4.3 Article

Hourly maximum individual wave height in the Indian shelf seas-its spatial and temporal variations in the recent 40 years

Journal

OCEAN DYNAMICS
Volume 70, Issue 10, Pages 1283-1302

Publisher

SPRINGER HEIDELBERG
DOI: 10.1007/s10236-020-01395-z

Keywords

Climate indices; Maximum wave height; North Indian Ocean; Reanalysis data; Surface waves; Wave climatology

Categories

Funding

  1. Council of Scientific and Industrial Research, New Delhi
  2. Indian National Centre for Ocean Information Services (INCOIS), Ministry of Earth Sciences

Ask authors/readers for more resources

The spatial and temporal variability of the high individual wave heights, which pose a hazard in India's shelf seas, has not been investigated. In this study, the spatial and temporal variation of hourly maximum individual wave height (H-max) in the Indian shelf seas is examined based on 40 years ERA5 Re-Analysis data from European Centre for Medium-Range Weather Forecasts. Waverider buoy data from five locations are used to assess ERA5 H-max. The variability of H(max)in different temporal scales; daily, monthly and interannual and their linkages with major ocean-atmosphere coupled interaction in the Pacific and the Indian Ocean are presented. Wave climatology throughout India's western shelf seas shows average H(max)exceeding 2 m during most of the year. Maximum H(max)in the western shelf seas is during May-July, whereas in the southern tip and the eastern shelf seas are during the tropical cyclones and are either in October-December or May. Maximum H(max)is 17.94 m, and it occurred at the northern Bay of Bengal on 25 May 2009 during the passage of tropical cyclone Aila. Spatial variations in H(max)between locations spaced at 1.5 degrees latitude are less than 10% in the northwestern and southeastern shelf seas, but large variations (similar to 28%) are in the southwestern and northeastern shelf seas. Annual mean H(max)shows contrasting trends when data for 1979 to 2018 and 1992 to 2018 is considered. Indian Ocean Dipole influence on the H(max)suggests negative correlations in the western shelf seas and positive correlations in the eastern shelf seas. The correlation with climate indices is similar for both significant wave height and H-max.

Authors

I am an author on this paper
Click your name to claim this paper and add it to your profile.

Reviews

Primary Rating

4.3
Not enough ratings

Secondary Ratings

Novelty
-
Significance
-
Scientific rigor
-
Rate this paper

Recommended

No Data Available
No Data Available