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Ecological Accomplishments of the Large Scale Biosphere- Atmosphere Experiment in Amazonia (LBA) Eric A. Davidson LBA-ECO Project Scientist The Woods Hole Research Center Lost in the Bloody Amazon? (LBA)

Lost in the Bloody Amazon? (LBA) - LCLUC Programlcluc.umd.edu/.../davidson_lcluc_apr2009_day1_presentation_0.pdf · NASA’s Terra satellite. LBA is an international, multi-disciplinary

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Ecological Accomplishments of the Large Scale Biosphere-Atmosphere Experiment in Amazonia (LBA)

Eric A. DavidsonLBA-ECO Project Scientist

The Woods Hole Research Center

Lost in the Bloody Amazon?(LBA)

Large Scale Biosphere-Atmosphere Experiment in Amazônia (LBA)

Amazônia

The Amazon region of South America as viewed by MODIS on NASA’s Terra satellite.

LBA is an international, multi-disciplinary cooperative research program led by Brazil. NASA leads the U.S. participation in LBA, working in close partnership with the Brazilian leaders and scientists.

LBA is the largest cooperative international scientific project ever to study the interaction between tropical forests and the atmosphere.

•climatological, ecological, biogeochemical, and hydrological functions of Amazônia

•impact of land use change on these functions

•interactions between Amazônia and the Earth system

LBA research is focused on producing new knowledge about the:

Low water

High water

Amazon Basin below 500m: wetlands 17%, uplands 83%

Hess et al. 2003

Methane Emissions:This 1.8 million km2 quadrant:

7 Tg C y-1

Extrapolated to basin below 500m: 22 Tg C y-1

Melack et al. 2004

Mosaicked L-band synthetic aperture radar (SAR) imagery acquired by the Japanese Earth Resources Satellite-1

Saatchi et al. 2007. Global Change Biology, 13, 816–837.

>500 plot measurements of biomass

MODIS, JERS-1,QuikSCAT, SRTM used in decision tree

Total C in Amazon Basin forest biomass (including the dead and belowground) = 86 PgC ± 20% uncertainty

Dry season precipitation is the best predictor of biomass, but unaccounted for variation may be due to soils, geomorphology, radiation hydrologic features, and management history.

Continuously wet

Long dry season

12,000-20,000 km2 y-1 logging16,000-23,000 km2 y-1 deforestation

Asner et al. Science 2005

Landsat ETM+ data analyzed with the Carnegie Landsat Analysis System (CLAS)

New INPE estimates for 2007:

Deforestation: 12,000 km2

Degradation: 15,000 km2

Distance Class from Major Roads (5 km increments)

0-5 5-10 10-15 15-20 20-25 25-30 30-35 35-40 40-45 45-50

Prop

ortio

n D

efor

este

d 4

Year

s La

ter

0.00

0.05

0.10

0.15

0.20

0.25ns

**

***

****

*** ** ns * *

0-5 5-10

10-15

15-20

20-25

25-30

30-35

35-40

40-45

45-50

Cum

ulat

ive

Prop

ortio

n of

Tot

al A

rea

0.65

0.70

0.75

0.80

0.85

0.90

0.95

1.00

Logging Intact forest

Logging Intact forest

Asner et al. PNAS 2006

32% of logged forest is cleared after 4 years

New INPE estimates:

Degradation in 2007: 15,000 km2

2007 degraded forest cleared in 2008: 1,800 km2

Distinguishing Fate of Deforestation with Phenology Derived from MODIS

Forest

Pasture CroplandPRIMARY

SECONDARY

2000-2003 Time Series, Quality flag adjusted

0

1000

2000

3000

4000

5000

6000

7000

8000

9000

10000

B1 B4 B7B10 B13 B16 B19 B22 B25 B28 B31 B34 B37 B40 B43 B46 B49 B52 B55 B58 B61 B64 B67 B70 B73 B76 B79 B82

16-day Periods (2000-129 to 2003-352)

ND

VI x

10,

000

2003 ConversionAgricultureForestPasture

Courtesy: R. DeFries

Morton et al., PNAS, 2006

Fate of deforestation from 2001-04 from MODIS phenology

~20% of deforestation in Mato Grosso is direct conversion of forest to cropland

0%10%20%30%40%50%60%70%80%

Perc

ent C

over

Mature Forest Secondary ForestPasture Other

1984

2001

1999

1994

2002

secondary forest cover secondary forest cover increased from ‘84 to ‘94 increased from ‘84 to ‘94 while mature forest cover while mature forest cover declined declined

After 1994, secondary After 1994, secondary forest cover declined forest cover declined while pasture cover while pasture cover increased. The cattle increased. The cattle herd approximately herd approximately doubled during this doubled during this period.period.

0%10%20%30%40%50%60%70%80%

Perc

ent C

over

Mature Forest Secondary ForestPasture Other

1984

2001

1999

1994

2002

secondary forest cover secondary forest cover increased from ‘84 to ‘94 increased from ‘84 to ‘94 while mature forest cover while mature forest cover declined declined

secondary forest cover secondary forest cover increased from ‘84 to ‘94 increased from ‘84 to ‘94 while mature forest cover while mature forest cover declined declined

After 1994, secondary After 1994, secondary forest cover declined forest cover declined while pasture cover while pasture cover increased. The cattle increased. The cattle herd approximately herd approximately doubled during this doubled during this period.period.

After 1994, secondary After 1994, secondary forest cover declined forest cover declined while pasture cover while pasture cover increased. The cattle increased. The cattle herd approximately herd approximately doubled during this doubled during this period.period.

An area not part of the current deforestation frontier is still losing forest cover & about 1.3 MgC ha -1 yr-1

Almeida, Stone, Vieira, and Davidson, unpublished

1995 –non-ENSO 1998 –ENSO

• Supervised classification of Landsat imagery and land owner interviews used to map fire scars.

• Results “scaled-up” using relationships of distance to roads, forest type, precipitation, and biomass estimates.

The estimated forest area burned by understory fire during the severe drought (ENSO) year (2.6 ×106 ha) was 13 times greater than during the average rainfall year (0.2 × 106 ha) and was twice the area of annual deforestation.Alencar et al. 2006. Earth Interactions 10:6

The middle and Upper Araguaia River basin showing CBERS-derived classification of remnant Cerrado (green) and altered lands (pink). About 62% of the basin vegetation and 45% of all riparian zones had been altered by 2006

• Discharge has increased by 25% since the 1970s• Simulations indicate that about 2/3 of the change in

discharge is attributable to changes in land cover

Coe, Latrubesse, Ferreira, Davidson, in review

m3/s

Topics covered here:

Wetland cover

Forest cover

Logging

Fire

Conversion to cropland

Conversion to pasture

Hydrologic consequences

Topics not covered include the consequences of the LCLUC on:

Local, regional, and global climate

Carbon and nutrient cycles

Biodiversity

Economic activity and human dimensions