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Heat pumps for all? Distributions of the costs and benefits of residential air-source heat pumps in the United States
<p>Dataset for the "<span>Heat pumps for all? Distributions of the costs and benefits of residential air-source </span><span>heat pumps in the United States" paper</span></p>
Data for: Characterization of large-scale preferential flow across continental United States
<p>Understanding preferential flow (PF) at large scales is critical for improving land management and groundwater (GW) quality. However, limited knowledge of this process, due to soil surface heterogeneity and observational constraints, hampers progress. In this study, we propose estimating effective PF at remote sensing footprint scale (4 – 9 km) by examining its impact on soil moisture (SM) distribution and shallow GW (SGW) table fluctuations (depth 5 m). Effective PF encompasses macropore, funnel, and finger flow pathways influencing SGW table fluctuations. We compiled daily SGW observations (2019-2021) from 19 continental US (CONUS) sites through USGS. Using inverse modeling in HYDRUS-1D, SGW data, and CHIRPS precipitation data, we inversely estimated soil hydraulic parameters of the dual porosity model (DPM) simulating vertical flow from soil surface to subsurface. Effective PF presence was inferred using three criteria: (1) daily precipitation >= the site-specific average across multiple (calibration) years, (2) daily observed SGW table increase, and (3) daily difference between observed and DPM simulated SGW tables 50% of the site-specific RMSE. Leveraging optimized DPM parameters and associated soil texture, classified PF events, and Soil Moisture Active Passive (SMAP L3E) satellite-based SM, a Random Forest algorithm with 10-fold cross validation predicted large-scale effective PF events. Results indicate seasonal dependence, with spring having the highest occurrence of PF events. The Random Forest model achieved 98% accuracy in predicting large-scale PF events, with SMAP SM and saturated hydraulic conductivity (Ks) among the 4 most impactful variables. Our approach provides a soil hydraulic property, site characteristic, soil texture and remote sensing based generalized tool to analyze large-scale effective PF.</p>
FIG. 7 in A new operculate symmoriiform chondrichthyan from the Late Mississippian Fayetteville Shale (Arkansas, United States)
FIG. 7. — Consensus of eight most parsimonious trees. Bootstrap values are shown above branches; bootstrap values below 50 are not shown. New taxon Cosmoselachus n. gen. indicated by yellow highlight, holocephalan group and symmoriiform group indicated in differing shades of gray.
FIG. 5. — Cosmoselachus mehlingi n. gen., n in A new operculate symmoriiform chondrichthyan from the Late Mississippian Fayetteville Shale (Arkansas, United States)
FIG. 5. — Cosmoselachus mehlingi n. gen., n. sp., specimen AMNH FF 20509: A, cross section through the posterior half of the specimen, at the point indicated by the inset 3D reconstruction, showing multilayered opercular structure made of cartilaginous branchial rays, fused to one another. Layer of rays from the first branchial arch (behind the hyoid arch) indicated by the second-from-left arrowhead. The right-most arrowhead marks the second row of pharyngeal rays (first branchial arch); another layer (second branchial arch) can be found just beneath it (second arrowhead from the right). Hyoid operculum appears to fold at the arrowhead furthest to the left; B, longitudinal section of posterior half of AMNH FF 20509 showing hyoid operculum (right-most arrowhead) and additional elongate branchial rays (left two arrowheads). Anterior to left, slice location within the specimen indicated by 3D reconstruction in the upper right corner. Scale bars: 5 cm.
FIG. 3. — A in A new operculate symmoriiform chondrichthyan from the Late Mississippian Fayetteville Shale (Arkansas, United States)
FIG. 3. — A, Tooth families of Cosmoselachus n. gen. on the Meckel's cartilages, with denticles between tooth families. Teeth make contact but have no fused bases, dorsal oblique labial view; B, detail of tooth batteries in axial section, anterior to right, showing denticles between each tooth family, on the scalloped Meckel's cartilage. Abbreviations: d, denticles; mc, Meckel's cartilage; t, teeth. Scale bars: A, B, 4 cm; C, 2 mm.
FIG. 2. — Cosmoselachus mehlingi n. gen., n in A new operculate symmoriiform chondrichthyan from the Late Mississippian Fayetteville Shale (Arkansas, United States)
FIG. 2. — Cosmoselachus mehlingi n. gen., n. sp., three-dimensional renderings of specimen AMNH FF 20509, produced by computed tomographic (CT) scanning: A, ventral view of posterior half of specimen, anterior to top; B, ventral view of anterior part of the specimen, anterior to right, with opercular elements removed; C, dorsal view of anterior half of specimen, anterior to right. Note loss of anterior portion of cranium due to taphonomy. Abbreviations: add, depression potentially for adductor musculature; c, cranium; cb, ceratobranchials; ch, ceratohyals; d, denticles; mc, Meckel's cartilage; op, opercular cartilage; pa f, pharyngeal arch fragments; pq, palatoquadrate fragment; t, teeth. Scale bars: 5 cm.
