The impact of atmospheric rivers on rainfall in New Zealand
Abstract This study quantifies the impact of atmospheric rivers (ARs) on rainfall in New Zealand. Using an automated AR detection algorithm, daily rainfall records from 654 rain gauges, and various atmospheric reanalysis datasets, we investigate the climatology of ARs, the characteristics of landfal...
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2021-03-01
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Online Access: | https://doi.org/10.1038/s41598-021-85297-0 |
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doaj-b9fa37ad11d146e89146d2e7e5fd05c42021-03-14T12:16:03ZengNature Publishing GroupScientific Reports2045-23222021-03-0111111110.1038/s41598-021-85297-0The impact of atmospheric rivers on rainfall in New ZealandJingxiang Shu0Asaad Y. Shamseldin1Evan Weller2Department of Civil and Environmental Engineering, The University of AucklandDepartment of Civil and Environmental Engineering, The University of AucklandSchool of Environment, The University of AucklandAbstract This study quantifies the impact of atmospheric rivers (ARs) on rainfall in New Zealand. Using an automated AR detection algorithm, daily rainfall records from 654 rain gauges, and various atmospheric reanalysis datasets, we investigate the climatology of ARs, the characteristics of landfalling ARs, the contribution of ARs to annual and seasonal rainfall totals, and extreme rainfall events between 1979 and 2018 across the country. Results indicate that these filamentary synoptic features play an essential role in regional water resources and are responsible for many extreme rainfall events on the western side of mountainous areas and northern New Zealand. In these regions, depending on the season, 40–86% of the rainfall totals and 50–98% of extreme rainfall events are shown to be associated with ARs, with the largest contributions predominantly occurring during the austral summer. Furthermore, the median daily rainfall associated with ARs is 2–3 times than that associated with other storms. The results of this study extend the knowledge on the critical roles of ARs on hydrology and highlight the need for further investigation on the landfalling AR physical processes in relation to global circulation features and AR sources, and hydrological hazards caused by ARs in New Zealand.https://doi.org/10.1038/s41598-021-85297-0 |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Jingxiang Shu Asaad Y. Shamseldin Evan Weller |
spellingShingle |
Jingxiang Shu Asaad Y. Shamseldin Evan Weller The impact of atmospheric rivers on rainfall in New Zealand Scientific Reports |
author_facet |
Jingxiang Shu Asaad Y. Shamseldin Evan Weller |
author_sort |
Jingxiang Shu |
title |
The impact of atmospheric rivers on rainfall in New Zealand |
title_short |
The impact of atmospheric rivers on rainfall in New Zealand |
title_full |
The impact of atmospheric rivers on rainfall in New Zealand |
title_fullStr |
The impact of atmospheric rivers on rainfall in New Zealand |
title_full_unstemmed |
The impact of atmospheric rivers on rainfall in New Zealand |
title_sort |
impact of atmospheric rivers on rainfall in new zealand |
publisher |
Nature Publishing Group |
series |
Scientific Reports |
issn |
2045-2322 |
publishDate |
2021-03-01 |
description |
Abstract This study quantifies the impact of atmospheric rivers (ARs) on rainfall in New Zealand. Using an automated AR detection algorithm, daily rainfall records from 654 rain gauges, and various atmospheric reanalysis datasets, we investigate the climatology of ARs, the characteristics of landfalling ARs, the contribution of ARs to annual and seasonal rainfall totals, and extreme rainfall events between 1979 and 2018 across the country. Results indicate that these filamentary synoptic features play an essential role in regional water resources and are responsible for many extreme rainfall events on the western side of mountainous areas and northern New Zealand. In these regions, depending on the season, 40–86% of the rainfall totals and 50–98% of extreme rainfall events are shown to be associated with ARs, with the largest contributions predominantly occurring during the austral summer. Furthermore, the median daily rainfall associated with ARs is 2–3 times than that associated with other storms. The results of this study extend the knowledge on the critical roles of ARs on hydrology and highlight the need for further investigation on the landfalling AR physical processes in relation to global circulation features and AR sources, and hydrological hazards caused by ARs in New Zealand. |
url |
https://doi.org/10.1038/s41598-021-85297-0 |
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AT jingxiangshu theimpactofatmosphericriversonrainfallinnewzealand AT asaadyshamseldin theimpactofatmosphericriversonrainfallinnewzealand AT evanweller theimpactofatmosphericriversonrainfallinnewzealand AT jingxiangshu impactofatmosphericriversonrainfallinnewzealand AT asaadyshamseldin impactofatmosphericriversonrainfallinnewzealand AT evanweller impactofatmosphericriversonrainfallinnewzealand |
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