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[grants JP19K12301 and JP17H06323]. The surface velocity data were produced by SSALTO/ DUACS and distributed by Aviso+, with support from Cnes (http:// www.aviso.altimetry.fr/duacs/). The altimetry sea ice thickness data used in this study (doi 10.6096/CTOH_SEAICE_2019_12) wer
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p?project_id=430 Recent Publication Baughman, C.A., Loehman, R.A., Saperstein, L., Magnes, D., and Sherriff, R., 2020, Land cover estimates for the Kenai Penin sula lowlands;1973, 2002, and 2017: U.S. Geological Survey data release, https://doi.org/10.5066/P92BGHW1. 62
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/dl_based_prognosis. Data availability Three out of four cohorts used in this study can be found on The Cancer Imaging Archive (TCIA)24: Canadian benchmark dataset23: https://doi.org/10.7937/K9/TCIA.2017.8oje5q00. MAASTRO dataset30: https://doi.org/10. 7937/tcia.2019.8kap372n. PM
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n be accessed via the AEROCLO-sA database at https://doi.org/10.6096/AEROCLO.1754 (Perrin and Richard, 2018) and now have DOIs. The LNG lidar data DOI is https://doi.org/10.6096/AEROCLO.1774 (Flamant, 2018). The dropsonde data DOI is https://doi.org/10.6096/AEROCLO.1777 (Per
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T-2015-0007.1 Conrad, J. E., and Rudebusch, J. A. (2023). Methane seeps derived from water- column acoustic backscatter data collected along Cascadia margin offshore Oregon and Northern California, 2018-2021. U.S. Geological Survey Data Release. doi:10.5066/ P9TW2X7Y Cru
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. Journal of Oceanography, 71(6), 637661. https://doi.org/10.1007/s1087201503064 Key, R. M. , Olsen, A. , van Heuven, S. , Lauvset, S. K. , Velo, A. , Lin, X. , et al. (2015): Global Ocean Data Analysis Project, Version 2 (GLODAPv2), https://doi.org/10.3334/CDIAC/OTG.NDP093_GLODAPv2 Khid
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paleocurrent directions where direct evidence is otherwise scarce. Data Availability Statement All data used for this publication can be accessed through the public domain Data Repository for the Uni- versity of Minnesota (DRUM) (at https://doi.org/10.13020/jjdx-1m95). Re
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t-science_center_objects Recent Publications Avdievitch, N., Schmitt, R.G., Coe, J.A., 2020, Inventory map of submarine landslides in Glacier Bay, Glacier Bay National Park and Preserve, Alaska: U.S. Geological Survey data release, https://doi.org/10.5066/P9GCDYT2. Bes
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7/peerj.12422 16/20 Capreolus capreolus: https://doi.org/10.15468/dl.wp98ts (28 May 2021), Cervus elaphus: https://doi.org/10.15468/dl.72ddmz (28 May 2021), Ciconia ciconia: https://doi.org/10.15468/dl.k6jv69 (28 May 2021), Soricidae https://doi.org/10.15468/dl.czyyq2 (01
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OBS v23.1 are available for down- load following this URL: https://surfobs.climate.copernicus.eu/ dataaccess/access_eobs_months.php (Cornes et al., 2018). The Remote sensing MODIS (MOD10A1F) dataset is available fol- lowing this DOI: https://doi.org/10.5067/MODIS/MOD10A1F.061 (Hal
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icolas, J., Peubey, C., Radu, R., Rozum, I., Schepers, D., Simmons, A., Soci, C., Dee, D., and Thpaut, J.-N.: ERA5 hourly data on single levels from 1979 to present, Coper- nicus Climate Change Service (C3S) Climate Data Store (CDS), https://doi.org/10.24381/cds.adbb2d47, 201
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sing, reading the different data sources, statistical analyses and making figures. For the snow depth in situ observation availability, please refer to this article: https://doi.org/10.5194/tc-15-1343-2021 (Matiu et al., 2021a) (DOI: https://doi.org/10.5281/zenodo.5109574, Mat