FIG. 1. — Cosmoselachus mehlingi n. gen., n in A new operculate symmoriiform chondrichthyan from the Late Mississippian Fayetteville Shale (Arkansas, United States)
FIG. 1. — Cosmoselachus mehlingi n. gen., n. sp., specimen AMNH FF 20509, anterior to right: A, entire specimen, ventral view. Abbreviations: mc, Meckel's cartilage; op, opercular flap; B, detail of opercular flap. Scale bars: A, 5 cm; B, 2 cm. Photographs by Lorraine Meeker.
FIG. 6. — Cosmoselachus mehlingi n. gen., n in A new operculate symmoriiform chondrichthyan from the Late Mississippian Fayetteville Shale (Arkansas, United States)
FIG. 6. — Cosmoselachus mehlingi n. gen., n. sp., partial basicranium of specimen AMNH FF 20509: A, dorsal view; B, ventral view. Anterior to top. Abbreviations: da?, possible opening for the dorsal aorta; occ, occiput; ot cap, otic capsule. Scale bar: 3 cm.
Text-fig. 1. Map of the early Eocene Okanagan Highlands British Columbia, Canada and Washington, United States of America. Modified from Archibald et al. 2014: fig. 2, courtesy of Bruce Archibald. in The Early Eocene Flora Of Horsefly, British Columbia, Canada And Its Phytogeographic Significance
Text-fig. 1. Map of the early Eocene Okanagan Highlands British Columbia, Canada and Washington, United States of America. Modified from Archibald et al. 2014: fig. 2, courtesy of Bruce Archibald.
An ensemble of 48 physically perturbed model estimates of the 1/8° terrestrial water budget over the conterminous United States, 1980–2015
<p>This dataset contains the 1980–2015 monthly terrestrial water budget simulated by a 48-member perturbed-physics ensemble configured from the Noah LSM with multi-physics options (Noah‑MP v3.6). Simulation outputs include total evapotranspiration and its constituents (canopy evaporation, soil evaporation, and transpiration), runoff (the surface and subsurface components), as well as terrestrial water storage (snow water equivalent, four-layer soil water content from the surface down to 2 m, and the groundwater storage anomaly). The file name has four parts: the abbreviation for "terrestrial water budget", the used parameterization, the time scale, and the suffix.</p> <p>The 48 physics configurations are generated by combining four runoff parameterizations (run1: SIMGM, run2: SIMTOP, run3: NOAHR, run4: BATS), two parameterizations of stomatal conductance (can1: Ball–Berry, can2: Jarvis), three parameterizations of soil moisture stress factor (btr1:NOAHB, btr2: CLM, btr3: SSiB), and two parameterizations of near-surface atmospheric turbulence (tub1: M-O, tub2: Chen97).</p> <p>The simulation domain covers the all of conterminous United States (25°–53°N, 125°–67°W), which is also called the NLDAS-2 testbed (Xia et al., 2012a, b). The simulations were performed at a spatial resolution of 0.125°, which is the same as for NLDAS-2 models. Details of the simulation settings and spin-up run can be found in Section 2.3 of Zheng et al. (2019) and Section 2.2 of Fei et al. (2021).</p>
Sci-Fi movies by inflation-adjusted gross revenue in the United States.
<p>Sci-Fi movies by inflation-adjusted gross revenue in the United States.</p> <p>The dataset is a .csv file with < ; >used as separator.</p> <p>The dataset has the next columns:</p> <ul> <li>Title: movie title.</li> <li>Release_Year: year of the movie's release.</li> <li>Watchtime: movie duration in minutes.</li> <li>Genre: genre.</li> <li>Movie_Rating: IMDB movie rating.</li> <li>Metascore: metacritic movie rating.</li> <li>Votes: number of ratings.</li> <li>Gross_collection: incomes generated by the movie.</li> <li>Sinopsis.</li> <li>Director.</li> <li>Star: main actors.</li> <li>Gross_equivalent: income generated by movies with dollar devaluation correction.</li> </ul> <p> </p> <p> </p> <p> </p> <p> </p> <p> </p> <p> </p>
FIG. 1 in New occurrences of crabs (Decapoda, Brachyura, Eubrachyura) in the Pliocene of Florida (United States)
FIG. 1. — Location map of the two fossiliferous localities of the Pliocene Tamiami Formation in Sarasota County, Florida (United States). Locality A: SMR Aggregates quarry (27°20'05"N, 82°19'58"W). Locality B: Old APAC Shell quarry (27°14'18"N, 82°27'11"W). Maps modified after different sources and ViaMichelin.
FIG. 2 in New occurrences of crabs (Decapoda, Brachyura, Eubrachyura) in the Pliocene of Florida (United States)
FIG. 2. — Persephona cf. P. subovata (Rathbun, 1893), USNM PAL 720104 from the Pinecrest Member of Tamiami Formation (middle Piacenzian, Pliocene) of locality A in Sarasota County, Florida (United States): A, dorsal view; B, frontal view; C, left lateral view; D, posterior view. Scale bar: 10 mm. Photographs by À. Ossó.
