Space-time variability of extreme rainfall in the River Nile basin

KU Leuven IRO PhD scholarship FRIEND/Nile project of UNESCO & Flanders FUST In this study, spatio-temporal variability in daily rainfall extremes based on 0.5∘ × 0.5∘ gridded data over the Nile basin was analysed using the quantile perturbation method. The co-occurrence of the extreme rainfall v...

Full description

Bibliographic Details
Published in:International Journal of Climatology
Main Authors: Onyutha, Charles, Willems, Patrick
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2017
Subjects:
Online Access:https://lirias.kuleuven.be/handle/123456789/584862
https://doi.org/10.1002/joc.5132
https://lirias.kuleuven.be/bitstream/123456789/584862/5//Onyutha-Nilerainfall+%28IJC+2017%29.pdf
id ftunivleuven:oai:lirias.kuleuven.be:123456789/584862
record_format openpolar
spelling ftunivleuven:oai:lirias.kuleuven.be:123456789/584862 2023-05-15T17:33:33+02:00 Space-time variability of extreme rainfall in the River Nile basin Onyutha, Charles Willems, Patrick 2017 3242088 bytes application/pdf https://lirias.kuleuven.be/handle/123456789/584862 https://doi.org/10.1002/joc.5132 https://lirias.kuleuven.be/bitstream/123456789/584862/5//Onyutha-Nilerainfall+%28IJC+2017%29.pdf en eng Wiley International Journal of Climatology vol:37 pages:4915-4924 https://lirias.kuleuven.be/handle/123456789/584862 0899-8418 doi:10.1002/joc.5132 1097-0088 https://lirias.kuleuven.be/bitstream/123456789/584862/5//Onyutha-Nilerainfall+%28IJC+2017%29.pdf 484154;intranet Rainfall Nile basin Climate variability Article IT 484154;Article 2017 ftunivleuven https://doi.org/10.1002/joc.5132 2018-01-06T16:24:11Z KU Leuven IRO PhD scholarship FRIEND/Nile project of UNESCO & Flanders FUST In this study, spatio-temporal variability in daily rainfall extremes based on 0.5∘ × 0.5∘ gridded data over the Nile basin was analysed using the quantile perturbation method. The co-occurrence of the extreme rainfall variability with the variation in the large-scale ocean–atmosphere conditions was also investigated. Based on a 15-year moving window, it was found that the extreme rainfall shows oscillatory behaviour over multi-decadal time scales. The latitudinal difference in the multi-decadal extreme rainfall oscillations divides the study area into the Northern, Central, and Southern regions. The variability in the extreme rainfall of the Central region is dominantly driven by the variation in the sea surface temperatures of the Atlantic and Pacific Oceans. For the Southern region, extreme rainfall variability is linked to the anomalies in the sea level pressure of the North Atlantic Ocean and the variation in the sea surface temperature of the Indian Ocean. The variation in the extreme rainfall of the Northern region corresponds to the anomalies in sea surface temperatures of the Indian and Atlantic Oceans as well as from the Pacific Ocean. status: published Article in Journal/Newspaper North Atlantic KU Leuven: Lirias Indian Pacific International Journal of Climatology 37 14 4915 4924
institution Open Polar
collection KU Leuven: Lirias
op_collection_id ftunivleuven
language English
topic Rainfall
Nile basin
Climate variability
spellingShingle Rainfall
Nile basin
Climate variability
Onyutha, Charles
Willems, Patrick
Space-time variability of extreme rainfall in the River Nile basin
topic_facet Rainfall
Nile basin
Climate variability
description KU Leuven IRO PhD scholarship FRIEND/Nile project of UNESCO & Flanders FUST In this study, spatio-temporal variability in daily rainfall extremes based on 0.5∘ × 0.5∘ gridded data over the Nile basin was analysed using the quantile perturbation method. The co-occurrence of the extreme rainfall variability with the variation in the large-scale ocean–atmosphere conditions was also investigated. Based on a 15-year moving window, it was found that the extreme rainfall shows oscillatory behaviour over multi-decadal time scales. The latitudinal difference in the multi-decadal extreme rainfall oscillations divides the study area into the Northern, Central, and Southern regions. The variability in the extreme rainfall of the Central region is dominantly driven by the variation in the sea surface temperatures of the Atlantic and Pacific Oceans. For the Southern region, extreme rainfall variability is linked to the anomalies in the sea level pressure of the North Atlantic Ocean and the variation in the sea surface temperature of the Indian Ocean. The variation in the extreme rainfall of the Northern region corresponds to the anomalies in sea surface temperatures of the Indian and Atlantic Oceans as well as from the Pacific Ocean. status: published
format Article in Journal/Newspaper
author Onyutha, Charles
Willems, Patrick
author_facet Onyutha, Charles
Willems, Patrick
author_sort Onyutha, Charles
title Space-time variability of extreme rainfall in the River Nile basin
title_short Space-time variability of extreme rainfall in the River Nile basin
title_full Space-time variability of extreme rainfall in the River Nile basin
title_fullStr Space-time variability of extreme rainfall in the River Nile basin
title_full_unstemmed Space-time variability of extreme rainfall in the River Nile basin
title_sort space-time variability of extreme rainfall in the river nile basin
publisher Wiley
publishDate 2017
url https://lirias.kuleuven.be/handle/123456789/584862
https://doi.org/10.1002/joc.5132
https://lirias.kuleuven.be/bitstream/123456789/584862/5//Onyutha-Nilerainfall+%28IJC+2017%29.pdf
geographic Indian
Pacific
geographic_facet Indian
Pacific
genre North Atlantic
genre_facet North Atlantic
op_relation International Journal of Climatology vol:37 pages:4915-4924
https://lirias.kuleuven.be/handle/123456789/584862
0899-8418
doi:10.1002/joc.5132
1097-0088
https://lirias.kuleuven.be/bitstream/123456789/584862/5//Onyutha-Nilerainfall+%28IJC+2017%29.pdf
op_rights 484154;intranet
op_doi https://doi.org/10.1002/joc.5132
container_title International Journal of Climatology
container_volume 37
container_issue 14
container_start_page 4915
op_container_end_page 4924
_version_ 1766132093891379200