cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.6073/pasta/231fce6ed9630cc4fac6e8b95688a7ef
title: Kuparuk River 2011 summer temperature and discharge calculated from stage height.

description: This file is out of date has been combined in a multi-year file. See: Bowden, W. 2020. Kuparuk River stream temperature and discharge measured each summer, Dalton Road crossing, Arctic LTER Toolik Field Staion, Alaska 1978-2019 Environmental Data Initiative. http://dx.doi.org/10.6073/pasta/b407edbe788d9be27662009e1be8331b Water temperature and stream discharge were determined for the Kuparuk River. In many years, temperature and stream height were recorded manually each day. In recent years, dataloggers have measured stream temperature and stream height at regular intervals. A rating curve was developed to calculate continuous discharge from stage height. Temperature was also measured on an hourly basis. Stage height was measured on the Kuparuk about 1 km above the Dalton Highway crossing.
DOI: 10.6073/pasta/d6e12afa5600d9f0082f96b95158b1b0
title: Kuparuk River 2000 summer temperature and discharge calculated from stage height.

description: This file is out of date has been combined in a multi-year file. See: Bowden, W. 2020. Kuparuk River stream temperature and discharge measured each summer, Dalton Road crossing, Arctic LTER Toolik Field Staion, Alaska 1978-2019 Environmental Data Initiative. http://dx.doi.org/10.6073/pasta/b407edbe788d9be27662009e1be8331b Stream temperature and discharge Each summer, water temperature and stream discharge are determined for the Kuparuk River. In many years, temperature and stream height were recorded manually each day. In recent years, data loggers have measured stream temperature and stream height at regular intervals. The Kuparuk River data is maintained by Dough Kane on the Water and Environmental Research Center at UAF (http://www.uaf.edu/water/projects/NorthSlope/upper_kuparuk/uk_river/uk_r...) Stream height is converted into stream discharge based on a rating curve calculated from manual discharge measurements throughout the season. The principal investigator in charge of the temperature and discharge measurements is Dr. Breck Bowden.
DOI: 10.6073/pasta/73e260adeaba19e031b2b9bde7317f6f
title: Kuparuk River 2001 summer temperature and discharge calculated from stage height.

description: This file is out of date has been combined in a multi-year file. See: Bowden, W. 2020. Kuparuk River stream temperature and discharge measured each summer, Dalton Road crossing, Arctic LTER Toolik Field Staion, Alaska 1978-2019 Environmental Data Initiative. http://dx.doi.org/10.6073/pasta/b407edbe788d9be27662009e1be8331b Stream temperature and discharge for the Kuparuk river in 2001. Each summer, water temperature and stream discharge are determined for the Kuparuk River. In recent years, dataloggers have measured stream temperature and stream height at regular intervals. The Kuparuk River data is maintained by Doug Kane on the Water and Environmental Research Center at UAF (http://www.uaf.edu/water/projects/NorthSlope/upper_kuparuk/uk_river/uk_r...) Stream height is converted into stream discharge based on a rating curve calculated from manual discharge measurements throughout the season. The principal investigator in charge of the temperature and discharge measurements is Dr. Breck Bowden.
DOI: 10.6073/pasta/7eccde622103beefdfdaea11a1f85c95
title: Kuparuk River 2002 summer temperature and discharge calculated from stage height.

description: This file is out of date has been combined in a multi-year file. See: Bowden, W. 2020. Kuparuk River stream temperature and discharge measured each summer, Dalton Road crossing, Arctic LTER Toolik Field Staion, Alaska 1978-2019 Environmental Data Initiative. http://dx.doi.org/10.6073/pasta/b407edbe788d9be27662009e1be8331b Stream temperature and discharge for the Kuparuk River in 2002. Each summer, water temperature and stream discharge are determined for the Kuparuk River. In many years, temperature and stream height were recorded manually each day. In recent years, dataloggers have measured stream temperature and stream height at regular intervals. The Kuparuk River data is maintained by Dough Kane on the Water and Environmental Research Center at UAF (http://www.uaf.edu/water/projects/NorthSlope/upper_kuparuk/uk_river/uk_r...) Stream height is converted into stream discharge based on a rating curve calculated from manual discharge measurements throughout the season. The principal investigator in charge of the temperature and discharge measurements is Dr. Breck Bowden.
DOI: 10.6073/pasta/4580d08c26a2cbbfcfa3778cbeaab4f3
title: Kuparuk River 1987 summer discharge calculated from stage height.

