On the temporal clustering of US floods and its relationship to climate teleconnection patterns

Abstract This article examines whether the temporal clustering of flood events can be explained in terms of climate variability or time‐varying land‐surface state variables. The point process modelling framework for flood occurrence is based on Cox processes, which can be represented as Poisson proc...

Full description

Bibliographic Details
Published in:International Journal of Climatology
Main Authors: Villarini, Gabriele, Smith, James A., Vitolo, Renato, Stephenson, David B.
Other Authors: Willis Research Network
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2012
Subjects:
Online Access:http://dx.doi.org/10.1002/joc.3458
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fjoc.3458
https://rmets.onlinelibrary.wiley.com/doi/pdf/10.1002/joc.3458
id crwiley:10.1002/joc.3458
record_format openpolar
spelling crwiley:10.1002/joc.3458 2024-06-23T07:55:11+00:00 On the temporal clustering of US floods and its relationship to climate teleconnection patterns Villarini, Gabriele Smith, James A. Vitolo, Renato Stephenson, David B. Willis Research Network 2012 http://dx.doi.org/10.1002/joc.3458 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fjoc.3458 https://rmets.onlinelibrary.wiley.com/doi/pdf/10.1002/joc.3458 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor International Journal of Climatology volume 33, issue 3, page 629-640 ISSN 0899-8418 1097-0088 journal-article 2012 crwiley https://doi.org/10.1002/joc.3458 2024-06-13T04:23:06Z Abstract This article examines whether the temporal clustering of flood events can be explained in terms of climate variability or time‐varying land‐surface state variables. The point process modelling framework for flood occurrence is based on Cox processes, which can be represented as Poisson processes with randomly varying rate of occurrence. In the special case that the rate of occurrence is deterministic, the Cox process simplifies to a Poisson process. Poisson processes represent flood occurrences which are not clustered. The Cox regression model is used to examine the dependence of the rate of occurrence on covariate processes. We focus on 41 stream gauge stations in Iowa, with discharge records covering the period 1950–2009. The climate covariates used in this study are the North Atlantic Oscillation (NAO) and the Pacific/North American Teleconnection (PNA). To examine the influence of land‐surface forcing on flood occurrence, the antecedent 30 d rainfall accumulation is considered. In 27 out of 41 stations, either PNA or NAO, or both are selected as significant predictors, suggesting that flood occurrence in Iowa is influenced by large‐scale climate indices. Antecedent rainfall, used as a proxy for soil moisture, plays an important role in driving the occurrence of flooding in Iowa. These results point to clustering as an important element of the flood occurrence process. Copyright © 2012 Royal Meteorological Society Article in Journal/Newspaper North Atlantic North Atlantic oscillation Wiley Online Library Pacific International Journal of Climatology 33 3 629 640
institution Open Polar
collection Wiley Online Library
op_collection_id crwiley
language English
description Abstract This article examines whether the temporal clustering of flood events can be explained in terms of climate variability or time‐varying land‐surface state variables. The point process modelling framework for flood occurrence is based on Cox processes, which can be represented as Poisson processes with randomly varying rate of occurrence. In the special case that the rate of occurrence is deterministic, the Cox process simplifies to a Poisson process. Poisson processes represent flood occurrences which are not clustered. The Cox regression model is used to examine the dependence of the rate of occurrence on covariate processes. We focus on 41 stream gauge stations in Iowa, with discharge records covering the period 1950–2009. The climate covariates used in this study are the North Atlantic Oscillation (NAO) and the Pacific/North American Teleconnection (PNA). To examine the influence of land‐surface forcing on flood occurrence, the antecedent 30 d rainfall accumulation is considered. In 27 out of 41 stations, either PNA or NAO, or both are selected as significant predictors, suggesting that flood occurrence in Iowa is influenced by large‐scale climate indices. Antecedent rainfall, used as a proxy for soil moisture, plays an important role in driving the occurrence of flooding in Iowa. These results point to clustering as an important element of the flood occurrence process. Copyright © 2012 Royal Meteorological Society
author2 Willis Research Network
format Article in Journal/Newspaper
author Villarini, Gabriele
Smith, James A.
Vitolo, Renato
Stephenson, David B.
spellingShingle Villarini, Gabriele
Smith, James A.
Vitolo, Renato
Stephenson, David B.
On the temporal clustering of US floods and its relationship to climate teleconnection patterns
author_facet Villarini, Gabriele
Smith, James A.
Vitolo, Renato
Stephenson, David B.
author_sort Villarini, Gabriele
title On the temporal clustering of US floods and its relationship to climate teleconnection patterns
title_short On the temporal clustering of US floods and its relationship to climate teleconnection patterns
title_full On the temporal clustering of US floods and its relationship to climate teleconnection patterns
title_fullStr On the temporal clustering of US floods and its relationship to climate teleconnection patterns
title_full_unstemmed On the temporal clustering of US floods and its relationship to climate teleconnection patterns
title_sort on the temporal clustering of us floods and its relationship to climate teleconnection patterns
publisher Wiley
publishDate 2012
url http://dx.doi.org/10.1002/joc.3458
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fjoc.3458
https://rmets.onlinelibrary.wiley.com/doi/pdf/10.1002/joc.3458
geographic Pacific
geographic_facet Pacific
genre North Atlantic
North Atlantic oscillation
genre_facet North Atlantic
North Atlantic oscillation
op_source International Journal of Climatology
volume 33, issue 3, page 629-640
ISSN 0899-8418 1097-0088
op_rights http://onlinelibrary.wiley.com/termsAndConditions#vor
op_doi https://doi.org/10.1002/joc.3458
container_title International Journal of Climatology
container_volume 33
container_issue 3
container_start_page 629
op_container_end_page 640
_version_ 1802647665811390464