2016
DOI: 10.1016/j.jmarsys.2016.04.005
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Response of waves and coastline evolution to climate variability off the Niger Delta coast during the past 110years

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Cited by 31 publications
(18 citation statements)
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“…The quality of ERA20 data is affected, particularly in regions of sparse observational coverage [51], so it is better in the Northern Hemisphere than in the Southern Hemisphere. However, ERA20 has been used globally in the study of historical wave and coastal evolution [53][54][55]. ERA20's spatial resolution is approximately 125 km and wave parameters can be obtained 3-hourly.…”
Section: Literature Reviewmentioning
confidence: 99%
“…The quality of ERA20 data is affected, particularly in regions of sparse observational coverage [51], so it is better in the Northern Hemisphere than in the Southern Hemisphere. However, ERA20 has been used globally in the study of historical wave and coastal evolution [53][54][55]. ERA20's spatial resolution is approximately 125 km and wave parameters can be obtained 3-hourly.…”
Section: Literature Reviewmentioning
confidence: 99%
“…However, the ERA20 reanalysis has been used in both hemispheres, e.g. for the study of long-term coastal evolution [34,23] and the global study of the relation between historical extreme waves and climate change [35].…”
Section: Wave Datamentioning
confidence: 99%
“…More observations are available, the more reliable are the data generated via the ERA20 reanalysis [34]. Consequently, the data provided by the ERA20 reanalysis are more accurate in the northern hemisphere, although they have also been used for the study of historical wave trends and coastal evolution in different locations of the southern hemisphere [35][36][37]. The spatial resolution of the ERA20 reanalysis is approximately 125 km and wave parameters can be obtained three-hourly [34].…”
Section: Era20c and Era-interim Reanalysesmentioning
confidence: 99%