

FOLLOWUS
1.South China Sea Information Center of State Oceanic Administration, Guangzhou 510310, China
2.Key Laboratory of Marine Environmental Survey Technology and Application, Ministry of Natural Resources, Guangzhou 510300, China
3.South China Sea Marine Surveying and Technology Center, State Ocean Administration, Guangzhou 510300, China
huangcj@scs.mnr.gov.cn
收稿:2022-01-30,
网络首发:2022-08-22,
纸质出版:2023-03-01
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Applicability evaluation of ERA5 wind and wave reanalysis data in the South China Sea[J]. 海洋湖沼学报(英文), 2023,41(2):495-517.
ZHAI Rongwei,HUANG Caijing,YANG Wei,et al.Applicability evaluation of ERA5 wind and wave reanalysis data in the South China Sea[J].Journal of Oceanology and Limnology,2023,41(02):495-517.
Applicability evaluation of ERA5 wind and wave reanalysis data in the South China Sea[J]. 海洋湖沼学报(英文), 2023,41(2):495-517. DOI:
ZHAI Rongwei,HUANG Caijing,YANG Wei,et al.Applicability evaluation of ERA5 wind and wave reanalysis data in the South China Sea[J].Journal of Oceanology and Limnology,2023,41(02):495-517. DOI:
Wind and wave data are essential in climatological and engineering design applications. In this study
data from 15 buoys located throughout the South China Sea (SCS) were used to evaluate the ERA5 wind and wave data. Applicability assessment are beneficial for gaining insight into the reliability of the ERA5 data in the SCS. The bias range between the ERA5 and observed wind-speed data was -0.78–0.99 m/s. The result indicates that
while the ERA5 wind-speed data underestimation was dominate
the overestimation of such data existed as well. Additionally
the ERA5 data underestimated annual maximum wind-speed by up to 38%
with a correlation coefficient >0.87. The bias between the ERA5 and observed significant wave height (SWH) data varied from -0.24 to 0.28 m. And the ERA5 data showed positive SWH bias
which implied a general underestimation at all locations
except those in the Beibu Gulf and central-western SCS
where overestimation was observed. Under extreme conditions
annual maximum SWH in the ERA5 data was underestimated by up to 30%. The correlation coefficients between the ERA5 and observed SWH data at all locations were greater than 0.92
except in the central-western SCS (0.84). The bias between the ERA5 and observed mean wave period (MWP) data varied from -0.74 to 0.57 s. The ERA5 data showed negative MWP biases implying a general overestimation at all locations
except for B1 (the Beibu Gulf) and B7 (the northeastern SCS)
where underestimation was observed. The correlation coefficient between the ERA5 and observed MWP data in the Beibu Gulf was the smallest (0.56)
and those of other locations fluctuated within a narrow range from 0.82 to 0.90. The intercomparison indicates that during the analyzed time-span
the ERA5 data generally underestimated wind-speed and SWH
but overestimated MWP. Under non-extreme conditions
the ERA5 wind-speed and SWH data can be used with confidence in most regions of the SCS
except in the central-western SCS.
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