Seasonal isotope hydrology of a coffee agroforestry watershed in Costa Rica

Improved information of seasonal variations in watershed hydrology in the tropics can strengthen models and understanding of hydrology of these areas. Seasonality in the tropics produces rainy seasons versus dry seasons, leading to different hydrologic and water quality processes throughout the year. We questioned whether stable isotopes in water can be used to trace the seasonality in this region, despite experiencing a “drier” season, such as in a Tropical Humid location. This study examines the fluctuations of stable isotope compositions (δ O and δD) in water balance components in a small (<1 km ) coffee agroforestry watershed located in central Costa Rica on the Caribbean side. Samples were collected in precipitation, groundwater, and stream water for more than two years, across seasons and at an hourly frequency during storm events to better characterize spatial and temporal variations of the isotopic composition and of the respective contribution of surface and deeper groundwater to streamflow in the watershed. Isotope composition in precipitation ranged from -18.5 to -0.3‰ (∂18O) and -136.4 to 13.7‰ (∂D), and data indicate that atmospheric moisture cycling plays an important role in this region. A distinct seasonality was observed in monthly-averaged data between enriched dry season events as compared with the rainy season events. Streamflow data indicate that a deep groundwater system contributes significantly to baseflow, although a shallow, spring-driven system also contributes to stream water within the watershed. During storm events, precipitation contributes to stormflow in the short-term, confirming the role of superficial runoff. These results indicate that isotopes are helpful to partition the water balance even in a Tropical Humid situation where the rainfall seasonality is weak.

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Main Authors: Boll, Jan, Welsh, Kristen, Roupsard, Olivier
Format: conference_item biblioteca
Language:eng
Published: AGU
Subjects:F08 - Systèmes et modes de culture, P40 - Météorologie et climatologie,
Online Access:http://agritrop.cirad.fr/578794/
http://agritrop.cirad.fr/578794/1/Boll%20AGU_isotopes_poster_2014.pdf
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spelling dig-cirad-fr-5787942020-05-14T08:02:05Z http://agritrop.cirad.fr/578794/ http://agritrop.cirad.fr/578794/ Seasonal isotope hydrology of a coffee agroforestry watershed in Costa Rica. Boll Jan, Welsh Kristen, Roupsard Olivier. 2014. . San Francisco : AGU, 1 p. AGU Fall Meeting, San Francisco, États-Unis, 15 Décembre 2014/19 Décembre 2014. Researchers Seasonal isotope hydrology of a coffee agroforestry watershed in Costa Rica Boll, Jan Welsh, Kristen Roupsard, Olivier eng 2014 AGU F08 - Systèmes et modes de culture P40 - Météorologie et climatologie Improved information of seasonal variations in watershed hydrology in the tropics can strengthen models and understanding of hydrology of these areas. Seasonality in the tropics produces rainy seasons versus dry seasons, leading to different hydrologic and water quality processes throughout the year. We questioned whether stable isotopes in water can be used to trace the seasonality in this region, despite experiencing a “drier” season, such as in a Tropical Humid location. This study examines the fluctuations of stable isotope compositions (δ O and δD) in water balance components in a small (<1 km ) coffee agroforestry watershed located in central Costa Rica on the Caribbean side. Samples were collected in precipitation, groundwater, and stream water for more than two years, across seasons and at an hourly frequency during storm events to better characterize spatial and temporal variations of the isotopic composition and of the respective contribution of surface and deeper groundwater to streamflow in the watershed. Isotope composition in precipitation ranged from -18.5 to -0.3‰ (∂18O) and -136.4 to 13.7‰ (∂D), and data indicate that atmospheric moisture cycling plays an important role in this region. A distinct seasonality was observed in monthly-averaged data between enriched dry season events as compared with the rainy season events. Streamflow data indicate that a deep groundwater system contributes