SMIAH
Civil/Environmental
- Jan 26, 2009
- 482
I have to prepare the hydraulic study of a dam. This dam is located 1 mile downstream from the outlet of a lake (where it represents the only possible outlet).
On the lake are recorded maximum daily water levels for nearly 100 years now. The maximum instantaneous water levels are also available for over 40 years, but they do not vary dramatically from the daily maximum levels (the max deviation is around 1 inch).
The dam is equiped with multiple gates and it controls the water level of the lake. Thus, closing the gates in order to reduce the peak flows evacuated downstream (e.g. to protect people and infrastructure downstream) has a significant impact on the lake’s water level.
However, the opening height of these gates is rarely noted, and it is difficult to access the rules of exploitations used back in the 50s, for example.
I think that the basic method to estimate the hydrologic conditions in the lake would be to simulate the passage of a flood hydrograph, taking into account the presence of the dam. However, the watershed of this lake has an area of nearly 775 square miles...
I already have estimated the probabilities associated with the recorded water levels using the Adjustment law of Log-Pearson III (WRC). Then I think that I could simulate the water level reached at the dam using the water levels of the lake as the upstream boundary condition in a model like HEC RAS (I have cross section data).
But I doubt that these water levels are representative of the hydrological conditions and this based on the fact that it is possible that the dam operators have used different strategies like, for example, letting the water level of the lake increase by closing the gates in order to reduce peak flows and protect downstream populations as there were less issues related to flooding around the lake back then. And this is not shown in the maximum recorded water levels...
I'm stuck right now.
Tips? Similar situations solved?
On the lake are recorded maximum daily water levels for nearly 100 years now. The maximum instantaneous water levels are also available for over 40 years, but they do not vary dramatically from the daily maximum levels (the max deviation is around 1 inch).
The dam is equiped with multiple gates and it controls the water level of the lake. Thus, closing the gates in order to reduce the peak flows evacuated downstream (e.g. to protect people and infrastructure downstream) has a significant impact on the lake’s water level.
However, the opening height of these gates is rarely noted, and it is difficult to access the rules of exploitations used back in the 50s, for example.
I think that the basic method to estimate the hydrologic conditions in the lake would be to simulate the passage of a flood hydrograph, taking into account the presence of the dam. However, the watershed of this lake has an area of nearly 775 square miles...
I already have estimated the probabilities associated with the recorded water levels using the Adjustment law of Log-Pearson III (WRC). Then I think that I could simulate the water level reached at the dam using the water levels of the lake as the upstream boundary condition in a model like HEC RAS (I have cross section data).
But I doubt that these water levels are representative of the hydrological conditions and this based on the fact that it is possible that the dam operators have used different strategies like, for example, letting the water level of the lake increase by closing the gates in order to reduce peak flows and protect downstream populations as there were less issues related to flooding around the lake back then. And this is not shown in the maximum recorded water levels...
I'm stuck right now.
Tips? Similar situations solved?