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.
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页数:15
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