description: This file is out of date has been combined in a multi-year file. See: Bowden, W. 2020. Kuparuk River stream temperature and discharge measured each summer, Dalton Road crossing, Arctic LTER Toolik Field Staion, Alaska 1978-2019 Environmental Data Initiative. http://dx.doi.org/10.6073/pasta/b407edbe788d9be27662009e1be8331b Stream temperature and discharge each summer, water temperature and stream discharge are determined for the Kuparuk River. In many years, temperature and stream height were recorded manually each day. In recent years, data loggers have measured stream temperature and stream height at regular intervals. The Kuparuk River data is maintained by Dough Kane on the Water and Environmental Research Center at UAF (http://www.uaf.edu/water/projects/NorthSlope/upper_kuparuk/uk_river/uk_r...) Stream height is converted into stream discharge based on a rating curve calculated from manual discharge measurements throughout the season. The principal investigator in charge of the temperature and discharge measurements is Dr. Breck Bowden.
DOI: 10.6073/pasta/c030bc5ee47659a6d17f850e90ff5cb7
title: Kuparuk River 1988 summer temperature and discharge calculated from stage height.

description: This file is out of date has been combined in a multi-year file. See: Bowden, W. 2020. Kuparuk River stream temperature and discharge measured each summer, Dalton Road crossing, Arctic LTER Toolik Field Staion, Alaska 1978-2019 Environmental Data Initiative. http://dx.doi.org/10.6073/pasta/b407edbe788d9be27662009e1be8331b Stream temperature and discharge each summer, water temperature and stream discharge are determined for the Kuparuk River. In many years, temperature and stream height were recorded manually each day. In recent years, data loggers have measured stream temperature and stream height at regular intervals. The Kuparuk River data is maintained by Dough Kane on the Water and Environmental Research Center at UAF (http://www.uaf.edu/water/projects/NorthSlope/upper_kuparuk/uk_river/uk_r...) Stream height is converted into stream discharge based on a rating curve calculated from manual discharge measurements throughout the season. The principal investigator in charge of the temperature and discharge measurements is Dr. Breck Bowden.
DOI: 10.6073/pasta/e5eb8b9f1018672611eed2d6b89461b9
title: Kuparuk River 1989 summer temperature and discharge calculated from stage height.

description: This file is out of date has been combined in a multi-year file. See: Bowden, W. 2020. Kuparuk River stream temperature and discharge measured each summer, Dalton Road crossing, Arctic LTER Toolik Field Staion, Alaska 1978-2019 Environmental Data Initiative. http://dx.doi.org/10.6073/pasta/b407edbe788d9be27662009e1be8331b Stream temperature and discharge each summer, water temperature and stream discharge are determined for the Kuparuk River. In many years, temperature and stream height were recorded manually each day. In recent years, data loggers have measured stream temperature and stream height at regular intervals. The Kuparuk River data is maintained by Dough Kane on the Water and Environmental Research Center at UAF (http://www.uaf.edu/water/projects/NorthSlope/upper_kuparuk/uk_river/uk_r...) Stream height is converted into stream discharge based on a rating curve calculated from manual discharge measurements throughout the season. The principal investigator in charge of the temperature and discharge measurements is Dr. Breck Bowden.
DOI: 10.26300/84eh-g517
title: Project: Screening for Hypertension in Children and Adolescents: Systematic Review for the U.S. Preventive Services Task Force
DOI: 10.6073/pasta/4548854f007214060d5aea218e42f480
title: Kuparuk River 1990 summer temperature and discharge calculated from stage height.

description: This file is out of date has been combined in a multi-year file. See: Bowden, W. 2020. Kuparuk River stream temperature and discharge measured each summer, Dalton Road crossing, Arctic LTER Toolik Field Staion, Alaska 1978-2019 Environmental Data Initiative. http://dx.doi.org/10.6073/pasta/b407edbe788d9be27662009e1be8331b Stream temperature and discharge each summer, water temperature and stream discharge are determined for the Kuparuk River. In many years, temperature and stream height were recorded manually each day. In recent years, data loggers have measured stream temperature and stream height at regular intervals. The Kuparuk River data is maintained by Dough Kane on the Water and Environmental Research Center at UAF (http://www.uaf.edu/water/projects/NorthSlope/upper_kuparuk/uk_river/uk_r...) Stream height is converted into stream discharge based on a rating curve calculated from manual discharge measurements throughout the season. The principal investigator in charge of the temperature and discharge measurements is Dr. Breck Bowden.
DOI: 10.6073/pasta/48cf755e0f85bcf93ffce7bb0ad42acb
title: Kuparuk River 1991 summer temperature and discharge calculated from stage height.

