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Impacts of large-scale drought and deluge on phenology and vegetation
productivity in Southeastern Australia
Xuanlong Ma1, Alfredo Huete1, Susan Moran2, Guillermo Ponce-Campos2, Derek Eamus3
1 Plant Functional Biology & Climate Change ClusterUniversity of Technology Sydney
2 Southwest Watershed Research Centre,USDA Agriculture Research Service
3 School of Life Sciences, University of Technology Sydney
6 October 2015 @ Kusadasi, Turkey
Xuanlong Ma [email protected] 1
International Conference on Phenology Impact of Climate Extremes on Phenology
MOTIVATION
Xuanlong Ma [email protected] 2
International Conference on Phenology Impact of Climate Extremes on Phenology
IN THE NEWS
Lake Hume (NSW), 2007
Credit:Tim
J Keegan
Xuanlong Ma [email protected]
Credit: Epoc Tinm
es
Stockman Gordon Litchfield at Leigh Creek (SA), 2006
33
International Conference on Phenology Impact of Climate Extremes on Phenology
Drought had significant impacts, including dramatic reduction in agricultural
production, reduced water availability for industrial and civil consumptions, increased forest die-back and bushfire (Sempel et al., 2010).
Xuanlong Ma [email protected] 44
International Conference on Phenology Impact of Climate Extremes on Phenology
There is an increasing trend in the frequency and spatial extent of extreme
climate events around globe and in Australia, yet the impacts of these extreme climate on
ecosystem function remains uncertain.
Xuanlong Ma [email protected] 55
International Conference on Phenology Impact of Climate Extremes on Phenology
Vegetation phenology and primary productivity represent key functions of an ecosystem,
potential changes in phenology and primary productivity under climate change will have
great implications to regional & global climate and biogeochemical cycles.
Xuanlong Ma [email protected] 66
International Conference on Phenology Impact of Climate Extremes on Phenology
Phenology is the study of life cycles of flora and fauna and their interactions
with seasonal and inter-annual variations in climate and other factors.
Xuanlong Ma [email protected] 77
International Conference on Phenology Impact of Climate Extremes on Phenology
Phenology is an integrative indicator of vegetation
responses to climate variability and change.
Xuanlong Ma [email protected] 88
International Conference on Phenology Impact of Climate Extremes on Phenology
Vegetation phenology and primary productivity together represent key functions of an
ecosystem.
Xuanlong Ma [email protected] 99
International Conference on Phenology Impact of Climate Extremes on Phenology
Therefore, understanding their relationships with environment is of great importance in global change studies that
aim to predict how ecosystem function will be affected by future climate changes.
Xuanlong Ma [email protected] 1010
International Conference on Phenology Impact of Climate Extremes on Phenology
Remote Sensing uses satellites to track seasonal changes in
vegetation activity on regional, continental, and global scales.
Xuanlong Ma [email protected] 1111
International Conference on Phenology Impact of Climate Extremes on Phenology
Remote sensing provide unparalleled way for detection and mapping vegetation phenological and functional responses to climate over broad-
scales, which complement the restricted coverage afforded by ground-based plots
observations.
Xuanlong Ma [email protected] 1212
International Conference on Phenology Impact of Climate Extremes on Phenology
The objective of this study is to investigate the shifts in
phenology and vegetation productivity under climatic
extremes.
Xuanlong Ma [email protected] 13
International Conference on Phenology Impact of Climate Extremes on Phenology
DATA & METHOD
Xuanlong Ma [email protected] 14
International Conference on Phenology Impact of Climate Extremes on Phenology
Southeastern Australia (SEA)
Land cover map of the SEA
Xuanlong Ma [email protected] 1515
Ma et al. (2015) JGR-Biogeosciences, in press
International Conference on Phenology Impact of Climate Extremes on Phenology
1.3 million km2
Southeastern Australia (SEA)
Land cover map of the SEA
Xuanlong Ma [email protected] 16
Martin WellsBroken Hill
Yanco
TumbarumbaWarracknabeal
16
Chowilla
Ma et al. (2015) JGR-Biogeosciences, in press
International Conference on Phenology Impact of Climate Extremes on Phenology
1.3 million km2
Satellite Data• Moderate Resolution Imaging
Spectroradiometer (MODIS) onboard NASA’s Terra satellite;
• Enhanced Vegetation Index (EVI);
• MOD13C1, 16-day, 0.05° resolution;
• 2000-2014;
• Quality Control (QC) applied.
Xuanlong Ma [email protected] 1717
International Conference on Phenology Impact of Climate Extremes on Phenology
Xuanlong Ma [email protected] 1818
International Conference on Phenology Impact of Climate Extremes on Phenology
Wavelength (microns)
Refl
ecta
nce
Xuanlong Ma [email protected] 1919
International Conference on Phenology Impact of Climate Extremes on Phenology
Wavelength (microns)
Refl
ecta
nce
Xuanlong Ma [email protected] 2020
International Conference on Phenology Impact of Climate Extremes on Phenology
Vegetation Index is based on the contrast between the reflectances at
NIR region and VIS region.
Wavelength (microns)
Refl
ecta
nce
Standardised Precipitation-Evapotranspiration Index (SPEI)
• SPEI is a multi-scaler drought index which takes into account both precipitation (P) and potential evapotranspiration (PET) in determine the drought severity (Vicente-Serrano et al., 2011);
• SPEI reflect the cumulative effect of the imbalance between atmospheric supply (P) and demand (PET);
Xuanlong Ma [email protected] 2121
International Conference on Phenology Impact of Climate Extremes on Phenology
Phenological Metrics ExtractionSeasonal maximum EVI
Prior Season Minimum EVI
10%
After Season Minimum EVI
10%
Soil background EVI = 0.08(yellow shaded area)
Annual integrated EVI (iEVI)(green shaded area)
SGS
PGS
EGSLGS●
Warracknabeal (Cropland)
0.0
0.1
0.2
0.3
0.4
0.5
Feb−2003 Apr−2003 Jun−2003 Aug−2003 Oct−2003 Dec−2003Date
EVI
Xuanlong Ma [email protected] 2222
Ma et al. (2015) JGR-Biogeosciences, in press
International Conference on Phenology Impact of Climate Extremes on Phenology
RESULTS
Xuanlong Ma [email protected] 23
International Conference on Phenology Impact of Climate Extremes on Phenology
First, we show the hydroclimatic impacts on seasonality of
vegetation growth.
