Towards a Sustainable Stability of Coastal Zone at Rosetta Promontory/Mouth, Egypt

Seven major old deltaic branches of the Nile River are mentioned in various historical documents and in ancient maps. At the point of discharge of the Nile into the Mediterranean, the great Nile delta has formed and furnishes the most fertile area for cultivation in the Egyptian territory [1]. Currently, the Nile delta is embraced by two large branches of the Nile (the Rosetta and Damietta branches and their promontories). Both the Rosetta and Damietta branches discharge some freshwater directly and indirectly into the Mediterranean Sea to form the Nile estuary (also known as the Nile delta coastal area). Fluctuations in both quantity and quality of the Nile water reaching the Mediterranean, especially as a result of the Aswan High Dam (AHD) construction in 1965, have profoundly influenced the ecological characteristics of the river and the surrounding marine environment. These two main branches developed the Rosetta and Damietta promontories which have pro-graded during Holocene times into the Mediterranean Sea [2]. Rosetta Branch flows downstream Delta Barrage to the North-West where it ends with Edfina Barrage which releases excess water to the Mediterranean Sea. The Rosetta Branch water serves for a wide range of functions including tourism, trading and agricultural activities, industrial and domestic water supply, fisheries and recreation [3,4]. Rosetta Promontory is located on the eastern end of Abu-Quir Bay and at a distance of about 60 km to the east of Alexandria city. It was built during the years from 500 to 1000 AD when the water from the Canopic and Sebennitic branches, (Figure 1) was diverted naturally and/or artificially into an existing canal known afterwards as Rosetta Nile Branch [5].


Introduction
Seven major old deltaic branches of the Nile River are mentioned in various historical documents and in ancient maps. At the point of discharge of the Nile into the Mediterranean, the great Nile delta has formed and furnishes the most fertile area for cultivation in the Egyptian territory [1]. Currently, the Nile delta is embraced by two large branches of the Nile (the Rosetta and Damietta branches and their promontories). Both the Rosetta and Damietta branches discharge some freshwater directly and indirectly into the Mediterranean Sea to form the Nile estuary (also known as the Nile delta coastal area). Fluctuations in both quantity and quality of the Nile water reaching the Mediterranean, especially as a result of the Aswan High Dam (AHD) construction in 1965, have profoundly influenced the ecological characteristics of the river and the surrounding marine environment. These two main branches developed the Rosetta and Damietta promontories which have pro-graded during Holocene times into the Mediterranean Sea [2]. Rosetta Branch flows downstream Delta Barrage to the North-West where it ends with Edfina Barrage which releases excess water to the Mediterranean Sea. The Rosetta Branch water serves for a wide range of functions including tourism, trading and agricultural activities, industrial and domestic water supply, fisheries and recreation [3,4]. Rosetta Promontory is located on the eastern end of Abu-Quir Bay and at a distance of about 60 km to the east of Alexandria city. It was built during the years from 500 to 1000 AD when the water from the Canopic and Sebennitic branches, ( Figure  1) was diverted naturally and/or artificially into an existing canal known afterwards as Rosetta Nile Branch [5].
This promontory continued growing up actively till the beginning of the 20th century where it extended seaward by about 14 km [6]. The old maps showed that Rosetta city which was built hundreds years ago at the outlet of this Nile branch now became inland some kilometers south of the sea shore. Figure 2 shows the advance and retreat of the eastern and western sides of Rosetta promontory.
Since 1900 to the present time the water flow and sediments carried out by Rosetta branch to the sea have been reduced due to: the climate changes, the construction of dams and control works along the river Nile itself, the continuous use of water for permanent irrigation requirements and/or man interference with the shoreline. Consequently serious erosion began to affect Rosetta promontory causing the damage to its coastal zone environment. The erosion rate has been accelerated since the completion of the High Aswan Dam in 1964 which trapped all the sediments transported by the River in its upstream side. However erosion is not the only trouble facing this promontory, but sedimentation of its coastal outlet is taking place. This sedimentation is causing serious and intensive shoaling of the exit which hinders fishing operation, coastal navigation of the fishing boats in the area and disturbs the ecosystem of the Rosetta branch [7]. Many protective measures had been executed and/ or under execution to combat the erosion and sedimentation problems of Rosetta area. A comprehensive study of the forces affecting the coastal changes in the area began in 1981 including: hydrographic survey, directional wave and current measurements and the movement of the sediment and their characteristics. This paper continues focusing on the sedimentation problem inside Rosetta estuary which has been studied in details by previous works [8,9]. It aims to improve the Mediterranean coast stability at the Rosetta outlet by developing an integrated sustainable solution to enhance stability conditions using calibrated/validated Coastal Modeling System.

Methodology
Based on the collected field data, a calibrated/validated depth averaged model has been built to understand the hydrodynamic processes, the sediment transport mechanism and check the validity of a suggested integrated approach based on a combination of hard measures, soft measures and nourishment. The calibrated/verified  Model results for each scenario are compared to the case of morphological changes in the case of no action (the recent situation without addition coastal structures).

