2016
DOI: 10.1007/s00382-016-3385-z
|View full text |Cite
|
Sign up to set email alerts
|

Temporal variability in wind–wave climate and its validation with ESSO-NIOT wave atlas for the head Bay of Bengal

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
2
1
1
1

Citation Types

1
12
0

Year Published

2017
2017
2022
2022

Publication Types

Select...
7
1

Relationship

1
7

Authors

Journals

citations
Cited by 39 publications
(14 citation statements)
references
References 14 publications
1
12
0
Order By: Relevance
“…It is evident that, from both the validations, the offshore locations revealed high correlation with the SWAN simulated wave heights. In case of, the near‐shore locations, higher correlations were obtained in comparison with ERA‐Interim data than altimeter data and the results shows good agreement qualitatively with the study reported by Patra and Bhaskaran () for the head Bay region. The study mainly focuses to emphasize the impact of seasonal winds on wave attenuation by mangroves for a mangrove‐dominated region.…”
Section: Resultssupporting
confidence: 88%
“…It is evident that, from both the validations, the offshore locations revealed high correlation with the SWAN simulated wave heights. In case of, the near‐shore locations, higher correlations were obtained in comparison with ERA‐Interim data than altimeter data and the results shows good agreement qualitatively with the study reported by Patra and Bhaskaran () for the head Bay region. The study mainly focuses to emphasize the impact of seasonal winds on wave attenuation by mangroves for a mangrove‐dominated region.…”
Section: Resultssupporting
confidence: 88%
“…Presumably, the main reason to neglect wave period trends is that wave period variations are of little interest for other research areas or industries than wave energy, which is still an immature industry. Some very recent research works study wave period variations by means of statistical models similar to those used in the present paper: wave period trends in the Bay of Bengal are analysed in [23] combining satellite altimeter data with ERA-Interim and ERA-20 reanalyses and the evolution of peak periods and wave heights is studied all over the world in [24]. However, wave period trends are analysed for coastal impact assessment in [23,24], where wave climate variations are rather projected towards the future (1979-2100), instead of studying historical records of the last century, as in the present paper.…”
Section: Literature Reviewmentioning
confidence: 99%
“…Some very recent research works study wave period variations by means of statistical models similar to those used in the present paper: wave period trends in the Bay of Bengal are analysed in [23] combining satellite altimeter data with ERA-Interim and ERA-20 reanalyses and the evolution of peak periods and wave heights is studied all over the world in [24]. However, wave period trends are analysed for coastal impact assessment in [23,24], where wave climate variations are rather projected towards the future (1979-2100), instead of studying historical records of the last century, as in the present paper. Although [24] is a global study, more localised areas, such as Southern Australia and Western South America, are also selected for finer studies.…”
Section: Literature Reviewmentioning
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%