Xuanlong Ma [email protected] 2424
International Conference on Phenology Impact of Climate Extremes on Phenology
Xuanlong Ma [email protected]
(a)
(b)
(c)
(d)
(e)
(f)
Tumbarumba (Wet sclerophyll forest)
Yanco (Pasture)
Chowilla (Mallee woodland)
Warracknabeal (Wheat cropland)
Broken Hill (Hummock grassland)
Martins Wells (Acacia shrublands)
−2
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−2
0
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−2
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−2
0
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−2
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2
Sep−2000 Mar−2002 Sep−2003 Mar−2005 Sep−2006 Mar−2008 Sep−2009 Mar−2011 Sep−2012Date
EVI sd
or S
PEI
SPEI Dry Wet EVI
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Tumbarumba (Wet sclerophyll forest)
Yanco (Pasture)
Chowilla (Mallee woodland)
Warracknabeal (Wheat cropland)
Broken Hill (Hummock grassland)
Martins Wells (Acacia shrublands)
0.30
0.35
0.40
0.45
0.2
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0.14
0.16
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0.20
0.1
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0.08
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0.14
0.16
0.08
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0.14
Jan Apr Jul OctDate
EVI M
OD
IS
● ●2002 (Drought) 2010 (Wet)
(a)
(b)
(c)
(d)
(e)
(f)
Tumbarumba (Wet sclerophyll forest)
Yanco (Pasture)
Chowilla (Mallee woodland)
Warracknabeal (Wheat cropland)
Broken Hill (Hummock grassland)
Martins Wells (Acacia shrublands)
−2
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Sep−2000 Mar−2002 Sep−2003 Mar−2005 Sep−2006 Mar−2008 Sep−2009 Mar−2011 Sep−2012Date
EVI sd
or S
PEI
SPEI Dry Wet EVI
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Tumbarumba (Wet sclerophyll forest)
Yanco (Pasture)
Chowilla (Mallee woodland)
Warracknabeal (Wheat cropland)
Broken Hill (Hummock grassland)
Martins Wells (Acacia shrublands)
0.30
0.35
0.40
0.45
0.2
0.3
0.4
0.5
0.14
0.16
0.18
0.20
0.1
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0.5
0.08
0.10
0.12
0.14
0.16
0.08
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0.12
0.14
Jan Apr Jul OctDate
EVI M
OD
IS
● ●2002 (Drought) 2010 (Wet)
Seasonal and inter-annual variations in EVI and SPEI at local sites, 2000-2013
2525
All sites experienced severe and protracted drought condition throughout 2002 and 2003, as indicated by consecutive negative SPEI lasted for 9 - 14 monthsMa et al. (2015) JGR-Biogeosciences, in press
International Conference on Phenology Impact of Climate Extremes on Phenology
Second, we show the biogeographical patterns in vegetation phenology and productivity across drought and wet
years
Xuanlong Ma [email protected] 2626
International Conference on Phenology Impact of Climate Extremes on Phenology
Xuanlong Ma [email protected] 27
SPEI
LGS (days)
iEVISD
27
In 2002, 87% areas of the SEA experienced drought impact, 76% areas experienced wet condition during the 2010
Ma et al. (2015) JGR-Biogeosciences, in press
International Conference on Phenology Impact of Climate Extremes on Phenology
Xuanlong Ma [email protected] 28
SPEI
LGS (days)
iEVISD
28
In 2002, 87% areas of the SEA experienced drought impact, 76% areas experienced wet condition during the 2010
Within the areas that phenology was detected during both 2002 and 2010, there was an increasing trend in LGS over
70% areas of the SEA in the wet year.
Ma et al. (2015) JGR-Biogeosciences, in press
International Conference on Phenology Impact of Climate Extremes on Phenology
Xuanlong Ma [email protected] 29
SPEI
LGS (days)
iEVISD
29
Region-wide averaged productivity was reduced by 21% in the 2002 drought year and was increased by 20% in the
2010 wet year relative to 2000-2013 average.
In 2002, 87% areas of the SEA experienced drought impact, 76% areas experienced wet condition during the 2010
Within the areas that phenology was detected during both 2002 and 2010, there was an increasing trend in LGS over
70% areas of the SEA in the wet year.
Ma et al. (2015) JGR-Biogeosciences, in press
International Conference on Phenology Impact of Climate Extremes on Phenology
Quite dramatically, we found drought resulted in widespread reduction or
collapse in seasonality, associated with no detectable phenology over vast
drylands ecosystems.
Xuanlong Ma [email protected] 3030
International Conference on Phenology Impact of Climate Extremes on Phenology
Xuanlong Ma [email protected] 3131
Ma et al. (2015) JGR-Biogeosciences, in press
International Conference on Phenology Impact of Climate Extremes on Phenology
Xuanlong Ma [email protected] 32
2002 drought year
2010 wet year
2002 drought year
2010 wet year
EVI
32
Ma et al. (2015) JGR-Biogeosciences, in press
International Conference on Phenology Impact of Climate Extremes on Phenology
Xuanlong Ma [email protected] 33
2002 drought year
2010 wet year
2002 drought year
2010 wet year
EVI
33
Ma et al. (2015) JGR-Biogeosciences, in press
International Conference on Phenology Impact of Climate Extremes on Phenology
Length of greening season > 6 months in normal or wet year
Xuanlong Ma [email protected] 34
2002 drought year
2010 wet year
2002 drought year
2010 wet year
EVI
34
Ma et al. (2015) JGR-Biogeosciences, in press
International Conference on Phenology Impact of Climate Extremes on Phenology
Length of greening season = 0 day in drought year
Length of greening season > 6 months in normal or wet year
DISCUSSIONS
Xuanlong Ma [email protected] 35
International Conference on Phenology Impact of Climate Extremes on Phenology
First…
Xuanlong Ma [email protected] 3636
International Conference on Phenology Impact of Climate Extremes on Phenology
Phenology: the study of periodic plant and animal life
cycle events.