Testing hard structures (boundary jetties)
This main aim of using the boundary jetties with different lengths is to select the scenario which most control the sediment transport east and west of the promontory via modeling process [7] The eroded sediments from the eastern tip of the promontory move into two directions: one portion towards the west to be deposited on the eastern side of the estuary causing sedimentation of its eastern side, while the second portion is directed towards the east of the promontory. On the other hand, the western jetty is selected to decrease the wave energy Coastal Modeling System (CMS) is used to test the different scenarios in terms of hydrodynamic and morphodynamic effects of these scenarios. A total of 24 scenarios are tested.
The Coastal Modeling System (CMS) interactively calculates wave transformation and wave-induced currents, water level change by tide, wind, waves, interacting waves and currents, sediment transport and morphology change [6] The description of the model was described in details by [10] The setup of the CMS model (flow, and wave), forcing data, sensitivity analysis , and the calibration of the model were described in details by Masria et al. [11,12].The modeling procedure is briefly presented in Figure 3. In order to achieve the objective of this paper, 24 scenarios are tested. The effect of the hard structures at the center of the outlet and at the boundary on the erosion and sedimentation is investigated. The optimal scenario is selected then used with the beach nourishment or near shore nourishment. Six cross sections inside the

Results and Discussion
Hard structures effect on the outlet stability Eastern jetty: In this group, four scenarios were tested. The boundary jetty has been used in this group at the eastern tip of the promontory to cut the vortex within this area which causes the sedimentation problem in the outlet.
The model results are summarized in Figure 5. The results show that the eastern jetty has a remarkable effect on decreasing the siltation problem inside the outlet especially for jetty length exceeds 350 m. The new outlet cross section is more suitable for navigation compared to the case of no action. On the other hand, these jetties partially eliminate the erosion in front of the east revetment as well as the tip of the west revetment. But the accumulation of sediment in the eastern side of the jetty causes sand bypass which regenerate the siltation problem in the outlet.
In general, the eastern jetty with length more than 350 m can help in improving the hydrodynamic condition of the promontory. The main point here is sediment filling in the upstream of the jetty should at the outlet, hence decreasing the radiation stress that generates the sediment transport inside the outlet.

Sand nourishment scenarios
The sand nourishment is considered to overcome or at least minimize the erosion in front of the seawalls. Two different nourishment sets were simulated: beach nourishment, and near shore nourishment. The authors Masriaet. al. [13] checked the availability of sediment resources for the nourishment and identify two main sources; offshore source with mean grain size range between 0.1 and 0.18 mm and land source with mean grain size range between 0.24-0.32 mm. Also by using Particle Tracking Model (PTM) they found that the sediment source come from El Khatatba which located 150 km from the site landward with mean grain size 0.32 mm is more efficient within this area.

Testing a combination of using jetties and nourishment
These group of scenarios used a combination of the optimal jetties from 2.1 and the nourishment. From 2.2 to obtain an improved integrated solution for long term stability (sustainable) to Rosetta promontory/eastury. not be allowed to avoid sediment bypass which will accumulate inside the estuary (Figure 5f).

Western jetty:
In the western jetties group, four scenarios were tested including the boundary jetty at western tip of the promontory to eliminate the hydrodynamic force west of the estuary. Figure 6 shows the effect of the different lengths of the western jetty on the bed morphology as well as on the hydrodynamic parameters at Rosetta promontory after one year. It is clear that the western jetty decreases the wave energy that reaches the outlet which accelerates the sediment accumulation within the estuary. Increase the jetty length will move the sedimentation area seaward. Generally, the western jetty is not sufficient alone to solve the promontory problems but can be useful if combined with other system of protection measures.
In spite of the eastern jetty which has some advantage in developing the hydrodynamic characteristics of the Rosetta promontory, all the above alternatives failed to solve the promontory problems. Accordingly, the next group of alternatives is proposed to reach the desired stability condition of the promontory. These alternatives are combination of the best scenarios concluded from the centered, eastern, and western control measures.
Combination between the best of eastern and western: In this group, additional three scenarios were tested. The first two successive scenarios represent a combination between the eastern jetty of 360 m length and the western one with two different lengths (500 m, 800 m) , and the last one is to add centered front jetty (the best in the centered jetties group) with the eastern jetty (360 m) and the western one (800 m). Figure 7 shows the effect of these scenarios on the bed level at different outlet's cross sections after one year. Generally, it is concluded that both eastern jetty alone and the combination between the eastern (360 m) and the western one (800m), enhance the hydrodynamic condition of the estuary and can be used to stabilize the Rosetta outlet. The only restriction in these two solutions is the request for continuous dredging for the accreted area behind the eastern jetty and bypassing the sediment to the hotspot areas in front of the revetments which suffer from severe erosion as shown in Figure 8.
Although that eastern jetty of length 360 m or a combination between the eastern jetty and the western jetty of length 800 m show good results compared to the other alternatives in term of decreasing the accretion inside the outlet, but still not have a significant effect on mitigating erosion in front of the revetments. So, the second approach as mentioned earlier will focus on obtaining an integrated solution to maintain the stability at the promontory.

