Using hydrological connectivity to detect transitions and degradation thresholds: Applications to dryland systems

Patricia M. Saco*, José F. Rodríguez, Mariano Moreno-de las Heras, Saskia Keesstra, Samira Azadi, Steven Sandi, Jantiene Baartman, Jesús Rodrigo-Comino, María Julieta Rossi

*Corresponding author for this work

Research output: Contribution to journalArticleAcademicpeer-review

Abstract

In arid and semi-arid ecosystems, shortage of water can trigger changes in landscapes’ structures and function leading to degradation and desertification. Hydrological connectivity is a useful framework for understanding water redistribution and scaling issues associated with runoff and sediment production, since human and/or natural disturbances alter surface water availability and pathways increasing/decreasing connectivity. In this paper, we illustrate the use of the connectivity framework for several examples of dryland systems that are analysed at a variety of spatial and temporal scales. In doing so, we draw particular attention to the analysis of coevolution of system structures and function, and how they may drive threshold behaviour leading to desertification and degradation. We first analyse the case of semi-arid rangelands, where feedbacks between the decline in vegetation density and landscape erosion reinforces degradation processes driven by changes in connectivity until a threshold is crossed above which the return to a functional system is unlikely. We then focus on semi-arid wetlands, where decreases in water volumes promote terrestrial vegetation encroachment that changes drainage conditions and connectivity, potentially reinforcing redistribution of flow paths to other wetland areas. The analysis of dryland wetlands is based on a novel hydrologic connectivity index derived using inundation requirements for wetland vegetation associations. The examples presented highlight the need to incorporate a coevolutionary framework for the analysis of changing connectivity patterns and the emergence of thresholds in arid and semi-arid systems.

Original languageEnglish
Article number104354
JournalCatena
Volume186
DOIs
Publication statusPublished - Mar 2020

Fingerprint

connectivity
degradation
wetland
desertification
vegetation
landscape structure
coevolution
rangeland
water availability
water
drainage
runoff
surface water
erosion
disturbance
ecosystem
sediment
analysis

Keywords

  • Geoecology
  • Hydrological connectivity
  • Land degradation
  • Landscape evolution
  • Semi-arid environments

Cite this

Saco, P. M., Rodríguez, J. F., Moreno-de las Heras, M., Keesstra, S., Azadi, S., Sandi, S., ... Rossi, M. J. (2020). Using hydrological connectivity to detect transitions and degradation thresholds: Applications to dryland systems. Catena, 186, [104354]. https://doi.org/10.1016/j.catena.2019.104354
Saco, Patricia M. ; Rodríguez, José F. ; Moreno-de las Heras, Mariano ; Keesstra, Saskia ; Azadi, Samira ; Sandi, Steven ; Baartman, Jantiene ; Rodrigo-Comino, Jesús ; Rossi, María Julieta. / Using hydrological connectivity to detect transitions and degradation thresholds: Applications to dryland systems. In: Catena. 2020 ; Vol. 186.
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abstract = "In arid and semi-arid ecosystems, shortage of water can trigger changes in landscapes’ structures and function leading to degradation and desertification. Hydrological connectivity is a useful framework for understanding water redistribution and scaling issues associated with runoff and sediment production, since human and/or natural disturbances alter surface water availability and pathways increasing/decreasing connectivity. In this paper, we illustrate the use of the connectivity framework for several examples of dryland systems that are analysed at a variety of spatial and temporal scales. In doing so, we draw particular attention to the analysis of coevolution of system structures and function, and how they may drive threshold behaviour leading to desertification and degradation. We first analyse the case of semi-arid rangelands, where feedbacks between the decline in vegetation density and landscape erosion reinforces degradation processes driven by changes in connectivity until a threshold is crossed above which the return to a functional system is unlikely. We then focus on semi-arid wetlands, where decreases in water volumes promote terrestrial vegetation encroachment that changes drainage conditions and connectivity, potentially reinforcing redistribution of flow paths to other wetland areas. The analysis of dryland wetlands is based on a novel hydrologic connectivity index derived using inundation requirements for wetland vegetation associations. The examples presented highlight the need to incorporate a coevolutionary framework for the analysis of changing connectivity patterns and the emergence of thresholds in arid and semi-arid systems.",
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Saco, PM, Rodríguez, JF, Moreno-de las Heras, M, Keesstra, S, Azadi, S, Sandi, S, Baartman, J, Rodrigo-Comino, J & Rossi, MJ 2020, 'Using hydrological connectivity to detect transitions and degradation thresholds: Applications to dryland systems', Catena, vol. 186, 104354. https://doi.org/10.1016/j.catena.2019.104354

Using hydrological connectivity to detect transitions and degradation thresholds: Applications to dryland systems. / Saco, Patricia M.; Rodríguez, José F.; Moreno-de las Heras, Mariano; Keesstra, Saskia; Azadi, Samira; Sandi, Steven; Baartman, Jantiene; Rodrigo-Comino, Jesús; Rossi, María Julieta.

In: Catena, Vol. 186, 104354, 03.2020.

Research output: Contribution to journalArticleAcademicpeer-review

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T1 - Using hydrological connectivity to detect transitions and degradation thresholds: Applications to dryland systems

AU - Saco, Patricia M.

AU - Rodríguez, José F.

AU - Moreno-de las Heras, Mariano

AU - Keesstra, Saskia

AU - Azadi, Samira

AU - Sandi, Steven

AU - Baartman, Jantiene

AU - Rodrigo-Comino, Jesús

AU - Rossi, María Julieta

PY - 2020/3

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AB - In arid and semi-arid ecosystems, shortage of water can trigger changes in landscapes’ structures and function leading to degradation and desertification. Hydrological connectivity is a useful framework for understanding water redistribution and scaling issues associated with runoff and sediment production, since human and/or natural disturbances alter surface water availability and pathways increasing/decreasing connectivity. In this paper, we illustrate the use of the connectivity framework for several examples of dryland systems that are analysed at a variety of spatial and temporal scales. In doing so, we draw particular attention to the analysis of coevolution of system structures and function, and how they may drive threshold behaviour leading to desertification and degradation. We first analyse the case of semi-arid rangelands, where feedbacks between the decline in vegetation density and landscape erosion reinforces degradation processes driven by changes in connectivity until a threshold is crossed above which the return to a functional system is unlikely. We then focus on semi-arid wetlands, where decreases in water volumes promote terrestrial vegetation encroachment that changes drainage conditions and connectivity, potentially reinforcing redistribution of flow paths to other wetland areas. The analysis of dryland wetlands is based on a novel hydrologic connectivity index derived using inundation requirements for wetland vegetation associations. The examples presented highlight the need to incorporate a coevolutionary framework for the analysis of changing connectivity patterns and the emergence of thresholds in arid and semi-arid systems.

KW - Geoecology

KW - Hydrological connectivity

KW - Land degradation

KW - Landscape evolution

KW - Semi-arid environments

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DO - 10.1016/j.catena.2019.104354

M3 - Article

VL - 186

JO - Catena

JF - Catena

SN - 0341-8162

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ER -