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Nature-based
solutions and
climate-adaptation
for west
Mediterranean urban
beaches
Rationale:
• Beach sand: a scarce natural resource, within an altered morphodynamic
environment, providing huge amounts of ES, but without an
comprehensive integrated management plan.
• Current management system does not include emerged sand
management.
• Recent storm events show a relevant vulnerability that will increase with
climatic change.
SIZE MATTERS
The 15,5 km of public beaches at the
Llobregat delta amount only 2.370.000 m3
of backshore and dunes, less than the
12% of the replenishment of the Sand
Engine experiment at the Netherlands.
SIZE MATTERS
Very few sand, with no sand inflow after the construction of the new port dyke entering
into the sea 1,8 km. No more sand arriving from the river. No sand cleaning by the sea,
as it is a micro tidal environment.
SIZE MATTERS
Very few sand but:
• Delivering huge amounts
of ES.
• The most visited
landscape of Catalonia.
• Densities arriving to 500
sun-bathers/100m.
• The “brandscape” of the
Metropolitan Area of
Barcelona.
PURPOSE:
• Can an ES-based management plan aim to achieve a
resilient beach in front of climatic change?
• Explore the limits of the dune construction as a NBS.
SCOPE:
• Information sources
• What kind of sand needed?
• How much dry sand needed?
High resolution LIDAR (1 point/m2)
Wave environment & wind direction
Wind intensity, direction and
seasonality
Satellite imaginery and flights, one of them only 4 days
after the biggest storm in 15 years.
Geotagged photos
And citizen science opportunity
Basic elements of a beach
Basic elements of a beach Size needs for intensive use
Dry sand anywhere over 1,2 m height.
Sewage dischargeWashover flooding
Limit of wind
scouring
Low energy wave limit
Minimum volume needed to cope with the highest density
of sunbathers found on fieldwork: 4.950 m3 /100 m beach
stretch (if slope optimized!).
Urbanized areas with less than 5.000m3 of sand, and without dunes
Relevant drivers:
Dyke south-west
Pets
Intensive social
use-Mechanical
sand screening
Coastal
regression Climatic
change
Sand inflow
interruption
100.000 m3 of
beach
nourishment
each year
The expected sand transport model within the sand nourishment project did not work.
Analysis:
Processes triggered by the most determinant drivers:
• Concave beaches.
• Beaches losing natural recovering capacity.
• Beach regression.
• Limits on dune formation and management.
Digital Shoreline Analysis System (DSAS)
shows how the construction of the Dyke
has affected the whole beach System.
Extensive beach widening Coastal regression
DSAS analysis show how 69% of the beaches have widened from 2004, when the
construction of the dyke ends.
Pressures:
At the SW half of the
beaches, significant widening
due to sediment
accumulation by Port Ginesta
Mechanical sieving impedes vegetation growth.
Strong winter winds scour the beach till arriving to the saturated level.
This process has lead to the loss of
more than 42.000 m3 of sand in just
the 6 year period (2008-14).
A process growing in intensity, frequency and affected area.
The concavity affected by wave overwash, but also by sewage on storm events.
The risk of a non linear response to sea level rise.
A process leading to other dysfunctions
Winter profiles that do not restore spontaneously
Pressures:
We have found that the process of scouring, which leads to higher sand loss, is
related to beach slope (> 6%).
Wavedistance
20
40
60
80
100
120
140
160
1970-2003 2004-2016
group
Excluded Rows 3
1970-2003
2004-2016
Level
13
20
Number
59,2308
84,5000
Mean
13,8212
26,7001
Std Dev
3,8333
5,9703
Std Err Mean
50,879
72,004
Lower 95%
67,583
96,996
Upper 95%
Means and Std Deviations
Oneway Analysis of Wav e distance By group
Probably sand nourishment operations
increases the volume of sandbars and its
distance to the shoreline, thus creating
lower wave energy environments.
Not enough space for a ratio of
5m2/person and 500 visitors/100 m
More spectacular sand bars related to sand
nourishment works from 2004 .
Slope determines vulnerability
When higher than 5%
A second storm, even of a much lower intensity, can scour a
much bigger amount of sand. Leaving flat beaches with
much less sand volume and increased vulnerability.
