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Carbon loss on the other side of drought:  excess wet season precipitation during La Niña suppresses Amazon forest photosynthesis Natalia Restrepo-Coupe,

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Presentation on theme: "Carbon loss on the other side of drought:  excess wet season precipitation during La Niña suppresses Amazon forest photosynthesis Natalia Restrepo-Coupe,"— Presentation transcript:

1 Carbon loss on the other side of drought:  excess wet season precipitation during La Niña suppresses Amazon forest photosynthesis Natalia Restrepo-Coupe, Brad Christoffersen, Daniel F. Amaral, Plínio B. de Camargo; Scott R. Saleska

2 Motivation: will Amazon forest die-back with future climate change?
45 S 90S 90W Mean daily temperature change(K) Precipitation change (mm day-1) Differences relative to mean Change in Vegetation Carbon (kg C m-2) Adapted from: Cox et al., 2003, Amazon Dieback under Climate-Carbon Cycle Projections for the 21st Century

3 Motivation: August 2008 – June 2008 La Niña Event
Oceanic Nino Index, ONI (ERSST.v3b ONI) Upper ocean heat anomalies ( ) 4 3 2 1 -1 -2 -3 Sea Surface Temperature Anomlies (C) El Niño neutral La Niña The basin-wide equatorial upper ocean (0-300 m) heat content is greatest prior to and during the early stages of a Pacific warm (El Niño) episode (compare top 2 panels) and least prior to and during the early stages of a cold (La Niña) episode. La Niña ONI value for ASO 2007 – AMJ 2008 is oC The most recent ONI value (July – September 2009) is +0.8oC. Source:

4 Motivation: 2008 – June 2008 La Niña Event
Oceanic Nino Index, ONI (ERSST.v3b ONI) Upper ocean heat anomalies ( ) 4 3 2 1 -1 -2 -3 1.5 1 0.5 -0.5 -1 -2 Sea Surface Temperature Anomlies (C) neutral La Niña Sea Surface Temperature Anomlies (C) The basin-wide equatorial upper ocean (0-300 m) heat content is greatest prior to and during the early stages of a Pacific warm (El Niño) episode (compare top 2 panels) and least prior to and during the early stages of a cold (La Niña) episode. NOV JAN MAR MAY JUL Source:

5 Motivation: South America precipitation 2008 – 2009
Apr-May Normilized anomaly K67 K67 Anomaly=((precip)m,y -(mean precip)m, )/(std dev precip)m, ) departure from the 1998–2009 mean (TRMM1998 – 2009), normalized by the standard deviation (s). Lon Lon Tropical Rainfall Measuring Mission (TRMM) data, at 0.25 spatial resolution 1998 – [NASA, 2006]

6 … on the other side of drought …
Caxiuana calculate the anomaly

7 Tapajós K67 tropical forest

8 Tapajós K67 tropical forest: Climate
dry season wet season Aug 2008 – Jul 2009 dry season wet season Dry season starts ~15 July dry season wet season Hydrological year: Dry season – Wet season HY2002: Aug 1, 2002 – Jul 31, 2003 HY2003: Aug 1, 2003 – Jul 31, 2004 HY2004: Aug 1, 2004 – Jul 31, 2005 HY2005: Aug 1, 2005 – Jan 6, 2006 HY2008: Aug 1, 2008 – Jul 31, 2009

9 Result 1: La Niña Event corresponds to C Forest Loss
Aug 2008 – Jul 2009 dry season wet season Net ecosystem exchange Forest C losses Forest C uptake

10 Result 1: La Niña Event corresponds to C Forest Loss
Aug 2008 – Jul 2009 dry season wet season dry season wet season Instantaneous C-flux Cumulative C-flux and Precipitation

11 What is the cause of C-loss? (split into photosynthesis & respiration)
NEE: Net Ecosystem Exchange R: Ecosystem Respiration GEE: Gross Ecosystem Productivity ~ Photosynthetic activity Higher C losses dry season wet season Higher C uptake NEE = R + GEE

12 Result 2: Forest C Loss is due to reduced photosynthesis
NEE: Net Ecosystem Exchange R: Ecosystem Respiration GEE: Gross Ecosystem Productivity ~ Photosynthetic activity Higher C losses dry season wet season dry season wet season dry season wet season Higher C uptake NEE = R + GEE Reduced photosynthesis (less negative)

13 What is the cause of reduced photosynthesis?
Higher C losses dry season wet season dry season wet season Higher C uptake

14 What is the cause of reduced photosynthesis?
Higher C losses Lower PAR and… dry season wet season dry season wet season Higher C uptake

15 Decreased photosynthetic response
Result 3: decreased photosynthetic response Decreased photosynthetic response Jan Higher C losses dry season wet season GEP = -GEE dry season wet season Feb Higher C uptake

16 What is the cause of reduced photosynthetic response?
Earlier onset of the wet season? High soil moisture? ….

17 Summary: at Tapajós K67 tropical forest
Result 1: La Niña Event (wet wet season and earlier onset of the wet season, corresponds to C Forest Loss. Result 2: Forest C Loss is due to reduced photosynthesis. Result 3: decreased photosynthetic response. Future work: Investigaion on the cause of reduced photosynthetic response?

18 Acknowledgments This research was funded by the National Science Foundation’s Partnerships for International Research and Education (PIRE) and the National Aeronautics and Space Administration (NASA) LBA investigation CD-32. Thank you

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