description: This file is out of date has been combined in a multi-year file. See: Bowden, W. 2020. Kuparuk River stream temperature and discharge measured each summer, Dalton Road crossing, Arctic LTER Toolik Field Staion, Alaska 1978-2019 Environmental Data Initiative. http://dx.doi.org/10.6073/pasta/b407edbe788d9be27662009e1be8331b Stream temperature and discharge each summer, water temperature and stream discharge are determined for the Kuparuk River. In many years, temperature and stream height were recorded manually each day. In recent years, data loggers have measured stream temperature and stream height at regular intervals. The Kuparuk River data is maintained by Dough Kane on the Water and Environmental Research Center at UAF (http://www.uaf.edu/water/projects/NorthSlope/upper_kuparuk/uk_river/uk_r...) Stream height is converted into stream discharge based on a rating curve calculated from manual discharge measurements throughout the season. The principal investigator in charge of the temperature and discharge measurements is Dr. Breck Bowden.
DOI: 10.6073/pasta/d22fbd24966f07d930ec92f03ad7723a
title: Kuparuk River 1992 summer temperature and discharge calculated from stage height.

description: This file is out of date has been combined in a multi-year file. See: Bowden, W. 2020. Kuparuk River stream temperature and discharge measured each summer, Dalton Road crossing, Arctic LTER Toolik Field Staion, Alaska 1978-2019 Environmental Data Initiative. http://dx.doi.org/10.6073/pasta/b407edbe788d9be27662009e1be8331b Stream temperature and discharge each summer, water temperature and stream discharge are determined for the Kuparuk River. In many years, temperature and stream height were recorded manually each day. In recent years, data loggers have measured stream temperature and stream height at regular intervals. The Kuparuk River data is maintained by Dough Kane on the Water and Environmental Research Center at UAF (http://www.uaf.edu/water/projects/NorthSlope/upper_kuparuk/uk_river/uk_r...) Stream height is converted into stream discharge based on a rating curve calculated from manual discharge measurements throughout the season. The principal investigator in charge of the temperature and discharge measurements is Dr. Breck Bowden.
DOI: 10.6073/pasta/a523c13eac2314215707956485521ce7
title: Kuparuk River 1993 summer temperature and discharge calculated from stage height.

description: This file is out of date has been combined in a multi-year file. See: Bowden, W. 2020. Kuparuk River stream temperature and discharge measured each summer, Dalton Road crossing, Arctic LTER Toolik Field Staion, Alaska 1978-2019 Environmental Data Initiative. http://dx.doi.org/10.6073/pasta/b407edbe788d9be27662009e1be8331b Stream temperature and discharge Each summer, water temperature and stream discharge are determined for the Kuparuk River. In many years, temperature and stream height were recorded manually each day. In recent years, data loggers have measured stream temperature and stream height at regular intervals. The Kuparuk River data is maintained by Dough Kane on the Water and Environmental Research Center at UAF (http://www.uaf.edu/water/projects/NorthSlope/upper_kuparuk/uk_river/uk_r...) Stream height is converted into stream discharge based on a rating curve calculated from manual discharge measurements throughout the season. The principal investigator in charge of the temperature and discharge measurements is Dr. Breck Bowden.
DOI: 10.6073/pasta/ea32963d40ca039b249c0229fd05eff1
title: Kuparuk River 1994 summer temperature and discharge calculated from stage height.

description: This file is out of date has been combined in a multi-year file. See: Bowden, W. 2020. Kuparuk River stream temperature and discharge measured each summer, Dalton Road crossing, Arctic LTER Toolik Field Staion, Alaska 1978-2019 Environmental Data Initiative. http://dx.doi.org/10.6073/pasta/b407edbe788d9be27662009e1be8331b Stream temperature and discharge Each summer, water temperature and stream discharge are determined for the Kuparuk River. In many years, temperature and stream height were recorded manually each day. In recent years, data loggers have measured stream temperature and stream height at regular intervals. The Kuparuk River data is maintained by Dough Kane on the Water and Environmental Research Center at UAF (http://www.uaf.edu/water/projects/NorthSlope/upper_kuparuk/uk_river/uk_r...) Stream height is converted into stream discharge based on a rating curve calculated from manual discharge measurements throughout the season. The principal investigator in charge of the temperature and discharge measurements is Dr. Breck Bowden.
DOI: 10.5281/zenodo.5747627
title: Metrics of Social Curiosity: The WhatsApp Case

description: We provide a database file with the anonymized messages shared in WhatsApp.
DOI: 10.6073/pasta/d0565f834477acb5aa49fbdee577230d
title: Kuparuk River 1995 summer temperature and discharge calculated from stage height.