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w.bas.ac. uk/project/krillbase/). KRILLBASE length frequency data are available from the British Antarctic Survey by request (contact: Simeon Hill, [email protected]), and the Palmer LTER length frequency data are avail able online (https://doi.org/10.6073/pasta/be42bb841e696b7bca d9957aed33db5e). O
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, P.-G., Bentsen, M., Guo, C., Tjiputra, J., Kirkevg, A., Olivi, D. J. L., Seland, ., Fan, Y., Lawrence, P., Eldevik, T., and Keenlyside, N.: NCC NorCPM1 model output prepared for CMIP6 CMIP, Earth System Grid Fed- eration [dataset], https://doi.org/10.22033/ESGF/CMIP6.10843, 201
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0915c6. The authors did not download the data to distribute them. The results contain modi- fied Copernicus Climate Change Service information 2020. Ice wa- ter path data were taken from the MODIS MYD06_L2 product with the identifier https://doi.org/10.5067/MODIS/MYD06_L2.006 (Pla
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en we used nhm- mer (Wheeler and Eddy 2013) to search each genome. We downloaded the Jarvis et al. (2014) UCE alignments from http://gigadb.org/dataset/101041 and the Edwards et al. (2017) CNEE alignments from https://datadryad. org/resource/doi:10.5061/dryad.25f7g. The
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sed by anyone for any lawful purpose. The work is made available under the Creative Commons CC0 public domain dedication. Data Availability Statement: All data used in support of this manuscript are publicly available through USGS at https://doi.org/10.5066/ F72J69RM. Fu
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n, D. T., Nelkin, E. J., and Jackson, T.: GPM IMERG Final Precipitation L3 1 day 0.1 degree 0.1 degree V06, edited by: Savtchenko, A., Greenbelt, MD, Goddard Earth Sciences Data and Information Services Center (GES DISC) [data set], https://doi.org/10.5067/GPM/IMERGDF/DAY/06, 201
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020) hindcast simula- tions can be downloaded from the ESGF website (https:// esgf-node.ipsl.upmc.fr/projects/esgf-ipsl/, last access: 1 Febru- ary 2023). The ERA5 dataset is available on the Copernicus Data Store following this DOI: https://doi.org/10.24381/cds.adbb2d47 (Her
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ects=0#qt-science_center_objects Recent Publications Herman-Mercer, N.M., Loehman, R.A., Toohey, R.C., and Paniyak, C., 2019, Yukon-Kuskokwim Delta berry outlookResults from local expert surveys: U.S. Geological Survey data release, https://doi.org/10.5066/P9HDXE32. Her
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and techniques. American Fisheries Society, Bethesda, Maryland. Long, J. M., and P. M. Kocovsky. 2022. Daily ages of young-of-year Silver Chub from western Lake Erie, 2017-2018: U.S. Geological Survey data release. Available: https://doi.org/10.5066/ P90A4UGJ. Lo
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ly those drugs that are selective and known to 721 have relevance in various forms of cancer are considered here. 722 In addition to DrugBank searches, we also conducted exhaustive searches in ChEMBL 723 (Gaulton et al., 2017) (http://doi.org/10.6019/CHEMBL.database.23) to
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software package is available at https://doi.org/10.5281/zenodo.3733448 (Delene et al., 2020). Data availability. All ORACLES data are accessible via the digi- tal object identifiers provided under ORACLES Science Team refer- ences: https://doi.org/10.5067/Suborbital/ORACLES/P3/2018_V2 (ORA
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eir support and welcome. This work was made possible thanks to: the MALIS 1 and MALIS 2 oceano- graphic cruises in Raroia Atoll (https://doi.org/10.17600/18000582, Andrfout, 2018), and the MALIS 3 cruise in Apataki and Takaroa Atoll (https://doi.org/10.17600/18001644, And
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