The impact of atmospheric teleconnections on the coastal aquifers of Ria Formosa (Algarve, Portugal)

Fluctuations in groundwater level in the Ria Formosa coastal aquifers, southern Portugal, owe 80% of the variability to climate-induced oscillations. Wavelet coherences computed between hydraulic heads and the North Atlantic Oscillation (NAO) and East Atlantic (EA) atmospheric teleconnections show n...

Full description

Bibliographic Details
Published in:Hydrogeology Journal
Main Authors: C. Neves, Maria, Costa, Luis, Hugman, Rui, P. Monteiro, J.
Format: Article in Journal/Newspaper
Language:English
Published: Springer 2019
Subjects:
Nao
Online Access:http://hdl.handle.net/10400.1/14176
https://doi.org/10.1007/s10040-019-02052-6
id ftunivalgarve:oai:sapientia.ualg.pt:10400.1/14176
record_format openpolar
spelling ftunivalgarve:oai:sapientia.ualg.pt:10400.1/14176 2023-05-15T17:35:40+02:00 The impact of atmospheric teleconnections on the coastal aquifers of Ria Formosa (Algarve, Portugal) C. Neves, Maria Costa, Luis Hugman, Rui P. Monteiro, J. 2019-11 http://hdl.handle.net/10400.1/14176 https://doi.org/10.1007/s10040-019-02052-6 eng eng Springer 1431-2174 http://hdl.handle.net/10400.1/14176 doi:10.1007/s10040-019-02052-6 restrictedAccess Groundwater level response Iberian Peninsula Precipitation Water Variability Circulation Patterns Nao Vulnerability Resources Groundwater level Portugal Coastal aquifers Over-abstraction Climate article 2019 ftunivalgarve https://doi.org/10.1007/s10040-019-02052-6 2022-05-30T08:49:12Z Fluctuations in groundwater level in the Ria Formosa coastal aquifers, southern Portugal, owe 80% of the variability to climate-induced oscillations. Wavelet coherences computed between hydraulic heads and the North Atlantic Oscillation (NAO) and East Atlantic (EA) atmospheric teleconnections show nonstationary and spatially varying relationships. The NAO is the most important teleconnection and the main driver of long-term variability, inducing cycle periods of 6-10 years. The NAO fingerprint is ubiquitous and it accounts for nearly 50% of the total variance of groundwater levels. The influence of EA emerges coupled to NAO and is mainly associated with oscillations in the 2-4-year band. These cycles contribute to less than 5% of the variance in groundwater levels and are more evident further from the coast, in the northern part of the system near the main recharge area. Inversely, the power of the annual cycle increases towards the shoreline. The weight of the annual cycle (related to direct recharge) is greatest in the Campina de Faro aquifer, where it is responsible for 20-50% of the variance of piezometric levels. There, signals linked to atmospheric teleconnections (related to regional recharge) are low-pass filtered and have periods >8 years. This behavior (lack of power in the 2-8-year band) emphasizes the vulnerability of coastal groundwater levels to multi-year droughts, particularly in the already stressed Quinta do Lago region, where hydraulic heads are persistently below sea level. FCTPortuguese Foundation for Science and Technology [UID/GEO/50019/2019] Fundacao para a Ciencia e Tecnologia (FCT)Portuguese Foundation for Science and Technology [SFRH/BD/131568/2017] info:eu-repo/semantics/publishedVersion Article in Journal/Newspaper North Atlantic North Atlantic oscillation Universidade do Algarve: Sapienta Hydrogeology Journal 27 8 2775 2787
institution Open Polar
collection Universidade do Algarve: Sapienta
op_collection_id ftunivalgarve
language English
topic Groundwater level response
Iberian Peninsula
Precipitation
Water
Variability
Circulation
Patterns
Nao
Vulnerability
Resources
Groundwater level
Portugal
Coastal aquifers
Over-abstraction
Climate
spellingShingle Groundwater level response
Iberian Peninsula
Precipitation
Water
Variability
Circulation
Patterns
Nao
Vulnerability
Resources
Groundwater level
Portugal
Coastal aquifers
Over-abstraction
Climate
C. Neves, Maria
Costa, Luis
Hugman, Rui
P. Monteiro, J.
The impact of atmospheric teleconnections on the coastal aquifers of Ria Formosa (Algarve, Portugal)
topic_facet Groundwater level response
Iberian Peninsula
Precipitation
Water
Variability
Circulation
Patterns
Nao
Vulnerability
Resources
Groundwater level
Portugal
Coastal aquifers
Over-abstraction
Climate
description Fluctuations in groundwater level in the Ria Formosa coastal aquifers, southern Portugal, owe 80% of the variability to climate-induced oscillations. Wavelet coherences computed between hydraulic heads and the North Atlantic Oscillation (NAO) and East Atlantic (EA) atmospheric teleconnections show nonstationary and spatially varying relationships. The NAO is the most important teleconnection and the main driver of long-term variability, inducing cycle periods of 6-10 years. The NAO fingerprint is ubiquitous and it accounts for nearly 50% of the total variance of groundwater levels. The influence of EA emerges coupled to NAO and is mainly associated with oscillations in the 2-4-year band. These cycles contribute to less than 5% of the variance in groundwater levels and are more evident further from the coast, in the northern part of the system near the main recharge area. Inversely, the power of the annual cycle increases towards the shoreline. The weight of the annual cycle (related to direct recharge) is greatest in the Campina de Faro aquifer, where it is responsible for 20-50% of the variance of piezometric levels. There, signals linked to atmospheric teleconnections (related to regional recharge) are low-pass filtered and have periods >8 years. This behavior (lack of power in the 2-8-year band) emphasizes the vulnerability of coastal groundwater levels to multi-year droughts, particularly in the already stressed Quinta do Lago region, where hydraulic heads are persistently below sea level. FCTPortuguese Foundation for Science and Technology [UID/GEO/50019/2019] Fundacao para a Ciencia e Tecnologia (FCT)Portuguese Foundation for Science and Technology [SFRH/BD/131568/2017] info:eu-repo/semantics/publishedVersion
format Article in Journal/Newspaper
author C. Neves, Maria
Costa, Luis
Hugman, Rui
P. Monteiro, J.
author_facet C. Neves, Maria
Costa, Luis
Hugman, Rui
P. Monteiro, J.
author_sort C. Neves, Maria
title The impact of atmospheric teleconnections on the coastal aquifers of Ria Formosa (Algarve, Portugal)
title_short The impact of atmospheric teleconnections on the coastal aquifers of Ria Formosa (Algarve, Portugal)
title_full The impact of atmospheric teleconnections on the coastal aquifers of Ria Formosa (Algarve, Portugal)
title_fullStr The impact of atmospheric teleconnections on the coastal aquifers of Ria Formosa (Algarve, Portugal)
title_full_unstemmed The impact of atmospheric teleconnections on the coastal aquifers of Ria Formosa (Algarve, Portugal)
title_sort impact of atmospheric teleconnections on the coastal aquifers of ria formosa (algarve, portugal)
publisher Springer
publishDate 2019
url http://hdl.handle.net/10400.1/14176
https://doi.org/10.1007/s10040-019-02052-6
genre North Atlantic
North Atlantic oscillation
genre_facet North Atlantic
North Atlantic oscillation
op_relation 1431-2174
http://hdl.handle.net/10400.1/14176
doi:10.1007/s10040-019-02052-6
op_rights restrictedAccess
op_doi https://doi.org/10.1007/s10040-019-02052-6
container_title Hydrogeology Journal
container_volume 27
container_issue 8
container_start_page 2775
op_container_end_page 2787
_version_ 1766134894266679296