Xuanlong Ma [email protected] 3737
International Conference on Phenology Impact of Climate Extremes on Phenology
In temperate ecosystems, phenology profile as observed from satellite sensors normally
looks like…
Xuanlong Ma [email protected]
Trends in Environmental Research Series (TIERS) 8 April 2015
3838
International Conference on Phenology Impact of Climate Extremes on Phenology
Xuanlong Ma [email protected]
Harvard Forest, MA, USA, deciduous broadleaf forest Fisher & Mustad, 2007
Hmimina et al., 2013
Trends in Environmental Research Series (TIERS) 8 April 2015
3939
International Conference on Phenology Impact of Climate Extremes on Phenology
Xuanlong Ma [email protected]
Harvard Forest, MA, USA, deciduous broadleaf forest Fisher & Mustad, 2007
Fontainebleau, France, deciduous broadleaf forest Hmimina et al., 2013
Trends in Environmental Research Series (TIERS) 8 April 2015
4040
International Conference on Phenology Impact of Climate Extremes on Phenology
Xuanlong Ma [email protected]
Harvard Forest, MA, USA, deciduous broadleaf forest Fisher & Mustad, 2007
Fontainebleau, France, deciduous broadleaf forest Hmimina et al., 2013
Darwin, NT, Australia, tropical savanna Ma et al., 2013
4141
International Conference on Phenology Impact of Climate Extremes on Phenology
However, we found under highly variable climate, such as in Australia, phenology profile
looks like…
Xuanlong Ma [email protected] 4242
International Conference on Phenology Impact of Climate Extremes on Phenology
Xuanlong Ma [email protected]
(a)
(b)
(c)
(d)
(e)
(f)
Tumbarumba (Wet sclerophyll forest)
Yanco (Pasture)
Chowilla (Mallee woodland)
Warracknabeal (Wheat cropland)
Broken Hill (Hummock grassland)
Martins Wells (Acacia shrublands)
−2
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Sep−2000 Mar−2002 Sep−2003 Mar−2005 Sep−2006 Mar−2008 Sep−2009 Mar−2011 Sep−2012Date
EVI sd
or S
PEI
SPEI Dry Wet EVI
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Tumbarumba (Wet sclerophyll forest)
Yanco (Pasture)
Chowilla (Mallee woodland)
Warracknabeal (Wheat cropland)
Broken Hill (Hummock grassland)
Martins Wells (Acacia shrublands)
0.30
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0.40
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0.14
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0.20
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0.5
0.08
0.10
0.12
0.14
0.16
0.08
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0.12
0.14
Jan Apr Jul OctDate
EVI M
OD
IS
● ●2002 (Drought) 2010 (Wet)
(a)
(b)
(c)
(d)
(e)
(f)
Tumbarumba (Wet sclerophyll forest)
Yanco (Pasture)
Chowilla (Mallee woodland)
Warracknabeal (Wheat cropland)
Broken Hill (Hummock grassland)
Martins Wells (Acacia shrublands)
−2
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Sep−2000 Mar−2002 Sep−2003 Mar−2005 Sep−2006 Mar−2008 Sep−2009 Mar−2011 Sep−2012Date
EVI sd
or S
PEI
SPEI Dry Wet EVI
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Tumbarumba (Wet sclerophyll forest)
Yanco (Pasture)
Chowilla (Mallee woodland)
Warracknabeal (Wheat cropland)
Broken Hill (Hummock grassland)
Martins Wells (Acacia shrublands)
0.30
0.35
0.40
0.45
0.2
0.3
0.4
0.5
0.14
0.16
0.18
0.20
0.1
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0.4
0.5
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0.10
0.12
0.14
0.16
0.08
0.10
0.12
0.14
Jan Apr Jul OctDate
EVI M
OD
IS
● ●2002 (Drought) 2010 (Wet)
(a)
(b)
(c)
(d)
(e)
(f)
Tumbarumba (Wet sclerophyll forest)
Yanco (Pasture)
Chowilla (Mallee woodland)
Warracknabeal (Wheat cropland)
Broken Hill (Hummock grassland)
Martins Wells (Acacia shrublands)
−2
0
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−2
0
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−2
0
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−2
0
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0
2
Sep−2000 Mar−2002 Sep−2003 Mar−2005 Sep−2006 Mar−2008 Sep−2009 Mar−2011 Sep−2012Date
EVI sd
or S
PEI
SPEI Dry Wet EVI
●
●
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● ● ● ● ● ● ● ● ● ● ● ● ● ● ●●
●
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●
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●
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● ● ●●
●
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●
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●
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● ● ●● ●
●●
●● ●
●
●●
●
● ●
● ●
●
●
●
●● ●
●
●
●
●
●
●
●
●
●
Tumbarumba (Wet sclerophyll forest)
Yanco (Pasture)
Chowilla (Mallee woodland)
Warracknabeal (Wheat cropland)
