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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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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1766134654413307904 |