significantly to baseflow, although a shallow, spring-driven system also contributes to stream water within the watershed. During storm events, precipitation contributes to stormflow in the short-term, confirming the role of superficial runoff. These results indicate that isotopes are helpful to partition the water balance even in a Tropical Humid situation where the rainfall seasonality is weak. conference_item info:eu-repo/semantics/conferenceObject Conference info:eu-repo/semantics/publishedVersion http://agritrop.cirad.fr/578794/1/Boll%20AGU_isotopes_poster_2014.pdf text cc_0 info:eu-repo/semantics/openAccess https://creativecommons.org/publicdomain/zero/1.0/
institution CIRAD FR
collection DSpace
country Francia
countrycode FR
component Bibliográfico
access En linea
databasecode dig-cirad-fr
tag biblioteca
region Europa del Oeste
libraryname Biblioteca del CIRAD Francia
language eng
topic F08 - Systèmes et modes de culture
P40 - Météorologie et climatologie
F08 - Systèmes et modes de culture
P40 - Météorologie et climatologie
spellingShingle F08 - Systèmes et modes de culture
P40 - Météorologie et climatologie
F08 - Systèmes et modes de culture
P40 - Météorologie et climatologie
Boll, Jan
Welsh, Kristen
Roupsard, Olivier
Seasonal isotope hydrology of a coffee agroforestry watershed in Costa Rica
description Improved information of seasonal variations in watershed hydrology in the tropics can strengthen models and understanding of hydrology of these areas. Seasonality in the tropics produces rainy seasons versus dry seasons, leading to different hydrologic and water quality processes throughout the year. We questioned whether stable isotopes in water can be used to trace the seasonality in this region, despite experiencing a “drier” season, such as in a Tropical Humid location. This study examines the fluctuations of stable isotope compositions (δ O and δD) in water balance components in a small (<1 km ) coffee agroforestry watershed located in central Costa Rica on the Caribbean side. Samples were collected in precipitation, groundwater, and stream water for more than two years, across seasons and at an hourly frequency during storm events to better characterize spatial and temporal variations of the isotopic composition and of the respective contribution of surface and deeper groundwater to streamflow in the watershed. Isotope composition in precipitation ranged from -18.5 to -0.3‰ (∂18O) and -136.4 to 13.7‰ (∂D), and data indicate that atmospheric moisture cycling plays an important role in this region. A distinct seasonality was observed in monthly-averaged data between enriched dry season events as compared with the rainy season events. Streamflow data indicate that a deep groundwater system contributes significantly to baseflow, although a shallow, spring-driven system also contributes to stream water within the watershed. During storm events, precipitation contributes to stormflow in the short-term, confirming the role of superficial runoff. These results indicate that isotopes are helpful to partition the water balance even in a Tropical Humid situation where the rainfall seasonality is weak.
format conference_item
topic_facet F08 - Systèmes et modes de culture
P40 - Météorologie et climatologie
author Boll, Jan
Welsh, Kristen
Roupsard, Olivier
author_facet Boll, Jan
Welsh, Kristen
Roupsard, Olivier
author_sort Boll, Jan
title Seasonal isotope hydrology of a coffee agroforestry watershed in Costa Rica
title_short Seasonal isotope hydrology of a coffee agroforestry watershed in Costa Rica
title_full Seasonal isotope hydrology of a coffee agroforestry watershed in Costa Rica
title_fullStr Seasonal isotope hydrology of a coffee agroforestry watershed in Costa Rica
title_full_unstemmed Seasonal isotope hydrology of a coffee agroforestry watershed in Costa Rica
title_sort seasonal isotope hydrology of a coffee agroforestry watershed in costa rica
publisher AGU
url http://agritrop.cirad.fr/578794/
http://agritrop.cirad.fr/578794/1/Boll%20AGU_isotopes_poster_2014.pdf
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AT welshkristen seasonalisotopehydrologyofacoffeeagroforestrywatershedincostarica
AT roupsardolivier seasonalisotopehydrologyofacoffeeagroforestrywatershedincostarica
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