description: This file is out of date has been combined in a multi-year file. See: Bowden, W. 2020. Kuparuk River stream temperature and discharge measured each summer, Dalton Road crossing, Arctic LTER Toolik Field Staion, Alaska 1978-2019 Environmental Data Initiative. http://dx.doi.org/10.6073/pasta/b407edbe788d9be27662009e1be8331b Stream temperature and discharge Each summer, water temperature and stream discharge are determined for the Kuparuk River. In many years, temperature and stream height were recorded manually each day. In recent years, dataloggers have measured stream temperature and stream height at regular intervals. The Kuparuk River data is maintained by Dough Kane on the Water and Environmental Research Center at UAF (http://www.uaf.edu/water/projects/NorthSlope/upper_kuparuk/uk_river/uk_r...) Stream height is converted into stream discharge based on a rating curve calculated from manual discharge measurements throughout the season. The principal investigator in charge of the temperature and discharge measurements is Dr. Breck Bowden.
DOI: 10.6073/pasta/82104807a4f72c40e0ad4e4da4c8e453
title: Kuparuk River 1996 summer temperature and discharge calculated from stage height.

description: This file is out of date has been combined in a multi-year file. See: Bowden, W. 2020. Kuparuk River stream temperature and discharge measured each summer, Dalton Road crossing, Arctic LTER Toolik Field Staion, Alaska 1978-2019 Environmental Data Initiative. http://dx.doi.org/10.6073/pasta/b407edbe788d9be27662009e1be8331b Stream temperature and discharge Each summer, water temperature and stream discharge are determined for the Kuparuk River. In many years, temperature and stream height were recorded manually each day. In recent years, data loggers have measured stream temperature and stream height at regular intervals. The Kuparuk River data is maintained by Dough Kane on the Water and Environmental Research Center at UAF (http://www.uaf.edu/water/projects/NorthSlope/upper_kuparuk/uk_river/uk_r...) Stream height is converted into stream discharge based on a rating curve calculated from manual discharge measurements throughout the season. The principal investigator in charge of the temperature and discharge measurements is Dr. Breck Bowden.
DOI: 10.6073/pasta/6eca6669299b6b162d648c67036e690e
title: Kuparuk River 1997 summer temperature and discharge calculated from stage height.

description: This file is out of date has been combined in a multi-year file. See: Bowden, W. 2020. Kuparuk River stream temperature and discharge measured each summer, Dalton Road crossing, Arctic LTER Toolik Field Staion, Alaska 1978-2019 Environmental Data Initiative. http://dx.doi.org/10.6073/pasta/b407edbe788d9be27662009e1be8331b Stream temperature and discharge Each summer, water temperature and stream discharge are determined for the Kuparuk River. In many years, temperature and stream height were recorded manually each day. In recent years, data loggers have measured stream temperature and stream height at regular intervals. The Kuparuk River data is maintained by Dough Kane on the Water and Environmental Research Center at UAF (http://www.uaf.edu/water/projects/NorthSlope/upper_kuparuk/uk_river/uk_r...) Stream height is converted into stream discharge based on a rating curve calculated from manual discharge measurements throughout the season. The principal investigator in charge of the temperature and discharge measurements is Dr. Breck Bowden.
DOI: 10.6073/pasta/3de6efd6730e239cc8759d814e27515e
title: Kuparuk River 1998 summer discharge calculated from stage height.

description: This file is out of date has been combined in a multi-year file. See: Bowden, W. 2020. Kuparuk River stream temperature and discharge measured each summer, Dalton Road crossing, Arctic LTER Toolik Field Staion, Alaska 1978-2019 Environmental Data Initiative. http://dx.doi.org/10.6073/pasta/b407edbe788d9be27662009e1be8331b Discharge Each summer, water temperature and stream discharge are determined for the Kuparuk River. In many years, stream height were recorded manually each day. In recent years, data loggers have measured stream temperature and stream height at regular intervals. The Kuparuk River data is maintained by Dough Kane on the Water and Environmental Research Center at UAF (http://www.uaf.edu/water/projects/NorthSlope/upper_kuparuk/uk_river/uk_r...) Stream height is converted into stream discharge based on a rating curve calculated from manual discharge measurements throughout the season. The principal investigator in charge of the temperature and discharge measurements is Dr. Breck Bowden. 1998 had no temperature file.
DOI: 10.5281/zenodo.5744343
title: Greenkeeper Overhead - Online Appendix

description: Supplementary material for Greenkeeper Overhead paper, submitted to the Transaction on Software Engineering and Methodology (TOSEM) journal.
DOI: 10.5281/zenodo.5744342
title: Greenkeeper Overhead - Online Appendix

description: Supplementary material for Greenkeeper Overhead paper, submitted to the Transaction on Software Engineering and Methodology (TOSEM) journal.
DOI: 10.6073/pasta/29785b2fc1d108fe0961c49d34a7ad13
title: Kuparuk River 1999 summer temperature and discharge calculated from stage height.

