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Comparison of L and P band radar time series for the monitoring of Sahelian area P.-L. Frison, G. Mercier, E. Mougin, P. Hiernaux
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Comparison of L and P band radar time series for the monitoring of Sahelian area

Jan 20, 2016

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Silva Silva

Comparison of L and P band radar time series for the monitoring of Sahelian area. P.-L. Frison, G. Mercier, E. Mougin, P. Hiernaux. Context : Better understanding Sahelian surface processes and their interaction with monsoon variability - PowerPoint PPT Presentation
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Page 1: Comparison of L and P band radar time series for the monitoring of Sahelian area

Comparison of L and P band radar time series for the monitoring of Sahelian area

P.-L. Frison, G. Mercier, E. Mougin, P. Hiernaux

Page 2: Comparison of L and P band radar time series for the monitoring of Sahelian area

Context:• Better understanding Sahelian surface processes and their interaction with monsoon variability

• Improve our understanding and documentation of long term trend in vegetation in response to climate change

• radar data: 2 key parameters: soil moisture and vegetation

Goal:• Comparison of L band PALSAR and C band ASAR data

for Sahelian surface monitoring. Relation between radar vs surface parameter temporal evolution

Page 3: Comparison of L and P band radar time series for the monitoring of Sahelian area

Outline:

• Study site

• PALSAR and ASAR data

• change detection method

• Results and discussion

Page 4: Comparison of L and P band radar time series for the monitoring of Sahelian area

The Sahel

Semi-arid area

herbaceous layer (0-50 %) (annual grasses)

Dry season (Nov. – Apr.)

bare soil

Rainy season (May – Oct.)

shrub (0-20 %)

trees (1-5 %)+

Page 5: Comparison of L and P band radar time series for the monitoring of Sahelian area

Region of study: the Gourma - Mali

Seno

Page 6: Comparison of L and P band radar time series for the monitoring of Sahelian area

PALSAR acquisitions: L band (Jan. 2007 - Apr. 2009)

DATASET

Mode # Polarization Resolution Incidence angle

Pass

Fine Beam 7 HH 15 m 40° Ascending

Fine Beam 5 HH / HV 15 m 40° Ascending

Wide Swath 6 HH 100 m 30° Descending

ASAR acquisitions: C band (Jul. - Dec. 2005)

Mode # Polarization Resolution Incidence angle

Pass

Wide Swath 41 HH 150 m 18-35° Ascending+

Descending

Page 7: Comparison of L and P band radar time series for the monitoring of Sahelian area

Gourma Region (MALI)ASAR –Wide Swath - HH

20th Dec 2005

Page 8: Comparison of L and P band radar time series for the monitoring of Sahelian area

GOURMA Region (MALI)PALSAR–WIDE BEAM- HH

1st Jan 2008

Page 9: Comparison of L and P band radar time series for the monitoring of Sahelian area

Gourma Region (MALI)ASARC-band

PALSARL-band

C-band (ASAR):Shallow sand and silt soils

L -band (PALSAR):Better discrimination of geological features

Remnant of alluvial systems and lacustrine depressions

Page 10: Comparison of L and P band radar time series for the monitoring of Sahelian area

Gourma Region (MALI)ASARC-band

PALSARL-band

C-band (ASAR):Shallow sand and silt soils

L -band (PALSAR):Better discrimination of geological features

Remnant of alluvial systems and lacustrine depressions

Page 11: Comparison of L and P band radar time series for the monitoring of Sahelian area

PALSAR Fine Beam – HH polarizationTemporal color composite image

GOURMA - MALI17 Jan. 200720 Oct. 200722 Jan.2009

Water ponds

Hombori mounts

Low-land (accacia forest)

Page 12: Comparison of L and P band radar time series for the monitoring of Sahelian area

Change detection method

Constraints:

Large dynamic range (high differences over bright patterns)

Even after multi-looking, presence of noise (speckle)

absolute or relative differences, ratios, rms,….. not

significant

Time series color composite image Relative differences

Page 13: Comparison of L and P band radar time series for the monitoring of Sahelian area

Temporally stable regions gray

Change detection colored areas

Case of 3 channels

Change detection method

Constraints:

Large dynamic range (high differences over bright patterns)

Even after multi-looking, presence of noise (speckle)

absolute or relative differences, ratio, rms,….. not

significant

Page 14: Comparison of L and P band radar time series for the monitoring of Sahelian area

Temporally stable areas gray areas (no saturation)

Change detection colored areas (saturation)

RGB space R

B

G0

HSV space

Case of 3 channels

Value

Saturation

Hue

Change detection method

Constraints:

Large dynamic range (high differences over bright patterns)

Even after multi-looking, presence of noise (speckle)

absolute or relative differences, ratio, rms,….. not

significant

Page 15: Comparison of L and P band radar time series for the monitoring of Sahelian area

