EO-1 Hyperion Spectral Time Series - NASA...EO-1 Hyperion Spectral Time Series for assessment of...

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EO-1 Hyperion Spectral Time Series for assessment of ecosystem function

Petya K. E. Campbell1, 2

K. Fred Huemmrich1, 2 , Elizabeth M. Middleton1

and Sarah Voorhies 2

1 NASA/Goddard Space Flight Center, USA2 University of Maryland Baltimore County

Hotspots of bio-diversityhttp://www.plants2020.net/about-the-gspc

EO-1 Acquisitions Since Launch

>85,000 (2000 through May 2016)

Repeated Collections at: CEOS calibration sites (blue triangles), FLUX sites (green

triangles), NEON (white circles) and Volcanoes (purple diamonds)

EO-1 Hyperion Spectral Time Series

FLUX site locations and number of

Hyperion cloud free images

EO-1 Spectral Time Series at FLUX Sites

Seasonal Spectral Changes

0

0.05

0.1

0.15

0.2

0.25

0.3

0.35

0.4

0.45

0.5

42

7

51

8

61

0

70

2

79

3

88

5

98

3

10

74

11

65

12

55

13

46

14

37

15

28

16

19

17

10

18

00

18

91

19

82

20

73

21

63

22

54

23

45

Re

fle

cta

nc

e

Wavelength (nm)

Harvard Forest, Deciduous2001248

2002251

2002260

2002363

2003014

2008128

2008146

2008192

2008120

2008338

2013094

2013136

00.05

0.10.15

0.20.25

0.30.35

0.40.45

0.5R

efl

ec

tan

ce

Acquisition date (YearDOY)

Stable - Sand Pith

641 549 651 844

1003 1679 2204

Changes in the chemical and physical configuration of vegetation canopies are expressed as changes in the contiguous spectral signatures.

Green et al. 2012

Data and Processing

• Gross Primary Production (GPP = GEP, µmol m-2 s-1) • Ecosystem Respiration (Re) -calculated from relationships between

nighttime Net Ecosystem Exchange (NEE) and air temperature• Net Ecosystem Production -> from the observed GEE and Re

GEE = gross ecosystems exchangeNEP = GEE – ReNEE = -NEP

FLUX Site, Location Harvard Forest, MA, USA Park Falls, WI, USA Skukuza, South Africa

Climate Temperate Temperate Arid, Steppe, Hot

Vegetation type

Northern Hardwoods: EMS

Evergreen: Eastern

hemlock

Deciduous Broadleaf

MixedGrassland Savannah

Tower height (m)US-Ha1 and US-Ha2

30 m

US-Pfa

30 m, 122 m, 396 m

ZA-Kru

30 m

Hyperion images 12 (2001-2013) 47 (2008-2014) 72 (2008-2014)

Sites

GEE

maps

Date (mm/dd/yy)

GEE

, Te

mp

era

ture

& H

um

idit

y

OSA

VI

Hyperion Time Series at Skukuza

Midday GEP estimated using a partial least squares regression

Average Hyperion spectral reflectance for Skukuza (black) and the coefficients derived

from PLSR vs. GEP (red)

FD

FWHM

FA

Changes in Vegetation Reflectance and Spectral Features, Skukuza

Chlorophyll

Water absorption

2008-2014 (76) Wavelength (nm)

Chlorophyll Feature (PRISM) and GEE

Narrow-band VIs and GEE

Seasonal Variation in GEE and Spectral VIs (G31), Skukuza

-15 5(μmol m-2 s-1, estimates based on FD)

GEE at Skukuza, Based on FD

Skukuza, Hyperion VIs, Regression Coefficients (R2)

-5

0

5

10

15

20

25

0

1

2

3

4

5

6

0 50 100 150 200 250 300 350

NEP

(CO

mo

lm-2

s-1),

Pre

cip

itat

ion

(cm

)

G3

2 =

(R

75

0-R

44

5)/

((R

70

0-R

44

5)

G32 CO2 flux Precipitation

Spectral bio-indicator associated with chlorophyll content best captured the CO2

dynamics related to vegetation phenology. Required multitemporal data set.

Corresponding Spectral and NEP Phenology

Day of Year

A. Dry season (DOY 214)B. Wet season (DOY 22)

Mongu : Campbell et al. 2013

• The results indicate a strong correlation between CO2 flux

parameters and Hyperion's spectral parameters associated with

chlorophyll and photosynthetic function.

• The spectral parameters associated with photosynthetic

dynamics across all sites require continuous spectra.

– In the conifer forests chlorophyll levels do not change as significantly as in

the deciduous forest. In the hemlock forest (Ha 2: HL) phenology was

traceable with the PRI3 SBI, when in the deciduous canopies (Ha1: EMS,

Park Falls and Skukuza) derivative and feature depth SBIs performed

better.

• The approach requires a diverse spectral coverage

representative of the seasonal dynamics in vegetation function.

This study provides a step toward a common (global) hyperspectral

strategy to monitor the vegetation ability to uptake CO2.

Conclusions

Locations with >10 Hyperion Acquisitions

Spectral Parameters and LUE, Skukuza