Monitoring Beach Shape Development and Sediment Dynamics on a Sandy Beach with Low Anthropogenic Influence
Abstract
:1. Introduction
2. Materials and Methods
2.1. Study Area
2.2. Sand Sample and Beach Profiles
2.3. Granulometric Analysis
2.4. Beach Profile Analysis
2.5. Tropical Storms and Hurricanes
3. Results
3.1. Temporal and Spatial Variability
3.2. Textural Parameters of Sediment
3.3. Erosion Versus Accumulation
4. Discussion
4.1. Geomorphologic Variation of the Beach Profile
4.2. Relationship between Granulometric Parameters and Wind
4.3. Relationship between Recovery Time and Hydrometeorological Events
4.4. Relationship between Alongshore Transport Direction and Winds
4.5. Quasi-Equilibrium System
5. Conclusions
- (a)
- Low-energy stage: both mouths of the Marabasco River are closed at this time of the year (Meyer et al., 2006) [13]. Therefore, there is no supply of sediment. The processes of erosion and accumulation are carried out with the previously deposited sediment. There is a quasi-equilibrium between the processes of erosion and accumulation.
- (b)
- Medium-energy stage: both mouths of the Marabasco River are open. There is a large supply of sediment to Playa del Coco. This material is mostly deposited on the beach, although a part of it can go to the ocean. Destructive and constructive processes are present, although the latter dominate over the former.
- (c)
- High-energy stage: both mouths of the Marabasco River are open, and since the energy of the river and the supply of sediments to Playa del Coco is greater than it is in the medium-energy stage, erosion of the previously deposited material occurs. The loss of sediment on the beach is greater than the supply of the Marabasco River, and it is assumed that a large part of the supply of the Marabasco River could be deposited in submerged sandbars. The first dune cordon disappears.
Author Contributions
Funding
Data Availability Statement
Acknowledgments
Conflicts of Interest
Appendix A
References
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Station | M1 September 2013 | M2 November 2013 | M3 January 2014 | M4 March 2014 | M5 May 2014 | M6 July 2014 | M7 September 2014 |
---|---|---|---|---|---|---|---|
S1 | L | L | L | M | M | M | H |
S2 | L | M | L | M | L | M | H |
S3 | M | M | L | M | M | M | H |
S4 | M | L | M | M | M | M | H |
S5 | M | M | M | M | L | M | H |
S6 | M | M | L | M | M | M | H |
S7 | M | L | L | M | L | M | H |
Station | M1 September 2013 | M2 November 2013 | M3 January 2014 | M4 March 2014 | M5 May 2014 | M6 July 2014 | M7 September 2014 |
---|---|---|---|---|---|---|---|
S1–S2 | 47,836 | 60,850 | 43,575 | 27,198 | 28,527 | 41,362 | 8850 |
S2–S3 | 37,329 | 49,008 | 43,051 | 40,990 | 27,861 | 40,264 | 9826 |
S3–S4 | 32,329 | 52,498 | 33,670 | 45,520 | 25,399 | 37,821 | 8874 |
S4–S5 | 34,630 | 51,747 | 33,723 | 37,276 | 25,366 | 38,979 | 6793 |
S5–S6 | 30,484 | 51,157 | 39,918 | 44,046 | 34,149 | 38,434 | 7974 |
S6–S7 | 26,143 | 55,629 | 41,866 | 48,525 | 35,559 | 37,555 | 10,323 |
Sampling Date | Name | Duration | Minimal Distance to Study Area | Type | Wind Speed |
---|---|---|---|---|---|
M1 September 2013 | Lorena | 5–7 September 2013 | 232 km SW from Manzanillo | Tropical Storm | 83 km/h |
Manuel | 13–19 September 2013 | 509 km SE from Manzanillo | Hurricane (I) | 120 km/h | |
M2 November 2013 | Calm season | ||||
M3 January 2014 | Calm season | ||||
M4 March 2014 | Calm season | ||||
M5 May 2014 | Amanda | 22–29 May 2014 | 1005 km SE from Manzanillo | Hurricane (III) | 195 km/h |
M6 July 2014 | Cristina | 9–16 June 2014 | 375 km SSW from Manzanillo | Hurricane (II) | 155 km/h |
Douglas | 28 June—5 July 2014 | 525 km SSW from Manzanillo | Tropical Storm | 55 km/h | |
Elida | 30 June—2 July 2014 | 195 km SSE from Manzanillo | Tropical Storm | 85 km/h | |
Hernan | 26–29 July 2014 | 580 km SW from Manzanillo | Tropical Storm | 85 km/h | |
Karina | 13–26 August 2014 | 370 km SW from Manzanillo | Tropical Depression | 55 km/h | |
Marrie | 21–29 August 2014 | 555 km SSW from Manzanillo | Hurricane (I) | 148 km/h | |
M7 September 2014 | Norbert | 2–8 September 2014 | 230 km W from Manzanillo | Tropical Storm | 75 km/h |
Odile | 10–18 September 2014 | 260 km W from Manzanillo | Hurricane (III) | 175 km/h | |
Polo | 16–22 September 2014 | 215 km W from Manzanillo | Tropical Storm | 110 km/h |
Station | September–November 2013 | November–January 2013–2014 | January–March 2014 | March–May 2014 | May–July 2014 | July–September 2014 |
---|---|---|---|---|---|---|
S1–S2 | 13,014 | −17,275 | −16,377 | 1374 | 12,790 | −32,512 |
S2–S3 | 11,679 | −5956 | −2061 | −13,129 | 12,403 | −30,438 |
S3–S4 | 19,923 | −18,828 | 11,850 | −20,121 | 12,421 | −28,947 |
S4–S5 | 17,116 | −18,024 | 3553 | −11,910 | 13,612 | −32,185 |
S5–S6 | 20,673 | −11,239 | 4128 | −9897 | 4285 | −30,460 |
S6–S7 | 29,485 | −13,762 | 6658 | −12,966 | 1996 | −27,232 |
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Zuber, A.; Álvarez, M.-C.; Mendoza, E.; Díaz-Flores, M.Á.; Galicia-Pérez, M.; Torres-Orozco, E. Monitoring Beach Shape Development and Sediment Dynamics on a Sandy Beach with Low Anthropogenic Influence. Land 2022, 11, 2219. https://doi.org/10.3390/land11122219
Zuber A, Álvarez M-C, Mendoza E, Díaz-Flores MÁ, Galicia-Pérez M, Torres-Orozco E. Monitoring Beach Shape Development and Sediment Dynamics on a Sandy Beach with Low Anthropogenic Influence. Land. 2022; 11(12):2219. https://doi.org/10.3390/land11122219
Chicago/Turabian StyleZuber, Alain, María-Carmen Álvarez, Edgar Mendoza, Miguel Ángel Díaz-Flores, Marco Galicia-Pérez, and Ernesto Torres-Orozco. 2022. "Monitoring Beach Shape Development and Sediment Dynamics on a Sandy Beach with Low Anthropogenic Influence" Land 11, no. 12: 2219. https://doi.org/10.3390/land11122219
APA StyleZuber, A., Álvarez, M.-C., Mendoza, E., Díaz-Flores, M. Á., Galicia-Pérez, M., & Torres-Orozco, E. (2022). Monitoring Beach Shape Development and Sediment Dynamics on a Sandy Beach with Low Anthropogenic Influence. Land, 11(12), 2219. https://doi.org/10.3390/land11122219