Broken Hill (Hummock grassland)
Martins Wells (Acacia shrublands)
0.30
0.35
0.40
0.45
0.2
0.3
0.4
0.5
0.14
0.16
0.18
0.20
0.1
0.2
0.3
0.4
0.5
0.08
0.10
0.12
0.14
0.16
0.08
0.10
0.12
0.14
Jan Apr Jul OctDate
EVI M
OD
IS
● ●2002 (Drought) 2010 (Wet)
(a)
(b)
(c)
(d)
(e)
(f)
Tumbarumba (Wet sclerophyll forest)
Yanco (Pasture)
Chowilla (Mallee woodland)
Warracknabeal (Wheat cropland)
Broken Hill (Hummock grassland)
Martins Wells (Acacia shrublands)
−2
0
2
−2
0
2
−2
0
2
−2
0
2
−2
0
2
−2
0
2
Sep−2000 Mar−2002 Sep−2003 Mar−2005 Sep−2006 Mar−2008 Sep−2009 Mar−2011 Sep−2012Date
EVI sd
or S
PEI
SPEI Dry Wet EVI
●
●
● ●
●
●
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●
●
●
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●
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● ● ● ● ● ● ● ● ● ● ● ● ● ● ●●
●
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●●
●
●● ● ●
● ● ●●
●
●● ●
●
●
● ●● ● ● ●
●
●●
● ●● ●
● ● ●● ●
●●
●● ●
●
●●
●
● ●
● ●
●
●
●
●● ●
●
●
●
●
●
●
●
●
●
Tumbarumba (Wet sclerophyll forest)
Yanco (Pasture)
Chowilla (Mallee woodland)
Warracknabeal (Wheat cropland)
Broken Hill (Hummock grassland)
Martins Wells (Acacia shrublands)
0.30
0.35
0.40
0.45
0.2
0.3
0.4
0.5
0.14
0.16
0.18
0.20
0.1
0.2
0.3
0.4
0.5
0.08
0.10
0.12
0.14
0.16
0.08
0.10
0.12
0.14
Jan Apr Jul OctDate
EVI M
OD
IS
● ●2002 (Drought) 2010 (Wet)
4343
Ma et al. (2015) JGR-Biogeosciences, in press
International Conference on Phenology Impact of Climate Extremes on Phenology
Xuanlong Ma [email protected]
(a)
(b)
(c)
(d)
(e)
(f)
Tumbarumba (Wet sclerophyll forest)
Yanco (Pasture)
Chowilla (Mallee woodland)
Warracknabeal (Wheat cropland)
Broken Hill (Hummock grassland)
Martins Wells (Acacia shrublands)
−2
0
2
−2
0
2
−2
0
2
−2
0
2
−2
0
2
−2
0
2
Sep−2000 Mar−2002 Sep−2003 Mar−2005 Sep−2006 Mar−2008 Sep−2009 Mar−2011 Sep−2012Date
EVI sd
or S
PEI
SPEI Dry Wet EVI
●
●
● ●
●
●
●●
●
●
●
●
●
●
●
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● ● ● ● ● ● ● ● ● ● ● ●●
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● ● ● ● ● ● ● ● ● ● ● ● ● ● ●●
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● ● ●● ●
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●
●●
●
● ●
● ●
●
●
●
●● ●
●
●
●
●
●
●
●
●
●
Tumbarumba (Wet sclerophyll forest)
Yanco (Pasture)
Chowilla (Mallee woodland)
Warracknabeal (Wheat cropland)
Broken Hill (Hummock grassland)
Martins Wells (Acacia shrublands)
0.30
0.35
0.40
0.45
0.2
0.3
0.4
0.5
0.14
0.16
0.18
0.20
0.1
0.2
0.3
0.4
0.5
0.08
0.10
0.12
0.14
0.16
0.08
0.10
0.12
0.14
Jan Apr Jul OctDate
EVI M
OD
IS
● ●2002 (Drought) 2010 (Wet)
(a)
(b)
(c)
(d)
(e)
(f)
Tumbarumba (Wet sclerophyll forest)
Yanco (Pasture)
Chowilla (Mallee woodland)
Warracknabeal (Wheat cropland)
Broken Hill (Hummock grassland)
Martins Wells (Acacia shrublands)
−2
0
2
−2
0
2
−2
0
2
−2
0
2
−2
0
2
−2
0
2
Sep−2000 Mar−2002 Sep−2003 Mar−2005 Sep−2006 Mar−2008 Sep−2009 Mar−2011 Sep−2012Date
EVI sd
or S
PEI
SPEI Dry Wet EVI
●
●
● ●
●
●
●●
●
●
●
●
●
●
●
●●
●
●●
●
●
●●
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●● ●
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●
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●
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●● ●
●●
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● ● ●●
● ● ●
● ● ● ● ●● ● ● ●
● ● ● ● ●
●
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●
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●
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●
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●
● ●
● ●
●
●
● ● ● ● ● ● ● ● ● ● ● ●●
● ● ●● ●
●● ● ● ●
●● ● ●
● ● ● ● ● ●●
●
●
●
●
●
● ●
●
●
●
● ●
● ● ● ● ● ● ●●
● ● ● ● ● ● ● ● ● ● ● ● ● ● ●●
●
●
●
●
●
●●
●
●● ● ●
● ● ●●
●
●● ●
●
●
● ●● ● ● ●
●
●●
● ●● ●
● ● ●● ●
●●
●● ●
●
●●
●
● ●
● ●
●
●
●
●● ●
●
●
●
●
●
●
●
●
●
Tumbarumba (Wet sclerophyll forest)
Yanco (Pasture)
Chowilla (Mallee woodland)
Warracknabeal (Wheat cropland)
Broken Hill (Hummock grassland)
Martins Wells (Acacia shrublands)
0.30
0.35
0.40
0.45
0.2
0.3
0.4
0.5
0.14
0.16
0.18
0.20
0.1
0.2
0.3
0.4
0.5
0.08
0.10
0.12
0.14
0.16
0.08
0.10
0.12
0.14
Jan Apr Jul OctDate
EVI M
OD
IS
● ●2002 (Drought) 2010 (Wet)
(a)
(b)
(c)
(d)
(e)
(f)
Tumbarumba (Wet sclerophyll forest)
Yanco (Pasture)
Chowilla (Mallee woodland)
Warracknabeal (Wheat cropland)
Broken Hill (Hummock grassland)
Martins Wells (Acacia shrublands)
−2
0
2
−2
0
2
−2
0
2
−2
0
2
−2
0
2
−2
0
2
Sep−2000 Mar−2002 Sep−2003 Mar−2005 Sep−2006 Mar−2008 Sep−2009 Mar−2011 Sep−2012Date
EVI sd
or S
PEI
SPEI Dry Wet EVI
●
●
● ●
●
●
●●
●
●
●
●
●
●
●
●●
●
●●
●
●
●●
●
●
