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F. Javier García-Haro (UV: University of Valencia, Spain) With contributions from Fernando Camacho (EOLAB), Beatriz Martínez (UV) Other contributors: Isabel Monteiro, Julia Stoyanova, K. Guan The LSA SAF vegetation products and applications: drought monitoring EUMeTrain Event Week 2014: Droughts, Floods and Landslides 1-5 December 2014

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F. Javier García-Haro (UV: University of Valencia, Spain)

With contributions from Fernando Camacho (EOLAB), Beatriz Martínez (UV)Other contributors: Isabel Monteiro, Julia Stoyanova, K. Guan

The LSA SAF vegetation products and applications: drought monitoring

EUMeTrain Event Week 2014: Droughts, Floods and Landslides 1-5 December 2014

INDEX

LSA SAF vegetation products

Expert knowledge: advantages and limitations

Some applications

Derivation of phenological information

Response of vegetation to rainfall deficit

Near real time detection/monitoring of drought related disturbances

3

LSA SAF VEGA SEVIRI daily products

Example: 15 April 2007

Euro

NAfr

SAfr

SAme

http://landsat.meteo.pt

LAIFVC FAPARSEVIRI “VEGA”: daily products

landsaf.ipma.pt

4

VEGA: Daily (MDVEGA) and 10-day (MTVEGA)

10-day VEGA (MTVEGA) based on AL3 (time scale of 30-day)

Daily and 10-day are spatially and temporally consistent

• Fraction of ‘ green’ Vegetation Cover (FVC)⇒ Probabilistic Spectral Mixture Analysis

( )0

0ln)0(

1a

FVCaGb

LAIs

−⋅

Ω⋅=⋅−

Algorithms description

V1

V2

V3

S1

S2

S3

Banda 1

∑=

= N

i iij

KKjjK

MMrp

MMrprMp

1)()|(

)()|()|(

π

π

×

Mixed pixel, Rj

2 components (veg,soil): R = Rv fv + Rs fs

Each component: mixture of gaussians

∑=

ΣjG

kjkjkkk

1),(µφτ

Bayesian Theory

• ‘True’ Leaf Area Index (LAI)Pragmatic approach of Roujean and Lacaze, (2002) based on a modified Beer’s law:

b=0.97, G=0.5, clumping (Ω) from a GLC-2000 lookup table (Chen et al. 2005). 5

• ’Daily’ Fraction of Absorbed PAR (FAPAR)Statistical relationship established between a vegetation index (RDVI) in anoptimal geometry and daily integrated FAPAR by using RT simulations withPROSPECT+SAIL model (Roujean and Breon, 1995).

FAPAR=1.81*(RDVI)opt - 0.21

Minimum dispersion FAPAR-RDVI was found in the Principal Plane, VZA=45ºand SZA=60º.

Algorithms description

RNIRRNIRDVINDVIRDVI+−

=⋅= 2/1)(

Ropt(λ)= k0(λ) - 0.240*k1(λ) + 0.202*k2(λ)

6

Error k0 Error k2

Sources of uncertainty: input errors

• BRDF parameters (Roujean et al,. 1992)k0 (RED, NIR, SWIR) for FVC LAIk0,k1,k2 (RED,NIR) for FAPAR

Introduction

7

See related documents (PUM, VR)

Product content: QF information

8

Error Map (Sept’05-Sept’07) FVC v2.1

9

EuropeError Map consistency between products

10

Mean values over 2007Quality and coverage

0%

10%

20%

30%

40%

50%

60%

70%

80%

90%

100%

% O

f Dat

a

2007

0115

2007

0215

2007

0315

2007

0415

2007

0515

2007

0615

2007

0715

2007

0815

2007

0915

2007

1015

2007

1115

2007

1215

FVC -Euro-

Unprocessed

Bad Input

Snow Traces

Snow

Poor

Medium-Low

Optimal

0%

10%

20%

30%

40%

50%

60%

70%

80%

90%

100%

% O

f Dat

a

2007

0115

2007

0215

2007

0315

2007

0415

2007

0515

2007

0615

2007

0715

2007

0815

2007

0915

2007

1015

2007

1115

2007

1215

FVC - N_Africa

Unprocessed

Bad Input

Snow Traces

Snow

Poor

Medium-Low

Optimal

0%

10%

20%

30%

40%

50%

60%

70%

80%

90%

100%

% O

f Dat

a

2007

0115

2007

0215

2007

0315

2007

0415

2007

0515

2007

0615

2007

0715

2007

0815

2007

0915

2007

1015

2007

1115

2007

1215

FVC - S_America

Unprocessed

Bad Input

Snow Traces

Snow

Poor

Medium-Low

Optimal

0%

20%

40%

60%

80%

100%

% O

f Dat

a

2007

0115

2007

0215

2007

0315

2007

0415

2007

0515

2007

0615

2007

0715

2007

0815

2007

0915

2007

1015

2007

1115

2007

1215

FVC - S_Africa

Unprocessed

Bad Input

Snow Traces

Snow

Poor

Medium-Low

Optimal

11

Quality and coverage

Percentage of gaps over 1 year of data

Optimal: Err(FVC)<0.10Medium: 0.10<Err(FVC)<0.15Low: 0.15<Err(FVC)<0.20Unusable Err(FVC)>0.20

