Rainwater Isotopic Composition in the Ecuadorian Andes and Amazon Reflects Cross-Equatorial Flow Seasonality

The variability of the rainfall stable isotopic values (δ 2 H p, δ 18 O p ) in the Ecuadorian Amazon to the Andes presents a marked local “altitude” effect. At the same time, this complex orography creates diverse precipitation regimes (unimodal, bimodal, and three-modal) that make it difficult to e...

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Published in:Water
Main Authors: Danny Vargas, Oscar Chimborazo, Elemér László, Marjan Temovski, László Palcsu
Format: Article in Journal/Newspaper
Language:English
Published: MDPI AG 2022
Subjects:
Online Access:https://doi.org/10.3390/w14132121
https://doaj.org/article/0f9db46c8df24ed48077db039d1e436d
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spelling ftdoajarticles:oai:doaj.org/article:0f9db46c8df24ed48077db039d1e436d 2023-05-15T17:35:29+02:00 Rainwater Isotopic Composition in the Ecuadorian Andes and Amazon Reflects Cross-Equatorial Flow Seasonality Danny Vargas Oscar Chimborazo Elemér László Marjan Temovski László Palcsu 2022-07-01T00:00:00Z https://doi.org/10.3390/w14132121 https://doaj.org/article/0f9db46c8df24ed48077db039d1e436d EN eng MDPI AG https://www.mdpi.com/2073-4441/14/13/2121 https://doaj.org/toc/2073-4441 doi:10.3390/w14132121 2073-4441 https://doaj.org/article/0f9db46c8df24ed48077db039d1e436d Water, Vol 14, Iss 2121, p 2121 (2022) cross-equatorial flow stable isotopes V-Index low-level jet precipitation aerial lake Hydraulic engineering TC1-978 Water supply for domestic and industrial purposes TD201-500 article 2022 ftdoajarticles https://doi.org/10.3390/w14132121 2022-12-30T22:22:20Z The variability of the rainfall stable isotopic values (δ 2 H p, δ 18 O p ) in the Ecuadorian Amazon to the Andes presents a marked local “altitude” effect. At the same time, this complex orography creates diverse precipitation regimes (unimodal, bimodal, and three-modal) that make it difficult to establish a relationship with the local amount. Nevertheless, stations along these regions show a similar intra-annual isotopic variability, with lower values during MAM and ON. In contrast, higher values are found during DJF and JAS in a w-shaped pattern, suggesting a common regional controller. A monthly δ 2 H p and δ 18 O p collection campaign was established in Central Ecuador ( n = 30) to complement stations biased towards the northern and southern parts. Based on back trajectory analysis, the results demonstrated that moisture arrives from two primary sources: the Tropical North Atlantic (DJFM) and the Amazon Basin (JAS). Nevertheless, their convergence (AMJ and ON) is the crucial factor modulating the lowest isotopic values. Precisely, this convergence is stronger at the V-Index region (5° S–5° N, 65°–75° W), where the wind seasonality and reversal at low levels are enhanced, allowing the inter-hemispheric moisture flux transport (cross-equatorial flow). We propose that the amount of rainfall located at the V-Index region is a more robust approach for explaining the δ 2 H p and δ 18 O p variability rather than the local amount. Article in Journal/Newspaper North Atlantic Directory of Open Access Journals: DOAJ Articles Water 14 13 2121
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic cross-equatorial flow
stable isotopes
V-Index
low-level jet
precipitation
aerial lake
Hydraulic engineering
TC1-978
Water supply for domestic and industrial purposes
TD201-500
spellingShingle cross-equatorial flow
stable isotopes
V-Index
low-level jet
precipitation
aerial lake
Hydraulic engineering
TC1-978
Water supply for domestic and industrial purposes
TD201-500
Danny Vargas
Oscar Chimborazo
Elemér László
Marjan Temovski
László Palcsu
Rainwater Isotopic Composition in the Ecuadorian Andes and Amazon Reflects Cross-Equatorial Flow Seasonality
topic_facet cross-equatorial flow
stable isotopes
V-Index
low-level jet
precipitation
aerial lake
Hydraulic engineering
TC1-978
Water supply for domestic and industrial purposes
TD201-500
description The variability of the rainfall stable isotopic values (δ 2 H p, δ 18 O p ) in the Ecuadorian Amazon to the Andes presents a marked local “altitude” effect. At the same time, this complex orography creates diverse precipitation regimes (unimodal, bimodal, and three-modal) that make it difficult to establish a relationship with the local amount. Nevertheless, stations along these regions show a similar intra-annual isotopic variability, with lower values during MAM and ON. In contrast, higher values are found during DJF and JAS in a w-shaped pattern, suggesting a common regional controller. A monthly δ 2 H p and δ 18 O p collection campaign was established in Central Ecuador ( n = 30) to complement stations biased towards the northern and southern parts. Based on back trajectory analysis, the results demonstrated that moisture arrives from two primary sources: the Tropical North Atlantic (DJFM) and the Amazon Basin (JAS). Nevertheless, their convergence (AMJ and ON) is the crucial factor modulating the lowest isotopic values. Precisely, this convergence is stronger at the V-Index region (5° S–5° N, 65°–75° W), where the wind seasonality and reversal at low levels are enhanced, allowing the inter-hemispheric moisture flux transport (cross-equatorial flow). We propose that the amount of rainfall located at the V-Index region is a more robust approach for explaining the δ 2 H p and δ 18 O p variability rather than the local amount.
format Article in Journal/Newspaper
author Danny Vargas
Oscar Chimborazo
Elemér László
Marjan Temovski
László Palcsu
author_facet Danny Vargas
Oscar Chimborazo
Elemér László
Marjan Temovski
László Palcsu
author_sort Danny Vargas
title Rainwater Isotopic Composition in the Ecuadorian Andes and Amazon Reflects Cross-Equatorial Flow Seasonality
title_short Rainwater Isotopic Composition in the Ecuadorian Andes and Amazon Reflects Cross-Equatorial Flow Seasonality
title_full Rainwater Isotopic Composition in the Ecuadorian Andes and Amazon Reflects Cross-Equatorial Flow Seasonality
title_fullStr Rainwater Isotopic Composition in the Ecuadorian Andes and Amazon Reflects Cross-Equatorial Flow Seasonality
title_full_unstemmed Rainwater Isotopic Composition in the Ecuadorian Andes and Amazon Reflects Cross-Equatorial Flow Seasonality
title_sort rainwater isotopic composition in the ecuadorian andes and amazon reflects cross-equatorial flow seasonality
publisher MDPI AG
publishDate 2022
url https://doi.org/10.3390/w14132121
https://doaj.org/article/0f9db46c8df24ed48077db039d1e436d
genre North Atlantic
genre_facet North Atlantic
op_source Water, Vol 14, Iss 2121, p 2121 (2022)
op_relation https://www.mdpi.com/2073-4441/14/13/2121
https://doaj.org/toc/2073-4441
doi:10.3390/w14132121
2073-4441
https://doaj.org/article/0f9db46c8df24ed48077db039d1e436d
op_doi https://doi.org/10.3390/w14132121
container_title Water
container_volume 14
container_issue 13
container_start_page 2121
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