poster: p2210 09 - control of mangrove abundance by decadal changes in oceanic wave fields

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We found that changes in mangrove extent covary with the North Atlantic Oscillation winter index 1960 1965 1970 1975 1980 1985 1990 1995 2000 -3 -2 -1 0 1 2 3 -10 -5 0 5 10 -600 -400 -200 0 200 400 NAO winter index Wave heights PC1 (Expl. var. = 73%) Mangrove PC1 (Expl. var. = 75%) Expl. covar. (SVD1) = 94.5% 0 0.02 0.04 0.06 0.08 -0.02 0.1 0 0.04 0.02 0 0.02 0 0 0.04 70° 10° 20° 30° 40° 50° 60° 70° 60° 50° 40° 30° 20° 10° Wave heights EOF1 (Expl. var. = 73%) The NAO is the dominant mode of climate variability in the North Atlantic-European region. It is characterized by a large-scale seesaw pattern of sea-level pressure anomalies between the Azores High and Icelandic Low (bottom right hand corner). The North Atlantic trade winds are strongly coupled to the winter NAO, which leads to strengthening (weakening) wave heights during positive-NAO (negative-NAO) phases. Increased (decreased) wave heights favour mangrove shoreline landward (seaward) retreat (expansion). HS NAO MS Walcker, R., Anthony, E. J., Cassou, C., Aller, R. C., Gardel, A., Proisy, C., Martinez, J-M. & Fromard, F. (in press) Fluctuations in the extent of mangroves driven by multi-decadal changes in North Atlantic waves. Journal of Biogeography. Mangroves are uprooted by waves 1950 2014 1975 We mapped changes in mangrove extent using archival remote sensing images from 1950 to 2014 in French Guiana 40 50 1950 1960 1970 1980 1990 2000 2010 Total mangrove extent (ha×10³) 60 Mangrove extent Spot cnes 2010/09/27 10 km SPOT 28/02/2009 Wave exposed zone Mud bank Amazon turbid plume Mangrove extent Amazone estuary Mud bank (>340Mt) 754 Mt.an1 150 Mt.an1 Atlantic ocean Brazil Guyana Suriname Venezuela French Guiana Amazon turbid plume Amazon sediment dispersal system We studied the natural 300-km-open coast mangrove system of French Guiana (South America) Control of mangrove abundance by decadal changes in oceanic wave fields Romain Walcker, François Fromard EcoLab (Laboratoire Ecologie Fonctionnelle et Environnement) UMR 5245 (CNRS, UPS, INP), 118 route de Narbonne, 31062 Toulouse, France [email protected] & [email protected] The North Atlantic Oscillation (NAO) controls mangrove forest expansion and retreat in French Guiana (South America). This mechanism operates through wave pounding, which alters the mud substrates on which mangroves thrive. Wave pounding increases (decreases) during positive (negative) phases of the NAO. Over the 65 last years in French Guiana, mean winter wave heights fluctuated between 1.6m and 2.2m, leading to changes in mangrove extent of ± 15 000 ha. Our Common Future Under Climate Change - International Scientific Conference 7-10 July 2015 Paris, France

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Page 1: Poster: P2210 09 - Control of mangrove abundance by decadal changes in oceanic wave fields

We found that changes in mangrove extent covary with the North Atlantic Oscillation winter index

1960 1965 1970 1975 1980 1985 1990 1995 2000−3

−2

−1

0

1

2

3

−10

−5

0

5

10

−600

−400

−200

0

200

400NAO winter indexWave heights PC1 (Expl. var. = 73%) Mangrove PC1 (Expl. var. = 75%)

Expl. covar. (SVD1) = 94.5%

0

0.02

0.04

0.06

0.08

-0.02

0.1

0

0.04

0.02

0

0.02

0

0

0.04

70° 10°20°30°40°50°60°

70°

60°

50°

40°

30°

20°

10°

Wave heights EOF1 (Expl. var. = 73%)

►The NAO is the dominant mode of climate variability in the North Atlantic-European region. It is characterized by a large-scale seesaw pattern of sea-level pressure anomalies between the Azores High and Icelandic Low (bottom right hand corner).

►The North Atlantic trade winds are strongly coupled to the winter NAO, which leads to strengthening (weakening) wave heights during positive-NAO (negative-NAO) phases.

► Increased (decreased) wave heights favour mangrove shoreline landward (seaward) retreat (expansion).

HS NAO MS

Walcker, R., Anthony, E. J., Cassou, C., Aller, R. C., Gardel, A., Proisy, C., Martinez, J-M. & Fromard, F. (in press) Fluctuations in the extent of mangroves driven by multi-decadal changes in North Atlantic waves. Journal of Biogeography.

Mangroves are uprooted by waves

1950 20141975

We mapped changes in mangrove extent using archival remote sensing images from 1950 to 2014 in French Guiana

40

50

1950 1960 1970 1980 1990 2000 2010

Total mangrove extent (ha×10³)60

Mangrove extent

Spot cnes 2010/09/2710 km SPOT 28/02/2009

Wave exposed zoneMud bank

Amazon turbid plume

Mangrove extent

Amazone estuary

Mud bank (>340Mt)

754 Mt.an−1

150 Mt.an−1

Atlantic ocean

Brazil

Guyana

Suriname

Venezuela

FrenchGuiana

Amazon turbid plume

Amazon sediment dispersal system

We studied the natural 300-km-open coast mangrove system of French Guiana (South America)

Control of mangrove abundance by decadal changes in oceanic wave �eldsRomain Walcker, François Fromard

EcoLab (Laboratoire Ecologie Fonctionnelle et Environnement) UMR 5245 (CNRS, UPS, INP), 118 route de Narbonne, 31062 Toulouse, [email protected] & [email protected]

► The North Atlantic Oscillation (NAO) controls mangrove forest expansion and retreat in French Guiana (South America).► This mechanism operates through wave pounding, which alters the mud substrates on which mangroves thrive.► Wave pounding increases (decreases) during positive (negative) phases of the NAO.► Over the 65 last years in French Guiana, mean winter wave heights fluctuated between 1.6m and 2.2m, leading to changes in mangrove extent of ± 15 000 ha.

Our Common Future Under Climate Change - International Scienti�c Conference 7-10 July 2015 Paris, France

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