BUSCADOR RECOLECTA

We provide the DSM and DTm files as geotiffs for ease of use. DSM_winter_3cm_NORTH.tif DSM_summer_3cm_NORTH.tif DTM_winter_3cm_NORTH.tif DTM_summer_3cm_NORTH.tif DSM_winter_3cm_SOUTH.tif DSM_summer_3cm_SOUTH.tif DTM_winter_3cm_SOUTH.tif DTM_summer_3cm_SOUTH.tif The filenames are split into 4 parts: XXX_yyy_zzz_www.tif XXX = Either DSM or DTM. For summer images, DSM corresponds to the surface elevation including vegetation and DTM to the surface elevation with the vegetation cover removed. For winter images, DSM corresponds to the elevation of the snow surface and vegetation sticking out of the snowpack, and DTM to the elevation of the snowpack with the vegetation ignored. yyy = Either summer or winter. Summer corresponds to the snow-free acquisitions on the 28-29 September 2017. Winter denotes the snow-covered acquisitions acquired on 25-26 April 2018. zzz = 3cm. The spatial resolution of the dataset. WWW = Either SOUTH or NORTH. Indicates which site the survey was performed over. The data are projected in EPSG: 2951 (NAD83(CSRS) / MTM zone 9)., We performed high-resolution snow height measurements using drone-based lidar over two 0.5 km long areas near the community of Umiujaq, in Tasiapik valley. The North site is centered around (N:56.5684°; W:76.4895°, elevation 122 m) and the South site around (N:56.5594°; W:76.4816°, elevation 133 m). A snow-free survey was performed on 28-29 September 2017 and a snow survey on 25-26 April 2018. We produced 3 cm digital terrain and digital surface models (DTM and DSM) from the lidar cloud points for each site for both lidar campaigns., French Polar Institute of Research and Technology, Plouzané (IFRTP), grant/award no. 2014-4284: IPEV grant 1042, Institut Polaire Français Paul Émile Victor (IPEV), grant/award no. 1042: ESCAPE-Arctic 3, Natural Sciences and Engineering Research Council (NSERC), grant/award no. 2018-03941: NSERC discovery grant, Peer reviewed

1. Modern Lake hydrogeology and geological settin.-- 2. Sediment core and age model.--3. Stable isotope data.-- 4. Calculations of saturation of gypsum saturation index, estimated water levels and salinities.-- 5. Lake Zóñar hydrological balance under spring diversion and drier conditions.-- 6. Isotope Model Parametrization.-- 7.7 Archaeological observations., Peer reviewed

PDF file contains: Supplementary material Table S1 and Figures S1-S9. © Author(s) 2023. CC BY 4.0 License. The copyright of individual parts of the supplement might differ from the article licence, Peer reviewed

Supplementary tables S1-S6 and figures S1-S5., Peer reviewed

This dataset contains estimates of Live Fuel Moisture Content (LFMC) in the Western United States. LFMC is the percentage of vegetation water mass over the dry biomass of the plants. Here, LFMC is retrieved by isolating the water component of the passive microwaves vegetation optical depth (VOD) signal at three frequencies: L-band (1.4 GHz), X-band (10.65 GHz) and Ku-band (18.7 GHz). Each frequency represents a different canopy sensing depth. To isolate LFMC from VOD, auxiliary information to account for the biomass and structure of the vegetation has been used: radar backscatter data from Sentinel-1 and canopy height data from GEDI/Sentinel-2. The dataset spans between April 2015 and December 2018 for L- and X-bands, and between April 2015 and July 2018 for Ku-band retrievals., Peer reviewed

The 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., Peer reviewed

PDF file contains: Supplementary Text; Supplementary Figures S1-S5; Supplementary Table S1., Peer reviewed

Dataset of the scientific article "Nestling sex and behaviour determine the host preference of insect vectors in avian nests"., Peer reviewed

Figure S1 - spectrum.02623-23-s0001.docx Observed viable counts of Hp ATCC 700392 following exposure to the Hp-fld inhibitor compound IV at four times the MIC., Peer reviewed

[Description of methods used for collection/generation of data] Meteorological and limnological methodologies., This dataset compiles meteorological and limnological variables recorded by the author in Las Madres lake and its environment in 1991-2021., Peer reviewed