Spatiotemporal variability in carbon exchange fluxes across the Sahel

Research output: Contribution to journalJournal articleResearchpeer-review

Standard

Spatiotemporal variability in carbon exchange fluxes across the Sahel. / Tagesson, Håkan Torbern; Fensholt, Rasmus; Cappelaere, Bernard; Mougin, Eric; Horion, Stéphanie Marie Anne F; Kergoat, Laurent; Nieto Solana, Hector; Mbow, Cheikh; Ehammer, Andrea; Demarty, Jérôme; Ardö, Jonas.

In: Agricultural and Forest Meteorology, Vol. 226-227, 2016, p. 108-118.

Research output: Contribution to journalJournal articleResearchpeer-review

Harvard

Tagesson, HT, Fensholt, R, Cappelaere, B, Mougin, E, Horion, SMAF, Kergoat, L, Nieto Solana, H, Mbow, C, Ehammer, A, Demarty, J & Ardö, J 2016, 'Spatiotemporal variability in carbon exchange fluxes across the Sahel', Agricultural and Forest Meteorology, vol. 226-227, pp. 108-118. https://doi.org/10.1016/j.agrformet.2016.05.013

APA

Tagesson, H. T., Fensholt, R., Cappelaere, B., Mougin, E., Horion, S. M. A. F., Kergoat, L., Nieto Solana, H., Mbow, C., Ehammer, A., Demarty, J., & Ardö, J. (2016). Spatiotemporal variability in carbon exchange fluxes across the Sahel. Agricultural and Forest Meteorology, 226-227, 108-118. https://doi.org/10.1016/j.agrformet.2016.05.013

Vancouver

Tagesson HT, Fensholt R, Cappelaere B, Mougin E, Horion SMAF, Kergoat L et al. Spatiotemporal variability in carbon exchange fluxes across the Sahel. Agricultural and Forest Meteorology. 2016;226-227:108-118. https://doi.org/10.1016/j.agrformet.2016.05.013

Author

Tagesson, Håkan Torbern ; Fensholt, Rasmus ; Cappelaere, Bernard ; Mougin, Eric ; Horion, Stéphanie Marie Anne F ; Kergoat, Laurent ; Nieto Solana, Hector ; Mbow, Cheikh ; Ehammer, Andrea ; Demarty, Jérôme ; Ardö, Jonas. / Spatiotemporal variability in carbon exchange fluxes across the Sahel. In: Agricultural and Forest Meteorology. 2016 ; Vol. 226-227. pp. 108-118.

Bibtex

@article{e59548f3d355464aaba5d076c3a22453,
title = "Spatiotemporal variability in carbon exchange fluxes across the Sahel",
abstract = "Semi-arid regions play an increasingly important role as a sink within the global carbon (C) cycle and is the main biome driving inter-annual variability in carbon dioxide (CO2) uptake by terrestrial ecosystems. This indicates the need for detailed studies of spatiotemporal variability in C cycling for semi-arid ecosystems. We have synthesized data on the land-atmosphere exchange of CO2 measured with the eddy covariance technique from the six existing sites across the Sahel, one of the largest semi-arid regions in the world. The overall aim of the study is to analyse and quantify the spatiotemporal variability in these fluxes and to analyse to which degree spatiotemporal variation can be explained by hydrological, climatic, edaphic and vegetation variables. All ecosystems were C sinks (average ± total error -162 ± 48 g C m-2 y-1), but were smaller when strongly impacted by anthropogenic influences. Spatial and inter-annual variability in the C flux processes indicated a strong resilience to dry conditions, and were correlated with phenological metrics. Gross primary productivity (GPP) was the most important flux process affecting the sink strength, and diurnal variability in GPP was regulated by incoming radiation, whereas seasonal dynamics was closely coupled with phenology, and soil water content. Diurnal variability in ecosystem respiration was regulated by GPP, whereas seasonal variability was strongly coupled to phenology and GPP. A budget for the entire Sahel indicated a strong C sink mitigating the global anthropogenic C emissions. Global circulation models project an increase in temperature, whereas rainfall is projected to decrease for western Sahel and increase for the eastern part, indicating that the C sink will possibly decrease and increase for the western and eastern Sahel, respectively.",
keywords = "Carbon dioxide, Climate change, Dryland, Net ecosystem exchange, Photosynthesis, Respiration",
author = "Tagesson, {H{\aa}kan Torbern} and Rasmus Fensholt and Bernard Cappelaere and Eric Mougin and Horion, {St{\'e}phanie Marie Anne F} and Laurent Kergoat and {Nieto Solana}, Hector and Cheikh Mbow and Andrea Ehammer and J{\'e}r{\^o}me Demarty and Jonas Ard{\"o}",
year = "2016",
doi = "10.1016/j.agrformet.2016.05.013",
language = "English",
volume = "226-227",
pages = "108--118",
journal = "Agricultural and Forest Meteorology",
issn = "0168-1923",
publisher = "Elsevier",

