Identification of a change in climate state using regional flood data
Flood frequency analysis typically assumes that annual floods arise from a single distribution and are independent. However, there is significant evidence for the existence of persistent climate modes. Timescales associated with climate variability range from inter-annual through to longer, multi-de...
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2002-01-01
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Online Access: | http://www.hydrol-earth-syst-sci.net/6/11/2002/hess-6-11-2002.pdf |
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doaj-eee1163aa1be4667bb744afde878c5312020-11-25T00:51:36ZengCopernicus PublicationsHydrology and Earth System Sciences1027-56061607-79382002-01-01611116Identification of a change in climate state using regional flood dataS. W. FranksS. W. FranksFlood frequency analysis typically assumes that annual floods arise from a single distribution and are independent. However, there is significant evidence for the existence of persistent climate modes. Timescales associated with climate variability range from inter-annual through to longer, multi-decadal time scales. In the case of the Australian climate, previous studies of the Indian and Pacific Oceans have indicated marked multi-decadal variability in both mean Sea Surface Temperatures (SST) and typical circulation patterns. In this light, data from 40 stream gauges around New South Wales are examined to determine whether flood frequency data are indeed independent and distributed identically. Given likely correlation in flood records between gauges, an assessment of the regional significance of observed changes in flood frequency is required. To achieve this, flood observations are aggregated into a regional index. A simple non-parametric test is then employed to identify the timing and magnitude of any change in mean annual flood. Finally, it is shown that the identified change in flood frequency corresponds directly to an observed shift in SST and mean circulation. These results demonstrate the role of natural variability in climate parameters and the need for an improved conceptual framework for flood frequency estimation.</p> <p style='line-height: 20px;'><b>Keywords: </b>Floods, flood frequency, climate variability, IPO, PDO, climate changehttp://www.hydrol-earth-syst-sci.net/6/11/2002/hess-6-11-2002.pdf |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
S. W. Franks S. W. Franks |
spellingShingle |
S. W. Franks S. W. Franks Identification of a change in climate state using regional flood data Hydrology and Earth System Sciences |
author_facet |
S. W. Franks S. W. Franks |
author_sort |
S. W. Franks |
title |
Identification of a change in climate state using regional flood data |
title_short |
Identification of a change in climate state using regional flood data |
title_full |
Identification of a change in climate state using regional flood data |
title_fullStr |
Identification of a change in climate state using regional flood data |
title_full_unstemmed |
Identification of a change in climate state using regional flood data |
title_sort |
identification of a change in climate state using regional flood data |
publisher |
Copernicus Publications |
series |
Hydrology and Earth System Sciences |
issn |
1027-5606 1607-7938 |
publishDate |
2002-01-01 |
description |
Flood frequency analysis typically assumes that annual floods arise from a single distribution and are independent. However, there is significant evidence for the existence of persistent climate modes. Timescales associated with climate variability range from inter-annual through to longer, multi-decadal time scales. In the case of the Australian climate, previous studies of the Indian and Pacific Oceans have indicated marked multi-decadal variability in both mean Sea Surface Temperatures (SST) and typical circulation patterns. In this light, data from 40 stream gauges around New South Wales are examined to determine whether flood frequency data are indeed independent and distributed identically. Given likely correlation in flood records between gauges, an assessment of the regional significance of observed changes in flood frequency is required. To achieve this, flood observations are aggregated into a regional index. A simple non-parametric test is then employed to identify the timing and magnitude of any change in mean annual flood. Finally, it is shown that the identified change in flood frequency corresponds directly to an observed shift in SST and mean circulation. These results demonstrate the role of natural variability in climate parameters and the need for an improved conceptual framework for flood frequency estimation.</p> <p style='line-height: 20px;'><b>Keywords: </b>Floods, flood frequency, climate variability, IPO, PDO, climate change |
url |
http://www.hydrol-earth-syst-sci.net/6/11/2002/hess-6-11-2002.pdf |
work_keys_str_mv |
AT swfranks identificationofachangeinclimatestateusingregionalflooddata AT swfranks identificationofachangeinclimatestateusingregionalflooddata |
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1725244914414911488 |