Spatially distributed tracer-aided modelling to explore water and isotope transport, storage and mixing in a pristine, humid tropical catchment

Joni Dehaspe, Christian Birkel* (Corresponding Author), Doerthe Tetzlaff, Ricardo Sánchez-Murillo, Ana María Durán-Quesada, Chris Soulsby

*Corresponding author for this work

Research output: Contribution to journalArticle

2 Citations (Scopus)

Abstract

Rapidly transforming headwater catchments in the humid tropics provide important resources for drinking water, irrigation, hydropower, and ecosystem connectivity. However, such resources for downstream use remain unstudied. To improve understanding of the behaviour and influence of pristine rainforests on water and tracer fluxes, we adapted the relatively parsimonious, spatially distributed tracer-aided rainfall–runoff (STARR) model using event-based stable isotope data for the 3.2-km2 San Lorencito catchment in Costa Rica. STARR was used to simulate rainforest interception of water and stable isotopes, which showed a significant isotopic enrichment in throughfall compared with gross rainfall. Acceptable concurrent simulations of discharge (Kling–Gupta efficiency [KGE] ~0.8) and stable isotopes in stream water (KGE ~0.6) at high spatial (10 m) and temporal (hourly) resolution indicated a rapidly responding system. Around 90% of average annual streamflow (2,099 mm) was composed of quick, near-surface runoff components, whereas only ~10% originated from groundwater in deeper layers. Simulated actual evapotranspiration (ET) from interception and soil storage were low (~420 mm/year) due to high relative humidity (average 96%) and cloud cover limiting radiation inputs. Modelling suggested a highly variable groundwater storage (~10 to 500 mm) in this steep, fractured volcanic catchment that sustains dry season baseflows. This groundwater is concentrated in riparian areas as an alluvial–colluvial aquifer connected to the stream. This was supported by rainfall–runoff isotope simulations, showing a “flashy” stream response to rainfall with only a moderate damping effect and a constant isotope signature from deeper groundwater (~400-mm additional mixing volume) during baseflow. The work serves as a first attempt to apply a spatially distributed tracer-aided model to a tropical rainforest environment exploring the hydrological functioning of a steep, fractured-volcanic catchment. We also highlight limitations and propose a roadmap for future data collection and spatially distributed tracer-aided model development in tropical headwater catchments.

Original languageEnglish
Pages (from-to)3206-3224
Number of pages19
JournalHydrological Processes
Volume32
Issue number21
Early online date7 Sep 2018
DOIs
Publication statusPublished - 15 Oct 2018

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tracer
isotope
catchment
rainforest
stable isotope
groundwater
modeling
baseflow
interception
headwater
water
humid tropics
rainfall
throughfall
resource
cloud cover
damping
simulation
streamflow
dry season

Keywords

  • Costa Rica
  • humid tropics
  • ReBAMB
  • stable isotopes
  • tracer-aided modelling
  • tracers

ASJC Scopus subject areas

  • Water Science and Technology

Cite this

Spatially distributed tracer-aided modelling to explore water and isotope transport, storage and mixing in a pristine, humid tropical catchment. / Dehaspe, Joni; Birkel, Christian (Corresponding Author); Tetzlaff, Doerthe; Sánchez-Murillo, Ricardo; Durán-Quesada, Ana María; Soulsby, Chris.

In: Hydrological Processes, Vol. 32, No. 21, 15.10.2018, p. 3206-3224.

