BOUMBA_BEK








Location

lon / lat [deg]: 14.612 / 3.095

Source network: ALBEDOVAL2







Geostationary surface albedo (GSA) data


“+000”


“+057/+063”


Landcover information (based on ESA CCI landcover data)


Landcover fractions @ 2km distance


Landcover fractions @ 20 km distance




Legend



Distance to open water bodies [km]:

71.65

Distance to urban areas [km]:

65.35



Radius: 1 km

Number of landcover classes:

1

Dominant landcover type:

50: Tree cover, broadleaved, evergreen, closed to open (>15%)

Fraction of dominant landcover type [%]:

100.0



Radius: 2 km

Number of landcover classes:

1

Dominant landcover type:

50: Tree cover, broadleaved, evergreen, closed to open (>15%)

Fraction of dominant landcover type [%]:

100.0



Radius: 5 km

Number of landcover classes:

1

Dominant landcover type:

50: Tree cover, broadleaved, evergreen, closed to open (>15%)

Fraction of dominant landcover type [%]:

100.0



Radius: 10 km

Number of landcover classes:

1

Dominant landcover type:

50: Tree cover, broadleaved, evergreen, closed to open (>15%)

Fraction of dominant landcover type [%]:

100.0



Radius: 20 km

Number of landcover classes:

1

Dominant landcover type:

50: Tree cover, broadleaved, evergreen, closed to open (>15%)

Fraction of dominant landcover type [%]:

100.0





Disturbances









Heterogeneity analysis

The heterogeneity analysis provides information about the spatial and temporal heterogeneity of the site.

Topography



Roman et al. (2009) index


St

1.9847611854

Rcv

0.512438746758

Rse

0.0

Rst

-6.56236895421e-06

Rsv

-0.999071553494



Height range @ 1km [m]

3

Height range @ 2km [m]

7

Height range @ 5km [m]

15

Height range @ 10km [m]

-999

Height range @ 20km [m]

-999



Variance slope @ 1 km

0

Variance slope @ 2 km

1

Variance slope @ 5 km

4

Variance slope @ 10 km

-999

Variance slope @ 20 km

-999







NDVI (max. NDVI composite)


Roman et al. (2009) index


St

7.38829250101e-07

Rcv

0.300981882299

Rse

0.0

Rst

0.117489931279

Rsv

4060477.69551



NDVI range @ 1km [-]

0.01

NDVI range @ 2km [-]

0.01

NDVI range @ 5km [-]

0.03

NDVI range @ 10km [-]

0.03

NDVI range @ 20km [-]

0.04



Variance slope @ 1 km

7.18767867017e-06

Variance slope @ 2 km

8.68527556037e-06

Variance slope @ 5 km

7.65873382201e-06

Variance slope @ 10 km

5.44117060022e-06

Variance slope @ 20 km

5.46318198295e-06







NDVI (min. NDVI composite)I


Roman et al. (2009) index


St

1.95360148135

Rcv

0.404565897608

Rse

0.0

Rst

-0.131059694055

Rsv

-0.999999779548



NDVI range @ 1km [-]

0.02

NDVI range @ 2km [-]

0.03

NDVI range @ 5km [-]

0.04

NDVI range @ 10km [-]

0.05

NDVI range @ 20km [-]

0.06



NDVI slope @ 1 km

2.53646138344e-05

NDVI slope @ 2 km

2.77549954454e-05

NDVI slope @ 5 km

2.20101437258e-05

NDVI slope @ 10 km

1.42989584473e-05

NDVI slope @ 20 km

9.76782329643e-06







Temporal stability analysis

+000 deg (BHR)




BHR statistics

Temporal stability [1/decade]:



abs

rel


Weighted least square:

-0.00958808060119






Ordinary least square:

-0.00696158051892










Probabilities that GCOS criteria is met:

Weighted least square:

2.9 %

Ordinary least square:

4.2 %





DHR statistics

Temporal stability [1/decade]:



abs

rel


Weighted least square:

-0.00461375651346






Ordinary least square:

-0.00936198440614










Probabilities that GCOS criteria is met:

Weighted least square:

3.7 %

Ordinary least square:

3.7 %





+057/+063 deg (BHR)




BHR statistics

Temporal stability [1/decade]:



abs

rel


Weighted least square:

0.0207531423243






Ordinary least square:

-0.0250964229044










Probabilities that GCOS criteria is met:

Weighted least square:

0.0 %

Ordinary least square:

4.6 %





DHR statistics

Temporal stability [1/decade]:



abs

rel


Weighted least square:

0.0278046463165






Ordinary least square:

-0.0322187862053










Probabilities that GCOS criteria is met:

Weighted least square:

0.0 %

Ordinary least square:

4.5 %







Temporal anomaly analyis

The variance of the temporal anomalies provides an additional measure about the stability of the signal AFTER removal of the mean seasonal cylce.

+000 deg


+057/+063 deg