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Research data keyboard_double_arrow_right Dataset 2023Publisher:Zenodo Funded by:EC | REINFORCEEC| REINFORCEInput files for the ForClim model (version 4.0.1) used in the associated paper. They can be used to to reproduce results of the simulation study. The ForClim model, including the source code, executable and documentation, is freely available under an Open Access license from the website of the original developers at https://ites-fe.ethz.ch/openaccess/. The original climatic dataset used to generate the ForClim input climate files at each site in South Tyrol is freely available at https://doi.pangaea.de/10.1594/PANGAEA.924502 while the CHELSA climate data for future scenarios are available at https://www.chelsa-climate.org. If interested in using this dataset for a research study or a project, please contact Marco Mina ----------------------------------------------------------------------- Hillebrand L, Marzini S, Crespi A, Hiltner U & Mina M (2023) Contrasting impacts of climate change on protection forests of the Italian Alps. Frontiers in Forests and Global Change, 6, 2023 https://doi.org/10.3389/ffgc.2023.1240235 ABSTRACT. Protection forests play a key role in protecting settlements, people, and infrastructures from gravitational hazards such as rockfalls and avalanches in mountain areas. Rapid climate change is challenging the role of protection forests by altering their dynamics, structure, and composition. Information on local- and regional-scale impacts of climate change on protection forests is critical for planning adaptations in forest management. We used a model of forest dynamics (ForClim) to assess the succession of mountain forests in the Eastern Alps and their protective effects under future climate change scenarios. We investigated eleven representative forest sites along an elevational gradient across multiple locations within an administrative region, covering wide differences in tree species structure, composition, altitude, and exposition. We evaluated protective performance against rockfall and avalanches using numerical indices (i.e., linker functions) quantifying the degree of protection from metrics of simulated forest structure and composition. Our findings reveal that climate warming has a contrasting impact on protective effects in mountain forests of the Eastern Alps. Climate change is likely to not affect negatively all protection forest stands but its impact depends on site and stand conditions. Impacts were highly contingent to the magnitude of climate warming, with increasing criticality under the most severe climate projections. Forests in lower-montane elevations and those located in dry continental valleys showed drastic changes in forest structure and composition due to drought-induced mortality while subalpine forests mostly profited from rising temperatures and a longer vegetation period. Overall, avalanche protection will likely be negatively affected by climate change, while the ability of forests to maintain rockfall protection depends on the severity of expected climate change and their vulnerability due to elevation and topography, with most subalpine forests less prone to loosing protective effects. Proactive measures in management should be taken in the near future to avoid losses of protective effects in the case of severe climate change in the Alps. Given the heterogeneous impact of climate warming, such adaptations can be aided by model-based projections and high local resolution studies to identify forest stand types that might require management priority for maintaining protective effects in the future.