}

RIS

TY - JOUR

T1 - Spatiotemporal variability in carbon exchange fluxes across the Sahel

AU - Tagesson, Håkan Torbern

AU - Fensholt, Rasmus

AU - Cappelaere, Bernard

AU - Mougin, Eric

AU - Horion, Stéphanie Marie Anne F

AU - Kergoat, Laurent

AU - Nieto Solana, Hector

AU - Mbow, Cheikh

AU - Ehammer, Andrea

AU - Demarty, Jérôme

AU - Ardö, Jonas

PY - 2016

Y1 - 2016

N2 - Semi-arid regions play an increasingly important role as a sink within the global carbon (C) cycle and is the main biome driving inter-annual variability in carbon dioxide (CO2) uptake by terrestrial ecosystems. This indicates the need for detailed studies of spatiotemporal variability in C cycling for semi-arid ecosystems. We have synthesized data on the land-atmosphere exchange of CO2 measured with the eddy covariance technique from the six existing sites across the Sahel, one of the largest semi-arid regions in the world. The overall aim of the study is to analyse and quantify the spatiotemporal variability in these fluxes and to analyse to which degree spatiotemporal variation can be explained by hydrological, climatic, edaphic and vegetation variables. All ecosystems were C sinks (average ± total error -162 ± 48 g C m-2 y-1), but were smaller when strongly impacted by anthropogenic influences. Spatial and inter-annual variability in the C flux processes indicated a strong resilience to dry conditions, and were correlated with phenological metrics. Gross primary productivity (GPP) was the most important flux process affecting the sink strength, and diurnal variability in GPP was regulated by incoming radiation, whereas seasonal dynamics was closely coupled with phenology, and soil water content. Diurnal variability in ecosystem respiration was regulated by GPP, whereas seasonal variability was strongly coupled to phenology and GPP. A budget for the entire Sahel indicated a strong C sink mitigating the global anthropogenic C emissions. Global circulation models project an increase in temperature, whereas rainfall is projected to decrease for western Sahel and increase for the eastern part, indicating that the C sink will possibly decrease and increase for the western and eastern Sahel, respectively.

AB - Semi-arid regions play an increasingly important role as a sink within the global carbon (C) cycle and is the main biome driving inter-annual variability in carbon dioxide (CO2) uptake by terrestrial ecosystems. This indicates the need for detailed studies of spatiotemporal variability in C cycling for semi-arid ecosystems. We have synthesized data on the land-atmosphere exchange of CO2 measured with the eddy covariance technique from the six existing sites across the Sahel, one of the largest semi-arid regions in the world. The overall aim of the study is to analyse and quantify the spatiotemporal variability in these fluxes and to analyse to which degree spatiotemporal variation can be explained by hydrological, climatic, edaphic and vegetation variables. All ecosystems were C sinks (average ± total error -162 ± 48 g C m-2 y-1), but were smaller when strongly impacted by anthropogenic influences. Spatial and inter-annual variability in the C flux processes indicated a strong resilience to dry conditions, and were correlated with phenological metrics. Gross primary productivity (GPP) was the most important flux process affecting the sink strength, and diurnal variability in GPP was regulated by incoming radiation, whereas seasonal dynamics was closely coupled with phenology, and soil water content. Diurnal variability in ecosystem respiration was regulated by GPP, whereas seasonal variability was strongly coupled to phenology and GPP. A budget for the entire Sahel indicated a strong C sink mitigating the global anthropogenic C emissions. Global circulation models project an increase in temperature, whereas rainfall is projected to decrease for western Sahel and increase for the eastern part, indicating that the C sink will possibly decrease and increase for the western and eastern Sahel, respectively.

KW - Carbon dioxide

KW - Climate change

KW - Dryland

KW - Net ecosystem exchange

KW - Photosynthesis

KW - Respiration

U2 - 10.1016/j.agrformet.2016.05.013

DO - 10.1016/j.agrformet.2016.05.013

M3 - Journal article

AN - SCOPUS:84975452626

VL - 226-227

SP - 108

EP - 118

JO - Agricultural and Forest Meteorology

JF - Agricultural and Forest Meteorology

SN - 0168-1923

ER -

ID: 170215136