Sea level variability in Gulf of Guinea from satellite altimetry

被引:4
作者
Ghomsi, Franck Eitel Kemgang [1 ,2 ,3 ]
Raj, Roshin P. [4 ,5 ]
Bonaduce, Antonio [4 ,5 ]
Halo, Issufo [3 ,6 ]
Nyberg, Bjoern [7 ]
Cazenave, Anny [8 ]
Rouault, Mathieu [1 ,3 ]
Johannessen, Ola M. [9 ]
机构
[1] Univ Cape Town, Dept Oceanog, Cape Town, South Africa
[2] Natl Inst Cartog, Geodesy Res Lab, POB 157, Yaounde, Cameroon
[3] Univ Cape Town, Nansen Tutu Ctr Marine Environm Res, Cape Town, South Africa
[4] Nansen Environm & Remote Sensing Ctr, Bergen, Norway
[5] Bjerknes Ctr Climate Res, Bergen, Norway
[6] Dept Forestry Fisheries & Environm, Oceans & Coasts Res, Cape Town, South Africa
[7] 7Analytics, Innovat Dist Solheimsviken 7c, N-5054 Bergen, Norway
[8] 18 Av E Belin, F-31401 Toulouse 9, France
[9] Nansen Sci Soc, Bergen, Norway
关键词
COASTAL-TRAPPED WAVES; TROPICAL ATLANTIC; EQUATORIAL ATLANTIC; PACIFIC; WARM; SURFACE; NINO; PROPAGATIONS; EVOLUTION; EVENTS;
D O I
10.1038/s41598-024-55170-x
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
Coastal zones with dense populations, low elevations and/or inadequate adaptive capacity are on the frontline of unprecedented impacts from climate change. The Gulf of Guinea (GoG), stretching from Liberia to Gabon, is in particular vulnerable to coastal flooding caused by local and/or climate-induced sea level rise. In this region, interannual to decadal coastal sea level changes remain poorly understood, mainly due to a lack of tide gauge stations. Here we use nearly three decades (1993-2021) of satellite altimetry data to study the link between the Equatorial Atlantic and coastal GoG sea level variability. The rate of mean sea level rise increased from 3.47 to 3.89 +/- 0.10 mm/yr from the Equatorial oceanic domain to the GoG coastal area, with an acceleration of 0.094 +/- 0.050 mm/yr2. This corresponds to a mean sea level rise of about 8.9 cm over the entire altimetry period, 1993-2021. We focus on the (extreme) warm/cold events that occur in both the GoG during Atlantic Ninos, and along the Angola-Namibia coast during Benguela Ninos. Both events are driven by remote forcing via equatorial Kelvin waves and local forcing by local winds, freshwater fluxes and currents intensifications. Analysis of altimetry-based sea level, sea surface temperature anomalies, 20 degrees C isotherm based PIRATA moorings, and the Argo-based steric and thermometric sea level allows us to follow the coastal trapped waves (CTWs) along the GoG, and its link with major events observed along the strong Equatorial Atlantic warmings in 2010, 2012, 2019 and 2021. Both 2019 and 2021 warming have been identified as the warmest event ever reported in this region during the last 40 years. A lag of 1 month is observed between equatorial and West African coastal trapped wave propagation. This observation may help to better anticipate and manage the effects of extreme events on local ecosystems, fisheries, and socio-economic activities along the affected coastlines. In order to enable informed decision-making and guarantee the resilience of coastal communities in the face of climate change, it emphasises the significance of ongoing study in this field.
引用
收藏
页数:15
相关论文
共 89 条
  • [1] Uncertainty in satellite estimates of global mean sea-level changes, trend and acceleration
    Ablain, Michael
    Meyssignac, Benoit
    Zawadzki, Lionel
    Jugier, Remi
    Ribes, Aurelien
    Spada, Giorgio
    Benveniste, Jerome
    Cazenave, Anny
    Picot, Nicolas
    [J]. EARTH SYSTEM SCIENCE DATA, 2019, 11 (03) : 1189 - 1202
  • [2] A global analysis of extreme coastal water levels with implications for potential coastal overtopping
    Almar, Rafael
    Ranasinghe, Roshanka
    Bergsma, Erwin W. J.
    Diaz, Harold
    Melet, Angelique
    Papa, Fabrice
    Vousdoukas, Michalis
    Athanasiou, Panagiotis
    Dada, Olusegun
    Almeida, Luis Pedro
    Kestenare, Elodie
    [J]. NATURE COMMUNICATIONS, 2021, 12 (01)
  • [3] Influence of sea level variability on a micro-tidal beach
    Angnuureng, D. B.
    Addo, K. Appeaning
    Almar, R.
    Dieng, H.
    [J]. NATURAL HAZARDS, 2018, 93 (03) : 1611 - 1628
  • [4] TROPICAL ATLANTIC SEA-LEVEL VARIABILITY FROM GEOSAT (1985-1989)
    ARNAULT, S
    CHENEY, RE
    [J]. JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS, 1994, 99 (C9) : 18207 - 18223
  • [5] Sea Surface Salinity Signature of the Tropical Atlantic Interannual Climatic Modes
    Awo, F. M.
    Alory, G.
    Da-Allada, C. Y.
    Delcroix, T.
    Jouanno, J.
    Kestenare, E.
    Baloitcha, E.
    [J]. JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS, 2018, 123 (10) : 7420 - 7437
  • [6] Mechanism of generation and propagation characteristics of coastal trapped waves in the Black Sea
    Aydin, Mujdat
    Besiktepe, Sukru Turan
    [J]. OCEAN SCIENCE, 2022, 18 (04) : 1081 - 1091
  • [7] Bissolli P, 2022, B AM METEOROL SOC, V103, pS348
  • [8] Physical processes and biological productivity in the upwelling regions ofthe tropical Atlantic
    Brandt, Peter
    Alory, Gael
    Awo, Founi Mesmin
    Dengler, Marcus
    Djakoure, Sandrine
    Koungue, Rodrigue Anicet Imbol
    Jouanno, Julien
    Koerner, Mareike
    Roch, Marisa
    Rouault, Mathieu
    [J]. OCEAN SCIENCE, 2023, 19 (03) : 581 - 601
  • [9] Equatorial upper-ocean dynamics and their interaction with the West African monsoon
    Brandt, Peter
    Caniaux, Guy
    Bourles, Bernard
    Lazar, Alban
    Dengler, Marcus
    Funk, Andreas
    Hormann, Verena
    Giordani, Herve
    Marin, Frederic
    [J]. ATMOSPHERIC SCIENCE LETTERS, 2011, 12 (01): : 24 - 30
  • [10] Casas NM., 2022, CLIMATE FINANCE W AF, DOI [10.21201/2022.9363, DOI 10.21201/2022.9363]