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For further information contact us at helpdesk@openaire.euResearch data keyboard_double_arrow_right Dataset 2021Publisher:Dryad Authors:Leahy, Lily;
Scheffers, Brett R.; Andersen, Alan N.; Hirsch, Ben T.; +1 AuthorsLeahy, Lily
Leahy, Lily in OpenAIRELeahy, Lily;
Scheffers, Brett R.; Andersen, Alan N.; Hirsch, Ben T.; Williams, Stephen E.;Leahy, Lily
Leahy, Lily in OpenAIREAim: We propose that forest trees create a vertical dimension for ecological niche variation that generates different regimes of climatic exposure, which in turn drives species elevation distributions. We test this hypothesis by statistically modelling the vertical and elevation distributions and microclimate exposure of rainforest ants. Location: Wet Tropics Bioregion, Australia Methods: We conducted 60 ground-to-canopy surveys to determine the vertical (tree) and elevation distributions, and microclimate exposure of ants (101 species) at 15 sites along four mountain ranges. We statistically modelled elevation range size as a function of ant species’ vertical niche breadth and exposure to temperature variance for 55 species found at two or more trees. Results: We found a positive association between vertical niche and elevation range of ant species: for every 3 m increase in vertical niche breadth our models predict a ~150% increase in mean elevation range size. Temperature variance increased with vertical height along the arboreal gradient and ant species exposure to temperature variance explained some of the variation in elevation range size. Main Conclusions: We demonstrate that arboreal ants have broader elevation ranges than ground-dwelling ants and are likely to have increased resilience to climatic variance. The capacity of species to expand their niche by climbing trees could influence their ability to persist over broader elevation ranges. We propose that wherever vertical layering exists - from oceans to forest ecosystems - vertical niche breadth is a potential mechanism driving macrogeographic distribution patterns and resilience to climate change. Data_collections.csv Main survey collections data in a site by species matrix showing all data for all sites surveyed. Tuna baited vials were placed every three metres from ground to canopy in trees at elevation sites at four subregion mountain ranges of the Australian Wet Tropics Bioregion. Note data file includes empty vials that lacked ants. Microclimate_AthertonTemp.csv This file contains Atherton Uplands temperature data from ibuttons deployed at one tree per elevation (200, 400, 600, 800, 1000) at every three metres in height in Dec-Jan 2017- 2018 set to record every half hour. See file Metadata for details of column names and data values.
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visibility 28visibility views 28 download downloads 34 Powered bymore_vert add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.euResearch data keyboard_double_arrow_right Dataset 2022Publisher:Zenodo Authors:Vidaller, Ixeia;
Vidaller, Ixeia
Vidaller, Ixeia in OpenAIREIzagirre, Eñaut;
Izagirre, Eñaut
Izagirre, Eñaut in OpenAIREdel Río, Luis Mariano;
del Río, Luis Mariano
del Río, Luis Mariano in OpenAIREAlonso-González, Esteban;
+5 AuthorsAlonso-González, Esteban
Alonso-González, Esteban in OpenAIREVidaller, Ixeia;
Vidaller, Ixeia
Vidaller, Ixeia in OpenAIREIzagirre, Eñaut;
Izagirre, Eñaut
Izagirre, Eñaut in OpenAIREdel Río, Luis Mariano;
del Río, Luis Mariano
del Río, Luis Mariano in OpenAIREAlonso-González, Esteban;
Alonso-González, Esteban
Alonso-González, Esteban in OpenAIRERojas-Heredia, Francisco;
Rojas-Heredia, Francisco
Rojas-Heredia, Francisco in OpenAIRESerrano, Enrique;
Serrano, Enrique
Serrano, Enrique in OpenAIREMoreno, Ana;
Moreno, Ana
Moreno, Ana in OpenAIRELópez-Moreno, Juan Ignacio;
López-Moreno, Juan Ignacio
López-Moreno, Juan Ignacio in OpenAIRERevuelto, Jesús;
Revuelto, Jesús
Revuelto, Jesús in OpenAIREThe Aneto Glacier, is the largest glacier in the Pyrenees. Its shrinkage and wastage have been continuous in recent decades, and there are signs of accelerated melting in recent years. In this study, changes in the surface and ice thickness of the Aneto Glacier from 1981 to 2022 are investigated using historical aerial imagery, airborne LiDAR point clouds, and UAV imagery. A GPR survey conducted in 2020, combined with data from photogrammetric analyses, allowed us to reconstruct the current ice thickness and also the existing ice distribution in 1981 and 2011. Over the last 41 years, the total glaciated area has shrunk by 64.7% and the ice thickness has decreased, on average, by 30.5 m. The mean remaining ice thickness in autumn 2022 was 11.9 m, as against the mean thicknesses of 32.9 m, 19.2 m reconstructed for 1981 and 2011 and 15.0 m observed in 2020 respectively. The results demonstrate the critical situation of the glacier, with an imminent segmentation into two smaller ice bodies and no evidence of an accumulation zone. We also found that the occurrence of an extremely hot and dry year, as observed in the 2021–2022 season, leads to a drastic degradation of the glacier, posing a high risk to the persistence of the Aneto Glacier, a situation that could extend to the rest of the Pyrenean glaciers in a relatively short time.
