README: the Supplementary material of
"Macro-turbulent flow and its impacts on sediment transport potential of a subarctic river during ice-covered and open-channel conditions 
Eliisa Lotsari (1, 2), Michael Dietze (3), Maria Kämäri (4), Petteri Alho (2,5), Elina Kasvi (6,2)

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
2 Department of Geography and Geology, University of Turku, FI-20014 Turun yliopisto, Turku, Finland.
3 Section 4.6 Geomorphology, German Research Centre for Geosciences GFZ Potsdam, D-14473 Potsdam, Germany. mdietze@gfz-potsdam.de
4 Finnish Environment Institute, Latokartanonkaari 11, FI-00790 Helsinki, Finland. maria.kamari@ymparisto.fi
5 Finnish Geospatial Research Institute, National Land Survey of Finland, Geodeetinrinne 2, FI-02430, Masala, Finland. mipeal@utu.fi
6 Turku University of Applied Sciences, Joukahaisenkatu 3, FI-20520, Turku, Finland. elina.kasvi@turkuamk.fi


Supplementary material "Supplementary_material_Lotsari_et_al_macroturbulent_flow.zip" includes:

R package folder S1: S1_adcp_R_package_windows_computer
R package folder S2: S2_adcp_R_package_linux_computer
Figure S3: S3_W2018_streamwise_velocity
Figure S4: S4_W2018_vertical_velocity
Figure S5: S5_S2017_streamwise_velocity
Figure S6: S6_S2017_vertical_velocity
Figure S7: S7_CS1_streamwise_velocity_winters
Figure S8: S8_CS1_streamwise_velocity_openchannel_conditions
Figure S9: S9_CSB_streamwise_velocity
Figure S10: S10_CS4_streamwise_velocity
Figure S11: S11_LISA_W2018_vertical_velocity
Figure S12: S12_LISA_S2017_vertical_velocity

See details of the R packages S1 and S2 form the above-mentioned paper
and online from https://github.com/coffeemuggler/adcp

The letters in the acronyms of the measurement times (cf. Figures S3-S10) stand for: W=winter, S=spring, A=autumn.
The measurement locations 1 (inlet), A, 2, B (apex), 3, C and 4 (outlet) are within a symmetrical meander bend,
and their precise locations are shown in the Figures 1 and 2 of the above-mentioned paper
(CS stands for cross-section).

The scales of the streamwise flow velocity figures (Figures S3, S5, S7–10) were defined either between 0 and 1 m/s,
or between 0 and 0.5 m/s, for gaining the best visualisation of the flow structures at each measurement time
and location, as most of the flow was within those magnitude ranges. Few occasional cells had 
velocities higher than 1, or slow flow towards upstream (i.e. negative), but these were rare and did
not affect on the overall detection of the high and low flow patterns. 

Figure S11: The LISA analysis results at each measurement location, calculated based on vertical
velocity of W2018. Measurement ID equals with samples (n), and also represents seconds. The black 
dots indicate the occurrence times of statistically significant strong high and low flow wedges 
reaching from surface to river bed, and the grey dots indicate the times when there is weaker wedge,
i.e. cluster has broken with few cells within the vertical water column.

Figure S12:The LISA analysis results at each measurement location, calculated based on vertical 
velocity of S2017. Measurement ID equals with samples (n), and also represents seconds. The black 
dots indicate the occurrence times of statistically significant strong high and low flow wedges 
reaching from surface to river bed, and the grey dots indicate the times when there is weaker wedge,
i.e. cluster has broken with few cells within the vertical water column.