KONGO_00002







Location

lon / lat [deg]: 20.718 / -0.757

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]:

20.02

Distance to urban areas [km]:

53.98



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 [%]:

99.0



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 [%]:

99.0



Radius: 20 km

Number of landcover classes:

3

Dominant landcover type:

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

Fraction of dominant landcover type [%]:

86.0





Disturbances







Heterogeneity analysis

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

Topography



Roman et al. (2009) index


St

0.00107069697491

Rcv

0.629365948673

Rse

0.0

Rst

2.17315860033e-05

Rsv

2801.28382427



Height range @ 1km [m]

2

Height range @ 2km [m]

5

Height range @ 5km [m]

14

Height range @ 10km [m]

-999

Height range @ 20km [m]

-999



Variance slope @ 1 km

1

Variance slope @ 2 km

2

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

2.23171829712e-07

Rcv

0.00430599858847

Rse

0.0

Rst

0.479425331111

Rsv

13442556.3294



NDVI range @ 1km [-]

0.01

NDVI range @ 2km [-]

0.02

NDVI range @ 5km [-]

0.03

NDVI range @ 10km [-]

0.03

NDVI range @ 20km [-]

0.04



Variance slope @ 1 km

1.04144621173e-05

Variance slope @ 2 km

1.22517309339e-05

Variance slope @ 5 km

1.12244836709e-05

Variance slope @ 10 km

8.774778575e-06

Variance slope @ 20 km

4.23248096334e-06







NDVI (min. NDVI composite)I


Roman et al. (2009) index


St

5.49913572278

Rcv

0.0517395781326

Rse

0.0

Rst

-0.0583223405334

Rsv

0.435478353703



NDVI range @ 1km [-]

0.01

NDVI range @ 2km [-]

0.03

NDVI range @ 5km [-]

0.03

NDVI range @ 10km [-]

0.03

NDVI range @ 20km [-]

0.04



NDVI slope @ 1 km

9.8089737965e-06

NDVI slope @ 2 km

1.17744200219e-05

NDVI slope @ 5 km

1.06620027163e-05

NDVI slope @ 10 km

7.44323697065e-06

NDVI slope @ 20 km

4.91450844885e-06







Temporal stability analysis

+000 deg (BHR)




BHR statistics

Temporal stability [1/decade]:


abs

rel


Weighted least square:

-0.0102407039189






Ordinary least square:

-0.00535699476622










Probabilities that GCOS criteria is met:

Weighted least square:

2.5 %

Ordinary least square:

4.1 %





DHR statistics

Temporal stability [1/decade]:


abs

rel


Weighted least square:

-0.0108838151245






Ordinary least square:

-0.00706106678966










Probabilities that GCOS criteria is met:

Weighted least square:

2.4 %

Ordinary least square:

3.6 %





+057/+063 deg (BHR)




BHR statistics

Temporal stability [1/decade]:


abs

rel


Weighted least square:

-0.000727462482905






Ordinary least square:

-0.0396563974585










Probabilities that GCOS criteria is met:

Weighted least square:

6.0 %

Ordinary least square:

4.4 %





DHR statistics

Temporal stability [1/decade]:


abs

rel


Weighted least square:

-0.00436819259847






Ordinary least square:

-0.0481638930349










Probabilities that GCOS criteria is met:

Weighted least square:

4.8 %

Ordinary least square:

4.4 %







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