ZENODO arrow_drop_down Recolector de Ciencia Abierta, RECOLECTADataset . 2022 . Peer-reviewedData sources: Recolector de Ciencia Abierta, RECOLECTAadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
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more_vert ZENODO arrow_drop_down Recolector de Ciencia Abierta, RECOLECTADataset . 2022 . Peer-reviewedData sources: Recolector de Ciencia Abierta, RECOLECTAadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.euResearch data keyboard_double_arrow_right Dataset 2023Embargo end date: 09 Mar 2023Publisher:Dryad Authors:Wolfe, Kennedy David;
Desbiens, Amelia; Mumby, Peter;Wolfe, Kennedy David
Wolfe, Kennedy David in OpenAIREPatterns of movement of marine species can reflect strategies of reproduction and dispersal, species’ interactions, trophodynamics, and susceptibility to change, and thus critically inform how we manage populations and ecosystems. On coral reefs, the density and diversity of metazoan taxa is greatest in dead coral and rubble, which is suggested to fuel food webs from the bottom-up. Yet, biomass and secondary productivity in rubble is predominantly available in some of the smallest individuals, limiting how accessible this energy is to higher trophic levels. We address the bioavailability of motile coral reef cryptofauna based on small-scale patterns of emigration in rubble. We deployed modified RUbble Biodiversity Samplers (RUBS) and emergence traps in a shallow rubble patch at Heron Island, Great Barrier Reef, to detect community-level differences in the directional influx of motile cryptofauna under five habitat accessibility regimes. The mean density (0.13–4.5 ind.cm-3) and biomass (0.14–5.2 mg.cm-3) of cryptofauna were high and varied depending on microhabitat accessibility. Emergent zooplankton represented a distinct community (dominated by the Appendicularia and Calanoida) with the lowest density and biomass, indicating constraints on nocturnal resource availability. Mean cryptofauna density and biomass were greatest when interstitial access within rubble was blocked, driven by the rapid proliferation of small harpacticoid copepods from the rubble surface, leading to trophic simplification. Individuals with high biomass (e.g., decapods, gobies, and echinoderms) were greatest when interstitial access within rubble was unrestricted. Treatments with a closed rubble surface did not differ from those completely open, suggesting that top-down predation does not diminish rubble-derived resources. Our results show that conspecific cues and species’ interactions (e.g., competition and predation) within rubble are most critical in shaping ecological outcomes within the cryptobiome. These findings have implications for prey accessibility through trophic and community size structuring in rubble, which may become increasingly relevant as benthic reef complexity shifts in the Anthropocene. We address the bioavailability of coral reef cryptofauna in rubble based on small-scale patterns of emigration. We adapted the accessibility of Rubble Biodiversity Samplers (RUBS), models used to standardise biodiversity sampling in rubble (Wolfe and Mumby 2020), to explore the local movement patterns of rubble-dwelling fauna, with inference to predation processes within and beyond the cryptobenthos. Five treatments were developed to detect community-level differences in the directional influx of motile cryptofauna under various habitat accessibility regimes. Four of these treatments were developed by modifying accessibility into RUBS (https://www.thingiverse.com/thing:4176644/files) to understand limitations on the directional influx and movement of cryptofauna within coral rubble patches using four treatments; (1) open (completely accessible), (2) interstitial access (top closed), (3) surficial access (sides and bottom closed), and (4) raised (above rubble substratum). The fifth treatment involved a series of emergence plankton traps, designed to target demersal cryptofauna that vertically migrate from within the rubble benthos at night, given emergent zooplankton biomass and diversity are greatest at night. Fieldwork was conducted over several weeks (11th September to 5th October 2021) in a shallow (~3–5 m depth) reef slope site on the southern margin of Heron Island (-23˚26.845’ S, 151˚54.732’ E), Great Barrier Reef, Australia (Fig. 1). All collections were conducted under the Great Barrier Reef Marine Park Authority permit G20/44613.1.
