Evaluation of MODIS GPP product and scaling up GPP over Northern Australian savannas Kasturi Devi...
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Transcript of Evaluation of MODIS GPP product and scaling up GPP over Northern Australian savannas Kasturi Devi...
Evaluation of MODIS GPP product and scaling up GPP
over Northern Australian savannas
Kasturi Devi KanniahJason Beringer Lindsay Hutley
Nigel TapperXuan Zhu
Objectives
• To validate different versions/collections of MODIS GPP (MOD17) -Collections 4.5, 4.8 and 5
• To validate input parameters used to estimate MODIS
GPP - LAI/fPAR (MOD 15A2), Light Use Efficiency and
meteorological variables (VPD, PAR)
• To estimate GPP using MOD17 algorithm with site
specific values
Howard Springs• Open woodland savannas forest
50-60% canopy cover.
• Over storey - evergreen trees
• Under storey - by C4 grasses
• Wet season GPP 7-8 g C m-2 day-1
• Dry season GPP– 0.3 to 1.6 g C m-2 day-1
Wet season(Dec-Mac)
Dry season (May-Sept)
MODIS GPP
Tmin & VPD scalar
Light UseEfficiency
APAR
GPPMOD17A
Max. LUE
fPAR
PAR
NASA DAO/GMAO
BCG model
MOD15A2
NASA DAO/GMAO
Global product, 1 km, 8 day Only useful if its relative accuracy can be determined
MODIS Collections
Input parameters
Col. 4.5 Col. 4.8 Col.5
fPAR Col.4 Col.4 Col.5
Met (PAR, VPD, Temp)
DAO GMAO GMAO
Maximum light use efficiency (g C MJ-1)
0.80 1.03 1.03
Period 2000-2003
2000-2006
2000- present
Seasonal GPP pattern• Correct seasonal pattern
• GPP Col. 4.5 & 5 < 4.8
• Col 4.8- good agreement
with tower in the wet
(RPE 1%, IOA 0.72,
RMSE 1 g C m-2 day-1 &
explained 75% variation
in tower GPP.
• Poor performance in the
dry (RPE 31%, RMSE
1.4, IOA 0.59, R2 0.33)
•Col. 4.5 good in the dry (RPE 4%, RMSE 1, IOA 0.72 R2 0.35), but poor
in the wet (RPE -14%, RMSE 1.53, IOA 0.63 and R2 0.46)•Col. 5 underestimated by ~40% in the wet and +10% in the dry
LAI/fPAR
• Wet season –MODIS ~3.8 vs.
site 2.2
• Dry season LAI -MODIS 1.3
vs. site 0.9
• Wet- MODIS fPAR 0.90 vs. site fPAR 0.67
• Dry- MODIS 0.67 vs. site 0.35
• ~correct LAI & fPAR in Col. 5
• Rapid increase in fPAR from September
Meteorology
Underestimation of PAR in the wet season-RPE 9% in DAO & 11% in GMAOIn the dry- underestimation of 5-6%Underestimation of VPD scalar in DAO- 4%, but negligible in GMAOIn the dry- underestimation 11% in DAO & 17% in GMAO
Maximum LUE
• LUE= GPP/APAR
• Site specific max = 1.26
g C MJ-1
• 17% higher than
standard MODIS
algorithm value of 1.03
gCMJ-1 in col. 4.8
• 35% higher than col.
4.5 (0.80 gCMJ-1)
Source of error
Wet -13%Dry -12%
Wet -7%Dry -15%
Wet 35%Dry 106%
Test 1- MODIS LUETest 2- MODIS meteorologyTest 3- MODIS fPAR
Algorithm improvements
GPP was recalculated using MOD17 algorithm but with
site specific values
GPP was recalculated using MOD17 algorithm with VPD scalar was replaced with soil moisture index.
– Evaporative Fraction= LE/(LE+H) from flux tower
– EF - indicator of soil or vegetation moisture conditions
because decreasing amounts of energy partitioned into
latent heat flux suggests a stronger moisture limitation
Improved methods• Improved methods
captured the start of the wet season correctly- used correct fPAR
• Method with VPD still overestimates GPP in the dry season
• Method with EF accurately reduce GPP in the dry season & captured the beginning of the wet season.
Overall these methods reduced RPE by ~50%, RMSE by 42%, increased IOA by 6% compared to Col. 4.8 and explained >90% variation in tower GPP
Conclusion• MODIS - reasonable estimation of GPP (<12%) - annual basis and
perfect in the wet in Col. 4.8 (1%) and in the dry in Col. 4.5 (4%).
• Main source of error in MODIS- fPAR, and use of VPD as a surrogate
for soil water deficit in the dry season
• Overestimation in fPAR was compensated by relatively low PAR,
VPD scalar and LUE in the wet season.
• In the dry season, VPD scalar & PAR was underestimated, but high
fPAR resulted in the overestimation of GPP
• Col. 5 fPAR accurate but low PAR &LUE- underestimated GPP- LUT
need to be readjusted
• Use of VPD in MOD17 has limitation-arid & semi arid areas
Future work
• Validation at other locations
• Analyse the spatial & temporal patterns of GPP over NT
using MOD 4.5 & 4.8
• Estimate GPP using fPAR from collection 5 & other site
specific values