August 13, 2018

Satellite observations reveal secrets of dry tropical forest greening

In dry tropical forests, vegetation takes up water at the end of the wet season and stores it during the driest season of the year. This large amount of stored water enables trees to flush new leaves about one month before the next rainy season. This surprising phenomenon has been revealed for the first time using satellite observations, mainly in the African region of Miombo (around four times the surface area of France), in a study coordinated by the University of Copenhagen and INRA in collaboration with the CEA, CNRS, CNES and Bordeaux Science Agro . These findings, published on 13 August 2018 in Nature Ecology and Evolution, will help researchers improve current Earth system models (which do not fully account for plant hydraulic mechanisms) and future climate change and water cycle projections in these regions of the world.

What are the relationships between plant water storage and leaf development? Are both variables closely related in time and space across the Earth’s surface?  These are critical questions to improve vegetation-atmosphere feedback in Earth system models and predict ecosystem responses to climate change.

A discovery in the African tropical forest of Miombo

Using satellite observations, the study conducted by the University of Copenhagen and INRA, in collaboration with the CEA, CNRS, CNES and Bordeaux Science Agro, demonstrated that seasonal variations in plant water storage and leaf development are highly synchronous in boreal and temperate regions. However, more surprisingly, the researchers showed that these variations are highly asynchronous in dry tropical forests, where an increase in plant water storage precedes vegetation greening by 25 to 180 days. The study focused on the Miombo woodlands, which cover an immense surface area of more than 2.7 million square kilometres to the south of the African rainforests. Satellite observations of this region clearly show that the leaf area index (LAI) begins to increase several weeks before the rainy season begins, a clear sign of “pre-rain” green up that has already been documented in numerous studies. The mechanisms behind this phenomenon are not yet fully understood but likely involve large construction costs to the plants, which must invest in their rooting system to access deep ground water and in their woody stems to increase their water storage capacity.

Dans cette région, les observations satellites montrent clairement que l'indice foliaire (LAI) commence à augmenter plusieurs semaines avant le début des pluies, un signe clair du verdissement « pré-pluie » déjà révélé par de nombreuses études. Les mécanismes impliqués dans ce phénomène ne sont pas encore bien compris mais impliquent probablement des coûts énergétiques importants pour les plantes, qui doivent développer non seulement leur système racinaire pour accéder à l'eau du sol en profondeur mais également leurs branches pour accroître leur capacité de stockage.

The novelty comes from observations of the L-band vegetation optical depth (L-VOD) index (a crucial indicator of the plant water content dynamic) from the European Space Agency (ESA)-CNES SMOS satellite that show that vegetation in Miombo takes up water at the end of the rainy season (when transpiration losses fall) and stores it in woody tissues during most of the dry season until the emergence of new leaves a few weeks before rain starts. This early leaf flushing has physiological and ecological advantages, reducing the time lag between the onset of the rainy season and that of photosynthetic activity. This intriguing hydraulic behaviour had previously been seen in in situ experiments of a few trees in dry tropical forests, particularly in Costa Rica. However, this new study is the first demonstrating that this is a large-scale phenomenon, visible over forested areas as large as the Miombo woodlands, as well as in the northern African woodlands and the Brazilian Cerrado.

Moreover, these physiological and hydrological processes are still not included in Earth system models. The new L-VOD data set will be key for improving the next generation of Earth system models, leading to more robust projections of the future climate and water cycle in these regions of the world.


Temporal coupling between L-VOD and LAI seasonality: lag time for L-VOD to obtain the highest correlation with LAI for pixels with a clear seasonality. The black rectangle includes the Miombo woodlands. © F. Tian – University of Copenhagen

A large set of satellite observations

This study was based on a large set of satellite observations that aim to characterise the time variations in key hydrological and vegetation parameters at the ecosystem scale. The research benefited from the new SMOS-IC data set of the vegetation index referred to as L-band vegetation optical depth, or L-VOD, retrieved from space-borne observations of the ESA-CNES SMOS satellite. This index is closely related to the vegetation water content (VWC, kg/m2) of the whole canopy layer. More specifically, along with the L-VOD (a proxy of vegetation water storage), the other variables considered in the study include leaf area index (LAI) retrieved from optical satellite observations and used to parameterise foliar phenology, terrestrial groundwater storage anomalies (TWS) retrieved from GRACE satellites, surface soil moisture, rainfall and transpiration. Surface soil moisture observations considered here were retrieved simultaneously with L-VOD from the multi-angular SMOS observations.


Seasonal water balance in the African tropical Miombo woodlands. The time series (2011-2012) of plant water storage (L-VOD), leaf area index and rainfall for a 1°×1° area (centred at 11.5°S, 18.5°E). The grey shaded rectangles indicate the dry seasons. © F. Tian – University of Copenhagen

When averaged at a yearly scale, the L-VOD index has been found to be closely related to global patterns of plant aboveground biomass, a feature that was used recently to quantify annual changes in sub-Saharan aboveground biomass carbon stock. For more information: http://presse.inra.fr/Communiques-de-presse/un-nouvel-outil-pour-suivre-...

More informations : http://presse.inra.fr/Communiques-de-presse/un-nouvel-outil-pour-suivre-...


The Miombo woodlands during the “pre-rain” season.
© C. Ryan, University of Edinburgh

 

1 Department of Geosciences and Natural Resource Management, University of Copenhagen, Copenhagen, Denmark
  2 Unité « Interaction Sol Plante Atmosphère » (Inra, Bordeaux Sciences Agro), centre Inra Nouvelle-Aquitaine – Bordeaux
  3 Les autres laboratoires français impliqués dans ces travaux : Laboratoire des sciences du climat et de l’environnement (CEA-CNRS-UVSQ), Evolution et diversité biologique (CNRS-IRD-UT3 Paul Sabatier-ENFA), Centre d’études spatiales de la biosphère (CNES-CNRS-IRD-UT3 Paul Sabatier), Bordeaux Science Agro, (National School of Agricultural Engineering of Bordeaux)

References :
F. Tian, J.-P. Wigneron, P. Ciais, J. Chave, J. Ogée, J. Peñuelas, A. Ræbild, J-C Domec, X. Tong, M. Brandt, A. Mialon, N. Rodriguez-Fernandez, T. Tagesson, A. Al-Yaari, Y. Kerr, C. Chen, R. B. Myneni, W. Zhang, J. Ardö, R. Fensholt, "Coupling of ecosystem-scale plant water storage and leaf phenology observed by satellite", Nature Ecology & Evolution, 13 août 2018   https://doi.org/10.1038/s41559-018-0630-3

Scientific contact :
Jean-Pierre Wigneron : jean-pierre.wigneron@inra.fr - T. +33 5 57 12 24 19
Unité Interaction sol plante atmosphère (Inra, Bordeaux Sciences Agro)
Départements scientifiques « Environnement et Agronomie » et « Ecologie des Forêts, Prairies et Milieux Aquatiques »
Centre Inra Nouvelle Aquitaine Bordeaux

Presse contact :
Inra service de presse : presse@inra.fr – T. +33 1 42 75 91 86

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