Mathematical modelling as a tool for the assessment of impact of thermodynamics on the algal growth in dam reservoirs – case study of the Goczalkowice Reservoir
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May 25, 2018
About this article
Published Online: May 25, 2018
Page range: 21 - 29
DOI: https://doi.org/10.2478/oszn-2018-0005
Keywords
© 2018 Rafał Ulańczyk, Czesław Kliś, Damian Absalon, Marek Ruman, published by Sciendo
This work is licensed under the Creative Commons Attribution-NonCommercial-NoDerivatives 3.0 License.
Figure 1

Figure 2
![Meteorological conditions and water temperature in Goczałkowice Reservoir in analysed period [based on archival data of the ZiZOZap project].](https://sciendo-parsed.s3.eu-central-1.amazonaws.com/647269d0215d2f6c89dc7232/j_oszn-2018-0005_fig_002.jpg?X-Amz-Algorithm=AWS4-HMAC-SHA256&X-Amz-Content-Sha256=UNSIGNED-PAYLOAD&X-Amz-Credential=AKIA6AP2G7AKOUXAVR44%2F20250912%2Feu-central-1%2Fs3%2Faws4_request&X-Amz-Date=20250912T032549Z&X-Amz-Expires=3600&X-Amz-Signature=ab5a39dc70b93698393b6846107a029e440cbc29f220fa6973c14e6f54518cde&X-Amz-SignedHeaders=host&x-amz-checksum-mode=ENABLED&x-id=GetObject)
Figure 3

Figure 4
![Model calibration results (grey: range of modelled temperatures ELCOM, black: observed temperatures) [observations based on archival data of the ZiZOZap project]](https://sciendo-parsed.s3.eu-central-1.amazonaws.com/647269d0215d2f6c89dc7232/j_oszn-2018-0005_fig_004.jpg?X-Amz-Algorithm=AWS4-HMAC-SHA256&X-Amz-Content-Sha256=UNSIGNED-PAYLOAD&X-Amz-Credential=AKIA6AP2G7AKOUXAVR44%2F20250912%2Feu-central-1%2Fs3%2Faws4_request&X-Amz-Date=20250912T032549Z&X-Amz-Expires=3600&X-Amz-Signature=0a51c313c811315ae54f4ee46d54627340b8c8d9be719a4b80963ad449f42d75&X-Amz-SignedHeaders=host&x-amz-checksum-mode=ENABLED&x-id=GetObject)
Figure 5
![Comparison of modelled (ELCOM) and observed temperatures in the water column before and after calibration [observations based on archival data of the ZiZOZap project]](https://sciendo-parsed.s3.eu-central-1.amazonaws.com/647269d0215d2f6c89dc7232/j_oszn-2018-0005_fig_005.jpg?X-Amz-Algorithm=AWS4-HMAC-SHA256&X-Amz-Content-Sha256=UNSIGNED-PAYLOAD&X-Amz-Credential=AKIA6AP2G7AKOUXAVR44%2F20250912%2Feu-central-1%2Fs3%2Faws4_request&X-Amz-Date=20250912T032549Z&X-Amz-Expires=3600&X-Amz-Signature=734c3cb0062226f51840a019c22c01b4695d32543dff0bf180f007bbc4ff9222&X-Amz-SignedHeaders=host&x-amz-checksum-mode=ENABLED&x-id=GetObject)
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Figure 7
![Comparison of temperature difference in water profile ΔT (ELCOM model) and observed concentration of ChlA [observations based on archival data of the ZiZOZap project]](https://sciendo-parsed.s3.eu-central-1.amazonaws.com/647269d0215d2f6c89dc7232/j_oszn-2018-0005_fig_007.jpg?X-Amz-Algorithm=AWS4-HMAC-SHA256&X-Amz-Content-Sha256=UNSIGNED-PAYLOAD&X-Amz-Credential=AKIA6AP2G7AKOUXAVR44%2F20250912%2Feu-central-1%2Fs3%2Faws4_request&X-Amz-Date=20250912T032549Z&X-Amz-Expires=3600&X-Amz-Signature=6459c499148296507f5e77276a57b74e0d20f8090a8438e920f6133833197b52&X-Amz-SignedHeaders=host&x-amz-checksum-mode=ENABLED&x-id=GetObject)
Parameters used in ELCOM model_
Parameter | Value |
---|---|
Mean albedo of the water for shortwave radiation | 0.08 |
Mean albedo of the water for long wave radiation | 0.03 |
Drag coefficient on bottom cells | 0.005 |
Initial wind speed for domain | 0 m/s |
Initial water temperature for domain | 11.4°C |
Light extinction coefficients for shortwave radiation bands used to calculate the shortwave penetration: | |
Photosynthetically Active Radiation (PAR) | 0.2-0.4 m–1 |
Near Infrared (NIR) | 1 m–1 |
Ultra Violet A (UVA) | 1-1.8 m–1 |
Ultra Violet B (UVB) | 2.5-2.8 m–1 |
Sediments reflectivity | 0.9 |
Surface heat transfer coefficient | 0.0013-0.0015 |