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You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://beta.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.5061/dryad.0k6djhb4k&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.euResearch data keyboard_double_arrow_right Dataset 2019Publisher:Zenodo Funded by:EC | HIT2GAPEC| HIT2GAPAuthors: Massana i Raurich, Joaquim; Pous, Carles; Burgas i Nadal, Llorenç; Melendez, Joaquim; +1 AuthorsMassana i Raurich, Joaquim; Pous, Carles; Burgas i Nadal, Llorenç; Melendez, Joaquim; Colomer, Joan;This dataset supplements the journal paper: "Short-term load forecasting for non-residential buildings contrasting artificial occupancy attributes". Authors: J. Massana, C. Pous et al. Journal: Energy and Buildings, 2015, vol. 130, p. 519-531. The paper is accessible in the below link: https://doi.org/10.1016/j.enbuild.2016.08.081 Description: Each excel file contains hourly data of one building located at the Campus of Unviersity of Gironal. Data were collected from 2011 to 2014. Column information for the excel files: - Hora: hour of the day (0, 1... 23). - Dia: day of the month (1, 2... 31). - Mes: month (1,2... 12) - Any: year (2011... 2014). - Dia_set: day of the week (1,2... 7). - Temp: Outdoor temperature (oC). - Perfil_dia: daily profile (school day, non-school day, examination day, school-leaving examination day, August day, holiday and weekend day and, finally, Easter and Christmas holiday). - Indicador X.X: occupancy indicators, as described in the paper. - Cons: electrical consumption (kWh)
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You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.euResearch data keyboard_double_arrow_right Dataset 2019Publisher:Zenodo Funded by:EC | IRPWINDEC| IRPWINDAuthors: Raymundo E. Torres-Olguin;These are the raw data generated in the 2do Joint Experiments sponsored by IRP Wind EU project
add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
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more_vert add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.euResearch data keyboard_double_arrow_right Dataset 2020Embargo end date: 30 Nov 2023Publisher:Zenodo Funded by:EC | HyCAREEC| HyCAREAuthors:Erika Michela Dematteis;
David Michael Dreistadt;Erika Michela Dematteis
Erika Michela Dematteis in OpenAIREGiovanni Capurso;
Giovanni Capurso
Giovanni Capurso in OpenAIREJulian Jepsen;
+2 AuthorsJulian Jepsen
Julian Jepsen in OpenAIREErika Michela Dematteis;
David Michael Dreistadt;Erika Michela Dematteis
Erika Michela Dematteis in OpenAIREGiovanni Capurso;
Giovanni Capurso
Giovanni Capurso in OpenAIREJulian Jepsen;
Julian Jepsen
Julian Jepsen in OpenAIREFermin Cuevas;
Fermin Cuevas
Fermin Cuevas in OpenAIREMichel Latroche;
Michel Latroche
Michel Latroche in OpenAIREData type: Experimental measurements, correlations and Van't Hoff plot. Date format: .opj. Origin of the data: Experimental pressure composition isotherm measurements. Data generated by a home-made Sieverts’ type apparatus from CNRS, ICMPE, Thiais, France. Software needed to plot the data: Origin.
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For further information contact us at helpdesk@openaire.eu1 citations 1 popularity Average influence Average impulse Average Powered by BIP!
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For further information contact us at helpdesk@openaire.euResearch data keyboard_double_arrow_right Dataset 2020Publisher:Zenodo Funded by:EC | PARACATEC| PARACATAuthors:Gadde, Karthik;
Gadde, Karthik
Gadde, Karthik in OpenAIREMampuys, Pieter;
Mampuys, Pieter
Mampuys, Pieter in OpenAIREGuidetti, Andrea;
H. Y. Vincent Ching; +4 AuthorsGuidetti, Andrea
Guidetti, Andrea in OpenAIREGadde, Karthik;
Gadde, Karthik
Gadde, Karthik in OpenAIREMampuys, Pieter;
Mampuys, Pieter
Mampuys, Pieter in OpenAIREGuidetti, Andrea;
H. Y. Vincent Ching;Guidetti, Andrea
Guidetti, Andrea in OpenAIREHerrebout, Wouter A.;
Doorslaer, Sabine Van; Kourosch Abbaspour Tehrani; Maes, Bert U. W.;Herrebout, Wouter A.
