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New constraints on the Amazonian carbon balance from airborne observations of the stable isotopes of CO2

Project description

A closer look at Amazonia’s carbon balance mystery

Severe droughts ravaged Amazonia in 2005 and 2010. The loss of carbon from the terrestrial biosphere was alarmingly high, nearly doubling the annual fossil fuel CO2 emissions in the EU. This suggests a high sensitivity of the Amazonian carbon balance to the projected intensification of droughts in the coming decades. However, there is no scientific consensus on key metrics of Amazonian carbon exchange, such as gross primary production (GPP) and its response to moisture deficits. Previous efforts to measure these metrics on a large scale were impossible. In this context, the EU funded ASICA project plans to provide the first observation-based estimate of pan Amazonian GPP and its variations during drought, using stable isotopes and an aircraft monitoring programme in Brazil.

Objective

Severe droughts in Amazonia in 2005 and 2010 caused widespread loss of carbon from the terrestrial biosphere. This loss, almost twice the annual fossil fuel CO2 emissions in the EU, suggests a large sensitivity of the Amazonian carbon balance to a predicted more intense drought regime in the next decades. This is a dangerous inference though, as there is no scientific consensus on the most basic metrics of Amazonian carbon exchange: the gross primary production (GPP) and its response to moisture deficits in the soil and atmosphere. Measuring them on scales that span the whole Amazon forest was thus far impossible, but in this project I aim to deliver the first observation-based estimate of pan-Amazonian GPP and its drought induced variations.
My program builds on two recent breakthroughs in our use of stable isotopes (13C, 17O, 18O) in atmospheric CO2: (1) Our discovery that observed δ¹³C in CO2 in the atmosphere is a quantitative measure for vegetation water-use efficiency over millions of square kilometers, integrating the drought response of individual plants. (2) The possibility to precisely measure the relative ratios of 18O/16O and 17O/16O in CO2, called Δ17O. Anomalous Δ17O values are present in air coming down from the stratosphere, but this anomaly is removed upon contact of CO2 with leaf water inside plant stomata. Hence, observed Δ17O values depend directly on the magnitude of GPP. Both δ¹³C and Δ17O measurements are scarce over the Amazon-basin, and I propose more than 7000 new measurements leveraging an established aircraft monitoring program in Brazil. Quantitative interpretation of these observations will break new ground in our use of stable isotopes to understand climate variations, and is facilitated by our renowned numerical modeling system “CarbonTracker”. My program will answer two burning question in carbon cycle science today: (a) What is the magnitude of GPP in Amazonia? And (b) How does it vary over different intensities of drought?

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Topic(s)

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Funding Scheme

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ERC-COG - Consolidator Grant

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Call for proposal

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(opens in new window) ERC-2014-CoG

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Host institution

WAGENINGEN UNIVERSITY
Net EU contribution

Net EU financial contribution. The sum of money that the participant receives, deducted by the EU contribution to its linked third party. It considers the distribution of the EU financial contribution between direct beneficiaries of the project and other types of participants, like third-party participants.

€ 827 975,00
Address
DROEVENDAALSESTEEG 4
6708 PB Wageningen
Netherlands

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Region
Oost-Nederland Gelderland Veluwe
Activity type
Higher or Secondary Education Establishments
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Total cost

The total costs incurred by this organisation to participate in the project, including direct and indirect costs. This amount is a subset of the overall project budget.

€ 827 975,00

Beneficiaries (5)

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