Finally the most exposed beaches keep enduring
a continued erosion process.
Pressures:
2005
2017
Slow but constant
Pressures:
The role of dunes:
Exploring their limits as Nature Based solution.
Dune erosion shows how that the root system of
marram grass and other dune plants don’t oppose
any resistance to erosion.
Marram grass (Ammophila arenaria) protects the coast by capturing sand
Biotic soil factors affecting the growth and development of
Ammophila arenaria.
A negative feed back with vegetation cover increase.
The need of mobile and semi-mobile dunes.
Transverse dunes linked to summer winds
Mechanical sieving and intensive social use impedes the natural sand aeolian transport, but is only one of
the relevant factors
But wind still keeps its ability to erode dunes and uproot marram grass
Wind direction and its angle
with the shore leads to
different responses
Erosion risk areas can be thus determined. Relative slope is also a relevant factor.
We have developed a new system to transform marram grass plantings in to efficient sand-trapping
systems
Marram grass as natural capital (dune builder)
Marram grass as natural capital and core element of a nature
based solution
Also by the design of “illegal” dunes
(in geomorphologic terms!).
Constructed dunes that are
perpendicular to shoreline. Thus being
able to capture winter sand transport
(when a critical size has been
achieved).
0
200
400
600
800
1000
1 2 3 4 5 6 7 8 9 10 11 12
nº ½ h events>11knts 180º-270º
13
13.5
14
14.5
15
15.5
16
1 2 3 4 5 6 7 8 9 10 11 12
Mean velocity knts
sknt
12
14
16
18
20
22
24
26
28
1 2 3 4 5 6 7 8 9 10 11 12
Month
Excluded Rows 8761
1
2
3
4
5
6
7
8
9
10
11
12
Level
12
12
12
12
12
12
12
12
12
12
12
12
Minimum
12
12
12
12
12
12
12
12
12
12
12
12
10%
13
13
13
13
13
12
13
13
12
13
12
12
25%
14,5
14
14
15
15
14
14
14
13
14
14
14
Median
17
17
17
18
17
16
16
15
15
16
16
15
75%
20
19
19
20
19
18
17
17
18
17
18
18
90%
27
25
28
25
25
25
25
20
22
21
25
24
Maximum
Quantiles
Rsquare
Adj Rsquare
Root Mean Square Error
Mean of Response
Observations (or Sum Wgts)
0,043359
0,04181
2,602155
14,80318
6803
Summary of Fit
Month
Error
C. Total
Source
11
6791
6802
DF
2084,166
45983,285
48067,451
Sum of Squares
189,470
6,771
Mean Square
27,9817
F Ratio
<,0001
Prob > F
Analysis of Variance
1
2
3
4
5
6
7
8
9
10
11
12
Level
400
558
610
748
889
702
831
691
393
381
324
276
Number
15,3900
15,0771
15,1328
15,7527
15,3127
14,3533
14,4079
14,0883
14,2494
14,2887
14,6389
14,2717
Mean
0,13011
0,11016
0,10536
0,09514
0,08727
0,09821
0,09027
0,09899
0,13126
0,13331
0,14456
0,15663
Std Error
15,135
14,861
14,926
15,566
15,142
14,161
14,231
13,894
13,992
14,027
14,355
13,965
Lower 95%
15,645
15,293
15,339
15,939
15,484
14,546
14,585
14,282
14,507
14,550
14,922
14,579
Upper 95%
Std Error uses a pooled estimate of error variance
Means for Oneway Anova
Oneway Anova
Oneway Analysis of sknt By Month
0
500
1000
1500
1 2 3 4 5 6 7 8 9 10 11 12
nº 1/2h events >11 knots 270º-360º
sknt
12
14
16
18
20
22
24
26
28
30
32
34
1 2 3 4 5 6
7
8
9
10 11 12
Month
Excluded Rows 10182
1
2
3
4
5
6
7
8
9
10
11
12
Level
12
12
12
12
12
12
12
12
12
12
12
12
Minimum
12
12
12
12
12
12
12
12
12
12
12
12
10%
12
12
13
12
12
12
12
12
12
12
12
12
25%
13
14
14
13
13
13
13
13
13
13
13
13
Median
15
16
17
15
14
14
14
14
15
14,25
14
15
75%
17
18,7
20
16
17
16,3
15
15
19
16
16
16
90% M
Quantiles
Rsquare
Adj Rsquare
Root Mean Square Error
Mean of Response
Observations (or Sum Wgts)
0,040347
0,038382
2,450314
14,02267
5382
Summary of Fit
Month
Error
C. Total
Source
11
5370
5381
DF
1355,557
32241,678
33597,234
Sum of Squares
123,232
6,004
Mean Square
20,5249
F Ratio
<,0001
Prob > F
Analysis of Variance
Level Number Mean Std Error Lower 95% Upper 95%
Means for Oneway Anova
Oneway Anova
Oneway Analysis of sknt By Month
12
12.5
13
13.5
14
14.5
15
15.5
1 2 3 4 5 6 7 8 9 10 11 12
mean velocity knts
Recommendations and
results:
• Data driven adaptive management systems would work quite well.
