BELMANIP_00140








Location

lon / lat [deg]: 12.7904 / -0.3649

Source network: BELMANIP







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]:

34.54

Distance to urban areas [km]:

47.78



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

1.78415450991

Rcv

0.683073117105

Rse

0.0

Rst

-0.000560986124933

Rsv

-0.997834616739



Height range @ 1km [m]

31

Height range @ 2km [m]

67

Height range @ 5km [m]

185

Height range @ 10km [m]

-999

Height range @ 20km [m]

-999



Variance slope @ 1 km

240

Variance slope @ 2 km

460

Variance slope @ 5 km

909

Variance slope @ 10 km

-999

Variance slope @ 20 km

-999







NDVI (max. NDVI composite)


Roman et al. (2009) index


St

2.14833917842

Rcv

0.0382474019182

Rse

0.0

Rst

-0.358180691738

Rsv

-0.999999449134



NDVI range @ 1km [-]

0.0

NDVI range @ 2km [-]

0.02

NDVI range @ 5km [-]

0.04

NDVI range @ 10km [-]

0.06

NDVI range @ 20km [-]

0.05



Variance slope @ 1 km

1.89923013867e-05

Variance slope @ 2 km

2.07541202529e-05

Variance slope @ 5 km

1.7971828101e-05

Variance slope @ 10 km

1.40700555552e-05

Variance slope @ 20 km

7.641948694e-06







NDVI (min. NDVI composite)I


Roman et al. (2009) index


St

nan

Rcv

0.445585088162

Rse

nan

Rst

nan

Rsv

16.4362620042



NDVI range @ 1km [-]

0.01

NDVI range @ 2km [-]

0.02

NDVI range @ 5km [-]

0.04

NDVI range @ 10km [-]

0.05

NDVI range @ 20km [-]

0.05



NDVI slope @ 1 km

2.47925122189e-05

NDVI slope @ 2 km

2.60829849775e-05

NDVI slope @ 5 km

1.89537639909e-05

NDVI slope @ 10 km

1.10729936174e-05

NDVI slope @ 20 km

4.66048301624e-06







Temporal stability analysis

+000 deg (BHR)




BHR statistics

Temporal stability [1/decade]:



abs

rel


Weighted least square:

-0.0284449994948






Ordinary least square:

-0.00923543292968










Probabilities that GCOS criteria is met:

Weighted least square:

3.5 %

Ordinary least square:

4.4 %





DHR statistics

Temporal stability [1/decade]:



abs

rel


Weighted least square:

-0.0272297679642






Ordinary least square:

-0.00762694332713










Probabilities that GCOS criteria is met:

Weighted least square:

3.4 %

Ordinary least square:

4.4 %





+057/+063 deg (BHR)




BHR statistics

Temporal stability [1/decade]:



abs

rel


Weighted least square:

0.0740200972036






Ordinary least square:

-0.0206097941147










Probabilities that GCOS criteria is met:

Weighted least square:

2.2 %

Ordinary least square:

4.6 %





DHR statistics

Temporal stability [1/decade]:



abs

rel


Weighted least square:

0.075085341985






Ordinary least square:

-0.0264433845036










Probabilities that GCOS criteria is met:

Weighted least square:

2.5 %

Ordinary least square:

4.6 %







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