17 Jan. 200720 Oct. 200722 Jan.2009

RGB Space

Page 16: Comparison of L and P band radar time series for the monitoring of Sahelian area

Value

Hue

Saturation

HSV Space

Areas that have changed

Page 17: Comparison of L and P band radar time series for the monitoring of Sahelian area

Color composite image Saturation image

17 Jan. 200720 Oct. 200722 Jan.2009

Change detection for a 3-date color composite image

PALSAR Fine BeamHH polarization

Page 18: Comparison of L and P band radar time series for the monitoring of Sahelian area

Change detection method

Case of N channels (N>3):

P iterations:

1) random draw of 3 among the N available

channels

2) Compute the saturation channel from HSV

space

Average of the P saturation channels

Example: 12 Finebeam acquisitions at HH pol.

N=12 12! / (9! * 3!) = 220 possible random

draws

P =50 (arbitrary)

Page 19: Comparison of L and P band radar time series for the monitoring of Sahelian area

Color composite image Saturation image

17 Jan. 200720 Oct. 200722 Jan.2009

Change detection for a 3-date color composite image

PALSAR Fine BeamHH polarization

Page 20: Comparison of L and P band radar time series for the monitoring of Sahelian area

Color composite image Saturation image

Change detection for 12 FineBeam acquisitions (HH polarization)

17 Jan. 200720 Oct. 200722 Jan.2009

PALSAR Fine BeamHH polarization

Jan. 2007 – Apr. 2009

Page 21: Comparison of L and P band radar time series for the monitoring of Sahelian area

Temporal changes detected over 12 Fine Beam acquisitions

PALSAR dataHH polarisationJan. 2007 – Mar. 2009

Water ponds

Fields (millet) dep. Orientation!

Significant penetration depth over sandy soils

Page 22: Comparison of L and P band radar time series for the monitoring of Sahelian area

Changes in dry seasonChanges in rainy season

Temporal changes detected over 12 Fine Beam acquisitions

Water pondspermanent

PALSAR dataHH polarisationJan. 2007 – Mar. 2009

Fields (millet) dep. Orientation!

Page 23: Comparison of L and P band radar time series for the monitoring of Sahelian area

ALOS/PALSAR – FBD6th June 2008

HH HV

Sandy soils

Shallow soils

INFLUENCE OF POLARISATION

Page 24: Comparison of L and P band radar time series for the monitoring of Sahelian area

Change detection between HH and HV

PALSAR DUAL POLARIZATION

Shallow soils+

Water ponds

Page 25: Comparison of L and P band radar time series for the monitoring of Sahelian area

ALOS/PALSAR – WB1: HH Polarization

Water ponds discrimination

2008 dry season:1 Jan16 Feb2 Apr

3-date color composite image

Page 26: Comparison of L and P band radar time series for the monitoring of Sahelian area

Change detection (dry season)

ALOS/PALSAR – WB1: HH Polarization

Water ponds discrimination

• Main water resource • Hydrological indicator

surface runoffareas increase since begining of drought

period (50’s)

Page 27: Comparison of L and P band radar time series for the monitoring of Sahelian area

ASAR –Wide Swath – HH polarisation

41 acquisitions22 acquisitions in ascending pass

5 acquisitions same incidence angle (35°) – Jul. –Dec. 2005

Page 28: Comparison of L and P band radar time series for the monitoring of Sahelian area

ASAR –Wide Swath - HH polarisation

2nd Sept. 2005 change detection (5 dates)

low penetration over sandy soil upper surface changes

sandy soils

Page 29: Comparison of L and P band radar time series for the monitoring of Sahelian area

ASAR –Wide Swath - HH polarisation

2nd Sept. 2005 change detection (5 dates)

low penetration over sandy soil upper surface changes

sandy soils, water ponds

Page 30: Comparison of L and P band radar time series for the monitoring of Sahelian area

change detection (5 dates)PALSAR (L-band)

low penetration over sandy soil upper surface changes

sandy soils, water ponds

High penetration dpeth over sandy soilswater ponds millet fields

Comparison P band / L band temporal change detection

Page 31: Comparison of L and P band radar time series for the monitoring of Sahelian area

Conclusion

• RGB HSV simple but performant for change detection!

• Temporal change detection: penetration depth illustration

histogram must be the same across the hole image!

C band (low penetration over sandy soils)

mix of upper surface changessandy soils (soil moisture + vegetation)water ponds

more difficult te discriminate special features

• L band: some variation over sandy soils (soil moisture?) Cross over with SMOS mission

L band (high penetration over sandy soils)Water pondsMillet fields

Page 32: Comparison of L and P band radar time series for the monitoring of Sahelian area

Thank you for your attention!