• 3D beach structure is as relevant as the total emerged sand volume.
• Dune construction can be a core element of the sand budget management,
and a very efficient and effective nature based solution.
• Dune construction must be balanced and complemented with other actions
like beach profile reconstruction (and beach slope control), and coastal
lagoons excavation.
• A sound improvement of the governance system is needed.
Slope 2014
Volume 2014
Slope and its relation
with emerged sand
volume
Slope and its relation with vulnerability
Zones que escapen a la
lògica de la correlació
indiquen processos
diferents: escarpaments
permanents i cubetes
inundables.
Allows to identify zones
that do not follow the
correlation trend: areas
with permanent sand
escarpments, and flood-
prone concavities.
It is possible to have a global view of pressure trends and its
response to management measures
Moving emerged dry sand is very cheap and effective!
A good way to protect coast against storm surges and erosion
Governance needs, transparency, social involvement .
Thank you very much
@volemdunes
#volemdunes
lascurain@sgm.es

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Nature-based solutions and climate adaptation for the Metropolitan Beach of Barcelona

  • 2. Rationale: • Beach sand: a scarce natural resource, within an altered morphodynamic environment, providing huge amounts of ES, but without an comprehensive integrated management plan. • Current management system does not include emerged sand management. • Recent storm events show a relevant vulnerability that will increase with climatic change.
  • 3. SIZE MATTERS The 15,5 km of public beaches at the Llobregat delta amount only 2.370.000 m3 of backshore and dunes, less than the 12% of the replenishment of the Sand Engine experiment at the Netherlands.
  • 4. SIZE MATTERS Very few sand, with no sand inflow after the construction of the new port dyke entering into the sea 1,8 km. No more sand arriving from the river. No sand cleaning by the sea, as it is a micro tidal environment.
  • 5. SIZE MATTERS Very few sand but: • Delivering huge amounts of ES. • The most visited landscape of Catalonia. • Densities arriving to 500 sun-bathers/100m. • The “brandscape” of the Metropolitan Area of Barcelona.
  • 6. PURPOSE: • Can an ES-based management plan aim to achieve a resilient beach in front of climatic change? • Explore the limits of the dune construction as a NBS.
  • 7. SCOPE: • Information sources • What kind of sand needed? • How much dry sand needed?
  • 8. High resolution LIDAR (1 point/m2)
  • 9. Wave environment & wind direction Wind intensity, direction and seasonality
  • 10. Satellite imaginery and flights, one of them only 4 days after the biggest storm in 15 years.
  • 11. Geotagged photos And citizen science opportunity
  • 12. Basic elements of a beach
  • 13. Basic elements of a beach Size needs for intensive use
  • 14. Dry sand anywhere over 1,2 m height. Sewage dischargeWashover flooding Limit of wind scouring Low energy wave limit
  • 15. Minimum volume needed to cope with the highest density of sunbathers found on fieldwork: 4.950 m3 /100 m beach stretch (if slope optimized!).