●●
●●
●● ●
●
●
●
●
● ●
●
●
●
●
●
●
●
● ●
●
●
●● ●
●●
●●
● ● ●●
● ● ●
● ● ● ● ●● ● ● ●
● ● ● ● ●
●
●
●
●
●●
● ●
●
●
●
●
● ●
●
●
●
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●●
●
●
●
●
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●●
●
●
● ●
●●
●
●●
●●●
●
●
● ●● ● ●
●
● ●●
●
●
●
●
● ●
● ●
●
●
● ● ● ● ● ● ● ● ● ● ● ●●
● ● ●● ●
●● ● ● ●
●● ● ●
● ● ● ● ● ●●
●
●
●
●
●
● ●
●
●
●
● ●
● ● ● ● ● ● ●●
● ● ● ● ● ● ● ● ● ● ● ● ● ● ●●
●
●
●
●
●
●●
●
●● ● ●
● ● ●●
●
●● ●
●
●
● ●● ● ● ●
●
●●
● ●● ●
● ● ●● ●
●●
●● ●
●
●●
●
● ●
● ●
●
●
●
●● ●
●
●
●
●
●
●
●
●
●
Tumbarumba (Wet sclerophyll forest)
Yanco (Pasture)
Chowilla (Mallee woodland)
Warracknabeal (Wheat cropland)
Broken Hill (Hummock grassland)
Martins Wells (Acacia shrublands)
0.30
0.35
0.40
0.45
0.2
0.3
0.4
0.5
0.14
0.16
0.18
0.20
0.1
0.2
0.3
0.4
0.5
0.08
0.10
0.12
0.14
0.16
0.08
0.10
0.12
0.14
Jan Apr Jul OctDate
EVI M
OD
IS
● ●2002 (Drought) 2010 (Wet)
(a)
(b)
(c)
(d)
(e)
(f)
Tumbarumba (Wet sclerophyll forest)
Yanco (Pasture)
Chowilla (Mallee woodland)
Warracknabeal (Wheat cropland)
Broken Hill (Hummock grassland)
Martins Wells (Acacia shrublands)
−2
0
2
−2
0
2
−2
0
2
−2
0
2
−2
0
2
−2
0
2
Sep−2000 Mar−2002 Sep−2003 Mar−2005 Sep−2006 Mar−2008 Sep−2009 Mar−2011 Sep−2012Date
EVI sd
or S
PEI
SPEI Dry Wet EVI
●
●
● ●
●
●
●●
●
●
●
●
●
●
●
●●
●
●●
●
●
●●
●
●
●●
●●
●● ●
●
●
●
●
● ●
●
●
●
●
●
●
●
● ●
●
●
●● ●
●●
●●
● ● ●●
● ● ●
● ● ● ● ●● ● ● ●
● ● ● ● ●
●
●
●
●
●●
● ●
●
●
●
●
● ●
●
●
●
●
●●
●
●
●
●
●
●●
●
●
● ●
●●
●
●●
●●●
●
●
● ●● ● ●
●
● ●●
●
●
●
●
● ●
● ●
●
●
● ● ● ● ● ● ● ● ● ● ● ●●
● ● ●● ●
●● ● ● ●
●● ● ●
● ● ● ● ● ●●
●
●
●
●
●
● ●
●
●
●
● ●
● ● ● ● ● ● ●●
● ● ● ● ● ● ● ● ● ● ● ● ● ● ●●
●
●
●
●
●
●●
●
●● ● ●
● ● ●●
●
●● ●
●
●
● ●● ● ● ●
●
●●
● ●● ●
● ● ●● ●
●●
●● ●
●
●●
●
● ●
● ●
●
●
●
●● ●
●
●
●
●
●
●
●
●
●
Tumbarumba (Wet sclerophyll forest)
Yanco (Pasture)
Chowilla (Mallee woodland)
Warracknabeal (Wheat cropland)
Broken Hill (Hummock grassland)
Martins Wells (Acacia shrublands)
0.30
0.35
0.40
0.45
0.2
0.3
0.4
0.5
0.14
0.16
0.18
0.20
0.1
0.2
0.3
0.4
0.5
0.08
0.10
0.12
0.14
0.16
0.08
0.10
0.12
0.14
Jan Apr Jul OctDate
EVI M
OD
IS
● ●2002 (Drought) 2010 (Wet)
Yanco, NSW (Pasture)
Warracknabeal, VIC (Wheat crop)
Broken Hill, NSW (Hummock grass)
Martin Wells, SA (Acacia shrubland)
Red: 2002 Blue: 2010
4444
Ma et al. (2015) JGR-Biogeosciences, in press
International Conference on Phenology Impact of Climate Extremes on Phenology
Finding #1
Xuanlong Ma [email protected] 4545
International Conference on Phenology Impact of Climate Extremes on Phenology
Phenology is not repeated event, at least for Australia’s
dryland ecosystems.
Xuanlong Ma [email protected]
Trends in Environmental Research Series (TIERS) 8 April 2015
46
Trends in Environmental Research Series (TIERS) Impact of Climate Extremes on Terrestrial Ecosystems
46
International Conference on Phenology Impact of Climate Extremes on Phenology
Drought resulted in widespread reductions or collapse in the normal patterns of seasonality such that in many cases there was no detectable
phenological cycle during drought years.
Xuanlong Ma [email protected]
Trends in Environmental Research Series (TIERS) 8 April 2015
47
Trends in Environmental Research Series (TIERS) Impact of Climate Extremes on Terrestrial Ecosystems
47
International Conference on Phenology Impact of Climate Extremes on Phenology
Implication of finding #1
Xuanlong Ma [email protected]
Trends in Environmental Research Series (TIERS) 8 April 2015
48
Trends in Environmental Research Series (TIERS) Impact of Climate Extremes on Terrestrial Ecosystems
48
International Conference on Phenology Impact of Climate Extremes on Phenology
The direction of the gradual shifting in ecosystem function and structure as induced by
global change (e.g., warming and CO2 fertilisation effect) in a long-run might be
suddenly altered, or even reversed direction, by short-term extreme climatic events.
Xuanlong Ma [email protected]
Trends in Environmental Research Series (TIERS) 8 April 2015
49
Trends in Environmental Research Series (TIERS) Impact of Climate Extremes on Terrestrial Ecosystems
49
International Conference on Phenology Impact of Climate Extremes on Phenology
Our findings highlight the need for models to explicitly take into account
climate-induced abrupt shifts in phenology and productivity for
predicting future ecosystem states, particularly in global semi-arid and arid regions where climate is highly
variable and vegetation growth is not or less limited by temperature but rather limited by water-availability.