Sand nourishment effect on rosetta outlet stability
This approach is conducted by supplying sediments (sand nourishment) in front of revetments. The sediments are supplied through the following nourishment techniques: beach nourishment and near shore nourishment.
The proposed placement sites of the nourishment material were selected in a previous work by Masria et al. [10] according to the hot spots of the erosion at both the (nodal point) at the eastern side of the promontory where long shore sediment transport is diverted to east and west and also at the western side of the promontory with different volumes and geometries for both techniques.
The morphological change after one year, for different scenarios of applying 100,000 m 3 , 200,000 m 3 , and 300,000 m 3 were simulated using the CMS software. Figure 9 shows a sample of the results for the near shore nourishment volume of 300,000 m 3 . From the results, it is clear that all scenarios almost have the same trend at the accreted areas. To accurately study the second scenarios with different volumes, the hotspot area was divided into three subareas; the eastern, middle and western as shown in Figure 10. The bed profiles are plotted compared to the initial profile before adding the nourishment material. It is clear that all scenarios showed a negligible effect compared to no action scenario except scenario two which showed slight improvement at the eastern profile WBP 3.8 as shown in Figure 11.
Although the second set of scenarios with sand volume (300,000 m 3 ) is slightly better than other scenarios in comparison with no action scenario, it is clear that there is no significant effect of the near shore nourishment technique in decreasing the severe erosion in front of the seawalls. It may be due to the interaction between the revetment and the hydrodynamic force which guide the sediment outside the desirable area. On the other hand, it increases the siltation problem inside the outlet.
So, it is recommended in the next section to test boundary jetties which control the flow and sediment from the outlet with beach nourishment east and west of the promontory to solve the erosion problem.

Combination between hard and soft measures
From above mentioned alternatives, it was found that both beach nourishment and near shore nourishment are not sufficient to mitigate the promontory problems. So, the best solution from each of the previous methods will be combined with the hard structures in order to trap the long shore sediment that present the key for erosion problem.
In this section two scenarios are tested. The first scenario include the best from the near-shore nourishment (placement site is at eastern side centered on the nodal point for sand volume 300,000 m 3 ) with an inclined groins at the western revetment (to prevent the erosion occurs at the western tip of the revetment), and eastern jetty of 360 m length   (to prevent the accumulation of the sediments through nodal point inside the inlet). The second scenario is the same as the first one; the only difference is that the eastern jetty is inclined. Figure 12 shows the two proposed scenarios in this section. Figures 13 and 14 show the morphology change and annual sediment volumes after one year, for the two scenarios. It is illustrated from this figure that the both scenarios enhance the inlet stability compared to the no action case in terms of reducing the sediment accumulation inside the inlet. In addition, it decreases the erosion rate at the hotspot areas in front of the eastern and western revetments (especially the western one).
Generally, it is concluded that both scenarios improve the stability of the promontory, therefore, the scenario with lower construction cost will be preferred. In Egypt, the cost of the breakwater ranges between 6000 to 8000$ per meter) depends on the depth. For the sand nourishment, the cost ranged from 8 to 10$/m 3 depending on the location. For Rosetta, the construction cost of the hard structure can be roughly calculated as 7000$ per meter and the nourishment as 9$/m3, "Egyptian Coastal Research Institute". The construction cost consists of the cost of constructing the hard measures and the cost of sand nourishment, as follows: Cost for first scenario=(400+400+360)* 7000+(300000*9)=8,120,000 $ Cost for second scenario=(400+400+580)* 7000+(300000*9)=9,660,000 $ So, according to construction cost, the best scenario from this group is the first one.

Conclusion
The hydrodynamic modeling was applied through two approaches to solve the coastal problems (erosion and accretion) at Rosetta promontory in terms of obtaining an integrated long-term (sustainable) solution to enhance stability conditions of Rosetta estuary. Different measures including hard (jetties), soft (sand nourishment) and combination between both are presented to investigate the effect of each one on the Rosetta promontory stability, hence reach to an integrated solution.
CMS was used to check the tested alternatives. The hard measures shows a significant effect in mitigating the accretion problem, but the promontory still suffers from erosion in front of the seawalls. On the other hand, it is clear that there is no strong effect of the near shore nourishment technique in overcoming the severe erosion in front of the seawalls. The combination between the hard structures and soft one proved to be an efficient method to mitigate the coastal problems as it decreases the siltation problems inside the inlet, in addition to decrease the erosion in front of the seawalls.