12

Product Validation

MonguPandamatenga

Maun Okwa River Tshane

0,0

0,5

1,0

1,5

2,0

2,5

Mongu Panda. Maun Okwa Tshane

MSG

TRAC

ACCUPAR

LAI

0,0

0,1

0,2

0,3

0,4

0,5

0,6

0,7

Mongu Panda. Maun Okw a Tshane

MSG

TRAC

FVC

FVC/LAI SAfr

13

14

Product validation Comparison with VGT4SAFRICA FVC

14

Quality monitoring Consistency LSASAF and Copernicus Global Land

Quality monitoring Consistency LSASAF and Copernicus Global Land

Quality monitoring Consistency LSASAF and Copernicus Global Land

Quality monitoring Consistency LSASAF and Copernicus Global Land

Quality monitoring Consistency LSASAF and Copernicus Global Land

Quality monitoring Consistency LSASAF and Copernicus Global Land

Quality monitoring Consistency LSASAF and Copernicus Global Land

2006 2007 2008 2009 2010 2011 2012 20130

1

2

3

4

5

6

DOY

LAI

SudOuest

LAI MSGMOD15A2LAI BIOPARIN SITU

Quality monitoring Temporal consistency

2006 2007 2008 2009 2010 2011 2012 20130

1

2

3

4

5

6

DOY

LAI

Mongu

LAI MSGMOD15A2LAI BIOPARIN SITU

Identified artefacts

Input (BRDF K0)

Artefacts during late winter 2011 at some specific locations in the four SEVIRI regions. Caused by a sharp decrease in the BRDF bands, unadressed by quality flag

LAI

Documented in Updated Validation Report

Quality monitoring

24

25

Strips in FVC and LAI at some periods of year 2010 Assigned an erroneous value of 0 Unaddressed by quality flag

Documented in Updated Validation ReportThis justifies the reprocessing (foreseen for March 2015)

Iberian Peninsula

Madagascar

Identified artefactsQuality monitoring

Canopy Water Content (CWC)

Products under develpment

Gross PrimaryProductivity (GPP)

Global FVC, LAI, FAPAR from AVHRR/Metop

Sequence of products over a 50-day period, S_Africa (0º S, 11.2º E – 8.3ºS, 23.2ºE).

INDIRECT VALIDATIONMODIS LAI Land-SAF LAI

The temporal continuity and stability of LAI MSG product clearly outperforms that of MODIS product.

Added value with regard to similar products Expert knowledge

27

Reconstruction of seasonal curves

False second-season False second-seasonFalse second-season

Potential applications

Ja Fe Ma Ap Ma Jun Jul Au Se

Start of growing season 2007

Africa is a consolidated region: no gaps, temporal continuity, improving the capabilities of polar orbiters to characterise the phenology

Deriving phenologic attributes Potential applications

Seasonal metrics Base level, amplitude,

phase indicators of productivity,

and timing. More reliable than

(MODIS, VGT) derived

30by Isabel Monteiro (EUMETRAIN)

Guan, K., E. F. Wood, D. Medvigy, K. K. Caylor, S. Li and S. J. Jeong, (2013), Derive vegetation phenological time and structure information over Africa using SEVIRI daily LAI, IEEE transactions on Geoscience and Remote Sensing, 52:1113-1130.

Deriving phenologic attributes Potential applications

SEVERE DROUGHT OVER EAST AFRICA: 10 million people afected (state of emergency)

Drought monitoring

LAI

by Isabel Monteiro (EUMETRAIN: Monitoring Vegetation from space)http://www.satreponline.org/landsaf/

Potential applications

31

32•From Julia Stoyanova (Bulgarian National Institute of Meteorology and Hydrology)

Drought monitoring from LSA SAF products

33

Meterological data

Moisture index

Extremely drySeverely dryModerately drySlightly drySlightly wetModerately wetVery wetExtremely wet

Extremely drySeverely dryModerately drySlightly drySlightly wetModerately wetVery wetExtremely wet

SPI

AFRICA 10-day rainfall estimates (RFE 2.0) for Africa from the NOAA Climate Prediction

Center (NOAA/CPC) at a spatial resolution of 8-km monthly and 3-montly accumulated

SPAIN Monthly P,T records from all AEMET (Spanish Agency of Meteorology) stations. Images of climatic variables were interpolated (2-km) Thornthwaite Moisture index ⇒ climatic classification Standardised Precipitation index (SPI-i) at i-month scales (i=1,3,6,12)

Drought Applications

Impact of 2004-06 drought in SpainFEEDBACKS CLIMATE-VEGETATION

FVC anomaly (June’05) vs SPI-3 (March-May)

FVC shows large deviation for certains classes/periods in water-limited areas

Shrub, herbaceous and broadleaved are very sensitive to drought

Extremely drySeverely dryModerately drySlightly drySlightly wetModerately wetVery wetExtremely wet