Xuanlong Ma [email protected]
Trends in Environmental Research Series (TIERS) 8 April 2015
50
Trends in Environmental Research Series (TIERS) Impact of Climate Extremes on Terrestrial Ecosystems
50
International Conference on Phenology Impact of Climate Extremes on Phenology
Second…
Xuanlong Ma [email protected]
Trends in Environmental Research Series (TIERS) 8 April 2015
51
Trends in Environmental Research Series (TIERS) Impact of Climate Extremes on Terrestrial Ecosystems
51
International Conference on Phenology Impact of Climate Extremes on Phenology
Agricultural ecosystems, including cropland and
pastures, are important…
Xuanlong Ma [email protected]
Trends in Environmental Research Series (TIERS) 8 April 2015
52
Trends in Environmental Research Series (TIERS) Impact of Climate Extremes on Terrestrial Ecosystems
52
International Conference on Phenology Impact of Climate Extremes on Phenology
However, we found…
Xuanlong Ma [email protected]
Trends in Environmental Research Series (TIERS) 8 April 2015
53
Trends in Environmental Research Series (TIERS) Impact of Climate Extremes on Terrestrial Ecosystems
53
International Conference on Phenology Impact of Climate Extremes on Phenology
Xuanlong Ma [email protected]
(a)
(b)
(c)
(d)
(e)
(f)
Tumbarumba (Wet sclerophyll forest)
Yanco (Pasture)
Chowilla (Mallee woodland)
Warracknabeal (Wheat cropland)
Broken Hill (Hummock grassland)
Martins Wells (Acacia shrublands)
−2
0
2
−2
0
2
−2
0
2
−2
0
2
−2
0
2
−2
0
2
Sep−2000 Mar−2002 Sep−2003 Mar−2005 Sep−2006 Mar−2008 Sep−2009 Mar−2011 Sep−2012Date
EVI sd
or S
PEI
SPEI Dry Wet EVI
●
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●
●
Tumbarumba (Wet sclerophyll forest)
Yanco (Pasture)
Chowilla (Mallee woodland)
Warracknabeal (Wheat cropland)
Broken Hill (Hummock grassland)
Martins Wells (Acacia shrublands)
0.30
0.35
0.40
0.45
0.2
0.3
0.4
0.5
0.14
0.16
0.18
0.20
0.1
0.2
0.3
0.4
0.5
0.08
0.10
0.12
0.14
0.16
0.08
0.10
0.12
0.14
Jan Apr Jul OctDate
EVI M
OD
IS
● ●2002 (Drought) 2010 (Wet)
(a)
(b)
(c)
(d)
(e)
(f)
Tumbarumba (Wet sclerophyll forest)
Yanco (Pasture)
Chowilla (Mallee woodland)
Warracknabeal (Wheat cropland)
Broken Hill (Hummock grassland)
Martins Wells (Acacia shrublands)
−2
0
2
−2
0
2
−2
0
2
−2
0
2
−2
0
2
−2
0
2
Sep−2000 Mar−2002 Sep−2003 Mar−2005 Sep−2006 Mar−2008 Sep−2009 Mar−2011 Sep−2012Date
EVI sd
or S
PEI
SPEI Dry Wet EVI
●
●
● ●
●
●
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● ● ● ● ● ● ● ● ● ● ● ● ● ● ●●
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● ●
●
●
●
●● ●
●
●
●
●
●
●
●
●
●
Tumbarumba (Wet sclerophyll forest)
Yanco (Pasture)
Chowilla (Mallee woodland)
Warracknabeal (Wheat cropland)
Broken Hill (Hummock grassland)
Martins Wells (Acacia shrublands)
0.30
0.35
0.40
0.45
0.2
0.3
0.4
0.5
0.14
0.16
0.18
0.20
0.1
0.2
0.3
0.4
0.5
0.08
0.10
0.12
0.14
0.16
0.08
0.10
0.12
0.14
Jan Apr Jul OctDate
EVI M
OD
IS
● ●2002 (Drought) 2010 (Wet)
Red: 2002 Blue: 2010
Victoria wheat belt
Trends in Environmental Research Series (TIERS) 8 April 2015
54
Trends in Environmental Research Series (TIERS) Impact of Climate Extremes on Terrestrial Ecosystems
54
Yanco
Warracknabeal
Ma et al. (2015) JGR-Biogeosciences, in press
International Conference on Phenology Impact of Climate Extremes on Phenology
Xuanlong Ma [email protected]
(a)
(b)
(c)
(d)
(e)
(f)
Tumbarumba (Wet sclerophyll forest)
Yanco (Pasture)
Chowilla (Mallee woodland)
Warracknabeal (Wheat cropland)
Broken Hill (Hummock grassland)
Martins Wells (Acacia shrublands)
−2
0
2
−2
0
2
−2
0
2
−2
0
2
−2
0
2
−2
0
2
Sep−2000 Mar−2002 Sep−2003 Mar−2005 Sep−2006 Mar−2008 Sep−2009 Mar−2011 Sep−2012Date
EVI sd
or S
PEI
SPEI Dry Wet EVI
●
●
● ●
●
●
●●
●
●
●
●
●
●
●
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● ● ●● ●
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●●
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● ●
●
●
●
●● ●
●
●
●
●
●
●
●
●
●
Tumbarumba (Wet sclerophyll forest)
Yanco (Pasture)
Chowilla (Mallee woodland)
Warracknabeal (Wheat cropland)
Broken Hill (Hummock grassland)
Martins Wells (Acacia shrublands)
0.30
0.35
0.40
0.45
0.2
0.3
0.4
0.5
0.14
0.16
0.18
0.20
0.1
0.2
0.3
0.4
0.5
0.08
0.10
0.12
0.14
0.16
0.08
0.10
0.12
0.14
Jan Apr Jul OctDate
EVI M
OD
IS
● ●2002 (Drought) 2010 (Wet)
(a)
(b)
(c)
(d)
(e)
(f)
Tumbarumba (Wet sclerophyll forest)
Yanco (Pasture)
Chowilla (Mallee woodland)
Warracknabeal (Wheat cropland)
Broken Hill (Hummock grassland)
Martins Wells (Acacia shrublands)
−2
0
2
−2
0
2
−2
0
2
−2
0
2
−2
0
2
−2
0
2
Sep−2000 Mar−2002 Sep−2003 Mar−2005 Sep−2006 Mar−2008 Sep−2009 Mar−2011 Sep−2012Date
EVI sd
or S
PEI
SPEI Dry Wet EVI
●
●
● ●
●
●
●●
●
●
●
●
●
●
●
●●
●
●●
●
●
●●
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●
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●
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●
● ●
●
●
●● ●
●●
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● ● ●●
● ● ●
● ● ● ● ●● ● ● ●
● ● ● ● ●
●
●
●
●
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●
●
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●
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●
●
● ●● ● ●
●
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●
●
●
●
● ●
● ●
●
●
● ● ● ● ● ● ● ● ● ● ● ●●
● ● ●● ●
●● ● ● ●
●● ● ●
● ● ● ● ● ●●
●
●
●
●
●
● ●
●
●
●
● ●
● ● ● ● ● ● ●●
● ● ● ● ● ● ● ● ● ● ● ● ● ● ●●
●
●
●
●
●
●●
●
●● ● ●
● ● ●●
●
●● ●
●
●
● ●● ● ● ●
●
●●
● ●● ●
● ● ●● ●
●●
●● ●
●
●●
●
● ●
● ●
●
●
●
●● ●
●
●
●
●
●
●
●
●
●
Tumbarumba (Wet sclerophyll forest)
Yanco (Pasture)
Chowilla (Mallee woodland)
Warracknabeal (Wheat cropland)
Broken Hill (Hummock grassland)
Martins Wells (Acacia shrublands)
0.30
0.35
0.40
0.45
0.2
0.3
0.4
0.5
0.14
0.16
0.18
0.20
0.1
0.2
0.3
0.4
0.5
0.08
0.10
0.12
0.14
0.16
0.08
0.10
0.12
0.14
Jan Apr Jul OctDate
EVI M
OD
IS
● ●2002 (Drought) 2010 (Wet)
Red: 2002 Blue: 2010
Victoria wheat belt “We want to see the Murray flow.” NSW farmer Gilbert Bain is harvesting
his withered wheat near Deniliquin.