Herrebout, Wouter A. in OpenAIREOrigin of the data: Experimental spectroscopic measurements Data Type: experimental measurements, open access supporting information The data are in CSV, DSW and FBSW format. Supporting information are supplied in PDF format. Data generated by instruments: Varian Cary 5E-UV-Vis-NIR spectrophotometer for UV-Vis measurements, Varian Cary Eclipse fluorescence spectrophotomer for fluorescence quenching measurements. Analytical and procedural information: Stern-Volmer fluorescence quenching experiments, UV-Vis measurements and Fluorescent Quantum Yield determination via ferrioxalate actinometry. Definition of variables: Wavelength, Absorbance, Concentration Units of measurement: nanometers (nm), moles-per-litre (mol/l) Abbreviations: File names and data headers use the following abbreviations: FQY refers to Fluorescence Quantum Yield determination experiments Light refers to irradiated samples in the actinometry experiment, as detailed in the procedure in the supporting information. Dark refers to non-irradiated samples in the actinometry experiment, as detailed in the procedure in the supporting information. SVQuench refers to Stern-Volmer quenching experiments RAxx refer to measurements related to allylbenzene. Xx is the amount of quencher in mol/l (05 should be intended as 0.5 mol/l and so on). RTxx refer to measurements related to S-(4-methylphenyl) 4-methylbenzenethiosulfonate. Xx is the amount of quencher in mol/l as above. RExx refer to measurements related to 1,2-dimethoxy-4-(prop-2-en-1-yl)benzene. Xx is the amount of quencher in mol/l as above. RSxx refer to measurements related to styrene. Xx is the amount of quencher in mol/l. RTFxx refer to measurements related to S-(4-fluorophenyl) 4-fluorobenzenethiosulfonate. Xx is the amount of quencher in mol/l as above. MesAcrMe Xx refers to data related to catalyst 9-mesityl-10-methylacridinium. Xx is the amount of catalyst in mol/l as above. DMC for measurements employing dimethylcarbonate as solvent. ACN for measurements employing acetonitrile as solvent. FBSW and DSW data are used by the proprietary software of the Varian spectrometers (CARY WinUV and Cary Eclipse). Information can be found at https://www.agilent.com/en/product/molecular-spectroscopy/uv-vis-uv-vis-nir-spectroscopy/uv-vis-uv-vis-nir-software/cary-winuv-software and https://www.agilent.com/en/product/molecular-spectroscopy/fluorescence-spectroscopy/fluorescence-software/cary-eclipse-software
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You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.eu1 citations 1 popularity Average influence Average impulse Average Powered by BIP!
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For further information contact us at helpdesk@openaire.euResearch data keyboard_double_arrow_right Dataset 2024Embargo end date: 01 May 2024Publisher:Zenodo This file contains the AiNU data used for the article entitled by Physics-based material parameters extraction from perovskite experiments via Bayesian optimization (https://arxiv.org/abs/2402.11101).
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You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.eu1 citations 1 popularity Average influence Average impulse Average Powered by BIP!
