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ADCP data of ice-covered and open-channel (macro-turbulent) flow, Pulmanki River, 2016-2020

<p>README of ADCP_data_Lotsari_et_al_Water_opened.zip</p> <p><br> The ADCP data was the basis of the following paper:<br> Macro-turbulent flow and its impacts on sediment transport potential of a subarctic river during ice-covered and open-channel conditions&nbsp;<br> Eliisa Lotsari (1, 2), Michael Dietze (3), Maria K&auml;m&auml;ri (4), Petteri Alho (2,5), Elina Kasvi (6,2)</p> <p>1 Department of Geographical and Historical Studies, University of Eastern Finland, Yliopistokatu 2, P.O. Box 111, FI-80101, Joensuu, Finland. eliisa.lotsari@uef.fi<br> 2 Department of Geography and Geology, University of Turku, FI-20014 Turun yliopisto, Turku, Finland.<br> 3 Section 4.6 Geomorphology, German Research Centre for Geosciences GFZ Potsdam, D-14473 Potsdam, Germany. mdietze@gfz-potsdam.de<br> 4 Finnish Environment Institute, Latokartanonkaari 11, FI-00790 Helsinki, Finland. maria.kamari@ymparisto.fi<br> 5 Finnish Geospatial Research Institute, National Land Survey of Finland, Geodeetinrinne 2, FI-02430, Masala, Finland. mipeal@utu.fi<br> 6 Turku University of Applied Sciences, Joukahaisenkatu 3, FI-20520, Turku, Finland. elina.kasvi@turkuamk.fi</p> <p>(Note: During the time of data gathering, Maria K&auml;m&auml;ri worked at the University of Eastern Finland, and Elina Kasvi at the University of Turku)</p> <p>The data set has been measured with Sontek M9 or S5 sensors, depending on the time step (Table 1).</p> <p>Table 1. The measurement times, their acronyms (applied in the above mentioned publication)<br> and applied sensors. In the acronyms of the measurement times W=winter low flow period, S=spring<br> (snow-melt flood period), A=autumn low flow period. These information are presented also<br> in the Table 1 of the above-mentioned publication.<br> Date&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp; &nbsp;Acronym &nbsp;Sensor<br> 17.2.2016&nbsp;&nbsp; &nbsp;W2016&nbsp;&nbsp;&nbsp;&nbsp;M9<br> 25.5.2016&nbsp;&nbsp; &nbsp;S2016&nbsp;&nbsp;&nbsp;&nbsp;S5&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;<br> 10.9.2016&nbsp;&nbsp; &nbsp;A2016&nbsp;&nbsp;&nbsp;&nbsp;M9<br> 16.2.2017&nbsp;&nbsp; &nbsp;W2017&nbsp;&nbsp;&nbsp;&nbsp;M9&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;<br> 31.5.2017&nbsp;&nbsp; &nbsp;S2017&nbsp;&nbsp;&nbsp;&nbsp;M9&nbsp;&nbsp;&nbsp;&nbsp;<br> 9.9.2017&nbsp;&nbsp;&nbsp;&nbsp;&nbsp; &nbsp;A2017&nbsp;&nbsp;&nbsp;&nbsp;M9&nbsp;&nbsp;&nbsp;&nbsp;<br> 9.2.2018&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp; &nbsp;W2018&nbsp;&nbsp;&nbsp;&nbsp;M9&nbsp;&nbsp;&nbsp;&nbsp;<br> 23.5.2018&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp; &nbsp;S2018&nbsp;&nbsp;&nbsp;&nbsp;S5&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;<br> 8.9.2018&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp; &nbsp;A2018&nbsp;&nbsp;&nbsp;&nbsp;S5&nbsp;&nbsp;&nbsp;&nbsp;<br> 8.2.2019&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp; &nbsp;W2019&nbsp;&nbsp;&nbsp;&nbsp;M9&nbsp;&nbsp;&nbsp;&nbsp;<br> 21.5.2019&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp; &nbsp;S2019&nbsp;&nbsp;&nbsp;&nbsp;M9&nbsp;&nbsp;&nbsp;&nbsp;<br> 6.2.2020&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp; &nbsp;W2020&nbsp;&nbsp;&nbsp;&nbsp;M9&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;</p> <p>RiverSurveyor Live software, and its most recent version, was used each time.<br> The measurements have been done at Pulmanki River (69&deg;55&#39;59.09&quot; N; &nbsp;28&deg; 2&#39;34.32&quot; E), Northern Finland, during 2016 - 2020.&nbsp;<br> The data is in directories of corresponding measurement times. The measurement<br> locations cs1, cs2, cs3, cs4, csA, csB and csC can be found in the paper (Figs. 1 and 2).&nbsp;<br> The data is in raw Matlab file format, as exported from the RiverSurveyor Live software.<br> The coordinate system is ENU.</p> <p>When used, the referencing to the paper and DOI ( 10.5281/zenodo.3855035 ) are required.</p>

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40/100

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These five areas show where the dataset supports — or may limit — practical reuse.

Stewardship
8
Harmonization
4
Access
16
Reuse readiness
8
Engagement
4

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