BELMANIP_00154








Location

lon / lat [deg]: 13.1937 / 2.4092

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]:

55.71

Distance to urban areas [km]:

none in region



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

1.91570978469

Rcv

0.56630847118

Rse

0.0

Rst

-0.000174667383738

Rsv

-0.999516066522



Height range @ 1km [m]

11

Height range @ 2km [m]

22

Height range @ 5km [m]

53

Height range @ 10km [m]

-999

Height range @ 20km [m]

-999



Variance slope @ 1 km

11

Variance slope @ 2 km

23

Variance slope @ 5 km

56

Variance slope @ 10 km

-999

Variance slope @ 20 km

-999







NDVI (max. NDVI composite)


Roman et al. (2009) index


St

nan

Rcv

nan

Rse

nan

Rst

nan

Rsv

nan



NDVI range @ 1km [-]

0.01

NDVI range @ 2km [-]

0.02

NDVI range @ 5km [-]

0.03

NDVI range @ 10km [-]

0.04

NDVI range @ 20km [-]

0.04



Variance slope @ 1 km

1.18463764093e-05

Variance slope @ 2 km

1.31780993004e-05

Variance slope @ 5 km

9.27601135133e-06

Variance slope @ 10 km

7.1326474248e-06

Variance slope @ 20 km

5.21949917287e-06







NDVI (min. NDVI composite)I


Roman et al. (2009) index


St

nan

Rcv

nan

Rse

nan

Rst

nan

Rsv

nan



NDVI range @ 1km [-]

0.04

NDVI range @ 2km [-]

0.04

NDVI range @ 5km [-]

0.05

NDVI range @ 10km [-]

0.06

NDVI range @ 20km [-]

0.07



NDVI slope @ 1 km

2.85023823018e-05

NDVI slope @ 2 km

2.84292572759e-05

NDVI slope @ 5 km

1.86799195236e-05

NDVI slope @ 10 km

1.36362265094e-05

NDVI slope @ 20 km

1.21346906252e-05







Temporal stability analysis

+000 deg (BHR)




BHR statistics

Temporal stability [1/decade]:



abs

rel


Weighted least square:

-0.0115425589621






Ordinary least square:

-0.00779839901156










Probabilities that GCOS criteria is met:

Weighted least square:

3.2 %

Ordinary least square:

4.3 %





DHR statistics

Temporal stability [1/decade]:



abs

rel


Weighted least square:

-0.00971203101068






Ordinary least square:

-0.00546033843697










Probabilities that GCOS criteria is met:

Weighted least square:

2.9 %

Ordinary least square:

4.5 %





+057/+063 deg (BHR)




BHR statistics

Temporal stability [1/decade]:



abs

rel


Weighted least square:

-0.0212687061771






Ordinary least square:

-0.0146961363631










Probabilities that GCOS criteria is met:

Weighted least square:

4.2 %

Ordinary least square:

4.7 %





DHR statistics

Temporal stability [1/decade]:



abs

rel


Weighted least square:

-0.0198579494083






Ordinary least square:

-0.0122204869625










Probabilities that GCOS criteria is met:

Weighted least square:

4.2 %

Ordinary least square:

4.7 %







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






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