TY - JOUR
T1 - Moisture transport and seasonal variations in the stable isotopic composition of rainfall in Central American and Andean Páramo during El Niño conditions (2015–2016)
AU - Esquivel-Hernández, Germain
AU - Mosquera, Giovanny M.
AU - Sánchez-Murillo, Ricardo
AU - Quesada-Román, Adolfo
AU - Birkel, Christian
AU - Crespo, Patricio
AU - Célleri, Rolando
AU - Windhorst, David
AU - Breuer, Lutz
AU - Boll, Jan
N1 - Publisher Copyright:
© 2019 John Wiley & Sons, Ltd.
PY - 2019/6/30
Y1 - 2019/6/30
N2 - High-elevation tropical grassland systems, called Páramo, provide essential ecosystem services such as water storage and supply for surrounding and lowland areas. Páramo systems are threatened by climate and land use changes. Rainfall generation processes and moisture transport pathways influencing precipitation in the Páramo are poorly understood but needed to estimate the impact of these changes, particularly during El Niño conditions, which largely affect hydrometeorological conditions in tropical regions. To fill this knowledge gap, we present a stable isotope analysis of rainfall samples collected on a daily to weekly basis between January 2015 and May 2016 during the strongest El Niño event recorded in history (2014–2016) in two Páramo regions of Central America (Chirripó, Costa Rica) and the northern Andes (Cajas, south Ecuador). Isotopic compositions were used to identify how rainfall generation processes (convective and orographic) change seasonally at each study site. Hybrid Single Particle Lagrangian Integrated Trajectory model (HYSPLIT) air mass back trajectory analysis was used to identify preferential moisture transport pathways to each Páramo site. Our results show the strong influence of north-east trade winds to transport moisture from the Caribbean Sea to Chirripó and the South American low-level jet to transport moisture from the Amazon forest to Cajas. These moisture contributions were also related to the formation of convective rainfall associated with the passage of the Intertropical Convergence Zone over Costa Rica and Ecuador during the wetter seasons and to orographic precipitation during the transition and drier seasons. Our findings provide essential baseline information for further research applications of water stable isotopes as tracers of rainfall generation processes and transport in the Páramo and other montane ecosystems in the tropics.
AB - High-elevation tropical grassland systems, called Páramo, provide essential ecosystem services such as water storage and supply for surrounding and lowland areas. Páramo systems are threatened by climate and land use changes. Rainfall generation processes and moisture transport pathways influencing precipitation in the Páramo are poorly understood but needed to estimate the impact of these changes, particularly during El Niño conditions, which largely affect hydrometeorological conditions in tropical regions. To fill this knowledge gap, we present a stable isotope analysis of rainfall samples collected on a daily to weekly basis between January 2015 and May 2016 during the strongest El Niño event recorded in history (2014–2016) in two Páramo regions of Central America (Chirripó, Costa Rica) and the northern Andes (Cajas, south Ecuador). Isotopic compositions were used to identify how rainfall generation processes (convective and orographic) change seasonally at each study site. Hybrid Single Particle Lagrangian Integrated Trajectory model (HYSPLIT) air mass back trajectory analysis was used to identify preferential moisture transport pathways to each Páramo site. Our results show the strong influence of north-east trade winds to transport moisture from the Caribbean Sea to Chirripó and the South American low-level jet to transport moisture from the Amazon forest to Cajas. These moisture contributions were also related to the formation of convective rainfall associated with the passage of the Intertropical Convergence Zone over Costa Rica and Ecuador during the wetter seasons and to orographic precipitation during the transition and drier seasons. Our findings provide essential baseline information for further research applications of water stable isotopes as tracers of rainfall generation processes and transport in the Páramo and other montane ecosystems in the tropics.
KW - El Niño–Southern Oscillation (ENSO)
KW - HYSPLIT
KW - moisture recycling
KW - precipitation
KW - tropical Páramo
KW - water stable isotopes
UR - http://www.scopus.com/inward/record.url?scp=85064553422&partnerID=8YFLogxK
U2 - 10.1002/hyp.13438
DO - 10.1002/hyp.13438
M3 - Article
AN - SCOPUS:85064553422
SN - 0885-6087
VL - 33
SP - 1802
EP - 1817
JO - Hydrological Processes
JF - Hydrological Processes
IS - 13
ER -