Extremely drySeverely dryModerately drySlightly drySlightly wetModerately wetVery wetExtremely wet

SPI-12 (August’04 – July’05)

0 100 200 3000

0.2

0.4

0.6

0.8

Herbaceous

Day of Year

FVC

0 100 200 3000

0.2

0.4

0.6

0.8

Broadleaved Forest

Day of Year

FVC

Spatial distributionINTERRELATION CLIMATE-VEGETATION

Climatic Type Moisture IndexA Very humid ≥ 100 B4 Humid 80 to100B3 Humid 60 to 80B2 Humid 40 to 60B1 Humid 20 to 40C2 Moist subhumid 0 to 20C1 Dry subhumid -20 to 0

D Semiarid -40 to -20E Arid -60 to -40

0

0.2

0.4

0.6

0.8

1

FVC

Climatic Type

E D C1

C2 B1

B2

B3

B4 A

2096 24912 67968 23776 11072 5840 4928 5904 10432

relationships between water availability and vegetation coverage in Spain

Vulnerability of natural ecosystemsFEEDBACKS CLIMATE-VEGETATION

0

0.1

0.2

0.3

0.4

0.5

0.6

0.7

0.8

0.9

R2 (FV

C -

SPI)

Climatic Type

E D C1

C2 B1

B2

B3

B4 A

2096 24816 67744 23616 11056 5840 4864 5840 10320

R2 of Dummy-Variable Model between SPI (1 month lagged) and FVC anomaly during April-August

Strong relationships during March-June in dry regions ⇒ water stress limits vegetation growth

37

Vegetation response to climatic variability Potential applications

Sahelian semi-arid environments

tttt RandomStationalTrendY ++=

Model

Modeling the dynamics of vegetation Season-trend parametric model:

Example: Time series of SEVIRI FVC

Residual

Automated monitoring of vegetation disturbance

( )∑=

+++=3

110 sin)(

kkk kwtAtaatFVC ϕ

APPLICATIONS: Real time detection (drought, fire): Retrospectively monitoring of disturbances

Extent, severity, duration (start, period of recovery)

y

t YYtresidstd

σ

ˆ)(_

−=

Example: Disturbance measure

39

Automated monitoring of vegetation disturbance

Example: Drought in Somalia (2011)

FVC/MSG time series Savanna, 2 growing seasons

SEVIRI Capabilities (VEGA) High frequency and continuity Normal season-trend can be

usually captured from a single year

⇒ VEGA is specially suited for very rapid detection (e.g. < 1 month)

40

Drought monitoring Potential applications

Severe drought in Horn of Africa (2011): Shortage of rain in the two rainy seasons (autumn and spring)

41

Drought monitoring Horn of Africa (2011)

42

Drought monitoring Horn of Africa (2011)

43

Drought monitoring Horn of Africa (2011)

44

Drought monitoring Horn of Africa (2011)

45

Drought monitoring Horn of Africa (2011)

46

Drought monitoring Horn of Africa (2011)

47

Drought monitoring Horn of Africa (2011)

48

Drought monitoring Horn of Africa (2011)

49

Drought monitoring Horn of Africa (2011)

50

Drought monitoring Horn of Africa (2011)

51

Drought monitoring Horn of Africa (2011)

52

Drought monitoring Horn of Africa (2011)

53

Drought monitoring Horn of Africa (2011)

54

Drought monitoring Horn of Africa (2011)

55

Drought monitoring Horn of Africa (2011)

56

Drought monitoring Horn of Africa (2011)

57

Drought monitoring Horn of Africa (2011)

58

Drought monitoring Horn of Africa (2011)

59

Drought monitoring Horn of Africa (2011)

60

Drought monitoring Horn of Africa (2011)

61

Drought monitoring Horn of Africa (2011)

A similar example Drought in 2006

62

Drought monitoring Southern Europe

63

Drought monitoring Southern Europe

64

Drought monitoring

Central Europe (May, 2006)

Southern Europe

65

Drought monitoring Southern Europe

66

Drought monitoring

Eastern Europe (summer, 2007)

Southern Europe

67

Drought monitoring Southern Europe

68

Drought monitoring Southern Europe

69

Drought monitoring Southern Europe

70

Drought monitoring

Iberian Peninsula (spring, 2009)

Southern Europe

71

Drought monitoring Southern Europe

72

Drought monitoring Southern Europe

73

Drought monitoring Southern Europe

74

Drought monitoring

Mediterranean countries (spring, 2012)

Southern Europe

75

Drought monitoring

Mediterranean countries (spring, 2012)

Southern Europe

76

Drought monitoring

Mediterranean countries (spring, 2012)

Southern Europe

Summary

Vegetation estimates from satellite A complete integrator of the physical variables (moisture condition) closely related to rainfall dynamics in water limited ecosystems

LSA SAF VEGA products (FVC, LAI, FAPAR) spatial and temporally consistent indicators of vegetation structure and condition over wide FVC time series are suited for near real time drought monitoring Use of several LSA SAF products (ET, LST, FVC, FAPAR) to monitoring initiation of water stress and propagation of drought

Contact [email protected]