description: This file is out of date has been combined in a multi-year file. See: Bowden, W. 2020. Kuparuk River stream temperature and discharge measured each summer, Dalton Road crossing, Arctic LTER Toolik Field Staion, Alaska 1978-2019 Environmental Data Initiative. http://dx.doi.org/10.6073/pasta/b407edbe788d9be27662009e1be8331b Stream temperature and discharge Each summer, water temperature and stream discharge are determined for the Kuparuk River. In many years, temperature and stream height were recorded manually each day. In recent years, data loggers have measured stream temperature and stream height at regular intervals. The Kuparuk River data is maintained by Dough Kane on the Water and Environmental Research Center at UAF (http://www.uaf.edu/water/projects/NorthSlope/upper_kuparuk/uk_river/uk_r...) Stream height is converted into stream discharge based on a rating curve calculated from manual discharge measurements throughout the season. The principal investigator in charge of the temperature and discharge measurements is Dr. Breck Bowden.
DOI: 10.25345/c5xk3w
title: MassIVE MSV000088483 - GNPS Endophitic Fungi from Atlantic Forest
title: The data includes secondary metrabolites from an endophitic fungi from the Atlantic forest in Brazil.
DOI: 10.6084/m9.figshare.17105324.v1
title: ICFstroke_Rasch_Mokken

description: 130 inpatients with stroke assessed via <i>International Classification of Functioning, Disability and Health</i> (ICF)
DOI: 10.5519/qd.bommxjgw
title: Query on the Natural History Museum Data Portal (data.nhm.ac.uk) (1 records)
DOI: 10.5519/qd.i5zvcd00
title: Query on the Natural History Museum Data Portal (data.nhm.ac.uk) (2200 records)
DOI: 10.25422/azu.data.17086889
title: Arctic Amplification Feedbacks in Siberia: case study of the Yenisei River Basin

description: The submission includes 1) tree-ring data and hydrological gauge data used in river discharge and water balance modeling, 2) Environmental Research Letters accepted manuscript and supplemental materials explaining and discussing the data.Abstract<br>The Yenisei River is the largest contributor of freshwater and energy fluxes among all rivers draining to the Arctic Ocean. Modeling long-term variability of Eurasian runoff to the Arctic Ocean is complicated by the considerable variability of river discharge in time and space, and the monitoring constraints imposed by a sparse gauged-flow network and paucity of satellite data. We quantify tree growth response to river discharge at the upper reaches of the Yenisei River in Tuva, South Siberia. Two regression models built from eight tree-ring width chronologies of <i>Larix sibirica </i>are applied to reconstruct winter (Nov–Apr) discharge for the period 1784-1997 (214 years), and annual (Oct–Sept) discharge for the period 1701–2000 (300 years). The Nov–Apr model explains 52% of the discharge variance whereas Oct–Sept explains 26% for the calibration intervals 1927–1997 and 1927-2000, respectively. This new hydrological archive doubles the length of the instrumental discharge record at the Kyzyl gauge and resets the temporal background of discharge variability back to 1784. The reconstruction finds a remarkable 80% upsurge in winter flow over the last 25 years, which is unprecedented in the last 214 years. In contrast, annual discharge fluctuated normally for this system, with only a 7% increase over the last 25 years. Water balance modeling with CRU data manifests a significant discrepancy between decadal variability of the gauged flow and climate data after 1960. We discuss the impact on the baseflow rate change of both the accelerating permafrost warming in the discontinuous zone of South Siberia and widespread forest fires. The winter discharge accounts for only one third of the annual flow, yet the persistent 25-year upsurge is alarming. This trend is likely caused by Arctic Amplification, which can be further magnified by increased winter flow delivering significantly more fresh water to the Kara Sea during the cold season.<br><br><i><br>For inquiries regarding the contents of this dataset, please contact the Corresponding Author listed in the README.txt file. Administrative inquiries (e.g., removal requests, trouble downloading, etc.) can be directed to data-management@arizona.edu</i><br>