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DOI10.1002/joc.5380
Storm wave clustering around New Zealand and its connection to climatic patterns
Godoi, Victor A.1; Bryan, Karin R.1; Gorman, Richard M.2
2018-04-01
发表期刊INTERNATIONAL JOURNAL OF CLIMATOLOGY
ISSN0899-8418
EISSN1097-0088
出版年2018
卷号38页码:E401-E417
文章类型Article
语种英语
国家New Zealand
英文摘要

Clusters of storm waves contribute disproportionately to coastal erosion hazards because the coastline has insufficient time to recover between events. Here, the change in occurrence of clustered storms and its association with atmospheric oscillation modes were investigated in New Zealand waters using 44 years (1958-2001) of wave hindcast data. First, long-term averages of cluster parameters (number of storms within the cluster, potential for coastal erosion, and cluster duration) were assessed. Then, the relationships between clustering and the El Nino-Southern Oscillation (ENSO), Indian Ocean Dipole (IOD), Zonal Wavenumber-3 Pattern (ZW3), Pacific Decadal Oscillation (PDO), and Southern Annular Mode (SAM) were explored through correlation analysis over several timescales. Clusters were more frequently observed to the northeast of New Zealand and on the central eastern coast of the South Island. The most vulnerable regions to cluster-induced coastal erosion were southern New Zealand and the northwestern coast, which resulted from steady southwesterly swells, although clusters with the longest duration occurred on the east coast of the South Island. Trends suggest that clusters have incorporated more storms, have become more hazardous, and have increased in duration, particularly along the South Island coastline. Although these trends may be sensitive to the reanalysed wind fields used to force the wave hindcast, they reflect trends in the ENSO, PDO, and SAM. Stronger southwesterly winds during El Nino (negative ENSO) and El Nino-like conditions (positive IOD/PDO) generated more clustered storms mainly on the southwestern coast of New Zealand, whereas increases in clustering were observed on the north coast during La Nina and La Nina-like conditions (stronger northeasterly winds). Higher occurrence of clustering was also evident on the west coast during the strong atmospheric zonal flow associated with negative ZW3. Lastly, strengthened westerlies related to positive SAM led to increased clustering primarily to the south of New Zealand.


英文关键词storm wave clustering storm grouping climate patterns climate change coastal hazard New Zealand wave hindcasting
领域气候变化
收录类别SCI-E
WOS记录号WOS:000431999600028
WOS关键词SOUTHERN ANNULAR MODE ; EL-NINO EVENTS ; INDIAN-OCEAN ; EMBAYED BEACHES ; PACIFIC-OCEAN ; VARIABILITY ; HEMISPHERE ; OSCILLATION ; TRENDS ; CIRCULATION
WOS类目Meteorology & Atmospheric Sciences
WOS研究方向Meteorology & Atmospheric Sciences
引用统计
被引频次:12[WOS]   [WOS记录]     [WOS相关记录]
文献类型期刊论文
条目标识符http://119.78.100.173/C666/handle/2XK7JSWQ/37514
专题气候变化
作者单位1.Univ Waikato, Sch Sci, Hillcrest Rd, Hamilton 3216, Waikato, New Zealand;
2.Natl Inst Water & Atmospher Res, Hamilton, New Zealand
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Godoi, Victor A.,Bryan, Karin R.,Gorman, Richard M.. Storm wave clustering around New Zealand and its connection to climatic patterns[J]. INTERNATIONAL JOURNAL OF CLIMATOLOGY,2018,38:E401-E417.
APA Godoi, Victor A.,Bryan, Karin R.,&Gorman, Richard M..(2018).Storm wave clustering around New Zealand and its connection to climatic patterns.INTERNATIONAL JOURNAL OF CLIMATOLOGY,38,E401-E417.
MLA Godoi, Victor A.,et al."Storm wave clustering around New Zealand and its connection to climatic patterns".INTERNATIONAL JOURNAL OF CLIMATOLOGY 38(2018):E401-E417.
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