug 2023. Hourly, raw data are available upon request.

opencc-zeroSep 2023View details →

dryad36/100

Rapid and reversible humidity-dependent colour change by water film formation in a scaled springtail: Image compilations and video recordings

Colour is often not a static trait but can change over time either through biotic or abiotic factors. Humidity-dependent colour change can occur through either morphological change (e.g. to feather barbules in birds) or by the replacement of air by water causing a shift in refractive index, as seen in arthropod multilayer cuticles or scales. The scaled springtail Lepidocyrtus cyaneus has scales that produce color largely via thin film interference from their lamina. We observed a marked colour change from golden to violet/purple colouration in humid conditions. Light microscopy, microspectrophotometry, contact angle goniometry and optical modelling indicate that the formation of a thin film of water on top of the hydrophilic scales increases their laminar thin film thickness, causing a shift towards violet/purple colour. Evaporation of the water film causes the metallic golden colour to return. This constitutes a remarkably rapid colour change (in the order of seconds), only limited by the speed of water film condensation and evaporation, that may serve as inspiration for new dynamically coloured materials and sensors.

opencc-zeroSep 2023View details →

zenodo36/100

Runoff threshold responses in continental Boreal catchments: Nexus of sub-humid climate, low-relief, surficial geology and land cover

Revision in journal Water Resources Research,Paper # 2023WR034752RR the publication doi:  <a href="https://doi.org/10.1029/2023WR034752">doi.org/10.1029/2023WR034752</a> Abstract We examined annual runoff from 20 meso-scale catchments over 25 years, to elucidate how interactions between physiography and long-term weather patterns influence the magnitude of spatial-temporal thresholds in annual runoff responses in water-limited, low-relief, glaciated continental Boreal landscapes. Annual runoff ranged over two orders of magnitude (<3 to >300 mm) among catchments receiving similar annual precipitation. Threshold relationships were observed with cumulative regional moisture deficits that reflected spatial-temporal differences in effective storage and antecedent moisture among catchments with differing portions of glacial-deposit and land-cover types. The importance of the glacial-deposit texture and forest-peatland cover on runoff behavior among catchments varied with weather patterns and catchment antecedent moisture states. Dry states yielded low annual runoff that ranged by two orders of magnitude (0 to 80 mm), with higher values in catchments with predominantly coarse-textured deposits. During near normal antecedent moisture, annual runoff remained low (<10 mm) in catchments associated with fine-textured, hummocky landforms and deciduous forests. Annual runoff >10 mm was observed only in catchments with extensive peatlands. Infrequent wet states resulted in increased runoff in all catchments; however, ranges in maximum runoff were associated with heterogeneity in catchment landforms and land covers. Integrating cumulative precipitation with the proportion of glacial-deposit and land-cover types within catchments can: 1) represent water cycling and regional sink-source dynamics controlling runoff, and 2) provide an effective management framework for predicting climate and land-use impacts on regional runoff in water-limited, low-relief, glaciated landscapes such as the Boreal Plain.

opencc-by-4.0Sep 2023View details →

ClinicalTrials.gov36/100

The Effects of Cyclosporin A in a Low Humidity Environment, on the Ocular Surface

ClinicalTrials.gov study NCT02199964. IPD Sharing: NO. Countries: 1. Publications: 1.

closedIPD-NOFeb 2026View details →

ClinicalTrials.gov36/100

Effects of Taurine Supplementation on Repetitive Sprint Performance and Exhaustion Time in College Students Under High-Temperature and High-Humidity Conditions

ClinicalTrials.gov study NCT06824571. IPD Sharing: YES. Countries: 1. Publications: 0.

controlledIPD-YESFeb 2026View details →

dryad36/100