  • 16. Urbanized areas with less than 5.000m3 of sand, and without dunes
  • 17. Relevant drivers: Dyke south-west Pets Intensive social use-Mechanical sand screening Coastal regression Climatic change Sand inflow interruption 100.000 m3 of beach nourishment each year
  • 18. The expected sand transport model within the sand nourishment project did not work.
  • 19. Analysis: Processes triggered by the most determinant drivers: • Concave beaches. • Beaches losing natural recovering capacity. • Beach regression. • Limits on dune formation and management.
  • 20. Digital Shoreline Analysis System (DSAS) shows how the construction of the Dyke has affected the whole beach System. Extensive beach widening Coastal regression
  • 21. DSAS analysis show how 69% of the beaches have widened from 2004, when the construction of the dyke ends.
  • 22. Pressures: At the SW half of the beaches, significant widening due to sediment accumulation by Port Ginesta
  • 23. Mechanical sieving impedes vegetation growth. Strong winter winds scour the beach till arriving to the saturated level.
  • 24. This process has lead to the loss of more than 42.000 m3 of sand in just the 6 year period (2008-14).
  • 25. A process growing in intensity, frequency and affected area. The concavity affected by wave overwash, but also by sewage on storm events. The risk of a non linear response to sea level rise.
  • 26. A process leading to other dysfunctions
  • 27. Winter profiles that do not restore spontaneously Pressures:
  • 28. We have found that the process of scouring, which leads to higher sand loss, is related to beach slope (> 6%).
  • 29. Wavedistance 20 40 60 80 100 120 140 160 1970-2003 2004-2016 group Excluded Rows 3 1970-2003 2004-2016 Level 13 20 Number 59,2308 84,5000 Mean 13,8212 26,7001 Std Dev 3,8333 5,9703 Std Err Mean 50,879 72,004 Lower 95% 67,583 96,996 Upper 95% Means and Std Deviations Oneway Analysis of Wav e distance By group Probably sand nourishment operations increases the volume of sandbars and its distance to the shoreline, thus creating lower wave energy environments.
  • 30. Not enough space for a ratio of 5m2/person and 500 visitors/100 m More spectacular sand bars related to sand nourishment works from 2004 .
  • 33. A second storm, even of a much lower intensity, can scour a much bigger amount of sand. Leaving flat beaches with much less sand volume and increased vulnerability.
  • 34. Finally the most exposed beaches keep enduring a continued erosion process. Pressures:
  • 36. The role of dunes: Exploring their limits as Nature Based solution.
  • 37. Dune erosion shows how that the root system of marram grass and other dune plants don’t oppose any resistance to erosion.
  • 38. Marram grass (Ammophila arenaria) protects the coast by capturing sand
  • 39. Biotic soil factors affecting the growth and development of Ammophila arenaria. A negative feed back with vegetation cover increase. The need of mobile and semi-mobile dunes.
  • 40. Transverse dunes linked to summer winds
  • 41. Mechanical sieving and intensive social use impedes the natural sand aeolian transport, but is only one of the relevant factors
  • 42. But wind still keeps its ability to erode dunes and uproot marram grass
  • 43. Wind direction and its angle with the shore leads to different responses
  • 44. Erosion risk areas can be thus determined. Relative slope is also a relevant factor.
  • 45. We have developed a new system to transform marram grass plantings in to efficient sand-trapping systems Marram grass as natural capital (dune builder) Marram grass as natural capital and core element of a nature based solution
  • 46. Also by the design of “illegal” dunes (in geomorphologic terms!). Constructed dunes that are perpendicular to shoreline. Thus being able to capture winter sand transport (when a critical size has been achieved).
