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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Main Authors: Jingxiang Shu, Asaad Y. Shamseldin, Evan Weller
Format: Article
Language:English
Published: Nature Publishing Group 2021-03-01
Series:Scientific Reports
Online Access:https://doi.org/10.1038/s41598-021-85297-0
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spelling 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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