Research output: Contribution to journalArticle

Dehaspe, Joni ; Birkel, Christian ; Tetzlaff, Doerthe ; Sánchez-Murillo, Ricardo ; Durán-Quesada, Ana María ; Soulsby, Chris. / Spatially distributed tracer-aided modelling to explore water and isotope transport, storage and mixing in a pristine, humid tropical catchment. In: Hydrological Processes. 2018 ; Vol. 32, No. 21. pp. 3206-3224.
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abstract = "Rapidly transforming headwater catchments in the humid tropics provide important resources for drinking water, irrigation, hydropower, and ecosystem connectivity. However, such resources for downstream use remain unstudied. To improve understanding of the behaviour and influence of pristine rainforests on water and tracer fluxes, we adapted the relatively parsimonious, spatially distributed tracer-aided rainfall–runoff (STARR) model using event-based stable isotope data for the 3.2-km2 San Lorencito catchment in Costa Rica. STARR was used to simulate rainforest interception of water and stable isotopes, which showed a significant isotopic enrichment in throughfall compared with gross rainfall. Acceptable concurrent simulations of discharge (Kling–Gupta efficiency [KGE] ~0.8) and stable isotopes in stream water (KGE ~0.6) at high spatial (10 m) and temporal (hourly) resolution indicated a rapidly responding system. Around 90{\%} of average annual streamflow (2,099 mm) was composed of quick, near-surface runoff components, whereas only ~10{\%} originated from groundwater in deeper layers. Simulated actual evapotranspiration (ET) from interception and soil storage were low (~420 mm/year) due to high relative humidity (average 96{\%}) and cloud cover limiting radiation inputs. Modelling suggested a highly variable groundwater storage (~10 to 500 mm) in this steep, fractured volcanic catchment that sustains dry season baseflows. This groundwater is concentrated in riparian areas as an alluvial–colluvial aquifer connected to the stream. This was supported by rainfall–runoff isotope simulations, showing a “flashy” stream response to rainfall with only a moderate damping effect and a constant isotope signature from deeper groundwater (~400-mm additional mixing volume) during baseflow. The work serves as a first attempt to apply a spatially distributed tracer-aided model to a tropical rainforest environment exploring the hydrological functioning of a steep, fractured-volcanic catchment. We also highlight limitations and propose a roadmap for future data collection and spatially distributed tracer-aided model development in tropical headwater catchments.",
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N1 - This project was initiated with a BGS fellowship to Josie Geris (University of Aberdeen) and C. B. and an Ideawild grant to C. B. Support by Tito Maldonado with the cluster computing facility at CIGEFI, UCR, is greatly acknowledged. Furthermore, we thank Vanessa Solano and Sebastian Granados for processing the multispectral imagery. Many helping hands in the field are acknowledged. The UCR‐funded “Isotopes in tropical ecosystems network IsoNET” and the project 217‐B4‐39 is greatly acknowledged. We also thank the VEWA project that enabled early work on the STARR model. We thank one anonymous reviewer and Matthias Beyer for their constructive comments that helped improve the paper.

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N2 - Rapidly transforming headwater catchments in the humid tropics provide important resources for drinking water, irrigation, hydropower, and ecosystem connectivity. However, such resources for downstream use remain unstudied. To improve understanding of the behaviour and influence of pristine rainforests on water and tracer fluxes, we adapted the relatively parsimonious, spatially distributed tracer-aided rainfall–runoff (STARR) model using event-based stable isotope data for the 3.2-km2 San Lorencito catchment in Costa Rica. STARR was used to simulate rainforest interception of water and stable isotopes, which showed a significant isotopic enrichment in throughfall compared with gross rainfall. Acceptable concurrent simulations of discharge (Kling–Gupta efficiency [KGE] ~0.8) and stable isotopes in stream water (KGE ~0.6) at high spatial (10 m) and temporal (hourly) resolution indicated a rapidly responding system. Around 90% of average annual streamflow (2,099 mm) was composed of quick, near-surface runoff components, whereas only ~10% originated from groundwater in deeper layers. Simulated actual evapotranspiration (ET) from interception and soil storage were low (~420 mm/year) due to high relative humidity (average 96%) and cloud cover limiting radiation inputs. Modelling suggested a highly variable groundwater storage (~10 to 500 mm) in this steep, fractured volcanic catchment that sustains dry season baseflows. This groundwater is concentrated in riparian areas as an alluvial–colluvial aquifer connected to the stream. This was supported by rainfall–runoff isotope simulations, showing a “flashy” stream response to rainfall with only a moderate damping effect and a constant isotope signature from deeper groundwater (~400-mm additional mixing volume) during baseflow. The work serves as a first attempt to apply a spatially distributed tracer-aided model to a tropical rainforest environment exploring the hydrological functioning of a steep, fractured-volcanic catchment. We also highlight limitations and propose a roadmap for future data collection and spatially distributed tracer-aided model development in tropical headwater catchments.

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