Trends in Environmental Research Series (TIERS) 8 April 2015
55
Trends in Environmental Research Series (TIERS) Impact of Climate Extremes on Terrestrial Ecosystems
55
Yanco
Warracknabeal
Ma et al. (2015) JGR-Biogeosciences, in press
International Conference on Phenology Impact of Climate Extremes on Phenology
Xuanlong Ma [email protected]
(a) (b) (c)
(d) (e) (f)
(g) (h) (i)
Rainfed Cropland Rainfed Pasture Tussock Grassland
Hummock Grassland Shrubland Closed Forest
Open Forest Open Woodland Woodland
0.0
0.5
1.0
1.5
0.0
0.5
1.0
1.5
012345
0
1
2
3
0
1
2
0.0
0.3
0.6
0.9
1.2
0.0
0.3
0.6
0.9
0
1
2
3
4
0.0
0.5
1.0
1.5
−2 0 2 −2 0 2 −2 0 2∆iEVIsd or ∆SPEI
Den
sity
iEVI SPEI
2002 − Mean 2010 − Mean
(a) (b) (c)
(d) (e) (f)
(g) (h) (i)
Rainfed Cropland Rainfed Pasture Tussock Grassland
Hummock Grassland Shrubland Closed Forest
Open Forest Open Woodland Woodland
0.0
0.5
1.0
1.5
0.0
0.5
1.0
1.5
012345
0
1
2
3
0
1
2
0.0
0.3
0.6
0.9
1.2
0.0
0.3
0.6
0.9
0
1
2
3
4
0.0
0.5
1.0
1.5
−2 0 2 −2 0 2 −2 0 2∆iEVIsd or ∆SPEI
Den
sity
iEVI SPEI
2002 − Mean 2010 − Mean
(a) (b) (c)
(d) (e) (f)
(g) (h) (i)
Rainfed Cropland Rainfed Pasture Tussock Grassland
Hummock Grassland Shrubland Closed Forest
Open Forest Open Woodland Woodland
0.0
0.5
1.0
1.5
0.0
0.5
1.0
1.5
012345
0
1
2
3
0
1
2
0.0
0.3
0.6
0.9
1.2
0.0
0.3
0.6
0.9
0
1
2
3
4
0.0
0.5
1.0
1.5
−2 0 2 −2 0 2 −2 0 2∆iEVIsd or ∆SPEI
Den
sity
iEVI SPEI
2002 − Mean 2010 − Mean
(a) (b) (c)
(d) (e) (f)
(g) (h) (i)
Rainfed Cropland Rainfed Pasture Tussock Grassland
Hummock Grassland Shrubland Closed Forest
Open Forest Open Woodland Woodland
0.0
0.5
1.0
1.5
0.0
0.5
1.0
1.5
012345
0
1
2
3
0
1
2
0.0
0.3
0.6
0.9
1.2
0.0
0.3
0.6
0.9
0
1
2
3
4
0.0
0.5
1.0
1.5
−2 0 2 −2 0 2 −2 0 2∆iEVIsd or ∆SPEI
Den
sity
iEVI SPEI
2002 − Mean 2010 − Mean
(a) (b) (c)
(d) (e) (f)
(g) (h) (i)
Rainfed Cropland Rainfed Pasture Tussock Grassland
Hummock Grassland Shrubland Closed Forest
Open Forest Open Woodland Woodland
0.0
0.5
1.0
1.5
0.0
0.5
1.0
1.5
012345
0
1
2
3
0
1
2
0.0
0.3
0.6
0.9
1.2
0.0
0.3
0.6
0.9
0
1
2
3
4
0.0
0.5
1.0
1.5
−2 0 2 −2 0 2 −2 0 2∆iEVIsd or ∆SPEI
Den
sity
iEVI SPEI
2002 − Mean 2010 − Mean
Red: 2002 Blue: 2010
Negative impact of drought was amplified by cropland
Trends in Environmental Research Series (TIERS) 8 April 2015
56
Trends in Environmental Research Series (TIERS) Impact of Climate Extremes on Terrestrial Ecosystems
56
Ma et al. (2015) JGR-Biogeosciences, in press
International Conference on Phenology Impact of Climate Extremes on Phenology
Xuanlong Ma [email protected]
(a) (b) (c)
(d) (e) (f)
(g) (h) (i)
Rainfed Cropland Rainfed Pasture Tussock Grassland
Hummock Grassland Shrubland Closed Forest
Open Forest Open Woodland Woodland
0.0
0.5
1.0
1.5
0.0
0.5
1.0
1.5
012345
0
1
2
3
0
1
2
0.0
0.3
0.6
0.9
1.2
0.0
0.3
0.6
0.9
0
1
2
3
4
0.0
0.5
1.0
1.5
−2 0 2 −2 0 2 −2 0 2∆iEVIsd or ∆SPEI
Den
sity
iEVI SPEI
2002 − Mean 2010 − Mean
(a) (b) (c)
(d) (e) (f)
(g) (h) (i)
Rainfed Cropland Rainfed Pasture Tussock Grassland
Hummock Grassland Shrubland Closed Forest
Open Forest Open Woodland Woodland
0.0
0.5
1.0
1.5
0.0
0.5
1.0
1.5
012345
0
1
2
3
0
1
2
0.0
0.3
0.6
0.9
1.2
0.0
0.3
0.6
0.9
0
1
2
3
4
0.0
0.5
1.0
1.5
−2 0 2 −2 0 2 −2 0 2∆iEVIsd or ∆SPEI
Den
sity
iEVI SPEI
2002 − Mean 2010 − Mean
(a) (b) (c)
(d) (e) (f)
(g) (h) (i)
Rainfed Cropland Rainfed Pasture Tussock Grassland
Hummock Grassland Shrubland Closed Forest
Open Forest Open Woodland Woodland
0.0
0.5
1.0
1.5
0.0
0.5
1.0
1.5
012345
0
1
2
3
0
1
2
0.0
0.3
0.6
0.9
1.2
0.0
0.3
0.6
0.9
0
1
2
3
4
0.0
0.5
1.0
1.5
−2 0 2 −2 0 2 −2 0 2∆iEVIsd or ∆SPEI
Den
sity
iEVI SPEI
2002 − Mean 2010 − Mean
(a) (b) (c)
(d) (e) (f)
(g) (h) (i)
Rainfed Cropland Rainfed Pasture Tussock Grassland
Hummock Grassland Shrubland Closed Forest
Open Forest Open Woodland Woodland
0.0
0.5
1.0
1.5
0.0
0.5
1.0
1.5
012345
0
1
2
3
0
1
2
0.0
0.3
0.6
0.9
1.2
0.0
0.3
0.6
0.9
0
1
2
3
4
0.0
0.5
1.0
1.5
−2 0 2 −2 0 2 −2 0 2∆iEVIsd or ∆SPEI
Den
sity
iEVI SPEI
2002 − Mean 2010 − Mean
(a) (b) (c)
(d) (e) (f)
(g) (h) (i)
Rainfed Cropland Rainfed Pasture Tussock Grassland
Hummock Grassland Shrubland Closed Forest
Open Forest Open Woodland Woodland
0.0
0.5
1.0
1.5
0.0
0.5
1.0
1.5
012345
0
1
2
3
0
1
2
0.0
0.3
0.6
0.9
1.2
0.0
0.3
0.6
0.9
0
1
2
3
4
0.0
0.5
1.0
1.5
−2 0 2 −2 0 2 −2 0 2∆iEVIsd or ∆SPEI
Den
sity
iEVI SPEI
2002 − Mean 2010 − Mean
Red: 2002 Blue: 2010
Negative impact of drought was amplified by cropland
Trends in Environmental Research Series (TIERS) 8 April 2015
57
Trends in Environmental Research Series (TIERS) Impact of Climate Extremes on Terrestrial Ecosystems
