Grid-Point Rainfall Trends, Teleconnection Patterns, and Regionalised Droughts in Portugal (1919–2019)
This paper describes the long-term grid-point rainfall trends in the context of climate change, recent regionalised rainfall decline and drought events for mainland Portugal, which is teleconnected, in most cases, to the trends of mathematical descriptions of the North Atlantic Oscillation (NAO) dur...
Published in: | Water |
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Main Authors: | , |
Format: | Text |
Language: | English |
Published: |
Multidisciplinary Digital Publishing Institute
2022
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Subjects: | |
Online Access: | https://doi.org/10.3390/w14121863 |
_version_ | 1821647177261252608 |
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author | Luis Angel Espinosa Maria Manuela Portela |
author_facet | Luis Angel Espinosa Maria Manuela Portela |
author_sort | Luis Angel Espinosa |
collection | MDPI Open Access Publishing |
container_issue | 12 |
container_start_page | 1863 |
container_title | Water |
container_volume | 14 |
description | This paper describes the long-term grid-point rainfall trends in the context of climate change, recent regionalised rainfall decline and drought events for mainland Portugal, which is teleconnected, in most cases, to the trends of mathematical descriptions of the North Atlantic Oscillation (NAO) during the century from October 1919 to September 2019. Grid-point rainfall dataset (1919–2019, from 126 centroids in a regular mesh over the country) have been constructed from high-quality ground-based data and as such, it provides a reliable source for the analysis of rainfall trends at different timescales: October–December, January–March, December–March, and the hydrological year. The Mann–Kendall (MK) coupled with Sen’s slope estimator test are applied to quantify the trends. The Sequential Mann–Kendall (SQMK) analysis is implemented to obtain the fluctuation of the progressive trends along the studied 100-year period. Because of their pivotal role in linking and synchronising climate variability, teleconnections to the North Atlantic Ocean are also explored to explain the rainfall trends over the Portuguese continuum. The results provide a solid basis to explain the climate change effects on the Portuguese rainfall based on significant associations with strong negative correlations between changes in rainfall and in NAO indices. These strong opposing correlations are displayed in most of the winter seasons and in the year. After the late 1960s, a generalised rainfall decrease emerges against a background of significant upward trends of the NAO; such coupled behaviour has persisted for decades. Regionalised droughts at three identified climatic regions, based on factor analysis and Standardised Precipitation Index (SPI), are also discussed, concluding that the frequency of severe droughts may increase again, accompanied by a stronger influence of the recently more positive and unusual winter season and annual NAO indices. |
format | Text |
genre | North Atlantic North Atlantic oscillation |
genre_facet | North Atlantic North Atlantic oscillation |
geographic | Kendall |
geographic_facet | Kendall |
id | ftmdpi:oai:mdpi.com:/2073-4441/14/12/1863/ |
institution | Open Polar |
language | English |
long_lat | ENVELOPE(-59.828,-59.828,-63.497,-63.497) |
op_collection_id | ftmdpi |
op_coverage | agris |
op_doi | https://doi.org/10.3390/w14121863 |
op_relation | Hydrology https://dx.doi.org/10.3390/w14121863 |
op_rights | https://creativecommons.org/licenses/by/4.0/ |
op_source | Water; Volume 14; Issue 12; Pages: 1863 |
publishDate | 2022 |
publisher | Multidisciplinary Digital Publishing Institute |
record_format | openpolar |
spelling | ftmdpi:oai:mdpi.com:/2073-4441/14/12/1863/ 2025-01-16T23:38:33+00:00 Grid-Point Rainfall Trends, Teleconnection Patterns, and Regionalised Droughts in Portugal (1919–2019) Luis Angel Espinosa Maria Manuela Portela agris 2022-06-10 application/pdf https://doi.org/10.3390/w14121863 EN eng Multidisciplinary Digital Publishing Institute Hydrology https://dx.doi.org/10.3390/w14121863 https://creativecommons.org/licenses/by/4.0/ Water; Volume 14; Issue 12; Pages: 1863 climate change rainfall trends teleconnection regionalised drought SPI Portugal Text 2022 ftmdpi https://doi.org/10.3390/w14121863 2023-08-01T05:20:03Z This paper describes the long-term grid-point rainfall trends in the context of climate change, recent regionalised rainfall decline and drought events for mainland Portugal, which is teleconnected, in most cases, to the trends of mathematical descriptions of the North Atlantic Oscillation (NAO) during the century from October 1919 to September 2019. Grid-point rainfall dataset (1919–2019, from 126 centroids in a regular mesh over the country) have been constructed from high-quality ground-based data and as such, it provides a reliable source for the analysis of rainfall trends at different timescales: October–December, January–March, December–March, and the hydrological year. The Mann–Kendall (MK) coupled with Sen’s slope estimator test are applied to quantify the trends. The Sequential Mann–Kendall (SQMK) analysis is implemented to obtain the fluctuation of the progressive trends along the studied 100-year period. Because of their pivotal role in linking and synchronising climate variability, teleconnections to the North Atlantic Ocean are also explored to explain the rainfall trends over the Portuguese continuum. The results provide a solid basis to explain the climate change effects on the Portuguese rainfall based on significant associations with strong negative correlations between changes in rainfall and in NAO indices. These strong opposing correlations are displayed in most of the winter seasons and in the year. After the late 1960s, a generalised rainfall decrease emerges against a background of significant upward trends of the NAO; such coupled behaviour has persisted for decades. Regionalised droughts at three identified climatic regions, based on factor analysis and Standardised Precipitation Index (SPI), are also discussed, concluding that the frequency of severe droughts may increase again, accompanied by a stronger influence of the recently more positive and unusual winter season and annual NAO indices. Text North Atlantic North Atlantic oscillation MDPI Open Access Publishing Kendall ENVELOPE(-59.828,-59.828,-63.497,-63.497) Water 14 12 1863 |
spellingShingle | climate change rainfall trends teleconnection regionalised drought SPI Portugal Luis Angel Espinosa Maria Manuela Portela Grid-Point Rainfall Trends, Teleconnection Patterns, and Regionalised Droughts in Portugal (1919–2019) |
title | Grid-Point Rainfall Trends, Teleconnection Patterns, and Regionalised Droughts in Portugal (1919–2019) |
title_full | Grid-Point Rainfall Trends, Teleconnection Patterns, and Regionalised Droughts in Portugal (1919–2019) |
title_fullStr | Grid-Point Rainfall Trends, Teleconnection Patterns, and Regionalised Droughts in Portugal (1919–2019) |
title_full_unstemmed | Grid-Point Rainfall Trends, Teleconnection Patterns, and Regionalised Droughts in Portugal (1919–2019) |
title_short | Grid-Point Rainfall Trends, Teleconnection Patterns, and Regionalised Droughts in Portugal (1919–2019) |
title_sort | grid-point rainfall trends, teleconnection patterns, and regionalised droughts in portugal (1919–2019) |
topic | climate change rainfall trends teleconnection regionalised drought SPI Portugal |
topic_facet | climate change rainfall trends teleconnection regionalised drought SPI Portugal |
url | https://doi.org/10.3390/w14121863 |