FIG. 3 in New occurrences of crabs (Decapoda, Brachyura, Eubrachyura) in the Pliocene of Florida (United States)
FIG. 3. — Paractaea cf. P. nodosa (Stimpson, 1860), USNM PAL 720105 from the Pinecrest Member of Tamiami Formation (middle Piacenzian, Pliocene) of locality B in Sarasota County, Florida (United States): A, dorsal view; B, frontal view; C, posterior view. Scale bar: 10 mm. Photographs by À. Ossó.
Figures 1–3 in A new species of Buprestis (s. str.) Linnaeus, 1758 (Coleoptera: Buprestidae) from the southwestern United States
Figures 1–3. Buprestis (s. str.) pinyoni male holotype. 1) After being relaxed. 2) Prior to being relaxed. 3) Aedeagus, dorsal view.
Figure 2 in The eriophyid mite Aculops ailanthi Lin, Jin, & Kuang, 1997 (Acariformes: Prostigmata: Eriophyidae) from tree-of-heaven in the United States - new state records and morphological observations
Figure 2 Stereomicrographs (2a–b) and SEMs (2c–f) ofAculops ailanthi: General aspect of colonies on leaves and morphological traits:** 2a–b – prodorsal shield; 3c – mite infestation of a leaf; 2d – mite feeding on a trichome; 2e – nymph next to an egg, note the lack of reticulate cells on the prodorsal shield; 2f – dorsum.
Figure 1 in The eriophyid mite Aculops ailanthi Lin, Jin, & Kuang, 1997 (Acariformes: Prostigmata: Eriophyidae) from tree-of-heaven in the United States - new state records and morphological observations
Figure 1 Treeofheaven damaged byAculops ailanthi Lin, Jin, & Kuang feeding: 1a – healthy leaf without mite infestation; 1b – leaf showing severe stippling; 1c – leaf showing yellowing, stippling, and necrosis; 1d – leaf necrosis; 1e – mites on leaf surface after an application of a 2% solution of MPede insecticidal soap.
Interpolated depth to water table (groundwater) maps for the continental United States
<p><strong>DATA:</strong></p> <p>This is a collection of depth to water table maps with uncertainty estimates for the continental United States for years 1989 and 2019. Data used to create these maps were obtained from the National Ground-Water Monitoring Network (NGWMN). Data included 14,351 sites and 17,632,047 observations for the years 1989-2019. To improve our inference a set of auxiliary variables proven to have a relation with depth to water table were included. We paired point estimates of depth to water table data with environmental data, as well as terrain variables derived out of a base digital elevation model (DEM) created by NASA at a 1x1km resolution. Climatic layers (temperature, precipitation, and snow melt equivalent) for 1989-2019 were obtained from Daymet (Version 4), which provides a continuous grid of historical monthly and annual weather data, with a 1x1km spatial resolution (Thornton et al., 2020). Out of the DEM, primary (slope, aspect) and secondary terrain attributes (curvatures, upslope contributing areas) were used to calculate a compound topographic index (CTI). </p> <p> </p> <p><strong>MODELING FRAMEWORK:</strong></p> <p>Water table depth analyses were conducted using a three-step interpolation approach: 1) we utilized gradient boosted regression trees (GBRT) to make predictions, 2) we used kriging interpolation on GBRT residuals to reduce bias from spatial autocorrelation, to incorporate a spatial correlation structure and to create uncertainty maps, and 3) we then combined the GBRT and kriging predictions for the final map. This method is equivalent to a Universal Kriging, where in our case, we evaluated the trend using GBRT. Model metrics were calculated for the training (80% of the data) and validation (20% of the data) datasets to evaluate overall performance.</p> <p>*** Uncertainty is greater surrounding the 1989 interpolations due to a lower number of observations.</p>
Figures 1–9. Ardella magnaemirabilis Paulsen, new species. 1–4 in Ardella magnaemirabilis (Coleoptera: Scarabaeidae: Melolonthinae: Ardellini), a new scarabaeoid species, genus and tribe from the southwestern United States
Figures 1–9. Ardella magnaemirabilis Paulsen, new species. 1–4) Holotype male. 1) Dorsal view. 2) Lateral view. 3) Labels. 4) Ventral view of head and pronotum. 5–9) Paratype male. 5) Dorsal view of head and pronotum. 6) Oblique view of male genitalia. 7) Cleft protarsal (left) and metatarsal (right) claws. 8) Dorsal view of right metatibia and metatarsus showing spurs not reaching past tibial apex and simple claws. 9) Right wing, dorsal view.
Figures 73–78 in Culicoides Latreille and Leptoconops Skuse biting midges of the southwestern United States with emphasis on the Canyonlands of southeastern Utah (Diptera: Ceratopogonidae)
Figures 73–78. Male genitalia of Culicoides subgenus Diphaomyia, ventral view. 73) C. defoliarti-haematopotus, focused on aedeagus (A), paramere (P). 74) C. defoliarti-haematopotus, focused on ventral apodemes of gonocoxites (Gcva) and median lobes on parameres (Pml). 75) C. inyoensis, posterior projections on basal arms of aedeagus circled. 76) C. erikae, median lobes on parameres circled. 77) C. salihi, focused on aedeagus and parameres, posterior projections on basal arms of aedeagus (App). 78) C. salihi, focused on posterior portion of ventral apodemes of gonocoxites, circled.
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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.