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You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.euResearch data keyboard_double_arrow_right Dataset 2023Embargo end date: 09 Oct 2023Publisher:Dryad Authors:García-Barros, Enrique;
Álamo, Mario; Romo, Helena;García-Barros, Enrique
García-Barros, Enrique in OpenAIRE# sRGB Reflectances from Iberian butterflies [https://doi.org/10.5061/dryad.1g1jwsv0q](https://doi.org/10.5061/dryad.1g1jwsv0q) Data on wing reflectance (visible spectrum, mean standard RGB values (243.7= white, to 52= black) from 224 species of butterflies (Lepidoptera, Papilionoidea): 223 from the Iberian Peninsula and one (*C. webbianus*) from the Canaries. Average of male and female, sample size as indicated in column n. The data from *C. webbianus* and *C. marshalli* were not included in our analyses of reflectance. Text file, CSV format, columns delimited by periods, 225 rows (including headings) and 38 columns. Any means presented are weighted averages taking into account the areas of the parts involved. Wing reflectances refer to the parts of the wings exposed in a living butterfly (except FW\_AREA and HW\_AREA which are total wing surfaces). * **Ord**, row number (roughly a taxonomic arrangement) * **Species**, species name (abbreviated genus, contains a blank space, e.g., *Heteropterus morpheus*) * **N**, sample size * **FWL**, forewing length (mm) * **DFT**, reflectance, dorsal forewing * **DFp**, reflectance, dorsal forewing, proximal area * **DFd**, reflectance, dorsal forewing, distal area * **DHT**, reflectance, dorsal hindwing * **DHp**, reflectance, dorsal hindwing, proximal area * **DHd**, reflectance, dorsal hindwing, distal area * **DB**, reflectance, dorsal body area * **D(Tp+B)**, reflectance of the exposed dorsal body plus proximal wing surfaces * **DT**, reflectance of the dorsal areas (body plus whole wing) * **DTp**, reflectance of the dorsal, proximal wing areas * **DTd**, reflectance of the dorsal, distal wing areas * **VFT**, reflectance, ventral forewing * **VFp**, reflectance, ventral forewing, proximal area * **VFd**, reflectance, ventral forewing, distal area * **VHT**, reflectance, ventral hindwing * **VHp**, reflectance, ventral hindwing, proximal area * **VHd**, reflectance, ventral hindwing, distal area * **VB**, reflectance, ventral body area * **V(Tp+B)**, reflectance of the exposed ventral body plus proximal wing surfaces * **VT**, reflectance of the ventral areas (body plus whole wing) * **VTp**, reflectance of the ventral, proximal wing areas * **VTd**, reflectance of the ventral, distal wing areas * **Mean**, mean total reflectance (dorsal and ventral surfaces) * **p\_Mean**, mean reflectance of the proximal (dorsal and ventral) wing areas * **p\_Otimum**, mean reflectance of the proximal dorsal (for dorsal baskers) or ventral (for lateral basking species) wing areas. * **FW\_area**, total forewing area (mm2) * **HW\_area**, total hindwing area (mm2) * **T\_Mean\_Iberia\_10km**, Iberian mean species temperature, Centigrade degrees, 10 x 10 km resolution * **P\_Mean\_Iberia\_10km**, mean species annual precipitation, mm, Iberian Peninsula, 10 x 10 km resolution * **T\_Mean\_Ibera\_50km**, mean species temperature, Centigrade degrees, Iberian Peninsula, 50 x 50 km resolution * **P\_Mean\_Iberia\_50km**, mean species annual precipitation, mm, Iberian Peninsula, 50 x 50 km resolution Data on wing reflectance (visible spectrum, mean standard RGB values (243.7= white, to 52= black) from 224 species of butterflies (Lepidoptera, Papilionoidea): 223 from the Iberian Peninsula and one (Cyclyrius webbianus) from the Canary Islands. Average of male and female, sample size as indicated in column n. The data from C. webbianus and Cacyreus marshalli are provided although these species were not included in our analyses of reflectance. The data were measured from digital images of set (collection) specimens taken in fixed conditions, with grey (average RGB) values standardized a posteriori to fit the scale white= 243.7= white, to black= 52. The data set includes the mean length of the forewing (mm) and the total areas (mm2) of the fore and hind wings.
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For further information contact us at helpdesk@openaire.eu0 citations 0 popularity Average influence Average impulse Average Powered by BIP!
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