57
Native dryland vegetation buffered drought impact
very well Ma et al. (2015) JGR-Biogeosciences, in press
International Conference on Phenology Impact of Climate Extremes on Phenology
Finding #2:
Xuanlong Ma [email protected]
Trends in Environmental Research Series (TIERS) 8 April 2015
58
Trends in Environmental Research Series (TIERS) Impact of Climate Extremes on Terrestrial Ecosystems
58
International Conference on Phenology Impact of Climate Extremes on Phenology
SE Australia’s agricultural ecosystems, including cropland and
pastures, didn’t buffer drought impact as good as native
vegetations.
Xuanlong Ma [email protected]
Trends in Environmental Research Series (TIERS) 8 April 2015
59
Trends in Environmental Research Series (TIERS) Impact of Climate Extremes on Terrestrial Ecosystems
59
International Conference on Phenology Impact of Climate Extremes on Phenology
In a climate change perspective, predicted increases in drought
frequency and intensity will have great impact on Australia’s
agricultural ecosystems, resulted in a series of consequences, such as crop failures, forage loss, and
pasture degradation.
Xuanlong Ma [email protected]
Trends in Environmental Research Series (TIERS) 8 April 2015
60
Trends in Environmental Research Series (TIERS) Impact of Climate Extremes on Terrestrial Ecosystems
60
International Conference on Phenology Impact of Climate Extremes on Phenology
These pose concerns on their sustainable ability to support human livelihood and social
functioning, and suggested that improved management and
adaption strategies should be strengthened in these areas of
concerns.
Xuanlong Ma [email protected]
Trends in Environmental Research Series (TIERS) 8 April 2015
61
Trends in Environmental Research Series (TIERS) Impact of Climate Extremes on Terrestrial Ecosystems
61
International Conference on Phenology Impact of Climate Extremes on Phenology
Besides, our results highlighted the significant role of native vegetations,
particularly hummock grassland (spinifex) and shrubland (e.g., Acacia shrubland, or Mulga), in buffering the impacts of drought on regional carbon balance and subsequent feedback to
regional and global climate.
Xuanlong Ma [email protected]
Trends in Environmental Research Series (TIERS) 8 April 2015
6262
International Conference on Phenology Impact of Climate Extremes on Phenology
For example, the positive anomaly in global land carbon sink in 2010-11 was largely driven by semi-arid ecosystems in Southern Hemisphere, with 60% of global
carbon uptake anomaly was attributed to Australia’s drylands ecosystems (Poulter et al., 2014).
Xuanlong Ma [email protected]
Trends in Environmental Research Series (TIERS) 8 April 2015
6363
International Conference on Phenology Impact of Climate Extremes on Phenology
Summary
Xuanlong Ma [email protected]
Trends in Environmental Research Series (TIERS) Impact of Climate Extremes on Terrestrial Ecosystems
64
International Conference on Phenology Impact of Climate Extremes on Phenology
Summary
Xuanlong Ma [email protected]
Trends in Environmental Research Series (TIERS) Impact of Climate Extremes on Terrestrial Ecosystems
65
International Conference on Phenology Impact of Climate Extremes on Phenology
• We found dramatic impacts were exerted by drought and wet extremes on vegetation phenology & productivity, with abrupt change in phenology and productivity between dry and wet years.
• We found agricultural ecosystems did not buffer drought well, while native dryland ecosystems were quite resistant and resilient to hydroclimatic variations.
Summary
Xuanlong Ma [email protected]
Trends in Environmental Research Series (TIERS) Impact of Climate Extremes on Terrestrial Ecosystems
66
International Conference on Phenology Impact of Climate Extremes on Phenology
• We found dramatic impacts were exerted by drought and wet extremes on vegetation phenology & productivity, with abrupt change in phenology and productivity between dry and wet years.
• We found agricultural ecosystems did not buffer drought well, while native dryland ecosystems were quite resistant and resilient to hydroclimatic variations.
Thanks! Questions?
Xuanlong Ma [email protected]
Trend in Environment ResearchTrends in Environmental Research Series (TIERS) Impact of Climate Extremes on Terrestrial Ecosystems
67
International Conference on Phenology Impact of Climate Extremes on Phenology
Murray-Darling National ParkPhoto Credit: Ignacio Palacios/Lonely Planet