  • 47. 0 200 400 600 800 1000 1 2 3 4 5 6 7 8 9 10 11 12 nº ½ h events>11knts 180º-270º 13 13.5 14 14.5 15 15.5 16 1 2 3 4 5 6 7 8 9 10 11 12 Mean velocity knts sknt 12 14 16 18 20 22 24 26 28 1 2 3 4 5 6 7 8 9 10 11 12 Month Excluded Rows 8761 1 2 3 4 5 6 7 8 9 10 11 12 Level 12 12 12 12 12 12 12 12 12 12 12 12 Minimum 12 12 12 12 12 12 12 12 12 12 12 12 10% 13 13 13 13 13 12 13 13 12 13 12 12 25% 14,5 14 14 15 15 14 14 14 13 14 14 14 Median 17 17 17 18 17 16 16 15 15 16 16 15 75% 20 19 19 20 19 18 17 17 18 17 18 18 90% 27 25 28 25 25 25 25 20 22 21 25 24 Maximum Quantiles Rsquare Adj Rsquare Root Mean Square Error Mean of Response Observations (or Sum Wgts) 0,043359 0,04181 2,602155 14,80318 6803 Summary of Fit Month Error C. Total Source 11 6791 6802 DF 2084,166 45983,285 48067,451 Sum of Squares 189,470 6,771 Mean Square 27,9817 F Ratio <,0001 Prob > F Analysis of Variance 1 2 3 4 5 6 7 8 9 10 11 12 Level 400 558 610 748 889 702 831 691 393 381 324 276 Number 15,3900 15,0771 15,1328 15,7527 15,3127 14,3533 14,4079 14,0883 14,2494 14,2887 14,6389 14,2717 Mean 0,13011 0,11016 0,10536 0,09514 0,08727 0,09821 0,09027 0,09899 0,13126 0,13331 0,14456 0,15663 Std Error 15,135 14,861 14,926 15,566 15,142 14,161 14,231 13,894 13,992 14,027 14,355 13,965 Lower 95% 15,645 15,293 15,339 15,939 15,484 14,546 14,585 14,282 14,507 14,550 14,922 14,579 Upper 95% Std Error uses a pooled estimate of error variance Means for Oneway Anova Oneway Anova Oneway Analysis of sknt By Month 0 500 1000 1500 1 2 3 4 5 6 7 8 9 10 11 12 nº 1/2h events >11 knots 270º-360º sknt 12 14 16 18 20 22 24 26 28 30 32 34 1 2 3 4 5 6 7 8 9 10 11 12 Month Excluded Rows 10182 1 2 3 4 5 6 7 8 9 10 11 12 Level 12 12 12 12 12 12 12 12 12 12 12 12 Minimum 12 12 12 12 12 12 12 12 12 12 12 12 10% 12 12 13 12 12 12 12 12 12 12 12 12 25% 13 14 14 13 13 13 13 13 13 13 13 13 Median 15 16 17 15 14 14 14 14 15 14,25 14 15 75% 17 18,7 20 16 17 16,3 15 15 19 16 16 16 90% M Quantiles Rsquare Adj Rsquare Root Mean Square Error Mean of Response Observations (or Sum Wgts) 0,040347 0,038382 2,450314 14,02267 5382 Summary of Fit Month Error C. Total Source 11 5370 5381 DF 1355,557 32241,678 33597,234 Sum of Squares 123,232 6,004 Mean Square 20,5249 F Ratio <,0001 Prob > F Analysis of Variance Level Number Mean Std Error Lower 95% Upper 95% Means for Oneway Anova Oneway Anova Oneway Analysis of sknt By Month 12 12.5 13 13.5 14 14.5 15 15.5 1 2 3 4 5 6 7 8 9 10 11 12 mean velocity knts
  • 48. Recommendations and results: • Data driven adaptive management systems would work quite well. • 3D beach structure is as relevant as the total emerged sand volume. • Dune construction can be a core element of the sand budget management, and a very efficient and effective nature based solution. • Dune construction must be balanced and complemented with other actions like beach profile reconstruction (and beach slope control), and coastal lagoons excavation. • A sound improvement of the governance system is needed.
  • 49. Slope 2014 Volume 2014 Slope and its relation with emerged sand volume Slope and its relation with vulnerability
  • 50. Zones que escapen a la lògica de la correlació indiquen processos diferents: escarpaments permanents i cubetes inundables. Allows to identify zones that do not follow the correlation trend: areas with permanent sand escarpments, and flood- prone concavities.
  • 51. It is possible to have a global view of pressure trends and its response to management measures
  • 52. Moving emerged dry sand is very cheap and effective! A good way to protect coast against storm surges and erosion
  • 53. Governance needs, transparency, social involvement .
  • 54. Thank you very much @volemdunes #volemdunes lascurain@sgm.es