Cargando…

Complexity in water and carbon dioxide fluxes following rain pulses in an African savanna

The idea that many processes in arid and semi-arid ecosystems are dormant until activated by a pulse of rainfall, and then decay from a maximum rate as the soil dries, is widely used as a conceptual and mathematical model, but has rarely been evaluated with data. This paper examines soil water, evap...

Descripción completa

Detalles Bibliográficos
Autores principales: Williams, Christopher Alan, Hanan, Niall, Scholes, Robert J., Kutsch, Werner
Formato: Texto
Lenguaje:English
Publicado: Springer-Verlag 2009
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC2757614/
https://www.ncbi.nlm.nih.gov/pubmed/19582479
http://dx.doi.org/10.1007/s00442-009-1405-y
_version_ 1782172541687693312
author Williams, Christopher Alan
Hanan, Niall
Scholes, Robert J.
Kutsch, Werner
author_facet Williams, Christopher Alan
Hanan, Niall
Scholes, Robert J.
Kutsch, Werner
author_sort Williams, Christopher Alan
collection PubMed
description The idea that many processes in arid and semi-arid ecosystems are dormant until activated by a pulse of rainfall, and then decay from a maximum rate as the soil dries, is widely used as a conceptual and mathematical model, but has rarely been evaluated with data. This paper examines soil water, evapotranspiration (ET), and net ecosystem CO(2) exchange measured for 5 years at an eddy covariance tower sited in an Acacia–Combretum savanna near Skukuza in the Kruger National Park, South Africa. The analysis characterizes ecosystem flux responses to discrete rain events and evaluates the skill of increasingly complex “pulse models”. Rainfall pulses exert strong control over ecosystem-scale water and CO(2) fluxes at this site, but the simplest pulse models do a poor job of characterizing the dynamics of the response. Successful models need to include the time lag between the wetting event and the process peak, which differ for evaporation, photosynthesis and respiration. Adding further complexity, the time lag depends on the prior duration and degree of water stress. ET response is well characterized by a linear function of potential ET and a logistic function of profile-total soil water content, with remaining seasonal variation correlating with vegetation phenological dynamics (leaf area). A 1- to 3-day lag to maximal ET following wetting is a source of hysteresis in the ET response to soil water. Respiration responds to wetting within days, while photosynthesis takes a week or longer to reach its peak if the rainfall was preceded by a long dry spell. Both processes exhibit nonlinear functional responses that vary seasonally. We conclude that a more mechanistic approach than simple pulse modeling is needed to represent daily ecosystem C processes in semiarid savannas. ELECTRONIC SUPPLEMENTARY MATERIAL: The online version of this article (doi:10.1007/s00442-009-1405-y) contains supplementary material, which is available to authorized users.
format Text
id pubmed-2757614
institution National Center for Biotechnology Information
language English
publishDate 2009
publisher Springer-Verlag
record_format MEDLINE/PubMed
spelling pubmed-27576142009-10-07 Complexity in water and carbon dioxide fluxes following rain pulses in an African savanna Williams, Christopher Alan Hanan, Niall Scholes, Robert J. Kutsch, Werner Oecologia Physiological Ecology - Original Paper The idea that many processes in arid and semi-arid ecosystems are dormant until activated by a pulse of rainfall, and then decay from a maximum rate as the soil dries, is widely used as a conceptual and mathematical model, but has rarely been evaluated with data. This paper examines soil water, evapotranspiration (ET), and net ecosystem CO(2) exchange measured for 5 years at an eddy covariance tower sited in an Acacia–Combretum savanna near Skukuza in the Kruger National Park, South Africa. The analysis characterizes ecosystem flux responses to discrete rain events and evaluates the skill of increasingly complex “pulse models”. Rainfall pulses exert strong control over ecosystem-scale water and CO(2) fluxes at this site, but the simplest pulse models do a poor job of characterizing the dynamics of the response. Successful models need to include the time lag between the wetting event and the process peak, which differ for evaporation, photosynthesis and respiration. Adding further complexity, the time lag depends on the prior duration and degree of water stress. ET response is well characterized by a linear function of potential ET and a logistic function of profile-total soil water content, with remaining seasonal variation correlating with vegetation phenological dynamics (leaf area). A 1- to 3-day lag to maximal ET following wetting is a source of hysteresis in the ET response to soil water. Respiration responds to wetting within days, while photosynthesis takes a week or longer to reach its peak if the rainfall was preceded by a long dry spell. Both processes exhibit nonlinear functional responses that vary seasonally. We conclude that a more mechanistic approach than simple pulse modeling is needed to represent daily ecosystem C processes in semiarid savannas. ELECTRONIC SUPPLEMENTARY MATERIAL: The online version of this article (doi:10.1007/s00442-009-1405-y) contains supplementary material, which is available to authorized users. Springer-Verlag 2009-07-07 2009-09 /pmc/articles/PMC2757614/ /pubmed/19582479 http://dx.doi.org/10.1007/s00442-009-1405-y Text en © Springer-Verlag 2009
spellingShingle Physiological Ecology - Original Paper
Williams, Christopher Alan
Hanan, Niall
Scholes, Robert J.
Kutsch, Werner
Complexity in water and carbon dioxide fluxes following rain pulses in an African savanna
title Complexity in water and carbon dioxide fluxes following rain pulses in an African savanna
title_full Complexity in water and carbon dioxide fluxes following rain pulses in an African savanna
title_fullStr Complexity in water and carbon dioxide fluxes following rain pulses in an African savanna
title_full_unstemmed Complexity in water and carbon dioxide fluxes following rain pulses in an African savanna
title_short Complexity in water and carbon dioxide fluxes following rain pulses in an African savanna
title_sort complexity in water and carbon dioxide fluxes following rain pulses in an african savanna
topic Physiological Ecology - Original Paper
url https://www.ncbi.nlm.nih.gov/pmc/articles/PMC2757614/
https://www.ncbi.nlm.nih.gov/pubmed/19582479
http://dx.doi.org/10.1007/s00442-009-1405-y
work_keys_str_mv AT williamschristopheralan complexityinwaterandcarbondioxidefluxesfollowingrainpulsesinanafricansavanna
AT hananniall complexityinwaterandcarbondioxidefluxesfollowingrainpulsesinanafricansavanna
AT scholesrobertj complexityinwaterandcarbondioxidefluxesfollowingrainpulsesinanafricansavanna
AT kutschwerner complexityinwaterandcarbondioxidefluxesfollowingrainpulsesinanafricansavanna